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Permeability and Groundwater Enrichment Characteristics of the Loess-Paleosol Sequence in the Southern Chinese Loess Plateau

文献类型：期刊论文

作者Shao, Tianjie1,5; Wang, Ruojin5; Xu, Zhiping5; Wei, Peiru5; Zhao, Jingbo2,5; Niu, Junjie4; Song, Dianxing3
刊名WATER
出版日期2020-03-01
卷号12期号:3页码:16
关键词permeability groundwater resource palaeoclimatic change loess-paleosol sequence Chinese Loess Plateau
DOI10.3390/w12030870
通讯作者Zhao, Jingbo(zhaojb@snnu.edu.cn) ; Niu, Junjie(junjieniu@foxmail.com)
英文摘要To determine the permeability characteristics and the groundwater enrichment conditions of loess and paleosol layers, this article systematically investigated the permeability, magnetic susceptibility, porosity, and carbonate mass percentage of representative loess-paleosol layers (L1 to S5) on the Bailu tableland in the Chinese Loess Plateau south. The result of in situ permeability measurements showed that the average time to reach quasi-steady infiltration of loess layers is shorter than that of paleosol layers. In addition, loess layers have higher porosity and better water storage spaces than paleosol layers and were prone to form aquifers. Paleosol layers, on the contrary, are more likely to form aquitards. The difference between loess and paleosol in permeability, porosity and groundwater enrichment conditions is largely attributed to lower intensity pedogenesis of loess, which is in turn ascribed to the colder and drier palaeoclimatic conditions. It is worth mentioning that the CaCO3 concretion layer is a good aquifuge for its compact structure. Generally, the empirical formula of the Koctakob formula is applicable for describing the permeability rule of loess and paleosol layers, and the parameters of the empirical formulas can provide an important reference for hydrological and agricultural departments. In this regard, the Quaternary climatic change theory can contribute to the hydrogeology of the Chinese Loess Plateau, and the regional climatostratigraphy can be regarded as a baseline for local water resource positioning and revegetation in such a semi-arid area, which broadens the application field of Quaternary climatic change theory. Meanwhile, it also provides a reference path for solving water shortages of other loess distribution areas in China and other countries.
WOS关键词MAGNETIC-SUSCEPTIBILITY ; PALEOCLIMATIC SIGNIFICANCE ; SEDIMENTS ; DEPOSITS ; CAPACITY ; RECORDS ; MODELS ; ZONE
资助项目National Natural Science Foundation of China[41171423] ; Fundamental Research Funds for the Central Universities[GK201803055] ; Shaanxi Province Postdoctoral Science Foundation[2016BSHEDZZ27]
WOS研究方向Water Resources
语种英语
WOS记录号WOS:000529249500255
出版者MDPI
资助机构National Natural Science Foundation of China ; Fundamental Research Funds for the Central Universities ; Shaanxi Province Postdoctoral Science Foundation
源URL[http://ir.ieecas.cn/handle/361006/13976]  
专题地球环境研究所_黄土与第四纪地质国家重点实验室（2010~）
通讯作者Zhao, Jingbo; Niu, Junjie
作者单位1.Shaanxi Normal Univ, SNNU JSU Joint Res Ctr Nanoenvironm Sci & Hlth, Xian 710062, Peoples R China
2.Chinese Acad Sci, Earth Environm Inst, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China
3.Baoji Univ Arts & Sci, Shaanxi Key Lab Disaster Monitoring & Mech Modeli, Baoji 721013, Peoples R China
4.Taiyuan Normal Univ, Res Ctr Sci Dev Fenhe River Basin, Taiyuan 030001, Peoples R China
5.Shaanxi Normal Univ, Coll Geog Sci & Tourism, Xian 710062, Peoples R China
推荐引用方式
GB/T 7714		 Shao, Tianjie,Wang, Ruojin,Xu, Zhiping,et al. Permeability and Groundwater Enrichment Characteristics of the Loess-Paleosol Sequence in the Southern Chinese Loess Plateau[J]. WATER,2020,12(3):16.
APA Shao, Tianjie.,Wang, Ruojin.,Xu, Zhiping.,Wei, Peiru.,Zhao, Jingbo.,...&Song, Dianxing.(2020).Permeability and Groundwater Enrichment Characteristics of the Loess-Paleosol Sequence in the Southern Chinese Loess Plateau.WATER,12(3),16.
MLA Shao, Tianjie,et al."Permeability and Groundwater Enrichment Characteristics of the Loess-Paleosol Sequence in the Southern Chinese Loess Plateau".WATER 12.3(2020):16.

入库方式： OAI收割

来源：地球环境研究所

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