{"title":"印度古吉拉特邦天然气中的惰性气体和氮","authors":"S.V.S. Murty","doi":"10.1016/0168-9622(92)90015-3","DOIUrl":null,"url":null,"abstract":"<div><p>Isotopic and elemental ratios have been measured in three natural gas samples from Gujarat, India. The <sup>3</sup>He/<sup>4</sup>He ratio is radiogenic for Kalol-<em>166</em> and Kalol-<em>183</em>, while a mantle component is clearly indicated for Motwan-<em>2</em>. Although Ne is atmospheric in these Kalol gases, for Motwan-<em>2</em>, a clear excess <sup>21</sup>Ne due to <sup>18</sup>O(α,n)<sup>21</sup>Ne is present. All three gases have radiogenic <sup>40</sup>Ar and air values for <sup>36</sup>Ar/<sup>36</sup>Ar. Krypton is atmospheric in composition for all three gases. Xenon in Kalol-<em>183</em> is purely atmospheric, but for Kalol-<em>166</em> a pure fission Xe from <sup>238</sup>U is also present. Xenon from Motwan-<em>2</em>, on the other hand, shows excess <sup>129</sup>Xe, <sup>131</sup>Xe, <sup>132</sup>Xe, <sup>134</sup>Xe and <sup>136</sup>Xe which do not match either <sup>238</sup>U or <sup>244</sup>Pu fission yields. The higher yields of <sup>131</sup>Xe and <sup>132</sup>Xe are most likely a result of preferential migration or leaching of their radioactive precursors from their host rock. But the <sup>129</sup>Xe excess could not be due to such preferential effects, and represents a mantle component. Both <sup>3</sup>He and <sup>129</sup>Xe excesses can be accounted for by the presence of ∼20% mantle component.</p><p>The <em>δ</em><sup>15</sup>N-values for the three gases Kalol-<em>166</em>, Kalol-<em>183</em>, and Motwan-2 are (in ‰) +9.27, −12.56 and −11.48, respectively. They indicate a sedimentary source combined with effects due to migration.</p></div>","PeriodicalId":100231,"journal":{"name":"Chemical Geology: Isotope Geoscience section","volume":"94 3","pages":"Pages 229-240"},"PeriodicalIF":0.0000,"publicationDate":"1992-03-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0168-9622(92)90015-3","citationCount":"2","resultStr":"{\"title\":\"Noble gases and nitrogen in natural gases from Gujarat, India\",\"authors\":\"S.V.S. Murty\",\"doi\":\"10.1016/0168-9622(92)90015-3\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Isotopic and elemental ratios have been measured in three natural gas samples from Gujarat, India. The <sup>3</sup>He/<sup>4</sup>He ratio is radiogenic for Kalol-<em>166</em> and Kalol-<em>183</em>, while a mantle component is clearly indicated for Motwan-<em>2</em>. Although Ne is atmospheric in these Kalol gases, for Motwan-<em>2</em>, a clear excess <sup>21</sup>Ne due to <sup>18</sup>O(α,n)<sup>21</sup>Ne is present. All three gases have radiogenic <sup>40</sup>Ar and air values for <sup>36</sup>Ar/<sup>36</sup>Ar. Krypton is atmospheric in composition for all three gases. Xenon in Kalol-<em>183</em> is purely atmospheric, but for Kalol-<em>166</em> a pure fission Xe from <sup>238</sup>U is also present. Xenon from Motwan-<em>2</em>, on the other hand, shows excess <sup>129</sup>Xe, <sup>131</sup>Xe, <sup>132</sup>Xe, <sup>134</sup>Xe and <sup>136</sup>Xe which do not match either <sup>238</sup>U or <sup>244</sup>Pu fission yields. The higher yields of <sup>131</sup>Xe and <sup>132</sup>Xe are most likely a result of preferential migration or leaching of their radioactive precursors from their host rock. But the <sup>129</sup>Xe excess could not be due to such preferential effects, and represents a mantle component. Both <sup>3</sup>He and <sup>129</sup>Xe excesses can be accounted for by the presence of ∼20% mantle component.</p><p>The <em>δ</em><sup>15</sup>N-values for the three gases Kalol-<em>166</em>, Kalol-<em>183</em>, and Motwan-2 are (in ‰) +9.27, −12.56 and −11.48, respectively. They indicate a sedimentary source combined with effects due to migration.</p></div>\",\"PeriodicalId\":100231,\"journal\":{\"name\":\"Chemical Geology: Isotope Geoscience section\",\"volume\":\"94 3\",\"pages\":\"Pages 229-240\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1992-03-05\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0168-9622(92)90015-3\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Chemical Geology: Isotope Geoscience section\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0168962292900153\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemical Geology: Isotope Geoscience section","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0168962292900153","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Noble gases and nitrogen in natural gases from Gujarat, India
Isotopic and elemental ratios have been measured in three natural gas samples from Gujarat, India. The 3He/4He ratio is radiogenic for Kalol-166 and Kalol-183, while a mantle component is clearly indicated for Motwan-2. Although Ne is atmospheric in these Kalol gases, for Motwan-2, a clear excess 21Ne due to 18O(α,n)21Ne is present. All three gases have radiogenic 40Ar and air values for 36Ar/36Ar. Krypton is atmospheric in composition for all three gases. Xenon in Kalol-183 is purely atmospheric, but for Kalol-166 a pure fission Xe from 238U is also present. Xenon from Motwan-2, on the other hand, shows excess 129Xe, 131Xe, 132Xe, 134Xe and 136Xe which do not match either 238U or 244Pu fission yields. The higher yields of 131Xe and 132Xe are most likely a result of preferential migration or leaching of their radioactive precursors from their host rock. But the 129Xe excess could not be due to such preferential effects, and represents a mantle component. Both 3He and 129Xe excesses can be accounted for by the presence of ∼20% mantle component.
The δ15N-values for the three gases Kalol-166, Kalol-183, and Motwan-2 are (in ‰) +9.27, −12.56 and −11.48, respectively. They indicate a sedimentary source combined with effects due to migration.