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揭示了山地土壤形成的自然地理环境特点。分析了与辽阔堆积平原的异同点。阐述了山地土壤剖面的形成除成土过程本身的作用外,还有其它对地表产生作用的过程的影响。提出了把成土母质看成在构造上是非均质的疏松形成物的概念,其层理层次反映了山地地表发育的特定大地构造—生物气候周期。
Reveals the characteristics of natural geography environment formed by mountain soil. Analysis of the similarities and differences with the vast plains. In addition to the role of soil formation itself, there are other influences on the process of surface production. The concept of soil parent material is regarded as a loose formation that is structurally heterogeneous. The layering reflects the specific geotectonic-bioclimatic period of mountain surface development.