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- W2364456784 abstract "Red earth grain-size of seven typical sections in Zhejiang Province was tested.The results show that:(1)There were a variety of red earth parent materials in Zhejiang Province,sedimentary environment or rock characteristics influenced red earth grain-size feature notably.The grain-size feature not only contained the information of original sediment or rock,but also indicated the characteristics of pedogenesis,which could be used to distinguish different types of red earth effectively.(2)TX,SSSW,AJ and HHT sections had the highest content of silt(4～63 μm),the clay(4 μm) come in second,but TX,SSSW and AJ sections have low content of sand(63 μm),the mean values were between 0.13% and 1.18%;HHT section′s coarse ingredient(125～2 000 μm) was obvious,the former showed aeolian characteristics,the latter was altered by proximal power.Red earth with aeolian characteristics was significant in the recognizing of the distribution of the aeolian sediments in south of the Yangtze River during the Quaternary and the information of monsoon evolution.(3)Grain-size distributions of the weathering crust red earth depend on their parent materials and weathering characteristics.In contrast,mode peak was in 30～63 μm from sandstone red earth,in 15～30 μm from granite red earth,in 4～6 μm from basalt red earth.Furthermore,granite red earth has obvious middling and coarse sand ingredient between 125 μm and 2 000 μm;basalt red earth has obvious clay ingredient between 0.2 μm and 1 μm;Besides the mode peak,sandstone red earth still had other constituents at 2～4 μm,0.2～1 μm.Basalt red earth was more even than sandstone and granite red earth." @default.
- W2364456784 created "2016-06-24" @default.
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- W2364456784 date "2008-01-01" @default.
- W2364456784 modified "2023-09-28" @default.
- W2364456784 title "Comparative study of red earth grain-size from different parent materials in Zhejiang Province" @default.
- W2364456784 hasPublicationYear "2008" @default.
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