In natural channels there are often long periods of low flow during which solutes have repeated opportunity for contact with relatively immobile bed materials. Such conditions can exist in very small pool-and-riffle mountain streams. If a solute can sorb onto bed materials, then both hydrodynamic and chemical processes control solute transport. A simulation of these processes is presented for a carefully controlled and intensively monitored strontium injection experiment. The numerical model couples nonreactive, transient storage with a kinetic mass transport model for sorption. The results are compared to both in-stream and on-sediment strontium measurements. In mountain streams the stream hydrology is complex and is governed by a wide variety of time and distance scales. The present simulations assist in interpreting the relative roles of hydrologic and sorptive kinetic processes, and indicate the practical limits of our process and parameter knowledge. The simulations are relatively insensitive to the details of the kinetic mechanisms and to the spatial variability of the stream parameters.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR019i003p00732","usgsCitation":"Bencala, K.E., 1983, Simulation of solute transport in a mountain pool-and-riffle stream with a kinetic mass transfer model for sorption: Water Resources Research, v. 19, no. 3, p. 732-738, https://doi.org/10.1029/WR019i003p00732.","productDescription":"7 p.","startPage":"732","endPage":"738","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221226,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505b9083e4b08c986b319552","contributors":{"authors":[{"text":"Bencala, Kenneth E. kbencala@usgs.gov","contributorId":1541,"corporation":false,"usgs":true,"family":"Bencala","given":"Kenneth","email":"kbencala@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":360765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011286,"text":"70011286 - 1983 - Geophysical Logging in Carbonate Aquifers","interactions":[],"lastModifiedDate":"2024-03-21T12:20:47.503248","indexId":"70011286","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Geophysical Logging in Carbonate Aquifers","docAbstract":"Some logging methods are inherently superior to others for the analysis of limestone and dolomite aquifers. Three such systems are the density, neutron, and acousticvelocity logs.
Relative percentages of limestone and dolomite, average matrix (grain) densities of the rock mixtures, and porosity of the rock mass can be calculated from density, neutron, and acoustic-velocity logs. Wells drilled before the 1960's generally were logged with an uncalibrated neutron tool. In some instances, the resultant curve can be empirically calibrated.
With supporting data from resistivity logs, apparent water resistivity (Rwa) can be estimated. Depending on rock and mud resistivities, the two most useful resistivity curves for water-quality studies are the deeply-focused laterolog and the induction log. For older wells, the standard electric log may be used, if the drilling mud is not salt-saturated.
Rwa contour maps derived from geophysical data are useful to outline areas of recharge, direction of probable ground-water flow, and location and salinity of brine areas. Another useful application of well logs is estimation of ground-water temperature. These temperatures are obtained from maximum-reading thermometer data that generally are recorded on each logging run. Maps of porosity can be used to outline potential areas for completing large-yield wells.
Birdseyes, birdseye limestone, fenestrae, fenestral fabric, shrinkage pores, and loferites are considered similar or synonymous when occurring in lime mudstone or syndepositional dolomite, especially in association with mudcracks and stromatolites. Compaction experiments indicate, however, that without early cementation, these vugs can be obliterated, whereas mudcracks and stromatolites are unchanged. Lumping of burrows and root tubes under the general terms birdseyes or fenestrae, such as for example tubular fenestrae, burrow fenestrae, or root-tube fenestrae, is discouraged. They should be called burrows or root tubes because the birdseyes, fenestrae, and shrinkage pores are so intimately associated with tidal flats to most geologists. Submarine cementation of pelletal and oolitic botryoidal grainstone under 5 to 6 m of water on the Bahama Banks has resulted in vugs provocatively similar to many birdseyes and fenestrae generally attributed to peritidal conditions in the literature. Birdseyes and fenestrae in ancient grainstones cannot therefore be reliably identified without consideration of the sedimentary sequence and associated sedimentary structures.--Modified journal abstract.
Models which solve the governing groundwater flow or solute transport equations in conjunction with optimization techniques, such as linear and quadratic programing, are powerful aquifer management tools. Groundwater management models fall in two general categories: hydraulics or policy evaluation and water allocation. Groundwater hydraulic management models enable the determination of optimal locations and pumping rates of numerous wells under a variety of restrictions placed upon local drawdown, hydraulic gradients, and water production targets. Groundwater policy evaluation and allocation models can be used to study the influence upon regional groundwater use of institutional policies such as taxes and quotas. Furthermore, fairly complex groundwater-surface water allocation problems can be handled using system decomposition and multilevel optimization. Experience from the few real world applications of groundwater optimization-management techniques is summarized. Classified separately are methods for groundwater quality management aimed at optimal waste disposal in the subsurface. This classification is composed of steady state and transient management models that determine disposal patterns in such a way that water quality is protected at supply locations. Classes of research missing from the literature are groundwater quality management models involving nonlinear constraints, models which join groundwater hydraulic and quality simulations with political-economic management considerations, and management models that include parameter uncertainty.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR019i002p00305","usgsCitation":"Gorelick, S.M., 1983, A review of distributed parameter groundwater management modeling methods: Water Resources Research, v. 19, no. 2, p. 305-319, https://doi.org/10.1029/WR019i002p00305.","productDescription":"15 p.","startPage":"305","endPage":"319","costCenters":[],"links":[{"id":220971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5059e550e4b0c8380cd46c9e","contributors":{"authors":[{"text":"Gorelick, Steven M.","contributorId":8784,"corporation":false,"usgs":true,"family":"Gorelick","given":"Steven","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":360732,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011274,"text":"70011274 - 1983 - Role of fluid mixing and fault-related sulfide in the origin of the Ray Point uranium district, south Texas","interactions":[],"lastModifiedDate":"2024-01-11T16:42:28.609707","indexId":"70011274","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Role of fluid mixing and fault-related sulfide in the origin of the Ray Point uranium district, south Texas","docAbstract":"The Lamprecht and Felder deposits are roll-type deposits hosted by the Miocene Oakville Sandstone. Four distinct stages of FeS 2 mineral formation are recognized: (1) a generation of isotopically light (delta 34 S < -20 per mil) preore pyrite, (2) a generation of isotopically light (delta 34 S < -20 per mil) marcasite that formed mostly before, but also during ore deposition, (3) a postore generation of isotopically heavy pyrite (delta 34 S > 0 per mil), and (4) a yet later generation of marcasite with isotopically light sulfur close to the values of stages 1 and 2. Complex zone of mixing between saline brines migrating up the fault from depth and oxygenated meteoric water recharging at the outcrop. Bacterial activity.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.78.6.1043","issn":"03610128","usgsCitation":"Goldhaber, M., Reynolds, R.L., and Rye, R.O., 1983, Role of fluid mixing and fault-related sulfide in the origin of the Ray Point uranium district, south Texas: Economic Geology, v. 78, no. 6, p. 1043-1063, https://doi.org/10.2113/gsecongeo.78.6.1043.","productDescription":"21 p.","startPage":"1043","endPage":"1063","numberOfPages":"21","costCenters":[],"links":[{"id":220895,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"78","issue":"6","noUsgsAuthors":false,"publicationDate":"1983-10-01","publicationStatus":"PW","scienceBaseUri":"505aae50e4b0c8380cd87083","contributors":{"authors":[{"text":"Goldhaber, M. B. 0000-0002-1785-4243","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":103280,"corporation":false,"usgs":true,"family":"Goldhaber","given":"M. B.","affiliations":[],"preferred":false,"id":360726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, R. L. 0000-0002-4572-2942","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":79885,"corporation":false,"usgs":true,"family":"Reynolds","given":"R.","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":360725,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rye, R. O.","contributorId":66208,"corporation":false,"usgs":true,"family":"Rye","given":"R.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":360724,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011261,"text":"70011261 - 1983 - A method of calculating quartz solubilities in aqueous sodium chloride solutions","interactions":[],"lastModifiedDate":"2024-03-19T15:53:17.532025","indexId":"70011261","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"A method of calculating quartz solubilities in aqueous sodium chloride solutions","docAbstract":"The aqueous silica species that form when quartz dissolves in water or saline solutions are hydrated. Therefore, the amount of quartz that will dissolve at a given temperature is influenced by the prevailing activity of water. Using a standard state in which there are 1,000 g of water (55.51 moles) per 1,000 cm3 of solution allows activity of water in a NaCl solution at high temperature to be closely approximated by the effective density of water, pe, in that solution, i.e. the product of the density of the NaCl solution times the weight fraction of water in the solution, corrected for the amount of water strongly bound to aqueous silica and Na+ as water of hydration. Generally, the hydration of water correction is negligible.
The solubility of quartz in pure water is well known over a large temperature-pressure range. An empirical formula expresses that solubility in terms of temperature and density of water and thus takes care of activity coefficient and pressure-effect terms. Solubilities of quartz in NaCl solutions can be calculated by using that equation and substituting pe, for the density of pure water. Calculated and experimentally determined quartz solubilities in NaCl solutions show excellent agreement when the experiments were carried out in non-reactive platinum, gold, or gold plus titanium containers. Reactive metal containers generally yield dissolved silica concentrations higher than calculated, probably because of the formation of metal chlorides plus NaOH and H2. In the absence of NaOH there appears to be no detectable silica complexing in NaCl solutions, and the variation in quartz solubility with NaCl concentration at constant temperature can be accounted for entirely by variations in the activity of water.
The average hydration number per molecule of dissolved SiO2 in liquid water and NaCl solutions decreases from about 2.4 at 200°C to about 2.1 at 350°C. This suggests that H4SiO4 may be the dominant aqueous silica species at 350°C, but other polymeric forms become important at lower temperatures.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(83)90279-X","issn":"00167037","usgsCitation":"Fournier, R., 1983, A method of calculating quartz solubilities in aqueous sodium chloride solutions: Geochimica et Cosmochimica Acta, v. 47, no. 3, p. 579-586, https://doi.org/10.1016/0016-7037(83)90279-X.","productDescription":"8 p.","startPage":"579","endPage":"586","numberOfPages":"8","costCenters":[],"links":[{"id":220759,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e45ae4b0c8380cd465e0","contributors":{"authors":[{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":360689,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011259,"text":"70011259 - 1983 - Asymptotic distribution of the maximum deficit with correlated, partially regulated outflows","interactions":[],"lastModifiedDate":"2018-02-07T13:42:01","indexId":"70011259","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Asymptotic distribution of the maximum deficit with correlated, partially regulated outflows","docAbstract":"The asymptotic distribution of the maximum accumulated deficit with partially regulated, Markov-dependent net outflows having a Bernoulli distribution is derived, and the distribution for independent, continuous outflows is presented. It is demonstrated that under partial regulation the maximum deficit behaves as log n, where n is the length of the series; this is to be contrasted with the n½ behavior exhibited by fully regulated outflows. Also, as would be expected, the presence of correlation tends to increase the magnitude and variability of the maximum deficit.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR019i001p00104","usgsCitation":"Troutman, B.M., 1983, Asymptotic distribution of the maximum deficit with correlated, partially regulated outflows: Water Resources Research, v. 19, no. 1, p. 104-108, https://doi.org/10.1029/WR019i001p00104.","productDescription":"5 p.","startPage":"104","endPage":"108","costCenters":[],"links":[{"id":220696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5059ee99e4b0c8380cd49e5f","contributors":{"authors":[{"text":"Troutman, Brent M.","contributorId":195329,"corporation":false,"usgs":false,"family":"Troutman","given":"Brent","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":360679,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011258,"text":"70011258 - 1983 - Mechanical and chemical compaction in fine-grained shallow-water limestones","interactions":[],"lastModifiedDate":"2024-05-21T23:40:46.645777","indexId":"70011258","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Mechanical and chemical compaction in fine-grained shallow-water limestones","docAbstract":"Artificial compaction of in-situ cores of sediments resulted in: 1) reduction of sediment thickness by 50 percent and more; 2) reduction of initial porosities of 65 to 75 percent to 35 to 45 percent; 3) creation of megascopic textures almost identical to many ancient lime mud- and wackestone; 4) creation of organic, wispy \"stylolite-like\" layers; 5) chemical compaction, evidenced by thin sections showing quartz grains piercing mollusc shells without causing fractures and SEM evidence of solutional interfitting of 1 to 4-mu m-size aragonitic carbonate grains; 6) obliteration of pellets and birdseye or fenestral voids in those sediments where early cementation was lacking; obliteration of identifiable marine grasses and vertical \"root\" tube voids; 8) mashing of sediment-filled circular burrows to produce ellipsoidal structures. Significant mechanical compaction resulted from pressures simulating less than 1,000 ft of burial. Increasing loads to more than 10,000 ft did not significantly increase compaction. Chemical compaction was detected only in cores compacted to pressures greater than 10,000 ft of burial. These experiments suggest that chemical compaction would begin at much shallower depths given geologic time. Experiments that caused chemical compaction lend support to the hypothesis that cement required to produce a low-porosity/low-permeability fine-grained limestone is derived internally. Dissolution, ion diffusion, and reprecipitation are the most likely processes for creating significant thicknesses of dense limestones. Continuation of chemical compaction after significant porosity reduction necessitates expulsion of connate fluids, possibly including hydrocarbons.--Modified journal abstract.
Nine watersheds in the Colorado Front Range with steep bedrock channels were used to test the accuracy of paleohydraulic reconstruction of large flash floods using boulder deposits. The nine basins consist of eight small ungauged basins ranging in size from 1.6 to 29 km2 and the Big Thompson River at the mouth of the Big Thompson Canyon, draining 790 km2. Between 1923 and 1976, all nine basins had had one catastrophic flash flood, the magnitude of which has been estimated by the conventional slope-area method.
In each basin, coarse boulder deposits of the large flash floods were identified, and three axes of the five largest boulders were measured, along with at least two profiles of the valley cross section. A simple arithmetic average of two theoretical and two empirical relationships was used to estimate average flood velocity using boulder size and shape. Average depth was estimated as the arithmetic average of four values computed from the Manning equation, a regression equation for boulder size and unit stream power, a relative smoothness equation, and a modified Shields' relationship. The appropriate flood width for the estimated average depth was found by iteration, using the valley cross sections.
The paleohydraulic discharges thus computed generally underestimate conventional slope-area discharge estimates on small streams by as much as 75%, although the average amount is only 28% too low, and the reconstructed discharge in one stream was 31% too large. The Big Thompson River flood of 1976 was overestimated by 76%. Reasons for discrepancy in reconstructed peaks could include (1) the possibility that floods may have been able to move boulders larger than those available to be moved; (2) overestimation of the slope-area discharge because high-water marks were set prior to erosion of the channel; (3) underestimation of original roughness coefficients; and (4) macroturbulent effects during fast, deep flows.
The paleohydraulic technique is applied to two other streams in Colorado with sedimentological evidence of large flash floods, but no conventional indirect discharge estimates. A small tributary to the Big Thompson River draining 1.8 km2 has a paleohydraulic reconstructed flood peak of about 60 m3/s from a flood in 1976. Using boulders excavated from a foundation site in Holocene alluvium along Boulder Creek in Boulder, Colorado, a paleohydraulic reconstructed flood peak of between 860 and 1,512 m3/s is calculated. This is 1.4 to 2.4 times the magnitude of the estimated 500-yr flood.
A kinetic, first-order mass transfer model was used to describe the sorption of strontium onto sand- and gravel-sized streambed sediments. Rate parameters, empirically determined for strontium, allowed for the prediction of potassium sorption with moderate success. The model parameters varied significantly with particle size. The sorption data were collected during an experimental injection of several elements into a small mountain pool-and-riffle stream. The sorption process onto sand- and gravel-sized sediment was relatively slow compared to changes in the dissolved concentrations.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR019i003p00725","usgsCitation":"Bencala, K.E., Jackman, A.P., Kennedy, V.C., Avanzino, R.J., and Zellweger, G.W., 1983, Kinetic analysis of strontium and potassium sorption onto sands and gravels in a natural channel: Water Resources Research, v. 19, no. 3, p. 725-731, https://doi.org/10.1029/WR019i003p00725.","productDescription":"7 p.","startPage":"725","endPage":"731","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505a40a3e4b0c8380cd64f07","contributors":{"authors":[{"text":"Bencala, Kenneth E. kbencala@usgs.gov","contributorId":1541,"corporation":false,"usgs":true,"family":"Bencala","given":"Kenneth","email":"kbencala@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":360671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jackman, Alan P.","contributorId":28239,"corporation":false,"usgs":true,"family":"Jackman","given":"Alan","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":360669,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kennedy, Vance C.","contributorId":102063,"corporation":false,"usgs":true,"family":"Kennedy","given":"Vance","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":360668,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Avanzino, Ronald J.","contributorId":24355,"corporation":false,"usgs":true,"family":"Avanzino","given":"Ronald","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":360667,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zellweger, Gary W.","contributorId":71171,"corporation":false,"usgs":true,"family":"Zellweger","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":360670,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70011250,"text":"70011250 - 1983 - The nature of carbon dioxide waters in Snaefellsnes, western Iceland","interactions":[],"lastModifiedDate":"2024-04-19T18:38:31.995449","indexId":"70011250","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1828,"text":"Geothermics","active":true,"publicationSubtype":{"id":10}},"title":"The nature of carbon dioxide waters in Snaefellsnes, western Iceland","docAbstract":"Over 20 occurrences of thermal and non-thermal waters rich in carbon dioxide are known in the Snaefellsnes Peninsula of western Iceland. On the basis of the thermal, chemical and isotopic characteristics of these waters, and hydrological considerations, it is concluded that they represent meteoric waters which have seeped to variable depths into the bedrock. Ascending carbon dioxide gas originating from intrusions or the mantle mixes with the meteoric waters to produce carbon dioxide waters: at considerable depth in the case of the thermal carbon dioxide waters but close to the surface in the case of cold carbon dioxide waters. The occurrence of carbon dioxide waters cannot be regarded as evidence for underground geothermal reservoirs.
","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6505(83)90027-5","issn":"03756505","usgsCitation":"Arnorsson, S., and Barnes, I., 1983, The nature of carbon dioxide waters in Snaefellsnes, western Iceland: Geothermics, v. 12, no. 2-3, p. 171-176, https://doi.org/10.1016/0375-6505(83)90027-5.","productDescription":"6 p.","startPage":"171","endPage":"176","numberOfPages":"6","costCenters":[],"links":[{"id":221652,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Iceland","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -25.048828125,\n 63.11463763252091\n ],\n [\n -12.919921874999998,\n 63.11463763252091\n ],\n [\n -12.919921874999998,\n 66.8265202749748\n ],\n [\n -25.048828125,\n 66.8265202749748\n ],\n [\n -25.048828125,\n 63.11463763252091\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"12","issue":"2-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae03e4b08c986b323eb6","contributors":{"authors":[{"text":"Arnorsson, S.","contributorId":96828,"corporation":false,"usgs":true,"family":"Arnorsson","given":"S.","email":"","affiliations":[],"preferred":false,"id":360662,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, I.","contributorId":23678,"corporation":false,"usgs":true,"family":"Barnes","given":"I.","affiliations":[],"preferred":false,"id":360661,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1003836,"text":"1003836 - 1983 - Waterbird mortality from botulism type E in Lake Michigan: An update","interactions":[],"lastModifiedDate":"2023-09-23T02:25:24.804502","indexId":"1003836","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"Waterbird mortality from botulism type E in Lake Michigan: An update","docAbstract":"Three outbreaks of botulism type E occurring in waterbirds on Lake Michigan since autumn 1976 are discussed. Natural ingestion of food containing type E toxin by Ring-billed Gulls (Larus delawarensis) and the presence of type E toxin in blood from moribund gulls were demonstrated. Concurrent presence of type C and type E botulinal toxins was found in a die-off of Common Loons (Gavia immer). In combination with previous reported outbreaks, these incidents suggest that this disease is geographically widespread in Lake Michigan, and that environmental conditions conducive to type E botulinal toxin production and consumption occur in both summer and autumn.
","language":"English","publisher":"Wilson Ornithological Society","usgsCitation":"Brand, C.J., Duncan, R.M., Garrow, S.P., Olson, D., and Schumann, L.E., 1983, Waterbird mortality from botulism type E in Lake Michigan: An update: The Wilson Bulletin, v. 95, no. 2, p. 269-275.","productDescription":"7 p.","startPage":"269","endPage":"275","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":409588,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://sora.unm.edu/node/130032","linkFileType":{"id":5,"text":"html"}},{"id":134127,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Lake Michigan","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.4072265625,\n 41.4509614012039\n ],\n [\n -86.37451171875,\n 41.4509614012039\n ],\n [\n -85.836181640625,\n 42.601619944327965\n ],\n [\n -86.06689453125,\n 43.70759350405294\n ],\n [\n -85.968017578125,\n 44.5826428195842\n ],\n [\n -85.36376953125,\n 44.69989765840318\n ],\n [\n -85.1220703125,\n 45.236217535866025\n ],\n [\n -84.66064453125,\n 45.336701909968106\n ],\n [\n -84.57275390625,\n 46.14939437647686\n ],\n [\n -85.462646484375,\n 46.240651955001695\n ],\n [\n -85.74829101562499,\n 46.08847179577592\n ],\n [\n -86.37451171875,\n 46.042735653846506\n ],\n [\n -87.0556640625,\n 45.96642454131025\n ],\n [\n -87.791748046875,\n 45.46783598133375\n ],\n [\n -88.154296875,\n 44.59829048984011\n ],\n [\n -88.209228515625,\n 44.36313311380771\n ],\n [\n -87.857666015625,\n 44.12702800650004\n ],\n [\n -87.923583984375,\n 43.57243174740972\n ],\n [\n -88.187255859375,\n 43.100982876188546\n ],\n [\n -88.187255859375,\n 42.58544425738491\n ],\n [\n -88.13232421875,\n 41.95949009892465\n ],\n [\n -87.4072265625,\n 41.4509614012039\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"95","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c58","contributors":{"authors":[{"text":"Brand, Christopher J. cbrand@usgs.gov","contributorId":1186,"corporation":false,"usgs":true,"family":"Brand","given":"Christopher","email":"cbrand@usgs.gov","middleInitial":"J.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":314420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duncan, Ruth M.","contributorId":84720,"corporation":false,"usgs":true,"family":"Duncan","given":"Ruth","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":314423,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Garrow, Scott P.","contributorId":44513,"corporation":false,"usgs":false,"family":"Garrow","given":"Scott","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":314422,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Olson, Dan","contributorId":91010,"corporation":false,"usgs":false,"family":"Olson","given":"Dan","email":"","affiliations":[],"preferred":false,"id":314424,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schumann, Leonard E.","contributorId":27413,"corporation":false,"usgs":false,"family":"Schumann","given":"Leonard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":314421,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":47673,"text":"wri811182 - 1983 - Historical changes to Lake Washington and route of the Lake Washington Ship Canal, King County, Washington","interactions":[],"lastModifiedDate":"2022-08-29T13:55:24.290547","indexId":"wri811182","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-1182","title":"Historical changes to Lake Washington and route of the Lake Washington Ship Canal, King County, Washington","docAbstract":"Lake Washington, in the midst of the greater Seattle metropolitan area of the Puget Sound region (fig. 1), is an exceptional commercial, recreational, and esthetic resource for the region . In the past 130 years, Lake Washington has been changed from a \" wild \" lake in a wilderness setting to a regulated lake surrounded by a growing metropolis--a transformation that provides an unusual opportunity to study changes to a lake's shoreline and hydrologic characteristics -resulting from urbanization.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri811182","usgsCitation":"Chrzastowski, M.J., 1983, Historical changes to Lake Washington and route of the Lake Washington Ship Canal, King County, Washington: U.S. Geological Survey Water-Resources Investigations Report 81-1182, Report: 9 p.; Plate: 33.53 x 57.12 inches, https://doi.org/10.3133/wri811182.","productDescription":"Report: 9 p.; Plate: 33.53 x 57.12 inches","numberOfPages":"9","costCenters":[],"links":[{"id":162048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr811182.jpg"},{"id":405790,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1182/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405789,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1182/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","county":"King County","otherGeospatial":"Lake Washington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.46871948242186,\n 47.30903424774781\n ],\n [\n -122.46871948242186,\n 47.96510025611191\n ],\n [\n -121.40991210937499,\n 47.96510025611191\n ],\n [\n -121.40991210937499,\n 47.30903424774781\n ],\n [\n -122.46871948242186,\n 47.30903424774781\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6885d4","contributors":{"authors":[{"text":"Chrzastowski, Michael J.","contributorId":28643,"corporation":false,"usgs":true,"family":"Chrzastowski","given":"Michael","email":"","middleInitial":"J.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":235985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70184255,"text":"70184255 - 1983 - Detection of infectious hematopoietic necrosis virus in river water and demonstration of waterborne transmission","interactions":[],"lastModifiedDate":"2017-03-06T09:59:58","indexId":"70184255","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2286,"text":"Journal of Fish Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Detection of infectious hematopoietic necrosis virus in river water and demonstration of waterborne transmission","docAbstract":"In a study of the possible role of waterborne infectious haematopoietic necrosis virus in transmission of the disease among spawning sockeye salmon, Oncorhynchus nerka (Walbaum), both infection rates and virus titres were higher in fish held at high density in a side channel than in fish in the adjacent river. Virus was never isolated from river water, but was found in water from the side channel at levels ranging from 32.5 to 1600 plaque-forming units (p.f.u.)/ml. Uninfected yearling sockeye salmon held in a box in the side channel developed localized gill infections with IHN virus. The disease did not progress to the viscera until a threshold titre of about 105 p.f.u./g was reached in the gill. The effectiveness of the gill as a barrier limiting development of systemic infections means that waterborne IHN virus probably does not greatly increase the infection rate in a sockeye salmon population during spawning.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2761.1983.tb00083.x","usgsCitation":"Mulcahy, D.M., Pascho, R.J., and Jenes, C., 1983, Detection of infectious hematopoietic necrosis virus in river water and demonstration of waterborne transmission: Journal of Fish Diseases, v. 6, no. 4, p. 321-330, https://doi.org/10.1111/j.1365-2761.1983.tb00083.x.","productDescription":"10","startPage":"321","endPage":"330","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":336847,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Cedar River","volume":"6","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-04-07","publicationStatus":"PW","scienceBaseUri":"58be8350e4b014cc3a3a9a53","contributors":{"authors":[{"text":"Mulcahy, Daniel M. dmulcahy@usgs.gov","contributorId":3102,"corporation":false,"usgs":true,"family":"Mulcahy","given":"Daniel","email":"dmulcahy@usgs.gov","middleInitial":"M.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":680752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pascho, Ronald J.","contributorId":177070,"corporation":false,"usgs":false,"family":"Pascho","given":"Ronald","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":680753,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jenes, C.K.","contributorId":152262,"corporation":false,"usgs":false,"family":"Jenes","given":"C.K.","email":"","affiliations":[],"preferred":false,"id":680754,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1000337,"text":"1000337 - 1983 - Rediscovery of lake balls in Lake Michigan","interactions":[],"lastModifiedDate":"2016-03-31T15:04:12","indexId":"1000337","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2299,"text":"Journal of Freshwater Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Rediscovery of lake balls in Lake Michigan","docAbstract":"For the first time in 70 years, the occurrence of a 'lake ball' in Lake Michigan is here reported in the literature. According to a published system of classification, the object we collected in 1978 was a 'false' lake ball. Dissection revealed that it was colonized by 5 chironomid larvae and 162 oligochaetes. The species and numerical proportions of the oligochaetes indicated that it was formed in or near the mouth of a eutrophic tributary rather than in the open waters of Lake Michigan where it was found. Because of their mobility, false lake balls may be ecologically important, serving as natural vehicles for the dispersal of invertebrates.
","language":"English","publisher":"Elsevier","doi":"10.1080/02705060.1983.9664588","usgsCitation":"Schloesser, D.W., Hiltunen, J.K., and Owens, R.W., 1983, Rediscovery of lake balls in Lake Michigan: Journal of Freshwater Ecology, v. 2, no. 2, p. 159-163, https://doi.org/10.1080/02705060.1983.9664588.","productDescription":"5 p.","startPage":"159","endPage":"163","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-01-07","publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6352c5","contributors":{"authors":[{"text":"Schloesser, Donald W. dschloesser@usgs.gov","contributorId":3579,"corporation":false,"usgs":true,"family":"Schloesser","given":"Donald","email":"dschloesser@usgs.gov","middleInitial":"W.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":308413,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hiltunen, Jarl K.","contributorId":27820,"corporation":false,"usgs":true,"family":"Hiltunen","given":"Jarl","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":308415,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Owens, Randall W.","contributorId":23871,"corporation":false,"usgs":true,"family":"Owens","given":"Randall","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":308414,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10046,"text":"ofr83216 - 1983 - Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","interactions":[{"subject":{"id":10046,"text":"ofr83216 - 1983 - Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","indexId":"ofr83216","publicationYear":"1983","noYear":false,"title":"Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":38571,"text":"pp1307 - 1984 - Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","indexId":"pp1307","publicationYear":"1984","noYear":false,"title":"Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado"},"id":1}],"supersededBy":{"id":38571,"text":"pp1307 - 1984 - Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","indexId":"pp1307","publicationYear":"1984","noYear":false,"title":"Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado"},"lastModifiedDate":"2023-07-14T15:19:32.387946","indexId":"ofr83216","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-216","title":"Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","docAbstract":"No abstract available.
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Sea","interactions":[],"lastModifiedDate":"2018-05-20T11:33:37","indexId":"70180857","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":894,"text":"Arctic","active":true,"publicationSubtype":{"id":10}},"title":"Use of nearshore and estuarine areas by gray whales (Eschrichtius robustus) in the eastern Bering Sea","docAbstract":"During spring aerial surveys of the coast of the southeastern Bering Sea significant numbers of gray whales were seen in nearshore waters along the north side of the Alaska Peninsula. Many (50-80%) of these animals were observed surfacing with mud trails or lying on their sides, characteristics both associated with feeding. A migration route close to shore (within 1-2 km) was used until whales neared Egegik Bay, where they began to head west 5-8 km offshore, across northern Bristol Bay. Smaller numbers of gray whales were present throughout summer in nearshore waters and estuaries along the north side of the Alaska Peninsula. At Nelson Lagoon gray whales normally used the lagoon in spring, were absent during early summer, returned in mid-summer, and then were present until late November when they departed for the wintering grounds. Gray whales were present in the lagoon most often during periods of peak tidal flow; those that appeared to be feeding were oriented into the current. Three behaviors that appeared to be associated with feeding were observed: side-feeding from a stationary position within shallow waters of lagoon channels, diving within the lagoon and in nearshore waters, and elliptical side-feeding in the surf zone along the outer coast. Large crustaceans of the genus Crangon were available to and probably eaten by gray whales at Nelson Lagoon.
","language":"English","publisher":"Arctic Institute of North America","publisherLocation":"Calgary, AB","doi":"10.14430/arctic2276","usgsCitation":"Gill, R., and Hall, J.D., 1983, Use of nearshore and estuarine areas by gray whales (Eschrichtius robustus) in the eastern Bering Sea: Arctic, v. 36, no. 3, p. 275-281, https://doi.org/10.14430/arctic2276.","productDescription":"7 p.","startPage":"275","endPage":"281","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"links":[{"id":480225,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.14430/arctic2276","text":"Publisher Index Page"},{"id":334784,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -167.03613281249997,\n 54.08517342088679\n ],\n [\n -167.03613281249997,\n 59.80063426102869\n ],\n [\n -154.3359375,\n 59.80063426102869\n ],\n [\n -154.3359375,\n 54.08517342088679\n ],\n [\n -167.03613281249997,\n 54.08517342088679\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"36","issue":"3","noUsgsAuthors":false,"publicationDate":"1983-01-01","publicationStatus":"PW","scienceBaseUri":"589847abe4b0efcedb7072e5","contributors":{"authors":[{"text":"Gill, Robert E. Jr. 0000-0002-6385-4500 rgill@usgs.gov","orcid":"https://orcid.org/0000-0002-6385-4500","contributorId":171747,"corporation":false,"usgs":true,"family":"Gill","given":"Robert E.","suffix":"Jr.","email":"rgill@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":662612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hall, John D. 0000-0002-7670-5459","orcid":"https://orcid.org/0000-0002-7670-5459","contributorId":179094,"corporation":false,"usgs":false,"family":"Hall","given":"John","email":"","middleInitial":"D.","affiliations":[{"id":28155,"text":"Century Engineering, Anchorage, AK","active":true,"usgs":false}],"preferred":false,"id":662613,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27782,"text":"wri834192 - 1983 - Measurement of the reaeration coefficients of the North Fork Licking River at Utica, Ohio by radioactive tracers","interactions":[],"lastModifiedDate":"2023-03-29T21:16:33.711699","indexId":"wri834192","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4192","title":"Measurement of the reaeration coefficients of the North Fork Licking River at Utica, Ohio by radioactive tracers","docAbstract":"Reaeration coefficients of the North Fork Licking River at Utica, Ohio were measured by the radioactive-tracer method. The tests were conducted on a 2.1-mile reach on September 23 and October 7, 1981, during low-flow conditions. Krypton-85 gas and tritium were the radioopactive tracers, which were used in conjunction with rhodamine-WT dye.
The reaertion coefficients determined on September 23 were 3.09 days-1 (subreach 1-2) and 3.32 days-1 (subreach 2-3). On October 7, the values were 2.04 days-1 and 2.23 days-1 respectively.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834192","usgsCitation":"Hren, J., 1983, Measurement of the reaeration coefficients of the North Fork Licking River at Utica, Ohio by radioactive tracers: U.S. Geological Survey Water-Resources Investigations Report 83-4192, iv, 19 p., https://doi.org/10.3133/wri834192.","productDescription":"iv, 19 p.","costCenters":[],"links":[{"id":56625,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4192/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414929,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35841.htm","linkFileType":{"id":5,"text":"html"}},{"id":118726,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4192/report-thumb.jpg"}],"country":"United States","state":"Ohio","city":"Utica","otherGeospatial":"North Fork Licking River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.458,\n 40.242\n ],\n [\n -82.458,\n 40.208\n ],\n [\n -82.435,\n 40.208\n ],\n [\n -82.435,\n 40.242\n ],\n [\n -82.458,\n 40.242\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611210","contributors":{"authors":[{"text":"Hren, Janet","contributorId":69554,"corporation":false,"usgs":true,"family":"Hren","given":"Janet","email":"","affiliations":[],"preferred":false,"id":198678,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28427,"text":"wri834220 - 1983 - A method for estimating ground-water return flow to the lower Colorado River in the Yuma area, Arizona and California","interactions":[],"lastModifiedDate":"2023-04-06T18:31:52.318608","indexId":"wri834220","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4220","title":"A method for estimating ground-water return flow to the lower Colorado River in the Yuma area, Arizona and California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834220","usgsCitation":"Loeltz, O.J., and Leake, S.A., 1983, A method for estimating ground-water return flow to the lower Colorado River in the Yuma area, Arizona and California: U.S. Geological Survey Water-Resources Investigations Report 83-4220, ix, 86 p., https://doi.org/10.3133/wri834220.","productDescription":"ix, 86 p.","costCenters":[],"links":[{"id":57230,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4220/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119024,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4220/report-thumb.jpg"},{"id":415364,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35861.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona, California","city":"Yuma","otherGeospatial":"lower Colorado River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -114.731,\n 32.886\n ],\n [\n -114.731,\n 32.699\n ],\n [\n -114.429,\n 32.699\n ],\n [\n -114.429,\n 32.886\n ],\n [\n -114.731,\n 32.886\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae136","contributors":{"authors":[{"text":"Loeltz, Omar J.","contributorId":86312,"corporation":false,"usgs":true,"family":"Loeltz","given":"Omar","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":199777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leake, S. A.","contributorId":52164,"corporation":false,"usgs":true,"family":"Leake","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199776,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42071,"text":"ofr83137 - 1983 - Altitude of the top of the Matawan Group-Magothy Formation, Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2023-03-01T21:30:31.255374","indexId":"ofr83137","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-137","title":"Altitude of the top of the Matawan Group-Magothy Formation, Suffolk County, Long Island, New York","docAbstract":"The Magothy aquifer, with its irregular surface and deeply eroded buried valleys, has become the major source of fresh water in most of Suffolk Country. With the availability of recent data from deep wells and test holes, refinement of the surface-altitude contours has been possible and resulted in substantial revision in some areas. This 1-sheet map delineates the surface altitude of the Magothy aquifer (Matawan Group-Magothy Formation) and includes a brief text and bibliography.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83137","usgsCitation":"Krulikas, R.K., Koszalka, E., and Doriski, T.P., 1983, Altitude of the top of the Matawan Group-Magothy Formation, Suffolk County, Long Island, New York: U.S. Geological Survey Open-File Report 83-137, 1 Plate: 47.05 x 25.51 inches, https://doi.org/10.3133/ofr83137.","productDescription":"1 Plate: 47.05 x 25.51 inches","costCenters":[],"links":[{"id":135569,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79820,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0137/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413560,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13907.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New York","county":"Suffolk County","otherGeospatial":"Long Island, Matawan Group-Magothy Formation","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -73.5,\n 41.167\n ],\n [\n -73.5,\n 40.6\n ],\n [\n -71.917,\n 40.6\n ],\n [\n -71.917,\n 41.167\n ],\n [\n -73.5,\n 41.167\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686a7b","contributors":{"authors":[{"text":"Krulikas, Richard K.","contributorId":36910,"corporation":false,"usgs":true,"family":"Krulikas","given":"Richard","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":225905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koszalka, E. J.","contributorId":28949,"corporation":false,"usgs":true,"family":"Koszalka","given":"E. J.","affiliations":[],"preferred":false,"id":225904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doriski, Thomas P.","contributorId":20301,"corporation":false,"usgs":true,"family":"Doriski","given":"Thomas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":225903,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26859,"text":"wri834094 - 1983 - Impact of changes in land use on the ground-water system in the Sequim-Dungeness Peninsula, Clallam County, Washington","interactions":[],"lastModifiedDate":"2023-03-14T20:43:18.101534","indexId":"wri834094","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4094","title":"Impact of changes in land use on the ground-water system in the Sequim-Dungeness Peninsula, Clallam County, Washington","docAbstract":"A digital-computer model was developed to simulate three-dimensional ground-water flow in aquifers underlying the Sequim-Dungeness peninsula, Clallam County, Washington. Analysis using the model shows that leakage from irrigation ditches is the area 's most important source of ground-water recharge. Termination of the irrigation system would lead to lower heads throughout the ground-water system. After 10-20 years of no irrigation, the water-table aquifer would have average drawdowns of about 20 feet and some areas would become completely unsaturated. Several hundred wells could be in danger of going dry. If irrigation were terminated, leakage from the Dungeness River would become the major source of ground-water recharge. As of June 1980, ground-water quality has apparently not been affected in the study area by the use of on-site domestic sewage-disposal systems. The median nitrate-plus-nitrite (as N) concentration in the water-table aquifer was 0.25 milligrams per liter, and the maximum concentration was 2.5 milligrams per liter.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834094","usgsCitation":"Drost, B., 1983, Impact of changes in land use on the ground-water system in the Sequim-Dungeness Peninsula, Clallam County, Washington: U.S. Geological Survey Water-Resources Investigations Report 83-4094, viii, 69 p., https://doi.org/10.3133/wri834094.","productDescription":"viii, 69 p.","costCenters":[],"links":[{"id":414134,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35720.htm","linkFileType":{"id":5,"text":"html"}},{"id":55747,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4094/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123302,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4094/report-thumb.jpg"}],"country":"United States","state":"Washington","county":"Clallam County","otherGeospatial":"Sequim-Dungeness Peninsula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -123.267,\n 48.167\n ],\n [\n -123.267,\n 48.043\n ],\n [\n -123.033,\n 48.043\n ],\n [\n -123.033,\n 48.167\n ],\n [\n -123.267,\n 48.167\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4ac","contributors":{"authors":[{"text":"Drost, B. W.","contributorId":38526,"corporation":false,"usgs":true,"family":"Drost","given":"B. W.","affiliations":[],"preferred":false,"id":197136,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1016548,"text":"1016548 - 1983 - [Book review] Ducks, geese and swans of North America","interactions":[],"lastModifiedDate":"2017-05-16T10:40:32","indexId":"1016548","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"[Book review] Ducks, geese and swans of North America","docAbstract":"This is the 3rd edition of the classic work \"The Ducks, Geese and Swans of North America,\" which was first published in December 1942. The original edition was authored by Francis C. Kortright with color plates by T. M. Shortt. An authoritative reference on North American waterfowl for many years, the book had become outdated as a result of major advances in the field of waterfowl biology. The need to update the 1st edition culminated in the publication in 1976 of a 2nd edition authored by Frank Bellrose. Readers interested in comparing features of the 1976 edition with other major recent works on North American waterfowl by P. A. Johnsgard and R. S. Palmer should read Weller (1977, Auk 94: 173).
","language":"English","publisher":"American Ornithological Society","usgsCitation":"Krapu, G.L., 1983, [Book review] Ducks, geese and swans of North America: The Auk, v. 100, no. 1, p. 246-248.","productDescription":"3 p.","startPage":"246","endPage":"248","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":132503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":262274,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/4086319","linkFileType":{"id":5,"text":"html"}}],"volume":"100","issue":"1","publicComments":"A review of: Ducks, geese and swans of North America. Frank C. Bellrose. 1980. Harrisburg, Pennsylvania, Stackpole Books. A Wildlife Management Institute book sponsored jointly with the Illinois Natural History Survey. 540 pp., 55 maps, 24 color plates, 57 figures, 1 black-and-white photo, numerous drawings.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62ff13","contributors":{"authors":[{"text":"Krapu, Gary L. 0000-0001-8482-6130 gkrapu@usgs.gov","orcid":"https://orcid.org/0000-0001-8482-6130","contributorId":3074,"corporation":false,"usgs":true,"family":"Krapu","given":"Gary","email":"gkrapu@usgs.gov","middleInitial":"L.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":324364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014368,"text":"1014368 - 1983 - Use of surface water for rearing channel catfish in ponds","interactions":[],"lastModifiedDate":"2025-08-06T15:52:30.192193","indexId":"1014368","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Use of surface water for rearing channel catfish in ponds","docAbstract":"No abstract available.
","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8659(1983)45[179:UOSWFR]2.0.CO;2","usgsCitation":"Tackett, D.L., and Carter, R.R., 1983, Use of surface water for rearing channel catfish in ponds: Progressive Fish-Culturist, v. 45, no. 3, p. 179-180, https://doi.org/10.1577/1548-8659(1983)45[179:UOSWFR]2.0.CO;2.","productDescription":"2 p.","startPage":"179","endPage":"180","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129167,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685761","contributors":{"authors":[{"text":"Tackett, Dewey L.","contributorId":8024,"corporation":false,"usgs":true,"family":"Tackett","given":"Dewey","middleInitial":"L.","affiliations":[],"preferred":false,"id":320260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carter, Ray R.","contributorId":36879,"corporation":false,"usgs":true,"family":"Carter","given":"Ray","middleInitial":"R.","affiliations":[],"preferred":false,"id":320261,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1013656,"text":"1013656 - 1983 - Effects of hydrilla and grass carp on water quality in a Florida lake","interactions":[],"lastModifiedDate":"2013-02-19T14:48:58","indexId":"1013656","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"Effects of hydrilla and grass carp on water quality in a Florida lake","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Resources Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Water Resources Association","doi":"10.1111/j.1752-1688.1983.tb02801.x","collaboration":"None/GV","usgsCitation":"Canfield, D., Maceina, M., and Shireman, J., 1983, Effects of hydrilla and grass carp on water quality in a Florida lake: Water Resources Bulletin, v. 19, no. 5, p. 773-778, https://doi.org/10.1111/j.1752-1688.1983.tb02801.x.","productDescription":"p. 773-778","startPage":"773","endPage":"778","numberOfPages":"6","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":267767,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.1983.tb02801.x"},{"id":130226,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"5","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611e9b","contributors":{"authors":[{"text":"Canfield, D.E. Jr.","contributorId":57798,"corporation":false,"usgs":true,"family":"Canfield","given":"D.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":318982,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maceina, M.J.","contributorId":38934,"corporation":false,"usgs":true,"family":"Maceina","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":318981,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shireman, J.V.","contributorId":36083,"corporation":false,"usgs":true,"family":"Shireman","given":"J.V.","email":"","affiliations":[],"preferred":false,"id":318980,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1000548,"text":"1000548 - 1983 - Distribution and abundance of larval fish in the nearshore waters of western Lake Huron","interactions":[],"lastModifiedDate":"2016-03-31T15:22:32","indexId":"1000548","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Distribution and abundance of larval fish in the nearshore waters of western Lake Huron","docAbstract":"Ichthyoplankton was collected at 17 nearshore (bottom depth ≥5 m but ≤10 m) sites in western Lake Huron during 1973–75 with a 0.5-m net of 351-micron mesh towed at 99 m/min. Larvae of rainbow smelt (Osmerus mordax) dominated late spring and early summer catches and larvae of alewives (Alosa pseudoharengus) the midsummer catches. Larval yellow perch (Perca flavescens) were caught in early summer but were rarely the dominant species. The time of spawning and hatching, and thus occurrence of larvae, differed between areas but was less variable for alewives than for yellow perch. The appearance of larvae in Saginaw Bay was followed successively by their appearance in southern, central, and northern Lake Huron. Rainbow smelt were most abundant in northern Lake Huron and yellow perch and alewives in inner Saginaw Bay. Densities of either rainbow smelt or alewives occasionally exceeded 1/m3, whereas those of yellow perch never exceeded 0.1/m3. Abundance of alewives was usually highest 1 to 3 m beneath the surface and that of rainbow smelt 2 to at least 6 m beneath the surface. Important nursery areas of rainbow smelt were in bays and off irregular coastlines and those of yellow perch were in bays. All nearshore waters seemed equally important as nursery areas of alewives.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(83)71867-8","usgsCitation":"O’Gorman, R., 1983, Distribution and abundance of larval fish in the nearshore waters of western Lake Huron: Journal of Great Lakes Research, v. 9, no. 1, p. 14-22, https://doi.org/10.1016/S0380-1330(83)71867-8.","productDescription":"9 p.","startPage":"14","endPage":"22","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a171","contributors":{"authors":[{"text":"O’Gorman, Robert rogorman@usgs.gov","contributorId":3451,"corporation":false,"usgs":true,"family":"O’Gorman","given":"Robert","email":"rogorman@usgs.gov","affiliations":[],"preferred":true,"id":308744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}