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地球内部可能存在的原位³H和³He源:对地球深部³He起源的另一种解释

A possible in situ 3H and 3He source in Earth's interior: an alternative explanation of origin of 3He in deep Earth.

作者信息

Jiang Songsheng, Liu Jing, He Ming

机构信息

China Institute of Atomic Energy, Beijing, China.

出版信息

Naturwissenschaften. 2010 Jul;97(7):655-62. doi: 10.1007/s00114-010-0681-z. Epub 2010 May 26.

Abstract

Origin of (3)He in the Earth is a mystery. Lacking a production mechanism, scientists assume (3)He was trapped in the Earth, when the Earth was formed. In contrast to this assumption, we have found (3)He and (3)H concentrations in excess of the atmospheric values in the deep waters of the volcanic Lakes Pavin (France), Laacher (Germany) and Nemrut (Turkey). This paper reports the result of finding (3)H in these three volcanic lakes that appear to originate from the mantle. Because (3)H has a half-life of 12.3 years, this (3)H and the resulting (3)He must have formed recently in the mantle and not be part of a primordial reservoir. The nuclear reactions that generate tritium might be a source of "missing" energy in the interior of the Earth.

摘要

地球中氦-3的起源是个谜。由于缺乏产生机制,科学家们推测,氦-3是在地球形成时被困在地球内部的。与这一假设相反,我们在法国的帕万火山湖、德国的拉赫湖和土耳其的内姆鲁特火山湖的深水中发现了高于大气值的氦-3和氚浓度。本文报告了在这三个似乎起源于地幔的火山湖中发现氚的结果。由于氚的半衰期为12.3年,这些氚以及由此产生的氦-3肯定是最近在地幔中形成的,而不是原始储库的一部分。产生氚的核反应可能是地球内部“缺失”能量的一个来源。

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