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喀斯特地区不同植被下小生境土壤矿物组成及有机碳含量空间异质性初步研究
引用本文:廖洪凯,龙 健,李 娟,杨江江,冯业强.喀斯特地区不同植被下小生境土壤矿物组成及有机碳含量空间异质性初步研究[J].中国岩溶,2010,29(4):434-439.
作者姓名:廖洪凯  龙 健  李 娟  杨江江  冯业强
作者单位:1. 贵州师范大学贵州省山地环境重点实验室,贵州,贵阳,550001
2. 贵州师范大学地理与环境科学学院,贵州,贵阳,550001
3. 贵州师范大学贵州省山地环境重点实验室,贵州,贵阳,550001;贵州师范大学地理与环境科学学院,贵州,贵阳,550001
基金项目:国家自然科学基金(40971160)、贵州省优秀青年科技人才培养对象专项资金项目(黔科合人字[2009]21号)、贵州省高层次人才科研特助经费项目(TZJF-2008-40号)
摘    要:通过对喀斯特地区乔木林、灌木林和草丛不同植被类型覆盖下的土面、石面、石缝、石沟、石洞、石槽和石坑7类小生境土壤样品分析测定,探讨了小生境土壤矿物组成及有机碳的空间异质性特征。结果表明:(1)不同植被类型下土壤矿物组成存在明显差异,即从草丛→灌木林→乔木林,小生境土壤中的石英、高岭石基本保持不变,但草丛土壤中的白云石矿物全部消失,灌木林、乔木林土壤中逐渐出现绿泥石;(2)随着植被正向演替,土壤有机碳含量显著增加,小生境土壤有机碳含量在不同植被类型条件下存在明显的异质性,表现为草丛乔木林灌木林。与此同时,以小生境土壤有机碳含量及变异系数为评价因子,分别对乔木林、灌木林及草丛中小生境有机碳进行聚类分析,结果显示,小生境微地貌特征是土壤有机碳含量及空间变异性的重要影响因子。对于土壤有机碳保护,草丛及灌木林区应以提高植被覆盖率为主;乔木林区则主要是保持现有良好的植被状况,减少人为干扰。

关 键 词:喀斯特小生境  植被类型  土壤矿物  有机碳  空间异质性
收稿时间:2010/8/26 0:00:00

Preliminary study on spatial heterogeneity of soil mineral composition and organic carbon content at different micro-habitats that under different vegetation types in karst region
LIAO Hong-kai,LONG Jian,LI Juan,YANG Jiang-jiang and FENG Ye-qiang.Preliminary study on spatial heterogeneity of soil mineral composition and organic carbon content at different micro-habitats that under different vegetation types in karst region[J].Carsologica Sinica,2010,29(4):434-439.
Authors:LIAO Hong-kai  LONG Jian  LI Juan  YANG Jiang-jiang and FENG Ye-qiang
Institution:1.Guizhou Key Laboratory of Mountain Environment,Guizhou Normal University,Guiyang,Guizhou 550001,China;2.Department of Geography and Environment Science,Guizhou Normal University,Guiyang,Guizhou 550001,China)
Abstract:The spatial heterogeneity of soil mineral composition and soil organic carbon(SOC)are determined through sampling at 7 kinds of micro-habitats,including soil surface,rocky surface,stone crevice,stone gully,stone cavern and stone groove as well as stone pit,under different vegetation cover,arbor and shrub and grass as well,in karst region.The results prove that,(1) The composition of soil mineral is diversity under different vegetation types.Quartz and kaolinite in the soil do not change under grass and shrub as well as arbor vegetation cover,dolomite in the soil in grassland disappears,and chlorite gradually appears in the shrub and arbor forest.(2)With the vegetation succession,the content of SOC significantly increases,and the content of micro-habitats SOC shows evident heterogeneity as follows: grassland arbor forest shrub land.Moreover,taking the content of SOC and the coefficient of variation at micro-habitats as evaluation factors,cluster analysis to the SOC under arbor forest and shrub as well as glass covers is done.The results show that the micro-topography is very important factor affecting the content of SOC and its spatial heterogeneity.To protect the SOC,the major work is improving vegetation covered ratio in grass and shrub vegetation cover areas,and keeping the good conditions of vegetation and decreasing human interference in the arbor vegetation cover areas.
Keywords:karst micro-habitats  vegetation type  soil mineral  organic carbon  spatial heterogeneity
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