Interpreting the seasonal and long-term trend of nitrate in both groundwater and spring water in a typical headwater wetland with well-defined groundwater flow pathways
Interpreting the seasonal and long-term trend of nitrate in both groundwater and spring water in a typical headwater wetland with well-defined groundwater flow pathways
复制标题
解释具有明确地下水流路径的典型水源湿地地下水和泉水中硝酸盐的季节和长期趋势
DOI:
10.2166/ws.2016.047
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发表时间:
2016
期刊:
影响因子:
--
通讯作者:
Xing Li
中科院分区:
文献类型:
--
作者:
Yingjie Cao;C. Tang;Z. Han;Sako Yoko;Xing Li
Time scale problems of nitrate behavior (i.e. seasonal variation and long-term trend) in headwater are closely related to its hydrological process. In a typical agricultural headwater catchment in the Chiba prefecture, Japan, the groundwater nitrate concentration showed an increasing trend, while for spring water, a substantial decreasing trend was observed during our monitoring period. Two key issues, (1) identification of multiple flow pathways and (2) evaluation of the residence time for different pathways, were emphasized to reveal the factors controlling the different patterns of nitrate trend. Three major flow pathways including vertical soil water flow (VF), lateral groundwater flow (LG) and deep groundwater flow (DG) along the upland-slope-valley were discriminated. Different time scale of three flow pathways was identified. The residence time of VF was calculated as 9–10 years based on the soil water budget equation and the apparent age of LG was estimated as 41 years by chlorofluorocarbons traces. The increasing trend of NO3− in groundwater agreed well with the historical nitrate loading. And the decreasing trend of NO3− in spring was mainly influenced by nitrate behavior of LF, which substantially decreased due to reduction of nitrogen fertilizer loadings since 2000.