三个土壤剖面均有一定的漂洗和淀积粘化现象，但都不足以定义成漂白层或粘盘层。
Bleaching and characterization were morphologically apparent, but not well developed as to be defined as bleached or claying horizons.
野核桃林土壤在长期特定的生物、气候条件下，其腐殖化过程和钙积化过程明显，粘化过程较弱。
The humic process and calcific process are obvious in wild walnut forest soils, but it is weak in argillic process.
结果如下：1、贵阳市白云岩地区土层较薄，土壤主要由细砂和粉砂组成，没有出现粘化特征，土壤结构性较好。
Soil of dolomite areas in Guiyang is thin , soil component are mainly thick and thin sand , and there was not mucosity characteristic, soil structure is better.
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