Matches in SemOpenAlex for { <https://semopenalex.org/work/W4251104148> ?p ?o ?g. }
Showing items 1 to 62 of
62
with 100 items per page.
- W4251104148 abstract "INTRODUCTION The tertiary limestone aquifer system of the southeastern United States is a sequence of carbonate rocks referred to as the Floridan aquifer in Florida and the principal artesian aquifer in Georgia, Alabama, and South Carolina. More than 3 billion gallons of water are pumped daily from the limestone aquifer; and the system is the principal source of municipal, industrial, and agricultural water supply in south Georgia and most of Florida. The aquifer system includes units of Paleocene to early Miocene age that combine to form a continuous carbonate sequence that is hydraulically connected in varying degrees. In a small area near Brunswick, Ga., a thin sequence of rocks of Late Cretaceous age is part of the system. In and directly downdip from much of the outcrop area, the system consists of one continuous permeable unit. Further downdip the aquifer system generally consists of two major permeable zones separated by a less-permeable unit of highly variable hydraulic properties (very leaky to virtually nonleaky). Conditions for the system vary from unconfined to confined depending upon whether the argillaceous Miocene and younger rocks that form the upper confining unit have been removed by erosion. This report is one of a series of preliminary products depicting the hydrogeologic framework, water chemistry, and hydrology of the aquifer system. The map shows the distribution of chloride ions in water from the upper permeable zone of the limestone aquifer system. The upper permeable zone consists of several formations, primarily the Tampa, Suwannee, Ocala, and Avon Park Limestones (Miller 1981a, b). Chloride concentrations of water within the upper permeable zone vary from nearly zero in recharge areas to many thousands of milligrams per liter (mg/L) in coastal discharge areas. Where the aquifer system discharges into the sea, the upper permeable zone contains increasing amounts of seawater. In these areas, wells that fully penetrate the upper permeable zone will yield water with chloride concentrations that approach that of seawater, about 19500 mg/L." @default.
- W4251104148 created "2022-05-12" @default.
- W4251104148 date "1982-01-01" @default.
- W4251104148 modified "2023-09-26" @default.
- W4251104148 title "Chloride Concentration in Water from the Upper Permeable Zone of the Tertiary Limestone Aquifer System, Southeastern United States" @default.
- W4251104148 doi "https://doi.org/10.3133/wri811103" @default.
- W4251104148 hasPublicationYear "1982" @default.
- W4251104148 type Work @default.
- W4251104148 citedByCount "0" @default.
- W4251104148 crossrefType "report" @default.
- W4251104148 hasBestOaLocation W42511041481 @default.
- W4251104148 hasConcept C12294951 @default.
- W4251104148 hasConcept C127313418 @default.
- W4251104148 hasConcept C151730666 @default.
- W4251104148 hasConcept C169212394 @default.
- W4251104148 hasConcept C174091901 @default.
- W4251104148 hasConcept C17409809 @default.
- W4251104148 hasConcept C187320778 @default.
- W4251104148 hasConcept C191897082 @default.
- W4251104148 hasConcept C192562407 @default.
- W4251104148 hasConcept C26568496 @default.
- W4251104148 hasConcept C2780659211 @default.
- W4251104148 hasConcept C33556824 @default.
- W4251104148 hasConcept C44259058 @default.
- W4251104148 hasConcept C75622301 @default.
- W4251104148 hasConcept C76177295 @default.
- W4251104148 hasConcept C76886044 @default.
- W4251104148 hasConcept C97512367 @default.
- W4251104148 hasConceptScore W4251104148C12294951 @default.
- W4251104148 hasConceptScore W4251104148C127313418 @default.
- W4251104148 hasConceptScore W4251104148C151730666 @default.
- W4251104148 hasConceptScore W4251104148C169212394 @default.
- W4251104148 hasConceptScore W4251104148C174091901 @default.
- W4251104148 hasConceptScore W4251104148C17409809 @default.
- W4251104148 hasConceptScore W4251104148C187320778 @default.
- W4251104148 hasConceptScore W4251104148C191897082 @default.
- W4251104148 hasConceptScore W4251104148C192562407 @default.
- W4251104148 hasConceptScore W4251104148C26568496 @default.
- W4251104148 hasConceptScore W4251104148C2780659211 @default.
- W4251104148 hasConceptScore W4251104148C33556824 @default.
- W4251104148 hasConceptScore W4251104148C44259058 @default.
- W4251104148 hasConceptScore W4251104148C75622301 @default.
- W4251104148 hasConceptScore W4251104148C76177295 @default.
- W4251104148 hasConceptScore W4251104148C76886044 @default.
- W4251104148 hasConceptScore W4251104148C97512367 @default.
- W4251104148 hasLocation W42511041481 @default.
- W4251104148 hasLocation W42511041482 @default.
- W4251104148 hasOpenAccess W4251104148 @default.
- W4251104148 hasPrimaryLocation W42511041481 @default.
- W4251104148 hasRelatedWork W1535675219 @default.
- W4251104148 hasRelatedWork W1553671369 @default.
- W4251104148 hasRelatedWork W169858389 @default.
- W4251104148 hasRelatedWork W2262581972 @default.
- W4251104148 hasRelatedWork W2267080146 @default.
- W4251104148 hasRelatedWork W2350938107 @default.
- W4251104148 hasRelatedWork W2381910211 @default.
- W4251104148 hasRelatedWork W2916186022 @default.
- W4251104148 hasRelatedWork W351167174 @default.
- W4251104148 hasRelatedWork W985732587 @default.
- W4251104148 isParatext "false" @default.
- W4251104148 isRetracted "false" @default.
- W4251104148 workType "report" @default.