Impact of land use on nitrogen concentration in groundwater and river water |
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Authors: | Seiko Yoshikawa Hidehiro Takahashi Yasuko Sasada Hidetoshi Mochizuki |
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Affiliation: | 1. Carbon and Nutrient Cycles Division, National Institute for Agro-environmental Sciences, Kannondai 3-1-3, Tsukuba, 305-8604 Japanseikoyo@affrc.go.jp;3. Farming Systems and Agro-environmental Technologies Research Division, Western Region Agricultural Research Center, NARO, Nishi-fukatsu 6-12-1, Fukuyama, 721-8614 Japan;4. (former) Kagawa Pref. Res. Inst. Environ. Sci. Public Health, Takamatsu-cho 1673-3, Takamatsu, 761-0104 Japan |
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Abstract: | AbstractThe aim of this study was to evaluate the impact of land use on nitrate nitrogen (NO3-N) in shallow groundwater (G-N) and total nitrogen (N) in river water (R-N). The study area consisted of 26 watersheds (1342 km2) covering 72% of Kagawa Prefecture in Japan. We estimated G-N specific concentrations, which showed the magnitude of the upland fields, paddy fields, forests and urban land-use contributions to watershed-mean G-N. G-N specific concentrations were gained as partial regression coefficients using a multiple regression analysis of the watershed-mean G-N concentrations and the land-use ratios in each of the 26 watersheds. The results showed that the G-N specific concentration, which was gained as the partial regression coefficient for the multiple regression analysis, was 15.2 mg L?1, 10.3 mg L?1, 2.3 mg L?1 and 2.5 mg L?1 for the upland fields, paddy fields, forests and urban land-use types, respectively. R-N pollution load runoff to the river mouth was calculated by multiplying R-N specific concentration (previously reported) by river flow at the river mouth. Similarly, G-N pollution load arrival to groundwater was calculated by multiplying G-N specific concentration by the groundwater flow. The R-N pollution load runoff was 19.3 kg ha?1 y?1, 7.7 kg ha?1 y?1, 1.7 kg ha?1 y?1 and 7.6 kg ha?1 y?1, while the G-N pollution load arrival was 7.3 kg ha?1 y?1, 5.0 kg ha?1 y?1, 1.1 kg ha?1 y?1 and 1.2 kg ha?1 y?1, for upland fields, paddy fields, forests and urban areas, respectively. These results showed that the N in river water and groundwater was derived mainly from runoff and leaching from croplands. Therefore, the relationships between watershed-mean non-absorbed, applied nitrogen (NAA-N: nitrogen applied to cropland via fertilizer and manure without being absorbed by crops), R-N concentration and watershed-mean G-N concentration were investigated. A curvilinear correlation was observed between NAA-N and R-N concentrations (r2 = 0.68) except for one small, high-density, urban watershed, and a weak linear correlation was observed between NAA-N and G-N concentrations (r2 = 0.42). |
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Keywords: | land use specific concentration pollution load of non-point source non-absorbed applied N groundwater |
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