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Analysis and numerical simulation of natural and human-caused low dissolved oxygen in the Minjiang River Estuary

机译:Min江口自然和人为原因低溶解氧的分析和数值模拟

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摘要

The Minjiang River, a typical tidal channel in Southeast China, plays an important role in the supply of drinking water, flood control and drought relief, farming and navigation, as well as shipping and other functions. Dissolved oxygen (DO), as a basic living condition for aquatic biota, has been deteriorating in the Minjiang River in recent years. In order to understand how the spatial distribution of DO responds to river discharge, nutrient loading and water temperature, a three-dimensional Environmental Fluid Dynamics Code model was used to simulate water age and the distribution of DO in the Minjiang River. The model presented in this paper was used for water resource and water quality simulations under various physical, chemical, and biological scenarios. Sensitivity simulation results indicated that the three factors had a significant impact on the spatial distribution variation of DO in the Minjiang River. Increased river discharge or split ratio of the North Channel resulted in decreased water age and increased DO. Increased nutrient loading and water temperature caused lower DO. In order to protect coastal environments in the Minjiang River, river discharge should be increased and pollutants of local cities should be reduced during the high temperature and drought period.
机译:Southeast江是中国东南部的典型潮汐航道,在饮用水供应,防洪和抗旱,农业和航运以及航运等功能中发挥着重要作用。近年来,溶解氧(DO)作为水生生物的基本生活条件,一直在恶化。为了了解溶解氧的空间分布如何响应河流流量,养分含量和水温,使用三维环境流体动力学代码模型来模拟water江的水龄和溶解氧的分布。本文介绍的模型用于各种物理,化学和生物场景下的水资源和水质模拟。敏感性模拟结果表明,这三个因素对Min江水域溶解氧的空间分布变化具有显着影响。北河道的河流流量增加或分流比增加,导致水龄减少和溶解氧增加。营养物负荷增加和水温升高导致溶解氧降低。为了保护Min江沿岸环境,在高温干旱时期应增加河道流量,减少局部城市的污染物。

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