{"pageNumber":"1867","pageRowStart":"46650","pageSize":"25","recordCount":68927,"records":[{"id":70015680,"text":"70015680 - 1989 - Introduction to the hydrogeochemical investigations within the International Stripa Project","interactions":[],"lastModifiedDate":"2024-04-03T16:43:47.659437","indexId":"70015680","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Introduction to the hydrogeochemical investigations within the International Stripa Project","docAbstract":"The International Stripa Project (1980-1990) has sponsored hydrogeochemical investigations at several subsurface drillholes in the granitic portion of an abandoned iron ore mine, central Sweden. The purpose has been to advance our understanding of geochemical processes in crystalline bedrock that may affect the safety assessment of high-level radioactive waste repositories. More than a dozen investigators have collected close to a thousand water and gas samples for chemical and isotopic analyses to develop concepts for the behavior of solutes in a granitic repository environment. The Stripa granite is highly radioactive and has provided an exceptional opportunity to study the behavior of natural radionuclides, especially subsurface production. Extensive microfracturing, low permeability with isolated fracture zones of high permeability, unusual water chemistry, and a typical granitic mineral assemblage with thin veins and fracture coatings of calcite, chlorite, seriate, epidote and quartz characterize the site. Preliminary groundwater flow modeling indicates that the mine has perturbed the flow environment to a depth of about 3 km and may have induced deep groundwaters to flow into the mine. ?? 1989.","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(89)90293-7","issn":"00167037","usgsCitation":"Nordstrom, D.K., Olsson, T., Carlsson, L., and Fritz, P., 1989, Introduction to the hydrogeochemical investigations within the International Stripa Project: Geochimica et Cosmochimica Acta, v. 53, no. 8, p. 1717-1726, https://doi.org/10.1016/0016-7037(89)90293-7.","productDescription":"10 p.","startPage":"1717","endPage":"1726","numberOfPages":"10","costCenters":[],"links":[{"id":223783,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3dfce4b0c8380cd639f4","contributors":{"authors":[{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":371512,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olsson, T.","contributorId":102636,"corporation":false,"usgs":true,"family":"Olsson","given":"T.","email":"","affiliations":[],"preferred":false,"id":371513,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carlsson, L.","contributorId":28376,"corporation":false,"usgs":true,"family":"Carlsson","given":"L.","email":"","affiliations":[],"preferred":false,"id":371510,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fritz, P.","contributorId":83673,"corporation":false,"usgs":true,"family":"Fritz","given":"P.","email":"","affiliations":[],"preferred":false,"id":371511,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70015608,"text":"70015608 - 1989 - A comparison of instrumental dewatering methods for the separation and concentration of suspended sediment for subsequent trace element analysis","interactions":[],"lastModifiedDate":"2024-03-28T00:19:37.932914","indexId":"70015608","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"A comparison of instrumental dewatering methods for the separation and concentration of suspended sediment for subsequent trace element analysis","docAbstract":"<div class=\"abstract-group \"><div class=\"article-section__content en main\"><p>A comparison involving both field and laboratory trials was performed to evaluate the utility of two continuous-flow centrifuges and a tangential-flow filtration system for dewatering suspended sediments for subsequent trace element analysis. Although recovery efficiencies for the various devices differ, the analytical results from the separated suspended sediments indicate that any of the tested units can be used effectively and precisely for dewatering. Further, the three devices appear to concentrate and dewater suspended sediments in such a manner as to be equivalent to that which could be obtained by in-line filtration. Only the tangential-flow filtration system appears capable of providing both a dewatered sediment sample and a potentially usable effluent, which can be analysed for dissolved trace elements.</p><p>The continuous-flow centrifuges can process whole water at an influent feed rate of 41 per minute; however, when suspended sediment concentrations are low (&lt;30mg<sup>−1</sup>), when small volumes of whole water are to be processed (30 to 401), or when suspended sediment mean grain size is very fine (&lt;10 μm), influent feed rates of 21 per minute may be more efficient. Tangential-flow filtration can be used to process samples at the rate of 11 per minute.</p></div></div>","language":"English","publisher":"Wiley","doi":"10.1002/hyp.3360030206","issn":"08856087","usgsCitation":"Horowitz, A.J., Elrick, K.A., and Hooper, R., 1989, A comparison of instrumental dewatering methods for the separation and concentration of suspended sediment for subsequent trace element analysis: Hydrological Processes, v. 3, no. 2, p. 163-184, https://doi.org/10.1002/hyp.3360030206.","productDescription":"22 p.","startPage":"163","endPage":"184","numberOfPages":"22","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":224324,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-31","publicationStatus":"PW","scienceBaseUri":"5059e35ce4b0c8380cd45fd1","contributors":{"authors":[{"text":"Horowitz, A. J.","contributorId":102066,"corporation":false,"usgs":true,"family":"Horowitz","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":371357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elrick, K. A.","contributorId":98731,"corporation":false,"usgs":true,"family":"Elrick","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":371356,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hooper, R.C.","contributorId":53531,"corporation":false,"usgs":true,"family":"Hooper","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":371355,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70015605,"text":"70015605 - 1989 - The separation of the Hartland Formation and Ravenswood Granodiorite from the Fordham Gneiss at Cameron's Line in the New York City area","interactions":[],"lastModifiedDate":"2019-06-11T11:22:23","indexId":"70015605","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2896,"text":"Northeastern Geology","active":true,"publicationSubtype":{"id":10}},"title":"The separation of the Hartland Formation and Ravenswood Granodiorite from the Fordham Gneiss at Cameron's Line in the New York City area","docAbstract":"<p>Recent study of the rocks in City Water Tunnel Number 3 between Roosevelt Island and beneath 34th Street and the 63rd Street subway-rail tunnels at 41st Avenue in Long Island City, as well as study of drill core from other sites in western Queens, establishes that this area of New York City is underlain by the Ravenswood Granodiorite and the Hartland Formation. The Fordham Gneiss does not appear east of the East River at these sites. Cameron's Line can be traced down the east side of the East River, as learned from observations in the tunnels, separating the Middle Proterozoic Fordham Gneiss to the west from the Cambrian and Ordovician Hartland Formation and related Ravenswood Granodiorite to the east. The older, adequately defined, Ravenswood Granodiorite, Hartland Formation, and the Fordham Gneiss, are the rock units that make up the poorly defined Brooklyn gneiss or Brooklyn Injection Gneiss and thus appropriately should supersede these later classifications. -from Authors</p>","language":"English","usgsCitation":"Baskerville, C., and Mose, D., 1989, The separation of the Hartland Formation and Ravenswood Granodiorite from the Fordham Gneiss at Cameron's Line in the New York City area: Northeastern Geology, v. 11, no. 1, p. 22-28.","productDescription":"7 p.","startPage":"22","endPage":"28","numberOfPages":"7","costCenters":[],"links":[{"id":224321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb00de4b08c986b324bcf","contributors":{"authors":[{"text":"Baskerville, C.A.","contributorId":63482,"corporation":false,"usgs":true,"family":"Baskerville","given":"C.A.","affiliations":[],"preferred":false,"id":371345,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mose, D.G.","contributorId":33461,"corporation":false,"usgs":true,"family":"Mose","given":"D.G.","affiliations":[],"preferred":false,"id":371344,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47723,"text":"wri874234 - 1989 - Potentiometric surface of the lower Cape Fear aquifer in the central coastal plain of North Carolina, December 1986","interactions":[],"lastModifiedDate":"2023-04-18T18:36:50.931414","indexId":"wri874234","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4234","title":"Potentiometric surface of the lower Cape Fear aquifer in the central coastal plain of North Carolina, December 1986","docAbstract":"Water level measurements were made in four wells open to the lower Cape Fear aquifer at the end of 1986 to determine the configuration of its potentiometric surface over an area of approximately 4,100 sq mi. Because of the scarcity of data, five earlier measurements were also used to help estimate the position of the potentiometric contours. These were one-time measurements in temporary observation wells. A broad cone of depression has formed in the area between Kinston and New Bern where the potentiometric surface is below sea level and seems likely related to large groundwater withdrawals from the aquifers overlying the lower Cape Fear in that area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874234","usgsCitation":"Winner, M.D., Lyke, W.L., and Brockman, A., 1989, Potentiometric surface of the lower Cape Fear aquifer in the central coastal plain of North Carolina, December 1986: U.S. Geological Survey Water-Resources Investigations Report 87-4234, 1 Plate: 11.70 x 13.83 inches, https://doi.org/10.3133/wri874234.","productDescription":"1 Plate: 11.70 x 13.83 inches","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":162196,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":415929,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46887.htm","linkFileType":{"id":5,"text":"html"}},{"id":84630,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4234/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Cape Fear aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.75,\n              34.6667\n            ],\n            [\n              -77.75,\n              35.9167\n            ],\n            [\n              -77,\n              35.9167\n            ],\n            [\n              -77,\n              34.6667\n            ],\n            [\n              -77.75,\n              34.6667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682e8f","contributors":{"authors":[{"text":"Winner, M. D. Jr.","contributorId":51766,"corporation":false,"usgs":true,"family":"Winner","given":"M.","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":236084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyke, William L.","contributorId":38616,"corporation":false,"usgs":true,"family":"Lyke","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":236083,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brockman, Allen R.","contributorId":91828,"corporation":false,"usgs":true,"family":"Brockman","given":"Allen R.","affiliations":[],"preferred":false,"id":236085,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":47724,"text":"wri874235 - 1989 - Potentiometric surface of the upper Cape Fear aquifer in the central coastal plain of North Carolina, December 1986","interactions":[],"lastModifiedDate":"2023-03-31T19:37:12.565773","indexId":"wri874235","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4235","title":"Potentiometric surface of the upper Cape Fear aquifer in the central coastal plain of North Carolina, December 1986","docAbstract":"Water-level measurements were made in 84 wells open to the upper Cape Fear aquifer at the end of 1986 to determine the configuration of its potentiometric surface over an area of approximately 5,500 sq mi. The major feature of the potentiometric surface is the development of a large, almost circular cone of depression as a result of the merging of a number of smaller cones. The center of the large cone lies along an axis between Greenville and Kinston. The potentiometric surface in the upper Cape Fear is nearly 100 ft below sea level at Greenville; it is more than 100 ft above sea level south of the Neuse River near Colorado.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874235","usgsCitation":"Winner, M.D., Lyke, W.L., and Brockman, A., 1989, Potentiometric surface of the upper Cape Fear aquifer in the central coastal plain of North Carolina, December 1986: U.S. Geological Survey Water-Resources Investigations Report 87-4235, 1 Plate: 11.67 x 13.77 inches, https://doi.org/10.3133/wri874235.","productDescription":"1 Plate: 11.67 x 13.77 inches","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":162197,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":415029,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46888.htm","linkFileType":{"id":5,"text":"html"}},{"id":84631,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4235/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Coastal Plain, upper Cape Fear aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -78.1667,\n              36\n            ],\n            [\n              -78.1667,\n              34.5833\n            ],\n            [\n              -77,\n              34.5833\n            ],\n            [\n              -77,\n              36\n            ],\n            [\n              -78.1667,\n              36\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682eb3","contributors":{"authors":[{"text":"Winner, M. D. Jr.","contributorId":51766,"corporation":false,"usgs":true,"family":"Winner","given":"M.","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":236087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyke, William L.","contributorId":38616,"corporation":false,"usgs":true,"family":"Lyke","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":236086,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brockman, Allen R.","contributorId":91828,"corporation":false,"usgs":true,"family":"Brockman","given":"Allen R.","affiliations":[],"preferred":false,"id":236088,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70016051,"text":"70016051 - 1989 - Thermal infrared (2.5-13.5 μm) spectroscopic remote sensing of igneous rock types on particulate planetary surfaces","interactions":[],"lastModifiedDate":"2015-06-02T10:31:38","indexId":"70016051","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2312,"text":"Journal of Geophysical Research","active":true,"publicationSubtype":{"id":10}},"title":"Thermal infrared (2.5-13.5 μm) spectroscopic remote sensing of igneous rock types on particulate planetary surfaces","docAbstract":"<p><span>Fundamental molecular vibration bands are significantly diminished by scattering. Thus such bands in spectra of fine particulate regoliths (i.e., dominated by &lt;5-&mu;m particles), or regoliths displaying a similar scale of porosity, are difficult to use for mineralogical or rock type identification. Consequently, other spectral features have been sought that may be more useful in spectroscopic remote sensing of composition. We find that mineralogical information is retained in overtones and combination tones of the fundamental molecular vibrations in the 3.0- to 7.0-&mu;m region, but that relatively few minerals have a sufficiently distinctive band structure to be unambiguously identified with currently available techniques. More significantly, identification of general rock type, as defined by the SCFM chemical index (SCFM = SiO</span><span>2</span><span>/SiO</span><span>2</span><span>&nbsp;+ CaO + FeO + MgO), is possible using spectral features associated with the principal Christiansen frequency and with a region of relative transparency between the Si-O stretching and bending bands. However, environmental factors may affect the appearance and wavelengths of these features. Finally, prominent absorption bands may result from the presence of relatively small amounts of water, hydroxyl or carbonate, because absorption bands exhibited by these materials in the 2.7- to 4.0-&mu;m region, where silicate spectra are otherwise featureless, increase strongly in spectral contrast with decreasing particle size. Such materials are thus detectable in very small amounts in a particulate regolith composed predominantly of silicate minerals.</span></p>","language":"English","publisher":"AGU Publications","doi":"10.1029/JB094iB07p09192","issn":"01480227","usgsCitation":"Salisbury, J.W., and Walter, L.S., 1989, Thermal infrared (2.5-13.5 μm) spectroscopic remote sensing of igneous rock types on particulate planetary surfaces: Journal of Geophysical Research, v. 94, no. B7, p. 9192-9202, https://doi.org/10.1029/JB094iB07p09192.","productDescription":"11 p.","startPage":"9192","endPage":"9202","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":223192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"B7","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505bb228e4b08c986b32562d","contributors":{"authors":[{"text":"Salisbury, John W.","contributorId":96420,"corporation":false,"usgs":true,"family":"Salisbury","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":372428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walter, Louis S.","contributorId":97927,"corporation":false,"usgs":true,"family":"Walter","given":"Louis","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":372429,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001624,"text":"1001624 - 1989 - Rice available to waterfowl in harvested fields in the Sacramento Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:04:49","indexId":"1001624","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1153,"text":"California Fish and Game","active":true,"publicationSubtype":{"id":10}},"title":"Rice available to waterfowl in harvested fields in the Sacramento Valley, California","docAbstract":"Rice fields in the Sacramento Valley, California were sampled in 1985 and 1986 to determine the weight of rice seed remaining in the fields immediately after harvest and again after the fields were burned. No significant differences were found between years (P>0.05). The pooled mean was 388 kg/ha in harvested fields and 276 kg/ha in burned fields. These values are less than estimates previously available. The values for harvested fields both years were no different (P>0.05) than values obtained by the U.S. Department of Agriculture (USDA). Surveys of rice fields in December both years showed that most fields were left either harvested (26-32%) or burned (37-40%) through the winter. Fields flooded for duck hunting made up 15% of the total. The proportion of fields plowed by December increased from 14% in 1985 to 22% in 1986. Sixty-three percent of all fields that had been flooded for hunting were drained within two weeks after the end of the hunting season. Harvest yield field size levee type (contour, lasered), straw status (spread, windrowed), harvest date, and rice variety did not affect the quantity of seeds remaining after harvest (P>0.05). One harvester model, the Hardy Harvester, left more rice in fields than did others we tested (P<0.001). Specific management programs are recommended to mitigate annual variation in rice seed availability to waterfowl caused by differences in total hectares grown (15% less in 1986) and in the proportion of fields burned and plowed.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"California Fish and Game","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Miller, M.R., Sharp, D., Gilmer, D., and Mulvaney, W., 1989, Rice available to waterfowl in harvested fields in the Sacramento Valley, California: California Fish and Game, v. 75, no. 2, p. 113-123.","productDescription":"p. 113-123","startPage":"113","endPage":"123","numberOfPages":"10","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":134358,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"75","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699f0f","contributors":{"authors":[{"text":"Miller, M. R.","contributorId":19104,"corporation":false,"usgs":true,"family":"Miller","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":311366,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sharp, D.E.","contributorId":34460,"corporation":false,"usgs":true,"family":"Sharp","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":311368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gilmer, D.S.","contributorId":22270,"corporation":false,"usgs":true,"family":"Gilmer","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":311367,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mulvaney, W.R.","contributorId":91811,"corporation":false,"usgs":true,"family":"Mulvaney","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":311369,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70045318,"text":"70045318 - 1989 - Notes on sedimentation activities calendar year 1988","interactions":[],"lastModifiedDate":"2017-05-18T12:39:56","indexId":"70045318","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Notes on sedimentation activities calendar year 1988","docAbstract":"This report is a digest of information furnished by Federal agencies conducting sedimentation investigations. The decision to publish the report was made in 1946, from a proposal by the Chairman of the Federal Interagency River Basin Committee, Subcommittee on Ground Water. The subcommittee approved the proposal and agreed to issue this report as a means of effecting better coordination of the work of various Federal agencies in the field of sedimentation. The report was issued on a quarterly basis in 1946 and 1947, from 1948 to 1953 reports were issued every 6 months, and from 1954 to the present, the report has been issued annually.","language":"English","publisher":"U.S. Geological Survey, Office of Water Data Coordination","publisherLocation":"Reston, VA","usgsCitation":"U.S. Interagency Advisory Committee on Water Data- Subcommittee on Sedimentation, 1989, Notes on sedimentation activities calendar year 1988, xxvii, 177 p.","productDescription":"xxvii, 177 p.","numberOfPages":"210","additionalOnlineFiles":"N","temporalStart":"1988-01-01","temporalEnd":"1988-12-31","costCenters":[],"links":[{"id":272715,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045318/report.pdf"},{"id":270698,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045318/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51653870e4b077fa94dadff5","contributors":{"authors":[{"text":"U.S. Interagency Advisory Committee on Water Data- Subcommittee on Sedimentation","contributorId":127893,"corporation":true,"usgs":false,"organization":"U.S. Interagency Advisory Committee on Water Data- Subcommittee on Sedimentation","id":535474,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003212,"text":"1003212 - 1989 - Organochlorine contaminants in white-faced ibis eggs in southern Texas","interactions":[],"lastModifiedDate":"2020-05-13T16:47:25.24714","indexId":"1003212","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1272,"text":"Colonial Waterbirds","printIssn":"07386028","active":false,"publicationSubtype":{"id":10}},"title":"Organochlorine contaminants in white-faced ibis eggs in southern Texas","docAbstract":"<p>White-faced Ibis (<i>Plegadis chihi</i>) eggs collected from two colonies in southern Texas in 1985 had low mean concentrations of DDE (0.14-0.27 ppm wet weight). DDD, the only other organochlorine contaminant detected, was found in only 1 of 20 eggs. DDE concentrations in eggs were not significantly correlated with eggshell thickness. Mean DDE concentrations were significantly higher in eggs collected from nests where not all of the remaining eggs hatched (1.0 ppm) than in eggs collected from nests where all the remaining eggs hatched (0.15 ppm).</p>","largerWorkTitle":"","language":"English","publisher":"Waterbird Society","doi":"10.2307/1521325","usgsCitation":"Custer, T., and Mitchell, C.A., 1989, Organochlorine contaminants in white-faced ibis eggs in southern Texas: Colonial Waterbirds, v. 12, no. 1, p. 126-129, https://doi.org/10.2307/1521325.","productDescription":"4 p.","startPage":"126","endPage":"129","numberOfPages":"4","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":133872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","city":"Arroyo City, Port Mansfield","otherGeospatial":"Lower Laguna Madre","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.42984771728516,\n              26.5321761726167\n            ],\n            [\n              -97.39688873291016,\n              26.5321761726167\n            ],\n            [\n              -97.39688873291016,\n              26.575478297254726\n            ],\n            [\n              -97.42984771728516,\n              26.575478297254726\n            ],\n            [\n              -97.42984771728516,\n              26.5321761726167\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.4325942993164,\n              26.277716056691347\n            ],\n            [\n              -97.30316162109375,\n              26.277716056691347\n            ],\n            [\n              -97.30316162109375,\n              26.430613192903458\n            ],\n            [\n              -97.4325942993164,\n              26.430613192903458\n            ],\n            [\n              -97.4325942993164,\n              26.277716056691347\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"12","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a043","contributors":{"authors":[{"text":"Custer, T. W. 0000-0003-3170-6519","orcid":"https://orcid.org/0000-0003-3170-6519","contributorId":91802,"corporation":false,"usgs":true,"family":"Custer","given":"T. W.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":312966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mitchell, C. A.","contributorId":54543,"corporation":false,"usgs":true,"family":"Mitchell","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":312965,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043724,"text":"70043724 - 1989 - Publications of the U.S. Geological Survey, 1988","interactions":[],"lastModifiedDate":"2013-05-23T10:11:37","indexId":"70043724","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":378,"text":"Publications of the US Geological Survey","active":false,"publicationSubtype":{"id":6}},"title":"Publications of the U.S. Geological Survey, 1988","docAbstract":"This catalog is a list of (1) books and maps that were published during 1988, and (2) articles by Geological Survey personnel in non-Geological Survey journals and books that came to our attention in 1988; it supplements the permanent catalogs \"Publications of the Geological Survey, 1879-1961\", \"Publications of the Geological Survey, 1962-1970\", and \"Publications of the U.S. Geological Survey, 1971 through 1981.\"","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70043724","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1989, Publications of the U.S. Geological Survey, 1988: Publications of the US Geological Survey, v, 390 p., https://doi.org/10.3133/70043724.","productDescription":"v, 390 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":272670,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70043724/report.pdf"},{"id":267703,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70043724/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad65e4b0b6328103b503","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":535416,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003129,"text":"1003129 - 1989 - Reversed-phase thin-layer chromatography of homologs of Antimycin-A and related derivatives","interactions":[],"lastModifiedDate":"2012-02-02T00:04:50","indexId":"1003129","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2213,"text":"Journal of Chromatography","active":true,"publicationSubtype":{"id":10}},"title":"Reversed-phase thin-layer chromatography of homologs of Antimycin-A and related derivatives","docAbstract":"Using a reversed-phase high-performance liquid chromatographic (HPLC) technique, a mixture of antimycins A was separated into eight hitherto unreported subcomponents, Ala, Alb, A2a, A2b, A3a, A3b, A4a, and A4b. Although a base-line resolution of the known four major antimycins Al, A2, A3, and A4 was readily achieved with mobile phases containing acetate buffers, the separation of the new antibiotic subcomponents was highly sensitive to variation in mobile phase conditions. The type and composition of organic modifiers, the nature of buffer salts, and the concentration of added electrolytes had profound effects on capacity factors, separation factors, and peak resolution values. Of the numerous chromatographic systems examined, a mobile phase consisting of methanol-water (70:30) and 0.005 M tetrabutylammonium phosphate at pH 3.0 yielded the most satisfactory results for the separation of the subcomponents. Reversed-phase gradient HPLC separation of the dansylated or methylated antibiotic compounds produced superior chromatographic characteristics and the presence of added electrolytes was not a critical factor for achieving separation. Differences in the chromatographic outcome between homologous and structural isomers were interpretated based on a differential solvophobic interaction rationale. Preparative reversed-phase HPLC under optimal conditions enabled isolation of pure samples of the methylated antimycin subcomponents for use in structural studies.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Chromatography","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Abidi, S.L., 1989, Reversed-phase thin-layer chromatography of homologs of Antimycin-A and related derivatives: Journal of Chromatography, v. 464, no. 2, p. 453-458.","productDescription":"453-458","startPage":"453","endPage":"458","numberOfPages":"6","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":134483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"464","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6042eb","contributors":{"authors":[{"text":"Abidi, Sharon L.","contributorId":22305,"corporation":false,"usgs":true,"family":"Abidi","given":"Sharon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":312788,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015445,"text":"70015445 - 1989 - The campi flegrei (Italy) geothermal system: A fluid inclusion study of the mofete and San Vito fields","interactions":[],"lastModifiedDate":"2012-03-12T17:18:56","indexId":"70015445","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"The campi flegrei (Italy) geothermal system: A fluid inclusion study of the mofete and San Vito fields","docAbstract":"A fluid inclusion study of core from the Mofete 1, Mofete 2, Mofete 5, San Vito 1, and San Vito 3 geothermal wells (Campi Flegrei, Campania, Italy) indicates that the hydrothermal minerals were precipitated from aqueous fluids (??CO2) that were moderately saline (3-4 wt.% NaCl equiv.) to hypersaline (> 26 wt.% NaCl equiv.) and at least in part, boiling. Three types of primary fluid inclusions were found in authigenic K-feldspar, quartz, calcite, and epidote: (A) two-phase [liquid (L) + vapor (V)], liquid-rich inclusions with a range of salinity; (B) two-phase (L + V), vaporrich inclusions with low salinity; and (C) three-phase [L + V + crystals (NaCL)], liquid-rich inclusions with hypersalinity. Results of microthermometric and crushing studies are reported for twenty drill core samples taken from the lower portions of the five vertical wells. Data presented for selected core samples reveal a general decrease in porosity and increase in bulk density with increasing depth and temperature. Hydrothermal minerals commonly fill fractures and pore-spaces and define a zonation pattern, similar in all five wells studied, in response to increasing depth (pressure) and temperature. A greenschist facies assemblage, defined by albite + actinolite, gives way to an amphibolite facies, defined by plagioclase (andesine) + hornblende, in the San Vito 1 well at about 380??C. The fluid inclusion salinity values mimic the saline and hypersaline fluids found by drilling. Fluid inclusion V/L homogenization temperatures increase with depth and generally correspond to the extrapolated down-hole temperatures. However, fluid inclusion data for Mofete 5 and mineral assemblage data for San Vito 3, indicate fossil, higher-temperature regimes. A limited 87Sr/86Sr study of leachate (carbonate) and the leached cores shows that for most samples (except San Vito 3) the carbonate deposition has been from slightly 87Sr-enriched fluids and that Sr isotopic exchange has been incomplete. However, San Vito 3 cores show an approach to fluid/rock Sr equilibrium with a fluid similar to modern ocean water in 87Sr/86Sr ratio. The Campi Flegrei volcanic system has evolved undersaturated products, mostly trachyte, and defines a large (??? 12 km) caldera. The hydrothermal system developed in this location can be used as an analog for fossil systems in similar trachytic environments. The potential for ore mineralization is expressed by the recognition, from fluid inclusion and drilling data, of ore-forming environments such as boiling and brine stratification. ?? 1989.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"de, V.B., Belkin, H., Barbieri, M., Chelini, W., Lattanzi, P., Lima, A., and Tolomeo, L., 1989, The campi flegrei (Italy) geothermal system: A fluid inclusion study of the mofete and San Vito fields: Journal of Volcanology and Geothermal Research, v. 36, no. 4, p. 303-326.","startPage":"303","endPage":"326","numberOfPages":"24","costCenters":[],"links":[{"id":224095,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baa00e4b08c986b322673","contributors":{"authors":[{"text":"de, Vivo B.","contributorId":27324,"corporation":false,"usgs":true,"family":"de","given":"Vivo","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":370950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belkin, H. E. 0000-0001-7879-6529","orcid":"https://orcid.org/0000-0001-7879-6529","contributorId":38160,"corporation":false,"usgs":true,"family":"Belkin","given":"H. E.","affiliations":[],"preferred":false,"id":370951,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barbieri, M.","contributorId":73351,"corporation":false,"usgs":true,"family":"Barbieri","given":"M.","affiliations":[],"preferred":false,"id":370954,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chelini, W.","contributorId":45188,"corporation":false,"usgs":true,"family":"Chelini","given":"W.","email":"","affiliations":[],"preferred":false,"id":370953,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lattanzi, P.","contributorId":40034,"corporation":false,"usgs":true,"family":"Lattanzi","given":"P.","affiliations":[],"preferred":false,"id":370952,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lima, A.","contributorId":74884,"corporation":false,"usgs":true,"family":"Lima","given":"A.","affiliations":[],"preferred":false,"id":370955,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tolomeo, L.","contributorId":24639,"corporation":false,"usgs":true,"family":"Tolomeo","given":"L.","email":"","affiliations":[],"preferred":false,"id":370949,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":1003063,"text":"1003063 - 1989 - Seasonal reproductive development of Lampsilis cardium, Amblema plicata plicata, and Potamilus alatus","interactions":[],"lastModifiedDate":"2024-04-12T11:21:01.498993","indexId":"1003063","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2299,"text":"Journal of Freshwater Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal reproductive development of Lampsilis cardium, Amblema plicata plicata, and Potamilus alatus","docAbstract":"<div class=\"hlFld-Abstract\"><p class=\"last\">Adult specimens of three species of freshwater mussels common to the upper Mississippi River were examined histologically to determine seasonal patterns of development in gametogenesis and release of glochidia. Full maturation of gonadal materials in<span>&nbsp;</span><u class=\"uu\">Lampsilis cardium</u><span>&nbsp;</span>(formerly<span>&nbsp;</span><u class=\"uu\">L. ovata ventricosa</u>), a long-term breeder, occurred when ambient river temperatures reached 24° to 26°C, between late July and early August. By mid-August, glochidia were present in the marsupia. Glochidia were released from late May through mid-June of the following year once water temperatures reached 20°C. The long-term breeder<span>&nbsp;</span><u class=\"uu\">Potamilus alatus</u><span>&nbsp;</span>demonstrated full gonadal maturation earlier than seen in<span>&nbsp;</span><u class=\"uu\">L. cardium</u><span>&nbsp;</span>with reproduction completed by late July (26°C). Glochidia of<span>&nbsp;</span><u class=\"uu\">P. alatus</u><span>&nbsp;</span>were released over a period similar to that observed for<span>&nbsp;</span><u class=\"uu\">L. cardium</u>, late May through early July of the following year. Fully mature<span>&nbsp;</span><u class=\"uu\">Amblema plicata plicata</u>, a short-term breeder, were collected from late May through early July (18° to 21°C). Glochidia were were released from early June to early August of the same year.</p></div>","language":"English","publisher":"Taylor and Francis","doi":"10.1080/02705060.1989.9665216","issn":"02705060","usgsCitation":"Holland Bartels, L.E., and Kammer, T.W., 1989, Seasonal reproductive development of Lampsilis cardium, Amblema plicata plicata, and Potamilus alatus: Journal of Freshwater Ecology, v. 5, no. 1, p. 87-92, https://doi.org/10.1080/02705060.1989.9665216.","productDescription":"6 p.","startPage":"87","endPage":"92","numberOfPages":"6","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":130006,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f45d6","contributors":{"authors":[{"text":"Holland Bartels, L. E.","contributorId":71505,"corporation":false,"usgs":true,"family":"Holland Bartels","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":312678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kammer, T. W.","contributorId":9208,"corporation":false,"usgs":true,"family":"Kammer","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":312677,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20070,"text":"ofr89563 - 1989 - Analytical results for ten water-extractable ions from B-horizon soils on St. Thomas and St. Croix, U.S. Virgin Islands and K-Ar ages for seven rocks from St. John and St. Thomas, U.S. Virgin Islands","interactions":[],"lastModifiedDate":"2023-03-21T21:11:00.841197","indexId":"ofr89563","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","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":"89-563","title":"Analytical results for ten water-extractable ions from B-horizon soils on St. Thomas and St. Croix, U.S. Virgin Islands and K-Ar ages for seven rocks from St. John and St. Thomas, U.S. Virgin Islands","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr89563","usgsCitation":"McHugh, J.B., Tucker, R.E., and Alminas, H.V., 1989, Analytical results for ten water-extractable ions from B-horizon soils on St. Thomas and St. Croix, U.S. Virgin Islands and K-Ar ages for seven rocks from St. John and St. Thomas, U.S. Virgin Islands: U.S. Geological Survey Open-File Report 89-563, 19 p., https://doi.org/10.3133/ofr89563.","productDescription":"19 p.","costCenters":[],"links":[{"id":414508,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17721.htm","linkFileType":{"id":5,"text":"html"}},{"id":49624,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0563/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153605,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0563/report-thumb.jpg"}],"otherGeospatial":"St. Croix, St. John, St. Thomas, U.S. Virgin Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -64.91492658697186,\n              17.789936838842877\n            ],\n            [\n              -64.91492658697186,\n              17.665525136535422\n            ],\n            [\n              -64.56613328494335,\n              17.665525136535422\n            ],\n            [\n              -64.56613328494335,\n              17.789936838842877\n            ],\n            [\n              -64.91492658697186,\n              17.789936838842877\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -64.65,\n              18.3765628980681\n            ],\n            [\n              -64.79920519145531,\n              18.3765628980681\n            ],\n            [\n              -64.79920519145531,\n              18.294242756187813\n            ],\n            [\n              -64.65,\n              18.294242756187813\n            ],\n            [\n              -64.65,\n              18.3765628980681\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -65.04663104284987,\n              18.390870721801974\n            ],\n            [\n              -65.04663104284987,\n              18.29215530960927\n            ],\n            [\n              -64.83318371902449,\n              18.29215530960927\n            ],\n            [\n              -64.83318371902449,\n              18.390870721801974\n            ],\n            [\n              -65.04663104284987,\n              18.390870721801974\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c9e9","contributors":{"authors":[{"text":"McHugh, J. B.","contributorId":79462,"corporation":false,"usgs":true,"family":"McHugh","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":182006,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tucker, R. E.","contributorId":50520,"corporation":false,"usgs":true,"family":"Tucker","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":182005,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alminas, H. V.","contributorId":83926,"corporation":false,"usgs":true,"family":"Alminas","given":"H.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":182007,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185834,"text":"70185834 - 1989 - Solubility of jarosite solid solutions precipitated from acid mine waters, Iron Mountain, California","interactions":[],"lastModifiedDate":"2019-10-17T16:40:10","indexId":"70185834","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5350,"text":"Science Geological Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Solubility of jarosite solid solutions precipitated from acid mine waters, Iron Mountain, California","docAbstract":"<p>Because of the common occurrence of 15 to 25 mole percent hydronium substitution on the alkali site in jarosites, it is necessary to consider the hydronium content of jarosites in any attempt at rigorous evaluation of jarosite solubility or of the saturation state of natural waters with respect to jarosite. A Gibbs free energy of 3293.5±2.1 kJ mol-1 is recommended for a jarosite solid solution of composition K.77Na.03(H3O).20Fe3(SO4)2(OH)6. Solubility determinations for a wider range of natural and synthetic jarosite solid solutions will be necessary to quantify the binary and ternary mixing parameters in the (K-Na-H3O) system. In the absence of such studies, molar volume data for endmember minerals indicate that the K-H3O substitution in jarosite is probably closer to ideal mixing than either the Na-K or Na-H3O substitution. <br><br></p>","language":"English","usgsCitation":"Alpers, C.N., Nordstrom, D.K., and Ball, J., 1989, Solubility of jarosite solid solutions precipitated from acid mine waters, Iron Mountain, California: Science Geological Bulletin, v. 42, p. 281-298.","productDescription":"18 p. ","startPage":"281","endPage":"298","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338591,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Iron Mountain","volume":"42","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58dcc820e4b02ff32c68574a","contributors":{"authors":[{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":686854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":686855,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ball, J.W.","contributorId":67507,"corporation":false,"usgs":true,"family":"Ball","given":"J.W.","affiliations":[],"preferred":false,"id":686856,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70015488,"text":"70015488 - 1989 - Review of factors affecting recovery of freshwater stored in saline aquifers","interactions":[],"lastModifiedDate":"2012-03-12T17:18:57","indexId":"70015488","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Review of factors affecting recovery of freshwater stored in saline aquifers","docAbstract":"A simulation analysis reported previously, and summarized herein, identified the effects of various geohydrologic and operational factors on recoverability of the injected water. Buoyancy stratification, downgradient advection, and hydrodynamic dispersion are the principal natural processes that reduce the amount of injected water that can be recovered. Buoyancy stratification is shown to depend on injection-zone permeability and the density contrast between injected and saline native water. Downgradient advection occurs as a result of natural or induced hydraulic gradients in the aquifer. Hydrodynamic dispersion reduces recovery efficiency by mixing some of the injected water with native saline aquifer water. In computer simulations, the relation of recovery efficiency to volume injected and its improvement during successive injection-recovery cycles was shown to depend on changes in the degree of hydrodynamic dispersion that occurs. Additional aspects of the subject are discussed.","conferenceTitle":"Artificial Recharge of Ground Water - Proceedings of the International Symposium","conferenceDate":"23 August 1988 through 27 August 1988","conferenceLocation":"Anaheim, CA, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0872627136","usgsCitation":"Merritt, M.L., 1989, Review of factors affecting recovery of freshwater stored in saline aquifers, Artificial Recharge of Ground Water - Proceedings of the International Symposium, Anaheim, CA, USA, 23 August 1988 through 27 August 1988, p. 367-375.","startPage":"367","endPage":"375","numberOfPages":"9","costCenters":[],"links":[{"id":223991,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aac65e4b0c8380cd86cef","contributors":{"authors":[{"text":"Merritt, Michael L.","contributorId":29392,"corporation":false,"usgs":true,"family":"Merritt","given":"Michael","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":371067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015501,"text":"70015501 - 1989 - The non-participation of organic sulphur in acid mine drainage generation","interactions":[],"lastModifiedDate":"2019-06-11T11:24:37","indexId":"70015501","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1538,"text":"Environmental Geochemistry and Health","active":true,"publicationSubtype":{"id":10}},"title":"The non-participation of organic sulphur in acid mine drainage generation","docAbstract":"<p>Acid mine drainage is commonly associated with land disturbances that encounter and expose iron sulphides to oxidising atmospheric conditions. The attendant acidic conditions solubilise a host of trace metals. Within this flow regime the potential exists to contaminate surface drinking water supplies with a variety of trace materials. Accordingly, in evaluating the applications for mines located in the headwaters of water sheds, the pre-mining prediction of the occurrence of acid mine drainage is of paramount importance. There is general agreement among investigators that coal organic sulphur is a nonparticipant in acid mine drainage generation; however, there is no scientific documentation to support this consensus. Using simulated weathering, kinetic, mass balance, petrographic analysis and a peroxide oxidation procedure, coal organic sulphur is shown to be a nonparticipant in acid mine drainage generation. Calculations for assessing the acid-generating potential of a sedimentary rock should not include organic sulphur content.</p>","language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF01758669","issn":"02694042","usgsCitation":"Casagrande, D., Finkelman, R.B., and Caruccio, F., 1989, The non-participation of organic sulphur in acid mine drainage generation: Environmental Geochemistry and Health, v. 11, no. 3-4, p. 187-192, https://doi.org/10.1007/BF01758669.","productDescription":"6 p.","startPage":"187","endPage":"192","numberOfPages":"6","costCenters":[],"links":[{"id":224158,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae22e4b08c986b323f1f","contributors":{"authors":[{"text":"Casagrande, D.J.","contributorId":13378,"corporation":false,"usgs":true,"family":"Casagrande","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":371087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finkelman, R. B.","contributorId":20341,"corporation":false,"usgs":true,"family":"Finkelman","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":371088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Caruccio, F.T.","contributorId":21695,"corporation":false,"usgs":true,"family":"Caruccio","given":"F.T.","email":"","affiliations":[],"preferred":false,"id":371089,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70015497,"text":"70015497 - 1989 - Artificial reef observations from a manned submersible off southeast Florida","interactions":[],"lastModifiedDate":"2012-03-12T17:18:56","indexId":"70015497","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1106,"text":"Bulletin of Marine Science","active":true,"publicationSubtype":{"id":10}},"title":"Artificial reef observations from a manned submersible off southeast Florida","docAbstract":"Examination of 16 artificial reef structures in depths ranging from 30-120m indicated that the highest numbers of fish are found around reefs in water shallower than 46m. Fewer fish, especially those with tropical coral reef affinities, <46m was probably caused by a thermocline. Algae and reef community encrusters, abundant on shallower structures, were absent below 46m. Structures that penetrated above the thermocline, such as upright oil rigs and a hopper barge, were also effective reefs. The open structure and high profile of the rigs enhance their use as artificial reefs by providing a range of well-aerated habitats. Greatest diversity and numbers of fish were observed at the Miami sewer outfall. -from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Marine Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00074977","usgsCitation":"Shinn, E., and Wicklund, R., 1989, Artificial reef observations from a manned submersible off southeast Florida: Bulletin of Marine Science, v. 44, no. 2, p. 1041-1050.","startPage":"1041","endPage":"1050","numberOfPages":"10","costCenters":[],"links":[{"id":224154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059edb1e4b0c8380cd49955","contributors":{"authors":[{"text":"Shinn, E.A.","contributorId":38610,"corporation":false,"usgs":true,"family":"Shinn","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":371080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wicklund, R.I.","contributorId":89669,"corporation":false,"usgs":true,"family":"Wicklund","given":"R.I.","email":"","affiliations":[],"preferred":false,"id":371081,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1013718,"text":"1013718 - 1989 - Trammel net efficiency in the coastal waters of Everglades National Park","interactions":[],"lastModifiedDate":"2012-02-02T00:04:10","indexId":"1013718","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1106,"text":"Bulletin of Marine Science","active":true,"publicationSubtype":{"id":10}},"title":"Trammel net efficiency in the coastal waters of Everglades National Park","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Marine Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"89-042/NF","usgsCitation":"Dewey, M.R., Mengel, L., Funicelli, N., Bryant, H., Ludwig, G., and Meineke, D., 1989, Trammel net efficiency in the coastal waters of Everglades National Park: Bulletin of Marine Science, v. 44, no. 1, p. 516-517.","productDescription":"p. 516-517","startPage":"516","endPage":"517","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6270e9","contributors":{"authors":[{"text":"Dewey, M. R.","contributorId":48908,"corporation":false,"usgs":true,"family":"Dewey","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":319117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mengel, L.J.","contributorId":54141,"corporation":false,"usgs":true,"family":"Mengel","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":319118,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Funicelli, N.A.","contributorId":13573,"corporation":false,"usgs":true,"family":"Funicelli","given":"N.A.","email":"","affiliations":[],"preferred":false,"id":319115,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bryant, H.E.","contributorId":77092,"corporation":false,"usgs":true,"family":"Bryant","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":319120,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ludwig, G.M.","contributorId":70721,"corporation":false,"usgs":true,"family":"Ludwig","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":319119,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Meineke, D.A.","contributorId":30178,"corporation":false,"usgs":true,"family":"Meineke","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":319116,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70015362,"text":"70015362 - 1989 - Chemistry and origin of minor and trace elements in vitrinite concentrates from a rank series from the eastern United States, England, and Australia","interactions":[],"lastModifiedDate":"2024-02-23T01:06:18.685502","indexId":"70015362","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2033,"text":"International Journal of Coal Geology","active":true,"publicationSubtype":{"id":10}},"title":"Chemistry and origin of minor and trace elements in vitrinite concentrates from a rank series from the eastern United States, England, and Australia","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"aep-abstract-id10\" class=\"abstract author\"><div id=\"aep-abstract-sec-id11\"><p>A rank series consisting of twelve vitrinite concentrates and companion whole-coal samples from mined coal beds in the eastern United States, England, and Australia were analyzed for C, H, N, O, ash, and 47 trace and minor elements by standard elemental, instrumental neutron activation analysis (INAA), and direct-current-arc spectrographic (DCAS) techniques. The reflectance of vitrinite, atomic H:C and O:C, and ash-free carbon data were used to determine ranks that range from high-volatile C bituminous coal to meta-anthracite. A van Krevelen (atomic H:C vs. O:C) diagram of the vitrinite concentrates shows a smooth curve having its lowest point at H:C = 0.18 and O:C = 0.01. This improves the van Krevelen diagram by the addition of our vitrinite concentrate from meta-anthracite from the Narragansett basin of New England.</p><p>Boron content (400–450 ppm) in two Illinois basin vitrinite concentrates was about an order of magnitude higher than B contents in other concentrates analyzed. We attribute this to marine origin or hydrothermal activity. The alkaline-earth elements Ca, Mg and Ba (DCAS) have higher concentrations in our vitrinite concentrates from bituminous coals of the Appalachian basin, than they do in vitrinite concentrates from the marine-roofed bituminous coals of the Illinois basin; therefore, a nonmarine origin for these alkaline-earth elements is postulated for the Appalachian basin coals. An ion-exchange mechanism due to high concentrations of these elements as ions in diagenetic water, but probably not recent ground water, may be responsible for the relatively high values of these elements in Appalachian concentrates. Higher concentrations of Ni and Cr in one of the English vitrinite concentrates and of Zr in the Australian concentrate probably indicate organic association and detrital influence, respectively.</p></div></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0166-5162(89)90105-5","issn":"01665162","usgsCitation":"Lyons, P., Palmer, C., Bostick, N.H., Fletcher, J., Dulong, F., Brown, F.W., Brown, Z.A., Krasnow, M., and Romankiw, L., 1989, Chemistry and origin of minor and trace elements in vitrinite concentrates from a rank series from the eastern United States, England, and Australia: International Journal of Coal Geology, v. 13, no. 1-4, p. 481-527, https://doi.org/10.1016/0166-5162(89)90105-5.","productDescription":"47 p.","startPage":"481","endPage":"527","numberOfPages":"47","costCenters":[],"links":[{"id":224416,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f5a5e4b0c8380cd4c33c","contributors":{"authors":[{"text":"Lyons, P.C.","contributorId":87285,"corporation":false,"usgs":true,"family":"Lyons","given":"P.C.","email":"","affiliations":[],"preferred":false,"id":370747,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Palmer, C.A.","contributorId":81894,"corporation":false,"usgs":true,"family":"Palmer","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":370744,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bostick, N. H.","contributorId":67099,"corporation":false,"usgs":true,"family":"Bostick","given":"N.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":370742,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fletcher, J.D.","contributorId":24928,"corporation":false,"usgs":true,"family":"Fletcher","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":370740,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dulong, F.T.","contributorId":81490,"corporation":false,"usgs":true,"family":"Dulong","given":"F.T.","affiliations":[],"preferred":false,"id":370743,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brown, F. W.","contributorId":92653,"corporation":false,"usgs":true,"family":"Brown","given":"F.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":370748,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Brown, Z. A.","contributorId":82708,"corporation":false,"usgs":true,"family":"Brown","given":"Z.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":370745,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Krasnow, M.R.","contributorId":25952,"corporation":false,"usgs":true,"family":"Krasnow","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":370741,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Romankiw, L.A.","contributorId":85724,"corporation":false,"usgs":true,"family":"Romankiw","given":"L.A.","affiliations":[],"preferred":false,"id":370746,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70015519,"text":"70015519 - 1989 - Geochemical comparison of ground water in areas of New England, New York, and Pennsylvania","interactions":[],"lastModifiedDate":"2024-03-19T23:06:15.00875","indexId":"70015519","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical comparison of ground water in areas of New England, New York, and Pennsylvania","docAbstract":"In New England, the ground-water geochemistry results mainly from the reaction of CO2-charged water with feldspar and other primary silicates. Water in the New England bedrock is more highly evolved geochemically than water in the drift, presumably as a result of its longer residence time. In the New York area, the geochemistry of water in both types of aquifers results mainly from carbonate-mineral dissolution. Water in most glacial drift and bedrock is saturated with respect to calcite. In some parts of New York, the dissolution of evaporite minerals has a marked effect on the water chemistry of the bedrock. In most of the Pennsylvania area, the geochemistry of water in both types of aquifers indicates that, although carbonate minerals are the principal reactants, their influence on water chemistry is less than in New York. In parts of Pennsylvania, chemical differences between ground water from drift and ground water from bedrock are attributed to a higher proportion of reactive minerals in the drift than in the local bedrock as a result of glacial transport. -from Author","language":"English","publisher":"National Groundwater Association","issn":"0017467X","usgsCitation":"Rogers, R., 1989, Geochemical comparison of ground water in areas of New England, New York, and Pennsylvania: Groundwater, v. 27, no. 5, p. 690-712.","productDescription":"23 p.","startPage":"690","endPage":"712","numberOfPages":"23","costCenters":[],"links":[{"id":223606,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a15f3e4b0c8380cd54fcc","contributors":{"authors":[{"text":"Rogers, R.J.","contributorId":63024,"corporation":false,"usgs":true,"family":"Rogers","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":371139,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003828,"text":"1003828 - 1989 - Presumed drowning of Aleutian Canada geese on the Pacific coast of California and Oregon","interactions":[],"lastModifiedDate":"2017-09-19T11:37:35","indexId":"1003828","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Presumed drowning of Aleutian Canada geese on the Pacific coast of California and Oregon","docAbstract":"<p><span>Carcasses of 42 and 17 Aleutian Canada geese (</span><i>Branta canadensis leucopareia</i><span>), a federally listed endangered species, were found on ocean beaches near Crescent City, California, and near Pacific City, Oregon, respectively, following severe storms. Necropsies and other information suggest that the birds were flushed during the storms and somehow entered the water where they were washed into the surf and drowned.</span></p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-25.2.276","usgsCitation":"Springer, P.F., Lowe, R.W., Stroud, R.K., and Gullett, P.A., 1989, Presumed drowning of Aleutian Canada geese on the Pacific coast of California and Oregon: Journal of Wildlife Diseases, v. 25, no. 2, p. 276-279, https://doi.org/10.7589/0090-3558-25.2.276.","productDescription":"4 p.","startPage":"276","endPage":"279","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":486829,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-25.2.276","text":"Publisher Index 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F.","contributorId":70445,"corporation":false,"usgs":true,"family":"Springer","given":"Paul","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":314406,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lowe, Roy W.","contributorId":50847,"corporation":false,"usgs":false,"family":"Lowe","given":"Roy","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":314405,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stroud, Richard K.","contributorId":102837,"corporation":false,"usgs":true,"family":"Stroud","given":"Richard","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":314404,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gullett, Patricia A.","contributorId":65428,"corporation":false,"usgs":true,"family":"Gullett","given":"Patricia","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":314407,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70014938,"text":"70014938 - 1989 - Artificial recharge to the Floridan aquifer system, Orlando Area, Central Florida","interactions":[],"lastModifiedDate":"2012-03-12T17:18:58","indexId":"70014938","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Artificial recharge to the Floridan aquifer system, Orlando Area, Central Florida","docAbstract":"Approximately 400 drainage wells exist in Orange County, central Florida. The rate of recharge through drainage wells is limited by the rate of surface flow to the wells; the hydraulic properties of weirs, overflow pipes, and well casings; or the water level above the top of the casing. The rate commonly is not limited by the hydraulic properties of the very transmissive aquifer system.","conferenceTitle":"Artificial Recharge of Ground Water - Proceedings of the International Symposium","conferenceDate":"23 August 1988 through 27 August 1988","conferenceLocation":"Anaheim, CA, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0872627136","usgsCitation":"German, E.R., and Bradner, L.A., 1989, Artificial recharge to the Floridan aquifer system, Orlando Area, Central Florida, Artificial Recharge of Ground Water - Proceedings of the International Symposium, Anaheim, CA, USA, 23 August 1988 through 27 August 1988, p. 360-366.","startPage":"360","endPage":"366","numberOfPages":"7","costCenters":[],"links":[{"id":224227,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059edb1e4b0c8380cd49951","contributors":{"authors":[{"text":"German, E. R.","contributorId":86315,"corporation":false,"usgs":true,"family":"German","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":369658,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradner, L. A.","contributorId":21925,"corporation":false,"usgs":true,"family":"Bradner","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":369657,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003554,"text":"1003554 - 1989 - A macrophyte submodel for aquatic ecosystems","interactions":[],"lastModifiedDate":"2023-02-28T17:51:47.537351","indexId":"1003554","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":861,"text":"Aquatic Botany","active":true,"publicationSubtype":{"id":10}},"title":"A macrophyte submodel for aquatic ecosystems","docAbstract":"<p><span>A macrophyte submodel has been incorporated and tested in CE-QUAL-R1, a one-dimensional, vertically averaged model of reservoir water quality. A quasi two-dimensional scheme was necessary to represent the spatial relationship of macrophytes in reservoirs adequately. The macrophyte processes modeled were photosynthesis, dark respiration, excretion and nonpredatory mortality. Process equations for photosynthesis as a function of light and temperature, and dark respiration as a function of temperature were tested using data from laboratory studies. The submodel was field tested, along with other components of CE-QUAL-R1, using data collected at Eau Galle Reservoir, WI, U.S.A.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0304-3770(89)90037-5","usgsCitation":"Collins, C.D., and Wlosinski, J.H., 1989, A macrophyte submodel for aquatic ecosystems: Aquatic Botany, v. 33, no. 3-4, p. 191-206, https://doi.org/10.1016/0304-3770(89)90037-5.","productDescription":"16 p.","startPage":"191","endPage":"206","numberOfPages":"16","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":131379,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Eau Galle Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -92.25092258188174,\n              44.86636499940943\n            ],\n            [\n              -92.25092258188174,\n              44.85564026067513\n            ],\n            [\n              -92.23459609225418,\n              44.85564026067513\n            ],\n            [\n              -92.23459609225418,\n              44.86636499940943\n            ],\n            [\n              -92.25092258188174,\n              44.86636499940943\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"33","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae222","contributors":{"authors":[{"text":"Collins, Carol Desormeau","contributorId":95020,"corporation":false,"usgs":true,"family":"Collins","given":"Carol","email":"","middleInitial":"Desormeau","affiliations":[],"preferred":false,"id":313523,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wlosinski, Joseph H.","contributorId":75488,"corporation":false,"usgs":true,"family":"Wlosinski","given":"Joseph","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":313522,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015275,"text":"70015275 - 1989 - Flow separation of currents in shallow water","interactions":[],"lastModifiedDate":"2018-04-20T11:55:17","indexId":"70015275","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Flow separation of currents in shallow water","docAbstract":"Flow separation of currents in shallow coastal areas is investigated using a boundary layer model for two-dimensional (depth-averaged) tidal flow past an elliptic headland. If the shoaling region near the coast is narrow compared to the scale of the headland, bottom friction causes the flow to separate just downstream of the point where the pressure gradient switches from favoring to adverse. As long as the shoaling region at the coast is well resolved, the inclusion of eddy viscosity and a no-slip boundary condition have no effect on this result. An approximate analytic solution for the pressure gradient along the boundary is obtained by assuming the flow away from the immediate vicinity of the boundary is irrotational. On the basis of the pressure gradient obtained from the irrotational flow solution, flow separation is a strong function of the headland aspect ratio, an equivalent Reynolds number, and a Keulegan-Carpenter number.","conferenceTitle":"Estuarine and Coastal Modeling - Proceedings of the Conference","conferenceDate":"November 15-17, 1989","conferenceLocation":"Newport, RI","language":"English","publisher":"American Society of Civil Engineers","publisherLocation":"Boston, MA, United States","isbn":"0872627586","usgsCitation":"Signell, R.P., 1989, Flow separation of currents in shallow water, Estuarine and Coastal Modeling - Proceedings of the Conference, Newport, RI, November 15-17, 1989, p. 278-290.","startPage":"278","endPage":"290","numberOfPages":"13","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":223926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1252e4b0c8380cd54271","contributors":{"authors":[{"text":"Signell, Richard P. rsignell@usgs.gov","contributorId":1435,"corporation":false,"usgs":true,"family":"Signell","given":"Richard","email":"rsignell@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":370520,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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