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Stratified-drift aquifers in New Hampshire with potential to serve as future, large public water-supplies: Status, circa 2000; projected losses, circa 2025; and data accuracy.

机译:新罕布什尔州的分层漂移蓄水层有潜力作为未来的大型公共供水系统:状态,约2000年;预计损失,大约2025年;和数据准确性。

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Given the growing national water crisis, this research quantified and refined the states of stratified-drift aquifers with potential to yield 75+ gpm (OSDA75) and 150+ gpm (OSDA150) in New Hampshire for 2000 and 2025. Surface waters, cultural features and groundwater hazards from 13 federal/state datasets were buffered according to desired well yields, and then overlain within a geographic information system onto stratified-drift aquifer (OSDA) layer. Non-buffered, highly-transmissive polygons defined the aquifer areas remaining available with potential to meet 75+gpm or 150+ gpm well yields (RSDA75 or RSDA150). Aquifer losses for 2025 were modeled by principal-components regression as function of aquifer area and projected on-aquifer populations. Finally, the source OSDA area and RSDA estimates were reassessed using 1300 verification wells.;Results. OSDA encompasses 13.4% of New Hampshire, 41 % of its population and 58.3% of its groundwater hazards. The greatest population and groundwater-hazard densities exist on the most vulnerable aquifer areas, OSDA75 and OSDA150. After overlay analysis, RSDA75 and RSDA150 were estimated as 118.4 mi2 (9.5%) and 47.6 mi2 (3.8%), respectively. Most towns have less than 0.5 mi2 of RSDA75/150, while the majority of RSDA75/150 exists in relatively few towns. Regionally, the highly populated coast has minimal high-yield OSDA, while the more urban South and North each have about 5% and 2% of the state's RSDA75 and RSDA150, respectively. 1990-2000 population growth for Uplands and OSDA was 14% and 7% respectively. Projected OSDA75/150 losses for 2025 were unexpectedly low since historical OSDA population growth was lower than average; losses early in development are high, and the largest aquifers, (those forecast for the greatest population growth), accommodate additional people with lower per capita losses, since buffer overlap increases.;Verification wells suggest that 26% of all OSDA is either till, clay or unsaturated. Based on the Mazzafero equation, about 50% of the above RSDA75 and RSDA150 areas lack sufficient saturated thickness to sustain high yields. Existing water-quality issues will likely further reduce these estimates .;In summary, high-yield stratified-drift aquifers are far less available, and far more threatened than commonly thought. Given the national situation, these water resources need to be conserved to the greatest degree possible in the present.
机译:鉴于日益严重的国家水危机,这项研究量化和细化了分层漂移含水层的状态,它们有可能在2000年和2025年在新罕布什尔州分别生产75+ gpm(OSDA75)和150+ gpm(OSDA150)。地表水,文化特征和根据所需的井产量对来自13个联邦/州数据集的地下水危害进行缓冲,然后在地理信息系统中将其叠加到分层漂移含水层(OSDA)上。非缓冲,高透射率的多边形定义了仍可满足75 + gpm或150 + gpm井产量(RSDA75或RSDA150)的潜力的可用含水层面积。通过将主成分回归模型作为含水层面积的函数,对2025年的含水层损失进行建模,并预测含水层上的人口。最后,使用1300口验证井重新评估了源OSDA面积和RSDA估计值。 OSDA涵盖新罕布什尔州的13.4%,人口的41%和地下水危害的58.3%。最大的人口密度和地下水危害密度存在于最脆弱的含水层区域OSDA75和OSDA150。经过叠加分析后,估计RSDA75和RSDA150分别为118.4 mi2(9.5%)和47.6 mi2(3.8%)。大多数城镇的RSDA75 / 150面积不足0.5平方英里,而大多数RSDA75 / 150的城镇则相对较少。从区域来看,人口稠密的沿海地区的高产OSDA极少,而城市南部和北部分别占该州RSDA75和RSDA150的5%和2%。 1990-2000年,高地地区和OSDA的人口增长率分别为14%和7%。由于历史OSDA人口增长低于平均水平,预计2025年OSDA75 / 150的损失将出乎意料的低。开发初期的损失很高,最大的蓄水层(预测最大的人口增长)可容纳更多人,因为缓冲区重叠的增加,人均损失较低。验证井表明,所有OSDA的26%要么直到粘土或不饱和的。根据Mazzafero方程,上述RSDA75和RSDA150区域中约有50%缺乏足够的饱和厚度来维持高产量。现有的水质问题可能会进一步降低这些估算值。总之,高产分层漂移含水层的可获得性远低于人们普遍认为的水平,而且受到的威胁更大。考虑到国情,目前需要最大程度地保护这些水资源。

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