Arid
Source identification of nitrate in the upper aquifer system of the Wadi Shueib catchment area in Jordan based on stable isotope composition
Obeidat Mutawakil; Awawdeh Muheeb; Al-Kharabsheh Noor; Al-Ajlouni Ahmad
来源期刊干旱区科学
ISSN1674-6767
出版年2021
卷号13期号:4页码:1674-6767
英文摘要Groundwater forms the main freshwater supply in arid and semi-arid areas, and contamination of this precious resource is complicated by the slow rate of recharge in these areas. Nitrate contamination of groundwater is a global water quality problem, as it entails threat to human health as well as aquatic ecosystems. Source identification of contamination is the cornerstone and a prerequisite for any effective management program of water quality. Stable isotope composition of the dissolved nitrate (delta~(15)N-NO_3~- and delta~(18)O-NO_3~-) has been applied to identify NO_3~- sources and the main transformation processes in the upper aquifer system (A1/2, A4, and B2/A7 aquifers) in the Wadi Shueib catchment area, Jordan. Moreover, the stable isotope compositions of the groundwater (delta2H-H_2O and delta~(18)O-H_2O) in conjunction with the groundwater hydrochemistry were integrated to investigate the origin and evolution of the groundwater. Results revealed that groundwater in the study area is fresh and hard-very hard water, and mainly a Ca-Mg- Cl type. NO_3~- concentration was in the range of 7.0-74.0 mg/L with an average of 37.0 mg/L. Most of the samples showed concentration higher than the natural background concentration of NO_3~- (5.0-10.0 mg/L). The delta2H-H_2O and delta~(18)O-H_2O values indicated that the groundwater is meteoric, and of Mediterranean origin, with a strong evaporation effect. The delta~(15)N-NO_3~- values ranged between 6.0 and 11.3 with an average of 8.7, and the delta~(18)O-NO_3~- values ranged between 1.6 and 5.9 with an average of 3.4. These values are in conformity with the stable isotope composition of nitrate derived the nitrification of wastewater/manure, and soil NH4. Nitrification and denitrification are the main transformation processes affecting nitrogen species. Statistical analysis revealed no significant differences in the delta2H-H_2O and delta~(18)OH_2O values, and delta~(15)N-NO_3~- and delta~(18)O-NO_3~- values for the three aquifers (A1/2, A4, and B2/A7), indicating that the groundwater of these aquifers has the same origin, and a common source of pollution.
英文关键词delta~(15)N-NO_3~- delta~(18)O-NO_3~- nitrate sources pollution meteoric origin aquifer Jordan
类型Article
语种英语
国家中国
收录类别CSCD
WOS类目Environmental Sciences & Ecology
CSCD记录号CSCD:6959617
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/365043
作者单位Obeidat Mutawakil, Faculty of Science and Arts, Jordan University of Science and Technology, Irbid, 22110, Jordan.; Al-Ajlouni Ahmad, Faculty of Science and Arts, Jordan University of Science and Technology, Irbid, 22110, Jordan.; Awawdeh Muheeb, Laboratory of Applied Geoinformatics, Department of Earth and Environmental Sciences, Yarmouk University, Irbid, 21163, Jordan.; Al-Kharabsheh Noor, Department of Water Resources and Environmental Management, Al-Balqa Applied University, Al-Salt, 19117, Jordan.
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Obeidat Mutawakil,Awawdeh Muheeb,Al-Kharabsheh Noor,et al. Source identification of nitrate in the upper aquifer system of the Wadi Shueib catchment area in Jordan based on stable isotope composition[J],2021,13(4):1674-6767.
APA Obeidat Mutawakil,Awawdeh Muheeb,Al-Kharabsheh Noor,&Al-Ajlouni Ahmad.(2021).Source identification of nitrate in the upper aquifer system of the Wadi Shueib catchment area in Jordan based on stable isotope composition.干旱区科学,13(4),1674-6767.
MLA Obeidat Mutawakil,et al."Source identification of nitrate in the upper aquifer system of the Wadi Shueib catchment area in Jordan based on stable isotope composition".干旱区科学 13.4(2021):1674-6767.
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