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利用原位传感器描述一个五级郊区化流域的暴雨水氮通量特征。

Characterizing storm-event nitrate fluxes in a fifth order suburbanizing watershed using in situ sensors.

机构信息

Department of Natural Resources and Environment, University of New Hampshire , Durham, New Hampshire 03824, United States.

出版信息

Environ Sci Technol. 2014 Jul 15;48(14):7756-65. doi: 10.1021/es500252j. Epub 2014 Jul 1.

DOI:10.1021/es500252j
PMID:24945442
Abstract

Land use influences the distribution of nonpoint nitrogen (N) sources in urbanizing watersheds and storm events interact with these heterogeneous sources to expedite N transport to aquatic systems. In situ sensors provide high frequency and continuous measurements that may reflect storm-event N variability more accurately compared to grab samples. We deployed sensors from April to December 2011 in a suburbanizing watershed (479 km2) to characterize storm-event nitrate-N (NO3-N) and conductivity variability. NO3-N concentrations exhibited complex patterns both within and across storms and shifted from overall dilution (source limitation) before summer baseflows to subsequent periods of flushing (transport limitation). In contrast, conductivity generally diluted with increasing runoff. Despite diluted NO3-N concentrations, NO3-N fluxes consistently increased with flow. Sensor flux estimates for the entire deployment period were similar to estimates derived from weekly and monthly grab samples. However, significant differences in flux occurred at monthly time scales, which may have important implications for understanding impacts to temporally sensitive receiving waters. Evidence of both supply (nutrient-poor) and transport (nutrient-rich) limitation patterns during storms is consistent with watersheds undergoing land use transitions. Tracking shifts in these patterns could indicate N accumulation in developing watersheds and help identify mitigation opportunities prior to N impairment.

摘要

土地利用会影响城市化流域中非点源氮(N)源的分布,而暴雨事件会与这些非均一的污染源相互作用,加速 N 向水生系统的迁移。原位传感器可提供高频且连续的测量,与随机取样相比,可能更准确地反映暴雨事件中 N 的变化。我们于 2011 年 4 月至 12 月在一个郊区化流域(479 平方公里)部署了传感器,以表征暴雨事件中硝酸盐-N(NO3-N)和电导率的变化。NO3-N 浓度在暴雨事件内和之间表现出复杂的模式,在夏季基流前从整体稀释(源限制)转变为随后的冲刷(传输限制)。相比之下,电导率通常随着径流量的增加而稀释。尽管 NO3-N 浓度较低,但 NO3-N 通量仍随流量持续增加。整个部署期间传感器通量的估计值与每周和每月随机取样的估计值相似。然而,在每月的时间尺度上,通量存在显著差异,这对理解对时间敏感的受纳水体的影响可能具有重要意义。暴雨期间出现供应(养分贫瘠)和传输(养分丰富)限制模式的证据与经历土地利用转变的流域一致。跟踪这些模式的变化可以指示发展中流域中 N 的积累,并有助于在 N 损害之前确定缓解机会。

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