印度古吉拉特邦天然气中的惰性气体和氮

S.V.S. Murty
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引用次数: 2

摘要

对来自印度古吉拉特邦的三个天然气样品进行了同位素和元素比的测量。Kalol-166和Kalol-183的3He/4He比值为放射性成因,而Motwan-2的地幔成分明显。虽然在这些卡洛尔气体中Ne是大气中的,但对于Motwan-2,由于18O(α,n)21Ne存在明显过量的21Ne。这三种气体都具有放射性的40Ar和36Ar/36Ar的空气值。氪是大气中所有三种气体的组成。卡洛尔-183中的氙纯粹是大气中的,但卡洛尔-166中也存在来自238U的纯裂变Xe。另一方面,motwang -2的氙显示出过量的129Xe、131Xe、132Xe、134Xe和136Xe,这与238U或244Pu的裂变产率都不匹配。131Xe和132Xe的较高产率很可能是它们的放射性前体从宿主岩石中优先迁移或浸出的结果。但129Xe的过量不可能是由于这种优先效应,而是代表了地幔成分。3He和129Xe的过量都可以用~ 20%地幔成分的存在来解释。Kalol-166、Kalol-183和Motwan-2气体的δ 15n值分别为±9.27、±12.56和±11.48。它们表明了沉积源与运移作用的结合。
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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.

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