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中文摘要：
通过选取武夷山土壤垂直带中的7个代表性剖面（其中一个在黄坑，六个在黄岗山，），初步研究武夷山的土壤理化性质的垂直变化规律。用发生学的方法对土壤进行分类命名。通过实验测得指标数据表明：武夷山土壤理化性质不同，垂直地带性差异显著。通过与山东丘陵山地土壤对比，分析成土因素对土壤的影响，说明不同的情况下，成土因素对土壤形成过程的主导性不同。
英文摘要：
Through selecting 7 representative sections of Wuyi Mountain soil （ one of which was in Huang Keng, six in Huang Gang hilly ） , a preliminary study on vertical changes of physical and chemical properties from soil in Wuyi Mountain was carried out . Soil was named with the method of occurrence study. Through the experimental data, the results declared that： There were different soil physical and chemical properties in Wuyi Mountain and the distinction of its vertical bands was significant among the marked areas. Through comparing with the soil from Shandong hilly, the effects of soil factors on different soil were analyzed, the dominant of soil factors on soil formation was different.
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