Impact of land use on nitrogen concentration in groundwater and river water

被引:8
|
作者
Yoshikawa, Seiko [1 ]
Takahashi, Hidehiro [2 ]
Sasada, Yasuko [3 ]
Mochizuki, Hidetoshi [2 ]
机构
[1] Natl Inst Agroenvironm Sci, Carbon & Nutrient Cycles Div, Tsukuba, Ibaraki 3058604, Japan
[2] NARO, Farming Syst & Agroenvironm Technol Res Div, Western Reg Agr Res Ctr, Fukuyama, Hiroshima 7218614, Japan
[3] Kagawa Pref Res Inst Environ Sci Publ Hlth, Takamatsu, Kagawa 7610104, Japan
关键词
land use; specific concentration; pollution load of non-point source; non-absorbed applied N; groundwater; STREAM WATER; POLLUTION; JAPAN; AGRICULTURE; HOKKAIDO; QUALITY; AREAS;
D O I
10.1080/00380768.2015.1104521
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
The 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 (1342km(2)) 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 15.2mgL(-1), 10.3mgL(-1), 2.3mgL(-1) and 2.5mgL(-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 19.3kgha(-1)y(-1), 7.7kgha(-1)y(-1), 1.7kgha(-1)y(-1) and 7.6kgha(-1)y(-1), while the G-N pollution load arrival was 7.3kgha(-1)y(-1), 5.0kgha(-1)y(-1), 1.1kgha(-1)y(-1) and 1.2kgha(-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 (r(2)=0.68) except for one small, high-density, urban watershed, and a weak linear correlation was observed between NAA-N and G-N concentrations (r(2)=0.42).
引用
收藏
页码:898 / 909
页数:12
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