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Position: Home > Articles > Research Advances in Fe-Mn Nodules in Soil in China Hubei Agricultural Sciences 2010,49 (6) 1488-1491

我国土壤铁锰结核研究进展

作  者:
唐健生;苏春田;单海平;邹胜章;陈宏峰
单  位:
中国地质大学水资源与环境学院;中国地质科学院岩溶地质研究所
关键词:
土壤;铁锰结核;研究进展
摘  要:
铁锰结核是土壤成土过程中的产物。我国近年来对土壤铁锰结核的物理性状、内部结构、元素的地球化学特征、锰矿物类型的鉴定进行了系统研究,并分析了其形成原因及形成时代,同时对铁锰结核所引起的土壤环境效应进行了初步研究。今后一段时期铁锰结核的主要研究方向是深化土壤铁锰结核形成机制、铁锰结核的空间比较性研究以及铁锰结核与土壤环境的相关性研究。
译  名:
Research Advances in Fe-Mn Nodules in Soil in China
作  者:
TANG Jian-sheng1,2,SU Chun-tian2,SHAN Hai-ping2,ZOU Sheng-zhang2,CHEN Hong-feng1,2 (1. College of Water Resources and Environment;China University of Geoscience ,Beijing 100083,China; 2. Institute of Karst Geology,CAGS,Guilin 541004,Guangxi,China)
关键词:
soil; Fe-Mn nodule; research advance
摘  要:
Fe-Mn nodules are the product of soil process. In recent years, soil experts have not only studied physical properties,internal structure,geochemical characteristics of elements and identification of Mn oxide minerals, but also analyzed the causes and time of formation. Preliminary study was also carried out on the environmental effects of soil by Fe-Mn nodules. The future researches on Fe-Mn nodules should be focused on the forming process, the comparative study of space and the relationship between Fe-Mn nodules and environment of soil.

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