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":70011417,"text":"70011417 - 1983 - Simulation of solute transport in a mountain pool-and-riffle stream: A transient storage model","interactions":[],"lastModifiedDate":"2018-02-07T13:43:16","indexId":"70011417","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":"Simulation of solute transport in a mountain pool-and-riffle stream: A transient storage model","docAbstract":"The physical characteristics of mountain streams differ from the uniform and conceptually well- defined open channels for which the analysis of solute transport has been oriented in the past and is now well understood. These physical conditions significantly influence solute transport behavior, as demonstrated by a transient storage model simulation of solute transport in a very small (0.0125 m3s−1) mountain pool-and-riffle stream. The application is to a carefully controlled and intensively monitored chloride injection experiment. The data from the experiment are not explained by the standard convection-dispersion mechanisms alone. A transient storage model, which couples dead zones with the one-dimensional convection-dispersion equation, simulates the general characteristics of the solute transport behavior and a set of simulation parameters were determined that yield an adequate fit to the data. However, considerable uncertainty remains in determining physically realistic values of these parameters. The values of the simulation parameters used are compared to values used by other authors for other streams. The comparison supports, at least qualitatively, the determined parameter values.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR019i003p00718","usgsCitation":"Bencala, K.E., and Walters, R.A., 1983, Simulation of solute transport in a mountain pool-and-riffle stream: A transient storage model: Water Resources Research, v. 19, no. 3, p. 718-724, https://doi.org/10.1029/WR019i003p00718.","productDescription":"7 p.","startPage":"718","endPage":"724","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220904,"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":"505b9084e4b08c986b319558","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":361036,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walters, Roy A.","contributorId":74877,"corporation":false,"usgs":true,"family":"Walters","given":"Roy","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":361035,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011386,"text":"70011386 - 1983 - Ground-water models for water resource planning","interactions":[],"lastModifiedDate":"2012-03-12T17:19:10","indexId":"70011386","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1746,"text":"GeoJournal","active":true,"publicationSubtype":{"id":10}},"title":"Ground-water models for water resource planning","docAbstract":"In the past decade hydrogeologists have emphasized the development of computer-based mathematical models to aid in the understanding of flow, the transport of solutes, transport of heat, and deformation in the ground-water system. These models have been used to provide information and predictions for water managers. Too frequently, ground-water was neglected in water resource planning because managers believed that it could not be adequately evaluated in terms of availability, quality, and effect of development on surface-water supplies. Now, however, with newly developed digital ground-water models, effects of development can be predicted. Such models have been used to predict hydrologic and quality changes under different stresses. These models have grown in complexity over the last ten years from simple one-layer models to three-dimensional simulations of ground-water flow, which may include solute transport, heat transport, effects of land subsidence, and encroachment of saltwater. Case histories illustrate how predictive ground-water models have provided the information needed for the sound planning and management of water resources in the USA. ?? 1983 D. Reidel Publishing Company.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"GeoJournal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00194492","issn":"03432521","usgsCitation":"Moore, J., 1983, Ground-water models for water resource planning: GeoJournal, v. 7, no. 5, p. 453-458, https://doi.org/10.1007/BF00194492.","startPage":"453","endPage":"458","numberOfPages":"6","costCenters":[],"links":[{"id":205128,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00194492"},{"id":221582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2c91e4b0c8380cd5bd02","contributors":{"authors":[{"text":"Moore, J.E.","contributorId":34927,"corporation":false,"usgs":true,"family":"Moore","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":360980,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011376,"text":"70011376 - 1983 - Requirements for modeling trace metal partitioning in oxidized estuarine sediments","interactions":[],"lastModifiedDate":"2020-01-26T09:45:22","indexId":"70011376","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2662,"text":"Marine Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Requirements for modeling trace metal partitioning in oxidized estuarine sediments","docAbstract":"The fate of particulate-bound metals is of particular importance in estuaries because major biological energy flows involve consumption of detrital particles. The biological impact of particulate-bound metals is strongly influenced by the partitioning of metals among sediment components at the oxidized sediment-water interface. Adequate methods for directly measuring this partitioning are not available, thus a modeling approach may be most useful. Important requirements for such a model include: (1) determinations of metal binding intensities which are comparable among sediment components important in oxidized sediments; (2) comparable determinations of the binding capacities of the several forms of each component; (3) operational determinations of the abundance in natural sediments of components of defined binding capacity; (4) assessments of the influence of particle coatings and multicomponent aggregation on the available binding capacity of each substrate; (5) consideration of the effect of Ca and Mg competition on binding to different components; and (6) determinations of the kinetics of metal redistribution among components in oxidized sediments.
","language":"English","publisher":"Elsevier","doi":"10.1016/0304-4203(83)90078-6","issn":"03044203","usgsCitation":"Luoma, S.N., and Davis, J., 1983, Requirements for modeling trace metal partitioning in oxidized estuarine sediments: Marine Chemistry, v. 12, no. 2-3, p. 159-181, https://doi.org/10.1016/0304-4203(83)90078-6.","productDescription":"23 p.","startPage":"159","endPage":"181","numberOfPages":"23","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"2-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa90ce4b0c8380cd85bc0","contributors":{"authors":[{"text":"Luoma, Samuel N. 0000-0001-5443-5091 snluoma@usgs.gov","orcid":"https://orcid.org/0000-0001-5443-5091","contributorId":2287,"corporation":false,"usgs":true,"family":"Luoma","given":"Samuel","email":"snluoma@usgs.gov","middleInitial":"N.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":780292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, J.A.","contributorId":71694,"corporation":false,"usgs":true,"family":"Davis","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":360955,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011340,"text":"70011340 - 1983 - Variable tolerance to copper in two species from San Francisco Bay","interactions":[],"lastModifiedDate":"2020-01-26T09:47:13","indexId":"70011340","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2664,"text":"Marine Environmental Research","active":true,"publicationSubtype":{"id":10}},"title":"Variable tolerance to copper in two species from San Francisco Bay","docAbstract":"In static toxicity experiments, tolerance to soluble Cu of the bivalve, Macoma balthica, and the copepod, Acartia clausi, varied substantially among populations sampled within San Francisco Bay. Intraspecific tolerance differed ten-fold or more for both species over relatively small distances, suggesting geographical isolation of populations is not a prerequisite for the development of intraspecific differences in tolerance by aquatic organisms.In static toxicity experiments, tolerance to soluble Cu of the bivalve, Macoma balthica, and the copepod, Acartia clausi, varied substantially among populations sampled within San Francisco Bay. Intraspecific tolerance differed ten-fold or more for both species over relatively small distances, suggesting geographical isolation of populations is not a prerequisite for the development of intraspecific differences in tolerance by aquatic organisms.
","language":"English","publisher":"Elsevier","doi":"10.1016/0141-1136(83)90002-8","issn":"01411136","usgsCitation":"Luoma, S.N., Cain, D., Ho, K., and Hutchinson, A., 1983, Variable tolerance to copper in two species from San Francisco Bay: Marine Environmental Research, v. 10, no. 4, p. 209-222, https://doi.org/10.1016/0141-1136(83)90002-8.","productDescription":"14 p.","startPage":"209","endPage":"222","numberOfPages":"14","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":220831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California ","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.37646484374999,\n 37.07271048132943\n ],\n [\n -121.728515625,\n 37.07271048132943\n ],\n [\n -121.728515625,\n 38.41055825094609\n ],\n [\n -123.37646484374999,\n 38.41055825094609\n ],\n [\n -123.37646484374999,\n 37.07271048132943\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc148e4b08c986b32a4ef","contributors":{"authors":[{"text":"Luoma, Samuel N. 0000-0001-5443-5091 snluoma@usgs.gov","orcid":"https://orcid.org/0000-0001-5443-5091","contributorId":2287,"corporation":false,"usgs":true,"family":"Luoma","given":"Samuel","email":"snluoma@usgs.gov","middleInitial":"N.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":780293,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cain, D.J.","contributorId":68329,"corporation":false,"usgs":true,"family":"Cain","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":360875,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ho, K.","contributorId":18509,"corporation":false,"usgs":true,"family":"Ho","given":"K.","email":"","affiliations":[],"preferred":false,"id":360874,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hutchinson, A.","contributorId":94035,"corporation":false,"usgs":true,"family":"Hutchinson","given":"A.","email":"","affiliations":[],"preferred":false,"id":360877,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70011335,"text":"70011335 - 1983 - Nonequilibrium models for predicting forms of precipitated manganese oxides","interactions":[],"lastModifiedDate":"2020-01-20T19:56:53","indexId":"70011335","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":"Nonequilibrium models for predicting forms of precipitated manganese oxides","docAbstract":"Manganese oxides precipitated by bubbling air through 0.01 molar solutions of MnCl2, Mn(NO3)2, MnSO4, or Mn(ClO4)2 at a constantly maintained pH of 8.5 to 9.5 at temperatures of 25°C or higher consisted mainly of hausmannite, Mn3O4. At temperatures near 0°C, but with other conditions the same, the product is feitknechtite, βMnOOH, except that if the initial solution is MnSO4 and the temperature is near 0°C the product is a mixture of manganite, γMnOOH and groutite, αMnOOH.
All these oxides are metastable in aerated solution and alter by irreversible processes to more highly oxidized species during aging. A two-step nonequilibrium thermodynamic model predicts that the least stable species, βMnOOH, should be most readily converted to MnO2. Some preparations of βMnOOH aged in their native solution at 5°C attained a manganese oxidation state of +3.3 or more after 7 months. Hausmannite aged at 25°C altered to γMnOOH. The latter is more stable than a or βMnOOH, and manganese oxidation states above 3.0 were not reached in hausmannite precipitates during 4 months of aging. Initial precipitation of MnCO3 rather than a form of oxide is likely only where oxygen availability is very low.
Composition of solutions and oxidation state and morphology of solids were determined during the aging process by chemical analyses, X-ray and electron diffraction and transmission electron micrographs.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(83)90219-3","issn":"00167037","usgsCitation":"Hem, J., and Lind, C.J., 1983, Nonequilibrium models for predicting forms of precipitated manganese oxides: Geochimica et Cosmochimica Acta, v. 47, no. 11, p. 2037-2046, https://doi.org/10.1016/0016-7037(83)90219-3.","productDescription":"10 p.","startPage":"2037","endPage":"2046","numberOfPages":"10","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a676fe4b0c8380cd73325","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":360861,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lind, Carol J.","contributorId":36110,"corporation":false,"usgs":true,"family":"Lind","given":"Carol","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":360860,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011332,"text":"70011332 - 1983 - Snow and ice in a changing hydrological world","interactions":[],"lastModifiedDate":"2024-01-22T16:20:10.42955","indexId":"70011332","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1927,"text":"Hydrological Sciences Journal","active":true,"publicationSubtype":{"id":10}},"title":"Snow and ice in a changing hydrological world","docAbstract":"On the occasion of the 60th anniversary of the International Association of Hydrological Sciences, the 100th and 50th anniversaries of the First and Second International Polar Years, and the 25th anniversary of the International Geophysical Year, it seems appropriate to re-examine the world's water balance and the role of snow and ice in the global hydrological climatic system. Snow cover on land (especially in the Northern Hemisphere) and sea ice (especially in the Southern Hemisphere) vary seasonally, and this seasonal change has an important effect on the world climate because snow and sea ice reflect solar radiation efficiently and affect other heat flow processes between atmosphere and land or ocean. Glaciers, including ice sheets, store most of the fresh water on Earth, but change dimensions relatively slowly. There is no clear evidence that the glacier ice volume currently is declining, but more needs to be known about mountain glacier and ice sheet mass balances. The current rise in sea level poses an enigma: thermal expansion of the oceans may account for half of the present rise, but the other half is unexplained. Although major changes in the large ice sheets take place over time scales of 104 to 105 years, marine ice sheets may be subject to rapid disintegration due to grounding line instability, perhaps accompanied by surging. Ice cores may produce remarkably complete histories of air temperature, precipitation, fallout, and atmospheric composition. A recent core through the Greenland Ice Sheet shows an abrupt transition from glacial to modern climate just over 10000 years ago, suggesting that climate is an “almost intransitive” system. Because of the possibility of abrupt climate transitions and the uncertain stability of the West Antarctic Ice Sheet, future climatic variations are difficult to predict. The calculated heating of the atmosphere in the polar regions due to CO2 increase is, therefore, of special interest.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626668309491140","usgsCitation":"Meier, M.F., 1983, Snow and ice in a changing hydrological world: Hydrological Sciences Journal, v. 28, no. 1, p. 3-22, https://doi.org/10.1080/02626668309491140.","productDescription":"20 p.","startPage":"3","endPage":"22","numberOfPages":"20","costCenters":[],"links":[{"id":480236,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626668309491140","text":"Publisher Index Page"},{"id":220700,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-12-24","publicationStatus":"PW","scienceBaseUri":"505b91b1e4b08c986b319a33","contributors":{"authors":[{"text":"Meier, M. F.","contributorId":98713,"corporation":false,"usgs":true,"family":"Meier","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":360856,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011326,"text":"70011326 - 1983 - Methanogenesis of phenolic compounds by a bacterial consortium from a contaminated aquifer in St. Louis Park, Minnesota","interactions":[],"lastModifiedDate":"2020-03-10T07:11:54","indexId":"70011326","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1103,"text":"Bulletin of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Methanogenesis of phenolic compounds by a bacterial consortium from a contaminated aquifer in St. Louis Park, Minnesota","docAbstract":"No abstract available.
","language":"English","publisher":"Springer","doi":"10.1007/BF01610131","issn":"00074861","usgsCitation":"Godsy, E., Goerlitz, D., and Ehrlich, G.G., 1983, Methanogenesis of phenolic compounds by a bacterial consortium from a contaminated aquifer in St. Louis Park, Minnesota: Bulletin of Environmental Contamination and Toxicology, v. 30, no. 1, p. 261-268, https://doi.org/10.1007/BF01610131.","productDescription":"8 p.","startPage":"261","endPage":"268","numberOfPages":"8","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205134,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01610131"}],"country":"United States","state":"Minnesota ","city":"St. Louis Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.4006118774414,\n 44.914249368747086\n ],\n [\n -93.29280853271484,\n 44.914249368747086\n ],\n [\n -93.29280853271484,\n 44.98519915760114\n ],\n [\n -93.4006118774414,\n 44.98519915760114\n ],\n [\n -93.4006118774414,\n 44.914249368747086\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"30","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5540e4b0c8380cd6d17e","contributors":{"authors":[{"text":"Godsy, E.M.","contributorId":56685,"corporation":false,"usgs":true,"family":"Godsy","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":360843,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goerlitz, D.F.","contributorId":8445,"corporation":false,"usgs":true,"family":"Goerlitz","given":"D.F.","affiliations":[],"preferred":false,"id":360842,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ehrlich, G. G.","contributorId":89126,"corporation":false,"usgs":true,"family":"Ehrlich","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":360844,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011314,"text":"70011314 - 1983 - Gas-film coefficients for streams","interactions":[],"lastModifiedDate":"2020-01-26T09:43:34","indexId":"70011314","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2255,"text":"Journal of Environmental Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Gas-film coefficients for streams","docAbstract":"Equations for predicting the gas-film coefficient for the volatilization of organic solutes from streams are developed. The film coefficient is a function of windspeed and water temperature. The dependence of the coefficient on windspeed is determined from published information on the evaporation of water from a canal. The dependence of the coefficient on temperature is determined from laboratory studies on the evaporation of water. Procedures for adjusting the coefficients for different organic solutes are based on the molecular diffusion coefficient and the molecular weight. The molecular weight procedure is easiest to use because of the availability of molecular weights. However, the theoretical basis of the procedure is questionable. The diffusion coefficient procedure is supported by considerable data. Questions, however, remain regarding the exact dependence of the film coefficint on the diffusion coefficient. It is suggested that the diffusion coefficient procedure with a 0.68-power dependence be used when precise estimate of the gas-film coefficient are needed and that the molecular weight procedure be used when only approximate estimates are needed.","language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0733-9372(1983)109:5(1111)","usgsCitation":"Rathbun, R.E., and Tai, D.Y., 1983, Gas-film coefficients for streams: Journal of Environmental Engineering, v. 109, no. 5, p. 1111-1127, https://doi.org/10.1061/(ASCE)0733-9372(1983)109:5(1111).","productDescription":"17 p.","startPage":"1111","endPage":"1127","numberOfPages":"17","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221518,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"109","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14dce4b0c8380cd54bd5","contributors":{"authors":[{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":360802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tai, D. Y.","contributorId":59778,"corporation":false,"usgs":true,"family":"Tai","given":"D.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":360801,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011297,"text":"70011297 - 1983 - Process and rate of dedolomitization: Mass transfer and C14 dating in a regional carbonate aquifer","interactions":[],"lastModifiedDate":"2024-01-03T12:27:00.499197","indexId":"70011297","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Process and rate of dedolomitization: Mass transfer and C14 dating in a regional carbonate aquifer","docAbstract":"Regional dedolomitization is the major process that controls the chemical character of water in the Mississippian Pahasapa Limestone (Madison equivalent) surrounding the Black Hills, South Dakota and Wyoming. The process of dedolomitization consists of dolomite dissolution and concurrent precipitation of calcite; it is driven by dissolution of gypsum.
Deuterium and oxygen isotopic data from the ground water, coupled with regional potentiometric maps, show that recharge occurs on the western slope of the Black Hills and that the water flows northward and westward toward the Powder River Basin. A significant part flows around the southern end of the Black Hills to replenish the aquifer to the east of the Hills. Depth of flow was inferred from interpretation of the silica geothermometer based on the temperature-dependent solubilities of quartz and chalcedony in water. Chemical effects of warm water in the Pahasapa Limestone include changes in the solubility products of minerals, conversion of gypsum to anhydrite, solution and precipitation of minerals, and increases in the tendency for outgassing of carbon dioxide. Where sulfate reduction is not important, sulfur isotope data show that (1) in the Mississippian aquifer, most of the sulfate is from dissolution of gypsum and (2) some wells and springs have a hydrologic connection with overlying Permian and Pennsylvanian evaporites. Sulfate ion concentration, a progress variable, shows a strong correlation with pH as a result of the combined effects of the dedolomitization reactions.
Mass-balance and mass-transfer calculations were used to adjust 14C values to determine a range of ground-water flow velocities between 2 and 20 m/yr. These velocities are characteristic of carbonate aquifers. The average rates of dolomite and gypsum dissolution are 1.7 × 10−4 and 3.4 × 10−4 mmol/kg of H2O/yr, respectively. The precipitation of calcite is occurring at the rate of 3.4 × 10−4 mmol/kg of H2O/yr. The close agreement among the model results demonstrates that dedolomitization is controlling water-rock interactions in this regional carbonate aquifer system.
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":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":70011198,"text":"70011198 - 1983 - Conjunctive use of groundwater and surface water for irrigated agriculture: Risk aversion","interactions":[],"lastModifiedDate":"2018-02-07T13:41:14","indexId":"70011198","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":"Conjunctive use of groundwater and surface water for irrigated agriculture: Risk aversion","docAbstract":"In examining the South Platte system in Colorado where surface water and groundwater are used conjunctively for irrigation, we find the actual installed well capacity is approximately sufficient to irrigate the entire area. This would appear to be an overinvestment in well capacity. In this paper we examine to what extent groundwater is being developed as insurance against periods of low streamflow. Using a simulation model which couples the hydrology of a conjunctive stream aquifer system to a behavioral-economic model which incorporates farmer behavior in such a system, we have investigated the economics of an area patterned after a reach of the South Platte Valley in Colorado. The results suggest that under current economic conditions the most reasonable groundwater pumping capacity is a total capacity capable of irrigating the available acreage with groundwater. Installing sufficient well capacity to irrigate all available acreage has two benefits: (1) this capacity maximizes the expected net benefits and (2) this capacity also minimizes the variation in annual income: it reduces the variance to essentially zero. As pumping capacity is installed in a conjunctive use system, the value of flow forecasts is diminished. Poor forecasts are compensated for by pumping groundwater.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR019i005p01111","usgsCitation":"Bredehoeft, J.D., and Young, R.A., 1983, Conjunctive use of groundwater and surface water for irrigated agriculture: Risk aversion: Water Resources Research, v. 19, no. 5, p. 1111-1121, https://doi.org/10.1029/WR019i005p01111.","productDescription":"11 p.","startPage":"1111","endPage":"1121","costCenters":[],"links":[{"id":221576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"South Platte River","volume":"19","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5059f9c7e4b0c8380cd4d794","contributors":{"authors":[{"text":"Bredehoeft, John D.","contributorId":86747,"corporation":false,"usgs":true,"family":"Bredehoeft","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":360516,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, Richard A.","contributorId":38975,"corporation":false,"usgs":true,"family":"Young","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360517,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011190,"text":"70011190 - 1983 - A reexamination of the effects of adsorbates on the Raman spectrum of gibbsite","interactions":[],"lastModifiedDate":"2020-01-27T06:54:29","indexId":"70011190","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3419,"text":"Soil Science","active":true,"publicationSubtype":{"id":10}},"title":"A reexamination of the effects of adsorbates on the Raman spectrum of gibbsite","docAbstract":"Previous workers have attributed substantial changes in the Raman intensities of the OH stretching bands in solid, powdered gibbsite of surface area 10 m2/g to surface interactions with the adsorbates 093Ca2+,HxPO43x- and SiO2.xH2O. These changes apparently resulted from an unsatisfactory Raman measurement procedure as a re-examination using an internal intensity standard (Na2C2O4 crystals) with gibbsite of surface area 39 m2/g showed no significant changes in the low-frequency band-height ratios of gibbsite and adsorbates.-D.J.M.","language":"English","publisher":"Wolters Kluwer","doi":"10.1097/00010694-198308000-00006","issn":"0038075X","usgsCitation":"Cunningham, K., and Goldberg, M.C., 1983, A reexamination of the effects of adsorbates on the Raman spectrum of gibbsite: Soil Science, v. 136, no. 2, p. 102-110, https://doi.org/10.1097/00010694-198308000-00006.","productDescription":"9 p.","startPage":"102","endPage":"110","numberOfPages":"9","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221507,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"136","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e540e4b0c8380cd46c30","contributors":{"authors":[{"text":"Cunningham, K.W.","contributorId":11476,"corporation":false,"usgs":true,"family":"Cunningham","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":360492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldberg, M. C.","contributorId":89220,"corporation":false,"usgs":true,"family":"Goldberg","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":360493,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011600,"text":"70011600 - 1983 - The saltwater-freshwater interface in the Tertiary limestone aquifer, southeast Atlantic outer-continental shelf of the U.S.A.","interactions":[],"lastModifiedDate":"2025-04-11T16:49:26.1536","indexId":"70011600","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"The saltwater-freshwater interface in the Tertiary limestone aquifer, southeast Atlantic outer-continental shelf of the U.S.A.","docAbstract":"Hydrologic testing in an offshore oil well abandoned by Tenneco, Inc., determined the position of the saltwater-freshwater interface in Tertiary limestones underlying the Florida-Georgia continental shelf of the U.S.A. Previous drilling (JOIDES and U.S.G.S. AMCOR projects) established the existence of freshwater far offshore in this area. At the Tenneco well 55 mi. (∼88 km) east of Fernandina Beach, Florida, drill-stem tests made in the interval 1050–1070 ft. (320–326 m) below sea level in the Ocala Limestone recovered a sample with a chloride concentration of 7000 mg l−1. Formation water probably is slightly fresher. Pressure-head measurements indicated equivalent freshwater heads of 24–29 ft. (7.3–8.8 m) above sea level.
At the coast (Fernandina Beach), a relatively thin transition zone separating freshwater and saltwater occurs at a depth of 2100 ft. (640 m) below sea level. Fifty-five miles (∼88 km) offshore, at the Tenneco well, the base of freshwater is ∼1100 ft. (∼335 m) below sea level. The difference in approximate depth to the freshwater-saltwater transition at these two locations suggests an interface with a very slight landward slope. Assuming the Hubbert interface equation applies here (because the interface and therefore freshwater flow lines are nearly horizontal) the equilibrium depth to the interface should be 40 times the freshwater head above sea level. Using present-day freshwater heads along the coast in the Hubbert equation results in depths to the interface of less than the observed 2100 ft. (640 m). Substituting predevelopment heads in the equation yields depths greater than 2100 ft. (640 m). Thus the interface appears to be in a transient position between the position that would be compatible with present-day heads and the position that would be compatible with predevelopment heads. This implies that some movement of the interface from the predevelopment position has occurred during the past hundred years. The implied movement is incompatible with the hypothesis that the freshwater occurring far offshore in this area is trapped water remaining since the Pleistocene Epoch.
","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(83)90251-2","issn":"00221694","usgsCitation":"Johnston, R., 1983, The saltwater-freshwater interface in the Tertiary limestone aquifer, southeast Atlantic outer-continental shelf of the U.S.A.: Journal of Hydrology, v. 61, no. 1-3, p. 239-249, https://doi.org/10.1016/0022-1694(83)90251-2.","productDescription":"11 p.","startPage":"239","endPage":"249","costCenters":[],"links":[{"id":220712,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida, Georgia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.49895094186574,\n 30.906206797439737\n ],\n [\n -82.49895094186574,\n 29.80296540535703\n ],\n [\n -81.27672743461723,\n 29.80296540535703\n ],\n [\n -81.27672743461723,\n 30.906206797439737\n ],\n [\n -82.49895094186574,\n 30.906206797439737\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"61","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bafb0e4b08c986b324998","contributors":{"authors":[{"text":"Johnston, R.H.","contributorId":19536,"corporation":false,"usgs":true,"family":"Johnston","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":361516,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012118,"text":"70012118 - 1983 - Terpenoid marker compounds derived from biogenic precursors in volcanic ash from Mount St. Helens, Washington","interactions":[],"lastModifiedDate":"2020-01-26T09:50:23","indexId":"70012118","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":"Terpenoid marker compounds derived from biogenic precursors in volcanic ash from Mount St. Helens, Washington","docAbstract":"A volcanic-ash sample obtained after the 1980 eruption of Mount St. Helens, Washington, was analyzed for cyclic terpenoid organic compounds and polycyclic aromatic hydrocarbons using capillary gas chromatography-mass spectrometry-computer techniques. Various tricyclic diterpenoid acids and hydrocarbons were identified including dehydroabietic acid, dehydroabietin, dehydroabietane, simonellite, and retene. Preliminary evidence indicates that these compounds were derived from forest soils or atmospheric aerosols or both in the vicinity of coniferous forests. A diagenetic scheme involving three possible pathways for the conversion of abietic acid to retene is presented.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(83)90052-2","issn":"00167037","usgsCitation":"Pereira, W.E., and Rostad, C.E., 1983, Terpenoid marker compounds derived from biogenic precursors in volcanic ash from Mount St. Helens, Washington: Geochimica et Cosmochimica Acta, v. 47, no. 12, p. 2287-2291, https://doi.org/10.1016/0016-7037(83)90052-2.","productDescription":"5 p.","startPage":"2287","endPage":"2291","numberOfPages":"5","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":222116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mount St. Helens ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.31628417968749,\n 46.164614496897094\n ],\n [\n -122.04711914062499,\n 46.164614496897094\n ],\n [\n -122.04711914062499,\n 46.34123949998618\n ],\n [\n -122.31628417968749,\n 46.34123949998618\n ],\n [\n -122.31628417968749,\n 46.164614496897094\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"47","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba54ae4b08c986b32094c","contributors":{"authors":[{"text":"Pereira, W. E.","contributorId":46981,"corporation":false,"usgs":true,"family":"Pereira","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":362773,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rostad, Colleen E. cerostad@usgs.gov","contributorId":833,"corporation":false,"usgs":true,"family":"Rostad","given":"Colleen","email":"cerostad@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":780294,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011042,"text":"70011042 - 1983 - Ultrastructural changes in the hepatocytes of juvenile rainbow trout and mature brown trout exposed to copper or zinc","interactions":[],"lastModifiedDate":"2020-01-20T19:55:23","indexId":"70011042","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Ultrastructural changes in the hepatocytes of juvenile rainbow trout and mature brown trout exposed to copper or zinc","docAbstract":"Morphological changes in hepatocytes of mature brown trout (Salmo trutta Linnaeus) and juvenile rainbow trout (Salmo gairdneri Richardson), accompanying chronic exposures to copper and zinc, were examined by transmission electron microscopy. At a concentration of copper not inhibitory to the final stages of gonadal development or spawning of brown trout, structural alterations included contraction of mitochondria and a tendency for nuclei to be slightly enlarged. Concentrations of copper or zinc lethal to a small fraction (10% and 4%, respectively) of a population of juvenile rainbow trout exposed for 42 d during larval and early juvenile development caused hepatocyte changes in survivors indicative of a reduction in ability to maintain intracellular water and cation balance and possible intranuclear metal sequestering. Specific structural alterations included increased vesiculation of rough endoplasmic reticulum, an increase in the abundance of electron-dense particles in the nucleus, increases in the numbers of multilaminar and globular inclusions, pooling of glycogen, increased autophagocytic activity and an increase in the number of necrotic cells. At advanced stages of toxicosis (concentrations of copper or zinc lethal to approximately 50% of the juveniles exposed for 42 d during development), loss in integrity of mitochondrial membranes, rupturing of plasma and nuclear membranes, separation of granular and fibrillar nuclear components, fragmentation of endoplasmic reticulum, and extensive autophagic vacuolization were significant features of hepatocytes of surviving juvenile rainbow trout.
","language":"English","publisher":"Wiley","doi":"10.1002/etc.5620020312","issn":"07307268","usgsCitation":"Leland, H., 1983, Ultrastructural changes in the hepatocytes of juvenile rainbow trout and mature brown trout exposed to copper or zinc: Environmental Toxicology and Chemistry, v. 2, no. 3, p. 353-368, https://doi.org/10.1002/etc.5620020312.","productDescription":"16 p.","startPage":"353","endPage":"368","numberOfPages":"16","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"3","noUsgsAuthors":false,"publicationDate":"1983-07-01","publicationStatus":"PW","scienceBaseUri":"505bbc07e4b08c986b3289a9","contributors":{"authors":[{"text":"Leland, H.V.","contributorId":82455,"corporation":false,"usgs":true,"family":"Leland","given":"H.V.","email":"","affiliations":[],"preferred":false,"id":360146,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010638,"text":"70010638 - 1983 - U. S. GEOLOGICAL SURVEY LAND REMOTE SENSING ACTIVITIES.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:19","indexId":"70010638","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"U. S. GEOLOGICAL SURVEY LAND REMOTE SENSING ACTIVITIES.","docAbstract":"USGS uses all types of remotely sensed data, in combination with other sources of data, to support geologic analyses, hydrologic assessments, land cover mapping, image mapping, and applications research. Survey scientists use all types of remotely sensed data with ground verifications and digital topographic and cartographic data. A considerable amount of research is being done by Survey scientists on developing automated geographic information systems that can handle a wide variety of digital data. The Survey is also investigating the use of microprocessor computer systems for accessing, displaying, and analyzing digital data.","conferenceTitle":"Proceedings - Pecora VIII Symposium: Satellite Land Remote Sensing Advancements for the Eighties.","conferenceLocation":"Sioux Falls, ND, USA","language":"English","publisher":"Augustana Coll","publisherLocation":"Sioux Falls, SD, USA","usgsCitation":"Frederick, D.G., 1983, U. S. GEOLOGICAL SURVEY LAND REMOTE SENSING ACTIVITIES., Proceedings - Pecora VIII Symposium: Satellite Land Remote Sensing Advancements for the Eighties., Sioux Falls, ND, USA, p. 28-30.","startPage":"28","endPage":"30","numberOfPages":"3","costCenters":[],"links":[{"id":219308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb9e7e4b08c986b327ec4","contributors":{"authors":[{"text":"Frederick, Doyle G.","contributorId":88873,"corporation":false,"usgs":true,"family":"Frederick","given":"Doyle","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":359319,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010367,"text":"70010367 - 1983 - An enriched finite element for simulation of groundwater flow to a well or drain - Comment","interactions":[],"lastModifiedDate":"2025-04-30T14:59:26.057359","indexId":"70010367","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"An enriched finite element for simulation of groundwater flow to a well or drain - Comment","docAbstract":"No abstract available.
","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(83)90033-1","issn":"00221694","usgsCitation":"Kemblowski, M., 1983, An enriched finite element for simulation of groundwater flow to a well or drain - Comment: Journal of Hydrology, v. 60, no. 1-4, p. 381-382, https://doi.org/10.1016/0022-1694(83)90033-1.","productDescription":"2 p.","startPage":"381","endPage":"382","numberOfPages":"2","costCenters":[],"links":[{"id":219684,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ea3be4b0c8380cd4870f","contributors":{"authors":[{"text":"Kemblowski, M.","contributorId":54340,"corporation":false,"usgs":true,"family":"Kemblowski","given":"M.","affiliations":[],"preferred":false,"id":358754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21016,"text":"ofr8333 - 1983 - Hydrology of area 6, Eastern Coal Province, Maryland, West Virginia and Pennsylvania","interactions":[],"lastModifiedDate":"2023-03-29T19:53:53.242091","indexId":"ofr8333","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":"83-33","title":"Hydrology of area 6, Eastern Coal Province, Maryland, West Virginia and Pennsylvania","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8333","usgsCitation":"Staubitz, W., and Sobashinski, J.R., 1983, Hydrology of area 6, Eastern Coal Province, Maryland, West Virginia and Pennsylvania: U.S. Geological Survey Open-File Report 83-33, 131 p., https://doi.org/10.3133/ofr8333.","productDescription":"131 p.","costCenters":[],"links":[{"id":414908,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13985.htm","linkFileType":{"id":5,"text":"html"}},{"id":153732,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0033/report-thumb.jpg"},{"id":95445,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maryland, Pennsylvania, West Virginia","otherGeospatial":"Eastern Coal Province","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -79.488,\n 39.958\n ],\n [\n -79.488,\n 39.071\n ],\n [\n -78.558,\n 39.071\n ],\n [\n -78.558,\n 39.958\n ],\n [\n -79.488,\n 39.958\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f58","contributors":{"authors":[{"text":"Staubitz, W. W.","contributorId":73209,"corporation":false,"usgs":true,"family":"Staubitz","given":"W. W.","affiliations":[],"preferred":false,"id":183688,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sobashinski, John R.","contributorId":16856,"corporation":false,"usgs":true,"family":"Sobashinski","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":183687,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83216","usgsCitation":"Lindskov, K., and Kimball, B.A., 1983, Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado: U.S. Geological Survey Open-File Report 83-216, 100 p., https://doi.org/10.3133/ofr83216.","productDescription":"100 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":144898,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0216/report-thumb.jpg"},{"id":367637,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0216/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah, Colorado","otherGeospatial":"Uinta 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636538","contributors":{"authors":[{"text":"Lindskov, K.L.","contributorId":91077,"corporation":false,"usgs":true,"family":"Lindskov","given":"K.L.","affiliations":[],"preferred":false,"id":160725,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kimball, Briant A. bkimball@usgs.gov","contributorId":533,"corporation":false,"usgs":true,"family":"Kimball","given":"Briant","email":"bkimball@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":160724,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3192,"text":"wsp2195 - 1983 - Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden","interactions":[{"subject":{"id":23739,"text":"ofr81535 - 1981 - Hydrology of the Ferron sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah","indexId":"ofr81535","publicationYear":"1981","noYear":false,"title":"Hydrology of the Ferron sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3192,"text":"wsp2195 - 1983 - Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden","indexId":"wsp2195","publicationYear":"1983","noYear":false,"title":"Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden"},"id":1}],"lastModifiedDate":"2023-11-29T22:45:01.092093","indexId":"wsp2195","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2195","title":"Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden","docAbstract":"Coal in the Ferron Sandstone Member of the Mancos Shale of Cretaceous age has traditionally been mined by underground techniques in the Emery Coal Field in the southern end of Castle Valley in east-central Utah. However, approximately 99 million tons are recoverable by surface mining. Ground water in the Ferron is the sole source of supply for the town of Emery, but the aquifer is essentially untapped outside the Emery area.
The Ferron Sandstone Member crops out along the eastern edge of Castle Valley and generally dips 2 ? to 10 ? to the northwest. Sandstones in the Ferron are enclosed between relatively impermeable shale in the Tununk and Blue Gate Members of the Mancos Shale. Along the outcrop, the Ferron ranges in thickness from about 80 feet in the northern part of Castle Valley to 850 feet in the southern part. The Ferron also generally thickens in the subsurface downdip from the outcrop. Records from wells and test holes indicate that the full thickness of the Ferron is saturated with water in most areas downdip from the outcrop area.
Tests in the Emery area indicate that transmissivity of the Ferron sandstone aquifer ranges from about 200 to 700 feet squared per day where the Ferron is fully saturated. Aquifer transmissivity is greatest near the Paradise Valley-Joes Valley fault system where permeability has been increased by fracturing. Storage coefficient ranges from about 10 .6 to 10 -3 where the Ferron sandstone aquifer is confined and probably averages 5 x 10-2 where it is unconfined.
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