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黔中喀斯特坡地浅层裂隙土壤机械组成对降雨的响应
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  • 英文篇名:Response of mechanical composition of fractured soil to rainfall in shallow Karst slopes incentral Guizhou,China
  • 作者:杨宇琼 ; 戴全厚 ; 严友进 ; 彭旭东
  • 英文作者:YANG Yu-qiong;DAI Quan-hou;YAN You-jin;PENG Xu-dong;College of Forestry,Guizhou University;
  • 关键词:喀斯特坡地 ; 浅层裂隙 ; 土壤机械组成 ; 降雨 ; 地下土壤漏失
  • 英文关键词:Karst slope;;shallow fissure;;soil mechanical composition;;rainfall;;leakage of under ground soil
  • 中文刊名:应用生态学报
  • 英文刊名:Chinese Journal of Applied Ecology
  • 机构:贵州大学林学院;
  • 出版日期:2019-02-15
  • 出版单位:应用生态学报
  • 年:2019
  • 期:02
  • 基金:国家重点研发计划项目(2016YFC0502604);; 国家自然科学基金项目(41671275,41461057);; 贵州省重大专项(黔科合重大专项字[2016]3022号);; 贵州省一流学科建设项目(GNYL[2017]007);; 黔科合平台人才([2017]5788)资助~~
  • 语种:中文;
  • 页:189-196
  • 页数:8
  • CN:21-1253/Q
  • ISSN:1001-9332
  • 分类号:S157.1
摘要
运用野外取样调查结合室内吸管法,分析黔中喀斯特坡地不同土地利用类型浅层裂隙土壤机械组成随降雨的变化特征,以期为该区地下土壤漏失研究提供理论依据和技术支撑.结果表明:黔中喀斯特坡地浅层裂隙土壤粒径含量总体以粉粒为主,约占57%.在不同降雨量的作用下,坡耕地裂隙土壤颗粒含量变化整体表现为细砂粒含量的减少和粉粒、黏粒含量的增大.草地裂隙土壤颗粒的变化主要是细砂粒含量的减少和黏粒含量的增加.乔木林地和灌木林地裂隙土壤颗粒的变化不规律.降雨量与土壤砂粒含量变化之间存在正相关关系.随着土层深度的增加,各土地利用类型的裂隙对粉粒和极粗砂粒含量的变化有一定影响,其中,粉粒含量随土层深度的增加而减少.
        Field sampling and indoor pipette method was used to analyze the variation of soil mechanical composition of shallow Karst fissures in response to rainfall under different land uses in Karst rocky desertification region in central Guizhou. Results would supply important scientific basis and direction for further research of soil leakage in the Karst areas. The results showed that silt was the dominant component in soil mechanical composition of shallow Karst fissures,with a content of57%. In response to rainfall,the contents of silt and clay were increased and that of fine sand was reduced in slope cropland,while the content of fine sand was reduced and that of silt was increased in grassland. The changes of mechanical composition of shallow Karst fissures in forest and shrub land were irregular. Moreover,there was a positive correlation between rainfall and the sand content of shallow Karst fissures. The fissures of land use types had effects on the changes of silt and extremely coarse sand contents with the increase of soil depth,with a decreasing trend of silt.
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