首页> 外文会议>International Symposium on Groundwater Problems Related to GEO-Environment May 28-30, 2003 Okayama, Japan >Nitrate pollution in groundwater in the lower reach of the Yellow River, case study in Shandong Province, China
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Nitrate pollution in groundwater in the lower reach of the Yellow River, case study in Shandong Province, China

机译:黄河下游地下水中的硝酸盐污染-以山东省为例

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Yucheng and Qihe counties in the lower reaches of the Yellow River tended to be an important agricultural area after the Yellow River water was diverted in 1972. Field surveys and sampling wereimplemented in the area to examine the nitrate pollution of groundwater, which is recharged dominantly by the diverted water. Nitrate pollution was found to have occurred in the shallow layer of less than 8 m in depth with the highest concentration of more than 200mg/l. Though nitrate content was found in the Yellow River ranging from 16.3 to 37.1 mg NO_3/l, it was not found in the canal, ditch and pond used to convey and store the diverted water, excluding the N source from the Yellow River. ~(15)N was measured to identify the nitrogen of anthropogenic and fertilizer/soil organic sources. The upward potential gradient of the saturated zone observed in the piezometers at Yucheng Experimental Station, the occurrence of ZFP at 120 cm depth, and denitrification process deduced from the change in δ~(15)N and SO_4 concentration helped explain why NO_3 was found only in the shallow layer of the aquifer.
机译:1972年黄河水改道后,黄河下游的禹城县和齐河县往往成为重要的农业区。对该地区进行了实地调查和取样,以调查地下水中的硝酸盐污染,这些污染物主要由地下水补给。被转移的水。发现在深度小于8 m的浅层中发生了硝酸盐污染,最高浓度超过200 mg / l。尽管在黄河中发现硝酸盐含量为16.3至37.1 mg NO_3 / l,但在用于输送和储存分流水的运河,沟渠和池塘中却未发现硝酸盐含量,黄河中的氮源除外。测量〜(15)N以识别人为和肥料/土壤有机源的氮。在禹城实验站测压仪中观察到的饱和区的向上电位梯度,在120 cm深度处ZFP的发生以及由δ〜(15)N和SO_4浓度的变化推导的反硝化过程有助于解释为什么仅发现NO_3在含水层的浅层。

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