To investigate nitrate sources in the aquifer consisting of unconsolidated limestone, stable isotope of nitrogen (δ
15N) was measured in shallow groundwater from wells and springs under three land-use settings. The typical land-use settings and corresponding average nitrate concentrations and δ
15N values were : residental areas,7.1mg/L and 8.0‰; agricultural areas,7.2mg/L and 5.2‰; and natural, undeveloped areas,5.3mg/L and 5.6‰, respectively. Average 15N values of urine sewages and commercial inorganic fertilizers were 18.10‰ and 0.5‰, respectively. Values of δ
15N greater than 7‰ in residental areas suggest that nitrogen from sewages exists in groundwater. Values of δ
15N less than 7‰ in agricultural areas and a part of natural, undeveloped areas suggest that nitrogen in groundwater was supplied by commercial inorganic fertilizers. Low nitrate concentarations and low values of δ
15N in residental areas were caused by dilution with groundwater influenced by commercial fertilizers flowing into residental areas. High δ
15N values in agricultural areas suggested that denitrification occurred actively.
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