Next Article in Journal
Coupled Multifield Response to Coordinate Mining of Coal and Uranium: A Case Study
Next Article in Special Issue
Long-Term Isotope Records of Precipitation in Zagreb, Croatia
Previous Article in Journal
Numerical Simulation of the Fluid–Solid Coupling Mechanism of Internal Erosion in Granular Soil
Previous Article in Special Issue
What Do Plants Leave after Summer on the Ground?—The Effect of Afforested Plants in Arid Environments
Open AccessReview

Stable Isotopes of Water and Nitrate for the Identification of Groundwater Flowpaths: A Review

1
Department of Science Education, Ewha Womans University, Seoul 03760, Korea
2
Groundwater Department, Geologic Environment Division, Korea Institute of Geoscience and Mineral Resources, Daejeon 34132, Korea
3
Water Quality Research Center, K-Water Convergence Institute, Daejeon 34350, Korea
4
Department of Earth and Environmental Sciences & The Earth and Environmental Science System Research Center, Jeonbuk National University, Jeonju 54896, Korea
*
Author to whom correspondence should be addressed.
Water 2020, 12(1), 138; https://doi.org/10.3390/w12010138
Received: 1 December 2019 / Revised: 26 December 2019 / Accepted: 30 December 2019 / Published: 1 January 2020
(This article belongs to the Special Issue Use of Water Stable Isotopes in Hydrological Process)
Nitrate contamination in stream water and groundwater is a serious environmental problem that arises in areas of high agricultural activities or high population density. It is therefore important to identify the source and flowpath of nitrate in water bodies. In recent decades, the dual isotope analysis (δ15N and δ18O) of nitrate has been widely applied to track contamination sources by taking advantage of the difference in nitrogen and oxygen isotope ratios for different sources. However, transformation processes of nitrogen compounds can change the isotopic composition of nitrate due to the various redox processes in the environment, which often makes it difficult to identify contaminant sources. To compensate for this, the stable water isotope of the H2O itself can be used to interpret the complex hydrological and hydrochemical processes for the movement of nitrate contaminants. Therefore, the present study aims at understanding the fundamental background of stable water and nitrate isotope analysis, including isotope fractionation, analytical methods such as nitrate concentration from samples, instrumentation, and the typical ranges of δ15N and δ18O from various nitrate sources. In addition, we discuss hydrograph separation using the oxygen and hydrogen isotopes of water in combination with the nitrogen and oxygen isotopes of nitrate to understand the relative contributions of precipitation and groundwater to stream water. This study will assist in understanding the groundwater flowpaths as well as tracking the sources of nitrate contamination using the stable isotope analysis in combination with nitrate and water. View Full-Text
Keywords: groundwater; isotope hydrology; stable water isotopes; stable nitrate isotopes groundwater; isotope hydrology; stable water isotopes; stable nitrate isotopes
Show Figures

Figure 1

MDPI and ACS Style

Jung, H.; Koh, D.-C.; Kim, Y.S.; Jeen, S.-W.; Lee, J. Stable Isotopes of Water and Nitrate for the Identification of Groundwater Flowpaths: A Review. Water 2020, 12, 138.

Show more citation formats Show less citations formats
Note that from the first issue of 2016, MDPI journals use article numbers instead of page numbers. See further details here.

Article Access Map by Country/Region

1
Back to TopTop