The end-member identification by the intercorrelations between chemical and isotopic ratios shows three main sources, which are derived from weathering of limestone, dolomite and silicates.
对河水的化学计量分析表明河水化学组成受碳酸盐岩溶解控制，而碳酸盐岩主要受碳酸和硫酸作用而溶解。
The end-member identification by the intercorrelations between chemical and isotopic ratios shows three main sources, which are derived from weathering of limestone, dolomite and silicates.
对河水的化学计量分析表明河水化学组成受碳酸盐岩溶解控制，而碳酸盐岩主要受碳酸和硫酸作用而溶解。
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