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土地利用方式对红枫湖入湖流域土壤团聚体磷含量及其形态的影响
引用本文:杨华,龙健,李兆君,廖红凯,刘灵飞,李娟.土地利用方式对红枫湖入湖流域土壤团聚体磷含量及其形态的影响[J].农业环境保护,2013(11):2214-2220.
作者姓名:杨华  龙健  李兆君  廖红凯  刘灵飞  李娟
作者单位:[1]贵州师范大学贵州省山地环境重点实验室,贵阳550001 [2]中国农业科学院农业资源与农业区划研究所,北京100081 [3]贵州师范大学地理与环境科学学院,贵阳550001
基金项目:基金项目:贵州师范大学博士科研启动费;贵州省学位与研究生教育教学改革研究项目;贵州省社发攻关项目(黔科合SY字[2013]3162号);贵州省科技厅一贵州师范大学联合基金项目(黔科合J字LKS[2012]25号)
摘    要:以贵州省安顺市红枫湖入湖口4种典型土地利用方式(玉米地、菜园、林地及撂荒地)为研究对象,分别探讨了土地利用方式对0—15em和15~30cm两个层次土壤团聚体总磷含量及其形态的影响。结果表明,不同土地利用方式下,原状土壤及各粒级团聚体总磷含量均表现为玉米地〉菜园〉撂荒地〉林地。土壤各粒级团聚体磷形态含量以ResidualP、NaOH—P、NaHCO3-P为主,其中ResidualP在各土地利用方式中的含量均最高,变幅分别为玉米地28.3%~45.4%、林地61.1%-72.7%、菜园45.9%~53.0%、撂荒地52.1%-72.4%;玉米地和菜园土壤均表现为有机磷含量约为无机态含量的2倍;随团聚体粒径的减小,土壤对总磷含量的贡献率呈减少趋势,土壤团聚体对总磷含量贡献主要集中在5~2mm和2~0.5mm两个粒级中,贡献率均达77%以上,其中耕作土壤(玉米地、菜园)中5-2mm和2-0.5mm两个粒级团聚体中的磷是湖泊面源污染中磷素的主要贡献载体,也是造成湖泊富营养化的关键因素。

关 键 词:红枫湖人湖流域  土地利用方式  团聚体  磷含量  磷形态

Effects of Land Use Types on Phosphorus Forms and Their Contents in Soil Aggregates in Watershed of Hongfeng Lake
YANG Hua,LONG Jian,LI Zhao-jun,LIAO Hong-kai,LIU Ling-fei,LI Juan.Effects of Land Use Types on Phosphorus Forms and Their Contents in Soil Aggregates in Watershed of Hongfeng Lake[J].Agro-Environmental Protection,2013(11):2214-2220.
Authors:YANG Hua  LONG Jian  LI Zhao-jun  LIAO Hong-kai  LIU Ling-fei  LI Juan
Institution:1.Guizhou Key Laboratory of Mountain Environment, Guizhou Normal University, Guiyang 550001 ; 2.Institute of Agricultural Resources and Regional Planning, China Academy of Agricultural Sciences, Beijing 100081; 3.Department of Geography and Environment Science, Guizhou Normal University, Guiyang 550001 )
Abstract:Excessive phosphorus (P) in soils may increase the potential to pollute water through runoff and/or leaching. Different land use types may change phosphorus mobility. A study was performed to examine the chemical forms and their contents of P in bulk soil and soil aggregates at 0-15 cm and 15-30 cm under four land use types:cornfields, vegetable fields, forest land and abandoned land in the water- shed of Hongfeng Lake in Anshun, Guizhou Province. Total P contents in bulk soils and soil aggregates were in order of cornfields〉vegetable fields〉abandoned land〉forest land under different land use types. Residual P, NaOH-P, and NaHCO3-P were the major forms in soil aggre- gates at each depth. The residual P was the highest among all P forms in softs under four land use types, and ranged 28.3%-45.4%, 61.1% -72.7%, 45.9%-53.0% and 52.1%~72.4% in cornfield, forest land, vegetable field and abandoned land, respectively. The organic P con- tents were as about 2 times as inorganic P contents in cornfield and vegetable field. Soil P was mainly present in soil aggregates of 5-2 mm and 2-0.5 mm, accounting for more than 77% of soil total P. Phosphorus in aggregates of 5-2 mm and 2-0.5 mm in cultivated soils includ- ing cornfield and vegetable field were the main contributors to lake P and could be the key factor of the lake eutrophication.
Keywords:Hongfeng Lake watershed  land use  aggregate  phosphorus content  phosphorus form
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