中山湖
中山湖
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结果表明,中山站地区土壤中的高岭石含量存在明显的空间分异,含量范围为26%~57%;而中山站地区奈拉湖不同时间的湖泊沉积物中高岭石含量范围则为5.8%~23.2%。
Kaolinite content in the soil samples ranges between 26 % and 57 % , showing clear spacial differentiation , while its content in the sediment of Lake Nella ranges between 5.8 % - 23.2 % , showing temporal differentiation in different layers .