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湖北省土壤各级颗粒的磁化率
引用本文:余红家.湖北省土壤各级颗粒的磁化率[J].湖北农学院学报,1990(1).
作者姓名:余红家
摘    要:本试验对湖北省六种土壤五个粒级(>1,1-0.5,0.5-0.25,0.25-0.15.0.15-0.1mm)的磁化率进行了测定。结果表明:红壤、棕红壤、潮土和黄棕壤表土层磁化率大于母质层磁化率,而紫色土和黄褐土表土层磁化率小于下部土层的磁化率。棕红壤表土层磁化率小于淀积层磁化率。红壤、棕红壤、黄棕壤和黄褐土母质层磁化率随颗粒变细而明显增加,但这一现象在潮土、紫色土的母质层确不明显。0.25-0.15mm粒级是黄棕壤、红壤、棕红壤、潮土、紫色土磁化率随颗料大小变化的一个转折点。

关 键 词:磁化率  颗粒大小  土壤  母质

THE MAGNETIC SUSCEPTIBILITY OF DIFFERENT SIZE FRACTIONS OF THE SOILS IN HUBEI PROVINCE
She Hong jia.THE MAGNETIC SUSCEPTIBILITY OF DIFFERENT SIZE FRACTIONS OF THE SOILS IN HUBEI PROVINCE[J].Journal of Hubei Agricultural College,1990(1).
Authors:She Hong jia
Institution:She Hong jia
Abstract:The magnetic susceptibility of different size fractions of the soils in Hubei Province was investigated. The results showed that the na9netic susceptibility of the topsoil of purple soil and yellow-cinnamon soil was Less than that of their parent materiat, which was caused by their lower fertility and weak pedogenesis. The megnetic susceptibility of the topsoil of red earth, brown-red earth, alluvial soil and yellow-brown earth was greater than that of their parent material. The magnetic susceptibility of the topsoil of brown-red earth was less than that of its accumu-lation horizon. The magnetic susceptibility of the parent material of redearth, yellow-brown earth, brown-red earth and yellow-cinnamon soil increased with their partical size decreasing 0.25-0.15mm partical size fraction wasa transforming point of the magnetic susceptibility of redearth, allurial soil and purple soil with their partical size changing
Keywords:magnetic susceptibility  partical  size  soil  parent material
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