A method for estimating ground-water return flow to the Colorado River in the Parker area, Arizona and California
S. A. Leake
1984, Water-Resources Investigations Report 84-4229
Effects of hydraulic borehole mining on ground water at a test site in northeast St Johns County, Florida
P. S. Hampson
1984, Water-Resources Investigations Report 83-4149
An experimental mining project was conducted in northeast St. Johns County, Florida, to determine the feasibility of extracting deeply buried phosphate ore by hydraulic borehole mining techniques. The phosphate zone is between 232 and 250 feet below land surface and consists of approximately equal proportions of fine-grained phosphate, sand, and...
Generalized skew coefficient for flood frequency computations for the State of Hawaii
Reuben Lee
1984, Water-Resources Investigations Report 84-4027
In 1976, the Hydrology Committee of the U.S. Water Resources Council estimated a generalized skew coefficient for flood frequency computations of -0.05 for the State of Hawaii. This value is the average of 30 stream gaging stations with 25 or more years of record through water year 1973. This report...
Finite-element simulation of ground-water flow in the vicinity of Yucca Mountain, Nevada-California
J.B. Czarnecki, R. K. Waddell
1984, Water-Resources Investigations Report 84-4349
A finite-element model of the groundwater flow system in the vicinity of Yucca Mountain at the Nevada Test Site was developed using parameter estimation techniques. The model simulated steady-state ground-water flow occurring in tuffaceous, volcanic , and carbonate rocks, and alluvial aquifers. Hydraulic gradients in the modeled area range from...
Estimation of magnitude and frequency of floods in Pima County, Arizona, with comparisons of alternative methods
J.H. Eychaner
1984, Water-Resources Investigations Report 84-4142
Assessment of water resources at Fort Carson Military Reservation near Colorado Springs, Colorado
G.J. Leonard
1984, Water-Resources Investigations Report 83-4270
The Fort Carson Military Reservation adjoins the rapidly growning Colorado Springs metropolitan area, where locally available water supplies are limited and strictly administered. Fort Carson purchases about 3,400 acre-feet of treated water annually from the city of Colorado Springs. The major streams entering Fort Carson have an estimated average annual...
Reconnaissance evaluation of contamination in the alluvial aquifer in the East Poplar oil field, Roosevelt County, Montana
G. W. Levings
1984, Water-Resources Investigations Report 84-4174
Water moving from north to south in the alluvial aquifer of the Poplar River valley becomes contaminated with sodium chloride in the area underlain by the East Poplar oil fields. Four types of ground water were identified in the study area. Type 1 is sodium bicarbonate water. Type 2 is...
Sedimentation survey of Fena Reservoir, Guam, Mariana Islands, 1979
W. F. Curtis
1984, Water-Resources Investigations Report 84-4125
Fena Reservoir, in south-central Guam, was constructed in 1950-51 to provide a dependable water supply for the U.S. Navy. At the request of the U.S. Navy, the U.S. Geological Survey conducted a sedimentation survey of the Fena Reservoir during the months of November and December 1979. The sedimentation survey showed...
Planning report for the Gulf Coast Regional Aquifer-System Analysis in the Gulf of Mexico coastal plain, United States
Hayes F. Grubb
1984, Water-Resources Investigations Report 84-4219
Large quantities of water for municipal, industrial and agriculture use are supplied from the aquifers in Tertiary and younger sediments over an area of about 225,000 square miles in the Coastal Plain of Alabama, Arkansas, Florida, Illinois, Kentucky, Louisiana, Mississippi, Missouri, Tennessee, and Texas. Three regional aquifer systems, the Mississippi...
Water-resources of western Douglas County, Oregon
D. A. Curtiss, C. A. Collins, E. A. Oster
1984, Water-Resources Investigations Report 83-4017
In western Douglas County, Quaternary coastal dune sands and marine terrace deposits may have the best potential for ground-water development. Yields of 200 gallons per minute have been reported from wells completed in Quaternary fluvial deposits along the lower Umpqua River. The entire area is underlain by Tertiary marine sediments...
Computer model of one-dimensional equilibrium controlled sorption processes
D.B. Grove, K.G. Stollenwerk
1984, Water-Resources Investigations Report 84-4059
A numerical solution to the one-dimensional solute-transport equation with equilibrium-controlled sorption and a first-order irreversible-rate reaction is presented. The computer code is written in FORTRAN language, with a variety of options for input and output for user ease. Sorption reactions include Langmuir, Freundlich, and ion-exchange, with or without equal valance....
Hydrology and land use in Van Buren County, Michigan
T. R. Cummings, F. R. Twenter, D. J. Holtschlag
1984, Water-Resources Investigations Report 84-4112
This report gives the results of an investigation to determine the chemical and physical characteristics of ground and surface water in Van Buren County and to relate these characteristics to the agricultural use of land. Chemical inputs to the hydrologic system, including those from precipitation, animal wastes, septic tanks, and...
Estimates of dissolved and suspended substance yield of stream basins in Michigan
T. R. Cummings
1984, Water-Resources Investigations Report 83-4288
Water-quality data collected at 20 stations in Michigan were used to develop regression equations relating loads of dissolved and suspended substances to discharge. These equations and mean daily discharge were used to estimate long-term loads, which then were converted to estimates of drainage basin yields. These yields were compared to...
Hydrogeology and effects of tailings basins on the hydrology of Sands Plain, Marquette County, Michigan
N.G. Grannemann
1984, Water-Resources Investigations Report 84-4114
Sands Plain, a 225-square mile area, is near the Marquette iron-mining district in Michigan's Upper Peninsula. Gribben Basin, a settling basin for disposal of waste rock particles from iron-ore concentration, is in the western part. Because Sands Plain is near iron-ore deposits, but not underlain by them, parts of the...
Calibration and verification of a rainfall-runoff model and a runoff-quality model for several urban basins in the Denver metropolitan area, Colorado
J. B. Lindner-Lunsford, S. R. Ellis
1984, Water-Resources Investigations Report 83-4286
The U.S. Geological Survey 's Distributed Routing Rainfall-Runoff Model--Version II was calibrated and verified for five urban basins in the Denver metropolitan area. Land-use types in the basins were light commerical, multifamily housing, single-family housing, and a shopping center. The overall accuracy of model predictions of peak flows and runoff...
Potential effects of surface coal mining on the hydrology of the Corral Creek area, Hanging Woman Creek coal field, southeastern Montana
N. E. McClymonds
1984, Water-Resources Investigations Report 83-4260
The Corral Creek area of the Hanging Woman Creek coal field, 9 miles east of the Decker coal mines near the Tongue River, contains large reserves of Federal coal that have been identified for potential lease sale. A hydrologic study was conducted in the area to describe existing hydrologic systems...
Simulation of dynamic floodflows at gaged stations in the southeastern United States
R.E. Faye, M.E. Blalock
1984, Water-Resources Investigations Report 84-4000
Water-data program of the US Geological Survey in Kansas, fiscal year 1983
R.K. Livingston, K.D. Medina
1984, Water-Resources Investigations Report 84-4306
The U.S. Geological Survey is the principal Federal agency responsible for the collection of hydrologic data needed for the planning, development, use, and management of the water resources in Kansas. Hydrologic-data collection by the U.S. Geological Survey in Kansas began in 1895. The fiscal-year 1983 water-data program, operated in cooperation...
Storage analyses for ephemeral streams in semiarid regions
K. C. Glover
1984, Water-Resources Investigations Report 83-4078
A model has been developed for determining the probability of a reservoir being unable to provide a specified downstream water supply. By applying the model with a number of assumed storage capacities, the long-term water supply potential of a stream below a reservoir can be evaluated. Previous methods for determining...
Geohydrology of rocks penetrated by test well UE-25p#1, Yucca Mountain area, Nye County, Nevada
R. W. Craig, J. H. Robison
1984, Water-Resources Investigations Report 84-4248
Test well UE-25pNo1 was drilled in cooperation with the U.S. Department of Energy in the southwestern part of the Nevada Test Site, for investigations related to the isolation of high-level nuclear wastes. Rocks penetrated in the well are predominantly ash-flow tuffs of Tertiary age to a depth of 1,244 meters...
Techniques for estimating magnitude and frequency of floods on streams in Indiana
D.R. Glatfelter
1984, Water-Resources Investigations Report 84-4134
Equations are presented for estimating the magnitude and frequency of floods at ungaged sites on unregulated and nonurban streams in Indiana. The equations were developed by multiple-regression, analysis of basin characteristics and peak-flow statistical data from 242 gaged locations in Indiana, Ohio, and Illinois. The State of Indiana was divided...
Floods of March 1982, Indiana, Michigan, and Ohio
D.R. Glatfelter, G.K. Butch, J. A. Stewart
1984, Water-Resources Investigations Report 83-4201
Rapid melting of a snowpack containing 2 to 6 inches of water equivalent coinciding with moderate rainfall caused flooding in March 1982 across northern Indiana, southern Michigan, and northwestern Ohio. Millions of dollars in property damage and the loss of four lives resulted from the flooding. Peak discharges at several...
Regional flood relations for unregulated lakes in west-central Florida
M. A. Lopez, R.D. Hayes
1984, Water-Resources Investigations Report 84-4015
Regional lake flood altitude in the Southwest Florida Water Management District for 2- to 500-year recurrence intervals was estimated by multiple linear-regression analysis. The average lake altitude was used as a reference above which flood volumes are related to lake geometry, watershed characteristics, and rainfall. Average altitude at surface-outflow lakes...
Water-quality characteristics of urban runoff and estimates of annual loads in the Tampa Bay area, Florida, 1975-80
M. A. Lopez, R.F. Giovannelli
1984, Water-Resources Investigations Report 83-4181
Rainfall, runoff, and water quality data were collected at nine urban watersheds in the Tampa Bay area from 1975 to 1980. Watershed drainage area ranged from 0.34 to 0.45 sq mi. Land use was mixed. Development ranged from a mostly residential watershed with a 19% impervious surface, to a commercial-residential...
Analysis of urban storm-water runoff characteristics of four basins in the Baltimore metropolitan area, Maryland
G. T. Fisher, B. G. Katz
1984, Water-Resources Investigations Report 84-4099