首页> 外文期刊>Journal of Hydrology >Freshwater-saltwater transition zone movement during aquifer storage and recovery cycles in Brooklyn and Queens, New York City, USA
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Freshwater-saltwater transition zone movement during aquifer storage and recovery cycles in Brooklyn and Queens, New York City, USA

机译:美国纽约市布鲁克林和皇后区淡水-盐水过渡带在含水层存储和恢复周期中的运动

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Freshwater storage in deep aquifers of Brooklyn and Queens, New York, USA, is under consideration as an emergency water supply for New York City. The purpose of a New York City storage and recovery system is to provide an emergency water supply during times of drought or other contingencies and would entail longer-term storage phases than a typical annual cycle. There is concern amongst neighboring coastal communities that such a system would adversely impact their local water supplies via increased saltwater intrusion. This analysis uses three-dimensional modeling of variable-density ground-water flow and salt transport to study conditions under which hypothetical aquifer storage and recovery (ASR) may not adversely impact the coastal water supplies. A range of storage, pause, and recovery phase lengths and ASR cycle repetitions were used to test scenarios that emphasize control of potential saltwater intrusion. The USGS SUTRA code was used to simulate movement of the freshwater-saltwater transition zones in a detailed model of the upper glacial, Jameco, Magothy, and Lloyd aquifers of western Long Island, New York. Simulated transition zones in the upper glacial, Jameco, and Magothy aquifers reach a steady state for 1999 stress and recharge conditions within 1 ka; however, saltwater encroachment is ongoing in the Lloyd (deepest) aquifer, for which the effects of the rise in sea level since deglaciation on transition zone equilibration are retarded by many ka due to the thick, overlying Raritan confining unit. Pumping in the 20th century has also caused widening and landward movement of the Lloyd aquifer transition zone. Simulation of scenarios of freshwater storage by injection followed by phases of pause and recovery by extraction indicates that the effect of net storage when less water is recovered than injected is to set up a hydraulic saltwater intrusion barrier in the Lloyd aquifer which may have beneficial effects to coastal water users. (c) 2007 Elsevier B.V. All rights reserved.
机译:正在考虑将美国纽约布鲁克林和皇后区深层含水层中的淡水存储作为纽约市的应急水源。纽约市存储和恢复系统的目的是在干旱或其他突发事件期间提供紧急供水,并且与典型的年度周期相比,需要长期的存储阶段。在邻近的沿海社区中,人们担心这种系统会通过增加盐水入侵而对当地水供应产生不利影响。该分析使用可变密度地下水流和盐分运输的三维建模来研究假设的含水层存储和恢复(ASR)不会对沿海水源产生不利影响的条件。使用一系列存储,暂停和恢复阶段长度以及ASR循环重复来测试强调控制潜在盐水入侵的方案。 USGS SUTRA代码用于在纽约长岛西部的上部冰川,Jameco,Magothy和Lloyd含水层的详细模型中模拟淡水-盐水过渡带的运动。上冰川,Jameco和Magothy含水层中的模拟过渡带在1 ka内对1999年的应力和补给条件达到稳定状态;然而,在劳埃德(最深)含水层中,海水仍在侵蚀,由于里拉坦封闭单元较厚,由于冰消作用对过渡区平衡的影响,海平面上升的影响受到了许多钾的抑制。 20世纪的抽水还引起了劳埃德含水层过渡带的扩大和向陆运动。模拟注入淡水的情景,然后进行暂停和提取阶段的回收,表明当回收的水量少于注入水时的净储水效果是在劳埃德含水层中建立水力盐水入侵屏障,这可能对沿海用水者。 (c)2007 Elsevier B.V.保留所有权利。

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