Holocene climate and soil water balance in Baoji Region of Southern Loess Plateau
文献类型：期刊论文
| 作者 | Chu, Chun-Jie5; Zhao, Jing-Bo2,3,4; Guo, Nan2; Shao, Tian-Jie2; Ma, Yan-Dong1; Su, Min2; Zhu, Ya-Di2 |
| 刊名 | CATENA
 |
| 出版日期 | 2022-03-01 |
| 卷号 | 210页码:10 |
| 关键词 | Holocene paleosol water content Holocene environment Holocene water balance Paleowater index Southern Loess Plateau |
| ISSN号 | 0341-8162 |
| DOI | 10.1016/j.catena.2021.105941 |
| 通讯作者 | Zhao, Jing-Bo(zhaojb@snnu.edu) ; Ma, Yan-Dong(mayandongemail@163.com) |
| 英文摘要 | In this paper, changes in the Holocene climate, soil water and soil resources in Southern Loess Plateau are studied based on field investigation, grain size and chemical analysis. The purpose is to reveal the impact of the Holocene environmental change on soil water and human activities. The study shows that the mid-Holocene paleosol S0 in Baoji Region had a CaCO3 content close to 0, was enriched with Fe2O3, Al2O3, was of homogenous dense silty microstructure containing red argillans and had moderate chemical weathering. This shows that the paleosol is luvisol. The mean annual precipitation was about 800 mm at that time. The late-Holocene loess had a high CaCO3 content, low Fe2O3 and Al2O3 content and of pore-developed crumb microstructure, indicating that the climate was cold and dry. The migration depth of CaCO3 and Sr in the mid-Holocene paleosol indicates that the distribution depth of gravity water in the soil at that time reached 1.8 m, and the water content in the soil above 1.8 m during the vegetation growing season was higher than 20%. This made it suitable for the development of forest vegetation. The migration depth of CaCO3 in the Holocene loess was small and the water content in the layers of loess during rainy season was generally lower than 12%; thus, it was not suitable for the development of forest vegetation. In the mid-Holocene soil, water intake was greater than water consumption and soil water was positive balance. Moreover, trace elements, organic matters, water holding capacity and water content in S0 were higher than those in the early-Holocene and late-Holocene loess, which facilitated agricultural production and human activities. In fact, it is also the primary reason that the mid-Holocene village sites are significantly larger in quantity and greater in scale than the early-Holocene and late-Holocene village sites. |
| WOS关键词 | PALEOSOL SEQUENCE ; CHINA ; EVOLUTION ; ARIDITY ; IMPACT ; BASIN |
| 资助项目 | National Natural Science Founda-tion of China[42130507] ; Key Laboratory of Aerosol Chemistry and Physics, Institute of Earth Environment, Chinese Acad-emy of Sciences, China[KLACP-1904] ; State Key Labo-ratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, China[SKLLQG2013] ; State Key Labo-ratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, China[SKLLQG1934] ; State Key Labo-ratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, China[SKLLQG2106] |
| WOS研究方向 | Geology ; Agriculture ; Water Resources |
| 语种 | 英语 |
| WOS记录号 | WOS:000787584100001 |
| 出版者 | ELSEVIER |
| 资助机构 | National Natural Science Founda-tion of China ; Key Laboratory of Aerosol Chemistry and Physics, Institute of Earth Environment, Chinese Acad-emy of Sciences, China ; State Key Labo-ratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, China |
| 源URL | [http://ir.ieecas.cn/handle/361006/17707]  |
| 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, Jing-Bo; Ma, Yan-Dong |
| 作者单位 | 1.Shaanxi Acad Forestry, Key Lab State Forestry Adm Soil & Water Conservat, Xian 710082, Peoples R China 2.Shaanxi Normal Univ, Sch Geog & Tourism, Xian 710062, Shaanxi, Peoples R China 3.Chinese Acad Sci, Inst Earth Environm, Shaanxi Key Lab Atmospher & Haze Fog Pollut Preve, Xian 710061, Shaanxi, Peoples R China 4.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Shaanxi, Peoples R China 5.Pingdingshan Univ, Coll Resources & Environm Sci, Pingdingshan 467000, Henan, Peoples R China |
| 推荐引用方式 GB/T 7714 | Chu, Chun-Jie,Zhao, Jing-Bo,Guo, Nan,et al. Holocene climate and soil water balance in Baoji Region of Southern Loess Plateau[J]. CATENA,2022,210:10. |
| APA | Chu, Chun-Jie.,Zhao, Jing-Bo.,Guo, Nan.,Shao, Tian-Jie.,Ma, Yan-Dong.,...&Zhu, Ya-Di.(2022).Holocene climate and soil water balance in Baoji Region of Southern Loess Plateau.CATENA,210,10. |
| MLA | Chu, Chun-Jie,et al."Holocene climate and soil water balance in Baoji Region of Southern Loess Plateau".CATENA 210(2022):10. |
入库方式： OAI收割
来源：地球环境研究所
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