Hydrochemical and stable isotopic assessment of nitrate contamination in an alluvial aquifer underneath a riverside agricultural field
- Authors
- Chae, Gi-Tak; Yun, Seong-Taek; Mayer, Bernhard; Choi, Byoung-Young; Kim, Kyoung-Ho; Kwon, Jang-Soon; Yu, Soon-Young
- Issue Date
- 12월-2009
- Publisher
- ELSEVIER
- Keywords
- Nitrate; Groundwater pollution; Riverside alluvium aquifer; Nitrogen and oxygen isotopes; Mass balance modeling
- Citation
- AGRICULTURAL WATER MANAGEMENT, v.96, no.12, pp.1819 - 1827
- Indexed
- SCIE
SCOPUS
- Journal Title
- AGRICULTURAL WATER MANAGEMENT
- Volume
- 96
- Number
- 12
- Start Page
- 1819
- End Page
- 1827
- URI
- https://scholar.korea.ac.kr/handle/2021.sw.korea/118874
- DOI
- 10.1016/j.agwat.2009.08.001
- ISSN
- 0378-3774
- Abstract
- Major ions and stable isotopic (delta D-water, delta O-18(water), delta O-18(nitrate)) measurements in concert with hydrochemical modeling were used in order to elucidate the sources and geochemical processes controlling nitrate contamination of shallow alluvial groundwater underneath a riverside agricultural field in the Buyeo area, Korea. Beneath vegetable fields in the sandy soil, the mean nitrate concentration of groundwater was 148.6 mg/L, which is significantly higher than in groundwater (mean 28.8 mg/L) beneath silty soils underneath rice paddy fields. Nitrogen isotope data indicate that synthetic fertilizers are the predominant source of groundwater nitrate in the study area. Denitrification during recharge through rice paddy soils appears to be responsible for the lower nitrate concentrations in groundwater beneath the silty soil zone. The relationship between nitrogen and oxygen isotope data of nitrate also suggests mixing of two different groundwater bodies with nitrates from the silt zone and the sand zone. Geochemical mass balance modeling on hydrochemical data indicates that various agricultural chemicals such as urea, lime, magnesium sulfate and potassium chloride dissolve in vegetable fields of the sandy zone, resulting in significant enrichment of various solutes such as K+, Ca2+, Mg2+, NO3-, SO42- and Cl-. As a consequence of over-utilization of synthetic nitrogen fertilizers, the sand zone is characterized by very high nitrate concentrations in the groundwater. This study suggests that a reduction of over-fertilization especially on vegetable fields in the riverside sand zone is required to minimize the nitrate contamination of groundwater. This study also shows that combination of geochemical and isotopic techniques with simple mass balance modeling provides information about the causes and processes of nitrate contamination of groundwater underneath a riverside agricultural field. The study also provides sustainable measures to optimize fertilization rate as an important basis of eco-friendly agriculture. (C) 2009 Elsevier B.V. All rights reserved.
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