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侵蚀沉积物基本性质的研究
引用本文:郑毅 Full.,MA. 侵蚀沉积物基本性质的研究[J]. 云南农业大学学报(自然科学版), 1996, 11(1): 1-7
作者姓名:郑毅 Full.  MA
作者单位:云南农业大学农业科学技术学院
摘    要: 本文对英国中西部地区1985年至1986年间壤质砂土上冲刷下来的土壤沉积物基本性质进行了研究。结果表明,土壤沉积物中粘粒、粉粒、砂粒和大石砾含量分别是1.98%,13.07%,83.28%和1.67%(n=84),养分元素为Ca0.20%,Fe1.23%,K1.85%,Mg0.49%,Mn0.02%,P 0.06%,Cu<12.0mg·kg-1,S43.0mg·kg-1,有机质含量为1.65%pH值是514(H2O)和5.01(0.01MCaCl2),从1985年12月19日至1986年12月19日在十个径流小区所收集的侵蚀土壤沉积物来看,土壤的颗粒组成、有机质含量、pH值均随时间而变化,表现为沉积物中的细粒部分含量增加、有机质含量增加、pH值下降。研究结果还发现,坡度和沉积物颗粒组成之间、沉积物的有机质含量和颗粒组成之间有显着的相关性。

关 键 词:沉积物  基本性质
收稿时间:1994-12-22

Studies on The Properties Of Eroded Sediment
Zheng Yi,M.AFullen, R.T randsma. Studies on The Properties Of Eroded Sediment[J]. Journal of Yunnan Agricultural University, 1996, 11(1): 1-7
Authors:Zheng Yi  M.AFullen   R.T randsma
Affiliation:1. Yunnan AgriculturaI University, Kunming;2. The University of Wolverhampton, England
Abstract:The properties of Sediment eroded from the Loamy sand soils in West mid-lands,UK were studied.The results showed the contents of clay,silt,sand and coarse fraction of the sediment were 1.98%,13.07%, 83.28%and 1.67%(n=84)respectively.Nutrient contents were Ca 0.20%, Fe 1.23%,K1.85%,Mg 0.49%,Mn0.02%,P0.06%,Cu 12mg·kg-1,S 43.0mg·kg-1.Organic matter content was 1.59.PH Values were 5.14(H2O)and 5.01(0.01M CaCl2)From 19/12/1985 to 19/12/1986,Soil Particle size distribution,organic matter contents,pH Values of Sediments were changed:the fine fractions and organic matter content increased,PH values decreased.The relationships between organic matter content and particle size,slope angle and particle size were examined.
Keywords:Sediment  Properties  
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