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VERMONT PUBLIC COMMUNITY WATER SYSTEMS-GROUNDWATER INTERFERENCE STUDY

机译:佛蒙特州公共社区水系统 - 地下水干扰研究

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The Vermont Rural Water Association completed an assessment of groundwater interference caused by the pumping of Public Community Water Supply (PCWS) sources throughout Vermont. The majority of PCWS sources in Vermont are wells completed in fractured crystalline bedrock aquifers, with a more limited number completed in sand and gravel aquifers present in some valley locations. Due to the non-homogenous, anisotropic nature of these aquifers, interference with nearby private and public wells and springs is difficult to predict unless measured in the field. Existing source evaluation reports prepared since 1980 by the environmental consulting community were reviewed to develop a geodatabase with key information about the pumped wells and observation wells monitored during these tests. This information includes specific pumping test information, derived values such as aquifer transmissivity and storativity, the degree of interference noted at observation locations, and a determination of acceptable versus unacceptable interference. Although the review was limited to currently active or permitted drilled PCWS sources, over 200 sources and 1,100 observation points were evaluated across the state. The results of the study indicate that, overall, groundwater interference is not a chronic problem in Vermont. However, unacceptable interference - where a specific observation well source could no longer meet its intended demand - was noted in several instances in areas of higher concentrations of PCWS sources. It was also determined that cumulative interference at a given observation location is not always accurately tracked over time, as an effective method to track cumulative interference has not existed for use by state regulators. The geodatabase developed during this study, if kept updated as new PCWS sources are permitted, would allow for effective tracking of groundwater interference across Vermont.
机译:佛蒙特乡村水协会完成造成的公共社区供水(水焦浆)来源整个佛蒙特州抽地下水干扰的评估。在佛蒙特大部分水焦浆来源是井裂缝结晶基岩含水层完成后,用在存在于某些山谷的位置砂石含水层完成了更多数量有限。由于这些含水层的非均质,各向异性的性质,与附近的私人和公共水井和泉水的干扰很难预测,除非在现场测量。现有的由环保咨询社区自1980年以来编写源评价报告进行了审查,开发有关的机井和观察井的关键信息的地理数据库在这些测试监控。该信息包括特定抽水试验信息,如含水层的透射率和储水导出的值,干扰的程度在观察位置所指出的,和可接受的与不可接受的干扰的确定。虽然审查仅限于当前激活或允许钻孔水焦浆源,超过200的来源和1100个观测点横跨状态进行了评价。这项研究的结果表明,总体而言,地下水的干扰是不是在佛蒙特州的一个老大难问题。然而,不可接受的干扰 - 在一个特定的观测井源再也无法满足其需求的意图 - 在较高浓度的水焦浆源区几个实例指出。还确定,在给定观测位置的累积干扰不总是准确地跟踪随着时间的推移,作为一种有效的方法来跟踪累积干扰已不存在用于通过国家监管机构使用。在这项研究中开发的地理数据库,如果不断更新新的水焦浆源被允许,将允许跨佛蒙特州地下水干扰的有效跟踪。

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