5 edition of Characterization of springflow in the north coast limestone of Puerto Rico using physical, chemical, and stable isotopic methods found in the catalog.
Published 1998 by Administrator in U.S. Dept. of the Interior, U.S. Geological Survey
Includes bibliographical references (p. 52-53).Prepared in cooperation with the Puerto Rico Aqueduct and Sewer Authority.One folded leaf of ill. in pocket.
|Statement||U.S. Dept. of the Interior, U.S. Geological Survey|
|Publishers||U.S. Dept. of the Interior, U.S. Geological Survey|
|The Physical Object|
|Pagination||xvi, 136 p. :|
|Number of Pages||79|
|3||Water-resources investigations report ;|
nodata File Size: 6MB.
Chen M 1988 Some experiences in compiling hydrogeological maps of karstic terrains in China [abs]. Lorenz, Lauren Tarbox, Bryan Buck, Haiping Qi, Tyler B. Geochemistry and hydrogeologic framework of the saline-freshwater interface and the calculation of net recharge in the Dorado area, north-central Puerto Rico, U.
Technical report 163, Texas Water Resources Institute, College Station, TX, 84 pp• US Geol Surv Water Resour Invest Rep 84-4113, 39 pp• Improved knowledge of the travel time between rainfall and aquifer recharge will improve the management of groundwater resources in Puerto Rico.
Hartmann A, Goldscheider N, Wagener T, Lange J, Weiler M 2014 Karst water resources in a changing world: Review of hydrological modeling approaches. Rapid Communications in Mass Spectrometry 2014, 28 181987-1994.
a Calibrated hydraulic conductivity is positively skewed; and b Logarithmic hydraulic conductivity log K is negatively skewed. The SCP aquifer is recharged both by direct rainfall and from intermittent streams that flow out of the mountains that are north of the coastal plain.
The present study evaluates the utility of the Equivalent Porous Media EPM approach to simulate dynamic groundwater hydraulics and contaminant transport in highly permeable karst unconfined aquifers using an example from the North Coast limestone aquifer system in Puerto Rico at an intermediate scale area of 132.
The migration and extent of TCE plume over two decades. Coplen, Haiping Qi, Lauren Tarbox, Jennifer Lorenz, Bryan Buck.
Quinlan JF, Ewers RO 1989 Subsurface drainage in the Mammoth Cave area. Model Setup and Calibration To illustrate the application, performance, and limitations of the EPM modeling approach in evaluating the release and transport of contamination in karst aquifers, a MODFLOW model was developed and paired with MT3DMS; both were implemented in Visual MODFLOW Standard 2011.
Long JCS, Gilmour P, Witherspoon PA 1985 A model for steady fluid flow in random three-dimensional networks of disc shaped fractures.
Water Resour Res 21 8 :1105—1115• Further isotopic ratios of groundwater had a slightly lower slope than that of LMWL, indicating little evaporation before rainwater percolates to groundwater for most of the year.
Torbarov K 1976 Estimation of permeability and effective porosity in karst on the basis of recession curve analysis. An example of an observation well with no correlation between depth-to-water and water temperature is Maguayo 2 in Dorado and and stable isotopic methods data are shown in. Angelini P, Dragoni W 1997 The problem of modeling limestone springs: the case of Bagnara North Apennines, Italy.
02 after a transition area with S y of 0.
Natl Vital Stat Rep 59:6• Key Factors of Precipitation Stable Isotope Fractionation in Central-Eastern Africa and Central Mediterranean.
Cross correlations were calculated with a sample length of 48 months.