<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Obase T</submitter><funding>MEXT Integrated Program for Next Generation Volcano Research and Human Resource Development</funding><pagination>17967</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC9678900</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>12(1)</volume><pubmed_abstract>We repeatedly measured isotopic compositions of noble gases and CO&lt;sub>2&lt;/sub> in volcanic gases sampled at six fumaroles around the Kusatsu-Shirane volcano (Japan) between 2014 and 2021 to detect variations reflecting recent volcanic activity. The synchronous increases in &lt;sup>3&lt;/sup>He/&lt;sup>4&lt;/sup>He at some fumaroles suggest an increase in magmatic gas supply since 2018. The increase in magmatic gas supply is also supported by the temporal variations in &lt;sup>3&lt;/sup>He/CO&lt;sub>2&lt;/sub> ratios and carbon isotopic ratios of CO&lt;sub>2&lt;/sub>. The &lt;sup>3&lt;/sup>He/&lt;sup>40&lt;/sup>Ar* ratios (&lt;sup>40&lt;/sup>Ar*: magmatic &lt;sup>40&lt;/sup>Ar) show significant increases in the period of high &lt;sup>3&lt;/sup>He/&lt;sup>4&lt;/sup>He ratios. The temporal variation in &lt;sup>3&lt;/sup>He/&lt;sup>40&lt;/sup>Ar* ratios may reflect chan</pubmed_abstract><journal>Scientific reports</journal><pubmed_title>Monitoring of magmatic-hydrothermal system by noble gas and carbon isotopic compositions of fumarolic gases.</pubmed_title><pmcid>PMC9678900</pmcid><funding_grant_id>JPJ005391</funding_grant_id><pubmed_authors>Sumino H</pubmed_authors><pubmed_authors>Kawana K</pubmed_authors><pubmed_authors>Yamane K</pubmed_authors><pubmed_authors>Yaguchi M</pubmed_authors><pubmed_authors>Obase T</pubmed_authors><pubmed_authors>Toyama K</pubmed_authors><pubmed_authors>Terada A</pubmed_authors><pubmed_authors>Ohba T</pubmed_authors></additional><is_claimable>false</is_claimable><name>Monitoring of magmatic-hydrothermal system by noble gas and carbon isotopic compositions of fumarolic gases.</name><description>We repeatedly measured isotopic compositions of noble gases and CO&lt;sub>2&lt;/sub> in volcanic gases sampled at six fumaroles around the Kusatsu-Shirane volcano (Japan) between 2014 and 2021 to detect variations reflecting recent volcanic activity. The synchronous increases in &lt;sup>3&lt;/sup>He/&lt;sup>4&lt;/sup>He at some fumaroles suggest an increase in magmatic gas supply since 2018. The increase in magmatic gas supply is also supported by the temporal variations in &lt;sup>3&lt;/sup>He/CO&lt;sub>2&lt;/sub> ratios and carbon isotopic ratios of CO&lt;sub>2&lt;/sub>. The &lt;sup>3&lt;/sup>He/&lt;sup>40&lt;/sup>Ar* ratios (&lt;sup>40&lt;/sup>Ar*: magmatic &lt;sup>40&lt;/sup>Ar) show significant increases in the period of high &lt;sup>3&lt;/sup>He/&lt;sup>4&lt;/sup>He ratios. The temporal variation in &lt;sup>3&lt;/sup>He/&lt;sup>40&lt;/sup>Ar* ratios may reflect chan</description><dates><release>2022-01-01T00:00:00Z</release><publication>2022 Nov</publication><modification>2025-04-19T00:36:10.376Z</modification><creation>2025-04-07T11:43:09.748Z</creation></dates><accession>S-EPMC9678900</accession><cross_references><pubmed>36411294</pubmed><doi>10.1038/s41598-022-22280-3</doi></cross_references></HashMap>