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大别山北麓黄土古土壤磁组构参数特征与环境变化研究
引用本文:张华,宋传中,张妍. 大别山北麓黄土古土壤磁组构参数特征与环境变化研究[J]. 合肥工业大学学报(自然科学版), 2012, 0(2): 252-256
作者姓名:张华  宋传中  张妍
作者单位:合肥工业大学资源与环境工程学院;安徽建筑工业学院环境与能源工程学院
基金项目:国家自然科学基金资助项目(40772131;40372097;41072161);安徽省教育厅自然科学研究资助项目(KJ2011z049);中国地质调查局科技资助项目(1212011121114);安徽省公益性地质研究资助项目(2008-g-5)
摘    要:
文章对大别山北麓黄土-古土壤的磁化率各向异性进行了初步研究,结果表明:剖面上部的磁组构参数P、F、L平均值均低于底部的相应值;在磁组构参数F-L、P-q、P-F组合关系图上,上部样品的数据点集中分布于靠近坐标原点的区域,底部的多远离坐标原点;磁组构特征指示了上部为风成沉积而底部为水成沉积。

关 键 词:大别山  磁组构  黄土-古土壤  环境变化

Study of magnetic fabric parameters characteristics of loess-palaeosols from northern slope of Dabie Mountains and environmental changes
ZHANG Hua,SONG Chuan-zhong,ZHANG Yan. Study of magnetic fabric parameters characteristics of loess-palaeosols from northern slope of Dabie Mountains and environmental changes[J]. Journal of Hefei University of Technology(Natural Science), 2012, 0(2): 252-256
Authors:ZHANG Hua  SONG Chuan-zhong  ZHANG Yan
Affiliation:1(1.School of Resources and Environmental Engineering,Hefei University of Technology,Hefei 230009,China;2.College of Environment and Energy Engineering,Anhui University of Architecture,Hefei 230022,China)
Abstract:
The anisotropy of magnetic susceptibility of loess-palaeosols from the northern slope of Dabie Mountains is examined.The mean values of magnetic fabric parameters(P,F,L) of the upper part of the strata are less than those of the bottom.In the figures of F-L,P-q,P-F relation,the data of aeolian deposit are mostly concentrated in the vicinity of the coordinate origin,while the data of hydraulic deposit are mostly distant from the coordinate origin.Generally,the magnetic fabric characters show that the upper part of the strata is aeolian deposit and the bottom is hydraulic deposit.
Keywords:Dabie Mountain  magnetic fabric  loess-palaeosols  environmental change
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