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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Impacts of Hydrological Changes on Nutrient Transport From Diffuse Sources in a Rural River Basin, Western Japan
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Impacts of Hydrological Changes on Nutrient Transport From Diffuse Sources in a Rural River Basin, Western Japan

机译:日本西部农村河流盆地弥漫源水文变化水文变化对弥漫来源的影响

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摘要

Increased frequency of heavy rainfall caused by climate change may affect nutrient transport from forests and agricultural lands into downstream rivers. However, little information is available on how the effects of land cover on nutrient concentrations in the downstream rivers change depending on hydrological conditions. To elucidate this, we investigated the effects of changes in precipitation and river discharge on the relationship between river nutrient concentrations (total nitrogen, total phosphorus, nitrate, and phosphate) and land cover in eight subbasins of the Hii River basin, western Japan. We hypothesized that coniferous forests and agricultural lands including poorly managed ones, which require thinning and fertilizer management, respectively, contribute to increases in nutrient concentrations in downstream rivers during storms. Linear mixed-effects model analyses based on 18-year observation data were used for testing the hypothesis. Results revealed that the slopes of the multiple regression analysis between nutrient concentrations and coniferous and broad-leaved forest area ratios were negative and decreased with increasing daily precipitation. This suggests that forests contributed to the dilution of river nutrient concentrations during storms regardless of whether they were coniferous or broad leaved. In contrast, the slope of regression between nutrient concentrations and agricultural area ratio revealed the opposite trend, indicating that even a small percentage of agricultural area makes a large contribution to increases in nutrient concentrations as precipitation increases. Our results imply that storm runoff in response to rainfall results in an elevated supply of nitrogen and phosphorus attached to arable soils to the river.
机译:强降雨造成气候变化的频率增加可能会影响从森林和农田养分运输到下游的河流。然而,信息很少土地覆盖的养分浓度在下游河流的影响如何变化取决于水文条件上。为了阐明这一点,我们调查了斐伊川盆地,西日本八个次盆地对河流营养物浓度之间的关系在沉淀和河流放电变化的影响(总氮,磷,硝酸盐和磷酸盐)和土地覆盖。我们假设,针叶林和农田,包括管理不善的,这需要细化和肥水管理,分别贡献风暴期间增加养分含量下游河流。线性混合效应模型分析基于18年的观测数据用于测试的假设。结果表明,营养物浓度和针叶和阔叶林面积比之间的多重回归分析的斜率为阴性,并随着每日降水减少。这表明,森林风暴期间促成河流养分浓度的稀释,无论他们是否是针叶还是阔叶。与此相反,营养物浓度和农业面积比之间回归的斜率表明相反的趋势,这说明即使农业区的一个很小的比例,以使在营养物浓度作为沉淀的增加增加一个大的贡献。我们的结果意味着,雨水径流响应于降雨在升高的供给氮气和附接到耕地土壤的河流磷的结果。

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