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侵蚀背景下湘中红壤丘陵区土地利用方式对土壤活性有机碳分布特征的影响研究
引用本文:李忠武,王曙光,陈晓琳,聂小东,张艳,刘桂平,曾婉昀. 侵蚀背景下湘中红壤丘陵区土地利用方式对土壤活性有机碳分布特征的影响研究[J]. 湖南大学学报(自然科学版), 2014, 41(3): 88-93
作者姓名:李忠武  王曙光  陈晓琳  聂小东  张艳  刘桂平  曾婉昀
作者单位:(1. 湖南大学 环境科学与工程学院, 湖南 长沙410082;2. 邵阳市水土保持科学研究所, 湖南 邵阳422202)
基金项目:教育部新世纪人才计划项目(NCET-09-330);国家自然科学基金资助项目(40971170,41241297);湖南省自然科学基金资助项目(11JJ3041)
摘    要:以红壤丘陵区典型区域为对象,采用野外调查与室内分析相结合的方法,研究了侵蚀背景下红壤丘陵区不同土地利用方式对土壤活性有机碳的影响规律.结果表明,1)土地利用方式影响土壤活性有机碳主要体现在表层土壤.不同土地利用方式下表层土壤活性有机碳含量差异显著,而在表层以下的土壤中没有显著性差异;2)土地利用方式对不同侵蚀部位活性有机碳影响较大.不同土地利用方式下侵蚀部位土壤活性有机碳含量差异性明显高于沉积部位;3)不同土地利用方式之间活性有机碳的垂向分布规律基本一致,表现为表层活性有机碳含量最高,随着土层深度的增加,含量逐渐减小.

关 键 词:活性有机碳  红壤丘陵区  土地利用  土壤侵蚀  侵蚀部位

Effect of Land Use Type of Red Soil Hilly Region on Distribution of Soil Labile Organic Carbon Properties under the Condition of Soil Erosion
LI Zhong-wu,WANG Shu-guang,CHEN Xiao-lin,NIE Xiao-dong,ZHANG Yan,LIU Gui-ping,ZENG Wan-yun. Effect of Land Use Type of Red Soil Hilly Region on Distribution of Soil Labile Organic Carbon Properties under the Condition of Soil Erosion[J]. Journal of Hunan University(Naturnal Science), 2014, 41(3): 88-93
Authors:LI Zhong-wu  WANG Shu-guang  CHEN Xiao-lin  NIE Xiao-dong  ZHANG Yan  LIU Gui-ping  ZENG Wan-yun
Affiliation:(1. College of Environmental Science and Engineering, Hunan Univ, Changsha,Hunan410082, China; 2. Soil and Water Conservation Research Institute of Shaoyang, Hunan Province, Shaoyang,Hunan422002, China)
Abstract:Soil erosion is one of the major environmental problems affecting people's survival, and the exploration of the effect of land use type on soil labile organic carbon is of significance to regional soil environment protection under the condition of soil erosion. A typical area of red soil hilly region was selected as the research site. Integrating outdoor sampling with indoor analysis, this paper studied the effect of land use type of red soil hilly region on distribution of soil labile organic carbon properties under the condition of soil erosion. The result has shown 1) land use type affects the labile organic carbon of the surface soil. There is a significant difference in the content of labile organic carbon in the 0-5 cm soil layer, but it is almost the same in the sub-layers; 2) Land use type has a great impact on the content of labile organic carbon in different poisitions of eroded land and the difference of labile organic carbon content in erosion area is higher than in deposition area; and, 3) the vertical distributions of soil labile organic carbon are basically the same among the different land use types, and the difference in surface is big, and increasingly small with the increase of soil depth.
Keywords:
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