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分层式大坝水库中激流密度流的 DOC 浓度特征。

Characteristics of DOC concentration with storm density flows in a stratified dam reservoir.

机构信息

Department of Urban Engineering, Chungbuk National University, Cheongju, Chungbuk 361-763, Korea.

出版信息

Water Sci Technol. 2010;62(11):2467-76. doi: 10.2166/wst.2010.537.

Abstract

Among natural organic matter (NOM) defined as the complex matrix of organic materials abundant in natural waters, a gradual accumulation of recalcitrant organic matter (ROM) has been observed in impounded water bodies such as a lake or dam reservoir in spite of extensive efforts made to curtail organic pollutant loadings generated in their catchment areas. This paper aims to identify the effect of diffuse pollution resulting from allochthonous organic matters on the temporal and spatial characteristics of organic matters in a stratified dam reservoir, Daecheong Dam, using both intensive observation and CE-QUAL-W2 model simulation. With the limitation of observation data in terms of organic matters of inflow waters from boundary tributaries and impounded water in the reservoir, organic matter was represented by organic carbon including labile particular organic carbon (LPOC), refractory organic carbon (RPOC), labile dissolved organic carbon (LDOC), and refractory organic carbon (RDOC). Both autochthonous and allochthonous origins of organic carbon were considered in the modeling of eutrophication of the reservoir water using CE-QUAL-W2. The result of simulation during the period from 2001 to 2005 was observed to be a gradual accumulation of particular organic carbon (POC). It is clear that the model calculation results enable the explanation of the internal and external movement of constituents in the reservoir. In particular turbidity and NOM were well related in the upper region of the reservoir according to flow distance, gradually changing to dissolved form of organic matter, DOC affected organic matter concentration of reservoir water quality compared to turbidity.

摘要

在天然有机物 (NOM) 中,定义为自然水中丰富的有机物质复杂矩阵,尽管在集水区内广泛努力减少有机污染物负荷,但仍观察到在蓄水水体(如湖泊或大坝水库)中顽固有机物 (ROM) 的逐渐积累。本文旨在使用密集观测和 CE-QUAL-W2 模型模拟,确定来自异源有机物的扩散污染对分层大坝水库中有机物的时空特征的影响,该水库是大淸湖大坝。由于边界支流和水库中蓄水的入流水中有机物观测数据的限制,有机物由包括易变颗粒有机碳 (LPOC)、难降解有机碳 (RPOC)、易降解溶解有机碳 (LDOC) 和难降解有机碳 (RDOC) 在内的有机碳表示。在使用 CE-QUAL-W2 对水库富营养化进行建模时,考虑了有机碳的自源和异源起源。从 2001 年到 2005 年期间的模拟结果表明,颗粒有机碳 (POC) 逐渐积累。很明显,模型计算结果能够解释水库中成分的内部和外部运动。特别是在水库的上部区域,浊度和 NOM 根据水流距离很好地相关,逐渐转化为溶解态有机物,DOC 对水库水质中有机物浓度的影响与浊度相比。

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