摘要
通过对川东华蓥山区低山石灰岩槽谷土壤发育性质的研究，明确了这一区域的土壤基本类型为：均腐殖土纲的黑色石灰土类：铁硅铝土纲的黄色石灰土类，铁铝土纲的黄壤类．并进一步分析研究了土壤类型与其生境演替之间的关系．
Through the analysis of the characteristics of the development of soils, the study shows that there are three types of soils in the limestone trough valley, i. e. Rendzinqs, Yellow limestone soils and Yellow soils. It also demonstrates that the development of soils is largely related to their topographic position and vegetation, and meanwhile the environmental conditions have a great influ-ence upon the evolution of soils.
出处
《西南师范大学学报（自然科学版）》
CAS
CSCD
1994年第2期194-200,共7页
Journal of Southwest China Normal University(Natural Science Edition)
