No abstract available.
","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Nalley, G., and Rettman, P., 1988, Compilation of hydrologic data for the Edwards Aquifer, San Antonio area, Texas, 1987, with 1934-87 summary: Edwards Underground Water District Bulletin 47, 154 p.","productDescription":"154 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327778,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c6aef3e4b0f2f0cebe4637","contributors":{"authors":[{"text":"Nalley, G.M.","contributorId":23535,"corporation":false,"usgs":true,"family":"Nalley","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":646899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rettman, P.L.","contributorId":60663,"corporation":false,"usgs":true,"family":"Rettman","given":"P.L.","affiliations":[],"preferred":false,"id":646900,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70014419,"text":"70014419 - 1988 - A tentative protocol for measurement of radon availability from the ground","interactions":[],"lastModifiedDate":"2025-07-16T15:31:46.948915","indexId":"70014419","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3223,"text":"Radiation Protection Dosimetry","active":true,"publicationSubtype":{"id":10}},"title":"A tentative protocol for measurement of radon availability from the ground","docAbstract":"A procedure is being tested in order to determine its suitability for assessing the intrinsic ability of the ground at a particular site to supply 222Rn to a basement structure to be built on the site. Soil gas is sucked from a borehole probe through an alpha scintillation chamber and flow meter by a pump. The permeability of the soil is calculated from the flow rate and the pressure difference between the atmosphere and the borehole at the intake point. The diffusion coefficient is estimated from the water fraction in the soil pores. The upward migration distance for radon in such soil during one mean life is computed from an arbitrary steady pressure difference. This mean migration distance, multiplied by the measured radon concentration, gives the 'radon availability number'. Measurements at sites of known indoor radon concentration suggest that numbers below 2 kBq.m-2 indicate litte chance of elevated indoor radon and above 20 kBq.m-2 indicate that elevated indoor radon is likely. The range of uncertainty and the point-to-point and seasonal variations to be expected are under investigation.
","language":"English","publisher":"Oxford Academic","doi":"10.1093/oxfordjournals.rpd.a080246","issn":"01448420","usgsCitation":"Tanner, A., 1988, A tentative protocol for measurement of radon availability from the ground: Radiation Protection Dosimetry, v. 24, no. 1-4, p. 79-83, https://doi.org/10.1093/oxfordjournals.rpd.a080246.","productDescription":"5 p.","startPage":"79","endPage":"83","numberOfPages":"5","costCenters":[],"links":[{"id":226222,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"1-4","noUsgsAuthors":false,"publicationDate":"1988-08-01","publicationStatus":"PW","scienceBaseUri":"5059e5f5e4b0c8380cd47062","contributors":{"authors":[{"text":"Tanner, A.B.","contributorId":44155,"corporation":false,"usgs":true,"family":"Tanner","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":368359,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70014422,"text":"70014422 - 1988 - Effectiveness of an urban runoff detention pond - Wetlands system","interactions":[],"lastModifiedDate":"2024-04-22T15:10:49.126343","indexId":"70014422","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","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":"Effectiveness of an urban runoff detention pond - Wetlands system","docAbstract":"The effectiveness of an urban detention system, composed of a detention pond and wetlands in series, in reducing constituent loads carried in runoff was determined. The detention pond was effective in reducing loads of suspended solids and suspended metals. Suspendedphase efficiencies for solids, lead, and zinc ranged between 42 and 66%. Nutrient efficiencies were variable, ranging for all species and phases, from less than 0 to 72%. The wetlands generally was effective in reducing both suspended and dissolved loads of solids and metals. Total (dissolved + suspended) solids, lead, and zinc efficiencies ranged between 41 and 73%. Efficiencies for total nitrogen and phosphorus were 21 and 17%, respectively. The system, by combining the treatment of the pond and wetlands, was very effective in reducing loads of most constituents. Total solids, lead, and zinc efficiencies ranged between 55 and 83%. Total nitrogen and phosphorus efficiencies were 36 and 43%, respectively.
","language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0733-9372(1988)114:4(810)","issn":"07339372","usgsCitation":"Martin, E., 1988, Effectiveness of an urban runoff detention pond - Wetlands system: Journal of Environmental Engineering, v. 114, no. 4, p. 810-827, https://doi.org/10.1061/(ASCE)0733-9372(1988)114:4(810).","productDescription":"18 p.","startPage":"810","endPage":"827","costCenters":[],"links":[{"id":225252,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"114","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0638e4b0c8380cd51168","contributors":{"authors":[{"text":"Martin, E.H.","contributorId":27098,"corporation":false,"usgs":true,"family":"Martin","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":368363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70014421,"text":"70014421 - 1988 - Effects of sulfur dioxide emissions on stream chemistry in the western United States","interactions":[],"lastModifiedDate":"2018-02-21T11:05:57","indexId":"70014421","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","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":"Effects of sulfur dioxide emissions on stream chemistry in the western United States","docAbstract":"A 20-year record of water chemistry for seven headwater streams in the Rocky Mountain region of the western United States is compared to estimates of local and regional sulfur dioxide emissions for the same period. Emissions from smelters in the region comprise a significant part of sulfur dioxide emissions for the 11 states upwind of acid-sensitive watersheds in the Rocky Mountains, but smelter emissions have steadily decreased since 1970. Analysis of stream chemistry indicates conservative behavior of watershed sulfate, with atmospheric deposition as the dominant source of sulfate. No relation between regional stream chemistry and smelter or regional sulfur dioxide emissions is detected for the watersheds. Local emissions trends, however, do appear to affect sulfate concentrations in the streams. Year-to-year variability in stream sulfate concentration is much greater than any long-term trends that might be inferred.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR024i006p00871","usgsCitation":"Campbell, K., and Turk, J., 1988, Effects of sulfur dioxide emissions on stream chemistry in the western United States: Water Resources Research, v. 24, no. 6, p. 871-878, https://doi.org/10.1029/WR024i006p00871.","productDescription":"8 p.","startPage":"871","endPage":"878","costCenters":[],"links":[{"id":225251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"24","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505a07e8e4b0c8380cd518c0","contributors":{"authors":[{"text":"Campbell, K.","contributorId":63351,"corporation":false,"usgs":false,"family":"Campbell","given":"K.","affiliations":[{"id":47665,"text":"St. Anthony Falls Laboratory, University of Minnesota, Minneapolis, MN, USA","active":true,"usgs":false}],"preferred":false,"id":368361,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turk, J.T.","contributorId":94259,"corporation":false,"usgs":true,"family":"Turk","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":368362,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013242,"text":"70013242 - 1988 - Alteration in the Madera limestone and Sandia formation from core hole VC-1, Valles Caldera, New Mexico","interactions":[],"lastModifiedDate":"2024-06-05T16:00:01.052773","indexId":"70013242","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Alteration in the Madera limestone and Sandia formation from core hole VC-1, Valles Caldera, New Mexico","docAbstract":"Core hole VC-1 penetrated the southwestern ring fracture zone of the 1.1 Ma Valles caldera and at a depth of 333 m intersected the top of the Paleozoic section including the Abo Formation, Madera Limestone, and Sandia Formation, reaching a total depth of 856 m. The Paleozoic rocks, which consist of thin-bedded limestone, siltstone, mudstone, sandstone, and local conglomerate, are overlain by volcanic rocks of the caldera moat that are less than 0.6 Ma. Diagenetic and at least three hydrothermal alteration stages were identified in the Madera Limestone and Sandia Formation. Diagenetic clay alteration was pervasive throughout the sedimentary rocks. Volcanic activity at 16.5 Ma and continuing through the formation of the Valles caldera resulted in high thermal gradients, which caused recrystallization of diagenetic clay minerals. Interstratified smectite-illite is the most diagnostic clay mineral throughout the section; structurally, the illite component in the ordered interstratified illite-smectite changes gradationally from 70% at the top of the Madera Limestone to 95% at the base of the section in the Sandia Formation. Pyrite that occurs as small clots and lenses as well as finely disseminated is interpreted as being of diagenetic origin, especially in organic-rich beds. Low permeability of much of the Paleozoic section precluded the deposition of hydrothermal minerals except in fractures and intergranular space in some of the more permeable sandstone and brecciated horizons. Three stages of hydrothermal mineral deposition are defined. Stage I is widespread and includes mainly chlorite, calcite, pyrite, and interstratified smectite-illite that was formed prior to caldera development at temperatures approximating 200°C. Stage II is characterized by quartz, sericite, and scarce sulfides deposited locally by fluids at approximately 275°C shortly before or at the time of early caldera-related volcanism. The Stage III hydrothermal event, associated with formation of the Valles caldera, caused complex brecciation accompanied by deposition of phengite and molybdenite at temperatures locally approaching 300°C mostly in rocks underlying the Madera Limestone. During the present drilling program, thermal aquifers were encountered at 483 m (113°C), 533 m (125°C), and 845 m (184°C), very close to the Stage II and III mineralized zones; however, measured temperatures of the present hydrothermal system are much lower than during the main hydrothermal events. Good permeability has been maintained in these three levels for a long time while the rest of the Madera Limestone and Sandia Formation was sealed by hydrothermal mineral precipitation.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB093iB06p06068","issn":"01480227","usgsCitation":"Keith, T.E., 1988, Alteration in the Madera limestone and Sandia formation from core hole VC-1, Valles Caldera, New Mexico: Journal of Geophysical Research Solid Earth, v. 93, no. B6, p. 6068-6076, https://doi.org/10.1029/JB093iB06p06068.","productDescription":"9 p.","startPage":"6068","endPage":"6076","numberOfPages":"9","costCenters":[],"links":[{"id":220361,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"93","issue":"B6","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"5059e978e4b0c8380cd482d4","contributors":{"authors":[{"text":"Keith, T. E. C.","contributorId":11681,"corporation":false,"usgs":true,"family":"Keith","given":"T.","email":"","middleInitial":"E. C.","affiliations":[],"preferred":false,"id":365615,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70014465,"text":"70014465 - 1988 - Mechanistic characterization of chloride interferences in electrothermal atomization systems","interactions":[],"lastModifiedDate":"2020-01-12T14:22:27","indexId":"70014465","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Mechanistic characterization of chloride interferences in electrothermal atomization systems","docAbstract":"A computer-controlled spectrometer with a photodiode array detector has been used for wavelength and temperature resolved characterization of the vapor produced by an electrothermal atomizer. The system has been used to study the chloride matrix interference on the atomic absorption spectrometric determination of manganese and copper. The suppression of manganese and copper atom populations by matrix chlorides such as those of calcium and magnesium is due to the gas-phase formation of an analyte chloride species followed by the diffusion of significant fractions of these species from the atom cell prior to completion of the atomization process. The analyte chloride species cannot be formed when matrix chlorides with metal-chloride bond dissociation energies above those of the analyte chlorides are the principal entitles present. The results indicate that multiple wavelength spectrometry used to obtain temperature-resolved spectra is a viable tool in the mechanistic characterization of interference effects observed with electrothermal atomization systems.
","language":"English","publisher":"ACS","doi":"10.1021/ac00174a010","issn":"00032700","usgsCitation":"Shekiro, J., Skogerboe, R., and Taylor, H.E., 1988, Mechanistic characterization of chloride interferences in electrothermal atomization systems: Analytical Chemistry, v. 60, no. 23, p. 2578-2582, https://doi.org/10.1021/ac00174a010.","productDescription":"5 p.","startPage":"2578","endPage":"2582","numberOfPages":"5","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":225958,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"23","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a5373e4b0c8380cd6cac4","contributors":{"authors":[{"text":"Shekiro, J.M. Jr.","contributorId":11773,"corporation":false,"usgs":true,"family":"Shekiro","given":"J.M.","suffix":"Jr.","affiliations":[],"preferred":false,"id":368459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skogerboe, R.K.","contributorId":7348,"corporation":false,"usgs":true,"family":"Skogerboe","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":368458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":368460,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70014420,"text":"70014420 - 1988 - Radiolarian biostratigraphy of siliceous Eocene deposits in central California","interactions":[],"lastModifiedDate":"2012-03-12T17:19:33","indexId":"70014420","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2735,"text":"Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Radiolarian biostratigraphy of siliceous Eocene deposits in central California","docAbstract":"Abundant Eocene siliceous deposits in California are located in the San Joaquin and Sacramento valleys. The white shales to buff mudstones are characterized by radiolarians, diatoms, and silicoflagellates. Taxonomic descriptions and abundance data of key radiolarian species in existing monographs have limited biostratigraphic and paleoenvironmental interpretation. The California fauna is similar to faunas from the Norwegian Sea, Russian Platform, and southern oceans of Antarctica. Eocene faunas from the equatorial Pacific Ocean and Caribbean Sea differ considerably in diversity. In this study, the taxonomy and biostratigraphic information of species comprising more than 2% of the population are evaluated. Two radiolarian zones are erected for the middle Eocene of California, the Podocyrtis fasciata and Calocyclas semipolita Zones. Paleoenvironmental information suggests that some differences in the fauna may be environmentally controlled due to deposition in submarine canyons. -Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Micropaleontology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00262803","usgsCitation":"Blueford, J., 1988, Radiolarian biostratigraphy of siliceous Eocene deposits in central California: Micropaleontology, v. 34, no. 3, p. 236-258.","startPage":"236","endPage":"258","numberOfPages":"23","costCenters":[],"links":[{"id":225250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9400e4b0c8380cd81147","contributors":{"authors":[{"text":"Blueford, J.","contributorId":76890,"corporation":false,"usgs":true,"family":"Blueford","given":"J.","affiliations":[],"preferred":false,"id":368360,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70014410,"text":"70014410 - 1988 - Sr and Nd isotopic variations in ferromanganese crusts from the Central Pacific: Implications for age and source provenance","interactions":[],"lastModifiedDate":"2024-04-03T16:21:48.833884","indexId":"70014410","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","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":"Sr and Nd isotopic variations in ferromanganese crusts from the Central Pacific: Implications for age and source provenance","docAbstract":"Isotopic analyses of two hydrogenetic ferromanganese (Fe-Mn) crusts from volcanic edifices in the central Pacific Ocean reveal systematic variations in
A bored and encrusted late Pleistocene ooid grainstone was recovered from the seafloor at a depth of approximately 40 m on the outer continental shelf of eastern Florida. Ooid cortices are dominantly bimineralic, generally consisting of inner layers of radial magnesian calcite and outer layers of tangential aragonite. Ooid nuclei are dominantly rounded cryptocrystalline grains, although quartz grains and a variety of skeletal grains also occur as nuclei. Ooids are partially cemented by blocky calcite, and interparticle porosity is partially filled by micrite.
\n\n
Radial cortex layers are composed of brightly cathodoluminescent magnesian calcite having a composition of approximately 12 mol% MgCO3 and 1000 ppm strontium. The iron and manganese concentrations in radial cortex layers are generally in the range of 500–1000 ppm and 100–250 ppm, respectively. Tangential cortex layers are composed of noncathodoluminescent aragonite containing approximately 11 500 ppm strontium and less than 0.5 mol% MgCO3. Iron concentrations in tangential cortex layers are generally in the range of 150–400 ppm, and manganese concentrations are generally below the detection limit of 100 ppm. Echinoderm skeletal fragments, which are present as accessory grains, are composed of brightly cathodoluminescent magnesian calcite. Some ooid nuclei and the thin outer edges of some blocky calcite cement are cathodoluminescent; micrite matrix and the bulk of blocky calcite cement are noncathodoluminescent. Ooids do not exhibit textural evidence of recrystallization.
\n\n
The ooid grainstone underwent an episode of meteoric diagenesis. but ooid cortices were not affected by the event. We propose a previously unrecognized process by which the magnesian calcite cortex layers underwent diagenetic alteration in oxygen-depleted seawater. During this diagenesis, magnesium was lost and manganese was incorporated without apparent textural alteration and without mineralogical stabilization. Thus, we Suggest that cathodoluminescence may result from diagenetic alteration on the sea-floor.
\nNo abstract available
","language":"English","publisher":"Bonneville Power Administration","publisherLocation":"Portland, OR","usgsCitation":"Poe, T., and Rieman, B., 1988, Predation by resident fish on juvenile salmonids in John Day Reservoir.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334670,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"John Day reservoir ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.67176818847656,\n 45.74500616007653\n ],\n [\n -120.87570190429688,\n 45.682678322324904\n ],\n [\n -120.94642639160158,\n 45.67116404333791\n ],\n [\n -120.94917297363281,\n 45.63516665067313\n ],\n [\n -120.88874816894531,\n 45.62652383350405\n ],\n [\n -120.79399108886719,\n 45.67596194751415\n ],\n [\n -120.63400268554689,\n 45.73206686696598\n ],\n [\n -120.67176818847656,\n 45.74500616007653\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5895a4d5e4b0fa1e59bc1ea8","contributors":{"authors":[{"text":"Poe, T.P.","contributorId":51687,"corporation":false,"usgs":true,"family":"Poe","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":662448,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rieman, B.E.","contributorId":67283,"corporation":false,"usgs":true,"family":"Rieman","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":662449,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70014413,"text":"70014413 - 1988 - Geohydrologic aspects of water-quality problems of the San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-03-12T17:19:29","indexId":"70014413","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geohydrologic aspects of water-quality problems of the San Joaquin Valley, California","docAbstract":"Salinity and selenium concentrations in shallow ground water of the western San Joaquin Valley, California, are related to the geomorphology and hydrology of the alluvial fans. High salinity and selenium concentrations are associated with ephemeral-stream deposits. Low salinity and selenium concentrations are associated with intermittent-stream deposits, which represent the major alluvial fans of the area. The highest salinity and selenium concentrations at the margins of the alluvial fans are the result of evaporation and evapotranspiration of shallow ground water, as indicated by oxygen- and hydrogen-isotopic data. The extent and direction of movement of saline ground water to drain laterals in agricultural fields are influenced by the time since installation of the drainage system, drain lateral spacing, and the regional ground-water-flow system.","conferenceTitle":"Planning Now for Irrigation and Drainage in the 21st Century","conferenceDate":"18 July 1988 through 21 July 1988","conferenceLocation":"Lincoln, NE, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0872626660","usgsCitation":"Deverel, S.J., 1988, Geohydrologic aspects of water-quality problems of the San Joaquin Valley, California, Planning Now for Irrigation and Drainage in the 21st Century, Lincoln, NE, USA, 18 July 1988 through 21 July 1988, p. 694-699.","startPage":"694","endPage":"699","numberOfPages":"6","costCenters":[],"links":[{"id":226153,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a17a0e4b0c8380cd55575","contributors":{"authors":[{"text":"Deverel, S. J.","contributorId":65478,"corporation":false,"usgs":true,"family":"Deverel","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":368349,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013241,"text":"70013241 - 1988 - Molecular composition and mobility of torbanite precursors: Implications for the structure of coal","interactions":[],"lastModifiedDate":"2023-12-16T00:57:07.285115","indexId":"70013241","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1506,"text":"Energy & Fuels","active":true,"publicationSubtype":{"id":10}},"title":"Molecular composition and mobility of torbanite precursors: Implications for the structure of coal","docAbstract":"Coorongite, a torbanite precursor found in South Australia, and algal residues derived from Botryococcus braunii and other algae have been examined by solid-state 13C NMR techniques. The majority of carbon in these materials is present as (CH2)n. However, variable-temperature studies show that a considerable proportion of the alkyl chains have unusual dipolar-dephasing behavior and are more mobile than in rigid solids. It is suggested that these mobile structures contribute to the so-called \"guest phases\" in coal. The data are also consistent with a vascular and algal model of coal. ?? 1988 American Chemical Society.","language":"English","publisher":"American Chemical Society","doi":"10.1021/ef00011a012","issn":"08870624","usgsCitation":"Wilson, M.A., Batts, B., and Hatcher, P.G., 1988, Molecular composition and mobility of torbanite precursors: Implications for the structure of coal: Energy & Fuels, v. 2, no. 5, p. 668-672, https://doi.org/10.1021/ef00011a012.","productDescription":"5 p.","startPage":"668","endPage":"672","numberOfPages":"5","costCenters":[],"links":[{"id":220298,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"5","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a5cfee4b0c8380cd700af","contributors":{"authors":[{"text":"Wilson, M. A.","contributorId":107649,"corporation":false,"usgs":false,"family":"Wilson","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":365614,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Batts, B.D.","contributorId":15757,"corporation":false,"usgs":true,"family":"Batts","given":"B.D.","email":"","affiliations":[],"preferred":false,"id":365612,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hatcher, Patrick G.","contributorId":93625,"corporation":false,"usgs":true,"family":"Hatcher","given":"Patrick","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":365613,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70013304,"text":"70013304 - 1988 - A computer program to calculate centrifugation parameters for sedimentation analyses","interactions":[],"lastModifiedDate":"2013-01-21T15:31:32","indexId":"70013304","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"A computer program to calculate centrifugation parameters for sedimentation analyses","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(88)90034-9","issn":"00983004","usgsCitation":"Poppe, L., Fredericks, J., and Hathaway, J., 1988, A computer program to calculate centrifugation parameters for sedimentation analyses: Computers & Geosciences, v. 14, no. 4, p. 541-545, https://doi.org/10.1016/0098-3004(88)90034-9.","startPage":"541","endPage":"545","numberOfPages":"5","costCenters":[],"links":[{"id":266177,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(88)90034-9"},{"id":220301,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e38de4b0c8380cd460c3","contributors":{"authors":[{"text":"Poppe, L.J.","contributorId":72782,"corporation":false,"usgs":true,"family":"Poppe","given":"L.J.","affiliations":[],"preferred":false,"id":365766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fredericks, J.J.","contributorId":77517,"corporation":false,"usgs":true,"family":"Fredericks","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":365767,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hathaway, J.C.","contributorId":94280,"corporation":false,"usgs":true,"family":"Hathaway","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":365768,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7000053,"text":"7000053 - 1988 - Ground water and the rural homeowner","interactions":[],"lastModifiedDate":"2012-08-03T01:02:04","indexId":"7000053","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"Ground water and the rural homeowner","docAbstract":"As the salesmen sang in the musical The Music Man, \"You gotta know the territory.\" This saying is also true when planning to buy or build a house. Learn as much as possible about the land, the water supply, and the septic system of the house before buying or building. Do not just look at the construction aspects or the beauty of the home and surroundings. Be sure to consider the environmental conditions around and beneath the site as well. Try to visit the site under adverse conditions, such as during heavy rain or meltwater runoff, to observe the drainage characteristics, particularly the condition of the basement. Many of the conditions discussed in this book, such as lowered well-water levels, flooded basements, and contamination from septic systems, are so common that rural families often have to deal with one or more of them. The purpose of this book is to awaken an interest in ground water and an awareness of where it is available, how it moves, how people can adjust to its patterns to avoid problems, and how it can be protected and used wisely. This booklet provides both present and prospective rural homeowners, particularly those in the glaciated northern parts of the United States, with a basic but comprehensive description of ground water. It also presents problems one may expect to encounter with ground water and some solutions or suggestions for help with these problems.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/7000053","usgsCitation":"Waller, R., 1988, Ground water and the rural homeowner: General Interest Publication, 37 p. : col. ill. ; 23 cm., https://doi.org/10.3133/7000053.","productDescription":"37 p. : col. ill. ; 23 cm.","costCenters":[],"links":[{"id":258783,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/7000053/report.pdf","size":"6235","linkFileType":{"id":1,"text":"pdf"}},{"id":258784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/7000053/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dc86","contributors":{"authors":[{"text":"Waller, Roger M.","contributorId":90353,"corporation":false,"usgs":true,"family":"Waller","given":"Roger M.","affiliations":[],"preferred":false,"id":344027,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":85366,"text":"85366 - 1988 - Dabbling duck harvest dynamics in the Central Valley of California--implications for recruitment","interactions":[],"lastModifiedDate":"2012-02-02T00:04:01","indexId":"85366","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Dabbling duck harvest dynamics in the Central Valley of California--implications for recruitment","docAbstract":"Age and sex ratios and body weights were obtained for northern pintails (Anas acuta), mallards (A. platyrhynchos), American wigeon (A. americana), green-winged teal (A. crecca), and northern shovelers (A. clypeata) shot at Mendota State Wildlife Area in the San Joaquin Valley (SANJV) and at Sacramento National Wildlife Refuge in the Sacramento Valley (SACV) during 1982-83 and 1983-84. Age ratios were determined for pintails at four locations during 1980-83. Cooperative Waterfowl Parts Collection Survey (1982-84; U.S. Fish and Wildlife Service) and California preseason-banding data (1973-77, for mallards and pintails) also were used to measure age ratios of the California harvest. Harvest rate (ducks shot per day) was obtained and summed from all SACV and SANJV public hunting areas in 1982-84. All species except female wigeon and adult female mallards lost weight between October and January. Except for wigeon, harvest rate was high in October when hunting began. Harvest rates were low in November and December but rose markedly in January in the SACV for all species and for all except pintails in the SANJV. Proportion of adults in the bag as measured by all methods increased progressively through the hunting season. Proportion of adults in the harvest was higher in 1982-83 than in 1983-84 and was greater in the SACV than the SANJV both years for most species. Adult females formed a small component of total kill but 50% or more of female kill. The harvest of pintails at a SACV and a SANJV location consistently contained about half as many immatures per adult as that at two other California locations for 1980-83. The substantial harvest of adults in January eliminates the most productive breeders from the population. Thus, winter hunting mortality may influence age composition of the spring flight and, hence, recruitment potential of the breeding population.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Waterfowl in winter","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"University of Minnesota Press","publisherLocation":"Minneapolis, MN","usgsCitation":"Miller, M.R., Beam, J., and Connelly, D., 1988, Dabbling duck harvest dynamics in the Central Valley of California--implications for recruitment, chap. of Waterfowl in winter, p. 553-569 [624 pp.].","productDescription":"p. 553-569 [624 pp.]","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":127897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e9cf","contributors":{"editors":[{"text":"Weller, M.W.","contributorId":54562,"corporation":false,"usgs":true,"family":"Weller","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":504439,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Miller, M. R.","contributorId":19104,"corporation":false,"usgs":true,"family":"Miller","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":295959,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beam, J.","contributorId":66624,"corporation":false,"usgs":true,"family":"Beam","given":"J.","email":"","affiliations":[],"preferred":false,"id":295961,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Connelly, D.P.","contributorId":30166,"corporation":false,"usgs":true,"family":"Connelly","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":295960,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":95036,"text":"95036 - 1988 - Effects of LHRHa and testosterone implants on the maturation of snook","interactions":[],"lastModifiedDate":"2012-02-02T00:03:57","indexId":"95036","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Effects of LHRHa and testosterone implants on the maturation of snook","docAbstract":"No abstract available at this time","language":"English","publisher":"Texas Parks and Wildlife Department","collaboration":"89-060/FC","usgsCitation":"Henderson-Arzapalo, A., Colura, R., and Van Orman, J., 1988, Effects of LHRHa and testosterone implants on the maturation of snook.","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":128451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6250c5","contributors":{"authors":[{"text":"Henderson-Arzapalo, A.","contributorId":92607,"corporation":false,"usgs":true,"family":"Henderson-Arzapalo","given":"A.","email":"","affiliations":[],"preferred":false,"id":298566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colura, R.L.","contributorId":53721,"corporation":false,"usgs":true,"family":"Colura","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":298564,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Van Orman, J.","contributorId":56589,"corporation":false,"usgs":true,"family":"Van Orman","given":"J.","email":"","affiliations":[],"preferred":false,"id":298565,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70187626,"text":"70187626 - 1988 - Populations, productivity, and feeding habits of seabirds on St. Lawrence Island, Alaska: Final report","interactions":[],"lastModifiedDate":"2017-05-11T12:22:42","indexId":"70187626","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Populations, productivity, and feeding habits of seabirds on St. Lawrence Island, Alaska: Final report","docAbstract":"A field camp was established at Kongkok Bay near the southwest cape of St. Lawrence Island and occupied continuously from 24 May to 2 September 1987. Permanent study plots were selected for both cliff and crevice-nesting species, and regular observations were made throughout the breeding season to document attendance patterns, breeding phenology, and success. Periodic collections of adults offshore and of chick meals in the colonies were used to determine the food habits of study species. Additional plots for population monitoring of murres and kittiwakes were established in colonies near Savoonga on the north side of the island, and counts were made there between 23 July and 1 August. Shore based work was supplemented with offshore studies of seabird foraging distribution from the USFWS vessel TIGLAX between 18 August and 3 September 1987.
Populations of all study species in the Kongkok Bay area increased since the last study of seabirds there (murres 20, kittiwakes 87, Least Auklets 8, Crested Auklets 442). Pelagic Cormorants, Common Murres, and Thick-billed Murres exhibited average, or above average, breeding success at Kongkok in 1987. Black-legged Kittiwakes exhibited near-total reproductive failure. Crested and Least Auklets had high levels of breeding success after the effects of observer disturbance were taken into account. Predation by microtine rodents and foxes was a significant source of chick mortality on auklets.
Feeding concentrations were found primarily north of Gambell in the Anadyr Strait or western Chirikof Basin. Kittiwakes were dispersed widely over the study area. Diets of all species studied were normal and, with the exception of kittiwakes, there was no evidence of problems in obtaining food.
Current methods for assessing population changes in cliff-nesting species are considered adequate, but better techniques are needed for crevice-nesting auklets. Time-lapse photography offers the greatest potential for monitoring auklet numbers. A protocol is suggested for monitoring populations of murres, kittiwakes, and auklets at colonies in the Bering and Chukchi Seas. It calls for annual visits to selected colonies during two stages of the nesting cycle to assess numbers and breeding productivity.
The breeding failure of Black-legged Kittiwakes on St. Lawrence Island in 1987 was part of a pervasive syndrome of failure in this species observed throughout the Bering Sea and Gulf of Alaska in recent years. The causes of recurrent, widespread breeding failure need to be identified if kittiwakes are to have a role in area-wide population monitoring during the period of Alaskan development by the oil and gas industry.
","language":"English","publisher":"U.S. Fish and Wildlife Service, Alaska Fish and Wildlife Research Center","publisherLocation":"Anchorage, AK","usgsCitation":"Piatt, J.F., Hatch, S.A., Roberts, B.D., Lidster, W.W., Wells, J.L., and Haney, J.C., 1988, Populations, productivity, and feeding habits of seabirds on St. Lawrence Island, Alaska: Final report, xvi, 235 p.","productDescription":"xvi, 235 p.","numberOfPages":"254","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":341109,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":341108,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://alaska.usgs.gov/products/pubs/1988/1988_Piatt_etal_MMS_REP_88-022.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"St. Lawrence Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -172.386474609375,\n 62.72956747019657\n ],\n [\n -168.013916015625,\n 62.72956747019657\n ],\n [\n -168.013916015625,\n 63.95184936610536\n ],\n [\n -172.386474609375,\n 63.95184936610536\n ],\n [\n -172.386474609375,\n 62.72956747019657\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59157821e4b01a342e691472","contributors":{"authors":[{"text":"Piatt, John F. 0000-0002-4417-5748 jpiatt@usgs.gov","orcid":"https://orcid.org/0000-0002-4417-5748","contributorId":3025,"corporation":false,"usgs":true,"family":"Piatt","given":"John","email":"jpiatt@usgs.gov","middleInitial":"F.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":694823,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatch, Scott A. 0000-0002-0064-8187 shatch@usgs.gov","orcid":"https://orcid.org/0000-0002-0064-8187","contributorId":2625,"corporation":false,"usgs":true,"family":"Hatch","given":"Scott","email":"shatch@usgs.gov","middleInitial":"A.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":694824,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roberts, Bay D.","contributorId":181868,"corporation":false,"usgs":false,"family":"Roberts","given":"Bay","email":"","middleInitial":"D.","affiliations":[{"id":6987,"text":"U.S. Fish and Wildlife Sevice","active":true,"usgs":false}],"preferred":false,"id":694825,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lidster, Wayne W.","contributorId":189277,"corporation":false,"usgs":false,"family":"Lidster","given":"Wayne","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":694826,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wells, John L.","contributorId":189278,"corporation":false,"usgs":false,"family":"Wells","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":694827,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Haney, J. Christopher","contributorId":48043,"corporation":false,"usgs":true,"family":"Haney","given":"J.","email":"","middleInitial":"Christopher","affiliations":[{"id":6654,"text":"USFWS","active":true,"usgs":false}],"preferred":false,"id":694828,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70013354,"text":"70013354 - 1988 - Organic geothermometry of petroleum from Escanaba Trough, offshore northern California","interactions":[],"lastModifiedDate":"2025-03-14T21:01:25.200942","indexId":"70013354","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2958,"text":"Organic Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Organic geothermometry of petroleum from Escanaba Trough, offshore northern California","docAbstract":"We have measured the extent of hopane and sterane isomerization and of monoaromatic-steroid-hydrocarbon aromatization in a sample of hydrothermally derived petroleum from the Escanaba Trough, a sediment-covered, volcanically active ridge axis. The results, along with kinetic parameters, predict the possible time-temperature history of the petrolum-forming process for this sample. The extent of these reactions is consistent with petroleum formation by intense heating (about 300–350°C) if the time period of this heating was as short as about 100 yr. Such a time scale is reasonable for hydrothermal-discharge events associated with ridge-crest volcanism.
","language":"English","publisher":"Elsevier","doi":"10.1016/0146-6380(88)90055-1","usgsCitation":"Kvenvolden, K.A., Rapp, J., Hostettler, F.D., David, J., and Claypool, G., 1988, Organic geothermometry of petroleum from Escanaba Trough, offshore northern California: Organic Geochemistry, v. 13, no. 1-3, p. 351-355, https://doi.org/10.1016/0146-6380(88)90055-1.","productDescription":"5 p.","startPage":"351","endPage":"355","costCenters":[],"links":[{"id":220140,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Escanaba Trough, offshore northern California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -126.03302571989019,\n 41.99411164056443\n ],\n [\n -126.03302571989019,\n 40.815938197331036\n ],\n [\n -124.08714811107552,\n 40.815938197331036\n ],\n [\n -124.08714811107552,\n 41.99411164056443\n ],\n [\n -126.03302571989019,\n 41.99411164056443\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"13","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6fc2e4b0c8380cd75c56","contributors":{"authors":[{"text":"Kvenvolden, Keith A. kkvenvolden@usgs.gov","contributorId":3384,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"Keith","email":"kkvenvolden@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":365884,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rapp, John B.","contributorId":32028,"corporation":false,"usgs":true,"family":"Rapp","given":"John B.","affiliations":[],"preferred":false,"id":365882,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hostettler, Frances D. fdhostet@usgs.gov","contributorId":3383,"corporation":false,"usgs":true,"family":"Hostettler","given":"Frances","email":"fdhostet@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":365885,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"David, J.","contributorId":60915,"corporation":false,"usgs":true,"family":"David","given":"J.","email":"","affiliations":[],"preferred":false,"id":365883,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Claypool, George E.","contributorId":8475,"corporation":false,"usgs":true,"family":"Claypool","given":"George E.","affiliations":[],"preferred":false,"id":365881,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":94168,"text":"94168 - 1988 - Longevity of rainbow trout antibody-producing cells after in vitro immunization culture","interactions":[],"lastModifiedDate":"2012-02-02T00:03:59","indexId":"94168","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Longevity of rainbow trout antibody-producing cells after in vitro immunization culture","docAbstract":"No abstract available at this time","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Invertebrate and Fish Tissue Culture","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"Japan Scientific Societies Press; Springer-Verlag","publisherLocation":"Tokyo, Japan; Berlin, Germany","collaboration":"88-048/FH","usgsCitation":"Dixon, O.W., Anderson, D.P., Kimenai, R., and Lizzio, E.F., 1988, Longevity of rainbow trout antibody-producing cells after in vitro immunization culture, chap. of Invertebrate and Fish Tissue Culture, p. 228-231.","productDescription":"p. 228-231","startPage":"228","endPage":"231","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":128170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63f06a","contributors":{"editors":[{"text":"Kuroda, Y.","contributorId":55762,"corporation":false,"usgs":true,"family":"Kuroda","given":"Y.","email":"","affiliations":[],"preferred":false,"id":505241,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Kurstak, E.","contributorId":113556,"corporation":false,"usgs":true,"family":"Kurstak","given":"E.","email":"","affiliations":[],"preferred":false,"id":505243,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Maramorosch, K.","contributorId":64587,"corporation":false,"usgs":true,"family":"Maramorosch","given":"K.","email":"","affiliations":[],"preferred":false,"id":505242,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Dixon, O. W.","contributorId":101588,"corporation":false,"usgs":true,"family":"Dixon","given":"O.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":298393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, D. P.","contributorId":32469,"corporation":false,"usgs":true,"family":"Anderson","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":298391,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kimenai, R.","contributorId":8411,"corporation":false,"usgs":true,"family":"Kimenai","given":"R.","email":"","affiliations":[],"preferred":false,"id":298390,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lizzio, E. F.","contributorId":50471,"corporation":false,"usgs":true,"family":"Lizzio","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":298392,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70137833,"text":"70137833 - 1988 - Geophysical study of a magma chamber near Mussau Island, Papua New Guinea","interactions":[],"lastModifiedDate":"2015-01-13T10:10:37","indexId":"70137833","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"title":"Geophysical study of a magma chamber near Mussau Island, Papua New Guinea","docAbstract":"Analysis of a 24-channel seismic-reflection data collected near Mussau Island, Papua New Guinea, shows a high-amplitude, negative-polarity reflection that we believe is from the top of a magma chamber. The reflecting horizon lies at a depth of about 4.4 s subbottom and can be traced laterally for 2.6 km. On shot gathers, the reflection demonstrates normal moveout appropriate for an in-place event. The frequency spectrum of the reflection shows a decrease in high-frequency content when compared to the sea floor reflection, as would be expected for a deep subsurface event. The polarity of the reflection event is negative, suggesting that the reflection horizon is the top of a low-velocity zone. Magnetic data indicate that the ridge containing the reflecting horizon is magnetic, and the geology of Massau Island suggests that the ridge is volcanic in its origin. We speculate that the high-amplitude reflection is from the top of a magma chamber some 7-11 km deep.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geology and offshore resources of Pacific Island Arcs: New Ireland and Manus Region, Papa New Guinea","language":"English","publisher":"Circum-Pacific Council for Energy and Mineral Resources","usgsCitation":"Dadisman, S.V., and Marlow, M.S., 1988, Geophysical study of a magma chamber near Mussau Island, Papua New Guinea, chap. of Geology and offshore resources of Pacific Island Arcs: New Ireland and Manus Region, Papa New Guinea, v. 9, p. 211-219.","productDescription":"9 p.","startPage":"211","endPage":"219","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":297161,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":297160,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://archives.datapages.com/data/circ_pac/0010/0211_f.htm"}],"country":"Papa New Guinea","otherGeospatial":"Mussau Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 149.3865966796875,\n -1.2193903597622147\n ],\n [\n 150.09521484375,\n -1.263325357489324\n ],\n [\n 150.09521484375,\n -1.7794990011582128\n ],\n [\n 149.3646240234375,\n -1.763027383113869\n ],\n [\n 149.3865966796875,\n -1.2193903597622147\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2bb2e4b08de9379b348b","contributors":{"authors":[{"text":"Dadisman, Shawn V. sdadisman@usgs.gov","contributorId":2207,"corporation":false,"usgs":true,"family":"Dadisman","given":"Shawn","email":"sdadisman@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":true,"id":538127,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marlow, M. S.","contributorId":76743,"corporation":false,"usgs":true,"family":"Marlow","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":538128,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70184466,"text":"70184466 - 1988 - Survival of aluminum and monel bands on black brant","interactions":[],"lastModifiedDate":"2017-03-09T15:10:33","indexId":"70184466","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2881,"text":"North American Bird Bander","active":true,"publicationSubtype":{"id":10}},"title":"Survival of aluminum and monel bands on black brant","docAbstract":"Three recoveries of Black Brant (Branta bernicla nigricans) were recently reported in the \"Significant Encounters\" section of North American Bird Bander (Anon. 1986). At the time of recovery these Brant were 21.5, 22 and at least 22.5 years old. The significance of these recoveries caught my attention as all were of birds banded on the Yukon Delta, Alaska in 1963 by the Alaska Department of Fish and Game. In that year bands made of monel metal, a corrosion-resistant alloy consisting mainly of nickel and copper, were used for the first time in anticipation that they would survive significantly longer than standard aluminum bands in the estuarine and marine habitats used by Brant. Follow-up studies of the experimental banding were conducted by the Yukon Delta National Wildlife Refuge of which I was manager from 1964-1975.
","language":"English","publisher":"Western, Inland, and Eastern Bird Banding Associations","usgsCitation":"Lensink, C.J., 1988, Survival of aluminum and monel bands on black brant: North American Bird Bander, v. 13, no. 2, p. 33-35.","productDescription":"3 p.","startPage":"33","endPage":"35","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337253,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":337248,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.westernbirdbanding.org/publications_NABB.html","text":"Journal's Website"}],"volume":"13","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c277f9e4b014cc3a3e7706","contributors":{"authors":[{"text":"Lensink, Calvin J.","contributorId":99612,"corporation":false,"usgs":false,"family":"Lensink","given":"Calvin","email":"","middleInitial":"J.","affiliations":[{"id":33810,"text":"National Wildlife Refuge Association","active":true,"usgs":false}],"preferred":false,"id":681626,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1001272,"text":"1001272 - 1988 - Ingestion of lead shot and aluminum bands by bald eagles during winter in Nebraska","interactions":[],"lastModifiedDate":"2018-01-02T12:51:35","indexId":"1001272","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","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":"Ingestion of lead shot and aluminum bands by bald eagles during winter in Nebraska","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wilson Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Lingle, G., and Krapu, G., 1988, Ingestion of lead shot and aluminum bands by bald eagles during winter in Nebraska: The Wilson Bulletin, v. 100, no. 2, p. 326-327.","productDescription":"2 p.","startPage":"326","endPage":"327","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"100","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee4ab","contributors":{"authors":[{"text":"Lingle, G.R.","contributorId":26648,"corporation":false,"usgs":true,"family":"Lingle","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":310779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krapu, Gary L.","contributorId":56994,"corporation":false,"usgs":true,"family":"Krapu","given":"Gary L.","affiliations":[],"preferred":false,"id":310780,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1000543,"text":"1000543 - 1988 - Comparative biology of the sculpins of Lake Superior","interactions":[],"lastModifiedDate":"2016-03-24T15:31:40","indexId":"1000543","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","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":"Comparative biology of the sculpins of Lake Superior","docAbstract":"The slimy sculpin (Cottus cognatus), spoonhead sculpin (Cottus ricei), and deepwater sculpin (Myoxocephalus thompsoni) are abundant fishes in Lake Superior. Slimy and spoonhead sculpins occupy a zone from near shore to depths of 210 m but are generally most abundant in waters 50 to 90 m deep. Deepwater sculpins are found in waters from 15 to 407 m deep and are most abundant at depths greater than 70 m. All three species of sculpins eat mainly burrowing amphipods (Pontoporeia affinis) although deepwater sculpins also eat substantial quantities of opossum shrimp (Mysis relicta). The three sculpins grow at similar rates. Among the fishes aged, the maximum age of slimy sculpins was 5 years, compared with 6 years for spoonhead sculpins, and 7 years for deepwater sculpins. Indirect evidence indicates that slimy and spoonhead sculpins spawn in the spring, and deepwater sculpins spawn in midwinter.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(88)71531-2","usgsCitation":"Selgeby, J.H., 1988, Comparative biology of the sculpins of Lake Superior: Journal of Great Lakes Research, v. 14, no. 1, p. 44-51, https://doi.org/10.1016/S0380-1330(88)71531-2.","productDescription":"8 p.","startPage":"44","endPage":"51","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae563","contributors":{"authors":[{"text":"Selgeby, James H.","contributorId":89828,"corporation":false,"usgs":true,"family":"Selgeby","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308738,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000542,"text":"1000542 - 1988 - Use of aerial photography to inventory aquatic vegetation","interactions":[],"lastModifiedDate":"2016-03-21T14:31:39","indexId":"1000542","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2146,"text":"Journal of Aerospace Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Use of aerial photography to inventory aquatic vegetation","docAbstract":"This study demonstrates the feasibility of using low-altitude aerial photography to inventory submersed macrophytes in the connecting channels of the Great Lakes. For this purpose, we obtained aerial color transparencies and collateral ground truth information about submersed vegetation at 160 stations within four study sites in the St. Clair and Detroit rivers, September 17 to October 4, 1984. Photographs were interpreted by five test subjects to determine with what accuracy they could detect beds of submersed macrophytes, and the precision of delineating the extent of such vegetation beds. The interpreters correctly determined the presence or absence of vegetation 80% of the time (range 73-86%). Differences between individuals were statistically significant. Determination of the presence or absence of macrophytes depended partly on their relative abundance and water clarity. Analysis of one photograph from each of the four study sites revealed that photointerpreters delineated between 35 and 75 ha of river bottom covered by vegetation. This wide range indicates that individuals should be tested to assess their relative capability and be trained before they are employed to delineate plant beds in large-scale inventories. Within limits, low-altitude aerial photography, combined with collateral ground truth information, can be used to determine the presence or absence and delineate the extent of submersed macrophytes in connecting channels of the Great Lakes.
","language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0893-1321(1988)1:3(142)","usgsCitation":"Schloesser, D.W., Brown, C.L., and Manny, B.A., 1988, Use of aerial photography to inventory aquatic vegetation: Journal of Aerospace Engineering, v. 1, no. 3, p. 142-150, https://doi.org/10.1061/(ASCE)0893-1321(1988)1:3(142).","productDescription":"9 p.","startPage":"142","endPage":"150","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133254,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ff7","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":308735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Charles L.","contributorId":102421,"corporation":false,"usgs":true,"family":"Brown","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308737,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Manny, Bruce A. 0000-0002-4074-9329 bmanny@usgs.gov","orcid":"https://orcid.org/0000-0002-4074-9329","contributorId":3699,"corporation":false,"usgs":true,"family":"Manny","given":"Bruce","email":"bmanny@usgs.gov","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":308736,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1000544,"text":"1000544 - 1988 - Acute toxicity of Daphnia pulex to six classes of chemical compounds potentially hazardous to Great Lakes aquatic biota","interactions":[],"lastModifiedDate":"2013-02-04T09:25:55","indexId":"1000544","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","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":"Acute toxicity of Daphnia pulex to six classes of chemical compounds potentially hazardous to Great Lakes aquatic biota","docAbstract":"Of the six classes of chemicals potentially hazardous to Great Lakes aquatic biota, derivatives of polyaromatic hydrocarbons (PAHs) were the most acutely toxic (48-h EC 50) to Daphnia pulex. The other classes, listed in order of decreasing toxicity were alkyl halides, nitrogen-containing compounds, cyclic alkanes, heterocyclic nitrogen compounds, silicon-containing compounds. O f the 41 compounds representing the six chemical classes, 6 were extremely toxic (> 0.01 - 0.1 mg/L), 11 highly toxic (> 01. - 1.0 mg/L), 20 moderately toxic (> 1.0 - 10.0 mg/L), and 4 slightly toxic (>10 - 100 mg/L). The reference compound, p, p'DDT, was super toxic (< 0.01 mg/L). Based on toxicity and relative abundance (hazard ranking) of the 21 compounds that were detected in tissue of Great Lakes fishes, the classes of compounds that present the greatest threat to Great Lakes aquatic biota are PAH derivatives, alkyl halides, and cyclic aklanes.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Great Lakes Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/S0380-1330(88)71572-5","usgsCitation":"Smith, S.B., Savino, J.F., and Blouin, M.A., 1988, Acute toxicity of Daphnia pulex to six classes of chemical compounds potentially hazardous to Great Lakes aquatic biota: Journal of Great Lakes Research, v. 14, no. 4, p. 394-404, https://doi.org/10.1016/S0380-1330(88)71572-5.","productDescription":"11 p.","startPage":"394","endPage":"404","numberOfPages":"11","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":266714,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0380-1330(88)71572-5"},{"id":133504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c0a","contributors":{"authors":[{"text":"Smith, Stephen B.","contributorId":14765,"corporation":false,"usgs":true,"family":"Smith","given":"Stephen","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":308741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Savino, Jacqueline F. jsavino@usgs.gov","contributorId":2213,"corporation":false,"usgs":true,"family":"Savino","given":"Jacqueline","email":"jsavino@usgs.gov","middleInitial":"F.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":308739,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blouin, Marc A. mblouin@usgs.gov","contributorId":4670,"corporation":false,"usgs":true,"family":"Blouin","given":"Marc","email":"mblouin@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":308740,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}