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Quantitative Assessment of Regional Rock Aquifers, South-We stern Quebec, Canada

机译:加拿大魁北克省南韦斯特恩地区岩性含水层的定量评估

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The population of the St. Lawrence Lowlands platform in south-western Quebec, Canada, is heavily dependent on groundwater. The present study summarizes the quantity, quality and sustain-ability estimations of the groundwater resources found mainly in sedimentary rock aquifers. Results show that the regional groundwater flow in the considered domain of 1,500 km~2 is 97.7 Mm~3/y with: 86.6% infiltration from precipitation, 9.6% inflow from neighboring aquifers, and 3.8% induced recharge. The regional sustainability is defined with simulated drawdowns from uniform withdrawal scenarios. The current withdrawal rate of 18 Mm~3/y results in median drawdown of 0.6 m, compared to pre-development conditions. This drawdown is situated well in the sustainable range, an indication that regional aquifers are not overexploited. Hypothetical pumping rate of 24 Mm~3/y resulting in an average drawdown of 2.2 m is estimated as sustainable limit. Increasing exploitation from 24 to 51 Mm~3/y would need tight control and planning. Pumping rates beyond 51 Mm~3/y are judged not sustainable as regional drawdowns become high, ~8 m. The water levels in recharge areas are the most sensitive to groundwater extraction. Combining drawdown maps, groundwater quality zones, and aquifer vulnerability to surface contamination delineated the areas most suitable for future groundwater developments.
机译:加拿大西南魁北克的圣劳伦斯低地平台的人口严重依赖地下水。本研究总结了主要在沉积岩含水层中发现的地下水的数量,质量和可持续性估算。结果表明,在考虑的1,500 km〜2域内,区域地下水流量为97.7 Mm〜3 / y,其中:降水入渗量为86.6%,相邻含水层入渗量为9.6%,诱导补给量为3.8%。区域可持续性是通过统一撤出场景的模拟撤资来定义的。与开发前的条件相比,目前的撤出速度为18 Mm〜3 / y,导致中位数下降为0.6 m。这一下降幅度处于可持续范围之内,这表明区域含水层并未被过度开发。假设的平均抽水速率为24 Mm〜3 / y,导致平均回落为2.2 m,这是可持续的极限。将开采量从24 Mm增加到51 Mm〜3 / y需要严格的控制和计划。超过51 Mm〜3 / y的抽水速度被认为是不可持续的,因为区域水位下降很高,约为8 m。补给区的水位对地下水提取最敏感。结合水位图,地下水水质区和含水层对表面污染的脆弱性,这些区域最适合未来的地下水开发。

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