丰宁黄土-古土壤剖面常量元素地球化学特征

毛欣; 刘林敬; 李长安; 张玉芬; 赵红梅; 毕志伟; 姜高磊

doi:10.3799/dqkx.2017.538

Volume 42 Issue 10

Oct. 2017

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Article Navigation > Earth Science > 2017 > 42(10): 1750-1759

Mao Xin, Liu Linjing, Li Chang'an, Zhang Yufen, Zhao Hongmei, Bi Zhiwei, Jiang Gaolei, 2017. Elemental Composition Features of Loess-Paleosol Profile in Fengning, Hebei Province. Earth Science, 42(10): 1750-1759. doi: 10.3799/dqkx.2017.538

Citation:

Mao Xin, Liu Linjing, Li Chang'an, Zhang Yufen, Zhao Hongmei, Bi Zhiwei, Jiang Gaolei, 2017. Elemental Composition Features of Loess-Paleosol Profile in Fengning, Hebei Province. Earth Science, 42(10): 1750-1759. doi: 10.3799/dqkx.2017.538

Citation:

Mao Xin, Liu Linjing, Li Chang'an, Zhang Yufen, Zhao Hongmei, Bi Zhiwei, Jiang Gaolei, 2017. Elemental Composition Features of Loess-Paleosol Profile in Fengning, Hebei Province. Earth Science, 42(10): 1750-1759. doi: 10.3799/dqkx.2017.538

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Elemental Composition Features of Loess-Paleosol Profile in Fengning, Hebei Province

doi: 10.3799/dqkx.2017.538

1.
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
Institute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, China

Received Date: 2016-12-29
Publish Date: 2017-10-18

Abstract

Abstract

The loess deposited in the upper reaches of the Luanhe River valley is an important geological record of past palaeoclimate and palaeoenvironment in the Bashang Plateau of Hebei Province. Due to the scattered distribution and small thickness of the loess in this region, it has attracted little attention in previous studies. In order to discuss the genesis, provenance and chemical weathering intensity of loess in this region, the elemental composition analysis of 77 samples from typical loess-paleosol profile was carried out and compared with known typical aeolian deposits. The results show that: (1) The sum of major elements (SiO₂, Al₂O₃ and Fe₂O₃) and UCC (Upper Continental Crust)-normalized patterns of Fengning profile are similar to those of typical aeolian deposits, indicating that Fengning loess and paleosol were aeolian; (2) Fengning loess underwent weak chemical weathering and paleosol underwent moderate chemical weathering. Compared with the typical aeolian deposits, the sequence of chemical weathering intensity is as follows: Xuancheng aeolian red earth > > Xifeng red clay and Zhenjiang Xiashu loess > Fengning paleosol and Luochuan paleosol > Luochuan loess > Fengning leoss; (3) The migration feature of major elements reveal that Fengning loess and paleosol finished the primary process of chemical weathering characterized by leaching of Ca and Na, and almost reached the secondary process characterized by leaching of K; (4) The scatter diagram of K₂O/Al₂O₃ and Fe₂O₃/Al₂O₃ are similar to that of Luochuan loess, Luochuan paleosol, Zhenjiang Xiashu loess and Xifeng red clay, indicating that these aeolian deposits might have the same source. The ratio of TiO₂/ Al₂O₃ is less than that of other aeolian deposits, indicating that Fengning loess and paleosol have other source.
- Fengning loess-paleosol,
- genesis,
- chemical weathering intensity,
- element migration,
- provenance,
- geochemistry

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References(46)

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Elemental Composition Features of Loess-Paleosol Profile in Fengning, Hebei Province

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