By National Research Council, Division on Earth and Life Studies, Water Science and Technology Board, Committee on Sustainable Underground Storage of Recoverable Water
This ebook assesses event with controlled underground water garage platforms & identifies learn priorities for improvement of destiny underground garage initiatives, recommending how one can deal with the original demanding situations posed via such platforms via study & regulatory measures.
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All rights reserved. html INTRODUCTION 23 REFERENCES AWWA (American Water Works Association). 2002. Survey and Analysis of Aquifer Storage and Recovery (ASR) Systems and Associated Regulatory Programs in the United States. Denver, CO: AWWA. Bouwer, H. 1996. Issues in artificial recharge. Water Science and Technology 33: 381-390. Dillon, P. 2005. Future management of aquifer recharge. Hydrogeology Journal 13:313-316. 1007/s10040-004-0413-6. Hodgkins, G. , and R. W. Dudley. 2006. Changes in late-winter snowpack depth, water equivalent, and density in Maine, 1926-2004.
The committee hopes that the acronym MUS will become a useful and wellunderstood addition to the water management lexicon. The number of MUS projects is increasing rapidly. In 1983, there were three operating aquifer storage and recovery (ASR) systems in the United States. By 1994 there were 22 of these recharge well projects, and as of late 2005, there were about 72 systems in operation (Figure 1-2), with approximately 100 more in development (Pyne, 2005). These are located not only in the arid southwest- Copyright © National Academy of Sciences.
Land ownership and zoning are also considerations impacting the location of recovery wells. Not all recovery occurs with wells. Along the Platte River in Colorado, water is taken from the river during high-flow, low-demand periods to offset impacts of well withdrawals from alluvial aquifers on more senior surface water rights. The water is placed in recharge ponds or ditches during nonirrigation seasons, where it seeps into the aquifer. It then flows in the subsurface back to the stream, which “recovers” it directly as seepage.