by U.S. G.P.O., For sale by the Books and Open-File Reports Section, U.S. Geological Survey in Washington, Denver, CO .
Written in English
Bibliography: p. 15.
|Statement||by Allen L. Zack ; prepared in cooperation with Water Resources Research Institute, University of Puerto Rico.|
|Series||U.S. Geological Survey water-supply paper ;, 2328|
|Contributions||University of Puerto Rico (Mayagüez Campus). Water Resources Research Institute.|
|LC Classifications||TD223.P9 Z33 1988|
|The Physical Object|
|Pagination||iv, 15 p. :|
|Number of Pages||15|
|LC Control Number||87600408|
Get this from a library! A well system to recover usable water from a freshwater-saltwater aquifer in Puerto Rico. [Allen L Zack; University of Puerto Rico (Mayagüez Campus). Water Resources Research Institute.]. Hydrogeology of the North Coast Limestone Aquifer System of Puerto Rico By Jesus Rodriguez-Martmez Abstract The North Coast Limestone aquifer system of Puerto Rico is composed of three regional hydrogeologic units: an upper aquifer that contains an underlying saltwater zone near the coast, a middle confining unit, and a lower by: 4. A well system to recover usable water from a freshwater-saltwater aquifer in Puerto Rico. U.S. Geological Survey Water-Supply Paper U.S. Geological Survey Water-Supply Paper Google ScholarCited by: 1. A well system to recover usable water from a freshwater-saltwater aquifer in Puerto Rico. Laboratory experiments on a single well system built into a mini aquifer constructed of.
A well system to recover usable water from a freshwater-saltwater aquifer in Puerto Rico. U.S. Geological Survey Water-Supply Paper U.S. Geological Survey Water-Supply Paper Google ScholarAuthor: Robert G. Maliva. A well system to recover usable water from a freshwater-saltwater aquifer in Puerto Rico. While the focus is on resultant limitation in the agricultural usage of ground water, the book . The hydrogeologic framework for the Floridan aquifer system (Williams and Kuniansky, ; Williams and Dixon, ) has been revised by incorporating new studies and data that have become available since the original framework established by the U.S. Geological Survey in the s (Miller, ).Adjustments were made to the internal boundaries of the Upper and Lower Floridan aquifers as well. Gómez-Gómez, Fernando, , Hydrochemistry of the South Coastal Plain Aquifer System of Puerto Rico and its relation to surface-water recharge, in Gómez-Gómez, Fernando, Quiñones-Aponte, Vicente, and Johnson, A.I., eds., Aquifers of the Caribbean Islands, Proceedings of the International Symposium on Tropical Hydrology, San Juan, PR, July.
In Figure 5 a contour plot of the freshwater and salt water interface is shown. The location of the ”” contour line, which represents the toe of the saltwater intrusion wedge, occurs at a distance from the center of the island that varies between slightly below to feet, depending on direction. Note, theFile Size: 1MB. Freshwater And Saltwater Interactions In Coastal Groundwater Woods Hole, MA — Scientists have recently recognized an imbalance in the flow of salty groundwater into the coastal ocean: considerable saltwater discharge into the ocean has been observed, but little or no return flow has been seen. Figure 1: Saltwater intrusion in a coastal aquifer environment (Barlow, ) In standard transport modeling (using MT3DMS), it is assumed that the solute is dilute and miscible (soluble within groundwater), and that solute density does not affect the groundwater flow behaviour. Speiran, ). The freshwater/saltwater interface in the Upper Floridan Aquifer was located to the northeast of Hilton Head Island under predevelopment conditions. The natural balance between recharge to the Upper Floridan Aquifer and discharge from the aquifer served to establish the position of the freshwater/saltwater boundary offshore.