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本文提出中国土壤地带分布的气候指标Ｒ＝ｅｘｐ（－０．０８Ｔ）［１－ｅｘｐ（－０．００５Ｐ）］；并根据中国６５９个站点气候资料（１９６－１９７０），给出了森林土壤系列和草原土壤系列的Ｒ值分布；得到了单独由气候因于决定的中国东部季风区气候土壤地带分布图，发现它与中国土壤图和中国土壤区划图在整体上有较好的一致性；讨论了它们差异的成因，分析了土壤带的演变趋势；然后给出了森林土壤垂直地带谱的计算公式，通过个例计算发现它与实际土壤垂直地带分布吻合得相当好；最后指出确定土壤带变化与气候变化滞后时间的可能性。
This paper presents the climatic index R = exp (-0.08T) [1-exp (-0.005P)] of the soil distribution in China. Based on the climatic data of 659 sites in China (196-1970), the forest soil series And the R value distribution of the grassland soil series. The climatic soil zone map of the eastern China monsoon region, which is determined solely by the climate, is obtained and found to be in good agreement with the Chinese soil map and the Chinese soil zoning map as a whole. The causes of their differences were analyzed and the evolution trend of the soil zone was analyzed. Then, the formula of the vertical spectrum of the soil in the forest was given, and it was found through calculation of individual cases that it was in good agreement with the vertical distribution of the soil. Finally, With the possibility of lag time in climate change.