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利用高频水质数据和 MODHMS 模型综合应用识别低径流量产水区域的磷输出。

Identification of phosphorus export from low-runoff yielding areas using combined application of high frequency water quality data and MODHMS modelling.

机构信息

CSIRO Land and Water, Floreat, Western Australia, Private Bag 5, Wembley, WA 6913, Australia.

出版信息

Sci Total Environ. 2012 Jun 1;426:264-71. doi: 10.1016/j.scitotenv.2012.03.021. Epub 2012 Apr 12.

DOI:10.1016/j.scitotenv.2012.03.021
PMID:22503672
Abstract

In basins combining flat-sandy valleys and hilly-bedrock sub-catchments, the assessment of nutrient (phosphorus) exports from low-runoff yielding environments is difficult. To overcome this issue hydrological modelling and high frequency phosphorus measurements were simultaneously employed. A coupled surface water-groundwater interaction model (MODHMS) was used to determine runoff from the low-runoff yielding part of the catchment. The modelling results indicated that the lower catchment contributed less than 10% of annual catchment discharge over a number of weeks during mid-winter. High frequency phosphorus (P) measurements showed a threefold increase in P concentration during this period in 2008, which lasted for 3 weeks. Concentration-discharge analysis suggested that the increase in P concentration was associated with runoff generation processes in the low-runoff yielding sub-catchment. It was estimated that this area contributed 32% of the annual P load though only 2% of total annual discharge in 2008. Both runoff and P contributions occurred during the period when the water table rose to the surface causing inundation. It was shown that the P concentrations in discharge from the low-runoff yielding sub-catchment were similar to those observed in the shallow groundwater layers.

摘要

在兼具平坦沙质山谷和丘陵基岩子流域的盆地中,评估低径流量环境中营养物(磷)的输出是困难的。为了克服这个问题,同时采用了水文模型和高频磷测量。一个耦合的地表水-地下水相互作用模型(MODHMS)被用来确定集水区低径流量部分的径流量。模型结果表明,在 2008 年的数周内,冬季中期,下游流域的贡献不到年流域排放量的 10%。高频磷(P)测量显示,在此期间 P 浓度增加了三倍,持续了 3 周。浓度-流量分析表明,P 浓度的增加与低径流量子流域的径流产出过程有关。据估计,该区域在 2008 年贡献了 32%的年磷负荷,尽管仅占总年排放量的 2%。径流量和磷的贡献都发生在地下水位上升到地表导致淹没的时期。结果表明,低径流量子流域的排放中 P 浓度与浅层地下水中观察到的浓度相似。

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