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Two-dimensional modelling of hydrodynamics and water quality of a stratified dam reservoir in the southern side of the Mediterranean Sea

机译:地中海南侧分层坝库水动力和水质的二维建模

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A vertical two-dimensional, laterally averaged hydrodynamic and water quality model CE-QUAL-W2 was used to simulate water temperature, dissolved oxygen, electrical conductivity, chlorophyll a, total suspended solids, alkalinity, ammonium, phosphate, and total iron in the Sejnane Dam (North Tunisia) in response to external forcings that characterize main features of climate in the southern side of the Mediterranean Sea. The hydrodynamic modelling results show that the model is able to reproduce accurately the measured water surface elevation, spatio-temporal patterns of temperature, dissolved oxygen and other state of variables and to capture most of the seasonal changes in the reservoir. Three scenarios involving the impacts of severe drought season, summer rainfall and total suspended solids load on hydrodynamics and water quality are analyzed. Severe drought reduces the thickness of hypoxic waters from 10 to 2-4 m and shifts the temperature of the entire water column up to 5 ℃ during summer and about 1.2 ℃ in winter. The thermocline takes place 1 month before that of the reference and sinks to the bottom faster by 1-2 m per month. Summer rainfall dilutes the first waves of the autumn rains and disrupts the thermal gradient in the water column, which may show complex thermal structures. TSS load has the most negative effects on water quality in that it shifts the phosphorus concentration by 1-3 mg/l and promotes an early warming of surface water in spring and an early cooling since late summer by up to 1 ℃. During summer stratification, it contributes to the cooling of the metalimnion by 2 ℃ on average, which may alter its structure and dynamics as an aquatic biotope.
机译:使用垂直二维,横向平均流体动力学和水质模型CE-QUAL-W2来模拟水井中的水温,溶解氧,电导率,叶绿素a,总悬浮固体,碱度,铵,磷酸盐和总铁大坝(突尼斯北部)是对外部强迫的回应,外部强迫是地中海南部气候的主要特征。流体动力学建模结果表明,该模型能够准确地再现所测得的水面高度,温度的时空模式,溶解氧和其他变量状态,并能够捕获储层中的大多数季节性变化。分析了涉及严重干旱季节,夏季降雨和总悬浮固体负荷对水动力和水质影响的三种情况。严重的干旱使低氧水的厚度从10减少到2-4 m,并使整个水柱的温度在夏季升高到5℃,在冬季升高到约1.2℃。温度跃迁比参考温度早1个月发生,并且每月以1-2 m的速度下沉到底部。夏季降雨稀释了秋季降雨的第一波浪潮,并破坏了水柱中的热梯度,这可能显示出复杂的热结构。 TSS负荷对水质的负面影响最大,因为它使磷浓度移动了1-3 mg / l,并​​在春季促进了地表水的早期变暖,并从夏季末开始促进了至1℃的降温。在夏季分层过程中,它有助于使金属酰亚胺平均冷却2℃,这可能会改变其作为水生生物群落的结构和动力学。

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