No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrPA872","usgsCitation":"Loper, W., Behrendt, T., and Schaffstall, W., 1988, Water resources data for Pennsylvania, water year 1987. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Loper, W.C.","contributorId":49853,"corporation":false,"usgs":true,"family":"Loper","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":789717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Behrendt, T.E.","contributorId":27887,"corporation":false,"usgs":true,"family":"Behrendt","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":789718,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schaffstall, W.P.","contributorId":20010,"corporation":false,"usgs":true,"family":"Schaffstall","given":"W.P.","affiliations":[],"preferred":false,"id":789719,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70006561,"text":"70006561 - 1988 - Linear solvation energy relationships for toxicity of selected organic chemicals to Daphnia pulex and Daphnia magna","interactions":[],"lastModifiedDate":"2014-06-30T13:19:54","indexId":"70006561","displayToPublicDate":"1988-05-22T13:13:00","publicationYear":"1988","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"seriesTitle":{"id":443,"text":"Proceedings of the QSAR","active":false,"publicationSubtype":{"id":12}},"title":"Linear solvation energy relationships for toxicity of selected organic chemicals to Daphnia pulex and Daphnia magna","docAbstract":"In the Laurentian Great Lakes, more than 300 contaminants have been identified in fish, other biota, water, and sediment. Current hazard assessment of these chemicals by the National Fisheries Research Center-Great Lakes is based on their toxicity, occurrence in the environment, and source. Although scientists at the Center have tested over 70 chemicals with the crustacean Daphnia pulex, the number of experimental data needed to screen the huge array of chemicals in the Great Lakes exceeds the practical capabilities of conducting bioassays. This limitation can be partly circumvented, however, by using mathematical models based on quantitative structure-activity relationships (QSAR) to provide rapid, inexpensive estimates of toxicity. Many properties of chemicals, including toxicity, bioaccumulation and water solubility are well correlated and can be predicted by equations of the generalized linear solvation energy relationships (LSER). The equation we used to model solute toxicity is Toxicity = constant + mVI/100 + s (π* + dδ) + bβm + aαm where VI = intrinsic (Van der Waals) molar volume; π* = molecular dipolarity/polarizability; δ = polarizability 'correction term'; βm = solute hydrogen bond acceptor basicity; and αm = solute hydrogen bond donor acidity. The subscript m designates solute monomer values for α and β. We applied the LSER model to 48-h acute toxicity data (measured as immobilization) for six classes of chemicals detected in Great Lakes fish. The following regression was obtained for Daphnia pulex (concentration = μM): log EC50 = 4.86 - 4.35 VI/100; N = 38, r2 = 0.867, sd = 0.403 We also used the LSER modeling approach to analyze to a large published data set of 24-h acute toxicity for Daphnia magna; the following regression resulted, for eight classes of compounds (concentration = mM): log EC50 = 3.88 - 4.52 VI/100 - 1.62 π* + 1.66 βm - 0.916 αm; N = 62, r2 = 0.859, sd = 0.375 In addition we developed computer software that identifies chemical structures, estimates the LSER parameters, and predicts toxicity. The LSER models promise to be effective in differentiating between reactive and nonreactive toxicity behavior where other models have failed. Contaminants with reactive behavior are generally the most toxic and rank highest in hazard assessment of environmental chemicals.
","largerWorkTitle":"Proceedings of the QSAR: third international workshop on quantitative structure-activity relationships in environmental toxicology","conferenceTitle":"Proceedings of the QSAR: third international workshop on quantitative structure-activity relationships in environmental toxicology","conferenceDate":"1988-05-21T00:00:00","conferenceLocation":"Knoxville, TN","language":"English","publisher":"National Technical Information Service","publisherLocation":"Springfield, VA","usgsCitation":"Passino, D., Hickey, J.P., and Frank, A.M., 1988, Linear solvation energy relationships for toxicity of selected organic chemicals to Daphnia pulex and Daphnia magna: Proceedings of the QSAR, p. 131-146.","productDescription":"p. 131-146","numberOfPages":"16","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":289226,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"The Great Lakes","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.11,41.4 ], [ -92.11,48.85 ], [ -76.3,48.85 ], [ -76.3,41.4 ], [ -92.11,41.4 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53b286f5e4b07b8813a554d0","contributors":{"authors":[{"text":"Passino, Dora R. M.","contributorId":29345,"corporation":false,"usgs":true,"family":"Passino","given":"Dora R. M.","affiliations":[],"preferred":false,"id":354766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hickey, James P.","contributorId":83460,"corporation":false,"usgs":true,"family":"Hickey","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":354767,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frank, Anthony M.","contributorId":28922,"corporation":false,"usgs":true,"family":"Frank","given":"Anthony","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":354765,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185537,"text":"70185537 - 1988 - Arsenic in ground water of the Western United States","interactions":[],"lastModifiedDate":"2022-10-17T15:24:34.439165","indexId":"70185537","displayToPublicDate":"1988-05-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Arsenic in ground water of the Western United States","docAbstract":"Natural occurrences of ground water with moderate (10 to 50 micrograms per liter) to high (greater than 50 micrograms per liter) concentrations of arsenic are common throughout much of the Western United States. High concentrations of arsenic are generally associated with one of four geochemical environments: (1) basin-fill deposits of alluvial-lacustrine origin, particularly in semiarid areas, (2) volcanic deposits, (3) geothermal systems, and (4) uranium and gold-mining areas. These findings are based on an extensive literature review, compilation of unpublished reports and data, and the review of data bases containing more than 7,000 analyses of ground-water samples for arsenic. In the first two environments, arsenic appears to be associated with sediments derived, in part, from volcanic rocks of intermediate to acidic composition. Dissolved arsenic concentrations in water from volcanic aquifers in the same regions, however, may be low (less than 10 micrograms per liter). Solid phases (minerals, amorphous solids, and sedimentary organic matter) that supply the dissolved arsenic have not been identified in most areas. Alluvial and lacustrine sedimentary deposits appear to be an important source of arsenic in volcanic areas (such as Lane County, Oregon) and in areas underlain by basin-fill deposits (such as Carson Desert in Nevada and the Tulare Lake basin in California). Mobilization of arsenic in sedimentary aquifers may be, in part, a result of changes in the geochemical environment due to agricultural irrigation. In the deeper subsurface, elevated arsenic concentrations are associated with compaction caused by groundwater withdrawals.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1988.tb00397.x","usgsCitation":"Welch, A., Lico, M.S., and Hughes, J.L., 1988, Arsenic in ground water of the Western United States: Groundwater, v. 26, no. 3, p. 333-347, https://doi.org/10.1111/j.1745-6584.1988.tb00397.x.","productDescription":"15 p.","startPage":"333","endPage":"347","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338182,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Western United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -125.41992187499999,\n 31.353636941500987\n ],\n [\n -104.4140625,\n 31.353636941500987\n ],\n [\n -104.4140625,\n 49.38237278700955\n ],\n [\n -125.41992187499999,\n 49.38237278700955\n ],\n [\n -125.41992187499999,\n 31.353636941500987\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"26","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-03-21","publicationStatus":"PW","scienceBaseUri":"58d4df09e4b05ec79911d1ce","contributors":{"authors":[{"text":"Welch, Alan H.","contributorId":45286,"corporation":false,"usgs":true,"family":"Welch","given":"Alan H.","affiliations":[],"preferred":false,"id":685902,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lico, Michael S.","contributorId":75897,"corporation":false,"usgs":true,"family":"Lico","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":685903,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hughes, Jennifer L.","contributorId":189740,"corporation":false,"usgs":false,"family":"Hughes","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":685904,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1013383,"text":"1013383 - 1988 - Channel hydraulics, habitat use, and body form of juvenile coho salmon, steelhead, and cutthroat trout in streams","interactions":[],"lastModifiedDate":"2026-04-08T16:24:24.536855","indexId":"1013383","displayToPublicDate":"1988-05-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Channel hydraulics, habitat use, and body form of juvenile coho salmon, steelhead, and cutthroat trout in streams","docAbstract":"Habitat use by juvenile coho salmon Oncorhynchus kisutch, steelhead Salmo gairdneri, and the coastal subspecies of cutthroat trout Salmo clarki clarki in small streams in western Washington was influenced by hydraulic characteristics of different types of channel units. Coho salmon preferred pools with average velocities less than 20 cm/s; very few fish were found in riffles with high current velocities. Steelhead occurred in riffles and also utilized deep pools with relatively high velocities along the center of the channel. Cutthroat trout were intermediate between coho salmon and steelhead in their use of swiftly flowing habitats. Variation in body shape and fin size among the three species generally fit the predicted morphologies that would be favored in different locations within the channel. Coho salmon possessed a deep, laterally compressed body with large median and paired fins. These features are believed to facilitate rapid turns and quick but transient burst swimming. Steelhead possessed a more cylindrical body shape with short median fins and relatively large paired fins, attributes that appear well adapted to holding a position in swift water. The cutthroat troutˈs lack of morphological adaptation to either fast or slow water may help to explain why this species is dominated by coho salmon and steelhead in areas of sympatry.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1988)117<0262:CHHUAB>2.3.CO;2","usgsCitation":"Bisson, P., Sullivan, K., and Nielsen, J., 1988, Channel hydraulics, habitat use, and body form of juvenile coho salmon, steelhead, and cutthroat trout in streams: Transactions of the American Fisheries Society, v. 117, no. 3, p. 262-273, https://doi.org/10.1577/1548-8659(1988)117<0262:CHHUAB>2.3.CO;2.","productDescription":"12 p.","startPage":"262","endPage":"273","costCenters":[{"id":106,"text":"Alaska Biological Science Center","active":false,"usgs":true}],"links":[{"id":131241,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"117","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e628c","contributors":{"authors":[{"text":"Bisson, P.A.","contributorId":17944,"corporation":false,"usgs":true,"family":"Bisson","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":318628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sullivan, K.","contributorId":74342,"corporation":false,"usgs":true,"family":"Sullivan","given":"K.","email":"","affiliations":[],"preferred":false,"id":318629,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nielsen, J.L.","contributorId":105665,"corporation":false,"usgs":true,"family":"Nielsen","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":318630,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5220774,"text":"5220774 - 1988 - Survival of juvenile ring-necked ducks on wetlands of different pH","interactions":[],"lastModifiedDate":"2024-11-22T16:48:10.36356","indexId":"5220774","displayToPublicDate":"1988-04-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Survival of juvenile ring-necked ducks on wetlands of different pH","docAbstract":"Brood and duckling survival of ring-necked ducks (Aythya collaris) was examined in relation to wetland water chemistry in eastcentral Maine during 1983-85. Daily survival rates (DSR) of broods and ducklings were determined for 381 ducklings from 64 broods by counts of each brood at 6-10-day intervals during broodrearing. Twelve of 64 females lost entire broods. Only 176 of 381 (46%) ducklings survived to fledge. Brood survival for the 45-day rearing period was 0.7731; duckling survival was 0.3707. Young ducklings (≤24 days) survived at a lower rate (0.9750/day) than older (≥25 days) ducklings (0.9818/day) (P = 0.002). Survival rates of broods and ducklings did not differ among wetlands of high and low alkalinities. Brood survival did not differ among wetlands of different pH, but DSR of ducklings was lower (0.9763/day) on low-pH (<6.0) wetlands than on high-pH (≥6.1) wetlands (0.9816/day) (P = 0.049). Class IIb-III (25-45 days old) ducklings from the lowest-pH wetlands(<5.5) had the lowest DSR (0.9752) while Class IIb-III ducklings from the highest-pH wetlands (>6.5) had the highest DSR (0.9856) (P = 0.009).
","language":"English","publisher":"Wiley","doi":"10.2307/3801219","usgsCitation":"McAuley, D., and Longcore, J., 1988, Survival of juvenile ring-necked ducks on wetlands of different pH: Journal of Wildlife Management, v. 52, no. 2, p. 169-176, https://doi.org/10.2307/3801219.","productDescription":"8 p.","startPage":"169","endPage":"176","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197784,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maine","county":"Hancock County, Washington County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -69.04882868494023,\n 45.77994913044307\n ],\n [\n -69.04882868494023,\n 44.26057419211864\n ],\n [\n -67.06934253029306,\n 44.26057419211864\n ],\n [\n -67.06934253029306,\n 45.77994913044307\n ],\n [\n -69.04882868494023,\n 45.77994913044307\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"52","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688183","contributors":{"authors":[{"text":"McAuley, Daniel G.","contributorId":346357,"corporation":false,"usgs":false,"family":"McAuley","given":"Daniel G.","affiliations":[{"id":37196,"text":"Retired USGS employee","active":true,"usgs":false}],"preferred":false,"id":332450,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Longcore, Jerry R.","contributorId":346356,"corporation":false,"usgs":false,"family":"Longcore","given":"Jerry R.","affiliations":[{"id":37196,"text":"Retired USGS employee","active":true,"usgs":false}],"preferred":false,"id":332451,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185533,"text":"70185533 - 1988 - Internal inconsistencies in dispersion-dominated models that incorporate chemical and microbial kinetics","interactions":[],"lastModifiedDate":"2020-01-12T13:49:53","indexId":"70185533","displayToPublicDate":"1988-04-01T00:00:00","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":"Internal inconsistencies in dispersion-dominated models that incorporate chemical and microbial kinetics","docAbstract":"Current understanding of transport processes in aquifers is limited by lack of precise point chemical concentration measurements. Recently, however, some careful measurements of vertical chemical concentration profiles have been made at several locations around the world that appear to support a consistent picture concerning the persistence of large vertical concentration gradients in aquifers and, by implication, the existence of very small vertical transverse dispersivities. These data were obtained in aquifers supporting microbial activity. Data analysis using a mathematical model which considers microbial degradation coupled to nutrient and oxygen transport indicates that a vertical transverse dispersivity on the order of 0.1 cm or less is consistent with the concentration gradients that were measured. The existence of such large gradients and low dispersivities is not consistent with the use of two-dimensional vertically averaged (areal) models as currently applied, especially if one is interested in the development of transport models with predictive capability beyond that associated with standard calibration and extrapolation. Even three-dimensional models with large vertical transverse dispersivities compared to those measured will produce results inconsistent with measurements. Microbial-chemical activity is very sensitive to concentration distributions. Smearing of the oxygen profile can result in the prediction of aerobic activity where, in fact, none exists.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR024i004p00615","usgsCitation":"Molz, F.J., and Widdowson, M.A., 1988, Internal inconsistencies in dispersion-dominated models that incorporate chemical and microbial kinetics: Water Resources Research, v. 24, no. 4, p. 615-619, https://doi.org/10.1029/WR024i004p00615.","productDescription":"5 p.","startPage":"615","endPage":"619","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338178,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d4df0ae4b05ec79911d1d2","contributors":{"authors":[{"text":"Molz, Fred J.","contributorId":189737,"corporation":false,"usgs":false,"family":"Molz","given":"Fred","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":685893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Widdowson, Mark A.","contributorId":90379,"corporation":false,"usgs":true,"family":"Widdowson","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":685894,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1014507,"text":"1014507 - 1988 - Cooperative federal-state liming research on surface waters impacted by acidic deposition","interactions":[],"lastModifiedDate":"2026-03-18T16:02:48.616166","indexId":"1014507","displayToPublicDate":"1988-03-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Cooperative federal-state liming research on surface waters impacted by acidic deposition","docAbstract":"In the eastern and north-central United States, lakes and streams with low acid neutralizing capacity are at risk from acidity. Resource management agencies are interested in developing mitigation strategies that protect or restore fisheries in these waters. Addition of limestone (calcium carbonate) to improve water quality and prevent episodic depressions of pH during precipitation events and spring runoff is one mitigation technique being used. The ecological changes that accompany such treatment of streams and lakes are being investigated in a cooperative program between the U.S. Fish and Wildlife Service and individual states. Streams in Massachusetts, West Virginia and Tennessee, and a lake in Minnesota are included in this 5-yr research program. Intensive monitoring during pre- and post-liming tracks a suite of physical, chemical and biological parameters that influence the re-establishment or maintenance of healthy fisheries. Supporting studies on liming being conducted at Adirondack lakes in New York focus on fisheries management. A model on the influence of liming on light attenuation and thermal stratification is also being developed. Management guidelines are to be generated from the program results.
The diagenesis of amino acids in sediments from Clear Lake core CL-80-1 is indicated by changes in amino acid concentrations, compositions, and stereochemistry. Concentrations of total amino acids decrease with depth, but the decrease is not systematic, possibly reflecting a nonuniformity in sedimentary and postdepositional processes affecting the amino acids. Ratios of neutral/acidic amino acids may indicate that the pH of interstitial water is slightly alkaline to slightly acidic and that the organic matter is well humified. Ratios of nonprotein/protein amino acids suggest that some changes in amino acids with depth result from microbial degradations. The extent of racemization of alanine increases with depth; the trends of these data may be explained, in part, by rapid sedimentation within the lake. Agreement between extents of alanine racemization for sediments from equivalent depths in two cores from the lake suggests that diagenetic temperatures are uniform within the sediments of the northern basin of Clear Lake.
","largerWorkTitle":"Late Quaternary Climate, Tectonism, and Sedimentation in Clear Lake, Northern California Coast Ranges","language":"English","publisher":"GSA","doi":"10.1130/SPE214-p161","usgsCitation":"Blunt, D., and Kvenvolden, K.A., 1988, Amino-acid diagenesis and its implication for late Pleistocene lacustrine sediment, Clear Lake, California : GSA Special Papers, v. 214, p. 161-170, https://doi.org/10.1130/SPE214-p161.","productDescription":"10 p.","startPage":"161","endPage":"170","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":372063,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Clear Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.99331665039062,\n 38.885688179036094\n ],\n [\n -122.57583618164062,\n 38.885688179036094\n ],\n [\n -122.57583618164062,\n 39.18277200757995\n ],\n [\n -122.99331665039062,\n 39.18277200757995\n ],\n [\n -122.99331665039062,\n 38.885688179036094\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"214","noUsgsAuthors":false,"publicationDate":"1988-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Blunt, D.J.","contributorId":93189,"corporation":false,"usgs":true,"family":"Blunt","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":781552,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":781553,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70170910,"text":"70170910 - 1988 - Minnesota District Water Resources Division: Information and technical assistance","interactions":[],"lastModifiedDate":"2018-03-12T11:58:53","indexId":"70170910","displayToPublicDate":"1988-02-03T12:45:00","publicationYear":"1988","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Minnesota District Water Resources Division: Information and technical assistance","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Agrichemicals and Ground Water Protection--Resources and Strategies for State and Local Management, Proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Agrichemicals and Ground Water Protection--Resources and Strategies for State and Local Management","conferenceDate":"October 24-25, 1988","conferenceLocation":"St. Paul, MN","language":"English","publisherLocation":"St. Paul, MN","usgsCitation":"Herb, W., 1988, Minnesota District Water Resources Division: Information and technical assistance, in Agrichemicals and Ground Water Protection--Resources and Strategies for State and Local Management, Proceedings, St. Paul, MN, October 24-25, 1988, p. 93-97.","productDescription":"5 p.","startPage":"93","endPage":"97","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321085,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57330633e4b0dae0d5dcd1ff","contributors":{"authors":[{"text":"Herb, W.J.","contributorId":16847,"corporation":false,"usgs":true,"family":"Herb","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":629049,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039261,"text":"70039261 - 1988 - NCIC state affiliates","interactions":[],"lastModifiedDate":"2012-08-04T01:01:57","indexId":"70039261","displayToPublicDate":"1988-02-01T14:51:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"NCIC state affiliates","docAbstract":"In 1974, the U.S. Geological Survey, Department of the Interior, established the National Cartographic Information Center (NCIC) to serve as the public's primary source for information concerning the availability of cartographic, geographic,and remotely sensed data. As part of its program of providing information to the public, NCIC began in 1976 to develop a network of State affiliated offices to provide local access to this information.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039261","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, NCIC state affiliates: General Information Product, 2 p., https://doi.org/10.3133/70039261.","productDescription":"2 p.","numberOfPages":"2","costCenters":[{"id":409,"text":"National Cartographic Information Center","active":false,"usgs":true}],"links":[{"id":261502,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039261/report.pdf"},{"id":261503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039261/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a613be4b0c8380cd7186c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535274,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207902,"text":"70207902 - 1988 - Voluminous submarine lava flows from Hawaiian volcanoes ","interactions":[],"lastModifiedDate":"2020-01-20T06:18:23","indexId":"70207902","displayToPublicDate":"1988-01-17T13:09:52","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Voluminous submarine lava flows from Hawaiian volcanoes ","docAbstract":"The GLORIA long-range sonar imaging system has revealed fields of large lava flows in the Hawaiian Trough east and south of Hawaii in water as deep as 5.5 km. Flows in the most extensive field (110 km long) have erupted from the deep submarine segment of Kilauea's east rift zone. Other flows have been erupted from Loihi and Mauna Loa. This discovery confirms a suspicion, long held from subaerial studies, that voluminous submarine flows are erupted from Hawaiian volcanoes, and it supports an inference that summit calderas repeatedly collapse and fill at intervals of centuries to millenia owing to voluminous eruptions. These extensive flows differ greatly in form from pillow lavas found previously along shallower segments of the rift zones; therefore, revision of concepts of volcano stratigraphy and structure may be required.
","language":"English","publisher":"GSA","doi":"10.1130/0091-7613(1988)016<0400:VSLFFH>2.3.CO;2","usgsCitation":"Holcomb, R.T., Moore, J.G., Lipman, P.W., and Belderson, R., 1988, Voluminous submarine lava flows from Hawaiian volcanoes : Geology, v. 16, no. 5, p. 400-404, https://doi.org/10.1130/0091-7613(1988)016<0400:VSLFFH>2.3.CO;2.","productDescription":"5 p.","startPage":"400","endPage":"404","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":371357,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Hawaiian volcanoes","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -156.77490234375,\n 18.70869162255995\n ],\n [\n -154.44580078125,\n 18.70869162255995\n ],\n [\n -154.44580078125,\n 21.06399706324597\n ],\n [\n -156.77490234375,\n 21.06399706324597\n ],\n [\n -156.77490234375,\n 18.70869162255995\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"16","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Holcomb, Robin T.","contributorId":46938,"corporation":false,"usgs":true,"family":"Holcomb","given":"Robin","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":779698,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, James G. 0000-0002-7543-2401 jmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-7543-2401","contributorId":2892,"corporation":false,"usgs":true,"family":"Moore","given":"James","email":"jmoore@usgs.gov","middleInitial":"G.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":779699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":779700,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Belderson, R.H.","contributorId":221677,"corporation":false,"usgs":false,"family":"Belderson","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":779701,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70207840,"text":"70207840 - 1988 - Friction of ice","interactions":[],"lastModifiedDate":"2020-07-07T15:27:24.128613","indexId":"70207840","displayToPublicDate":"1988-01-15T13:16:59","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Friction of ice","docAbstract":"The frictional strength of ice seems to be well below that for all other rocks. Triaxial testing of cylinders of pure water ice containing a 45° inclined sawcut, at temperatures of 77 ≤ T ≤ 115 K and confining pressures 0.1 ≤ P ≤ 250 MPa, reveals the frictional laws τ = 0.20 σn + 8.3 MPa for P ≥ 10 MPa and τ = 0.55 σn + 1.0 MPa for P ≤ 5 MPa, where τ and σn are the shear and normal stresses on the sawcut surface. Friction is independent of T and, over the one order of magnitude tested, of average sliding velocity. The sliding behavior is invariably stick slip. Examination of sliding surfaces shows only minor gouge development. A curious arrangement of densely packed short vertical fractures occurs primarily in samples with anomalously low strength. These results apply to models of near‐surface tectonic activity on Jupiter's three large icy moons, Europa, Callisto, and Ganymede. They indicate, for example, that a global expansion on Ganymede of 3 linear percent will cause extensional movement on preexisting faults at depths to 7±3 km.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB093iB07p07625","usgsCitation":"Beeman, M.L., Durham, W., and Kirby, S.H., 1988, Friction of ice: Journal of Geophysical Research B: Solid Earth, v. 93, no. B7, p. 7625-7633, https://doi.org/10.1029/JB093iB07p07625.","productDescription":"9 p.","startPage":"7625","endPage":"7633","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":371268,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"93","issue":"B7","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Beeman, M. L.","contributorId":101392,"corporation":false,"usgs":true,"family":"Beeman","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":779491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Durham, W.B.","contributorId":72135,"corporation":false,"usgs":true,"family":"Durham","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":779492,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kirby, Stephen H. 0000-0003-1636-4688 skirby@usgs.gov","orcid":"https://orcid.org/0000-0003-1636-4688","contributorId":2752,"corporation":false,"usgs":true,"family":"Kirby","given":"Stephen","email":"skirby@usgs.gov","middleInitial":"H.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":779493,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70207747,"text":"70207747 - 1988 - Pyrite formation in the Lower Cretaceous Mowry Shale: Effect of organic matter type and reactive iron content","interactions":[],"lastModifiedDate":"2020-06-18T15:41:02.501163","indexId":"70207747","displayToPublicDate":"1988-01-09T11:15:54","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Pyrite formation in the Lower Cretaceous Mowry Shale: Effect of organic matter type and reactive iron content","docAbstract":"Geochemical analysis of the Lower Cretaceous Mowry Shale in Wyoming and Montana shows that organic matter type and reactive iron content limited pyrite formation during early diagenesis. Consequently, direct interpretation of paleosalinity cannot be made from a carbon/sulfur plot. Mowry Shale samples with hydrogen index (HI) less than 150 (mg hydrocarbon/ organic carbon) contain low amounts of sulfur. In these samples, bacterial reduction of sulfate may have been inhabited by low nutritive content of the organic matter. For Mowry samples with HI greater than 150 there is a range of sulfur values and a positive correlation between iron and sulfur. The iron sulfur regression is approximately parallel to the stoichiometric pyrite line and intersects the iron axis at 0.5 percent. On average, 60 percent of the iron present was nonreactive; the remaining iron reacted with sulfide to form pyrite. For samples with HI greater than 150, pyrite formation was limited by sulfide or organic carbon content but by reactive iron content. In one modern setting, where salinity is greater than one-half normal seawater, sulfate content does not limit pyrite formation (Berner and Raiswell, 1984). From this analysis then, it can be estimated that the Mowry Sea was not a fresh water body but was either of normal marine salinity or contained brackish water with greater than one-half normal salinity.
","language":"English","publisher":"Kline Geology Laboratory","doi":"10.2475/ajs.288.9.873","usgsCitation":"Davis, H.R., Byers, C.W., and Dean, W.E., 1988, Pyrite formation in the Lower Cretaceous Mowry Shale: Effect of organic matter type and reactive iron content: American Journal of Science, v. 288, p. 873-890, https://doi.org/10.2475/ajs.288.9.873.","productDescription":"18 p.","startPage":"873","endPage":"890","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":479990,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2475/ajs.288.9.873","text":"Publisher Index Page"},{"id":371106,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Mowry 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\"}}]}","volume":"288","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Davis, Hugh R.","contributorId":221617,"corporation":false,"usgs":false,"family":"Davis","given":"Hugh","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":779172,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Byers, Charles W.","contributorId":221618,"corporation":false,"usgs":false,"family":"Byers","given":"Charles","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":779173,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":779174,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":15379,"text":"ofr88464 - 1988 - Direct-current resistivity data from 94 sites in northeastern Palm Beach County, Florida","interactions":[],"lastModifiedDate":"2022-01-05T12:25:59.881854","indexId":"ofr88464","displayToPublicDate":"1988-01-03T22:05:00","publicationYear":"1988","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":"88-464","title":"Direct-current resistivity data from 94 sites in northeastern Palm Beach County, Florida","docAbstract":"Direct-current resistivity data were collected from 94 vertical electric sounding profiles in northeastern Palm Beach County, Florida. Direct-current resistivity data, which may be used to determine the location and thicknesses of shallow, semipermeable marls or locate zones of high chloride concentration, are presented in this report. The resistivity data consist of field data, smoothed data, layer resistivity from smoothed data, and Cartesian graphs of resistivity in relation to depth for 94 sites located in northeastern Palm Beach County. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr88464","usgsCitation":"Peterson, C.J., 1988, Direct-current resistivity data from 94 sites in northeastern Palm Beach County, Florida: U.S. Geological Survey Open-File Report 88-464, iv, 101 p., https://doi.org/10.3133/ofr88464.","productDescription":"iv, 101 p.","numberOfPages":"101","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":147550,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0464/report-thumb.jpg"},{"id":44278,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0464/ofr88464.pdf","text":"Report","size":"1.43 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 88-464"}],"country":"United States","state":"Florida","county":"Palm Beach County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.496826171875,\n 26.31311263768267\n ],\n [\n -79.8486328125,\n 26.31311263768267\n ],\n [\n -79.8486328125,\n 27.039556602163195\n ],\n [\n -80.496826171875,\n 27.039556602163195\n ],\n [\n -80.496826171875,\n 26.31311263768267\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Total water withdrawn for use in Florida for 1985, in million gal/day, was 17,057 of which 6,259, or nearly 37%, was freshwater and 10,798 was saline. The majority of freshwater withdrawn was groundwater (64%) and the majority of saline water withdrawn was surface water (99%). Thermoelectric power generation accounted for more than 99% of saline water withdrawals. Agricultural irrigation accounted for the majority of freshwater withdrawals for both groundwater (41%) and surface water (60%) in 1985.
Between 1975-85, Florida 's population increased by nearly 3 million people; tourism increased by nearly 13 million visitors; irrigated agricultural acreage increased by 70,000; freshwater used to support those activities increased by almost 388 million gal/day (excluding fresh surface-water withdrawals for thermoelectric power generation); and fresh groundwater withdrawals increased 718 million gal/day. Groundwater accounted for 64% of Florida 's total freshwater use , up from 51% in 1980 and 48% in 1975.
Florida ranked sixth in the Nation in groundwater withdrawals for 1985 with more than 4 ,000 million gal/day withdrawn. Groundwater is the primary source of freshwater in Florida because it is readily available and generally is suitable for most uses. The Floridan aquifer system, which underlies the entire State, supplied the majority (62%) of groundwater in Florida for 1985. In contrast to groundwater, withdrawals of surface water declined between 1975-85. (USGS)
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri884103","collaboration":"Prepared in cooperation with the Florida Department of Environmental Regulation, Northwest Florida Water Management District, St. Johns River Water Management District, South Florida Water Management District, Southwest Florida Water Management District, and Suwannee River Water Management District","usgsCitation":"Marella, R.L., 1988, Water withdrawals, use, and trends in Florida, 1985: U.S. Geological Survey Water-Resources Investigations Report 88-4103, iv, 43 p., https://doi.org/10.3133/wri884103.","productDescription":"iv, 43 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":57396,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4103/wri884103.pdf","text":"Report","size":"2.50 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\"}}]}","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
This study is part of a continued effort to assess the effects of urban stormwater recharge on the water quality of the Biscayne aquifer in southeast Florida. In this report, the water-quality effects on shallow ground water resulting from stormwater disposal by exfiltration trench and grassy swale were investigated at two small commercial areas in Dade County, Florida. One study area (airport) was located near the Miami International Airport and had a drainage area of about 10 acres overlying a sandy soil; the other study area (free zone) was located at the Miami International Free Trade Zone and had a drainage area of about 20 acres overlying limestone. The monitoring design for each study area consisted of seven sites and included water-quality sampling of the stormwater in the catch basin of the exfiltration trench, ground water from two wells 1 foot from the trench (trench wells), two wells 20 feet from the trench, and ground water from two wells at the swale from April 1985 through May 1986. Eleven water-quality variables (target variables) commonly found in high levels in urban stormwater runoff were used as tracers to estimate possible changes in ground-water quality that may have been caused by stormwater recharge.
Comparison of the distribution of target variables indicated that the concentrations tended to be greater in the stormwater in the exfiltration trench than in water from the two wells 1 foot from the trench at both study areas. The concentration difference for several target variables was statistically significant at the 5-percent level. Lead, for example, had median concentrations of 23 and 4 micrograms per liter, respectively, in stormwater and water from the two trench wells at the airport study area, and 38 and 2 micrograms per liter, respectively, in stormwater and groundwater at the free zone. Similar reductions in concentrations between stormwater and water from the two trench wells were indicated for zinc at both study areas and also for nitrogen, phosphorus, and organic content at the free zone. This trend suggested that the exfiltration trench at both study areas may function as a partial trap for some chemical substances present in stormwater.
A comparison of the distribution of the 11 target variables and major ionic composition in water from the two trench wells and the two wells 20 feet from the trench did not indicate a notable horizontal stratification at either study area. A vertical difference between 10 and 15 feet, however, was indicated at the free zone with major ions in greater concentrations at 15 feet. The vertical variability in groundwater near the trench at the free zone may have been the result of stormwater dilution in the upper (10-foot) zone.
The ground-water quality at the swale was quite dissimilar to that near the exfiltration trench at both the airport and free zone study areas. Data indicated that the groundwater environment at both sales was anaerobic as evidenced by abundant ammonia nitrogen and iron and trace levels of sulfate. Anaerobic conditions at the swale may have been the result of poor drainage and high organic content of soils. Significant biochemical cycling in the ground water at the swales precluded any assessment of quality effects that may result from storm-water infiltration.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri884069","collaboration":"Prepared in cooperation with the South Florida Water Management District","usgsCitation":"McKenzie, D.J., and Irwin, G.A., 1988, Effects of two stormwater management methods on the quality of water in the upper Biscayne aquifer at two commercial areas in Dade County, Florida: U.S. Geological Survey Water-Resources Investigations Report 88-4069, iii, 22 p., https://doi.org/10.3133/wri884069.","productDescription":"iii, 22 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":57501,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4069/wri884069.pdf","text":"Report","size":"873 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":124540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4069/coverthb.jpg"}],"country":"United States","state":"Florida","county":"Miami-Dade County","otherGeospatial":"Biscayne aquifer, Dade County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.38799285888672,\n 25.760010550981168\n ],\n [\n -80.20362854003906,\n 25.760010550981168\n ],\n [\n -80.20362854003906,\n 25.869727228306154\n ],\n [\n -80.38799285888672,\n 25.869727228306154\n ],\n [\n -80.38799285888672,\n 25.760010550981168\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Drainage and clearing of bottomland hardwoods have long been recognized by the U.S. Environmental Protection Agency (EPA) and the U.S. Fish and Wildlife Service (Service) as important impacts of Federal water projects in the lower Mississippi River Valley. More recently, the water quality impacts of such projects (e.g., increases in sediments, nutrients, and pesticides) have also become of concern. In 1984, in an effort to better define problems concerning wetland losses and water degradation, EPA initiated a cooperative project with the Western Energy and Land Use Team (now the National Ecology Research Center) of the Service. Three phases of the project were identified:
\n1. To collect existing literature and data;
\n2. To select, develop, and test the utility of methods to quantify the relationships between land use, cover types, soils, hydrology, and water quality (as represented by sediment); and
\n3. To apply selected methodologies to several sites within the Yazoo Basin of Mississippi to determine the, potential effectiveness of various management alternatives to reduce sediment yield, increase sediment deposition, and improve water quality.
\nMethods development focused on linking a simulation of water and sediment movement to a computerized geographic information system. We had several objectives for the resulting model. We desired that it should:
\n1. Estimate the importance of bottomland and hardwoods as a cover type that performs the functions of erosion and sediment control,
\n2. Simulate effects of proportions of ' various cover types and their specific spatial configurations,
\n3. Be applicable to moderately large spatial areas with minimal site-specific calibration,
\n4. Simulate spatial patterns of sediment loss-gain over time, and
\n5. Represent both sediment detachment and transport.
\nWhile it was recognized that impacts and management alternatives could be sorted roughly into landscape measures and channel measures, the decision was made to focus study efforts mainly on landscape measures. Landscape measures include altered drainage and flooding patterns, altered cover types (e.g., conversion of bottomland hardwoods to agricultural crops, reforestation of cropland to bottomland hardwoods, and creation of riparian buffer strips), altered cropping and tillage patterns, altered routing of water, and creation of buffer strips along wetlands and channel margins. Channel measures include vegetative bank stabilization, grade control structures, and regulation of channel water volume and velocity.
\nDuring the first year of the study, EPA decided not to fund the third phase of the project. This required considerable rescoping of the project with the result that application of the sediment mobilization, routing, and deposition models to various management alternatives and portions of the Yazoo Basin was somewhat restricted. We believe, however, that this report will provide a good understanding of the various modes of sediment mobilization, transport, and deposition within the Yazoo Basin, as well as of the role of bottomland hardwoods. The model developed in this study could be applied to a variety of management or mitigation alternatives prior to implementation to determine their relative effectiveness. Policy, political, and socio-economic consequences of any proposed management/mitigation practice, however, must ultimately be taken into consideration by those charged with management of water resources within the Yazoo Basin before any practice is implemented. This study makes no effort to judge the feasibility of management alternatives in this regard.
","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Molinas, A., Auble, G.T., Segelquist, C., and Ischinger, L.S., 1988, Assessment of the role of bottomland hardwoods in sediment and erosion control, 116 p.","productDescription":"116 p.","numberOfPages":"116","costCenters":[],"links":[{"id":293052,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fd9f43e4b0adaeea6c4de4","contributors":{"authors":[{"text":"Molinas, A.","contributorId":105235,"corporation":false,"usgs":true,"family":"Molinas","given":"A.","email":"","affiliations":[],"preferred":false,"id":499504,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Auble, Gregor T. 0000-0002-0843-2751 aubleg@usgs.gov","orcid":"https://orcid.org/0000-0002-0843-2751","contributorId":2187,"corporation":false,"usgs":true,"family":"Auble","given":"Gregor","email":"aubleg@usgs.gov","middleInitial":"T.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":499502,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Segelquist, C.A.","contributorId":108410,"corporation":false,"usgs":true,"family":"Segelquist","given":"C.A.","affiliations":[],"preferred":false,"id":499505,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ischinger, Lee S.","contributorId":34054,"corporation":false,"usgs":true,"family":"Ischinger","given":"Lee","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":499503,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70122705,"text":"70122705 - 1988 - The socially optimal and market utilization of ground-water resources","interactions":[],"lastModifiedDate":"2014-08-27T13:16:06","indexId":"70122705","displayToPublicDate":"1988-01-01T13:14:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"Technical Publication Series TPS-88-2","title":"The socially optimal and market utilization of ground-water resources","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Proceedings of the symposium on water-use data for water resources management","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"American Water Resources Association","publisherLocation":"Bethesda, MD","usgsCitation":"Douglas, A.J., 1988, The socially optimal and market utilization of ground-water resources, 3 p.","productDescription":"3 p.","startPage":"261","endPage":"263","numberOfPages":"3","costCenters":[],"links":[{"id":293125,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0f0e4b01f35f8fd6a5c","contributors":{"authors":[{"text":"Douglas, A. J.","contributorId":11172,"corporation":false,"usgs":true,"family":"Douglas","given":"A.","middleInitial":"J.","affiliations":[],"preferred":false,"id":499638,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70122700,"text":"70122700 - 1988 - Western state instream flow programs: a comparative assessment","interactions":[],"lastModifiedDate":"2014-08-27T13:10:12","indexId":"70122700","displayToPublicDate":"1988-01-01T13:09:34","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"No. 18, Biological Report 89(2)","title":"Western state instream flow programs: a comparative assessment","docAbstract":"During their early history, Western States water rights laws were primarily means for facilitating and regulating water diversions for offstream, consumptive use. More recently, a countervailing concern for instream values such as fish and wildlife habitat, recreation, aesthetic values, and water quality has emerged in the legislative and administrative handling of water rights. As of 1988, the Western United States show a variety of approaches to balancing instream and diversion water rights, from zero control through administrative actions to legislatively established rights for guaranteed instream flows. The nine Western States that have adopted statutory instream flow protection programs include Alaska, Colorado, Hawaii, Idaho, Montana, Oregon, Utah, Washington, and Wyoming. Arizona, California, and Nevada have relied, to date, on administrative and judicial decisions, while New Mexico has established no mechanism for protecting instream water uses. In the States with statutory protection, instream water uses are granted the same legal status as any other water uses under the prior appropriation doctrine. The success of instream flow protection has been remarkable, given the controversial nature of the issue, with nearly 2,000 stream reaches protected.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Instream Flow Information Paper","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"McKinney, M.J., and Taylor, J.G., 1988, Western state instream flow programs: a comparative assessment, 78 p.","productDescription":"78 p.","numberOfPages":"78","costCenters":[],"links":[{"id":293123,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0f3e4b01f35f8fd6a7b","contributors":{"authors":[{"text":"McKinney, Matthew J.","contributorId":52899,"corporation":false,"usgs":true,"family":"McKinney","given":"Matthew","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":499636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Jonathan G.","contributorId":37378,"corporation":false,"usgs":true,"family":"Taylor","given":"Jonathan","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":499635,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70006404,"text":"70006404 - 1988 - Historical changes in the major fish resources of the Great Lakes","interactions":[],"lastModifiedDate":"2016-03-24T15:40:02","indexId":"70006404","displayToPublicDate":"1988-01-01T12:46:11","publicationYear":"1988","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Historical changes in the major fish resources of the Great Lakes","docAbstract":"My purpose here is to review historic changes in the major fish resources of the five Great Lakes, and to identify the cause or causes for those changes. In some instances it will be clear that intensive fishing was the primary cause of change; in other instances it will be nearly as clear that predation by the sea lamprey played a significant if not dominant role in change; and in still others it will be clear (or at least circumstantial) that exotic species other than the sea lamprey have been implicated. The exotics that have invaded or been accidentally or purposefully released into the Great Lakes system have not only adversely affected indigenous fishes, but some have developed into new and valuable resources. However, when it comes to degradation of water quality and of critical habitat, the linkages to changes in fish populations are neither clear-cut nor quantifiable — their impacts were generally far more subtle and difficult to detect, but not necessarily of less importance. Inasmuch as a comprehensive review of all changes in fishery resources, water quality, and habitat conditions in the Great Lakes would be encyclopedic, I confine discussion here to prime examples related to the most historically important fish resources. One of the values of the approach used in this manuscript is the collation in a single-source document of the conclusions reached by many scientists on reasons for changes in the fish resources across the Great Lakes basin.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Toxic contaminants and ecosystem health: a Great Lakes focus","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"John Wiley","publisherLocation":"New York, NY","usgsCitation":"Hartman, W.L., 1988, Historical changes in the major fish resources of the Great Lakes, chap. of Toxic contaminants and ecosystem health: a Great Lakes focus, p. 103-131.","productDescription":"29 p.","startPage":"103","endPage":"131","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":289219,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"The Great Lakes","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.11,41.4 ], [ -92.11,48.85 ], [ -76.3,48.85 ], [ -76.3,41.4 ], [ -92.11,41.4 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53b286f0e4b07b8813a554bf","contributors":{"editors":[{"text":"Evans, Marlene S.","contributorId":22724,"corporation":false,"usgs":true,"family":"Evans","given":"Marlene S.","affiliations":[],"preferred":false,"id":508325,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Hartman, Wilbur L.","contributorId":14763,"corporation":false,"usgs":true,"family":"Hartman","given":"Wilbur","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":354444,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70122691,"text":"70122691 - 1988 - Results of a survey of U.S. Fish and Wildlife Service Endangered Species and Ecological Services Field Offices, Refuges, Hatcheries, and Research Centers","interactions":[],"lastModifiedDate":"2014-08-27T12:38:21","indexId":"70122691","displayToPublicDate":"1988-01-01T12:37:10","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"NERC-88/30","title":"Results of a survey of U.S. Fish and Wildlife Service Endangered Species and Ecological Services Field Offices, Refuges, Hatcheries, and Research Centers","docAbstract":"The National Ecology Research Center (Center), as part of an ongoing research study on the effects of low altitude aircraft operations on fish and wildlife, conducted a survey in January 1987 of all U.S. Fish and Wildlife Service (Service) regional directors, research center directors, Ecological Services and Endangered Species field offices supervisors, refuge manager, and hatchery manager. The objective of the survey was to determine the nature and extent of aircraft-induced impacts on fish and wildlife species, populations, and habitat utilization. The field installation managers and biologists were asked to provide background information or data on fish and wildlife reactions to low-altitude aircraft disturbances, including physiological, behavioral, and reproductive/population effects. Specifically, the survey asked for information such as: (1) observations of animal reaction(s) to aircraft operations, e.g., desert bighorn sheep scare behavior in response to aircraft overflights and hatchery fish seizures and death following intense sonic booms; and instances of areas where aircraft noise is known or believed to be responsible for reduced population size, e.g. areas along heavily used aircraft flight corridors where breeding waterfowl densities are lower than in similar habitat away from the noise area.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Effects of aircraft noise and sonic booms on fish and wildlife","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Fort Collins, CO","usgsCitation":"Gladwin, D.N., Asherin, D.A., and Manci, K.M., 1988, Results of a survey of U.S. Fish and Wildlife Service Endangered Species and Ecological Services Field Offices, Refuges, Hatcheries, and Research Centers, 24 p.","productDescription":"24 p.","numberOfPages":"24","costCenters":[],"links":[{"id":293117,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0e8e4b01f35f8fd6a1e","contributors":{"authors":[{"text":"Gladwin, Douglas N.","contributorId":56352,"corporation":false,"usgs":true,"family":"Gladwin","given":"Douglas","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":499626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Asherin, Duane A.","contributorId":51660,"corporation":false,"usgs":true,"family":"Asherin","given":"Duane","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":499625,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Manci, Karen M.","contributorId":8389,"corporation":false,"usgs":true,"family":"Manci","given":"Karen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":499624,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70231505,"text":"70231505 - 1988 - Thematic mapping from satellite imagery","interactions":[],"lastModifiedDate":"2022-05-11T17:30:20.853138","indexId":"70231505","displayToPublicDate":"1988-01-01T12:18:12","publicationYear":"1988","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":15,"text":"Monograph"},"title":"Thematic mapping from satellite imagery","docAbstract":"This report, produced between 1984 and 1987 in a bilingual edition (English and French), provides a wealth of information on a wide variety of cartographic applications which are being developed to make effective use of new data that is now being collected by Earth observation satellites. At a time when natural resource development and environmental problems have to be taken into account in their entirety, satellites provide an exceptional means of evaluating, synthesizing and creating geographic information. The production of new images, such as the Landsat Thematic Mapper, the SPOT High Resolution Visible Sensor and the adoption meteorological images such as AVHRR sensors on NOAA satellites, which have been extended to thematic domains such as agriculture and glaciology, have led to many new developments as well as problems for the cartographer. These problems are numerous and varied and recur frequently depending on the images and themes being processed e.g. how to select the graphic specification of maps and legends and account for classification accuracy; how to introduce the minimum of topographical data into an image in order to supply users with an adequate geographic reference; when using a physical terrain image, on which, by definition there are no `blanks' and where no details have been eliminated, how to overcome conceptual difficulties e.g. the side by side placing of different semiological information; the interpretation levels left to reader; achieving a balance between objectivity and readability. Obviously the cartographers role is of prime importance in solving these problems. In order to illustrate the way in which this information is presented, the report provides samples from 33 thematic applications taken from 13 different categories, including agriculture, town planning and water resources. Each application is provided with a descriptive note both in English and French indicating the objective, method and results obtained. This volume provides an important record of current developments in thematic mapping from satellite imagery and should be essential reference for all cartographers.
","language":"English","publisher":"Elsevier","doi":"10.1016/C2009-0-11248-5","usgsCitation":"1988, Thematic mapping from satellite imagery, 214 p., https://doi.org/10.1016/C2009-0-11248-5.","productDescription":"214 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":400521,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Denegre, J.","contributorId":291640,"corporation":false,"usgs":false,"family":"Denegre","given":"J.","email":"","affiliations":[],"preferred":false,"id":842801,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":70039377,"text":"70039377 - 1988 - River basins of the United States: the Potomac","interactions":[],"lastModifiedDate":"2018-03-14T10:54:41","indexId":"70039377","displayToPublicDate":"1988-01-01T11:49:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"River basins of the United States: the Potomac","docAbstract":"This leaflet, one of a series on the river basins of the United States, contains information on the Potomac River Basin, including a brief early history, a description of the physical characteristics, and other statistical data. 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