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Influence of Different Iron Oxides on Magnetic Susceptibility of Brown Earth Profile(PDF)

《北方园艺》[ISSN:1001-0009/CN:23-1247/S]

Issue:
2014年04期
Page:
144-148
Research Field:
Publishing date:

Info

Title:
Influence of Different Iron Oxides on Magnetic Susceptibility of Brown Earth Profile
Author(s):
ZHANG Da-gengLI Jie
School of Land and Environment,Shenyang Agriculture University,Shenyang,Liaoning 110866
Keywords:
iron oxidesbrown soil profilemagnetic susceptibility
PACS:
S 153
DOI:
-
Abstract:
Taking brown soil as research object,through measurement and analysis of magnetic susceptibility of brown soil profile and morphologically different iron oxides,the influence of iron oxides with chemically different morphologies on magnetic susceptibility of brown soil were studied.The results showed that magnetic susceptibility changing trended of brown soil profile generally was that surface soil magnetic susceptibility was the highest,magnetic susceptibility of deposition layer was locally greatened,in the parent material layer soil susceptibility was relatively low.The average frequency magnetic susceptibility of brown soil was 9.08%,so brown soil contains a lot of ultrafine paramagnetic particle produced by weathering pedogenesis.Free iron oxides and amorphous iron oxides were highly significantly correlated with magnetic susceptibility;total iron was significantly correlated with magnetic susceptibility on 60~200 cm layer.In terms of magnetic susceptibility of brown soil,the content of free iron oxides had more influences than that of amorphous iron oxides and organic combination iron oxides.

References:

[1]依艳丽,刘孝义.土壤、生物磁学研究及应用[M].北京:农业出版社,2001.

[2]卢瑛,龚子同,张甘霖.城市土壤磁化率特征及其环境意义[J].华南农业大学学报,2001,22(4)26-28.

[3]鸟居雅之,褔间浩司,苏黎,.黄土-古土壤磁化率述评[J].海洋地质与第四纪地质,199919(3)83-94.

[4]董元杰,史衍玺.鲁中山区小流域坡面土壤侵蚀强度与磁化率的空间分异特征研究[J].水土保持学报,200620(6)6-10,21.

[5]Ventura J R ENearing M ANorton L DDeveloping a magnetic tracer to study soil erosion[J].Catena,2001(43)277-279.

[6]刘青松,邓成龙.磁化率及其环境意义[J].地球物理学报,2009,52(4)1041-1048.

[7]卢升高.土壤频率磁化率与矿物粒度的关系及其环境意义[J].应用基础与工程科学学报,2000,8(1)9-15.

[8]马玉增,董元杰,史衍玺,.坡面侵蚀土壤化学性质对磁化率影响机理的研究[J].水土保持学报,200822(2)51-5397.

[9]刘孝义,依艳丽.磁场对土壤理化性质的影响及土壤磁化率与土壤有机质相关性[J].沈阳农业大学学报,198510(1)33-40.

[10]卢升高,俞劲炎.土壤氧化铁的磁性参数及其应用[J].土壤通报,1999,30(4)160-162.

[11]Maher B A.Characterization of soils minerals magnetic measurements[J].Phys Earth Planet Inter19864276-92.

[12]Fine P.New evidence for the origin of ferrimagnetisms minerals in Loess from China[J].Soil Sci Soc Am J,1993571537-1542.

[13]Sun J MLiu T S.Multiple origins and interpretations of the magnetic susceptibility signal in Chinese wind-blown sediments[J].Earth and Planetary Science Letters,2000180287-296.

[14]胡雪峰.“黄土-古土壤”序列中氧化铁和有机质对磁化率的影响[J].土壤学报,2004,41(1)7-11.

[15]Zhou L P,Oldfield F,Wintle A G,et al.Partly pedogenic origin of magnetic variations in Chinese loess[J].Nature,1990,364737-739.


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Last Update: 2014-08-08