大同盆地高砷地下水系统沉积物环境磁学特征

谢先军; 王焰新; 苏春利; 刘怀庆; 段萌语; 张宏达

Volume 33 Issue 1

Jan. 2008

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Article Navigation > Earth Science > 2008 > 33(1): 117-123

XIE Xian-jun, WANG Yan-xin, SU Chun-li, LIU Huai-qing, DUAN Meng-yu, ZHANG Hong-da, 2008. Environmental Magnetic Properties of Sediments of High Arsenic Groundwater System, Datong Basin. Earth Science, 33(1): 117-123.

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Environmental Magnetic Properties of Sediments of High Arsenic Groundwater System, Datong Basin

Shool of Erviroumental Studies & MOE Lalorutory of Biogeology and Eruironmental Geology, China Urirersity of Geasciences, Wuhan 430074, China

Received Date: 2007-03-26
Publish Date: 2008-02-25

Abstract

Abstract

The purpose of the study is to test the possible relationship between magnetic parameters and arsenic in high arsenic aquifer sediment. Magnetic and geochemical study on core sediments from Datong basin suggests that the dominant magnetic mineral is ferrimagnetic. Magnetic measurements and arsenic concentration analysis were carried out to understand the distribution characteristics of magnetic parameters and arsenic in sediments. All core samples with high arsenic content have low saturation isothermal remnant magnetism (SIRM) values, indicating the correlation between arsenic and paramagnetic mineral. The correlation factors between arsenic content and magnetic parameters are very low (R² < 0.5, α=0.05), but the magnetic susceptibility (χ) is better correlated than the other magnetic parameters with correlation factor of about 0.4 (α=0.05). The low correlation between magnetic proxies and arsenic content is attributed to the dilution of paramagnetic minerals by the ferrimagnetic and anti-ferromagnetic minerals. The occurrence of As-rich groundwater in this region may be due to dissolution of As-bearing Fe mineral (e.g. γFeOOH, 5Fe2O3·9H2O) and subsequent arsenic release.
- Datong basin,
- arsenic,
- groundwater system,
- sediment,
- environmental magnetism.

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Environmental Magnetic Properties of Sediments of High Arsenic Groundwater System, Datong Basin

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