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Evaluation of Major Dike-Impounded Ground-Water Reservoirs, Island of Oahu

机译:评估瓦胡岛主要堤防蓄水地下水库

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摘要

"Ground-water reservoirs on Oahu store a very large but only approximately estimatable quantity of freshwater. These reservoirs include interconnected water bodies that are impounded by volcanic dikes or other geologic structures, and water bodies that are floating on saline ground water in dike-free Java flows in the flanks of the volcanoes. A significant amount of water is stored above sea level, to an altitude of at least 2,000 feet in the Waianae Range, but most is stored below sea level. The depths of freshwater storage below sea level range from a few feet to 1,000 feet or more in the dike-free lavas, and probably to several thousands of feet in the compartmented lavas between dikes. Other water bodies, smalI in comparison, are perched above and isolated from these interconnected bodies."This report is primarily concerned with high-head dike-impounded ground-water reservoirs that underlie interior mountainous areas where rainfall and subsequent recharge to ground water are the greatest. These reservoirs, owing to their upgradient positions, play a very important role in the recharge, storage, movement, and discharge of alI ground water on the island."
机译:“Oahu上的地下水储存器非常大但只有大约估计的淡水。这些水库包括由火山堤防或其他地质结构扣押的相互连接的水体,以及漂浮在普遍的盐水地水上的水体Java在火山的侧翼流动。大量的水储存在海平面上方,到Waianae范围内至少2,000英尺的海拔高度,但大多数储存在海平面下方。海平面下方淡水储存的深度在无摩托的熔岩中,从几英尺到1000英尺或更长时间,可能在堤坝之间的隔间熔岩中的数千英尺。其他水体,相比之下,从这些相互连接的体中栖息地栖息。“这报告主要涉及高头堤防 - 被扣押的地下水储层,利润降雨和随后的地下水充电是GR的吃。由于其升级性职位,这些水库在岛上的充电,储存,运动和排放中发挥着非常重要的作用。“

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