KMS Institute Of Geographic Sciences And Natural Resources Research,CAS
Hydrologic processes of groundwater in a small monsoon-influenced mountainous watershed | |
Yuan, Ruiqiang1; Wang, Shiqin2; Yang, Lihu3![]() ![]() | |
2018-12-01 | |
Source Publication | HYDROLOGY RESEARCH
![]() |
ISSN | 0029-1277 |
Volume | 49Issue:6Pages:2016-2029 |
Corresponding Author | Yuan, Ruiqiang(rqyuan@sxu.edu.cn) |
Abstract | Mountain block recharge is the least well quantified owing to the lack of a thorough understanding of mountain block hydrological processes. Observations of spatio-temporal variations of groundwater were employed to clarify hydrologic processes in a semi-arid mountainous watershed of northern China. Results showed that the annual feeding rate of precipitation changed between 21% and 40%. However, infiltration of precipitation was mainly drained as interflow on slopes and recharged into the mountain valley as focused recharge. As a result, the mean correlation coefficient between precipitation and groundwater level was only 0.20 and seasonal variations were reduced. Mountain slope is essentially impermeable with no bedrock percolation under arid circumstances. Only a bedrock percolation event occurred after multiple closely-spaced heavy rains during the four-year observation, which induced a local rapid ascending of the water table and an enhanced lateral recharge from upgradient watersheds. The influence of the enhanced lateral recharge lasted three years, suggesting a huge groundwater catchment overcoming local watershed divides in mountain blocks. The average of the gradual recession of the water table was 5.1 mm/d with a maximum of 11.4 mm/d in the beginning stage. Both interflow and bedrock percolation are important. Our results highlight the changeability of hydrologic processes in mountain watersheds. |
Keyword | bedrock percolation groundwater recharge hydrologic processes mountain block recharge mountainous watershed North China Plain |
DOI | 10.2166/nh.2018.030 |
WOS Keyword | BLOCK RECHARGE ; STABLE-ISOTOPES ; FRONT ; BALANCE ; FLOW ; CATCHMENTS ; HILLSLOPE ; BASEFLOW ; MODEL ; STEEP |
Indexed By | SCI |
Language | 英语 |
Funding Project | National Natural Science Foundation of China[41301033] ; Institute of Geographical Sciences and Natural Resources Research[2012ZD003] ; Water and Soil Conservation Station of Baoding |
Funding Organization | National Natural Science Foundation of China ; Institute of Geographical Sciences and Natural Resources Research ; Water and Soil Conservation Station of Baoding |
WOS Research Area | Water Resources |
WOS Subject | Water Resources |
WOS ID | WOS:000452413800023 |
Publisher | IWA PUBLISHING |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://ir.igsnrr.ac.cn/handle/311030/51374 |
Collection | 中国科学院地理科学与资源研究所 |
Corresponding Author | Yuan, Ruiqiang |
Affiliation | 1.Shanxi Univ, Coll Environm & Resources, Taiyuan 030006, Shanxi, Peoples R China 2.Chinese Acad Sci, Inst Genet & Dev Biol, Ctr Agr Resources Res, Shijiazhuang 050021, Hebei, Peoples R China 3.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China 4.Jiangxi Normal Univ, Sch Geog & Environm, Nanchang 330022, Jiangxi, Peoples R China |
Recommended Citation GB/T 7714 | Yuan, Ruiqiang,Wang, Shiqin,Yang, Lihu,et al. Hydrologic processes of groundwater in a small monsoon-influenced mountainous watershed[J]. HYDROLOGY RESEARCH,2018,49(6):2016-2029. |
APA | Yuan, Ruiqiang,Wang, Shiqin,Yang, Lihu,Liu, Jianrong,Wang, Peng,&Song, Xianfang.(2018).Hydrologic processes of groundwater in a small monsoon-influenced mountainous watershed.HYDROLOGY RESEARCH,49(6),2016-2029. |
MLA | Yuan, Ruiqiang,et al."Hydrologic processes of groundwater in a small monsoon-influenced mountainous watershed".HYDROLOGY RESEARCH 49.6(2018):2016-2029. |
Files in This Item: | There are no files associated with this item. |
Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.
Edit Comment