{"pageNumber":"2020","pageRowStart":"50475","pageSize":"25","recordCount":68919,"records":[{"id":70156298,"text":"70156298 - 1985 - Seasonal cycles of zooplankton from San Francisco Bay","interactions":[],"lastModifiedDate":"2021-04-01T20:43:08.2016","indexId":"70156298","displayToPublicDate":"1986-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal cycles of zooplankton from San Francisco Bay","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>The two estuarine systems composing San Francisco Bay have distinct zooplankton communities and seasonal population dynamics. In the South Bay, a shallow lagoon-type estuary, the copepods<span>&nbsp;</span><i>Acartia</i><span>&nbsp;</span>spp. and<span>&nbsp;</span><i>Oithona davisae</i><span>&nbsp;</span>dominate. As in estuaries along the northeast coast of the U.S., there is a seasonal succession involving the replacement of a cold-season<span>&nbsp;</span><i>Acartia</i><span>&nbsp;</span>species (<i>A. clausi s.l.</i>) by a warm-season species (<i>A. californiensis</i>), presumably resulting from the differential production and hatching of dormant eggs.<span>&nbsp;</span><i>Oithona davisae</i><span>&nbsp;</span>is most abundant during the fall. Copepods of northern San Francisco Bay, a partially-mixed estuary of the Sacramento-San Joaquin Rivers, organize into discrete populations according to salinity distribution:<span>&nbsp;</span><i>Sinocalanus doerrii</i><span>&nbsp;</span>(a recently introduced species) at the riverine boundary, Eurytemora affinis in the oligohaline mixing zone,<span>&nbsp;</span><i>Acartia</i><span>&nbsp;</span>spp. in polyhaline waters (18–30\\%), and neritic species (e.g.,<span>&nbsp;</span><i>Paracalanus parvus</i>) at the seaward boundary.<span>&nbsp;</span><i>Sinocalanus doerrii</i><span>&nbsp;</span>and<span>&nbsp;</span><i>E. affinis</i><span>&nbsp;</span>are present year-round.<span>&nbsp;</span><i>Acartia clausi s.l.</i><span>&nbsp;</span>is present almost year-round in the northern reach, and<span>&nbsp;</span><i>A. californiensis</i><span>&nbsp;</span>occurs only briefly there in summer-fall. The difference in succession of<span>&nbsp;</span><i>Acartia</i><span>&nbsp;</span>species between the two regions of San Francisco Bay may reflect differences in the seasonal temperature cycle (the South Bay warms earlier), and the perennial transport of<span>&nbsp;</span><i>A. clausi s.l.</i><span>&nbsp;</span>into the northern reach from the seaward boundary by nontidal advection.</p><p>Large numbers (&gt;10<sup>6</sup><span>&nbsp;</span>m<sup>−3</sup>) of net microzooplankton (&gt;64 µm), in cluding the rotifer<span>&nbsp;</span><i>Synchaeta</i><span>&nbsp;</span>sp. and three species of tintinnid ciliates, occur in the South Bay and in the seaward northern reach where salinity exceeds about 5–10‰ Maximum densities of these microzooplankton are associated with high concentrations of chlorophyll. Meroplankton (of gastropods, bivalves, barnacles, and polychaetes) constitute a large fraction of zooplankton biomass in the South Bay during winter-spring and in the northern reach during summer-fall.</p><p>Seasonal cycles of zooplankton abundance appear to be constant among years (1978–1981) and are similar in the deep (&gt;10 m) channels and lateral shoals (&lt;3 m). The seasonal zooplankton community dynamics are discussed in relation to: (1) river discharge which alters salinity distribution and residence time of plankton; (2) temperature which induces production and hatching of dormant copepod eggs; (3) coastal hydrography which brings neritic copepods of different zoogeographic affinities into the bay; and (4) seasonal cycles of phytoplankton.</p></div></div><div id=\"cobranding-and-download-availability-text\" class=\"note test-pdf-link\"><br></div>","publisher":"Springer","doi":"10.1007/BF00048694","usgsCitation":"Ambler, J.W., Cloern, J.E., and Hutchinson, A., 1985, Seasonal cycles of zooplankton from San Francisco Bay: Hydrobiologia, v. 129, p. 177-197, https://doi.org/10.1007/BF00048694.","productDescription":"21 p.","startPage":"177","endPage":"197","numberOfPages":"21","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":306912,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.54974365234374,\n              37.43125050179356\n            ],\n            [\n              -122.54974365234374,\n              38.16047628099622\n            ],\n            [\n              -121.63787841796875,\n              38.156156969924915\n            ],\n            [\n              -121.9207763671875,\n              37.41816326969145\n            ],\n            [\n              -122.54974365234374,\n              37.43125050179356\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"129","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"579889c0e4b0589fa1c6bb1a","contributors":{"authors":[{"text":"Ambler, Julie W.","contributorId":23279,"corporation":false,"usgs":true,"family":"Ambler","given":"Julie","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":568552,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":568553,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hutchinson, Anne","contributorId":45316,"corporation":false,"usgs":true,"family":"Hutchinson","given":"Anne","email":"","affiliations":[],"preferred":false,"id":568554,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70156916,"text":"70156916 - 1985 - Remote sensing of tidal chlorophyll-a variations in estuaries","interactions":[],"lastModifiedDate":"2020-01-20T06:45:49","indexId":"70156916","displayToPublicDate":"1986-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2068,"text":"International Journal of Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Remote sensing of tidal chlorophyll-a variations in estuaries","docAbstract":"<p>Simultaneous acquisition of surface chlorophyll-a concentrations for 39 samples from boats and Daedalus 1260 Multispectral Scanner data from a U-2 aircraft was conducted in the northern reaches of San Francisco Bay on 28 August 1980. These data were used to develop regression models for predicting surface chlorophyll-a concentrations over the study area for ebb-tide (8.40 a.m. P.D.T. (Pacific Daylight Time)) and flood-tide (3.10 p.m. P.D.T.) conditions. After selection of a single &lsquo;best fitting&rsquo; model for both morning and afternoon data sets, the chlorophyll-a concentration was predicted for ebb and flood tide for the entire study area at approximately 40m &times; 40m resolution. The predicted spatial display of chlorophyll-a revealed a localized area of high phytoplankton biomass that has been inferred from field surveys and appears to be a common summer phenomenon.</p>\n<p class=\"last\">Knowledge of the distribution of phytoplankton and the location of this zone of high biomass is valuable in establishing management policies for this ecologically important estuary. Furthermore, the techniques used here may provide an alternative cost-effective method for assessing water-quality conditions and they may prove useful for studying spatial variations (patchiness) and seasonal variations in phytoplankton biomass in other estuaries and coastal waters.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/01431168508948318","usgsCitation":"Catts, G.P., Khorram, S., Cloern, J.E., Knight, A.W., and Degloria, S.D., 1985, Remote sensing of tidal chlorophyll-a variations in estuaries: International Journal of Remote Sensing, v. 6, no. 11, p. 1685-1706, https://doi.org/10.1080/01431168508948318.","productDescription":"22 p.","startPage":"1685","endPage":"1706","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1980-08-28","temporalEnd":"1980-08-28","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":307808,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.00292968749999,\n              37.339591851359174\n            ],\n            [\n              -121.83837890625,\n              37.339591851359174\n            ],\n            [\n              -121.83837890625,\n              38.156156969924915\n            ],\n            [\n              -123.00292968749999,\n              38.156156969924915\n            ],\n            [\n              -123.00292968749999,\n              37.339591851359174\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"11","noUsgsAuthors":false,"publicationDate":"2007-04-27","publicationStatus":"PW","scienceBaseUri":"560bb6f4e4b058f706e53e4c","contributors":{"authors":[{"text":"Catts, Glenn P.","contributorId":147307,"corporation":false,"usgs":false,"family":"Catts","given":"Glenn","email":"","middleInitial":"P.","affiliations":[{"id":7091,"text":"North Carolina State University","active":true,"usgs":false}],"preferred":false,"id":571138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Khorram, Siamak","contributorId":147308,"corporation":false,"usgs":false,"family":"Khorram","given":"Siamak","email":"","affiliations":[{"id":7091,"text":"North Carolina State University","active":true,"usgs":false}],"preferred":false,"id":571139,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":571140,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Knight, Allen W.","contributorId":147309,"corporation":false,"usgs":false,"family":"Knight","given":"Allen","email":"","middleInitial":"W.","affiliations":[{"id":7082,"text":"University of California - Davis","active":true,"usgs":false}],"preferred":false,"id":571141,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Degloria, Stephen D.","contributorId":147310,"corporation":false,"usgs":false,"family":"Degloria","given":"Stephen","email":"","middleInitial":"D.","affiliations":[{"id":13243,"text":"University of California Berkeley","active":true,"usgs":false}],"preferred":false,"id":571142,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70236860,"text":"70236860 - 1985 - Automated derivation of hydrologic basin characteristics from digital elevation model data","interactions":[],"lastModifiedDate":"2022-09-20T15:05:54.578789","indexId":"70236860","displayToPublicDate":"1985-12-31T09:49:07","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Automated derivation of hydrologic basin characteristics from digital elevation model data","docAbstract":"<p>Digital elevation model (DEM) data in a raster format can be used to automatically derive the drainage characteristics of an area. A procedure has been designed that is capable of operating on matrices of elevation data having no algorithmically imposed size limit, while performing within the resolution and accuracy tolerances of the DEM data. </p><p>Each cell is processed as the center of a 3- by 3-cell spatial window in the raster elevation data. If a cell is a local minimum in comparison with two of its non-adjacent neighbors, it is labeled as a drainage cell. The linkages of the drainage cells within user-specified distance and elevation thresholds are established in a separate process. The products of these processing steps are digital masks of the drainage cells and the watershed basins, both in raster format. </p><p>A drainage cell mask derived using this procedure is useful in computing slope values for a raster data base. Slope has traditionally been calculated for each cell by fitting a plane through the eight nearest cells. However, if the terrain represented by these cells is V-shaped, such as a gully, a plane does not fit well; in fact, the desired slope value is the slope along the bottom of the gully, regardless of the steepness of the gully sides. The automated drainage process will label such a cell as a drainage cell, and its slope can then be computed from the elevation values of neighboring drainage cells. </p>","largerWorkTitle":"Auto-Carto VII: Proceedings of the digital representations of spatial knowledge","conferenceTitle":"Auto-Carto VII: Digital Representations of Spatial Knowledge","conferenceDate":"Mar 11-14, 1985","conferenceLocation":"Washington D.C.","language":"English","publisher":"Cartography and Geographic Information Society","usgsCitation":"Jenson, S.K., 1985, Automated derivation of hydrologic basin characteristics from digital elevation model data, <i>in</i> Auto-Carto VII: Proceedings of the digital representations of spatial knowledge, Washington D.C., Mar 11-14, 1985, p. 301-310.","productDescription":"10 p.","startPage":"301","endPage":"310","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":407057,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://cartogis.org/docs/proceedings/archive/auto-carto-7/index.html"},{"id":407058,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Jenson, Susan K.","contributorId":66859,"corporation":false,"usgs":true,"family":"Jenson","given":"Susan","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":852389,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70189508,"text":"70189508 - 1985 - An investigation of hydraulic conductivity estimation in a ground-water flow study of Northern Long Valley, New Jersey","interactions":[],"lastModifiedDate":"2017-07-14T09:10:54","indexId":"70189508","displayToPublicDate":"1985-12-31T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":21,"text":"Thesis"},"publicationSubtype":{"id":28,"text":"Thesis"},"title":"An investigation of hydraulic conductivity estimation in a ground-water flow study of Northern Long Valley, New Jersey","docAbstract":"<p><span>The purpose of this study was to develop a methodology to be used to investigate the aquifer characteristics and water supply potential of an aquifer system. In particular, the geohydrology of northern Long Valley, New Jersey, was investigated. Geohydrologic data were collected and analyzed to characterize the site. Analysis was accomplished by interpreting the available data and by using a numerical simulation of the watertable aquifer. Special attention was given to the estimation of hydraulic conductivity values and hydraulic conductivity structure which together define the hydraulic conductivity of the modeled aquifer. Hydraulic conductivity and all other aspects of the system were first estimated using the trial-and-error method of calibration. The estimation of hydraulic conductivity was improved using a least squares method to estimate hydraulic conductivity values and by improvements in the parameter structure. These efforts improved the calibration of the model far more than a preceding period of similar effort using the trial-and-error method of calibration. In addition, the proposed method provides statistical information on the reliability of estimated hydraulic conductivity values, calculated heads, and calculated flows. The methodology developed and applied in this work proved to be of substantial value in the evaluation of the aquifer considered.</span></p>","language":"English","publisher":"Princeton University","usgsCitation":"Hill, M.C., 1985, An investigation of hydraulic conductivity estimation in a ground-water flow study of Northern Long Valley, New Jersey, 364.","productDescription":"364","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":343839,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5969d82fe4b0d1f9f060a1b2","contributors":{"authors":[{"text":"Hill, Mary C. mchill@usgs.gov","contributorId":974,"corporation":false,"usgs":true,"family":"Hill","given":"Mary","email":"mchill@usgs.gov","middleInitial":"C.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":704962,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70193880,"text":"70193880 - 1985 - Population biology of bluegills, Lepomis macrochirus, in lotic habitats on the irrigated San Joaquin Valley floor","interactions":[],"lastModifiedDate":"2018-09-26T10:02:03","indexId":"70193880","displayToPublicDate":"1985-12-31T00:00:00","publicationYear":"1985","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":"Population biology of bluegills, Lepomis macrochirus, in lotic habitats on the irrigated San Joaquin Valley floor","docAbstract":"<p>Rapid expansion of irrigated agriculture in the western United States has prompted concerns for aquatic resources. Although the impacts of irrigation activities on quality and quantity of river water are well documented (e.g., high turbidity from soil erosion, eutrophication from nutrient runoff, pesticide contamination, reduced dis- charge), their effects on fish populations are still poorly understood. We studied the food, growth, and relative weight (a measure of body condition) of bluegills, Lepo- mis macrochirus, in relation to environmental factors in reaches of the San Joaquin and Merced rivers that have been affected to varying degrees by irrigation return flows. Fry of bluegills ate mostly cladocerans and copepods; fingerlings and larger fish ate immature aquatic insects, terrestrial insects, amphipods, and mollusks. Bluegill stomachs were fuller and contained a higher diversity of forage taxa in habitats with low turbidity and conductivity, weak buffering capacity, and low nutrient levels; bluegills also ate a more diverse diet where the potential forage supply (benthic macroinvertebrates) was most diverse. Bluegills attained mean total lengths of about 42 mm at age I, 86 mm at age 11, 116 mm at age III, 153 mm at age IV, and 166 mm at age V. Mean relative weight ranged from 96-111. Growth rate and relative weight were not significantly correlated with environmental or dietary variables. On the basis of our study, we concluded that environmental degradation from irrigation activities affected the diet of bluegills primarily by modifying the food supply, but growth rate and body condition were not affected.</p>","language":"English","publisher":"California Department of Fish and Game","usgsCitation":"Saiki, M.K., and Schmitt, C., 1985, Population biology of bluegills, Lepomis macrochirus, in lotic habitats on the irrigated San Joaquin Valley floor: California Fish and Game, v. 71, no. 4, p. 225-244.","productDescription":"20 p.","startPage":"225","endPage":"244","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":348359,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley floor","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.95373535156249,\n              38.14751758025121\n            ],\n            [\n              -120.75622558593749,\n              36.47872381162464\n            ],\n            [\n              -119.0643310546875,\n              36.50963615733049\n            ],\n            [\n              -120.6683349609375,\n              38.14319750166766\n            ],\n            [\n              -121.95373535156249,\n              38.14751758025121\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"71","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a082a52e4b09af898c8ea21","contributors":{"authors":[{"text":"Saiki, M. K.","contributorId":28917,"corporation":false,"usgs":true,"family":"Saiki","given":"M.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":720870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmitt, C. J. 0000-0001-6804-2360","orcid":"https://orcid.org/0000-0001-6804-2360","contributorId":56339,"corporation":false,"usgs":true,"family":"Schmitt","given":"C. J.","affiliations":[],"preferred":false,"id":720871,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70169936,"text":"70169936 - 1985 - Iowa: a summary of water-resources activities of the United States Department of the Interior Geological Survey","interactions":[],"lastModifiedDate":"2016-03-30T14:58:16","indexId":"70169936","displayToPublicDate":"1985-12-01T16:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Iowa: a summary of water-resources activities of the United States Department of the Interior Geological Survey","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City, IA","doi":"10.3133/70169936","usgsCitation":"Karsten, R., 1985, Iowa: a summary of water-resources activities of the United States Department of the Interior Geological Survey, https://doi.org/10.3133/70169936.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":319653,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56fcffe1e4b0a6037df2c5b1","contributors":{"authors":[{"text":"Karsten, R.A.","contributorId":51755,"corporation":false,"usgs":true,"family":"Karsten","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":625681,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120920,"text":"70120920 - 1985 - Plant water status relationships among major floodplain sites of the Flathead River, Montana","interactions":[],"lastModifiedDate":"2014-08-18T13:19:21","indexId":"70120920","displayToPublicDate":"1985-12-01T13:17:17","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Plant water status relationships among major floodplain sites of the Flathead River, Montana","docAbstract":"Water status measurements of dominant species from major floodplain plant community types of the North Fork Flathead River, Montana were used to test the accuracy of site moisture gradient relationships postulated from floristic ordinations and site water balance estimates. Analysis of variance tests showed significant differences among the average predawn xylem pressure potential (ψp) of species in several community types. However, additional analyses failed to indicate a significant degree of association between averaged predawn Yp measurements and either floristic ordination or site water balance results. Sixty eight percent of 22 trials comparing the diurnal average ψp of the same species in different community types on the same day were less negative for a species in the wetter community types as predicted by floristic ordinations. Similarly, 64% of the trials indicated that the diurnal average stomatal conductance was higher for a species in the wetter type. These results suggest that although a floodplain moisture gradient exists, it alone does not limit the distribution of floodplain plant communities in the North Fork.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wetlands","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Wetland Scientists","publisherLocation":"McClean, VA","doi":"10.1007/BF03160785","usgsCitation":"Lee, L., Hinckley, T., and Scott, M.L., 1985, Plant water status relationships among major floodplain sites of the Flathead River, Montana: Wetlands, v. 5, no. 1, p. 15-34, https://doi.org/10.1007/BF03160785.","productDescription":"20 p.","startPage":"15","endPage":"34","numberOfPages":"20","costCenters":[],"links":[{"id":292441,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292440,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF03160785"}],"country":"United States","state":"Montana","otherGeospatial":"Flathead River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.309882,48.057693 ], [ -114.309882,48.393746 ], [ -114.083081,48.393746 ], [ -114.083081,48.057693 ], [ -114.309882,48.057693 ] ] ] } } ] }","volume":"5","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25feae4b0333418718941","contributors":{"authors":[{"text":"Lee, L.C.","contributorId":7194,"corporation":false,"usgs":true,"family":"Lee","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":498621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hinckley, T.M.","contributorId":37656,"corporation":false,"usgs":true,"family":"Hinckley","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":498622,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scott, M. L.","contributorId":75090,"corporation":false,"usgs":true,"family":"Scott","given":"M.","middleInitial":"L.","affiliations":[],"preferred":false,"id":498623,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70120888,"text":"70120888 - 1985 - Interspecific relationships between American coots and waterfowl during fall migration","interactions":[],"lastModifiedDate":"2014-08-18T11:46:03","indexId":"70120888","displayToPublicDate":"1985-12-01T11:31:03","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"Interspecific relationships between American coots and waterfowl during fall migration","docAbstract":"<p>Interactions between American Coots (<i>Fulica americana</i>) and water-fowl during the breeding season are well-documented (Ryder 1959, Nudds 1981).  Ducks and coots use similar nesting, feeding, brooding, and loafing sites during the breeding season (Munro 1939, Sooter 1945, Ryder 1959).  Coots create potential nest sites, repulse predators, provide predation buffers for ducks (Sooter 1945; Ryder 1958, 1959), and may also destroy eggs and young of other marsh-nesting birds (Munro 1937, Burger 1973, McNicholl 1975).  Coots, ducks, and swans often feed cooperatively (Ryder 1959, Anderson 1974, Ryan 1981); and American Wigeon (<i>Anas americana</i>) and Gadwell (<A. strepera</i>) may rob feeding coots (Knapton and Knudsen 1978, Ryan 1981).  Interspecies aggression between coots and waterfowl usually occurs when ducks approach coot nests or broods (Ryan and Dinsmore 1979).  Despite these interactions, the numbers of duck broods produced in areas in Utah with nesting coots and in areas where coots have been removed were similar (Ryder 1958, 1961).  Densities of coots and ducks, and brood counts of coots and ducks for a 26-year period in Saskatchewan also indicated no significant relationship between numbers of coots and waterfowl (Nudds 1981).</p>\n<br/>\n<p>Coots and waterfowl from large areas of breeding habitat concentrate on smaller areas during the nonbreeding season (Weller 1975:102).  These species may also change diets and habitats during migration and while wintering (Weller 1975).  This study documents associations between waterfowl and coots during fall migration and examines feeding and behavioral interactions between coots and waterfowl in mixed flocks.  Specifically, we (1) describe temporal and spatial overlap among migrations of coots and waterfowl, (2) present behavioral interactions among species, and (3) document food habits of birds feeding sympatrically during fall migration in Oklahoma.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wilson Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wilson Ornithological Society","publisherLocation":"Lawrence, KS","usgsCitation":"Eddleman, W.R., Patterson, C.T., and Knopf, F., 1985, Interspecific relationships between American coots and waterfowl during fall migration: The Wilson Bulletin, v. 97, no. 4, p. 463-472.","productDescription":"10 p.","startPage":"463","endPage":"472","numberOfPages":"10","costCenters":[],"links":[{"id":292417,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"97","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25fe6e4b0333418718926","contributors":{"authors":[{"text":"Eddleman, William R.","contributorId":40685,"corporation":false,"usgs":true,"family":"Eddleman","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":498551,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patterson, Craig T.","contributorId":15940,"corporation":false,"usgs":true,"family":"Patterson","given":"Craig","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":498549,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knopf, Fritz L.","contributorId":30549,"corporation":false,"usgs":true,"family":"Knopf","given":"Fritz L.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":498550,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70121039,"text":"70121039 - 1985 - Disturbance in a cypress-tupelo wetland: an interaction between thermal loading and hydrology","interactions":[],"lastModifiedDate":"2014-08-19T11:02:41","indexId":"70121039","displayToPublicDate":"1985-12-01T11:00:31","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Disturbance in a cypress-tupelo wetland: an interaction between thermal loading and hydrology","docAbstract":"The interaction between thermal loading and hydrology was examined in a forested wetland. As a result of flooding, portions of the wetland are periodically exposed to elevated water temperatures, resulting in progressive deterioration of the canopy. We chose three study sites along a gradient of canopy disturbance: most disturbed, intermediate disturbance and a least disturbed site. The timing of flooding has important effects on this wetland: floods which occur late in the growing season have greater impact on the timing of litterfall and the extent of tree mortality. Following a flood in May, there was no observed increase in litterfall, and woody detrital production (tree mortality) eliminated only o.4% and 1.1% of the aboveground woody biomass at the intermediate and least disturbed sites, respectively. In contrast. premature leaf senescence and literfall were observed at the intermediate site following an August flood, and tree mortality at the intermediate and least disturbed sites eliminated 10% and 8%, respectively, of the aboveground woody biomass. At the most disturbed site, where the majority of trees were already dead, no additional mortality was recorded during the study. Long-term effects of this disturbance regime are the loss of small stems and increased stem production of trees which remain. While stem production at the intermediate site (413 g.m<sup>−2</sup>.yr<sup>−1</sup>) exceeded that at the least disturbed site (373 g.m<sup>−2</sup>.y<sup>−1</sup>), total aboveground net primary production was highest at the least disturbed site (788 g·m<sup>−2</sup>· yr<sup>−1</sup>), primarily because of the greater stem density. Portions of this wetland continue to deteriorate after more than 30 years of thermal loading.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wetlands","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Wetland Scientists","publisherLocation":"McClean, VA","doi":"10.1007/BF03160787","usgsCitation":"Scott, M.L., Sharitz, R.R., and Lee, L.C., 1985, Disturbance in a cypress-tupelo wetland: an interaction between thermal loading and hydrology: Wetlands, v. 5, no. 1, p. 53-68, https://doi.org/10.1007/BF03160787.","productDescription":"16 p.","startPage":"53","endPage":"68","numberOfPages":"16","costCenters":[],"links":[{"id":292532,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292531,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF03160787"}],"volume":"5","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f464c9e4b073ff773a7cf5","contributors":{"authors":[{"text":"Scott, Michael L. scottm@usgs.gov","contributorId":1169,"corporation":false,"usgs":true,"family":"Scott","given":"Michael","email":"scottm@usgs.gov","middleInitial":"L.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":498714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sharitz, Rebecca R.","contributorId":44598,"corporation":false,"usgs":true,"family":"Sharitz","given":"Rebecca","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":498716,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, Lyndon C.","contributorId":36064,"corporation":false,"usgs":true,"family":"Lee","given":"Lyndon","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":498715,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185596,"text":"70185596 - 1985 - Concentration of trace elements in water samples by reductive precipitation","interactions":[],"lastModifiedDate":"2020-01-19T11:17:26","indexId":"70185596","displayToPublicDate":"1985-12-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Concentration of trace elements in water samples by reductive precipitation","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/ac00291a016","usgsCitation":"Skogerboe, R.K., Hanagan, W., and Taylor, H.E., 1985, Concentration of trace elements in water samples by reductive precipitation: Analytical Chemistry, v. 57, no. 14, p. 2815-2818, https://doi.org/10.1021/ac00291a016.","productDescription":"4 p. ","startPage":"2815","endPage":"2818","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338282,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"14","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"58d6303ae4b05ec7991310fd","contributors":{"authors":[{"text":"Skogerboe, R. K","contributorId":189803,"corporation":false,"usgs":false,"family":"Skogerboe","given":"R.","email":"","middleInitial":"K","affiliations":[],"preferred":false,"id":686068,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanagan, W.A.","contributorId":189804,"corporation":false,"usgs":false,"family":"Hanagan","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":686069,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":686070,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012937,"text":"70012937 - 1985 - Water resources activities of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2026-04-22T16:43:40.62591","indexId":"70012937","displayToPublicDate":"1985-12-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Water resources activities of the U.S. Geological Survey","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.1985.tb00185.x","issn":"00431370","usgsCitation":"Peck, D.L., 1985, Water resources activities of the U.S. Geological Survey: Journal of the American Water Resources Association, v. 21, no. 6, p. 901-907, https://doi.org/10.1111/j.1752-1688.1985.tb00185.x.","productDescription":"7 p.","startPage":"901","endPage":"907","costCenters":[],"links":[{"id":222626,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"6","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"505bc38fe4b08c986b32b24c","contributors":{"authors":[{"text":"Peck, Dallas L.","contributorId":60187,"corporation":false,"usgs":true,"family":"Peck","given":"Dallas","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":364883,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175830,"text":"70175830 - 1985 - Simulation of ground-water flow in the Prairie du Chien-Jordan aquifer and relation to ground-water contamination by coal-tar derivatives, St. Louis Park, Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T11:21:29","indexId":"70175830","displayToPublicDate":"1985-11-27T12:15:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Simulation of ground-water flow in the Prairie du Chien-Jordan aquifer and relation to ground-water contamination by coal-tar derivatives, St. Louis Park, Minnesota","docAbstract":"<p>No abstract available.</p>","conferenceTitle":"National Water Well Association Conference Exposition","conferenceDate":"August 19-20, 1985","conferenceLocation":"Worthington, Ohio","language":"English","publisher":"National Water Well Association","publisherLocation":"Worthington, Ohio","usgsCitation":"Stark, J., and Hult, M.F., 1985, Simulation of ground-water flow in the Prairie du Chien-Jordan aquifer and relation to ground-water contamination by coal-tar derivatives, St. Louis Park, Minnesota, National Water Well Association Conference Exposition, Worthington, Ohio, August 19-20, 1985, p. 290-310.","productDescription":"21 p.","startPage":"290","endPage":"310","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":326990,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82de6e4b03fd6b7da39b7","contributors":{"authors":[{"text":"Stark, J. R.","contributorId":100406,"corporation":false,"usgs":true,"family":"Stark","given":"J. R.","affiliations":[],"preferred":false,"id":646414,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hult, M. F.","contributorId":29817,"corporation":false,"usgs":true,"family":"Hult","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":646415,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70170777,"text":"70170777 - 1985 - Tsunamis – Scourge of the Pacific","interactions":[],"lastModifiedDate":"2016-05-02T14:43:00","indexId":"70170777","displayToPublicDate":"1985-11-13T10:15:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Tsunamis – Scourge of the Pacific","docAbstract":"<p>Although tsunamis occur most often in the Pacific Ocean, they can be generated by major earthquakes in other areas.&nbsp; The most frequent cause of tsunamis&hellip;is crustal movement along a fault: a large mass of rock drops or rises and displaces the column of water above it.&nbsp; This column of water &ndash; a tsunami &ndash; travels outward from the source at the fantastic speed of 500 mph or more.&nbsp; When an earthquake occurs in the Pacific Ocean Basin, authorities must quickly decide on a course of action.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","usgsCitation":"Lockridge, P., 1985, Tsunamis – Scourge of the Pacific: Earthquake Information Bulletin (USGS), v. 17, no. 6, p. 211-217.","productDescription":"7 p.","startPage":"211","endPage":"217","numberOfPages":"7","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320834,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57287a33e4b0b13d391865e9","contributors":{"authors":[{"text":"Lockridge, Patricia","contributorId":169082,"corporation":false,"usgs":false,"family":"Lockridge","given":"Patricia","email":"","affiliations":[],"preferred":false,"id":628364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185588,"text":"70185588 - 1985 - Field determination of the three-dimensional hydraulic conductivity tensor of anisotropic media: 1. Theory","interactions":[],"lastModifiedDate":"2020-01-19T11:11:34","indexId":"70185588","displayToPublicDate":"1985-11-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Field determination of the three-dimensional hydraulic conductivity tensor of anisotropic media: 1. Theory","docAbstract":"<p><span>A field method is proposed for determining the three-dimensional hydraulic conductivity tensor and specific storage of an anisotropic porous or fractured medium. The method, known as cross-hole testing (to distinguish it from conventional single-hole packer tests), consists of injecting fluid into (or withdrawing fluid from) packed-off intervals in a number of boreholes and monitoring the transient head response in similar intervals in neighboring boreholes. The directions of the principal hydraulic conductivities need not be known prior to the test, and the boreholes may have arbitrary orientations (e.g., they can all be vertical). An important aspect of the proposed method is that it provides direct field information on whether it is proper to regard the medium as being uniform and anisotropic on the scale of the test. The first paper presents theoretical expressions describing transient and steady state head response in monitoring intervals of arbitrary lengths and orientations, to constant-rate injection into (or withdrawal from) intervals having similar or different lengths and orientations. The conditions under which these intervals can be treated mathematically as points are investigated by an asymptotic analysis. The effect of planar no-flow and constant-head boundaries on the response is analyzed by the theory of images. The second paper describes the field methodology and shows how the proposed approach works in the case of fractured granitic rocks.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i011p01655","usgsCitation":"Hsieh, P.A., and Neuman, S.P., 1985, Field determination of the three-dimensional hydraulic conductivity tensor of anisotropic media: 1. Theory: Water Resources Research, v. 21, no. 1, p. 1655-1665, https://doi.org/10.1029/WR021i011p01655.","productDescription":"11 p. ","startPage":"1655","endPage":"1665","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338261,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"1","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"58d6303be4b05ec799131101","contributors":{"authors":[{"text":"Hsieh, Paul A. 0000-0003-4873-4874 pahsieh@usgs.gov","orcid":"https://orcid.org/0000-0003-4873-4874","contributorId":1634,"corporation":false,"usgs":true,"family":"Hsieh","given":"Paul","email":"pahsieh@usgs.gov","middleInitial":"A.","affiliations":[{"id":39113,"text":"WMA - Office of Quality Assurance","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":686040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neuman, Shlomo P.","contributorId":189795,"corporation":false,"usgs":false,"family":"Neuman","given":"Shlomo","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":686041,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185590,"text":"70185590 - 1985 - Assessment of the instantaneous unit hydrograph derived from the theory of topologically random networks","interactions":[],"lastModifiedDate":"2020-01-19T11:09:50","indexId":"70185590","displayToPublicDate":"1985-11-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Assessment of the instantaneous unit hydrograph derived from the theory of topologically random networks","docAbstract":"<p><span>An instantaneous unit hydrograph (iuh) based on the theory of topologically random networks (topological iuh) is evaluated in terms of sets of basin characteristics and hydraulic parameters. Hydrographs were computed using two linear routing methods for each of two drainage basins in the southeastern United States and are the basis of comparison for the topological iuh's. Elements in the sets of basin characteristics for the topological iuh's are the number of first-order streams only, (</span><i>N</i><span>), or the nuber of sources together with the number of channel links in the topological diameter (</span><i>N, D</i><span>); the hydraulic parameters are values of the celerity and diffusivity constant. Sensitivity analyses indicate that the mean celerity of the internal links in the network is the critical hydraulic parameter for determining the shape of the topological iuh, while the diffusivity constant has minimal effect on the topological iuh. Asymptotic results (source-only) indicate the number of sources need not be large to approximate the topological iuh with the Weibull probability density function.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i011p01693","usgsCitation":"Karlinger, M., and Troutman, B., 1985, Assessment of the instantaneous unit hydrograph derived from the theory of topologically random networks: Water Resources Research, v. 21, no. 11, p. 1693-1702, https://doi.org/10.1029/WR021i011p01693.","productDescription":"10 p. ","startPage":"1693","endPage":"1702","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338263,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"11","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"58d6303be4b05ec7991310ff","contributors":{"authors":[{"text":"Karlinger, M.R.","contributorId":95039,"corporation":false,"usgs":true,"family":"Karlinger","given":"M.R.","affiliations":[],"preferred":false,"id":686050,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Troutman, B.M.","contributorId":73638,"corporation":false,"usgs":true,"family":"Troutman","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":686051,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012768,"text":"70012768 - 1985 - Detectability of step trends in the rate of atmospheric deposition of sulfate","interactions":[],"lastModifiedDate":"2026-04-22T16:54:08.09578","indexId":"70012768","displayToPublicDate":"1985-10-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Detectability of step trends in the rate of atmospheric deposition of sulfate","docAbstract":"<p><span>A method is presented to assist policy makers in determining the combination of number of sampling stations and number of years of sampling necessary to state with a given probability that a step reduction in atmospheric deposition rates of a given magnitude has occurred at a pre-specified time. This pre-specified time would typically be the time at which a sulfate emission control program took effect, and the given magnitude of reduction is some percentage change in deposition rate one might expect to occur as a result of the emission control. In order to determine this probability of detection, a stochastic model of sulfate deposition rates is developed, based on New York State bulk collection network data. The model considers the effect of variation in precipitation, seasonal variations, serial correlation, and site-to-site (cross) correlation. A nonparametric statistical test which is well suited to detection of step changes in such multi-site data sets is developed. It is related to the Mann-Whitney Rank-Sum test. The test is used in Monte Carlo simulations along with the stochastic model to derive statistical power functions. These power functions describe the probability of detecting (α=0.05) a step trend in deposition rate as a function of the size of the step-trend, record length before and after the step-trend, and the number of stations sampled. The results show that, for an area the size of New York State, very little power is gained by increasing the number of stations beyond about eight. The results allow policy makers to determine the tradeoff between the cost of monitoring and time required to detect a step-trend of a given magnitude with a given probability.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.1985.tb00171.x","issn":"00431370","usgsCitation":"Hirsch, R., and Gilroy, E., 1985, Detectability of step trends in the rate of atmospheric deposition of sulfate: Journal of the American Water Resources Association, v. 21, no. 5, p. 773-784, https://doi.org/10.1111/j.1752-1688.1985.tb00171.x.","productDescription":"12 p.","startPage":"773","endPage":"784","costCenters":[],"links":[{"id":221848,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New 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York\",\"nation\":\"USA  \"}}]}","volume":"21","issue":"5","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"5059ff5ce4b0c8380cd4f144","contributors":{"authors":[{"text":"Hirsch, R.M.","contributorId":58639,"corporation":false,"usgs":true,"family":"Hirsch","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":364473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilroy, E.J.","contributorId":20306,"corporation":false,"usgs":true,"family":"Gilroy","given":"E.J.","affiliations":[],"preferred":false,"id":364472,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012925,"text":"70012925 - 1985 - Periodic autoregressive-moving average (PARMA) modeling with applications to water resources","interactions":[],"lastModifiedDate":"2026-04-23T15:53:37.465442","indexId":"70012925","displayToPublicDate":"1985-10-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Periodic autoregressive-moving average (PARMA) modeling with applications to water resources","docAbstract":"<p><span>Results involving correlation properties and parameter estimation for autoregressive-moving average models with periodic parameters are presented. A multivariate representation of the PARMA model is used to derive parameter space restrictions and difference equations for the periodic autocorrelations. Close approximation to the likelihood function for Gaussian PARMA processes results in efficient maximum-likelihood estimation procedures. Terms in the Fourier expansion of the parameters are sequentially included, and a selection criterion is given for determining the optimal number of harmonics to be included. Application of the techniques is demonstrated through analysis of a monthly streamflow time series.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.1985.tb00167.x","issn":"00431370","usgsCitation":"Vecchia, A.V., 1985, Periodic autoregressive-moving average (PARMA) modeling with applications to water resources: Journal of the American Water Resources Association, v. 21, no. 5, p. 721-730, https://doi.org/10.1111/j.1752-1688.1985.tb00167.x.","productDescription":"10 p.","startPage":"721","endPage":"730","costCenters":[],"links":[{"id":222450,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"5","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"505a7348e4b0c8380cd76f4d","contributors":{"authors":[{"text":"Vecchia, A. V.","contributorId":23533,"corporation":false,"usgs":true,"family":"Vecchia","given":"A.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":364852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70205228,"text":"70205228 - 1985 - Tracer test for evaluating nonpumping intraborehole flow in fractured media","interactions":[],"lastModifiedDate":"2019-09-08T03:49:22","indexId":"70205228","displayToPublicDate":"1985-09-08T03:45:44","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5139,"text":"Transactions of the American Nuclear Society","active":true,"publicationSubtype":{"id":10}},"title":"Tracer test for evaluating nonpumping intraborehole flow in fractured media","language":"English","publisher":"American Nuclear Society","usgsCitation":"Galloway, D.L., and Erickson, J., 1985, Tracer test for evaluating nonpumping intraborehole flow in fractured media: Transactions of the American Nuclear Society, v. 50, p. 192-193.","productDescription":"2 p.","startPage":"192","endPage":"193","numberOfPages":"2","costCenters":[{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":367277,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Galloway, Devin L. 0000-0003-0904-5355 dlgallow@usgs.gov","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":679,"corporation":false,"usgs":true,"family":"Galloway","given":"Devin","email":"dlgallow@usgs.gov","middleInitial":"L.","affiliations":[{"id":5078,"text":"Southwest Regional Director's Office","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true}],"preferred":true,"id":770457,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, J.R.","contributorId":66689,"corporation":false,"usgs":true,"family":"Erickson","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":770458,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5223357,"text":"5223357 - 1985 - Contaminant residues in fish and sediments from lakes in the Atchafalaya River Basin (Louisiana)","interactions":[],"lastModifiedDate":"2023-12-12T16:12:05.521341","indexId":"5223357","displayToPublicDate":"1985-09-01T12:18:59","publicationYear":"1985","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":"Contaminant residues in fish and sediments from lakes in the Atchafalaya River Basin (Louisiana)","docAbstract":"<p><span>Conversion of bottomland hardwood forests ℴ agricultural land has reduced habitat and water quality in many lakes in the floodplain of the lower Mississippi River. The objectives of this study were to ascertain current contaminant residue concentrations in fish and sediment from lakes in the Atchafalaya River Basin and to determine the influence of overflow and agricultural land use on contaminant levels. Fish and sediment samples were collected from eight lakes that differed in overflow (no overflow, headwater overflow, backwater overflow) and land-use characteristics (presence or absence of agricultural land). Residue analysis of 24 sediment and 82 fish samples collected from the study lakes showed that contaminant residues were uniformly low. Total DDT concentrations, consisting mainly of DDE, were found in 98% of the fish samples and generally were the highest residues though they rarely exceeded 0.50 μg/g. Dieldrin, α-BHC and γ-BHC, in concentrations rarely exceeding 0.05 μg/g, were detected in about 50% of the fish samples. Total organochlorine pesticide and PCB residues were less than 2.00 μg/g in all fish from all lakes, except for a 3.46 μg/g total in spotted gar (</span><i>Lepisosteus oculatus</i><span>) from one lake. Sediments were free from pesticide residues except for occasional traces (0.01 μg/g) of α-BHC. Metal residue concentrations in fish and sediment samples were typical of uncontaminated areas. Lake systems in the Atchafalaya River Basin appeared to be relatively uncontaminated by agricultural pesticides, but metal and organic residues in fish were similar from lakes with the same land-use and overflow characteristics.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF01055388","usgsCitation":"Winger, P.V., and Andreasen, J.K., 1985, Contaminant residues in fish and sediments from lakes in the Atchafalaya River Basin (Louisiana): Archives of Environmental Contamination and Toxicology, v. 14, no. 5, p. 579-586, https://doi.org/10.1007/BF01055388.","productDescription":"8 p.","startPage":"579","endPage":"586","numberOfPages":"8","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199348,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Louisiana","otherGeospatial":"Atchafalaya River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.35068322053141,\n              29.278637011487447\n            ],\n            [\n              -89.98641481029229,\n              29.706700645240673\n            ],\n            [\n              -90.07037935988335,\n              29.977215216142227\n            ],\n            [\n              -90.71810588529938,\n              30.029153141543134\n            ],\n            [\n              -91.197903311534,\n              30.309147206940025\n            ],\n            [\n              -91.63571846297276,\n              30.918204495029755\n            ],\n            [\n              -91.05396408366363,\n              32.17549525199841\n            ],\n            [\n              -91.20989810279053,\n              32.94885275839151\n            ],\n            [\n              -92.82321694850341,\n              32.94885275839151\n            ],\n            [\n              -92.52934102493508,\n              31.41086526110982\n            ],\n            [\n              -92.60730810669784,\n              30.85129000681927\n            ],\n            [\n              -92.57732076755853,\n              30.101817488823315\n            ],\n            [\n              -92.09152171464704,\n              29.550300375725115\n            ],\n            [\n              -91.0239724412757,\n              29.200135832922854\n            ],\n            [\n              -89.35068322053141,\n              29.278637011487447\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"14","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af6e4b07f02db6929bb","contributors":{"authors":[{"text":"Winger, Parley V.","contributorId":27983,"corporation":false,"usgs":true,"family":"Winger","given":"Parley","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":338522,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, J. K.","contributorId":38513,"corporation":false,"usgs":true,"family":"Andreasen","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":338521,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185594,"text":"70185594 - 1985 - Comment on “Evaluation of slug tests in wells containing a finite-thickness skin” by C. R. Faust and J. W. Mercer","interactions":[],"lastModifiedDate":"2020-01-19T10:36:06","indexId":"70185594","displayToPublicDate":"1985-09-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Comment on “Evaluation of slug tests in wells containing a finite-thickness skin” by C. R. Faust and J. W. Mercer","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i009p01459","usgsCitation":"Moench, A.F., and Hsieh, P.A., 1985, Comment on “Evaluation of slug tests in wells containing a finite-thickness skin” by C. R. Faust and J. W. Mercer: Water Resources Research, v. 21, no. 9, p. 1459-1461, https://doi.org/10.1029/WR021i009p01459.","productDescription":"3 p. ","startPage":"1459","endPage":"1461","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":480160,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/wr021i009p01459","text":"Publisher Index Page"},{"id":338276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"9","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"58d6303be4b05ec799131103","contributors":{"authors":[{"text":"Moench, Allen F. afmoench@usgs.gov","contributorId":3903,"corporation":false,"usgs":true,"family":"Moench","given":"Allen","email":"afmoench@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":686063,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hsieh, Paul A. 0000-0003-4873-4874 pahsieh@usgs.gov","orcid":"https://orcid.org/0000-0003-4873-4874","contributorId":1634,"corporation":false,"usgs":true,"family":"Hsieh","given":"Paul","email":"pahsieh@usgs.gov","middleInitial":"A.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":39113,"text":"WMA - Office of Quality Assurance","active":true,"usgs":true}],"preferred":true,"id":686064,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70113398,"text":"70113398 - 1985 - Landsat-faciliated vegetation classification of the Kenai National Wildlife Refuge and adjacent areas, Alaska","interactions":[],"lastModifiedDate":"2022-04-18T15:13:27.734632","indexId":"70113398","displayToPublicDate":"1985-08-20T15:30:04","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Landsat-faciliated vegetation classification of the Kenai National Wildlife Refuge and adjacent areas, Alaska","docAbstract":"<p>A Landsat-based vegetation map was prepared for Kenai National Wildlife Refuge and adjacent lands, 2 million and 2.5 million acres respectively.  The refuge lies within the middle boreal sub zone of south central Alaska.  Seven major classes and sixteen subclasses were recognized: forest (closed needleleaf, needleleaf woodland, mixed); deciduous scrub (lowland and montane, subalpine); dwarf scrub (dwarf shrub tundra, lichen tundra, dwarf shrub and lichen tundra, dwarf shrub peatland, string bog/wetlands); herbaceous (graminoid meadows and marshes); scarcely vegetated areas ; water (clear, moderately turbid, highly turbid); and glaciers.</p>\n<br/>\n<p>The methodology employed a cluster-block technique.  Sample areas were described based on a combination of helicopter-ground survey, aerial photo interpretation, and digital Landsat data.  Major steps in the Landsat analysis involved: preprocessing (geometric connection), spectral class labeling of sample areas, derivation of statistical parameters for spectral classes, preliminary classification of the entree study area using a maximum-likelihood algorithm, and final classification through ancillary information such as digital elevation data.</p>\n<br/>\n<p>The vegetation map (scale 1:250,000) was a pioneering effort since there were no intermediate-sclae maps of the area.  Representative of distinctive regional patterns, the map was suitable for use in comprehensive conservation planning and wildlife management.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Pecora 10 Symposium","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","publisherLocation":"Falls Church, VA","usgsCitation":"Talbot, S., Shasby, M., and Bailey, T., 1985, Landsat-faciliated vegetation classification of the Kenai National Wildlife Refuge and adjacent areas, Alaska, <i>in</i> Pecora 10 Symposium, p. 333-345.","productDescription":"13 p.","startPage":"333","endPage":"345","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288937,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Kenai National Wildlife Refuge","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -151.335508,60.516137 ], [ -151.335508,60.603701 ], [ -151.072172,60.603701 ], [ -151.072172,60.516137 ], [ -151.335508,60.516137 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7759e4b0abf75cf2c10b","contributors":{"authors":[{"text":"Talbot, Stephen S.","contributorId":73266,"corporation":false,"usgs":true,"family":"Talbot","given":"Stephen S.","affiliations":[],"preferred":false,"id":495088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shasby, M.B.","contributorId":68367,"corporation":false,"usgs":true,"family":"Shasby","given":"M.B.","affiliations":[],"preferred":false,"id":495089,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bailey, T.N.","contributorId":99896,"corporation":false,"usgs":true,"family":"Bailey","given":"T.N.","email":"","affiliations":[],"preferred":false,"id":495090,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70113321,"text":"70113321 - 1985 - New horizons in remote sensing for forest and range resource management","interactions":[],"lastModifiedDate":"2022-04-18T14:52:10.416845","indexId":"70113321","displayToPublicDate":"1985-08-20T13:20:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"New horizons in remote sensing for forest and range resource management","docAbstract":"<p>Forest and range resource scientists were among the first to recognize the potential of aircraft and satellite remote sensing for management of timber, forage, water, and wildlife resource.  Today, data from a variety of sensor systems are being put to practical use for inventorying, monitoring, and assessing forest and range resources.  In the future, improved sensor systems providing new kinds of data will be available.  Likewise, new types of data handling and processing systems can be anticipated.</p>\n<br/>\n<p>Among the new or anticipated aircraft and satellite systems and/or data are National High-Altitude Photograph II, U. S. Geological Survey-acquired Side-Looking Airborne  Radar, the Landsat thematic mapper, the National Oceanic Resolution Radiometer, the French Systeme Probatoire d'Observation de la Terre (SPOT) satellite, the European Space Agency Earth Resources Satellite, the National Aeronautics and Space Administration Large Format Camera and Shuttle Imaging Radar (SIR-A, -B, and -C), and a variety of other systems in existence or planned by the Soviets, Japanese, Canadians, Chinese, Brazilians, Indonesians, and other.</p>\n<br/>\n<p>Application examples are presented that illustrate uses of 1-kilometer-resolution AVHRR data, 80-meter Landsat multispectral scanner data, 30-meter Landsat thematic mapper data, and 10-meter SPOT-simulator data.  These examples address fire fuel monitoring, land cover mapping, rangeland assessment, and soils landscape mapping.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Pecora 10 Symposium","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","publisherLocation":"Falls Church, VA","usgsCitation":"Lauer, D.T., 1985, New horizons in remote sensing for forest and range resource management, <i>in</i> Pecora 10 Symposium, p. 30-41.","productDescription":"12 p.","startPage":"30","endPage":"41","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288929,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7784e4b0abf75cf2c16b","contributors":{"authors":[{"text":"Lauer, D. T.","contributorId":47907,"corporation":false,"usgs":true,"family":"Lauer","given":"D.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":495060,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14248,"text":"ofr84819 - 1985 - Ground-water data for the alluvial, buried channel, Basel Pleistocene and Dakota aquifer in west-central Iowa","interactions":[],"lastModifiedDate":"2023-08-24T20:10:09.628205","indexId":"ofr84819","displayToPublicDate":"1985-08-01T00:00:00","publicationYear":"1985","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":"84-819","title":"Ground-water data for the alluvial, buried channel, Basel Pleistocene and Dakota aquifer in west-central Iowa","docAbstract":"<p>The purpose of this investigation was to determine the availability, quantity and quality of groundwater from three principal aquifers in West-Central Iowa, the alluvial, buried channel, Basal Pleistocene and the Dakota aquifers. Specific objectives were to: (1) determine the location, extent and the nature of these aquifers; (2) evaluate the occurrence and movement of groundwater, including the sources of recharge and discharge; (3) estimate the quantities of water stored in the aquifers; (4) estimate the potential yields of wells tapping the aquifers; (5) estimate the water use; and (6) describe the chemical quality of the groundwater. This report is the compilation of the data collected during the investigation and has the purpose of providing a reference for an interpretive report describing groundwater resources and a bedrock topography map of the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84819","collaboration":"Prepared in cooperation with the Iowa Geological Survey","usgsCitation":"Hunt, P.K., and Runkle, D.L., 1985, Ground-water data for the alluvial, buried channel, Basel Pleistocene and Dakota aquifer in west-central Iowa: U.S. Geological Survey Open-File Report 84-819, iv, 168 p.  **PUBLICATION PAGES ARE IN INCORRECT ORDER**, https://doi.org/10.3133/ofr84819.","productDescription":"iv, 168 p.  **PUBLICATION PAGES ARE IN INCORRECT ORDER**","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":144681,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0819/report-thumb.jpg"},{"id":42934,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0819/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Iowa","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96.5,41.5 ], [ -96.5,42.5 ], [ -94,42.5 ], [ -94,41.5 ], [ -96.5,41.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d63d","contributors":{"authors":[{"text":"Hunt, Pamela K. B.","contributorId":89142,"corporation":false,"usgs":true,"family":"Hunt","given":"Pamela","email":"","middleInitial":"K. B.","affiliations":[],"preferred":false,"id":169149,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Runkle, Donna L. dlrunkle@usgs.gov","contributorId":2556,"corporation":false,"usgs":true,"family":"Runkle","given":"Donna","email":"dlrunkle@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":169148,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70171486,"text":"70171486 - 1985 - Application of a ground-water flow digital model in evaluating alternate dewatering systems in the Río Grande de Arecibo alluvial valley, Puerto Rico","interactions":[],"lastModifiedDate":"2016-06-01T14:34:13","indexId":"70171486","displayToPublicDate":"1985-07-17T10:45:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Application of a ground-water flow digital model in evaluating alternate dewatering systems in the Río Grande de Arecibo alluvial valley, Puerto Rico","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"American Water Resources Association, Technical Publication Series TPS-85-1","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Tropical Hydrology and Second Caribbean Islands Water-Resources Congress","conferenceDate":"May 5-8, 1985","conferenceLocation":"San Juan, Puerto Rico","language":"English","publisher":"American Geosciences Institute","issn":"0731-9789","usgsCitation":"Quinones-Aponte, V., and Heriberto Torres-Sierra, 1985, Application of a ground-water flow digital model in evaluating alternate dewatering systems in the Río Grande de Arecibo alluvial valley, Puerto Rico, <i>in</i> American Water Resources Association, Technical Publication Series TPS-85-1, San Juan, Puerto Rico, May 5-8, 1985, p. 129-134.","productDescription":"6 p.","startPage":"129","endPage":"134","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"links":[{"id":322030,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57500732e4b0ee97d51bb3ae","contributors":{"authors":[{"text":"Quinones-Aponte, Vicente","contributorId":48552,"corporation":false,"usgs":true,"family":"Quinones-Aponte","given":"Vicente","email":"","affiliations":[],"preferred":false,"id":631282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heriberto Torres-Sierra","contributorId":141082,"corporation":false,"usgs":false,"family":"Heriberto Torres-Sierra","affiliations":[{"id":12608,"text":"USGS, retired","active":true,"usgs":false}],"preferred":false,"id":631283,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211187,"text":"70211187 - 1985 - Rate and depth of pedogenic-carbonate accumulation in soils: Formation and testing of a compartment model.","interactions":[],"lastModifiedDate":"2020-07-16T18:10:30.180814","indexId":"70211187","displayToPublicDate":"1985-07-16T12:24:38","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1727,"text":"GSA Special Papers","active":true,"publicationSubtype":{"id":10}},"title":"Rate and depth of pedogenic-carbonate accumulation in soils: Formation and testing of a compartment model.","docAbstract":"<p>The rate and depth of pedogenic carbonate accumulation in soils formed in Quaternary alluvium may be viewed as a theoretical problem that involves the mutual interaction of several independent and dependent soil-forming variables. We propose a model for carbonate accumulation in which the soil column is defined by a vertical sequence of 1-cm<sup>2</sup>-area compartments, each with a specified texture, bulk density, water-holding content, lithologic and mineralogic composition, soil-air pCO<sub>2</sub>, ionic strength, and temperature. On the basis of these data, rates of carbonate solubility and dissolution within a given compartment are determined. In arkosic to lithic arkosic sandy parent materials, high carbonate solubility (0.137 to 0.212 mg/ml) and the large reactive surface area of eolian calcareous dust result in rapid carbonate dissolution (0.79 to 9.92 × 10<sup>−10</sup><span>&nbsp;</span>g/cm<sup>2</sup>/sec) that promotes rapid translocation of carbonate by infiltrating water. We derive a group of equations and use them to calculate net carbonate depletion or accumulation in a soil compartment over an interval of time as a function of the independent variables temperature and precipitation. These two variables largely determine or strongly influence soil-water balance, the external carbonate influx rate, and carbonate solubility.</p><p>The carbonate distribution that our model predicts closely resembles the observed carbonate distribution in soils associated with Holocene deposits forming in arid, hyperthermic to xeric, thermic moisture-temperature regimes in southern California. This modeling indicates that with a mean carbonate influx rate of 1 × 10<sup>−4</sup><span>&nbsp;</span>g/cm<sup>2</sup>/yr and in a semiarid, thermic climate, the maximum depression of the top of the Cca horizon is attained within only a few thousand years. In contrast, given the same influx rate, our model predicts that a noncalcareous B horizon cannot form in an arid, hyperthermic climate, a conclusion supported by field and laboratory studies of calcic soils in this climate.</p><p>The influence of glacial-to-interglacial climatic changes on carbonate accumulation can be modeled by calculating latest Pleistocene soil-water balance with the aid of published estimates of full-glacial temperature and precipitation. On the basis of these modeling results, we propose that either of two types of glacial-to-interglacial climatic changes may account for the strongly bimodal, apparently polygenetic carbonate distribution that is observed in late Pleistocene soils of the eastern Mojave Desert of southern California. Such results of compartment-strategy modeling are encouraging and indicate the great potential of combined theoretical and empirical methods for considering pedological problems of interest to Quaternary geologists.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/SPE203-p23","usgsCitation":"McFadden, L.D., and Tinsley, J., 1985, Rate and depth of pedogenic-carbonate accumulation in soils: Formation and testing of a compartment model.: GSA Special Papers, v. 203, p. 23-41, https://doi.org/10.1130/SPE203-p23.","productDescription":"19 p.","startPage":"23","endPage":"41","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":376441,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"203","noUsgsAuthors":false,"publicationDate":"1985-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"McFadden, Leslie D.","contributorId":139971,"corporation":false,"usgs":false,"family":"McFadden","given":"Leslie","email":"","middleInitial":"D.","affiliations":[{"id":13339,"text":"University of New Mexico, Albuquerque","active":true,"usgs":false}],"preferred":false,"id":793031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tinsley, John jtinsley@usgs.gov","contributorId":140545,"corporation":false,"usgs":true,"family":"Tinsley","given":"John","email":"jtinsley@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":793032,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}