The membrane potential of shaly sand was influenced by the cation exchange capacity, hydrocarbon saturation and concentration difference of the contacted solutions.
研究结果表明，泥质砂岩薄膜电位与岩石阳离子交换容量、含油气饱和度、接触溶液浓度差密切相关。
In this situation, the chemical potential difference in the two solutions generates a voltage over each membrane.
在此情况下，两种溶液产生的化学电位差才会在每个交换膜上方形成电压。
In this situation, the chemical potential difference in the two solutions generates a voltage over each membrane.
在此情况下，两种溶液产生的化学电位差才会在每个交换膜上方形成电压。
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