中山湖
中山湖-
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 .