Water movement and solute transport in deep vadose zone under four irrigated agricultural land-use types in the North China Plain
文献类型:期刊论文
作者 | Min, Leilei1; Shen, Yanjun1; Pei, Hongwei2; Wang, Ping3![]() |
刊名 | JOURNAL OF HYDROLOGY
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出版日期 | 2018-04-01 |
卷号 | 559页码:510-522 |
关键词 | Agricultural land-use types Deep vadose zone Groundwater recharge Solute transport North China Plain |
ISSN号 | 0022-1694 |
DOI | 10.1016/j.jhydrol.2018.02.037 |
通讯作者 | Shen, Yanjun(yjshen@sjziam.ac.cn) |
英文摘要 | Groundwater-fed agriculture has caused water table declines and groundwater quality degradation in the North China Plain. Based on sediment sampling in deep vadose zone (with a maximum depth of 11.0 m), groundwater recharge, seepage velocity, solute inventory and transport under four typical irrigated agricultural land-use types (winter wheat and summer maize, WM; pear orchards, PO; outdoor vegetables, VE; and cotton, CO) were investigated in this study. The results reveal that there are many solutes stored in the vadose zone. Nitrate storage per unit depth in the vadose zone is highest under PO (1703 kg/ha), followed by VE (970 kg/ha), WM (736 kg/ha) and CO (727 kg/ha). However, the amount of annual leached nitrate under the four land-use types results in a different order (VE, 404 kg/ha; WM, 108 kg/ha; PO, 23 kg/ha; CO, 13 kg/ha). The estimated average recharge rates are 180 mm/yr for WM, 27 mm/yr for CO, 320 mm/yr for VE and 49 mm/yr for PO. The seepage velocity under VE (2.22 m/yr) exceeds the values under the other three land-use types (WM, 0.85 m/yr; PO, 0.49 m/yr; CO, 0.09 m/yr). The highest seepage velocity under VE caused significant nitrate contamination in groundwater, whereas the other two land-use types (WM and PO) had no direct influence on groundwater quality. The results of this work could be used for groundwater resources management. (C) 2018 Elsevier B.V. All rights reserved. |
WOS关键词 | ESTIMATING GROUNDWATER RECHARGE ; ROTATE-N MODEL ; UNSATURATED ZONE ; ENVIRONMENTAL TRACERS ; CROPPING SYSTEMS ; UNITED-STATES ; SPATIAL VARIABILITY ; TYPICAL CROPLAND ; CITRUS ORCHARDS ; PIEDMONT REGION |
资助项目 | National Natural Scientific Foundation of China (NSFC)[41561124015] ; National Natural Scientific Foundation of China (NSFC)[41501035] ; National Natural Scientific Foundation of China (NSFC)[41471027] |
WOS研究方向 | Engineering ; Geology ; Water Resources |
语种 | 英语 |
WOS记录号 | WOS:000430902000039 |
出版者 | ELSEVIER SCIENCE BV |
资助机构 | National Natural Scientific Foundation of China (NSFC) |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/55089] ![]() |
专题 | 中国科学院地理科学与资源研究所 |
通讯作者 | Shen, Yanjun |
作者单位 | 1.Chinese Acad Sci, Inst Genet & Dev Biol, Ctr Agr Resources Res, Key Lab Agr Water Resources, Shijiazhuang 050021, Hebei, Peoples R China 2.Hebei Univ Architecture, Sch Energy & Environm Engn, 13 West Chaoyang St, Zhangjiakou 075000, Peoples R China 3.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, 11A Datun Rd, Beijing 100101, Peoples R China |
推荐引用方式 GB/T 7714 | Min, Leilei,Shen, Yanjun,Pei, Hongwei,et al. Water movement and solute transport in deep vadose zone under four irrigated agricultural land-use types in the North China Plain[J]. JOURNAL OF HYDROLOGY,2018,559:510-522. |
APA | Min, Leilei,Shen, Yanjun,Pei, Hongwei,&Wang, Ping.(2018).Water movement and solute transport in deep vadose zone under four irrigated agricultural land-use types in the North China Plain.JOURNAL OF HYDROLOGY,559,510-522. |
MLA | Min, Leilei,et al."Water movement and solute transport in deep vadose zone under four irrigated agricultural land-use types in the North China Plain".JOURNAL OF HYDROLOGY 559(2018):510-522. |
入库方式: OAI收割
来源:地理科学与资源研究所
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