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- W2355831343 abstract "Parent material of black soil in the Northeast China is mainly quaternary sediment.Based on chemical composition and XRD of two kinds of soil particles(less than 2 μm in diameter) from black soil profile,laterite parent material and loess parent material,the results show that the black soil in Northeast China developed from laterite parent material has strong desilication.The clay minerals are 1-1 and 2-1 types,mainly containing illite,vermiculite,and kaolinite.Soil particles from the upper soil have low contains of chlorite.Parent material has high content of montmorillonite but without chlorite.During the process of soil formation,it existed high contents of illite,with slight chlorite gradually formed,and montmorillonite was converted to vermiculite.Black soil particles developed from the loess parent material are 2-1 type clay minerals,containing illite,vermiculite,kaolinite,with slight chlorite.Some parent material contains feldspar.Feldspar in the soil minerals gradually disappeared after desillication.Some parent material contains montmorillonite.Distribution of soil particle developed from the loess parent material is relatively even,and conversion and evolution among minerals are relatively simple." @default.
- W2355831343 created "2016-06-24" @default.
- W2355831343 creator A5068378711 @default.
- W2355831343 date "2013-01-01" @default.
- W2355831343 modified "2023-09-26" @default.
- W2355831343 title "A Study on Clay Minerals from Different Parent Material of Black Soil" @default.
- W2355831343 hasPublicationYear "2013" @default.
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