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ACIDIFICATION OF A SMALL STREAM ON KUREHA HILL CAUSED BY NITRATE LEACHED FROM A FORESTED WATERSHED

机译:从森林流水中渗出的硝酸盐导致的吴羽丘陵小径流的酸化

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Nitrate leakage to a stream from a small forested watershed on Kureha Hill in Toyama Prefecture, Japan was investigated in order to assess its acid-base chemistry. Kureha Hill, located in Toyama City, receives high nitrogen loading from the atmosphere. In this area, there are several small streams characterized by a high concentration of nitrate and low ANC. Hyakumakidani, one of the most acidic streams on that hill, the average pH and ANC were 5.2 and -8 μeq/1, respectively. The weighted average nitrate concentration, which was 125 μeq/1, increased up to 370 μeq/1 during high-discharge periods caused by heavy rainfall, while ANC decreased to -24 μeq/1 at the same time. Our preliminary study using a two-stage tank model simulating the flow paths in the soil indicated that during high-discharge periods, the increased subsurface flow containing a high concentration of nitrate contributed to the increased nitrate concentration. In this watershed, the annual nitrogen budget from Aug. 1998 to Aug. 1999 showed that the loss of nitrogen exceeded the bulk nitrogen deposition, indicating that this watershed is under condition of nitrogen saturation. However, no visible attenuation has been observed.
机译:为了评估其酸碱化学性质,调查了日本富山县吴羽山一个小森林流域中硝酸盐泄漏到河流中的情况。位于富山市的吴羽山从大气中吸收高氮。在该地区,有几条小溪流,其特征是硝酸盐浓度高和ANC含量低。 Hyakumakidani是该山上酸性最强的水流之一,平均pH和ANC分别为5.2和-8μeq/ 1。在大雨引起的高放电期间,硝酸盐加权平均浓度为125μeq/ 1,增加到370μeq/ 1,而ANC同时降至-24μeq/ 1。我们使用两阶段水箱模型模拟土壤中的流动路径的初步研究表明,在高流量期间,包含高浓度硝酸盐的地下流量增加,导致硝酸盐浓度增加。在该流域中,1998年8月至1999年8月的年度氮预算表明,氮的损失超过了氮的大量沉积,表明该流域处于氮饱和状态。但是,没有观察到可见的衰减。

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