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	<id>http://wikiet.gssi.it/index.php?action=history&amp;feed=atom&amp;title=Sardinia_candidate_site</id>
	<title>Sardinia candidate site - Revision history</title>
	<link rel="self" type="application/atom+xml" href="http://wikiet.gssi.it/index.php?action=history&amp;feed=atom&amp;title=Sardinia_candidate_site"/>
	<link rel="alternate" type="text/html" href="http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;action=history"/>
	<updated>2026-05-25T21:57:14Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
	<generator>MediaWiki 1.32.0</generator>
	<entry>
		<id>http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=460&amp;oldid=prev</id>
		<title>Jan.harms at 13:40, 12 July 2023</title>
		<link rel="alternate" type="text/html" href="http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=460&amp;oldid=prev"/>
		<updated>2023-07-12T13:40:15Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
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				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 13:40, 12 July 2023&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l17&quot; &gt;Line 17:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 17:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Sos Enattos mine has been known to be active since the Roman age, when the first shafts and tunnels were excavated. Relics of the infrastructures dating back to the Roman age were present at the mine until the 1960s, when the intensive exploitation of the site erased any trace of its past. Today, the Sos Enattos mine is no longer active and most of its tunnels closed but it is still manned for environmental safety. Sos Enattos is also part of the ''Parco geominerario storico ed ambientale della Sardegna'', devoted to preserve the memory of the mining past of Sardinia, also acknowledged by UNESCO.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Sos Enattos mine has been known to be active since the Roman age, when the first shafts and tunnels were excavated. Relics of the infrastructures dating back to the Roman age were present at the mine until the 1960s, when the intensive exploitation of the site erased any trace of its past. Today, the Sos Enattos mine is no longer active and most of its tunnels closed but it is still manned for environmental safety. Sos Enattos is also part of the ''Parco geominerario storico ed ambientale della Sardegna'', devoted to preserve the memory of the mining past of Sardinia, also acknowledged by UNESCO.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Since Sos Enattos was chosen as one of the candidate sites to host Einstein Telescope, the former mine has been the target of several measurement campaigns aimed at characterizing the geophysical characteristics of the site and to evaluate if they are compliant with the requirements of the Einstein Telescope design. For this purpose, four permanent seismic stations were deployed at the site with other temporary instruments devoted at characterizing the surrounding environment both on the surface and underground&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;. The last measurement campaign started in March 2019 and it is expected to last until early 2021. The results of the first year of this campaign are expected to be published by the end of 2020&lt;/del&gt;. Furthermore, since 2018, Sos Enattos &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;hosts &lt;/del&gt;SAR-GRAV, a laboratory for fundamental physics research in low ambient noise environments that also provides a research and development infrastructure for ET.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Since Sos Enattos was chosen as one of the candidate sites to host Einstein Telescope, the former mine has been the target of several measurement campaigns aimed at characterizing the geophysical characteristics of the site and to evaluate if they are compliant with the requirements of the Einstein Telescope design. For this purpose, four permanent seismic stations were deployed at the site with other temporary instruments devoted at characterizing the surrounding environment both on the surface and underground. Furthermore, since 2018, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the surface facilities of &lt;/ins&gt;Sos Enattos &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;host &lt;/ins&gt;SAR-GRAV, a laboratory for fundamental physics research in low ambient noise environments that also provides a research and development infrastructure for ET.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Seismic measurements ==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Seismic measurements ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Jan.harms</name></author>
		
	</entry>
	<entry>
		<id>http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=459&amp;oldid=prev</id>
		<title>Jan.harms at 13:37, 12 July 2023</title>
		<link rel="alternate" type="text/html" href="http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=459&amp;oldid=prev"/>
		<updated>2023-07-12T13:37:15Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 13:37, 12 July 2023&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l11&quot; &gt;Line 11:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 11:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:mappa_2.png|600px|thumb|right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos in Sardinia. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:mappa_2.png|600px|thumb|right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos in Sardinia. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sardinia is known for its low seismicity and population density, providing ideal conditions for the Einstein Telescope. In fact, as opposed to continental Italy and most of the Mediterranean basin, Sardinia does not possess any known active faults on land. Moreover, Sardinia is scarcely populated: the average population density of the region is about 70/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;, well below the Italian (195/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) and European (112/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) average. This guarantees a very low ambient seismic noise caused by human activities. For these reasons, in 2011 the Einstein Telescope science team identified the mine of Sos Enattos, located about 30 km &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;not&lt;/del&gt;-east of the city of Nuoro, as an opportunity to obtain a first assessment of the site quality with underground seismic measurements.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sardinia is known for its low seismicity and population density, providing ideal conditions for the Einstein Telescope. In fact, as opposed to continental Italy and most of the Mediterranean basin, Sardinia does not possess any known active faults on land. Moreover, Sardinia is scarcely populated: the average population density of the region is about 70/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;, well below the Italian (195/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) and European (112/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) average. This guarantees a very low ambient seismic noise caused by human activities. For these reasons, in 2011 the Einstein Telescope science team identified the mine of Sos Enattos, located about 30 km &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;north&lt;/ins&gt;-east of the city of Nuoro, as an opportunity to obtain a first assessment of the site quality with underground seismic measurements.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;A survey in seismic catalogues also confirms the very low seismicity of the site: between 1980 and 2020, only 51 events were recorded within 170 km from the mine. Of these events, only 10 were recorded at less than 50 km from Sos Enattos, all with a magnitude less than 2.5. Furthermore, the population density within 10 km from Sos Enattos is only about 13/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; and there are no major railways, highways, large industrial or agricultural plants in a range of tens of kilometers from the site. It is likely that anthropic noise at Sos Enattos is limited to very local activities which, to our knowledge, only include mine maintenance (vehicles driving at the site, lorries unloading their cargo, active water pumps, miners inspecting the site) and, possibly, farming activities in the nearby fields and pastures. All these activities can be controlled and would be interrupted when ET will become operational.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;A survey in seismic catalogues also confirms the very low seismicity of the site: between 1980 and 2020, only 51 events were recorded within 170 km from the mine. Of these events, only 10 were recorded at less than 50 km from Sos Enattos, all with a magnitude less than 2.5. Furthermore, the population density within 10 km from Sos Enattos is only about 13/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; and there are no major railways, highways, large industrial or agricultural plants in a range of tens of kilometers from the site. It is likely that anthropic noise at Sos Enattos is limited to very local activities which, to our knowledge, only include mine maintenance (vehicles driving at the site, lorries unloading their cargo, active water pumps, miners inspecting the site) and, possibly, farming activities in the nearby fields and pastures. All these activities can be controlled and would be interrupted when ET will become operational.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Jan.harms</name></author>
		
	</entry>
	<entry>
		<id>http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=458&amp;oldid=prev</id>
		<title>Jan.harms at 13:36, 12 July 2023</title>
		<link rel="alternate" type="text/html" href="http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=458&amp;oldid=prev"/>
		<updated>2023-07-12T13:36:44Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 13:36, 12 July 2023&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l11&quot; &gt;Line 11:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 11:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:mappa_2.png|600px|thumb|right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos in Sardinia. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:mappa_2.png|600px|thumb|right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos in Sardinia. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sardinia is known for its low seismicity and population density, providing ideal conditions for the Einstein Telescope. In fact, as opposed to continental Italy and most of the Mediterranean basin, Sardinia &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;has long been known to be seismically quiet without &lt;/del&gt;any known active faults. Moreover, Sardinia is scarcely populated: the average population density of the region is about 70/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;, well below the Italian (195/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) and European (112/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) average. This guarantees a very low &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;background &lt;/del&gt;seismic &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;ambient &lt;/del&gt;noise caused by human activities. For these reasons, in 2011 the Einstein Telescope science team identified the mine of Sos Enattos, located about 30 km not-east of the city of Nuoro, as &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;one &lt;/del&gt;of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;candidate sites to host Einstein Telescope&lt;/del&gt;.  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sardinia is known for its low seismicity and population density, providing ideal conditions for the Einstein Telescope. In fact, as opposed to continental Italy and most of the Mediterranean basin, Sardinia &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;does not possess &lt;/ins&gt;any known active faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;on land&lt;/ins&gt;. Moreover, Sardinia is scarcely populated: the average population density of the region is about 70/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;, well below the Italian (195/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) and European (112/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) average. This guarantees a very low &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;ambient &lt;/ins&gt;seismic noise caused by human activities. For these reasons, in 2011 the Einstein Telescope science team identified the mine of Sos Enattos, located about 30 km not-east of the city of Nuoro, as &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;an opportunity to obtain a first assessment &lt;/ins&gt;of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;site quality with underground seismic measurements&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;A survey in seismic catalogues also confirms the very low seismicity of the site: between 1980 and 2020, only 51 events were recorded within 170 km from the mine. Of these events, only 10 were recorded at less than 50 km from Sos Enattos, all with a magnitude less than 2.5. Furthermore, the population density within 10 km from Sos Enattos is only about 13/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; and there are no major railways, highways, large industrial or agricultural plants in a range of tens of kilometers from the site. It is likely that anthropic noise at Sos Enattos is limited to very local activities which, to our knowledge, only include mine maintenance (vehicles driving at the site, lorries unloading their cargo, active water pumps, miners inspecting the site) and, possibly, farming activities in the nearby fields and pastures. All these activities can be controlled and would be interrupted when ET will become operational.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;A survey in seismic catalogues also confirms the very low seismicity of the site: between 1980 and 2020, only 51 events were recorded within 170 km from the mine. Of these events, only 10 were recorded at less than 50 km from Sos Enattos, all with a magnitude less than 2.5. Furthermore, the population density within 10 km from Sos Enattos is only about 13/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; and there are no major railways, highways, large industrial or agricultural plants in a range of tens of kilometers from the site. It is likely that anthropic noise at Sos Enattos is limited to very local activities which, to our knowledge, only include mine maintenance (vehicles driving at the site, lorries unloading their cargo, active water pumps, miners inspecting the site) and, possibly, farming activities in the nearby fields and pastures. All these activities can be controlled and would be interrupted when ET will become operational.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Jan.harms</name></author>
		
	</entry>
	<entry>
		<id>http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=457&amp;oldid=prev</id>
		<title>Jan.harms at 13:30, 12 July 2023</title>
		<link rel="alternate" type="text/html" href="http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=457&amp;oldid=prev"/>
		<updated>2023-07-12T13:30:57Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 13:30, 12 July 2023&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l11&quot; &gt;Line 11:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 11:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:mappa_2.png|600px|thumb|right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos in Sardinia. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:mappa_2.png|600px|thumb|right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos in Sardinia. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sardinia is known for its &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;very &lt;/del&gt;low seismicity and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;low &lt;/del&gt;population density, providing &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;a suitable environment &lt;/del&gt;for &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;measurements in a stable low seismic noise environments as required by gravitational wave interferometers&lt;/del&gt;. In fact, as opposed to continental Italy and most of the Mediterranean basin, Sardinia has long been known to be seismically quiet &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;because it is not involved in present-day geodynamics&lt;/del&gt;. Moreover, Sardinia is scarcely populated: the average population density of the region is about 70/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;, well below the Italian (195/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) and European (112/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) average. This guarantees a very low background seismic ambient noise caused by human activities. For these reasons, in 2011 the Einstein Telescope science team identified the mine of Sos Enattos, located about 30 km not-east of the city of Nuoro, as one of the candidate sites to host Einstein Telescope.  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sardinia is known for its low seismicity and population density, providing &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;ideal conditions &lt;/ins&gt;for &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the Einstein Telescope&lt;/ins&gt;. In fact, as opposed to continental Italy and most of the Mediterranean basin, Sardinia has long been known to be seismically quiet &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;without any known active faults&lt;/ins&gt;. Moreover, Sardinia is scarcely populated: the average population density of the region is about 70/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;, well below the Italian (195/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) and European (112/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) average. This guarantees a very low background seismic ambient noise caused by human activities. For these reasons, in 2011 the Einstein Telescope science team identified the mine of Sos Enattos, located about 30 km not-east of the city of Nuoro, as one of the candidate sites to host Einstein Telescope.  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;A survey in seismic catalogues also confirms the very low seismicity of the site: between 1980 and 2020, only 51 events were recorded within 170 km from the mine. Of these events, only 10 were recorded at less than 50 km from Sos Enattos, all with a magnitude less than 2.5. Furthermore, the population density within 10 km from Sos Enattos is only about 13/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; and there are no major railways, highways, large industrial or agricultural plants in a range of tens of kilometers from the site. It is likely that anthropic noise at Sos Enattos is limited to very local activities which, to our knowledge, only include mine maintenance (vehicles driving at the site, lorries unloading their cargo, active water pumps, miners inspecting the site) and, possibly, farming activities in the nearby fields and pastures. All these activities can be controlled and would be interrupted when ET will become operational.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;A survey in seismic catalogues also confirms the very low seismicity of the site: between 1980 and 2020, only 51 events were recorded within 170 km from the mine. Of these events, only 10 were recorded at less than 50 km from Sos Enattos, all with a magnitude less than 2.5. Furthermore, the population density within 10 km from Sos Enattos is only about 13/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; and there are no major railways, highways, large industrial or agricultural plants in a range of tens of kilometers from the site. It is likely that anthropic noise at Sos Enattos is limited to very local activities which, to our knowledge, only include mine maintenance (vehicles driving at the site, lorries unloading their cargo, active water pumps, miners inspecting the site) and, possibly, farming activities in the nearby fields and pastures. All these activities can be controlled and would be interrupted when ET will become operational.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Jan.harms</name></author>
		
	</entry>
	<entry>
		<id>http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=456&amp;oldid=prev</id>
		<title>Jan.harms at 13:28, 12 July 2023</title>
		<link rel="alternate" type="text/html" href="http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=456&amp;oldid=prev"/>
		<updated>2023-07-12T13:28:56Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 13:28, 12 July 2023&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l11&quot; &gt;Line 11:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 11:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:mappa_2.png|600px|thumb|right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos in Sardinia. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:mappa_2.png|600px|thumb|right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos in Sardinia. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sardinia is known for its very low &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;seismic hazard &lt;/del&gt;and low population density, providing a suitable environment for measurements in a stable low seismic noise environments as required by gravitational wave interferometers. In fact, as opposed to continental Italy and most of the Mediterranean basin, Sardinia has long been known to be seismically quiet because it is not involved in present-day geodynamics. Moreover, Sardinia is scarcely populated: the average population density of the region is about 70/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;, well below the Italian (195/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) and European (112/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) average. This guarantees a very low background seismic ambient noise caused by human activities. For these reasons, in 2011 the Einstein Telescope science team identified the mine of Sos Enattos, located about 30 km not-east of the city of Nuoro, as one of the candidate sites to host Einstein Telescope.  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sardinia is known for its very low &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;seismicity &lt;/ins&gt;and low population density, providing a suitable environment for measurements in a stable low seismic noise environments as required by gravitational wave interferometers. In fact, as opposed to continental Italy and most of the Mediterranean basin, Sardinia has long been known to be seismically quiet because it is not involved in present-day geodynamics. Moreover, Sardinia is scarcely populated: the average population density of the region is about 70/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;, well below the Italian (195/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) and European (112/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) average. This guarantees a very low background seismic ambient noise caused by human activities. For these reasons, in 2011 the Einstein Telescope science team identified the mine of Sos Enattos, located about 30 km not-east of the city of Nuoro, as one of the candidate sites to host Einstein Telescope.  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;A survey in seismic catalogues also confirms the very low seismicity of the site: between 1980 and 2020, only 51 events were recorded within 170 km from the mine. Of these events, only 10 were recorded at less than 50 km from Sos Enattos, all with a magnitude less than 2.5. Furthermore, the population density within 10 km from Sos Enattos is only about 13/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; and there are no major railways, highways, large industrial or agricultural plants in a range of tens of kilometers from the site. It is likely that anthropic noise at Sos Enattos is limited to very local activities which, to our knowledge, only include mine maintenance (vehicles driving at the site, lorries unloading their cargo, active water pumps, miners inspecting the site) and, possibly, farming activities in the nearby fields and pastures. All these activities can be controlled and would be interrupted when ET will become operational.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;A survey in seismic catalogues also confirms the very low seismicity of the site: between 1980 and 2020, only 51 events were recorded within 170 km from the mine. Of these events, only 10 were recorded at less than 50 km from Sos Enattos, all with a magnitude less than 2.5. Furthermore, the population density within 10 km from Sos Enattos is only about 13/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; and there are no major railways, highways, large industrial or agricultural plants in a range of tens of kilometers from the site. It is likely that anthropic noise at Sos Enattos is limited to very local activities which, to our knowledge, only include mine maintenance (vehicles driving at the site, lorries unloading their cargo, active water pumps, miners inspecting the site) and, possibly, farming activities in the nearby fields and pastures. All these activities can be controlled and would be interrupted when ET will become operational.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Jan.harms</name></author>
		
	</entry>
	<entry>
		<id>http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=455&amp;oldid=prev</id>
		<title>Jan.harms at 13:28, 12 July 2023</title>
		<link rel="alternate" type="text/html" href="http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=455&amp;oldid=prev"/>
		<updated>2023-07-12T13:28:36Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 13:28, 12 July 2023&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l11&quot; &gt;Line 11:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 11:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:mappa_2.png|600px|thumb|right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos in Sardinia. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:mappa_2.png|600px|thumb|right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos in Sardinia. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;In the European context, &lt;/del&gt;Sardinia is known for its very low seismic hazard and low population density, providing a suitable environment for measurements in a stable low seismic noise environments as required by gravitational wave interferometers. In fact, as opposed to continental Italy and most of the Mediterranean basin, Sardinia has long been known to be seismically quiet because it is not involved in present-day geodynamics. Moreover, Sardinia is scarcely populated: the average population density of the region is about 70/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;, well below the Italian (195/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) and European (112/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) average. This guarantees a very low background seismic ambient noise caused by human activities. For these reasons, in 2011 the Einstein Telescope science team identified the mine of Sos Enattos, located about 30 km not-east of the city of Nuoro, as one of the candidate sites to host Einstein Telescope.  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sardinia is known for its very low seismic hazard and low population density, providing a suitable environment for measurements in a stable low seismic noise environments as required by gravitational wave interferometers. In fact, as opposed to continental Italy and most of the Mediterranean basin, Sardinia has long been known to be seismically quiet because it is not involved in present-day geodynamics. Moreover, Sardinia is scarcely populated: the average population density of the region is about 70/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;, well below the Italian (195/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) and European (112/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) average. This guarantees a very low background seismic ambient noise caused by human activities. For these reasons, in 2011 the Einstein Telescope science team identified the mine of Sos Enattos, located about 30 km not-east of the city of Nuoro, as one of the candidate sites to host Einstein Telescope.  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;A survey in seismic catalogues also confirms the very low seismicity of the site: between 1980 and 2020, only 51 events were recorded within 170 km from the mine. Of these events, only 10 were recorded at less than 50 km from Sos Enattos, all with a magnitude less than 2.5. Furthermore, the population density within 10 km from Sos Enattos is only about 13/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; and there are no major railways, highways, large industrial or agricultural plants in a range of tens of kilometers from the site. It is likely that anthropic noise at Sos Enattos is limited to very local activities which, to our knowledge, only include mine maintenance (vehicles driving at the site, lorries unloading their cargo, active water pumps, miners inspecting the site) and, possibly, farming activities in the nearby fields and pastures. All these activities can be controlled and would be interrupted when ET will become operational.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;A survey in seismic catalogues also confirms the very low seismicity of the site: between 1980 and 2020, only 51 events were recorded within 170 km from the mine. Of these events, only 10 were recorded at less than 50 km from Sos Enattos, all with a magnitude less than 2.5. Furthermore, the population density within 10 km from Sos Enattos is only about 13/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; and there are no major railways, highways, large industrial or agricultural plants in a range of tens of kilometers from the site. It is likely that anthropic noise at Sos Enattos is limited to very local activities which, to our knowledge, only include mine maintenance (vehicles driving at the site, lorries unloading their cargo, active water pumps, miners inspecting the site) and, possibly, farming activities in the nearby fields and pastures. All these activities can be controlled and would be interrupted when ET will become operational.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Jan.harms</name></author>
		
	</entry>
	<entry>
		<id>http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=411&amp;oldid=prev</id>
		<title>Jan.harms at 17:48, 11 July 2023</title>
		<link rel="alternate" type="text/html" href="http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=411&amp;oldid=prev"/>
		<updated>2023-07-11T17:48:19Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 17:48, 11 July 2023&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;In order to reach the ambitious low-frequency sensitivity goal of the Einstein Telescope, it is important to carry out a careful and detailed site characterization. On the basis of this analysis, a suitable site of the Einstein Telescope can be selected. As outlined in a recent paper [[https://doi.org/10.1063/5.0018414 Amann et al (2020)]], a site evaluation needs to consider the impact of site conditions on:&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Detector sensitivity&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Detector operation and duty cycle&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Infrastructure lifetime&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Site-quality preservation&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Construction cost&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Socio-economic impact of ET&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Site conditions include geological, hydrogeological, and geotechnical conditions and concerns the construction and lifetime of surface and underground infrastructure and societal aspects. There is a direct impact of environmental fields on the sensitivity of a detector. Magnetic fields can couple to magnetic parts of the seismic isolation and suspension system, seismic disturbances can directly couple with test masses through gravitational interaction, or causes noise when scattered light reflects from unisolated parts of the detector, which partially make it back into the main laser beam.&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:mappa_2.png|600px|thumb|right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos in Sardinia. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:mappa_2.png|600px|thumb|right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos in Sardinia. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Jan.harms</name></author>
		
	</entry>
	<entry>
		<id>http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=335&amp;oldid=prev</id>
		<title>Jan.harms at 18:50, 17 September 2020</title>
		<link rel="alternate" type="text/html" href="http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=335&amp;oldid=prev"/>
		<updated>2020-09-17T18:50:07Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 18:50, 17 September 2020&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;CalaGonone&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;jpg&lt;/del&gt;|thumb|&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Cala Gonone beach &lt;/del&gt;in Sardinia]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;mappa_2&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;png|600px&lt;/ins&gt;|thumb|&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;right|(Left) Location of Sos Enattos in Europe. (Center) Location of Sos Enattos &lt;/ins&gt;in Sardinia&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;. (Right) Placement of three of the four seismic stations at the mine. The fourth seismic station was installed in July 2020 and is not present in this map.&lt;/ins&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[[File:SosEnattos_-_1.jpg|300px|thumb|right|The mine as it appears today.]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;In the European context, Sardinia is known for its very low seismic hazard and low population density, providing a suitable environment for measurements in a stable low seismic noise environments as required by gravitational wave interferometers. In fact, as opposed to continental Italy and most of the Mediterranean basin, Sardinia has long been known to be seismically quiet because it is not involved in present-day geodynamics. Moreover, Sardinia is scarcely populated: the average population density of the region is about 70/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;, well below the Italian (195/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) and European (112/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;) average. This guarantees a very low background seismic ambient noise caused by human activities. For these reasons, in 2011 the Einstein Telescope science team identified the mine of Sos Enattos, located about 30 km not-east of the city of Nuoro, as one of the candidate sites to host Einstein Telescope. &lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;A &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;team &lt;/del&gt;of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;scientist &lt;/del&gt;from &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Italy &lt;/del&gt;and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;other European countries &lt;/del&gt;is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;carrying out measurements of environmental fields &lt;/del&gt;(&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;seismic&lt;/del&gt;, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;acoustic&lt;/del&gt;, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;magnetic&lt;/del&gt;) to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;assess &lt;/del&gt;the site&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;'s quality as a potential host &lt;/del&gt;of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;the future Einstein Telescope underground infrastructure&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;These measurements are accompanied by in-depth geotechnical, hydrogeological&lt;/del&gt;, .&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;.. studies&lt;/del&gt;, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;which are required &lt;/del&gt;to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;understand &lt;/del&gt;the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;feasibility&lt;/del&gt;, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cost&lt;/del&gt;, and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;impact &lt;/del&gt;of Einstein Telescope at &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;this &lt;/del&gt;site. The &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;GSSI group participates &lt;/del&gt;in &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;the acoustic &lt;/del&gt;and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;seismic characterization&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;GSSI is also involved in a socio-economic impact study &lt;/del&gt;of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Einstein Telescope at Sardinia through &lt;/del&gt;the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Social Sciences department&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;A &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;survey in seismic catalogues also confirms the very low seismicity &lt;/ins&gt;of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the site: between 1980 and 2020, only 51 events were recorded within 170 km &lt;/ins&gt;from &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the mine. Of these events, only 10 were recorded at less than 50 km from Sos Enattos, all with a magnitude less than 2.5. Furthermore, the population density within 10 km from Sos Enattos is only about 13/km&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; &lt;/ins&gt;and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;there are no major railways, highways, large industrial or agricultural plants in a range of tens of kilometers from the site. It is likely that anthropic noise at Sos Enattos &lt;/ins&gt;is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;limited to very local activities which, to our knowledge, only include mine maintenance &lt;/ins&gt;(&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;vehicles driving at the site, lorries unloading their cargo&lt;/ins&gt;, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;active water pumps&lt;/ins&gt;, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;miners inspecting the site&lt;/ins&gt;) &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;and, possibly, farming activities in the nearby fields and pastures. All these activities can be controlled and would be interrupted when ET will become operational.&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt; &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;The Sos Enattos mine has been known to be active since the Roman age, when the first shafts and tunnels were excavated. Relics of the infrastructures dating back &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the Roman age were present at the mine until the 1960s, when the intensive exploitation of &lt;/ins&gt;the site &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;erased any trace &lt;/ins&gt;of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;its past&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Today&lt;/ins&gt;, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the Sos Enattos mine is no longer active and most of its tunnels closed but it is still manned for environmental safety&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Sos Enattos is also part of the ''Parco geominerario storico ed ambientale della Sardegna''&lt;/ins&gt;, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;devoted &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;preserve &lt;/ins&gt;the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;memory of the mining past of Sardinia&lt;/ins&gt;, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;also acknowledged by UNESCO.&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt; &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Since Sos Enattos was chosen as one of the candidate sites to host Einstein Telescope&lt;/ins&gt;, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the former mine has been the target of several measurement campaigns aimed at characterizing the geophysical characteristics of the site &lt;/ins&gt;and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;to evaluate if they are compliant with the requirements &lt;/ins&gt;of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the &lt;/ins&gt;Einstein Telescope &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;design. For this purpose, four permanent seismic stations were deployed &lt;/ins&gt;at &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the &lt;/ins&gt;site &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;with other temporary instruments devoted at characterizing the surrounding environment both on the surface and underground&lt;/ins&gt;. The &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;last measurement campaign started &lt;/ins&gt;in &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;March 2019 &lt;/ins&gt;and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;it is expected to last until early 2021&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;The results &lt;/ins&gt;of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;first year of this campaign are expected to be published by &lt;/ins&gt;the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;end of 2020. Furthermore, since 2018, Sos Enattos hosts SAR-GRAV, a laboratory for fundamental physics research in low ambient noise environments that also provides a research and development infrastructure for ET&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Seismic measurements ==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Seismic measurements ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Jan.harms</name></author>
		
	</entry>
	<entry>
		<id>http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=233&amp;oldid=prev</id>
		<title>Jan.harms: /* Infrasound measurements */</title>
		<link rel="alternate" type="text/html" href="http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=233&amp;oldid=prev"/>
		<updated>2020-04-18T12:59:14Z</updated>

		<summary type="html">&lt;p&gt;‎&lt;span dir=&quot;auto&quot;&gt;&lt;span class=&quot;autocomment&quot;&gt;Infrasound measurements&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 12:59, 18 April 2020&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l10&quot; &gt;Line 10:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 10:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Infrasound measurements ==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Infrasound measurements ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;While atmospheric density fluctuations are predicted to couple weakly with an underground GW detector, this coupling strongly depends on the depth of the detector, and as long as the final choice of the detector depth is not made, gravitational noise from acoustic atmospheric fields must be considered as a potential sensitivity limitation. Important for this purpose is the study of two-point correlations of the acoustic field, which, together with the detector depth, determine how strongly acoustic fields couple gravitationally with the interferometer's test masses. &lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt; &lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The deployment of a microphone array is currently being planned. Since this experiment requires an outdoor deployment of microphones, it is important to provide a shield against weather, which includes the detrimental influence of wind on acoustic correlation measurements. Without wind shield, the local turbulence formed around each microphone leads to local pressure fluctuations, which are uncorrelated between sensors, and which can easily override the contribution of the acoustic field.&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Jan.harms</name></author>
		
	</entry>
	<entry>
		<id>http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=232&amp;oldid=prev</id>
		<title>Jan.harms at 12:51, 18 April 2020</title>
		<link rel="alternate" type="text/html" href="http://wikiet.gssi.it/index.php?title=Sardinia_candidate_site&amp;diff=232&amp;oldid=prev"/>
		<updated>2020-04-18T12:51:13Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
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				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 12:51, 18 April 2020&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l6&quot; &gt;Line 6:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 6:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Our group contributes a seismometer array to the Sardinia studies, which will allow us to characterize the seismic sources and seismic wavefield in detail especially for an accurate prediction of Newtonian noise from seismic fields.  &lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Our group contributes a seismometer array to the Sardinia studies, which will allow us to characterize the seismic sources and seismic wavefield in detail especially for an accurate prediction of Newtonian noise from seismic fields.  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Einstein Telescope group at University of Pisa has set up a server for data storage and Jupyter notebooks, which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;has provided first estimates of environmental noise of Einstein Telescope &lt;/del&gt;at &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Sardinia &lt;/del&gt;[[https://etrepo.df.unipi.it:8000/ Razzano et al (2019)]].&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The Einstein Telescope group at University of Pisa has set up a server for data storage and Jupyter notebooks, which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;is being used to process seismic data acquired &lt;/ins&gt;at &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the candidate site at the surface and underground &lt;/ins&gt;[[https://etrepo.df.unipi.it:8000/ Razzano et al (2019)]].&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Infrasound measurements ==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Infrasound measurements ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Jan.harms</name></author>
		
	</entry>
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