2 edition of Hydrogeology and geochemistry of the unconfined aquifer, west-central and southwestern Delaware found in the catalog.
Hydrogeology and geochemistry of the unconfined aquifer, west-central and southwestern Delaware
J. M. Denver
by University of Delaware, Delaware Geological Survey in Newark, Del
Written in English
|Statement||by Judith Morton Denver.|
|Series||Report of investigations ;, no. 44, Report of investigations (Delaware Geological Survey) ;, no. 44.|
|LC Classifications||QE95 .A37 no. 44, GB1199.3.D3 .A37 no. 44|
|The Physical Object|
|Pagination||ix, 100 p. :|
|Number of Pages||100|
|LC Control Number||86623210|
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Hydrodynamics and Geochemistry of the Jurassic and Cretaceous Systems in the San Juan Basin, Northwestern New Mexico and Southwestern Colorado. Unpublished Ph.D. thesis, Stanford University. BERRY, F. A. F. Environmental & Engineering Geoscience Vol Number 1, February Table of Contents. 1. Simulations of Potential Future Conditions in the Cache Critical Groundwater Area, Arkansas Haveen M.
Downstream Channel Responses to Dam Impoundment, Delaware River Basin, Catskill Mountains, New York, Using Wetlands as a Natural Laboratory In the Middle School Classroom: An Example from the University of Tennessee National Science Foundation GK Program. The Patuxent aquifer crops out and subcrops in the northwestern part of the study area, but is confined to the southeast by the overlying Potomac Group clay-dominated lithofacies. Overlying the Potomac Group is a series of interbedded sands and .
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Hydrogeology and geochemistry of the unconfined aquifer, west-central and southwestern Delaware. Newark, Del.: University of Delaware, Delaware Geological Survey,  (OCoLC) Material Type: Government publication, State or province government publication: Document Type: Book: All Authors / Contributors: J M Denver; Delaware.
The unconfined aquifer is the major source of water supply in west-central and southwestern Delaware. The aquifer, which is composed of quartz sand, gravel, clay, and silt, ranges in thickness from 20 to feet.
The water table ranges from land surface to about 20 feet below land surface. Analyses of water from wells distributed throughout the area were used to study. Additional sources of ground water have been located in the Piedmont Province as a result of a ground-water exploration program conducted by the Delaware Geological Survey at the University of Delaware in cooperation with the City of Newark.
Drilling sites for relatively high-yielding wells were located through the use of geophysical investigations, air-photo interpretation, field. Kuniansky, Eve L., and Ardis, Ann F.,Hydrogeology and ground-water flow in the Edwards-Trinity aquifer system, west-central Texas: Regional aquifer-system analysis—Edwards-Trinity: U.S.
Geological Survey Professional Paper C, p. Library of Congress Cataloging-in-Publication Data Kuniansky, Eve by: 1. HYDROGEOLOGY AND GROUND-WATER CHEMISTRY OF THE SAN ANDRES-GLORIETA AQUIFER IN THEACOMA EMBAYMENTAND EASTERN ZUNI UPLIFT, WEST-CENTRAL NEW MEXICO By Joe A.
Baldwin and Scott K. Anderholm U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report Prepared in cooperation with the NEW MEXICO Cited by: 4. Hydrogeology and geochemistry of the Ogallala aquifer, Southern High Plains. Hydrol., The Ogallala aquifer, which underlies west-central and southwestern Delaware book Southern High Plains, consists of saturated sedi- ments of the Ogallala Formation (Neogene) that are deposited mainly as a set of humid-type alluvial fans derived from the Rocky by: An aquifer is an underground layer of water-bearing permeable rock, rock fractures or unconsolidated materials (gravel, sand, or silt).
Groundwater can be extracted using a water study of water flow in aquifers and the characterization of aquifers is called d terms include aquitard, which is a bed of low permeability along an.
Judith M Denver. United States Hydrogeology And Geochemistry Of The Unconfined Aquifer, West-Central And Southwestern Delaware. Article. Jan. Hydrogeology and ground-water chemistry of the San Andres-Glorieta aquifer in the Acoma embayment and eastern Zuni uplift, west-central New.
WRI No 31 - Investigation of Vertical Nitrate Gradients in a Shallow Unconfined Aquifer in North Dakota, by Jon C. Patch and Dr. Padmanabhan, WRI No 32 - Agricultural impact on water quality in a shallow confined aquifer and in the overlying saturated glacial till in eastern North Dakota: Movement of Pesticides, by W.M.
Schuh, D.L. Quantifying aquifer properties and freshwater resource in coastal barriers: a hydrogeophysical approach applied at Sasihithlu (Karnataka state, India).
Hydrology and Earth System Sciences, Vol. 16, Issue. 11, p. Cited by: Starks MJ () Mixing-zone diagenesis in a carbonate aquifer, west-central Florida.
Master’s thesis, Tampa, Univ South Fla Google Scholar Stewart JW Mills LR () Hydrogeology of the Sulphur Springs area, Tampa, : Sam Upchurch, Thomas M. Scott, Michael C. Alfieri, Beth Fratesi, Thomas L. Dobecki.
Hydrogeology and sources of recharge to the Buffalo and Wahpeton aquifers in the southern part of the Red River of the north drainage basin, west-central Minnesota and southeastern North Dakota / (Mounds View, Minn.: U.S.
Dept. of the Interior, U.S. Geological Survey ; Denver, CO: Branch of Information Services [distributor], ), by. MAIN LIBRARY. Perry-Castañeda Library East 21st St. Austin, TX. Phone: () Hydrogeology and simulation of ground-water flow in a deltaic sand-and-gravel aquifer, Cattaraugus Indian Reservation, southwestern New York / (Ithaca, N.Y.: U.S.
Dept. of the Interior, U.S. Geological Survey ; Denver, CO: Branch of Information Services [distributor], ), by Todd S.
Miller, Geological Survey (U.S.), and Seneca Nation (page. The subdisciplines of physical hydrogeology and chemical hydrogeology have evolved through a series of scales for the system under consideration.
For example, the regional study of artesian wells by Chamberlin () is generally recognized as the beginning of the science of hydrogeology in North America (Freeze and Back, ).Cited by: Research on Ground- and Surface-Water Contamination. Sort by Author The geologic origin and pathways of mobility of selenium from the California Coast Ranges to the west-central San Joaquin Valley M.W.,Distribution of dissolved atrazine and two metabolites in the unconfined aquifer, southeastern Delaware, in Mallard, G.E., and.
Salinityand Temperature-Dependent Groundwater Flow in the Floridan Aquifer System of South Florida by Joseph D.
Hughes A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Geology College of Arts and Sciences University of South Florida Major Professor: H.L.
Vacher, Ph.D. Ward. UT Austin Theses, by Year Geology dissertations and theses are listed in the following pages by the year completed, from through the end of. Levy, B.S., and Pannell, L.,Evaluation of a pressure system for estimating in-situ hydraulic conductivity, in Proceedings of the Fifth National Outdoor Action Conference on Aquifer Restoration, Ground Water Monitoring, and Geophysical Methods, Las Vegas, Nevada, MayDublin, Ohio, National Water Well Association, Ground Water.
Historic Shallow Natural Gas Occurrences in Cretaceous and Tertiary Aquifers in West-Central North Dakota GEOLOGIC INVESTIGATION NO. 58 NORTH DAKOTA GEOLOGICAL SURVEY Edward C. Murphy, State Geologist Lynn D. Helms, Director Dept. of Mineral Resources Reese RS () Hydrogeology, water quality, and distribution and sources of salinity in the Floridan aquifer system, Martin and St.
Lucie counties, Florida. US Geol Surv Water-Resour Invest Rept Google ScholarAuthor: Sam Upchurch, Thomas M. Scott, Michael C.
Alfieri, Beth Fratesi, Thomas L. Dobecki.ABSTRACT: Variables that describe well construction, hydrogeology, and land use were evaluated for use as possible indicators of the susceptibility of ground water in bedrock aquifers in the Newark Basin, New Jersey, to contamination by nitrate from the land surface.
Statistical analyses were performed on data for wells located throughout the Newark Basin. .