中国东部表层土壤磁化率特征及其指示意义

邱世藩; 欧阳婷萍; 朱照宇; 黄宁生; 李明坤; 田成静; 卞勇

doi:10.3799/dqkx.2014.138

Volume 39 Issue 10

Oct. 2014

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Article Navigation > Earth Science > 2014 > 39(10): 1454-1464

Qiu Shifan, Ouyang Tingping, Zhu Zhaoyu, Huang Ningsheng, Li Mingkun, Tian Chengjing, Bian Yong, 2014. Magnetic Susceptibility Characteristics of Weathering-Pedogenic Topsoil along East Part of China and Its Significance. Earth Science, 39(10): 1454-1464. doi: 10.3799/dqkx.2014.138

Citation:

Qiu Shifan, Ouyang Tingping, Zhu Zhaoyu, Huang Ningsheng, Li Mingkun, Tian Chengjing, Bian Yong, 2014. Magnetic Susceptibility Characteristics of Weathering-Pedogenic Topsoil along East Part of China and Its Significance. Earth Science, 39(10): 1454-1464. doi: 10.3799/dqkx.2014.138

Citation:

Qiu Shifan, Ouyang Tingping, Zhu Zhaoyu, Huang Ningsheng, Li Mingkun, Tian Chengjing, Bian Yong, 2014. Magnetic Susceptibility Characteristics of Weathering-Pedogenic Topsoil along East Part of China and Its Significance. Earth Science, 39(10): 1454-1464. doi: 10.3799/dqkx.2014.138

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Magnetic Susceptibility Characteristics of Weathering-Pedogenic Topsoil along East Part of China and Its Significance

doi: 10.3799/dqkx.2014.138

1.
Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
2.
University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 2014-01-26
Publish Date: 2014-10-01

Abstract

Abstract

Magnetic susceptibility is one of the most widely used and most easily to be obtained parameters of environmental magnetism. However, the meaning and interpretation of magnetic susceptibility is the most complicate. High, low frequency magnetic susceptibility and non-hysteresis remanence were measured for seventy-nine weathering-pedogenic topsoil samples collected from the east part of China, from north to south, covering the main climatic zones within China. Moreover, relationship between these magnetic parameters and climate indexes such as precipitation and annual average temperature was analyzed. The results indicate that: (1) Significant difference of magnetic properties is existed among weathering-pedogenesis topsoil that derived from different parent rocks. The relationship between all magnetic susceptibility parameters and climate indexes is much different. Difference of geological conditions and parent rocks must be taken full consideration when the relationship between magnetism and climate conditions is discussed in large spatial scale. (2) The non-hysteresis remanence magnetic susceptibility is negatively related to precipitation and annual average temperature for topsoil derived from granite. However, it is positively related to precipitation for topsoil derived from balsalt. The widely recognized relationship between magnetic strength of paleosol and pedogenesis of loess-paleosol sequence from the Chinese Loess Plateau isn't always proper to apply in other climate area. (3) Magnetic particles tend to be finer during weathering and soil-forming process. However, single magnetic parameter can't reflect the climate and environmental change because some ultrafine particles are easy to be carried out in situ due to increasing rainfall intensity. (4) Magnetic susceptibility of non-hysteresis remanence of weathering-pedogenic topsoil can reflect the weathering degree of weathering soil. The magnetic variation mechanism of weathering-pedogenic topsoil, especially magnetic mineral transformation of corresponding soil profile, is still needed further study.
- magnetic susceptibility,
- weathering-pedogenesis,
- topsoil,
- east part of China,
- environmental geology

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References(71)

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Magnetic Susceptibility Characteristics of Weathering-Pedogenic Topsoil along East Part of China and Its Significance

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