An unusual gross appearance of avian tuberculosis, where fluid-filled thin-walled cysts are produced and grossly apparent in preference to granulomas, is presented. Histopathology confirmed the granulomatous nature of the lesions and the presence of intracellular acid-fast organisms. Mycobacterium avium complex was cultured from affected organs. The unusual gross presentation in these cases indicates the need to consider tuberculosis in the differential of cystic diseases of avian livers.
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The rivers, from headwaters to outlet, are the St. Marys, St. Clair, Detroit, Niagara, and St. Lawrence. They share several characteristics with certain other large rivers: the fish stocks that historically congregated for spawning or feeding have been overfished, extensive channel modification have been made, and they have been used as a repository for domestic and industrial wastes and for hydroelectric energy generation. Levels of phosphorus, chlorophyll a, and particulate organic matter increase 3- to 5-fold from the St. Marys River to the St. Lawrence River. Biological communities dependent on nutrients in the water column, such as phytoplankton, periphyton, and zooplankton similarly increase progressively downstream through the system. The standing crop of emergent macrophytes is similar in all of the rivers, reflecting the relatively large nutrient pools in the sediments and atmosphere. Consequently, emergent macrophytes are an important source of organic matter (67% of total primary production) in the nutrient poor waters of the St. Marys River, whereas phytoplankton production dominates (76%) in the enriched St. Lawrence River. Submersed and emergent macrophytes and the associated periphyton are major producers of organic matter in the connecting channels. Another major source of organic matter (measured as ash free dry weight, AFDW) in the Detroit River is sewage, introduced at a rate of 26, 000 t per year. The production of benthos ranges from a low 5.4 g AFDW•m-2 in the Detroit River to a high of 15.5 g AFDW•m-2 in the St. Marys River. The rivers lack the organic transport from riparian sources upstream but receive large amounts of high quality phytoplankton and zooplankton from the Great Lakes.
","largerWorkTitle":"Proceedings of the International Large River Symposium","conferenceTitle":"Proceedings of the International Large River Symposium","language":"English","publisher":"Canadian Special Publication of Fisheries and Aquatic Sciences","usgsCitation":"Edwards, C.J., Hudson, P.L., Duffy, W.G., Nepszy, S.J., McNabb, C.D., Haas, R.C., Liston, C.R., Manny, B., and Busch, W.N., 1989, Hydrological, morphometrical, and biological characteristics of the connecting rivers of the International Great Lakes: a review: Canadian Special Publication of Fisheries and Aquatic Sciences, 25 p.","productDescription":"25 p.","startPage":"240","endPage":"264","numberOfPages":"25","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":289184,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53b286f1e4b07b8813a554c4","contributors":{"editors":[{"text":"Dodge, D.P.","contributorId":112637,"corporation":false,"usgs":true,"family":"Dodge","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":508345,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Edwards, Clayton J.","contributorId":99897,"corporation":false,"usgs":true,"family":"Edwards","given":"Clayton","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":354674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudson, Patrick L. 0000-0002-7646-443X phudson@usgs.gov","orcid":"https://orcid.org/0000-0002-7646-443X","contributorId":5616,"corporation":false,"usgs":true,"family":"Hudson","given":"Patrick","email":"phudson@usgs.gov","middleInitial":"L.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":354666,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Duffy, Walter G. wgd7001@usgs.gov","contributorId":66750,"corporation":false,"usgs":true,"family":"Duffy","given":"Walter","email":"wgd7001@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":false,"id":354671,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nepszy, Stephen J.","contributorId":40548,"corporation":false,"usgs":true,"family":"Nepszy","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":354668,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McNabb, Clarence D.","contributorId":34977,"corporation":false,"usgs":true,"family":"McNabb","given":"Clarence","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":354667,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Haas, Robert C.","contributorId":97450,"corporation":false,"usgs":true,"family":"Haas","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":354673,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Liston, Charles R.","contributorId":71603,"corporation":false,"usgs":true,"family":"Liston","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":354672,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Manny, Bruce","contributorId":49275,"corporation":false,"usgs":true,"family":"Manny","given":"Bruce","affiliations":[],"preferred":false,"id":354670,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Busch, Wolf-Dieter N.","contributorId":46039,"corporation":false,"usgs":true,"family":"Busch","given":"Wolf-Dieter","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":354669,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70039396,"text":"70039396 - 1989 - Suggestions for prospecting","interactions":[],"lastModifiedDate":"2012-08-04T01:01:57","indexId":"70039396","displayToPublicDate":"1989-01-01T10:17:00","publicationYear":"1989","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":"Suggestions for prospecting","docAbstract":"Prospectors have contributed much to the development of this Nation's mineral resources. Since the time of the earliest settlement, the need for iron for tools and guns, lead for bullets, and copper for utensils has prompted a search for sources of these metals. The lure of gold and silver provided the impetus for much of the development in the West between 1850 and 1910. Later, prospectors carried out successful ventures to fulfill the country's expanding industrial demands for other metals such as zinc, molybdenum, tungsten, chromium, vanadium, and many others. Even America's uninhabited rugged mountains or barren deserts have been prospected although perhaps only at a reconnaissance scale.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Reston, VA","doi":"10.3133/70039396","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1989, Suggestions for prospecting: General Information Product, 25 p., https://doi.org/10.3133/70039396.","productDescription":"25 p.","numberOfPages":"27","costCenters":[],"links":[{"id":261538,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039396/report.pdf"},{"id":261539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039396/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9db6e4b08c986b31da18","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":535286,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70199824,"text":"70199824 - 1989 - Transport and degradation of water-soluble creosote-derived compounds","interactions":[],"lastModifiedDate":"2018-11-20T12:48:02","indexId":"70199824","displayToPublicDate":"1989-01-01T10:16:16","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Transport and degradation of water-soluble creosote-derived compounds","docAbstract":"Creosote is the most extensively used insecticide and industrial wood preservative today. It is estimated that there are more than 600 wood-preserving plants in the United States, and their collective use of creosote exceeds 4.5xl06 kg/yr (von Rumker et al., 1975). Creosote is a complex mixture of more than 200 major individual organic compounds with differing molecular weights, polarities, and functionalities, along with dispersed solids and products of polymerization (Novotny et al., 1981). The major classes of compounds previously identified in creosote show that it consists of ∼85% (w/w) polynuclear aromatic compounds (PAH), ∼12% phenolic compounds, and ∼3% heterocyclic nitrogen, sulfur, and oxygen containing compounds (NSO).
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Intermedia pollutant transport: Modeling and field measurements ","language":"English","publisher":"Plenum","usgsCitation":"Godsy, E.M., Goerlitz, D., and Grbic-Galic, D., 1989, Transport and degradation of water-soluble creosote-derived compounds, chap. of Intermedia pollutant transport: Modeling and field measurements , p. 213-236.","productDescription":"24 p.","startPage":"213","endPage":"236","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":359610,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.springer.com/us/book/9780306432576"},{"id":357933,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5bf52b6ce4b045bfcae2802a","contributors":{"editors":[{"text":"Allen, D.","contributorId":86955,"corporation":false,"usgs":true,"family":"Allen","given":"D.","email":"","affiliations":[],"preferred":false,"id":746804,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Godsy, E. 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Some problems still exist.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Habitat management for migrating and wintering waterfowl in North America","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Texas Tech University Press","publisherLocation":"Lubbock","usgsCitation":"Hobaugh, W., Stutzenbaker, C., and Flickinger, E.L., 1989, Rice prairies, chap. of Habitat management for migrating and wintering waterfowl in North America, p. 367-383.","productDescription":"17 p.","startPage":"367","endPage":"383","numberOfPages":"560","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200500,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699eda","contributors":{"editors":[{"text":"Smith, L.M.","contributorId":82650,"corporation":false,"usgs":true,"family":"Smith","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":506480,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Pederson, R.L.","contributorId":55546,"corporation":false,"usgs":true,"family":"Pederson","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":506479,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Kaminski, R.M.","contributorId":53330,"corporation":false,"usgs":true,"family":"Kaminski","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":506478,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Hobaugh, W.C.","contributorId":103385,"corporation":false,"usgs":true,"family":"Hobaugh","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":328465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stutzenbaker, C.D.","contributorId":16544,"corporation":false,"usgs":true,"family":"Stutzenbaker","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":328463,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flickinger, Edward L.","contributorId":48907,"corporation":false,"usgs":true,"family":"Flickinger","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":328464,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7000091,"text":"7000091 - 1989 - Gazetteer of the Antarctic","interactions":[],"lastModifiedDate":"2012-07-24T01:01:46","indexId":"7000091","displayToPublicDate":"1989-01-01T01:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":66,"text":"Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"89-98","title":"Gazetteer of the Antarctic","docAbstract":"This gazetteer lists antarctic names approved by the United States Board on Geographic Names and by the Secretary of the Interior. The Board is the interagency body created by law to standardize and promulgate geographic names for official purposes. As the official standard for names in Antarctica, the gazetteer assures accuracy and uniformity for the specialist and the general user alike. Unlike the last (1981) edition, now out of print, the book contains neither historical notes nor textual descriptions of features. The gazetteer contains names of features in Antarctica and the area extending northward to the Antarctic Convergence that have been approved by the Board as recently as mid-1989. It supersedes previous Board gazetteers for the area. For each geographic feature, the book contains the name, cross references if any, and latitude and longitude. Coverage corresponds to that of maps at the scale of 1:250,000 or larger for islands, coastal Antarctica, and mountains and ranges of the continent. Much of the interior of Antarctica, an ice plateau, has been mapped at a smaller scale and is nearly devoid of features and toponyms. All of the names are for natural features; scientific stations are not listed. For the names of submarine features, reference should be made to the Gazetteer of Undersea Features, U.S. Board on Geographic Names (1981).","language":"English","publisher":"National Science Foundation","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Board on Geographic Names, Defense Mapping Agency, Water Resources Division, U.S. Geological Survey, and National Science Foundation, 1989, Gazetteer of the Antarctic (4th): Report 89-98, xii, 145 p.","productDescription":"xii, 145 p.","numberOfPages":"160","costCenters":[{"id":429,"text":"National Mapping Division","active":false,"usgs":true}],"links":[{"id":91856,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.archive.org/details/gazetteerofantar00unit","linkFileType":{"id":5,"text":"html"}},{"id":261235,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/msb/7000091/report.pdf"},{"id":261236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/msb/7000091/report-thumb.jpg"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -180,-90 ], [ -180,-60 ], [ 180,-60 ], [ 180,-90 ], [ -180,-90 ] ] ] } } ] }","edition":"4th","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b113d","contributors":{"authors":[{"text":"U.S. Board on Geographic Names","contributorId":128291,"corporation":true,"usgs":false,"organization":"U.S. Board on Geographic Names","id":535110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Defense Mapping Agency","contributorId":128000,"corporation":true,"usgs":false,"organization":"Defense Mapping Agency","id":535108,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535109,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"National Science Foundation","contributorId":127971,"corporation":true,"usgs":false,"organization":"National Science Foundation","id":535107,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":81367,"text":"81367 - 1989 - Premigrational movements and behavior of young mallards and wood ducks in north-central Minnesota","interactions":[],"lastModifiedDate":"2017-12-29T13:04:18","indexId":"81367","displayToPublicDate":"1989-01-01T01:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":25,"text":"Fish and Wildlife Research","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"5","title":"Premigrational movements and behavior of young mallards and wood ducks in north-central Minnesota","docAbstract":"Movements and behavior of 89 young mallards (Anas platyrhynchos) and 48 young wood ducks (Aix sponsa) were monitored on a 932-km2 study area in north-central Minnesota in late summer and fall, 1972-74, with telemetry, visual observation, and aerial surveys. Initial flights of both species were confined to the natal (brood) marsh; first flights away from the natal marsh occurred in the third week after fledging in both species. First flights of young mallards and wood ducks away from their natal marshes were not significantly different between the sexes (mallard, mean = 4.95 km for females and 5.83 km for males; wood ducks, mean = 2.31 km for females and 2.64 km for males). However, flights away from the brood marshes by wood ducks were significantly shorter than for mallards.As young mallards and wood ducks grew, their daytime use of the natal marshes decreased in an irregular pattern as both species began daily flights between day- and night-use areas. Locally reared mallards made longer daily flights between use areas than did wood ducks, but wood ducks changed use areas with greater frequency before 1 October. Despite often extensive movements, most locally reared mallards and wood ducks remained in the vicinity of their brood marshes throughout fall until migration.Movement of young birds to new habitat was not the result of random searching and thus fortuitous discovery of nearby areas. Instead, birds seemed to learn of new habitat and develop movement patterns by associating with other birds; locally reared young always moved in the company of flocks of conspecifics that included adults and older immatures.Differences in movement patterns between the sexes of young birds and between young and adult birds cause them to be differentially distributed by age and sex on and near the breeding grounds. These differences are ultimately reflected in the distribution of the hunter harvest. We have interpreted generalizations about such phenomena, developed from analysis of continent-wide mallard banding data, using our data obtained from individually marked birds. We document (a) greater distances moved by early than by late-hatched young in the postbreeding period before migration, (b) differential movement of age and sex cohorts that explains greater hunting mortality of young than adults and of females than males near natal marshes, (c) differences in length and timing of postbreeding movements of adult male mallards and the postfledging movements of immature male mallards that help explain the northerly continental recovery distribution of young males, and (d) differential timing and rate of movement by birds through harvest areas (early departure of males and some return of females to natal marshes after the beginning of hunting) that explain differences in the timing of hunting season recoveries. Behavioral differences between the age and sex cohorts in the fall waterfowl population on and near their breeding grounds in north-central Minnesota can explain observed differences in survival and recovery rates of adult and young birds.The behaviors observed suggest to us that restrictive harvest regulations such as small-area closure may have little or no local benefits at the breeding grounds because premigratory assemblages of birds make extensive movements. In particular, protection of postbreeding adult females and locally reared young might only occur by closing large areas or scheduling extreme delays in the season opening, neither of which may be compatible with equitably apportioning waterfowl harvest at higher latitudes. Additional research on the local effects of restrictive regulations, and on age- and sex-specific differences in the timing, rate, and direction of fall movements of postbreeding waterfowl is needed.","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Kirby, R., Cowardin, L., and Tester, J., 1989, Premigrational movements and behavior of young mallards and wood ducks in north-central Minnesota: Fish and Wildlife Research 5, 25 p.","productDescription":"25 p.","startPage":"0","endPage":"25","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a245","contributors":{"authors":[{"text":"Kirby, R.E.","contributorId":75871,"corporation":false,"usgs":true,"family":"Kirby","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":295300,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cowardin, L.M.","contributorId":106435,"corporation":false,"usgs":true,"family":"Cowardin","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":295301,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tester, J.R.","contributorId":70510,"corporation":false,"usgs":true,"family":"Tester","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":295299,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70016119,"text":"70016119 - 1989 - Data-collection program for Pamlico River Estuary model calibration and validation","interactions":[],"lastModifiedDate":"2012-03-12T17:18:47","indexId":"70016119","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Data-collection program for Pamlico River Estuary model calibration and validation","docAbstract":"An investigation is being conducted to collect and interpret continuous records relating to the flow characteristics of the Pamlico River Estuary, North Carolina, and to calibrate and validate a numerical model of estuarine hydrodynamics. The study reach is 50 kilometers long and ranges in width from 330 meters at the upstream boundary to 6.4 kilometers at the downstream end. Water levels are recorded at 6 locations along the estuary; daily water-level range is typically greater at the head of the estuary than at the mouth, most likely due to upstream narrowing of the channel. Water-quality data are recorded at 14 locations. These data indicate that saline waters with low dissolved oxygen concentrations move upstream along the bottom of the estuary. Point velocities were monitored for 3 weeks at 7 locations; vertical profiles of horizontal velocity were made at the boundaries of the study reach for about 32 hours. Local tributary inflows and wind speed and direction are also being determined.","conferenceTitle":"Estuarine and Coastal Modeling - Proceedings of the Conference","conferenceDate":"15 November 1989 through 17 November 1989","conferenceLocation":"Newport, RI, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"Boston, MA, United States","isbn":"0872627586","usgsCitation":"Bales, J.D., 1989, Data-collection program for Pamlico River Estuary model calibration and validation, Estuarine and Coastal Modeling - Proceedings of the Conference, Newport, RI, USA, 15 November 1989 through 17 November 1989, p. 492-501.","startPage":"492","endPage":"501","numberOfPages":"10","costCenters":[],"links":[{"id":223349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fdd1e4b0c8380cd4e961","contributors":{"authors":[{"text":"Bales, Jerad D. 0000-0001-8398-6984 jdbales@usgs.gov","orcid":"https://orcid.org/0000-0001-8398-6984","contributorId":683,"corporation":false,"usgs":true,"family":"Bales","given":"Jerad","email":"jdbales@usgs.gov","middleInitial":"D.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true}],"preferred":true,"id":372598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70015931,"text":"70015931 - 1989 - Extracting spectral contrast in Landsat Thematic Mapper image data using selective principal component analysis","interactions":[],"lastModifiedDate":"2012-03-12T17:18:44","indexId":"70015931","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Extracting spectral contrast in Landsat Thematic Mapper image data using selective principal component analysis","docAbstract":"A challenge encountered with Landsat Thematic Mapper (TM) data, which includes data from size reflective spectral bands, is displaying as much information as possible in a three-image set for color compositing or digital analysis. Principal component analysis (PCA) applied to the six TM bands simultaneously is often used to address this problem. However, two problems that can be encountered using the PCA method are that information of interest might be mathematically mapped to one of the unused components and that a color composite can be difficult to interpret. \"Selective' PCA can be used to minimize both of these problems. The spectral contrast among several spectral regions was mapped for a northern Arizona site using Landsat TM data. Field investigations determined that most of the spectral contrast seen in this area was due to one of the following: the amount of iron and hematite in the soils and rocks, vegetation differences, standing and running water, or the presence of gypsum, which has a higher moisture retention capability than do the surrounding soils and rocks. -from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Photogrammetric Engineering and Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Chavez, P., and Kwarteng, A.Y., 1989, Extracting spectral contrast in Landsat Thematic Mapper image data using selective principal component analysis: Photogrammetric Engineering and Remote Sensing, v. 55, no. 3, p. 339-348.","startPage":"339","endPage":"348","numberOfPages":"10","costCenters":[],"links":[{"id":223441,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0e5ae4b0c8380cd533e8","contributors":{"authors":[{"text":"Chavez, P.S. Jr.","contributorId":75147,"corporation":false,"usgs":true,"family":"Chavez","given":"P.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":372109,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kwarteng, Andy Y.","contributorId":7423,"corporation":false,"usgs":true,"family":"Kwarteng","given":"Andy","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":372108,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70015770,"text":"70015770 - 1989 - Oxygen-isotope composition of ground water and secondary minerals in Columbia Plateau basalts: Implications for the paleohydrology of the Pasco Basin","interactions":[],"lastModifiedDate":"2024-01-24T01:40:58.508164","indexId":"70015770","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Oxygen-isotope composition of ground water and secondary minerals in Columbia Plateau basalts: Implications for the paleohydrology of the Pasco Basin","docAbstract":"Concentrations of 18O and deuterium in ground waters beneath the Hanford Reservation, Washington State, suggest that the meteoric waters recharging the basalt aquifers have been progressively depleted in these isotopes since at least Pleistocene time. This conclusion is supported by oxygen-isotope analyses of low-temperature secondary minerals filling vugs and fractures in the basalts, which are used to approximate the 18O content of ground water at the time the mineral assemblage formed. A fossil profile of δ18O values projected for ground water in a 1500 m vertical section beneath the reservation suggests that the vertical mixing of shallow and deep ground water indicated by present-day hydrochemical data was also occurring during Neogene time. These data also suggest that a unidirectional depletion of 18O and deuterium recorded in Pleistocene ground waters may have extended considerably further back in time. This shift is tentatively attributed to the orographic depletion of 18O associated with the progressive uplift of the Cascade Range since the middle Miocene.
Thermodynamic models of aqueous solutions have indicated that the mixing of seawater and calcite-saturated fresh groundwater can produce a water that is undersaturated with respect to calcite. Mixing of such waters in coastal carbonate aquifers could lead to significant amounts of limestone dissolution. The potential for such dissolution in coastal saltwater mixing zones is analyzed by coupling the results from a reaction simulation model (PHREEQE) with a variable density groundwater flow and solute transport model. Idealized cross sections of coastal carbonate aquifers are simulated to estimate the potential for calcite dissolution under a variety of hydrologic and geochemical conditions. Results show that limestone dissolution in mixing zones is strongly dependent on groundwater flux and nearly independent of the dissolution kinetics of calcite. The amount of dissolution varies within a mixing zone, depending on the properties, physical dimensions, and boundary conditions of the aquifer system. Nearly all of the dissolution occurs in the fresher side of the mixing zone, with the maximum dissolution occurring in water that is fresher than that predicted solely by geochemical reaction models. The greatest porosity and permeability development occur at the toe and at the top of the mixing zone. If permeability increases as porosity increases, asymmetry in the dissolution causes the mixing zone to migrate landward over time. Dissolution rates indicated by the model show that this mechanism can produce significant increases in porosity and permeability over time spans on the order of tens of thousands of years. Given the comparatively long span of geologic time, this process may be largely responsible for porosity and permeability development observed in those carbonate rocks through which a freshwater-saltwater mixing zone had at one time migrated.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR025i004p00655","usgsCitation":"Sanford, W.E., and Konikow, L.F., 1989, Simulation of calcite dissolution and porosity changes in saltwater mixing zones in coastal aquifers: Water Resources Research, v. 25, no. 4, p. 655-667, https://doi.org/10.1029/WR025i004p00655.","productDescription":"13 p.","startPage":"655","endPage":"667","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":224434,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505b9015e4b08c986b3192f1","contributors":{"authors":[{"text":"Sanford, Ward E. 0000-0002-6624-0280 wsanford@usgs.gov","orcid":"https://orcid.org/0000-0002-6624-0280","contributorId":2268,"corporation":false,"usgs":true,"family":"Sanford","given":"Ward","email":"wsanford@usgs.gov","middleInitial":"E.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":371373,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Konikow, Leonard F. 0000-0002-0940-3856 lkonikow@usgs.gov","orcid":"https://orcid.org/0000-0002-0940-3856","contributorId":158,"corporation":false,"usgs":true,"family":"Konikow","given":"Leonard","email":"lkonikow@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":371372,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70015552,"text":"70015552 - 1989 - Effect of site conditions on ground motion and damage","interactions":[],"lastModifiedDate":"2023-09-28T16:10:11.176539","indexId":"70015552","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"Effect of site conditions on ground motion and damage","docAbstract":"Results of seismologic studies conducted by the U.S. reconnaissance team in conjunction with Soviet colleagues following the tragic earthquakes of December 7, 1988, suggest that site conditions may have been a major factor in contributing to increased damage levels in Leninakan. As the potential severity of these effects in Leninakan had not been previously identified, this chapter presents results intended to provide a preliminary quantification of these effects on both damage and levels of ground motion observed in Leninakan. The article describes the damage distribution geologic setting, ground motion amplification in Leninakan, including analog amplifications and spectral amplifications. Preliminary model estimates for site response are presented. It is concluded that ground motion amplification in the 0.5-2.5-second period range was a major contributing factor to increased damage in Leninakan as compared with Kirovakan. Leninakan is located on thick water saturated alluvial deposits.","language":"English","publisher":"Earthquake Engineering Research Institute","doi":"10.1193/1.1585233","usgsCitation":"Borcherdt, R., Glassmoyer, G., Andrews, M., and Cranswick, E., 1989, Effect of site conditions on ground motion and damage: Earthquake Spectra, v. 5, no. 1_suppl, p. 23-42, https://doi.org/10.1193/1.1585233.","productDescription":"20 p.","startPage":"23","endPage":"42","costCenters":[],"links":[{"id":224263,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Armenia","state":"Shirak","city":"Gyumri","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 43.80043029785156,\n 40.761300880922235\n ],\n [\n 43.847808837890625,\n 40.724364221722716\n ],\n [\n 43.88763427734374,\n 40.75818026660039\n ],\n [\n 43.89244079589844,\n 40.8210843390845\n ],\n [\n 43.83544921875,\n 40.83043687764923\n ],\n [\n 43.79493713378906,\n 40.805493843894155\n ],\n [\n 43.8079833984375,\n 40.78678041401646\n ],\n [\n 43.797683715820305,\n 40.763901280945866\n ],\n [\n 43.80043029785156,\n 40.761300880922235\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"5","issue":"1_suppl","noUsgsAuthors":false,"publicationDate":"1989-08-01","publicationStatus":"PW","scienceBaseUri":"505a0607e4b0c8380cd510b0","contributors":{"authors":[{"text":"Borcherdt, R. 0000-0002-8668-0849","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":83130,"corporation":false,"usgs":true,"family":"Borcherdt","given":"R.","affiliations":[],"preferred":false,"id":371211,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Glassmoyer, G.","contributorId":62751,"corporation":false,"usgs":true,"family":"Glassmoyer","given":"G.","email":"","affiliations":[],"preferred":false,"id":371210,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Andrews, M.","contributorId":10935,"corporation":false,"usgs":true,"family":"Andrews","given":"M.","email":"","affiliations":[],"preferred":false,"id":371209,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cranswick, E.","contributorId":85948,"corporation":false,"usgs":true,"family":"Cranswick","given":"E.","affiliations":[],"preferred":false,"id":371212,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70015899,"text":"70015899 - 1989 - Interrelationships among hydrologic-budget components of a northern Wisconsin seepage lake and implications for acid-deposition modeling","interactions":[],"lastModifiedDate":"2023-12-12T15:19:57.286534","indexId":"70015899","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":887,"text":"Archives of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Interrelationships among hydrologic-budget components of a northern Wisconsin seepage lake and implications for acid-deposition modeling","docAbstract":"Components of the hydrologic budget for a northern Wisconsin seepage lake were analyzed by applying correlation and regression techniques to monthly data. Analyses for the 1981–83 water years revealed a statistically significant, direct relationship between storage change and precipitation-evaporation balance. Ground-water outflow was negatively correlated with ground-water inflow, and this relationship was influenced by similar relationships for both hydraulic gradients and cross-sectional areas in outflow versus inflow regions of the lake. Neither ground-water outflow nor inflow was significantly related to precipitation, evaporation, storage change, or lake stage; this may reflect a lag in response time of the ground-water system compared to the lake. The results (1) emphasize the complexity of factors that influence ground-water interactions with seepage lakes and (2) suggest the importance of completing detailed hydrologic studies of these systems before mechanistic models, such as those developed to predict effects of acid deposition, are applied.
","language":"English","publisher":"Springer","doi":"10.1007/BF01056199","usgsCitation":"Wentz, D.A., and Rose, W., 1989, Interrelationships among hydrologic-budget components of a northern Wisconsin seepage lake and implications for acid-deposition modeling: Archives of Environmental Contamination and Toxicology, v. 18, no. 1-2, p. 147-155, https://doi.org/10.1007/BF01056199.","productDescription":"9 p.","startPage":"147","endPage":"155","numberOfPages":"9","costCenters":[],"links":[{"id":223032,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Vilas County","otherGeospatial":"Vandercook Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -89.69120679416645,\n 45.9894661436733\n ],\n [\n -89.69120679416645,\n 45.97500382959842\n ],\n [\n -89.67867191017365,\n 45.97500382959842\n ],\n [\n -89.67867191017365,\n 45.9894661436733\n ],\n [\n -89.69120679416645,\n 45.9894661436733\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"18","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3da4e4b0c8380cd63709","contributors":{"authors":[{"text":"Wentz, Dennis A. dawentz@usgs.gov","contributorId":1838,"corporation":false,"usgs":true,"family":"Wentz","given":"Dennis","email":"dawentz@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":372033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rose, William J. wjrose@usgs.gov","contributorId":2182,"corporation":false,"usgs":true,"family":"Rose","given":"William J.","email":"wjrose@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":372032,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70015387,"text":"70015387 - 1989 - Mass conservation: 1-D open channel flow equations","interactions":[],"lastModifiedDate":"2024-12-12T17:01:40.420247","indexId":"70015387","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2338,"text":"Journal of Hydraulic Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Mass conservation: 1-D open channel flow equations","docAbstract":"Unsteady flow simulation in natural rivers is often complicated by meandering channels of compound section. Hydraulic properties and the length of the wetted channel may vary significantly as a meandering river inundates its adjacent floodplain. The one-dimensional, unsteady, open-channel flow equations can be extended to simulate floods in channels of compound section if it is assumed that the lateral velocities are negligible, the water surface is level across the section, and the effects of turbulence and friction may be adequately described by resistance laws used for uniform flow. It is shown that the equations derived from the addition of differential equations individually describing flow in main and overbank channels do not conserve mass when overbank and main channels are of different lengths. Equations derived through the use of appropriate integral relations, however, do conserve mass and momentum in the general case and are not limited to the specification of one main and two overbank channels.
","language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0733-9429(1989)115:2(263)","issn":"07339429","usgsCitation":"DeLong, L.L., 1989, Mass conservation: 1-D open channel flow equations: Journal of Hydraulic Engineering, v. 115, no. 2, p. 263-269, https://doi.org/10.1061/(ASCE)0733-9429(1989)115:2(263).","productDescription":"7 p.","startPage":"263","endPage":"269","numberOfPages":"7","costCenters":[],"links":[{"id":223983,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"115","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a524ce4b0c8380cd6c2eb","contributors":{"authors":[{"text":"DeLong, Lewis L.","contributorId":91146,"corporation":false,"usgs":true,"family":"DeLong","given":"Lewis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":370822,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70015011,"text":"70015011 - 1989 - Estimating urban flood-frequency characteristics","interactions":[],"lastModifiedDate":"2012-03-12T17:18:51","indexId":"70015011","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Estimating urban flood-frequency characteristics","docAbstract":"Methods in use by the U.S. Geological Survey to estimate flood-frequency characteristics for urban watersheds are compared with estimates based on the Soil Conservation Service TR-55 model. Data from four small urban watersheds in Georgia are used in the flood-peak and hydrograph comparisons.","conferenceTitle":"Proceedings of the 1989 National Conference on Hydraulic Engineering","conferenceDate":"14 August 1989 through 18 August 1989","conferenceLocation":"New Orleans, LA, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0872627195","usgsCitation":"Jennings, M., Atkins, J., and Inman, E.J., 1989, Estimating urban flood-frequency characteristics, Proceedings of the 1989 National Conference on Hydraulic Engineering, New Orleans, LA, USA, 14 August 1989 through 18 August 1989, p. 516-521.","startPage":"516","endPage":"521","numberOfPages":"6","costCenters":[],"links":[{"id":224450,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0b6be4b0c8380cd526fa","contributors":{"authors":[{"text":"Jennings, M.E.","contributorId":76775,"corporation":false,"usgs":true,"family":"Jennings","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":369852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atkins, J.B.","contributorId":63842,"corporation":false,"usgs":true,"family":"Atkins","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":369851,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Inman, E. J.","contributorId":44193,"corporation":false,"usgs":true,"family":"Inman","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":369850,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70015532,"text":"70015532 - 1989 - Recharge of the early atmosphere of Mars by impact-induced release of CO2","interactions":[],"lastModifiedDate":"2013-10-29T15:18:09","indexId":"70015532","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Recharge of the early atmosphere of Mars by impact-induced release of CO2","docAbstract":"Channels on the Martian surface suggest that Mars had an early, relatively thick atmosphere. If the atmosphere was thick enough for water to be stable at the surface, CO2 in the atmosphere would have been fixed as carbonates on a relatively short time scale, previously estimated to be 1 bar every 107 years. This loss must have been offset by some replenishment mechanism to account for the numerous valley networks in the oldest surviving terrains. Impacts could have released CO2 into the atmosphere by burial, by shock-induced release during impact events, and by addition of carbon to Mars from the impacting bolides. Depending on the relationship between the transient cavity diameter and the diameter of the resulting crater, burial rates as a result of impact gardening at the end of heavy bombardment are estimated to range from 20 to 45 m/106 years, on the assumption that cratering rates in Mars were similar to those of the Nectarian Period on the Moon. At these rates 0.1-0.2 bar of CO2 could have been released every 107 years as a result of burial to depths where dissociation temperatures of carbonates were reached. Modeling of large impacts suggests that an additional 0.01 to 0.02 bar of CO2 could have been released every 107 years during the actual impacts. In the unlikely event that all the impacting material was composed of carbonaceous chondrites, a further 0.3 bar of CO2 could have been added to the atmosphere every 107 years by oxidation of meteoritic carbon. Even when supplemented by the volcanically induced release of CO2, these release rates are barely sufficient to sustain an early atmosphere if water were continuously present at the surface. The results suggest that water may have been only intermittently present on the surface early in the planet's history.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Icarus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(89)90080-8","issn":"00191035","usgsCitation":"Carr, M.H., 1989, Recharge of the early atmosphere of Mars by impact-induced release of CO2: Icarus, v. 79, no. 2, p. 311-327, https://doi.org/10.1016/0019-1035(89)90080-8.","startPage":"311","endPage":"327","numberOfPages":"17","costCenters":[],"links":[{"id":223827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":278565,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0019-1035(89)90080-8"}],"volume":"79","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9665e4b0c8380cd81f7e","contributors":{"authors":[{"text":"Carr, Michael H.","contributorId":61894,"corporation":false,"usgs":true,"family":"Carr","given":"Michael","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":371167,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70015013,"text":"70015013 - 1989 - 100 years of sedimentation study by the USGS","interactions":[],"lastModifiedDate":"2012-03-12T17:18:51","indexId":"70015013","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"100 years of sedimentation study by the USGS","docAbstract":"On January 15, 1889, the U.S. Geological Survey began collecting sediment data on the Rio Grande at Embudo, New Mexico. During the past 100 years the U.S. Geological Survey's Water Resources Division (WRD) has collected daily sediment data at more than 1,200 sites. Projects have addressed the problems associated with reservoir construction, agricultural irrigation projects, energy production, and transport and deposition of pollutants sorbed to sediments. The Survey has been active as a charter member of the Federal Interagency Sediment Project and currently has three full-time hydrologists working on the project. The WRD's sediment-research projects have covered a wide variety of subjects from the fundamental theories of resistance to flow and sediment transport in alluvial channels to lunar erosion mechanisms.","conferenceTitle":"Sediment Transport Modeling: Proceedings of the International Symposium","conferenceDate":"14 August 1989 through 18 August 1989","conferenceLocation":"New Orleans, LA, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0872627187","usgsCitation":"Glysson, G.D., 1989, 100 years of sedimentation study by the USGS, Sediment Transport Modeling: Proceedings of the International Symposium, New Orleans, LA, USA, 14 August 1989 through 18 August 1989, p. 260-265.","startPage":"260","endPage":"265","numberOfPages":"6","costCenters":[],"links":[{"id":224452,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e221e4b0c8380cd4599f","contributors":{"authors":[{"text":"Glysson, G. Douglas","contributorId":13607,"corporation":false,"usgs":true,"family":"Glysson","given":"G.","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":369855,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}