Variations of He gas concentration are widely applied in studies devoted to the location of faults and to monitor seismic activities. Up to now, its migration mechanism in soil is not fully understood. A systematic soil gas survey across an active fault in NW Taiwan provides the opportunity to closely examine the mechanism of He migration in the fault zone. Significant spatial and temporal correlations observed between soil N(2) and He gas support the hypothesis that N(2) is the probable carrier gas for He emission in the studied area. Based on N(2)/Ar ratios and N(2) isotopic results, the excess soil N(2) in this study is considered to be largely derived from ancient atmospheric air which was dissolved in groundwater. Furthermore, observations rule out the possibility of CO(2) being the dominant carrier gas for He in the studied area based on the C and He isotopic compositions and the relationship between concentrations of these gases. At least two soil gas sources. A and B, can be identified in the studied area. Source A is an abiogenic gas source characterized by excess N(2) and He, and very low O(2) and CO(2) content. Source B, on the other hand, is a mixture of biogenic gas and atmospheric air. The development of the fault system is an important factor affecting the degree of mixture between sources A and B. Therefore, variations of soil gas composition, in particular those derived from source A, could be a useful proxy for tracing faults in the area. (C) 2010 Elsevier Ltd. All rights reserved.
