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本文介绍了自1987年5月开始观测以来,小汤山温泉溶解H_2、CH_4及电导率在地震活动期的变化特征,并对小汤山(以下统称为井)的映震能力进行了初步讨论。
This paper introduces the characteristics of dissolved H_2, CH_4 and conductivity during the seismic activity in Xiaotangshan Hot Spring since the beginning of observation in May 1987, and discusses the seismic reflection ability of Xiaotangshan (hereinafter collectively referred to as the well).