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机构地区:[1]贵州大学林学院,贵阳550025 [2]息烽县林业绿化局,贵州息烽551100 [3]息烽县水务管理局,贵州息烽551100
出 处:《水土保持研究》2015年第1期158-162,167,共6页Research of Soil and Water Conservation
基 金:国家"十二五"科技支撑计划(2011BAC02B02);国家自然科学基金(41461057);贵州省重大应用基础专项(黔科合JZ字[2014]2002);贵州省喀斯特生态与环境专业学位研究生工作站(贵州省教育厅;2014)
摘 要:基于土壤粒径分形维数的计算方法,对草海不同石漠化程度土壤颗粒、微团聚体、团聚体粒径分布的分形维数进行了研究。结果表明:石漠化地区土壤颗粒分形维数与土壤粉粒(0.001~0.05mm)呈极显著负相关(r=-0.963**,P〈0.01),与土壤黏粒(〈0.001mm)呈极显著正相关(r=0.995^**,P〈0.01);土壤微团聚体主要以〉0.01mm的大粒级微团聚体为主,其分形维数与大粒级(〉0.01mm)微团聚体表现出呈极显著的负相关(r=-0.964^**,P〈0.01);土壤风干团聚体〉5mm粒级的含量达到70%以上。湿筛后,〉5mm土壤团聚体含量减少,其余粒级有不同程度的增加,其中〈0.25mm的增幅最大。石漠化程度的加剧,使土壤黏粒含量逐渐增多,土壤颗粒、土壤微团聚体分形维数逐渐增大。通过对草海地区石漠化土壤结构特征的研究,可为草海地区石漠化治理、草海湿地的保护提供参考。Based on the calculation method of soil fractal dimension,the fractal dimension of soil particle,micro-aggregates and water-stable aggregates in different degree of Stony Desertification in Caohai was studied.The results showed that the fractal dimension of particle size distribution was dramatically negatively correlated with soil silt(0.001—0.005mm)(r=-0.963^**,P〈0.01)and significantly positively correlated with soil clay(〈0.001mm)(r=0.995^**,P〈0.01).Soil micro-aggregates(〉0.01 mm)was main component of aggregate,its fractal dimension was significantly positively correlated with large size micro-aggregates(〉0.01mm)(r=-0.964^**,P〈0.01).Air-dried soil aggregate(〉5 mm)accounts for more than 70% of air-dried soil aggregate composition.Through wet screen processing,air-dried soil aggregate(〉5 mm)reduced,the other sizes of aggregates increase to some extent,increment of〈0.25 mm aggregate significant.In the process of desertification,soil clay content increased,the fractal dimension of soil particles and micro-aggregates fractal dimension increased gradually.This study aims to provide reference for desertification control and wetland protection of Caohai through the study of rocky desertification soil structure characteristics.
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