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Numerical modeling of flow dynamics of rivers with comprehensive channel patterns and wide floodplains during high water stage is considered to be one of the most effective methods for implementing both research and civil-engineering projects. However, realistic results of simulations can be obtained only if the model has been calibrated and validated against field observations and remote sensing data. This approach is realized for a 2D hydrodynamic model of the Oka River at the city of Ryazan (central European Russia). The Oka has a meandering channel and a wide floodplain with a complicated distributary network. The feasibility of allocating new residential quarters and infrastructure facilities on artificial “islands” on the floodplain was studied using STREAM_2D software package. Because of a significant decrease in the maximum runoff of the Oka in the recent decades, the simulations were made for the extreme spring snowmelt flood of 1970 for various scenarios of floodplain development in the past, present, and future.
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Abstract The Oka Belt, composed of clastic rocks and greenschists, extends for approximately 600 km in the South-Siberian Sayan region and adjacent northern Mongolia. For a long time the Oka Belt's age and tectonic setting were the most controversial problem in the region. We argue that the belt was formed in Late Neoproterozoic as an accretionary prism. The Oka Belt shows imbricated thrust structure, which had originally seaward vergence and reflected the Neoproterozoic accretion process. The Early Paleozoic orogeny had minor effect on its structural style. The belt contains tectonic slivers of mid-ocean ridge basalts, some oceanic-island basalts and possible pelagic sediments. In several localities they are associated with gabbro and serpentinite. All these rocks represent the oceanic lithosphere subducting beneath the Oka prism and trapped within it. In the inner zone of the Oka Belt are the blueschists exhumed from the deeper prism level. The northern Oka Belt includes mafic intrusions geochemically similar to normal mid-oceanic ridge basalt and felsic volcaniclastic rocks. This segment of the belt is very similar to the Tertiary portion of northern Shimanto Belt, in Japan, and has also experienced the subduction of orthogonal oceanic ridge beneath the prism. This event dates back to 753 ± 16 Ma (the U-Pb zircon discordia). The Oka prism started accreting in Mid-Neoproterozoic after the subduction had initiated under the Japan-like South-Siberian continental terrain. The prism existed through the second half of Neoproterozoic and accumulated a huge volume of sialic material to enlarge the nearby continent. Currently, the Oka Belt remains poorly studied and is very promising for further investigation and discoveries. 相似文献
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Water Resources - The article considers an approach to evaluating the change in surface, subsurface and groundwater flow on a large river catchment exemplified by the Oka River basin. The study is... 相似文献
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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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P. S. Badminov A. V. Ivanov B. I. Pisarskii A. I. Orgil’yanov 《Journal of Volcanology and Seismology》2013,7(4):265-276
The western flank of the Baikal Rift Zone contains the Oka hydrothermal system of the “volcanogenic type,” which is related to the occurrence of basaltic volcanism. It consists of springs for the discharge of thermal and subthermal waters confined to the intersections of faults of various settings at the boundary of two major lithospheric blocks. Helium isotope data were used to find heat flow for all springs of the hydrothermal system; this heat flow is comparable with that across the bottom of the Baikal southern basin. Predicted hydrotherm temperatures were calculated at the depths of their generation using silica and cation thermometers. The average depth of generation of the springs that form the Oka hydrothermal system is 2.8 km, which is 1.1 km nearer to the ground surface than the h of the hydrothermal occurrences around Lake Baikal. The spatial coincidence between the location of the hydrothermal system and the area of young volcanism provides evidence of a common source of heat, while the thermal parameters of the system, its gas and chemical compositions, correlate with the age of the volcanism. 相似文献
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Ashok Swain 《水文科学杂志》2013,58(7):1313-1322
ABSTRACTWater-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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阳澄湖若干水质资料的分析与评价 总被引：12，自引：0，他引：12
根据１９９４年５月于阳澄湖湖区７个采样点水质分析结果,表明湖水中矿化度较高,硬度较大,主要离子以ＨＣＯ３＾－,Ｎａ＾＋为主,分别占阴阳离子摩尔总数的５７．６１％、６３．９％。湖水水型西湖、中湖为重碳酸盐钠组Ⅰ型,东湖为重碳酸盐钠组Ⅱ型水。湖水中Ｎ、Ｐ营养元素丰富,ＮＨ３－Ｎ、ＮＯ２－Ｎ指标与７０年代相比明显增高,表明水体已曹室不程度地轻污染。 相似文献
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byWillem Jan Zaadnoordijk 《Ground water》2009,47(5):723-726
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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平谷赵各庄井深200 m, 观测含水层为182 m以下的全井段, 是浅层冷水和深层热水的混合水。 受开采及降雨影响, 水位、 水温长趋势及年动态具有同步协调性变化, 地下水开采使井筒内冷水比例变小, 水位下降, 水温上升; 降雨渗入补给使流入观测井筒内冷水占比例变大, 水位上升, 水温下降, 但雨季结束, 井筒内冷水流入量变少, 井水温逐渐回升。 气压和固体潮使井筒与含水层间有水流运动, 水位出现周期性波动, 从而改变井筒内冷热水比例, 引起水温周期性变化的次生效应, 两者有短期同步协调变化。 不同种干扰因素造成了不同周期的变化影响, 在排除干扰, 提取地震异常信息时, 应选用不同方法及取样周期进行分析。 相似文献
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The aim of this work is to study the removal of fluoride from brackish polluted water using electrodialysis. The influence of several parameters such as flow rate, initial feed concentration, co‐existing ions, and initial pH on process efficiency were studied. This efficiency is evaluated by the removal rate, demineralization rate, and power consumption. The defluoridation process showed to be independent of pH of feed solution. Although the remained studied parameters plays a significant role on the defluoridation efficiency and mainly on the specific power consumption. The defluoridation of a contaminated real water sample was investigated so as to improve the efficiency of the process. The fluoride concentration could be reduced from 2.9 to 0.4 mg L−1 which was lower than World Health Organization (WHO) standard (1.5 mg L−1). Moreover the concentrations of different species in the obtained treated water are below the amounts recommended by WHO for drinking water. 相似文献
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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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Analyzing Effects of Shrub Canopy on Throughfall and Phreatic Water Using Water Isotopes,Western China 总被引：1，自引：0，他引：1
Alpine shrub Quercus aquifolioides was selected to study the effects of shrub canopy on throughfall and phreatic water by analyzing the isotopic time series of precipitation, canopy throughfall and phreatic water and examining correlations among these series in Wolong Nature Reserve, Western China. Based on analysis of precipitation data in 2003, the local meteoric water line during the rainy season was δD = 8.28 × δ18O + 8.93, and the primary precipitation moisture in this region originated from the Pacific Ocean in the summer. Stable isotope analysis showed that the main supply of throughfall and phreatic water was from precipitation, and the shrub canopy has an important effect on the processes of rainwater transmuted into throughfall and phreatic water. Moreover, the differences of δD and δ18O values between rainwater and throughfall were relevant to rainfall. Due to interception of the shrub canopy, there had a response hysteresis of phreatic water to the various rainfall events, which was mostly 2 days, except that this hysteresis was ≤1 day when rainfall was >15 mm/day. 相似文献
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《Earth and Planetary Science Letters》2006,241(3-4):972-977
The temperature changes caused by water exsolution from magma have been determined through calorimetric measurements performed on phonolitic and albitic compositions. The enthalpies of mixing of water with these melts have been derived from HF solution calorimetry, made at 323 K on glass samples containing up to 5 wt.% water, together with heat capacity data for the same series of samples. Mixing between aluminosilicate melts and water appears nearly ideal at magmatic temperatures, with small enthalpies of mixing that are negative for both melts at low pressures but can become positive for albite at high pressure. Regardless of the endothermic or exothermic nature of the process, water exsolution is associated with negligible temperature changes of only a few degrees even when 5 wt.% H2O is degassed. However, thermal effects might be greater for more depolymerized melts such as basalts and related compositions. 相似文献
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Water security in north China and countermeasure to climate change and human activity 总被引：2，自引：0，他引：2
This paper addresses the emergent issues by the case study of Haihe River Basin in North China. The advantage of the water international study and the background for the cause of these problems from natural change and in particular human activity are analyzed. The key points are addressed as four aspects: (a) the study of the water cycle process impacted by climate change and high intensity human activity; (b) water utilization related to new economic partner change, such as saving water model; (c) study on eco-hydrology, and the interaction of water and ecology impacted by climate change and human activity; and (d) reasonable water allocation that includs water diversion from south to north and saving water issue in the local areas. Several suggestions are proposed both on the study on the water cycle, which is a very important base of water security in north China, and on the application study of water resources and eco-environmental rehabilitation. These key issues will benefit both the advantage of water science and the sustainable development in China. 相似文献