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测定分析了山西省关帝山林区山地灌丛植被上发育的土壤的理化性质，说明该土壤具有强烈的腐殖质累积过程，但不具斑纹特征，因此不属于我国暂行土壤分类中的山地草甸土，可称为灌丛腐殖质土。并对类似宜林地区的更新提出了建议。
The physical and chemical properties of the soil developed on the mountain shrub vegetation in Guandi Mountain of Shanxi Province were determined and analyzed. The results showed that the soil had a strong humus accumulation but no zebra pattern, so it did not belong to the mountain meadow soil in China’s tentative soil classification, Can be called brush humus soil. And made similar recommendations for the update of the Yilin region.