Climate Change Data Portal
DOI | 10.1002/hyp.15086 |
Spatial and temporal groundwater dynamics in extreme arid basins | |
Wei, Xuan; Guo, Yuchuan; Zhou, Mingtong; Wang, Ning; Wang, Huijing; Bai, Yunbao | |
发表日期 | 2024 |
ISSN | 0885-6087 |
EISSN | 1099-1085 |
起始页码 | 38 |
结束页码 | 2 |
卷号 | 38期号:2 |
英文摘要 | To accurately obtain the spatial distribution characteristics of groundwater level in an extremely arid zone and its dynamic change patterns under the influence of human activities, based on the data of 55 groundwater observation wells in the middle and lower reaches of the Kriya River, spatial interpolation of regional groundwater level data were performed using the inverse distance weight, spline function, trend surface, and the ordinary kriging methods. The optimal interpolation method was selected by its accuracy to spatially interpolate the groundwater level data in the study area from 2019 to 2021. The results show that: (1) the ordinary kriging method has the highest interpolation accuracy (MAE = 7.1393, MRE = 0.0058, RMSE = 9.4314) and reflects the spatial and temporal variability and distribution characteristics of groundwater levels with great accuracy. (2)The relationship between surface water-groundwater recharge and discharge in different areas of the river channel in the desert section varies depending on geological structure, surface water seepage, and other elements. (3) Groundwater in the Taklamakan Desert has little effect on groundwater recharge in the Dariyabui Oasis, and changes in groundwater dynamics in the oasis are predominantly influenced by surface runoff. (4) Monthly changes in groundwater levels in the Yutian Oasis are continuous, with 'V' shaped fluctuations, a declining trend in the southern part, no significant change in the central part, and a slight increase in the northern part. These results contribute to the sustainable management of water resources in the Kriya River Basin, provide a basis for groundwater prediction, and offer a reference for studies of other, similar extreme desert area basins. Ordinary kriging is optimal for groundwater interpolation in extreme arid zones; Analysis of the river channel in the desert section recharge relationships; Independently of the season and evaporation change, the groundwater in Taklimakan Desert has little effect on the groundwater recharge in Dariyabui Oasis. image |
英文关键词 | extreme arid zone; groundwater; Kriya River; spatial and temporal distribution; spatial interpolation preference |
语种 | 英语 |
WOS研究方向 | Water Resources |
WOS类目 | Water Resources |
WOS记录号 | WOS:001156029400001 |
来源期刊 | HYDROLOGICAL PROCESSES
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/303935 |
作者单位 | Xinjiang University; Xinjiang University; Xinjiang University |
推荐引用方式 GB/T 7714 | Wei, Xuan,Guo, Yuchuan,Zhou, Mingtong,et al. Spatial and temporal groundwater dynamics in extreme arid basins[J],2024,38(2). |
APA | Wei, Xuan,Guo, Yuchuan,Zhou, Mingtong,Wang, Ning,Wang, Huijing,&Bai, Yunbao.(2024).Spatial and temporal groundwater dynamics in extreme arid basins.HYDROLOGICAL PROCESSES,38(2). |
MLA | Wei, Xuan,et al."Spatial and temporal groundwater dynamics in extreme arid basins".HYDROLOGICAL PROCESSES 38.2(2024). |
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