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黄土覆盖区溪流和地下水中硝酸盐氮的迁移:来源、驱动因素及时空变化。

Nitrate-nitrogen transport in streamwater and groundwater in a loess covered region: Sources, drivers, and spatiotemporal variation.

机构信息

State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, College of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China.

Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, Shaanxi 710061, China.

出版信息

Sci Total Environ. 2021 Mar 20;761:143278. doi: 10.1016/j.scitotenv.2020.143278. Epub 2020 Oct 29.

Abstract

Water quality is an increasing concern in the dry regions of the world as it affects and reduces the quantity of available water. Our objective was to investigate the sources, drivers, spatiotemporal patterns of nitrate‑nitrogen (NO-N) transport in the streamwater and groundwater in a dry and a wet season in seven large rivers located in the Loess Plateau of China (640,000 km, 100 million population), which is a region with marked influence of human activities on streamflow and groundwater. We collected 510 streamwater and groundwater samples and found that NO-N was significantly lower in the dry season (< 5.0 mg L) than the wet season (> 5.0 mg L). In the wet season, NO-N was lower in the streamwater than groundwater; however, the spatial variation in the NO-N was greater in streamwater, with higher concentrations in two rivers (Wei and Fen). The source characterization using stable isotopes of NO from the Wei River showed that chemical N fertilizers and soil organic N contributed ~ 75% of NO to streamwater and that soil organic N was the greatest contributor of NO to groundwater (~ 60%) than streamwater (< 40%). The spatial pattern of NO-N was dominated by fertilizer application and varied seasonally with rainfall-runoff and streamflow-groundwater connectivity. Our results showed the complicated patterns and sources of NO pollution in streamwater and groundwater and highlight that more emphasis should be placed to prevent and restore the degraded water quality in the dry regions.

摘要

水质是世界干旱地区日益关注的问题,因为它会影响和减少可用水资源的数量。我们的目的是调查硝酸盐氮(NO-N)在位于中国黄土高原的七条大河(64 万平方公里,1 亿人口)的溪流和地下水中的来源、驱动因素和时空分布模式,该地区人类活动对溪流和地下水的影响显著。我们采集了 510 个地表水和地下水样本,发现 NO-N 在旱季(<5.0mg/L)明显低于雨季(>5.0mg/L)。在雨季,NO-N 在溪流水中的含量低于地下水中的含量;然而,NO-N 在溪流水中的空间变化更大,两条河流(渭和汾)的浓度更高。来自渭河水体中氮同位素的来源特征表明,化学氮肥和土壤有机氮对溪流水中的 NO 贡献了约 75%,而土壤有机氮对地下水(>60%)的 NO 贡献大于溪流水中的(<40%)。NO-N 的空间格局主要由施肥决定,且随降雨-径流和地表水-地下水的连通性季节性变化。我们的研究结果表明,NO 污染在地表水和地下水中存在复杂的模式和来源,这突出表明在干旱地区应更加重视防止和恢复退化的水质。

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