Time scales and mechanisms of estuarine variability, a synthesis from studies of San Francisco Bay
J. E. Cloern, F.H. Nichols
1985, Hydrobiologia (129) 229-237
This review of the preceding papers suggests that temporal variability in San Francisco Bay can be characterized by four time scales (hours, days-weeks, months, years) and associated with at least four mechanisms (variations in freshwater inflow, tides, wind, and exchange with coastal waters). The best understood component of temporal variability...
QUALITY ASSURANCE OF U. S. GEOLOGICAL SURVEY WATER-QUALITY FIELD MEASUREMENTS.
D. E. Erdmann, J.D. Thomas
1985, Conference Paper, ASTM Special Technical Publication
Reference samples are submitted semiannually to field analysts for measurement of these parameters with the same techniques and instruments used in the field. Both the personnel and the instruments involved in making the determinations are recorded. When the data are complete, a report defining the quality of the analytical results...
Vp/Vs ratios in the Yellowstone National Park region, Wyoming
S.N. Chatterjee, A.D. Pitt, H. M. Iyer
1985, Journal of Volcanology and Geothermal Research (26) 213-230
In this paper we study the variation of Vp/Vs and Poisson's ratio (??) in the Yellowstone National Park region, using earthquakes which were well recorded by a local seismic network. We find that the average Vp/Vs value within the geothermally active Yellowstone caldera is about 7% lower than in the...
Zeolites in Eocene basaltic pillow lavas of the Siletz River Volcanics, Central Coast Range, Oregon
Terry E.C. Keith, Lloyd W. Staplese
1985, Clays and Clay Minerals (33) 135-144
Zeolites and associated minerals occur in a tholeiitic basaltic pillow lava sequence that makes up part of the Eocene Siletz River Volcanics in the central Coast Range, Oregon. Regional zoning of zeolite assemblages is not apparent; the zeolites formed in joints, fractures, and interstices, although most occur in central cavities...
Water-level changes in the Ogallala aquifer, northwestern Oklahoma.
J.S. Havens
1985, Oklahoma Geology Notes (45) 205-210
The Ogallala aquifer, that part of the High Plains aquifer in Oklahoma, is part of a regional aquifer system that underlies parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming. In 1978 the US Geological Survey began a 5- year study of the High Plains regional...
GROUND-WATER DRAINAGE TO SURFACE MINES REFINED.
Linda S. Weiss
1985, Conference Paper
Changes in seepage flux and hydraulic head (ground-water level) resulting from ground-water drainage into the first and subsequent cuts of a surface coal mine can be estimated by a technique that considers drainage from the unsaturated zone and drainage effects of the advancing mine. A 'single-layer' technique is used, in...
New approach to calibrating bed load samplers
D. W. Hubbell, H.H. Stevens, J. V. Skinner, J.P. Beverage
1985, Journal of Hydraulic Engineering (111) 677-694
Cyclic variations in bed load discharge at a point, which are an inherent part of the process of bed load movement, complicate calibration of bed load samplers and preclude the use of average rates to define sampling efficiencies. Calibration curves, rather than efficiencies, are derived by two independent methods using...
Varechaetadrilus fulleri (Oligochaeta: Tubificidae): New record and amendment of morphological description
C. Rex Bingham, Jarl K. Hiltunen
1985, Freshwater Invertebrate Biology (4) 215-218
The tubificid worm Variechaetadrilus fulleri (Annelida: Oligochaeta) was described by Brinkhurst and Kathman (1983) from the Green River, Kentucky, the only locality from which the species has previously been reported. In 1982-84, a number of specimens of V. fulleri were found in the lower Mississippi River and in an adjacent...
WATER CHEMISTRY AND MINERALOGY OF MORGAN AND GROWLER HOT SPRINGS, LASSEN KGRA, CALIFORNIA.
J. Michael Thompson, Terry E.C. Keith, Jerry J. Consul
1985, Conference Paper, Transactions - Geothermal Resources Council
Because these springs contain substantial amounts of dissolved chloride, halite and sylvite are found above the water level as evaporitic deposits, along with gypsum. One spring is depositing pyrite that contains significant amounts of arsenic, antimony, and thallium. A yellow compound, composed of arsenic and sulfur, is being deposited in...
Food and feeding of fish in Hartwell Reservoir tailwater, Georgia-South Carolina
D. Hugh Barwick, Patrick L. Hudson
1985, Proceedings of the Annual Conference of the Southeastern Association of Fish and Wildlife Agencies (39) 185-193
Food of silver redhorse (Moxostoma anisurum), redbreast sunfish (Lepomis auritus), green sunfish (L. cyanellus), and bluegills (L. macrochirus) was examined to determine whether or not these fish in the Hartwell Reservoir tailwater (Savannah River, Georgia-South Carolina) ate organisms entrained from the reservoir or displaced from the tailwater during water releases...
Effects of abundance and water temperature on recruitment and growth of alewife (Alosa pseudoharengus) near South Bay, Lake Huron, 1954-82
Bryan A. Henderson, Edward H. Brown Jr.
1985, Canadian Journal of Fisheries and Aquatic Sciences (42) 1608-1613
Analysis of catches in pound nets provided indices of population size (ages 2–6) and of recruitment (ages 4–6) for alewives (Alosa pseudoharengus) spawning in South Bay (1954–82). Four hypotheses concerning the effects of stock size and water temperature on growth and recruitment were tested statistically. The number of recruits per...
STREAMFLOW LOSSES, CONSEQUENT FLOW THROUGH A THICK UNSATURATED ZONE, AND RECHARGE TO AN UNCONFINED AQUIFER.
J.R. Marie
1985, Conference Paper
Two experiments were conducted in conjunction with a 23-day aquifer test made in south-central Arizona to determine (1) water loss from a natural channel and (2) flow through a 330-foot-thick unsaturated zone overlying an unconfined aquifer. The experiments provided control for the aquifer test plus results relative to arid land...
VOLATILIZATION OF ALKYLBENZENES FROM WATER.
R. E. Rathbun, D. Y. Tai
1985, Conference Paper, National Meeting - American Chemical Society, Division of Environmental Chemistry
Volatilization is a physical process of importance in determining the fate of many organic compounds in streams and rivers. This process is frequently described by the conceptual-two-film model. The model assumes uniformly mixed water and air phases separated by thin films of water and air in which mass transfer is...
In-situ fluid-pressure measurements for earthquake prediction: An example from a deep well at Hi Vista, California
J. H. Healy, T. C. Urban
1985, Pure and Applied Geophysics PAGEOPH (122) 255-279
Short-term earthquake prediction requires sensitive instruments for measuring the small anomalous changes in stress and strain that precede earthquakes. Instruments installed at or near the surface have proven too noisy for measuring anomalies of the size expected to occur, and it is now recognized that even to have the possibility...
Quantification of transit losses, and its effects on surface-water resources, Arkansas River basin, Colorado
Russell K. Livingston
1985, Conference Paper
Colorado Water Law enables downstream water users to use natural river channels to convey water from upstream storage reservoirs to downstream canals, provided an equitable charge is made for transit loss. Charging a variable transit-loss rate for delivery of winter water stored in Pueblo Reservoir has resulted in better management...
Uranium mineralization in the Smith Lake district of the Grants uranium region, New Mexico.
N.S. Fishman, R. L. Reynolds, J. F. Robertson
1985, Economic Geology (80) 1348-1364
The Mariano Lake and Ruby 1 uranium orebodies, which together comprise much of the uranium ore in the Smith Lake district of the Grants uranium region, New Mexico, occur in sandstones in the lower part of the Brushy Basin Member of the Upper Jurassic Morrison Formation. The orebodies, which are...
Regional setting and new information on some critical geologic features of the West Shasta district, California
J. P. Albers, J.H.C. Bain
1985, Economic Geology (80) 2072-2091
The West Shasta massive sulfide district is in the easternmost of a series of accreted island-arc and oceanic crust terranes that comprise the Klamath Mountains. A sequence of submarine volcanic rocks of predominantly Early Devonian age is the principal component of the island-arc terrane in which the sulfide deposits are...
Diversion of lava during the 1983 eruption of Mount Etna
J. P. Lockwood, R. Romano
1985, Earthquake Information Bulletin (USGS) (17) 124-133
Mankind's first known attempt to divert a lava flow was in 1669, when a flow from Mount Etna volcano threatened the Sicilian city of Catania. This attempt was largely unsuccessful, in part due to opposition by citizens of another town, Paterno. Attempts to divert lava flows from Mauna Loa Volcano...
Geohydrology of the aquifer in the Santa Fe Group, northern West Mesa of the Mesilla Basin near Las Cruces, New Mexico
R. G. Myers, B. R. Orr
1985, Water-Resources Investigations Report 84-4190
Because of the heterogeneity of the Santa Fe Group, New Mexico, the hydrologic characteristics of the aquifer vary substantially from place to place. Hydraulic conductivities of 12 and 30 feet per day were estimated from aquifer tests for two wells in the eastern one-half of the study area. Well yields...
Notes on sedimentation activities calendar year 1984
U.S. Interagency Advisory Committee on Water Data- Subcommittee on Sedimentation
1985, Report
This report is a digest of information furnished by Federal agencies conducting sedimentation investigations. The decision to publish the report was made in 1946, from a proposal by the Chairman of the Federal Interagency River Basin Committee, Subcommittee on Ground Water. The Subcommittee approved the proposal and agreed to issue...
Installation of observation wells on hazardous waste sites in Kansas using a hollow-stem auger
C. A. Perry, R. J. Hart
1985, Ground Water Monitoring and Remediation (5) 70-73
Noncontaminating procedures were used during the hollow-stem auger installation of 12 observation wells on three hazardous waste sites in Kansas. Special precautions were taken to ensure that water samples were representative of the ground water in the aquifer and were not subjected to contamination from the land surface or cross...
Effects of cumulative loading level, as fish weight per unit flow, on water quality and growth of lake trout
J. W. Meade, J.S. Ramsey, J.C. Williams
1985, Journal of the World Mariculture Society (16) 40-51
Lake trout, Salvelinus namaycush, were cultured in a series of five rearing units (in triplicate). The fish removed available oxygen in each unit, from about 10.5 to 7.0 mg/L. Oxygen was replaced, through aeration, between rearing units. Effects of cumulative loading, as fish weight/flow rate, are described in terms of water...
A two-dimensional dam-break flood plain model
T. V. Hromadka II, C. E. Berenbrock, J. R. Freckleton, G. L. Guymon
1985, Advances in Water Resources (8) 7-14
A simple two-dimensional dam-break model is developed for flood plain study purposes. Both a finite difference grid and an irregular triangle element integrated finite difference formulation are presented. The governing flow equations are approximately solved as a diffusion model coupled to the equation of continuity. Application of the model to...
Foraminiferal, lithic, and isotopic changes across four major unconformities at Deep Sea Drilling Project Site 548, Goban Spur
C. Wylie Poag, Leslie A. Reynolds, James M. Mazzullo, Loyd D. Keigwin
1985, Book chapter, Initial reports of the Deep Sea Drilling Project
Sediment samples taken at close intervals across four major unconformities (middle Miocene/upper Miocene, lower Oligocene/upper Oligocene, lower Eocene/upper Eocene, lower Paleocene/upper Paleocene) at DSDP-IPOD Site 548, Goban Spur, reveal that coeval biostratigraphic gaps, sediment discontinuities, and seismic unconformities coincide with postulated low stands of sea level. Foraminiferal, lithic, and isotopic analyses demonstrate that...
Type curve analysis of inertial effects in the response of a well to a slug test.
Kenneth L. Kipp Jr.
1985, Water Resources Research (21) 1397-1408
The water level response to a slug or bailer test in a well completed in a confined aquifer has been evaluated taking into account well-bore storage and inertial effects of the water column in the well. The response range, from overdamped with negligible inertial effects to damped oscillation, was covered...