一、柴达木盆地的盐渍土类型盆地的盐土分布相当广泛。它们主要是在灰钙土和荒漠土带的低地、沿湖边缘及局部地形低洼的地区,有时呈斑块状分布,但更多呈大面积的分布。根据熊毅先生的分类,盆地的盐渍土应属于:残积型——荒漠与荒漠草原盐渍区。盐分是由于地壳的上升运动或地下水的下降而遗留下来的,多系原生盐渍土。 First, the saline soil in the Qaidam Basin saline soil distribution is quite extensive. They are mainly in the lowland of calcareous soil and desert soil, along the edge of the lake and the local low-lying areas, sometimes patchy distribution, but more widely distributed. According to the classification of Mr. Xiong Yi, the saline soil in the basin should belong to: the residual type - desert and desert steppe salinization area. Salinity is due to the crustal ascending movement or the decline of groundwater, more than the Department of native saline soil.