一条大型自由流动的砾石河床中磷的水文形态控制:加龙河(法国)

S. Garay, S. Sauvage, P. Vervier
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引用次数: 17

摘要

本文的目的是联系磷(P)的运输动力学和水文形态特征的一个大的人类影响的河流,加龙河在一个部门内接收污水处理厂的废水为60万人口。1997年和1999年在两个不同的低流量期水文条件下进行了两项研究。1997年的研究是在一条18公里长的河段上进行的,流量在33至53立方米/秒之间变化,波动很小。1999年的研究涉及一段较长的47公里河段,分为四个较小的河段,流量在40至108立方米/秒之间迅速波动。在污水处理厂下游,总磷(TP)浓度为0.19 ~ 0.27 mg/L,主要以溶解形式存在,60% ~ 78%的TP为溶解活性磷(DRP)。P浓度在污水处理厂上游显著降低。通过质量平衡方法,我们估计污水处理厂占所研究部门投入的一半以上(59%至67%)。当流量大于60m3 /s时,TP动态与悬浮固体有关。在1997年研究中确定的低流量期(60 m3 /s),磷潴留受到悬浮物质动力学的控制。我们得出结论,水文制度的管理可以影响P在敏感的低水位期间的保留。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydromorphological control of phosphorus in a large free‐flowing gravel bed river: the Garonne River (France)
The objective of this paper is to relate phosphorus (P) transport dynamics and hydromorphological characteristics of a large human-influenced river, the River Garonne within a sector receiving the waste water of a sewage treatment plant for a population of 600000. Two studies were conducted in 1997 and 1999 during two different hydrological conditions at low-flow periods. The 1997 study was carried out on an 18-km stretch with discharges varying between 33 and 53 m 3 /s and with very small fluctuations. The 1999 study concerned a longer stretch of 47 km, divided into four smaller reaches, and with discharges fluctuating rapidly from 40 to 108 m 3 /s. Downstream of the sewage treatment plant, total phosphorus (TP) concentrations ranged from 0.19 to 0.27 mg/L and were mainly in the dissolved form: between 60 and 78% of TP was dissolved reactive phosphorus (DRP). P concentrations were significantly lower upstream of the sewage treatment plant. By a mass-balance approach, we estimated that the sewage treatment plant represents more than half the input (between 59 and 67%) of the studied sector. TP dynamic is linked to suspended solids for discharges above 60 m 3 /s. During established low-flow period in the 1997 study ( 60 m 3 /s, P retention is controlled as expected by suspended matter dynamics. We conclude that management of the hydrological regime can influence P retention during sensitive low-water periods.
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