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青海湖水量平衡分析与水资源优化配置研究   总被引:18,自引:4,他引:14  
在充分收集有关资料的基础上研究青海湖1959-2000年间降水径流蒸发湖泊水位地下水补给量的动态变化建立水量平衡分析方程.青海湖水位在波动中持续下降42年来年平均水位累计下降了 3.32 m平均每年下降了0.079 m近年来下降的幅度减小. 同时青海湖储水量不断减少而湖区降水呈增加的趋势河川径流量地下水的入湖补给量 蒸发量呈现下降的趋势. 根据青海湖水平衡分析计算结果预测2010年青海湖流域耗水量将达1.27108m3为维护生态平衡和社会经济持续发展需要跨流域调水量引大济湖4.1108m3.  相似文献   

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Demin  A. P. 《Water Resources》2000,27(6):670-687
The development history of the accounting system of water supply in the USSR is presented. Various statistical abstracts of 1970–1998 on the water supply in the Russian Federation are analyzed. Reference data are shown to be in need of correction. The dynamics of waste, mine, and drain water disposal are considered. The change in water quality is shown to be inadequate to the reduction in the discharge of pollutants.  相似文献   

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Aiqing Kang  Li  Jiahong  Lei  Xiaohui  Ye  Mao 《Water Resources》2020,47(2):336-347
Water Resources - A water resource allocation model coupling quantity and quality is a topic of concern in China. The water resources supply modelling is set up according to the water quality, and...  相似文献   

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Water Resources - The reserves of natural and artificial water bodies in Europe were evaluated using a new procedure which had been developed for Russian territory and upgraded for the territories...  相似文献   

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The standard MODFLOW packages offer limited capabilities to model piecewise-linear boundary conditions to describe ground water–surface water interaction. Specifically, MODFLOW is incapable of representing a Cauchy-type boundary with different resistances for discharge or recharge conditions. Such a more sophisticated Cauchy boundary condition is needed to properly represent surface waters alternatively losing water through the bottom (high resistance) or gaining water mostly near the water surface (low resistance). One solution would be to create a new package for MODFLOW to accomplish this. However, it is also possible to combine multiple instances of standard packages in a single cell to the same effect. In this specific example, the general head boundary package is combined with the drain package to arrive at the desired piecewise-linear behavior. In doing so, the standard USGS MODFLOW version can be used without any modifications at the expense of a minor increase in preprocessing and postprocessing and computational effort. The extra preprocessing for creating the input and extra postprocessing to determine the water balance in terms of the physical entities from the MODFLOW cell fluxes per package can be taken care of by a user interface.  相似文献   

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ABSTRACT

Water-management issues cut across all sectors of governance and have a critical bearing on many post-conflict challenges. The imperative of adequate water supply and the weakness of the state in a post-conflict period provide a nexus which demands comprehensive and well thought-out policy planning, for the short term as well as for the long term. However, very little research has been conducted on the nexus between water management and sustainable development in war-torn societies that are undergoing processes of peacebuilding. This article, after critically reviewing the contribution of water scarcity to security challenges and peacemaking, makes an attempt to contribute to the policy debate on how carefully planned interventions in the water sector can significantly contribute to the post-conflict peacebuilding process, from immediate recovery and rebuilding to long-term sustainable development goals and lasting peace.

EDITOR D. Koutsoyiannis GUEST EDITOR K. Aggestam  相似文献   

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We have used stable water isotopes (δ18O, δ2H) in combination with lumped-parameter modeling for characterizing unsaturated flow in two lysimeters vegetated with maize. The lysimeters contained undisturbed soil cores dominated by sandy gravel (Ly1) and clayey sandy silt (Ly2). Stable water isotopes were analyzed in precipitation and lysimeter outflow water over about 3 years. The mean transit time of water T and dispersion parameter PD, obtained from modeling, were higher for the silt soil in Ly2 than for the gravel soil in Ly1 (T of 362 vs. 129 d, PD of 0.7 vs. 0.12). The consideration of preferential flow (PF) paths could substantially improve the model curve fits, with 13 and 11% contribution of PF for Ly1 and Ly2 as best estimates. Different assumptions were compared to estimate the input function, that is, stable water isotope content in the recharging water. Using the isotopic composition of precipitation as input (no modification) resulted in reasonable model estimations. Best model fits for the entire observation were obtained by weighting the recharging isotopes according to average precipitation within periods of 3 and 6 months, in correspondence to changing vegetation phases and seasonal influences. Input functions that consider actual evapotranspiration could significantly improve modeling at some periods, however, this led to deviations between modeled and observed δ18O at other periods. This may indicate the influence of variable flow, so that dividing the whole observation period into hydraulically characteristic sub-periods for lumped-parameter modeling (which implements steady-state flow) is recommended for possible further improvement.  相似文献   

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Adverse environmental changes in the condition of water sources and water supply systems as well as causes for these changes have been revealed using the results of analysis of economic development of Primorskii Krai over a long period of time. Some recommendations concerning the elimination of these causes have been proposed.  相似文献   

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