中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Mid-Holocene soil water and vegetation in the Xi'an area of the southern Chinese Loess Plateau

文献类型:期刊论文

作者Yue, Da-Peng1; Zhao, Jing-Bo2,3; Ma, Yan-Dong4; Cao, Jun-Ji3; Li, Yan-Hua1; Ma, Ai-Hua1; Liu, Xiu-Ming5
刊名GEODERMA
出版日期2021-02-01
卷号383页码:9
关键词Mid-Holocene palaeosol Palaeo-rainfall Palaeo-vegetation Palaeo-soil water Palaeo-hydrologic cycle
ISSN号0016-7061
DOI10.1016/j.geoderma.2020.114802
通讯作者Zhao, Jing-Bo(zhaojb@snnu.edu.cn) ; Ma, Yan-Dong(mayandongemail@163.com)
英文摘要This paper investigates mid-Holocene palaeo-vegetation and soil water in the Xi'an area of the southern Chinese Loess Plateau (CLP). A well-dated (8.5-6.0 ka BP and 5.0-3.1 ka BP) loess-palaeosol (unit S-0) was logged, sampled and analyzed at four sites in the Xi'an area of the southern CLP, from which we report soil micromorphological (type and occurrence of root pores), particle size and geochemical data (CaCO3 and Sr concentration) to: (i) infer changes in soil water content, (ii) infer the limits of gravity water and the types of hydrologic cycle, and (iii) reconstruct the palaeovegetation. Numerous woody plant root holes were identified (2-4 mm diameter) within the illuvial horizon underlying palaeosol S-0, the morphology of which is consistent with those produced by woody plants. The clay-rich argillic horizon of palaeosol S-0 was found to contain high concentrations of kaolinite, which in concert with the geochemical indices, indicates that soil gravity water attained a depth of 2.2-2.8 m, whilst soil water content was similar to 20-25%. This implies that pedogenic processes at this site were more intense during the mid- compared to late Holocene loessic soils elsewhere on the CLP, and ultimately attests to relatively wet climatic conditions (e.g. up to 800 mm yr(-1) rainfall), the hydrologic cycle type of precipitation-soil water-groundwater, and the vegetation of deciduous broad-leaved forest. We propose that combined analyses of root-channel morphology and mobile element geochemistry can be used to infer changes in palaeo-hydrology and ultimately, the strength of the Asian Summer Monsoon.
WOS关键词MILLENNIAL-SCALE ; ASIAN MONSOON ; HOLOCENE ; PALEOSOL ; MOUNTAINS ; STRENGTH ; CLIMATE ; BASIN
资助项目National Natural Science Foundation of China[41772180] ; National Natural Science Foundation of China[41930641] ; National Natural Science Foundation of China[41901034] ; Key Laboratory of Aerosol Chemistry and Physics, Institute of Earth Environment, Chinese Academy of Sciences, China[KLACP201904] ; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences[SKLLQG1713] ; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences[SKLLQG1847]
WOS研究方向Agriculture
语种英语
WOS记录号WOS:000590747800032
出版者ELSEVIER
资助机构National Natural Science Foundation of China ; Key Laboratory of Aerosol Chemistry and Physics, Institute of Earth Environment, Chinese Academy of Sciences, China ; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences
源URL[http://ir.ieecas.cn/handle/361006/15618]  
专题地球环境研究所_粉尘与环境研究室
通讯作者Zhao, Jing-Bo; Ma, Yan-Dong
作者单位1.Shaanxi Normal Univ, Sch Geog & Tourism, Xian 710119, Shaanxi, Peoples R China
2.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Shaanxi, Peoples R China
3.Chinese Acad Sci, Inst Earth Environm, Key Lab Aerosol Chem & Phys, Xian 710061, Shaanxi, Peoples R China
4.Changan Univ, Key Lab Subsurface Hydrol & Ecol Effects Arid Reg, Minist Educ, Xian 710054, Shaanxi, Peoples R China
5.Fujian Normal Univ, Sch Geog, Fuzhou 350000, Fujian, Peoples R China
推荐引用方式
GB/T 7714
Yue, Da-Peng,Zhao, Jing-Bo,Ma, Yan-Dong,et al. Mid-Holocene soil water and vegetation in the Xi'an area of the southern Chinese Loess Plateau[J]. GEODERMA,2021,383:9.
APA Yue, Da-Peng.,Zhao, Jing-Bo.,Ma, Yan-Dong.,Cao, Jun-Ji.,Li, Yan-Hua.,...&Liu, Xiu-Ming.(2021).Mid-Holocene soil water and vegetation in the Xi'an area of the southern Chinese Loess Plateau.GEODERMA,383,9.
MLA Yue, Da-Peng,et al."Mid-Holocene soil water and vegetation in the Xi'an area of the southern Chinese Loess Plateau".GEODERMA 383(2021):9.

入库方式: OAI收割

来源:地球环境研究所

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