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Page 4383, results 109551 - 109575

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Publication Extents

Not all publications have extents, not all extents are completely accurate
On the nature of persistence in dendrochronologic records with implications for hydrology
J.M. Landwehr, N.C. Matalas
1986, Journal of Hydrology (86) 239-277
Hydrologic processes are generally held to be persistent and not secularly independent. Impetus for this view was given by Hurst in his work which dealt with properties of the rescaled range of many types of long geophysical records, in particular dendrochronologic records, in addition to hydrologic records. Mandelbrot introduced an...
River meanders and channel size
G. P. Williams
1986, Journal of Hydrology (88) 147-164
This study uses an enlarged data set to (1) compare measured meander geometry to that predicted by the Langbein and Leopold (1966) theory, (2) examine the frequency distribution of the ratio radius of curvature/channel width, and (3) derive 40 empirical equations (31 of which are original) involving meander and channel...
Use of the chloride ion in determining hydrologic-basin water budgets - A 3-year case study in the San Juan Mountains, Colorado, U.S.A.
H.C. Claassen, M.M. Reddy, D.R. Halm
1986, Journal of Hydrology (85) 49-71
Measurement of chloride concentration and water equivalent in precipitation and recharge at a site can be extrapolated to determine available moisture in a nearby basin. This method also may be extrapolated to a basin with similar climatic characteristics if precipitation, vegetation, and topographic data are available. The average accuracy of...
Determination of the components of stormflow using water chemistry and environmental isotopes, Mattole River basin, California
V. C. Kennedy, C. Kendall, G. W. Zellweger, T.A. Wyerman, R.J. Avanzino
1986, Journal of Hydrology (84) 107-140
The chemical and isotopic composition of rainfall and stream water was monitored during a storm in the Mattole River basin of northwestern California. About 250 mm of rain fell during 6 days (∼80% within a 42 h period) in late January, 1972, following 24 days of little or no precipitation....
Groundwater flow into Lake Michigan from Wisconsin
D.S. Cherkauer, B.R. Hensel
1986, Journal of Hydrology (84) 261-271
Detailed hydrogeological study has been done at six sites along the Lake Michigan shoreline in Wisconsin. At each site a flux of groundwater to the lake has been calculated for both natural conditions and the existing conditions created by pumping. The values from each site have then been extrapolated to...
Limnological characteristics of selected lakes in the Nebraska sandhills, U.S.A., and their relation to chemical characteristics of adjacent ground water
J.W. La Baugh
1986, Journal of Hydrology (86) 279-298
Limnological characteristics of Crane, Hackberry, Island and Roundup Lakes, and chemical characteristics of shallow ground water, within the Crescent Lake National Wildlife Refuge, western Nebraska, were determined during a preliminary investigation of the interaction between lakes and ground water in this study area between 1980 and 1984. When ice cover...
A boundary element-Random walk model of mass transport in groundwater
M. Kemblowski
1986, Journal of Hydrology (85) 305-318
A boundary element solution to the convective mass transport in groundwater is presented. This solution produces a continuous velocity field and reduces the amount of data preparation time and bookkeeping. By combining this solution and the random walk procedure, a convective-dispersive mass transport model is obtained. This model may be...
A comparison of the coupled fresh water-salt water flow and the Ghyben-Herzberg sharp interface approaches to modeling of transient behavior in coastal aquifer systems
H.I. Essaid
1986, Journal of Hydrology (86) 169-193
A quasi-three dimensional finite difference model which simulates coupled, fresh water and salt water flow, separated by a sharp interface, is used to investigate the effects of storage characteristics, transmissivity, boundary conditions and anisotropy on the transient responses of such flow systems. The magnitude and duration of the departure of...
Groundwater model of the Blue River basin, Nebraska-Twenty years later
W.M. Alley, P. A. Emery
1986, Journal of Hydrology (85) 225-249
Groundwater flow models have become almost a routine tool of the practicing hydrologist. Yet, surprisingly little attention has been given to true verification analysis of studies using these models. This paper examines predictions for 1982 of water-level declines and streamflow depletions that were made in 1965 using an electric analog...
Stratigraphy and correlation of the glacial deposits on the Montana Plains
D. S. Fullerton, R. B. Colton
1986, Quaternary Science Reviews (5) 69-82
Till units representing at least three pre-Illinoian continental glaciations, at least one Illinoian glaciation, and a late Wisconsin glaciation have been identified on the Montana Plains. Early Wisconsin or middle Wisconsin till units have not been identified. The southernmost limit of late Wisconsin glaciation is in Montana, more than 170...
Determination of ammonium in a buddingtonite sample by ion-chromatography
P.R. Klock, P. J. Lamothe
1986, Talanta (33) 495-498
An ion-chromatographic method for the direct determination of ammonium, potassium, and sodium in geologic materials is described. Samples are decomposed with a mixture of hydrofluoric and hydrochloric acids in a sealed polycarbonate bottle heated in a microwave oven. The ion-chromatograph separates the cations and determines them by conductivity measurement. The...
An analytical scheme for determining forms of sulphur in oil shales and associated rocks
M. L. Tuttle, M. B. Goldhaber, D.L. Williamson
1986, Talanta (33) 953-961
An analytical scheme for determining various forms of sulphur in oil shales and associated rocks is presented. Acid-soluble sulphate, sulphur contained in monosulphide and in disulphide minerals, and organically-bound sulphur are all quantitatively recovered as separate fractions. Finely-ground oil-shale samples are treated in an inert atmosphere with 6M hydrochloric acid to...
Separation and preconcentration of the rare-earth elements and yttrium from geological materials by ion-exchange and sequential acid elution
J.G. Crock, F.E. Lichte, G. O. Riddle, C.L. Beech
1986, Talanta (33) 601-606
The abundance of rare-earth elements (REE) and yttrium in geological materials is generally low, and most samples contain elements that interfere in the determination of the REE and Y, so a separation and/or preconcentration step is often necessary. This is often achieved by ion-exchange chromatography with either nitric or hydrochloric...
The Outer Banks of North Carolina
Robert Dolan, Harry F. Lins
1986, Professional Paper 1177-B
Understanding the natural dynamics of barrier islands in the key to recognizing and estimation both the short-term and the long-term hazards of living on them. This report summarizes how the barrier islands were created, how they have changed, and why they will continue to change in spite of efforts to...
National water summary 1985: Hydrologic events and surface-water resources
United States Geological Survey
1986, Water Supply Paper 2300
The surface-water resources of the United States, the focal point for this National Water Summary, are extensively developed and managed to provide water supplies, hydroelectric power, navigation, recreational opportunities, and sufficient instream flows to maintain fish and wildlife habitats and adequate water quality. Surface water represents 77 percent of the...
Fluorometric procedures for dye tracing
James F. Wilson, Ernest D. Cobb, F. A. Kilpatrick
1986, Techniques of Water-Resources Investigations 03-A12
This manual describes the current fluorometric procedures used by the U.S. Geological Survey in dye tracer studies such as time of travel, dispersion, reaeration, and dilution-type discharge measurements. The advantages of dye tracing are (1) low detection and measurement limits and (2) simplicity and accuracy in measuring dye tracer concentrations using fluorometric techniques. The manual contains necessary...