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Figure 3 Distribution of soil gas concentrations.
The soil gas samples were collected in Vacutainer® tubes.
Pressure gradients induced by stress change may cause a rapid migration of trapped soil gas.
A total soil gas volume of 16 ml was extracted per sampling time.
The laboratory analysis of one soil gas sample provided evidence of C2+ hydrocarbons (Table 1).
The decomposition of organic matter is an important source to soil gas CO2.
The soil gas samples were extracted and analysed by HPR-20 Mass Spectrometer (MS).
Analysis of radon concentration in soil gas along with meteorological parameters viz.
Therefore, the anomaly variation of soil gas concentrations induced by the earthquake is difficult to distinguish.
This pathway generation can also enhance v and cause a nonequilibrium condition of soil gas.
We have designed a soil gas probe with minimal internal dead volume to allow us to sample soil gas volumes of 45 cm3.
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