U.S. Geological Survey, Carson City, NV 89701, USA.
Ground Water. 2010 Jul-Aug;48(4):526-37. doi: 10.1111/j.1745-6584.2009.00670.x. Epub 2010 Jan 22.
Arsenic concentrations can be managed with a relatively simple strategy of grouting instead of completely destroying a selected interval of well. The strategy of selective grouting was investigated in Antelope Valley, California, where groundwater supplies most of the water demand. Naturally occurring arsenic typically exceeds concentrations of 10 microg/L in the water produced from these long-screened wells. The vertical distributions of arsenic concentrations in intervals of the aquifer contributing water to selected supply wells were characterized with depth-dependent water-quality sampling and flow logs. Arsenic primarily entered the lower half of the wells where lacustrine clay deposits and a deeper aquifer occurred. Five wells were modified by grouting from below the top of the lacustrine clay deposits to the bottom of the well, which reduced produced arsenic concentrations to less than 2 microg/L in four of the five wells. Long-term viability of well modification and reduction of specific capacity was assessed for well 4-54 with AnalyzeHOLE, which creates and uses axisymmetric, radial MODFLOW models. Two radial models were calibrated to observed borehole flows, drawdowns, and transmissivity by estimating hydraulic-conductivity values in the aquifer system and gravel packs of the original and modified wells. Lithology also constrained hydraulic-conductivity estimates as regularization observations. Well encrustations caused as much as 2 microg/L increase in simulated arsenic concentration by reducing the contribution of flow from the aquifer system above the lacustrine clay deposits. Simulated arsenic concentrations in the modified well remained less than 3 microg/L over a 20-year period.
砷浓度可以通过相对简单的灌浆策略来管理,而不是完全破坏选定的井段。在加利福尼亚州的羚羊谷进行了选择性灌浆策略的研究,该地区的地下水供应了大部分的用水需求。这些长筛井生产的水中,天然存在的砷通常超过 10 微克/升。通过依赖深度的水质采样和流量记录,对供水井含水层中砷浓度的垂直分布进行了特征描述。砷主要进入到下部的井段,在那里存在湖泊粘土沉积物和更深的含水层。通过从湖泊粘土沉积物的顶部向下到井的底部对五口井进行灌浆改造,其中四口井的出水中砷浓度降低到 2 微克/升以下。使用 AnalyzeHOLE 评估了井 4-54 的井修改和比流量降低的长期可行性,该软件创建并使用轴对称、径向 MODFLOW 模型。通过估计含水层系统和原始和改造井的砾石填充的水力传导率值,对两个径向模型进行了校准,以拟合观测到的钻孔流量、水位下降和导水率。岩性也作为正则化观测来约束水力传导率的估计。由于湖泊粘土沉积物上方含水层系统的流量减少,井结垢导致模拟砷浓度增加了 2 微克/升。在 20 年的时间里,改造后的井中的模拟砷浓度仍保持在 3 微克/升以下。