{"pageNumber":"3409","pageRowStart":"85200","pageSize":"25","recordCount":184914,"records":[{"id":70021934,"text":"70021934 - 1999 - Test of two methods for faulting on finite-difference calculations","interactions":[],"lastModifiedDate":"2023-10-18T00:51:15.990546","indexId":"70021934","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Test of two methods for faulting on finite-difference calculations","docAbstract":"<div id=\"130406838\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Tests of two fault boundary conditions show that each converges with second order accuracy as the finite-difference grid is refined. The first method uses split nodes so that there are disjoint grids that interact via surface traction. The 3D version described here is a generalization of a method I have used extensively in 2D; it is as accurate as the 2D version. The second method represents fault slip as inelastic strain in a fault zone. Offset of stress from its elastic value is seismic moment density. Implementation of this method is quite simple in a finite-difference scheme using velocity and stress as dependent variables.</p></div>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/BSSA0890040931","issn":"00371106","usgsCitation":"Andrews, D., 1999, Test of two methods for faulting on finite-difference calculations: Bulletin of the Seismological Society of America, v. 89, no. 4, p. 931-937, https://doi.org/10.1785/BSSA0890040931.","productDescription":"7 p.","startPage":"931","endPage":"937","numberOfPages":"7","costCenters":[],"links":[{"id":229456,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"4","noUsgsAuthors":false,"publicationDate":"1999-08-01","publicationStatus":"PW","scienceBaseUri":"505ba5a5e4b08c986b320b9a","contributors":{"authors":[{"text":"Andrews, D.J.","contributorId":7416,"corporation":false,"usgs":true,"family":"Andrews","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":391763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70021935,"text":"70021935 - 1999 - Stochastic analysis of virus transport in aquifers","interactions":[],"lastModifiedDate":"2018-12-19T09:08:50","indexId":"70021935","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","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":"Stochastic analysis of virus transport in aquifers","docAbstract":"<p><span>A large-scale model of virus transport in aquifers is derived using spectral perturbation analysis. The effects of spatial variability in aquifer hydraulic conductivity and virus transport (attachment, detachment, and inactivation) parameters on large-scale virus transport are evaluated. A stochastic mean model of virus transport is developed by linking a simple system of local-scale free-virus transport and attached-virus conservation equations from the current literature with a random-field representation of aquifer and virus transport properties. The resultant mean equations for free and attached viruses are found to differ considerably from the local-scale equations on which they are based and include effects such as a free-virus effective velocity that is a function of aquifer heterogeneity as well as virus transport parameters. Stochastic mean free-virus breakthrough curves are compared with local model output in order to observe the effects of spatial variability on mean one-dimensional virus transport in three-dimensionally heterogeneous porous media. Significant findings from this theoretical analysis include the following: (1) Stochastic model breakthrough occurs earlier than local model breakthrough, and this effect is most pronounced for the least conductive aquifers studied. (2) A high degree of aquifer heterogeneity can lead to virus breakthrough actually preceding that of a conservative tracer. (3) As the mean hydraulic conductivity is increased, the mean model shows less sensitivity to the variance of the natural-logarithm hydraulic conductivity and mean virus diameter. (4) Incorporation of a heterogeneous colloid filtration term results in higher predicted concentrations than a simple first-order adsorption term for a given mean attachment rate. (5) Incorporation of aquifer heterogeneity leads to a greater range of virus diameters for which significant breakthrough occurs. (6) The mean model is more sensitive to the inactivation rate of viruses associated with solid surfaces than to the inactivation rate of viruses in solution.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/1999WR900059","usgsCitation":"Campbell Rehmann, L.L., Welty, C., and Harvey, R.W., 1999, Stochastic analysis of virus transport in aquifers: Water Resources Research, v. 35, no. 7, p. 1987-2006, https://doi.org/10.1029/1999WR900059.","productDescription":"20 p.","startPage":"1987","endPage":"2006","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":229457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9849e4b08c986b31bf5a","contributors":{"authors":[{"text":"Campbell Rehmann, Linda L.","contributorId":15073,"corporation":false,"usgs":false,"family":"Campbell Rehmann","given":"Linda","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":391765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welty, Claire","contributorId":39416,"corporation":false,"usgs":true,"family":"Welty","given":"Claire","email":"","affiliations":[],"preferred":false,"id":391766,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harvey, Ronald W. 0000-0002-2791-8503 rwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":564,"corporation":false,"usgs":true,"family":"Harvey","given":"Ronald","email":"rwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":391764,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70021936,"text":"70021936 - 1999 - Sulfur-bearing coatings on fly ash from a coal-fired power plant: Composition, origin, and influence on ash alteration","interactions":[],"lastModifiedDate":"2023-09-28T18:30:32.95995","indexId":"70021936","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1709,"text":"Fuel","active":true,"publicationSubtype":{"id":10}},"title":"Sulfur-bearing coatings on fly ash from a coal-fired power plant: Composition, origin, and influence on ash alteration","docAbstract":"<p><span>Fly ash samples collected from two locations in the exhaust stream of a coal-fired power plant differ markedly with respect to the abundance of thin (≈0.1</span><span>&nbsp;</span><span>μm) sulfur-rich surface coatings that are observable by scanning electron microscopy. The coatings, tentatively identified as an aluminum-potassium-sulfate phase, probably form upon reaction between condensed sulfuric acid aerosols and glass surfaces, and are preferentially concentrated on ash exposed to exhaust stream gases for longer. The coatings are highly soluble and if sufficiently abundant, can impart an acidic pH to solutions initially in contact with ash. These observations suggest that proposals for ash use and predictions of ash behavior during disposal should consider the transient, acid-generating potential of some ash fractions and the possible effects on initial ash leachability and alteration.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0016-2361(98)00146-X","issn":"00162361","usgsCitation":"Fishman, N., Rice, C.A., Breit, G.N., and Johnson, R., 1999, Sulfur-bearing coatings on fly ash from a coal-fired power plant: Composition, origin, and influence on ash alteration: Fuel, v. 78, no. 2, p. 187-196, https://doi.org/10.1016/S0016-2361(98)00146-X.","productDescription":"10 p.","startPage":"187","endPage":"196","costCenters":[],"links":[{"id":229458,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"78","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9de8e4b08c986b31db7e","contributors":{"authors":[{"text":"Fishman, N.S.","contributorId":59441,"corporation":false,"usgs":true,"family":"Fishman","given":"N.S.","email":"","affiliations":[],"preferred":false,"id":391767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rice, C. A.","contributorId":106116,"corporation":false,"usgs":true,"family":"Rice","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":391770,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Breit, G. N.","contributorId":94664,"corporation":false,"usgs":true,"family":"Breit","given":"G.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":391769,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, R.D.","contributorId":62360,"corporation":false,"usgs":true,"family":"Johnson","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":391768,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70021939,"text":"70021939 - 1999 - Effects of hydraulic roughness on surface textures of gravel‐bed rivers","interactions":[],"lastModifiedDate":"2018-03-20T15:28:15","indexId":"70021939","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Effects of hydraulic roughness on surface textures of gravel‐bed rivers","docAbstract":"<div class=\"article-section__content n/a main\"><p>Field studies of forest gravel‐bed rivers in northwestern Washington and southeastern Alaska demonstrate that bed‐surface grain size is responsive to hydraulic roughness caused by bank irregularities, bars, and wood debris. We evaluate textural response by comparing reach‐average median grain size (<i>D</i><sub>50</sub>) to that predicted from the total bank‐full boundary shear stress (т<sub>0</sub><sub><i>bf</i></sub>), representing a hypothetical reference condition of low hydraulic roughness. For a given т<sub>0</sub><sub><i>bf</i></sub>, channels with progressively greater hydraulic roughness have systematically finer bed surfaces, presumably due to reduced bed shear stress, resulting in lower channel competence and diminished bed load transport capacity, both of which promote textural fining. In channels with significant hydraulic roughness, observed values<span>&nbsp;</span><i>D</i><sub>50</sub><span>&nbsp;</span>can be up to 90% smaller than those predicted from т<sub>0</sub><sub><i>bf</i></sub>. We find that wood debris plays an important role at our study sites, not only providing hydraulic roughness but also influencing pool spacing, frequency of textural patches, and the amplitude and wavelength of bank and bar topography and their consequent roughness. Our observations also have biological implications. We find that textural fining due to hydraulic roughness can create usable salmonid spawning gravels in channels that otherwise would be too coarse.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/1999WR900138","usgsCitation":"Buffington, J.M., and Montgomery, D.R., 1999, Effects of hydraulic roughness on surface textures of gravel‐bed rivers: Water Resources Research, v. 35, no. 11, p. 3507-3521, https://doi.org/10.1029/1999WR900138.","productDescription":"15 p.","startPage":"3507","endPage":"3521","costCenters":[],"links":[{"id":229459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a071fe4b0c8380cd5157d","contributors":{"authors":[{"text":"Buffington, John M.","contributorId":124575,"corporation":false,"usgs":false,"family":"Buffington","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":391783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Montgomery, David R.","contributorId":67389,"corporation":false,"usgs":true,"family":"Montgomery","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":391782,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70021940,"text":"70021940 - 1999 - The carbon cycle and biogeochemical dynamics in lake sediments","interactions":[],"lastModifiedDate":"2012-03-12T17:19:39","indexId":"70021940","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2411,"text":"Journal of Paleolimnology","active":true,"publicationSubtype":{"id":10}},"title":"The carbon cycle and biogeochemical dynamics in lake sediments","docAbstract":"The concentrations of organic carbon (OC) and CaCO3 in lake sediments are often inversely related. This relation occurs in surface sediments from different locations in the same lake, surface sediments from different lakes, and with depth in Holocene sediments. Where data on accumulation rates are available, the relation holds for organic carbon and CaCO3 accumulation rates as well. An increase of several percent OC is accompanied by a decrease of several tens of percent CaCO3 indicating that the inverse relation is not due to simple dilution of one component by another. It appears from core data that once the OC concentration in the sediments becomes greater than about 12%, the CO2 produced by decomposition of that OC and production of organic acids lowers the pH of anoxic pore waters enough to dissolve any CaCO3 that reaches the sediment-water interface. In a lake with a seasonally anoxic hypolimnion, processes in the water column also can produce an inverse relation between OC and CaCO3 over time. If productivity of the lake increases, the rain rate of OC from the epilimnion increases. Biogenic removal of CO2 and accompanying increase in pH also may increase the production of CaCO3. However, the decomposition of organic matter in the hypolimnion will decrease the pH of the hypolimnion causing greater dissolution of CaCO3 and therefore a decrease in the rain rate of CaCO3 to the sediment-water interface.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Paleolimnology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1023/A:1008066118210","issn":"09212728","usgsCitation":"Dean, W., 1999, The carbon cycle and biogeochemical dynamics in lake sediments: Journal of Paleolimnology, v. 21, no. 4, p. 375-393, https://doi.org/10.1023/A:1008066118210.","startPage":"375","endPage":"393","numberOfPages":"19","costCenters":[],"links":[{"id":206337,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/A:1008066118210"},{"id":229460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baa05e4b08c986b32268f","contributors":{"authors":[{"text":"Dean, W.E.","contributorId":97099,"corporation":false,"usgs":true,"family":"Dean","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":391784,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70021941,"text":"70021941 - 1999 - Effects of humic substances on the bioconcentration of polycyclic aromatic hydrocarbons: Correlations with spectroscopic and chemical properties of humic substances","interactions":[],"lastModifiedDate":"2024-02-05T16:04:17.592232","indexId":"70021941","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Effects of humic substances on the bioconcentration of polycyclic aromatic hydrocarbons: Correlations with spectroscopic and chemical properties of humic substances","docAbstract":"<p><span>The presence of dissolved humic substances (HS, fulvic and humic acids) generally reduces the up take of hydrophobic organic compounds into aquatic organisms. The extent of this effect depends both on the concentration and on the origin of the HS. The aim of this study was to investigate the role of qualitative differences between HS from different origins. The effects of seven different HS on the bioconcentration of pyrene and benzo[</span><i>a</i><span>]pyrene (B</span><i>a</i><span>P) in the nematode&nbsp;</span><i>Caenorhabditis elegans</i><span>&nbsp;were related to the spectroscopic and chemical properties of the HS. The effect of each humic material on the bioconcentration of pyrene or B</span><i>a</i><span>P was quantified as a “biologically determined” partition coefficient&nbsp;</span><i>K</i><sub><span class=\"smallCaps\">DOC</span></sub><span>. We observed significant linear relationships between&nbsp;</span><i>K</i><sub><span class=\"smallCaps\">DOC</span></sub><span>&nbsp;and the atomic H/C ratio, the specific absorptivity at 254 nm, the content of aromatic carbons (as determined by&nbsp;</span><sup>13</sup><span>C nuclear magnetic resonance spectroscopy, the copper-complexing capacity, the content of phenolic OH groups, and the molecular weight of the HS. There was no discernible relationship of&nbsp;</span><i>K</i><sub><span class=\"smallCaps\">DOC</span></sub><span>&nbsp;with the atomic (N + O)/C ratio, an indicator of the polarity of HS. Taken together, our results show that the variability in the effects of HS from different origins could be related to variations in bulk properties of the HS. Parameters describing the aromaticity of the humic materials seemed to be most useful for estimating effects of HS on the bioconcentration of pyrene and B</span><i>a</i><span>P.</span></p>","language":"English","publisher":"Society of Environmental Toxicology and Chemistry","doi":"10.1002/etc.5620181219","issn":"07307268","usgsCitation":"Haitzer, M., Abbt-Braun, G., Traunspurger, W., and Steinberg, C., 1999, Effects of humic substances on the bioconcentration of polycyclic aromatic hydrocarbons: Correlations with spectroscopic and chemical properties of humic substances: Environmental Toxicology and Chemistry, v. 18, no. 12, p. 2782-2788, https://doi.org/10.1002/etc.5620181219.","productDescription":"7 p.","startPage":"2782","endPage":"2788","numberOfPages":"7","costCenters":[],"links":[{"id":229461,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"12","noUsgsAuthors":false,"publicationDate":"1999-12-01","publicationStatus":"PW","scienceBaseUri":"505a071be4b0c8380cd51570","contributors":{"authors":[{"text":"Haitzer, M.","contributorId":94812,"corporation":false,"usgs":true,"family":"Haitzer","given":"M.","affiliations":[],"preferred":false,"id":391787,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abbt-Braun, G.","contributorId":9021,"corporation":false,"usgs":true,"family":"Abbt-Braun","given":"G.","email":"","affiliations":[],"preferred":false,"id":391785,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Traunspurger, W.","contributorId":108272,"corporation":false,"usgs":true,"family":"Traunspurger","given":"W.","email":"","affiliations":[],"preferred":false,"id":391788,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steinberg, C.E.W.","contributorId":47536,"corporation":false,"usgs":true,"family":"Steinberg","given":"C.E.W.","email":"","affiliations":[],"preferred":false,"id":391786,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70021942,"text":"70021942 - 1999 - Metolachlor and its metabolites in tile drain and stream runoff in the canajoharie creek watershed","interactions":[],"lastModifiedDate":"2018-12-19T10:25:17","indexId":"70021942","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Metolachlor and its metabolites in tile drain and stream runoff in the canajoharie creek watershed","docAbstract":"<div class=\"hlFld-Abstract\"><div id=\"abstractBox\"><p class=\"articleBody_abstractText\">Water samples collected during April−November 1997 from tile drains beneath cultivated fields in central New York indicate that two metabolites of the herbicide metolachlor<img class=\"privateChar\" src=\"https://pubs.acs.org/entityImage/legacy/sbd.gif\" alt=\"\" data-mce-src=\"https://pubs.acs.org/entityImage/legacy/sbd.gif\">metolachlor ESA (ethanesulfonic acid) and OA (oxanilic acid)<img class=\"privateChar\" src=\"https://pubs.acs.org/entityImage/legacy/sbd.gif\" alt=\"\" data-mce-src=\"https://pubs.acs.org/entityImage/legacy/sbd.gif\">can persist in agricultural soils for 4 or more years after application and that fine-grained soils favor the transport of metolachlor ESA over metolachlor and metolachlor OA. Concentrations of metolachlor ESA from the tile drains ranged from 3.27 to 23.4 μg/L (200−1800 times higher than those of metolachlor), metolachlor OA concentrations ranged from 1.14 to 13.5 μg/L, and metolachlor concentrations ranged from less than 0.01 to 0.1 μg/L. In the receiving stream, concentrations of metolachlor ESA were always below 0.6 μg/L except during a November storm, when concentrations reached 0.85 μg/L. Concentrations of metolachlor ESA in the stream were 2−45 times higher than those of metolachlor, reflecting the greater relative concentrations of metolachlor in surface water runoff than in tile drain runoff. These results are consistent with findings in other studies that acetanilide herbicide degredates are found in much higher concentrations than parent compounds in both surface water and groundwater.</p></div></div>","language":"English","publisher":"ACS","doi":"10.1021/es9811997","issn":"0013936X","usgsCitation":"Phillips, P.J., Wall, G.R., Thurman, E., Eckhardt, D., and Vanhoesen, J., 1999, Metolachlor and its metabolites in tile drain and stream runoff in the canajoharie creek watershed: Environmental Science & Technology, v. 33, no. 20, p. 3531-3537, https://doi.org/10.1021/es9811997.","productDescription":"7 p.","startPage":"3531","endPage":"3537","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":229496,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":206351,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es9811997"}],"country":"United States","state":"New York","otherGeospatial":"Canajoharie Creek Watershed","volume":"33","issue":"20","noUsgsAuthors":false,"publicationDate":"1999-09-11","publicationStatus":"PW","scienceBaseUri":"505a5622e4b0c8380cd6d382","contributors":{"authors":[{"text":"Phillips, P. J.","contributorId":31728,"corporation":false,"usgs":true,"family":"Phillips","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":391789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wall, G. R.","contributorId":93652,"corporation":false,"usgs":true,"family":"Wall","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":391791,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":391793,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eckhardt, D. A.","contributorId":99591,"corporation":false,"usgs":true,"family":"Eckhardt","given":"D. A.","affiliations":[],"preferred":false,"id":391792,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Vanhoesen, J.","contributorId":39964,"corporation":false,"usgs":true,"family":"Vanhoesen","given":"J.","email":"","affiliations":[],"preferred":false,"id":391790,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70021943,"text":"70021943 - 1999 - Photoenhanced toxicity of a weathered oil on <i>Ceriodaphnia dubia</i> reproduction","interactions":[],"lastModifiedDate":"2017-05-23T13:07:23","indexId":"70021943","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1564,"text":"Environmental Science and Pollution Research","active":true,"publicationSubtype":{"id":10}},"title":"Photoenhanced toxicity of a weathered oil on <i>Ceriodaphnia dubia</i> reproduction","docAbstract":"<p><span>Traditionally, the toxic effects of petroleum have been investigated by conducting studies in the absence of ultraviolet radiation (UV). Photomediated toxicity is often not considered, and the toxic effects of an oil spill can be grossly underestimated. The toxicity of a weathered oil collected from a monitoring well at an abandoned oil field to</span><i class=\"EmphasisTypeItalic \">Ceriodaphnia dubia</i><span> was examined in the presence of UV. A solar simulator equipped with UVB, UVA, and cool white lamps was used to generate environmentally comparable solar radiation intensities.</span><i class=\"EmphasisTypeItalic \">C. dubia</i><span> were exposed to six concentrations of water accommodated fractions (WAF) of weathered oil in conjunction with three levels of laboratory simulated UV (Reference = &lt; 0.002 μW/cm</span><sup>2</sup><span>UVB; 3.0 μW/cm</span><sup>2</sup><span>UVA; Low = 0.30 μW/cm</span><sup>2</sup><span> UVB; 75.0 μW/cm</span><sup>2</sup><span> UVA; High = 2.0 μW/cm</span><sup>2</sup><span> UVB; 340.0 μW/cm</span><sup>2</sup><span>UVA) and visible light. Seven day static renewal bioassays were used to characterize WAF/UV toxicity. WAF toxicity significantly (p &lt; 0.05) increased when the organisms were exposed to WAF in the presence of UV. The photoenhanced toxicity of the WAF increased with WAF concentration within each UV regime. Relative to the reference light regime, the average number of neonates from adults exposed to 1.6 mg TPH/L decreased significantly by 20% within the low light regime, and by 60% within the high light regime. These results indicate that organisms exposed to dissolved-phase weathered oil in the presence of environmentally realistic solar radiation, exhibit 1.3–2.5 times greater sensitivity, relative to organisms exposed under traditional laboratory fluorescent lighting.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF02987329","issn":"09441344","usgsCitation":"Calfee, R., Little, E.E., Cleveland, L., and Barron, M., 1999, Photoenhanced toxicity of a weathered oil on <i>Ceriodaphnia dubia</i> reproduction: Environmental Science and Pollution Research, v. 6, no. 4, p. 207-212, https://doi.org/10.1007/BF02987329.","productDescription":"6 p.","startPage":"207","endPage":"212","numberOfPages":"6","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":229497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a78c9e4b0c8380cd787a5","contributors":{"authors":[{"text":"Calfee, R.D.","contributorId":85130,"corporation":false,"usgs":true,"family":"Calfee","given":"R.D.","affiliations":[],"preferred":false,"id":391796,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Little, E. E.","contributorId":13187,"corporation":false,"usgs":true,"family":"Little","given":"E.","email":"","middleInitial":"E.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":false,"id":391794,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cleveland, L.","contributorId":82084,"corporation":false,"usgs":true,"family":"Cleveland","given":"L.","email":"","affiliations":[],"preferred":false,"id":391795,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barron, M.G.","contributorId":87488,"corporation":false,"usgs":true,"family":"Barron","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":391797,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70022037,"text":"70022037 - 1999 - Movement of road salt to a small New Hampshire lake","interactions":[],"lastModifiedDate":"2018-12-19T07:59:52","indexId":"70022037","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Movement of road salt to a small New Hampshire lake","docAbstract":"Runoff of road salt from an interstate highway in New Hampshire has led to contamination of a lake and a stream that flows into the lake, in spite of the construction of a diversion berm to divert road salt runoff out of the lake drainage basin. Chloride concentration in the stream has increased by over an order of magnitude during the 23 yr since the highway was opened, and chloride concentration in the lake has tripled. Road salt moves to the lake primarily via the contaminated stream, which provides 53% of all the chloride to the lake and only 3% of the total streamflow to the lake. The stream receives discharge of salty water froth leakage through the diversion berm. Uncontaminated ground water dilutes the stream downstream of the berm. However, reversals of gradient during summer months, likely caused by transpiration from deciduous trees, result in flow of contaminated stream water into the adjacent ground water along the lowest 40-m reach of the stream. This contaminated ground water then discharges into the lake along a 70-m-wide segment of lake shore. Road salt is pervasive in the bedrock between the highway and the lake, but was not detected at all of the wells in the glacial overburden. Of the 500 m of shoreline that could receive discharge of saly ground water directly from the highway, only a 50-m-long segment appears to be contaminated.","language":"English","publisher":"Kluwer Academic Publishers","doi":"10.1023/A:1005041632056","issn":"00496979","usgsCitation":"Rosenberry, D., Bukaveckas, P., Buso, D., Likens, G., Shapiro, A., and Winter, T.C., 1999, Movement of road salt to a small New Hampshire lake: Water, Air, & Soil Pollution, v. 109, no. 1-4, p. 179-206, https://doi.org/10.1023/A:1005041632056.","productDescription":"28 p.","startPage":"179","endPage":"206","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":230400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":206621,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/A:1005041632056"}],"volume":"109","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5f21e4b0c8380cd70db0","contributors":{"authors":[{"text":"Rosenberry, D.O. 0000-0003-0681-5641","orcid":"https://orcid.org/0000-0003-0681-5641","contributorId":38500,"corporation":false,"usgs":true,"family":"Rosenberry","given":"D.O.","affiliations":[],"preferred":true,"id":392119,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bukaveckas, P.A.","contributorId":87322,"corporation":false,"usgs":true,"family":"Bukaveckas","given":"P.A.","affiliations":[],"preferred":false,"id":392121,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Buso, D.C.","contributorId":31392,"corporation":false,"usgs":true,"family":"Buso","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":392118,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Likens, G.E.","contributorId":68893,"corporation":false,"usgs":true,"family":"Likens","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":392120,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Shapiro, A.M. 0000-0002-6425-9607","orcid":"https://orcid.org/0000-0002-6425-9607","contributorId":88384,"corporation":false,"usgs":true,"family":"Shapiro","given":"A.M.","affiliations":[],"preferred":true,"id":392122,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Winter, T. C.","contributorId":23485,"corporation":false,"usgs":true,"family":"Winter","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":392117,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70021952,"text":"70021952 - 1999 - Seismic tomography as a tool for measuring stress in mines","interactions":[],"lastModifiedDate":"2012-03-12T17:19:38","indexId":"70021952","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2755,"text":"Mining Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Seismic tomography as a tool for measuring stress in mines","docAbstract":"Spokane Research Center personnel have been investigating the use of seismic tomography to monitor the behavior of a rock mass, detect hazardous ground conditions and assess the mechanical integrity of a rock mass affected by mining. Seismic tomography can be a valuable tool for determining relative stress in deep, >1,220-m (>4,000-ft), underground pillars. If high-stress areas are detected, they can be destressed prior to development or they can be avoided. High-stress areas can be monitored with successive seismic surveys to determine if stress decreases to a level where development can be initiated safely. There are several benefits to using seismic tomography to identify high stress in deep underground pillars. The technique is reliable, cost-effective, efficient and noninvasive. Also, investigators can monitor large rock masses, as well as monitor pillars during the mining cycle. By identifying areas of high stress, engineers will be able to assure that miners are working in a safer environment.Spokane Research Center personnel have been investigating the use of seismic tomography to monitor the behavior of a rock mass, detect hazardous ground conditions and assess the mechanical integrity of a rock mass affected by mining. Seismic tomography can be a valuable tool for determining relative stress in deep, >1,200-m (>4,000-ft), underground pillars. If high-stress areas are detected, they can be destressed prior to development or they can be avoided. High-stress areas can be monitored with successive seismic surveys to determine if stress decreases to a level where development can be initiated safely. There are several benefits to using seismic tomography to identify high stress in deep underground pillars. The technique is reliable, cost-effective, efficient and noninvasive. Also, investigators can monitor large rock masses, as well as monitor pillars during the mining cycle. By identifying areas of high stress. engineers will be able to assure that miners are working in a safer environment.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mining Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Soc for Mining","publisherLocation":"Metallurgy & Exploration Inc, Littleton, CO, United States","issn":"00265187","usgsCitation":"Scott, D.F., Williams, T., Denton, D., and Friedel, M., 1999, Seismic tomography as a tool for measuring stress in mines: Mining Engineering, v. 51, no. 1, p. 77-80.","startPage":"77","endPage":"80","numberOfPages":"4","costCenters":[],"links":[{"id":229569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8b6ee4b08c986b317818","contributors":{"authors":[{"text":"Scott, Douglas F.","contributorId":80726,"corporation":false,"usgs":true,"family":"Scott","given":"Douglas","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":391834,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, T.J.","contributorId":80446,"corporation":false,"usgs":true,"family":"Williams","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":391833,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Denton, D.K.","contributorId":43858,"corporation":false,"usgs":true,"family":"Denton","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":391832,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Friedel, M.J.","contributorId":90823,"corporation":false,"usgs":true,"family":"Friedel","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":391835,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70021954,"text":"70021954 - 1999 - Response of fall-staging brant and Canada geese to aircraft overflights in southwestern Alaska","interactions":[],"lastModifiedDate":"2024-07-29T23:18:02.408839","indexId":"70021954","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Response of fall-staging brant and Canada geese to aircraft overflights in southwestern Alaska","docAbstract":"Because much of the information concerning disturbance of waterfowl by aircraft is anecdotal, we examined behavioral responses of Pacific brant (Branta bernicla nigricans) and Canada geese (B. canadensis taverneri) to experimental overflights during fall staging at Izembek Lagoon, Alaska. These data were used to develop predictive models of brant and Canada goose response to aircraft altitude, type, noise, and lateral distance from flocks. Overall, 75% of brant flocks and 9% of Canada goose flocks flew in response to overflights. Mean flight and alert responses of both species were greater for rotary-wing than for fixed-wing aircraft and for high-noise than for low-noise aircraft. Increased lateral distance between an aircraft and a flock was the most consistent predictive parameter associated with lower probability of a response by geese. Altitude was a less reliable predictor because of interaction effects with aircraft type and noise. Although mean response of brant and Canada geese generally was inversely proportional to aircraft altitude, greatest response occurred at intermediate (305-760 m) altitudes. At Izembek Lagoon and other areas where there are large concentrations of waterfowl, managers should consider lateral distance from the birds as the primary criterion for establishing local flight restrictions, especially for helicopters.","language":"English","publisher":"Wildlife Management","doi":"10.2307/3802522","issn":"0022541X","usgsCitation":"Ward, D.H., Stehn, R., Erickson, W., and Derksen, D.V., 1999, Response of fall-staging brant and Canada geese to aircraft overflights in southwestern Alaska: Journal of Wildlife Management, v. 63, no. 1, p. 373-381, https://doi.org/10.2307/3802522.","productDescription":"9 p.","startPage":"373","endPage":"381","numberOfPages":"9","costCenters":[],"links":[{"id":438900,"rank":2,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9B98AK4","text":"USGS data release","linkHelpText":"Data Supporting Studies of Brant and Other Waterfowl Disturbance Behavior, Distribution, and Diet at Izembek Lagoon, Alaska, 1985-1988"},{"id":229537,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aaa44e4b0c8380cd8623a","contributors":{"authors":[{"text":"Ward, David H. 0000-0002-5242-2526 dward@usgs.gov","orcid":"https://orcid.org/0000-0002-5242-2526","contributorId":3247,"corporation":false,"usgs":true,"family":"Ward","given":"David","email":"dward@usgs.gov","middleInitial":"H.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":391839,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stehn, R.A.","contributorId":107642,"corporation":false,"usgs":true,"family":"Stehn","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":391841,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Erickson, W.P.","contributorId":65722,"corporation":false,"usgs":true,"family":"Erickson","given":"W.P.","email":"","affiliations":[],"preferred":false,"id":391840,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Derksen, Dirk V. dderksen@usgs.gov","contributorId":2269,"corporation":false,"usgs":true,"family":"Derksen","given":"Dirk","email":"dderksen@usgs.gov","middleInitial":"V.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":391838,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70181039,"text":"70181039 - 1999 - Status and biology of the Steller's eider in Yakutia, Russia","interactions":[],"lastModifiedDate":"2026-01-30T19:23:54.869475","indexId":"70181039","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1193,"text":"Casarca","active":true,"publicationSubtype":{"id":10}},"title":"Status and biology of the Steller's eider in Yakutia, Russia","docAbstract":"<p>No abstract available.</p>","language":"Russian, English","usgsCitation":"Degtyarev, A.G., Sleptsov, S., Troev, S., Pearce, J.M., and Petersen, M.R., 1999, Status and biology of the Steller's eider in Yakutia, Russia: Casarca, v. 5, p. 249-262.","productDescription":"14 p.","startPage":"249","endPage":"262","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"links":[{"id":335199,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia","state":"Yakutia","volume":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a18225e4b0c825128564ae","contributors":{"authors":[{"text":"Degtyarev, Andrei G.","contributorId":13775,"corporation":false,"usgs":false,"family":"Degtyarev","given":"Andrei","email":"","middleInitial":"G.","affiliations":[{"id":28156,"text":"Yakutsk Institute of Biology, Yakutsk, Russia","active":true,"usgs":false}],"preferred":false,"id":663423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sleptsov, S.M.","contributorId":179381,"corporation":false,"usgs":false,"family":"Sleptsov","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":663424,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Troev, S.P.","contributorId":179382,"corporation":false,"usgs":false,"family":"Troev","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":663425,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pearce, John M. 0000-0002-8503-5485 jpearce@usgs.gov","orcid":"https://orcid.org/0000-0002-8503-5485","contributorId":181766,"corporation":false,"usgs":true,"family":"Pearce","given":"John","email":"jpearce@usgs.gov","middleInitial":"M.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":663426,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Petersen, Margaret R. 0000-0001-6082-3189 mrpetersen@usgs.gov","orcid":"https://orcid.org/0000-0001-6082-3189","contributorId":167729,"corporation":false,"usgs":true,"family":"Petersen","given":"Margaret","email":"mrpetersen@usgs.gov","middleInitial":"R.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":663427,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70021966,"text":"70021966 - 1999 - Landscape patterns of CH4 fluxes in an alpine tundra ecosystem","interactions":[],"lastModifiedDate":"2012-03-12T17:19:56","indexId":"70021966","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1007,"text":"Biogeochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Landscape patterns of CH4 fluxes in an alpine tundra ecosystem","docAbstract":"We measured CH4 fluxes from three major plant communities characteristic of alpine tundra in the Colorado Front Range. Plant communities in this ecosystem are determined by soil moisture regimes induced by winter snowpack distribution. Spatial patterns of CH4 flux during the snow-free season corresponded roughly with these plant communities. In Carex-dominated meadows, which receive the most moisture from snowmelt, net CH4 production occurred. However, CH4 production in one Carex site (seasonal mean = +8.45 mg CH4 m-2 d-1) was significantly larger than in the other Carex sites (seasonal means = -0.06 and +0.05 mg CH4 m-2 d-1). This high CH4 flux may have resulted from shallower snowpack during the winter. In Acomastylis meadows, which have an intermediate moisture regime, CH4 oxidation dominated (seasonal mean = -0.43 mg CH4 m-2 d-1). In the windswept Kobresia meadow plant community, which receive the least amount of moisture from snowmelt, only CH4 oxidation was observed (seasonal mean = -0.77 mg CH4 m-2 d-1). Methane fluxes correlated with a different set of environmental factors within each plant community. In the Carex plant community, CH4 emission was limited by soil temperature. In the Acomastylis meadows, CH4 oxidation rates correlated positively with soil temperature and negatively with soil moisture. In the Kobresia community, CH4 oxidation was stimulated by precipitation. Thus, both snow-free season CH4 fluxes and the controls on those CH4 fluxes were related to the plant communities determined by winter snowpack.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Biogeochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1023/A:1006130911046","issn":"01682563","usgsCitation":"West, A., Brooks, P.D., Fisk, M., Smith, L.K., Holland, E., Jaeger, C.H., Babcock, S., Lai, R., and Schmidt, S., 1999, Landscape patterns of CH4 fluxes in an alpine tundra ecosystem: Biogeochemistry, v. 45, no. 3, p. 243-264, https://doi.org/10.1023/A:1006130911046.","startPage":"243","endPage":"264","numberOfPages":"22","costCenters":[],"links":[{"id":206198,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/A:1006130911046"},{"id":229091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4418e4b0c8380cd6685b","contributors":{"authors":[{"text":"West, A.E.","contributorId":84100,"corporation":false,"usgs":true,"family":"West","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":391886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooks, P. D.","contributorId":46060,"corporation":false,"usgs":true,"family":"Brooks","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":391881,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fisk, M.C.","contributorId":24944,"corporation":false,"usgs":true,"family":"Fisk","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":391880,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Lesley K.","contributorId":82657,"corporation":false,"usgs":true,"family":"Smith","given":"Lesley","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":391885,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Holland, E.A.","contributorId":7648,"corporation":false,"usgs":true,"family":"Holland","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":391879,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jaeger, C. H. III","contributorId":56818,"corporation":false,"usgs":true,"family":"Jaeger","given":"C.","suffix":"III","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":391882,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Babcock, S.","contributorId":58039,"corporation":false,"usgs":true,"family":"Babcock","given":"S.","email":"","affiliations":[],"preferred":false,"id":391883,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Lai, R.S.","contributorId":108270,"corporation":false,"usgs":true,"family":"Lai","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":391887,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Schmidt, S.K.","contributorId":58412,"corporation":false,"usgs":true,"family":"Schmidt","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":391884,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70021967,"text":"70021967 - 1999 - Chronology of polyphase extension in the Windermere Hills, northeast Nevada","interactions":[],"lastModifiedDate":"2023-12-19T13:03:16.951284","indexId":"70021967","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Chronology of polyphase extension in the Windermere Hills, northeast Nevada","docAbstract":"<div id=\"15009194\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Fission-track and<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar dating and chemical correlation of volcanic strata exposed in the Windermere Hills and northern Pequop Mountains, northeast Nevada, indicate a protracted, polyphase history of Tertiary (late Eocene–late Miocene) extension along the northern margin of a major Cordilleran metamorphic core complex. Early extension is recorded by a west-tilted half graben filled with early Oligocene (34.79 ± 0.18–39.18 ± 0.12 Ma) sedimentary rocks in the eastern Windermere Hills above the low-angle Black Mountain detachment fault. The early Oligocene half graben conformably overlies a widespread suite of late Eocene (39.18 ± 0.12–40.38 ± 0.06 Ma) calc-alkaline volcanic rocks, reflecting a temporal link between early extension at a high structural level and the end of the ignimbrite flare-up. These strata are cut by east-west–striking normal faults, which are exposed along, and parallel to, the northern margin of the metamorphic complex. Available age data (e.g., between 14.93 ± 0.08 and 34.79 ± 0.18 Ma) permit the interpretation that the east-west–striking faults formed at the same time as, or after, large-magnitude unroofing of high-grade rocks. We interpret the east-west–striking faults to accommodate differential uplift of greenschist-grade metamorphic rocks in the upper crust, above a lateral ramp in a west-northwest–directed mylonitic shear zone. Subsequent extension in the Windermere Hills is defined by deep, rapidly filled half grabens of middle Miocene (&lt;7.42 ± 2.0 to 14.93 ± 0.08 Ma) age that unconformably overlie older faults and synextensional deposits. These are the youngest half grabens in the region and are inferred to be initiated by extensional stresses imparted to the base of the lithosphere by a laterally spreading mantle plume (e.g., the Yellowstone hotspot) located in southeastern Oregon at this time.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1999)111<0011:COPEIT>2.3.CO;2","issn":"00167606","usgsCitation":"Mueller, K., Cerveny, P., Perkins, M.E., and Snee, L., 1999, Chronology of polyphase extension in the Windermere Hills, northeast Nevada: Geological Society of America Bulletin, v. 111, no. 1, p. 11-27, https://doi.org/10.1130/0016-7606(1999)111<0011:COPEIT>2.3.CO;2.","productDescription":"17 p.","startPage":"11","endPage":"27","numberOfPages":"17","costCenters":[],"links":[{"id":229092,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Windermere Hills","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.89568843034513,\n              41.97975529646908\n            ],\n            [\n              -116.89568843034513,\n              39.499640649297646\n            ],\n            [\n              -114.12713374284547,\n              39.499640649297646\n            ],\n            [\n              -114.12713374284547,\n              41.97975529646908\n            ],\n            [\n              -116.89568843034513,\n              41.97975529646908\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"111","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f5f8e4b0c8380cd4c50d","contributors":{"authors":[{"text":"Mueller, K.J.","contributorId":101403,"corporation":false,"usgs":true,"family":"Mueller","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":391891,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cerveny, P.K.","contributorId":94810,"corporation":false,"usgs":true,"family":"Cerveny","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":391889,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Perkins, M. E.","contributorId":92707,"corporation":false,"usgs":true,"family":"Perkins","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":391888,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Snee, L.W.","contributorId":99981,"corporation":false,"usgs":true,"family":"Snee","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":391890,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70021968,"text":"70021968 - 1999 - Regeneration alternatives for upland white spruce after burning and logging in interior Alaska","interactions":[],"lastModifiedDate":"2012-03-12T17:19:55","indexId":"70021968","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1170,"text":"Canadian Journal of Forest Research","active":true,"publicationSubtype":{"id":10}},"title":"Regeneration alternatives for upland white spruce after burning and logging in interior Alaska","docAbstract":"Site-preparation and regeneration methods for white spruce (Picea glauca (Moench) Voss) were tested near Fairbanks, Alaska, on two upland sites which had been burned in a wildfire and salvage logged. After 5 and 10 years, white spruce regeneration did not differ among the four scarification methods but tended to be lower without scarification. Survival of container-grown planted seedlings stabilized after 3 years at 93% with scarification and at 76% without scarification. Broadcast seeding was also successful, with one or more seedlings on 80% of the scarified 6-m2 subplots and on 60% of the unscarified subplots after 12 years. Natural regeneration after 12 years exceeded expectations, with seedlings on 50% of the 6-m2 subplots 150 m from a seed source and on 28% of the subplots 230 m from a seed source. After 5 years, 37% of the scarified unsheltered seed spots and 52% of the scarified seed spots with cone shelters had one or more seedlings, but only 16% of the unscarified seed spots had seedlings, with and without funnel shelters. Growth rates for all seedlings were higher than on similar unburned sites. The results show positive effects of burning in interior Alaska, and suggest planting seedlings, broadcast seeding, and natural seedfall, alone or in combination, as viable options for similar sites.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Forest Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00455067","usgsCitation":"Densmore, R., Juday, G., and Zasada, J., 1999, Regeneration alternatives for upland white spruce after burning and logging in interior Alaska: Canadian Journal of Forest Research, v. 29, no. 4, p. 413-423.","startPage":"413","endPage":"423","numberOfPages":"11","costCenters":[],"links":[{"id":229121,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a453e4b0e8fec6cdbb2f","contributors":{"authors":[{"text":"Densmore, R.V.","contributorId":72953,"corporation":false,"usgs":true,"family":"Densmore","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":391893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Juday, G.P.","contributorId":82082,"corporation":false,"usgs":true,"family":"Juday","given":"G.P.","email":"","affiliations":[],"preferred":false,"id":391894,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zasada, J.C.","contributorId":46245,"corporation":false,"usgs":true,"family":"Zasada","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":391892,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70022033,"text":"70022033 - 1999 - Greigite (Fe3S4) as an indicator of drought - The 1912-1994 sediment magnetic record from White Rock Lake, Dallas, Texas, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:19:51","indexId":"70022033","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2411,"text":"Journal of Paleolimnology","active":true,"publicationSubtype":{"id":10}},"title":"Greigite (Fe3S4) as an indicator of drought - The 1912-1994 sediment magnetic record from White Rock Lake, Dallas, Texas, USA","docAbstract":"Combined magnetic and geochemical studies were conducted on sediments from White Rock Lake, a reservoir in suburban Dallas (USA), to investigate how land use has affected sediment and water quality since the reservoir was filled in 1912. The chronology of a 167-cm-long core is constrained by the recognition of the pre-reservoir surface and by 137Cs results. In the reservoir sediments, magnetic susceptibility (MS) and isothermal remanent magnetization (IRM) are largely carried by detrital titanomagnetite that originally formed in igneous rocks. Titanomagnetite and associated hematite are the dominant iron oxides in a sample from the surficial deposit in the watershed but are absent in the underlying Austin Chalk. Therefore, these minerals were transported by wind into the watershed. After about 1960, systematic decreases in Ti, Fe, and Al suggest diminished input of detrital Fe-Ti oxides from the surficial deposits. MS and IRM remain constant over this interval, however, implying compensation by an increase in strongly magnetic material derived from human activity. Anthropogenic magnetite in rust and ferrite spherules (from fly ash?) are more common in sediment deposited after about 1970 than before and may account for the constant magnetization despite the implied decrease in detrital Fe-Ti oxides. An unexpected finding is the presence of authigenic greigite (Fe3S4), the abundance of which is at least partly controlled by climate. Greigite is common in sediments that predate about 1975, with zones of concentration indicated by relatively high IRM/MS. High greigite contents in sediment deposited during the early to mid-1950s and during the mid-1930s correspond to several-year periods of below-average precipitation and drought from historical records. Relatively long water-residence times in the reservoir during these periods may have led to elevated levels of sulfate available for bacterial sulfate reduction. The sulfate was probably derived via the oxidation of pyrite that is common in the underlying Austin Chalk. These results provide a basis for the paleoenvironmental interpretation of greigite occurrence in older lake sediments. The results also indicate that greigite formed rapidly and imply that it can be preserved in the amounts produced over a short time span (in this lake, only a few years). This finding thus suggests that, in some lacustrine settings, greigite is capable of recording paleomagnetic secular variation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Paleolimnology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1023/A:1008027815203","issn":"09212728","usgsCitation":"Reynolds, R.L., Rosenbaum, J.G., Van Metre, P., Tuttle, M., Callender, E., and Goldin, A., 1999, Greigite (Fe3S4) as an indicator of drought - The 1912-1994 sediment magnetic record from White Rock Lake, Dallas, Texas, USA: Journal of Paleolimnology, v. 21, no. 2, p. 193-206, https://doi.org/10.1023/A:1008027815203.","startPage":"193","endPage":"206","numberOfPages":"14","costCenters":[],"links":[{"id":206587,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/A:1008027815203"},{"id":230320,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2a6de4b0c8380cd5b186","contributors":{"authors":[{"text":"Reynolds, R. L. 0000-0002-4572-2942","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":79885,"corporation":false,"usgs":true,"family":"Reynolds","given":"R.","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":392106,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenbaum, J. G.","contributorId":96685,"corporation":false,"usgs":true,"family":"Rosenbaum","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":392107,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Van Metre, P.","contributorId":31142,"corporation":false,"usgs":true,"family":"Van Metre","given":"P.","affiliations":[],"preferred":false,"id":392104,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tuttle, M.","contributorId":26397,"corporation":false,"usgs":true,"family":"Tuttle","given":"M.","affiliations":[],"preferred":false,"id":392103,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Callender, E.","contributorId":72528,"corporation":false,"usgs":true,"family":"Callender","given":"E.","email":"","affiliations":[],"preferred":false,"id":392105,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Goldin, A.","contributorId":24950,"corporation":false,"usgs":true,"family":"Goldin","given":"A.","email":"","affiliations":[],"preferred":false,"id":392102,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70022032,"text":"70022032 - 1999 - Copper, lead, mercury and zinc in periphyton from the south Florida ecosystem","interactions":[],"lastModifiedDate":"2018-12-21T06:33:15","indexId":"70022032","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3609,"text":"Toxicological and Environmental Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Copper, lead, mercury and zinc in periphyton from the south Florida ecosystem","docAbstract":"Periphyton samples from the Big Cypress National Preserve were analyzed for concentrations of copper, lead, zinc, mercury, and methylmercury. Concentrations of organic carbon, inorganic carbon, nitrogen, and phosphorus in periphyton samples also were determined. The samples were extracted with sodium acetate solution at a pH of 5.5 to determine exchangeable and carbonate phase metal concentrations in periphyton. Total metal concentrations in the periphyton were directly related to the degree of calcite saturation in the water column. Exchangeable and carbonate phase metal concentrations were directly related to the percent inorganic carbon in the samples. A connection between the geochemistry of trace metals and calcite precipitation and dissolution is suggested.","language":"English","publisher":"Taylor and Francis","doi":"10.1080/02772249909358754","issn":"02772248","usgsCitation":"Cox, T., Simon, N., and Newland, L., 1999, Copper, lead, mercury and zinc in periphyton from the south Florida ecosystem: Toxicological and Environmental Chemistry, v. 70, no. 3-4, p. 259-274, https://doi.org/10.1080/02772249909358754.","productDescription":"16 p.","startPage":"259","endPage":"274","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":230319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"70","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fc01e4b0c8380cd4e093","contributors":{"authors":[{"text":"Cox, T.","contributorId":42249,"corporation":false,"usgs":true,"family":"Cox","given":"T.","email":"","affiliations":[],"preferred":false,"id":392099,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simon, N.S.","contributorId":103272,"corporation":false,"usgs":true,"family":"Simon","given":"N.S.","email":"","affiliations":[],"preferred":false,"id":392101,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Newland, L.","contributorId":96444,"corporation":false,"usgs":true,"family":"Newland","given":"L.","email":"","affiliations":[],"preferred":false,"id":392100,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70180174,"text":"70180174 - 1999 - Elwha River ecosystem restoration: Potential effects and restoration methods -- fisheries investigations","interactions":[],"lastModifiedDate":"2017-01-25T11:23:29","indexId":"70180174","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Elwha River ecosystem restoration: Potential effects and restoration methods -- fisheries investigations","docAbstract":"<p>Abstract not available</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Seattle, WA","doi":"10.3133/70180174","usgsCitation":"Reisenbichler, R., 1999, Elwha River ecosystem restoration: Potential effects and restoration methods -- fisheries investigations, 94 p. , https://doi.org/10.3133/70180174.","productDescription":"94 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":333892,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c79de4b0ba3b075e05ed","contributors":{"authors":[{"text":"Reisenbichler, R.R.","contributorId":77356,"corporation":false,"usgs":true,"family":"Reisenbichler","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":660625,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70022031,"text":"70022031 - 1999 - Deglaciation of the northwestern White Mountains, New Hampshire","interactions":[],"lastModifiedDate":"2023-11-15T17:34:08.03951","indexId":"70022031","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1773,"text":"Geographie Physique et Quaternaire","active":true,"publicationSubtype":{"id":10}},"title":"Deglaciation of the northwestern White Mountains, New Hampshire","docAbstract":"<p><span>The mode of deglaciation in the northwestern White Mountains of New Hampshire has been controversial since the mid 1800's. Early workers believed that active ice deposited the Bethlehem Moraine complex in the Ammonoosuc River basin during recession of the last ice sheet. In the 1930's this deglaciation model was replaced by the concept of widespread simultaneous stagnation and downwastage of Late Wisconsinan ice. The present authors reexamined the Bethlehem Moraine complex and support the original interpretation of a series of moraines deposited by active ice. We found other moraine clusters of similar age to the northeast in the Johns River and Israel River basins. Ice-marginal deposits that probably correlate with the Bethlehem Moraine also occur west of Littleton. The Bethlehem Moraine complex and equivalent deposits in adjacent areas were formed by readvance and oscillatory retreat of the Connecticut Valley lobe of the Laurentide Ice Sheet. This event is called the Littleton-Bethlehem Readvance. Throughout the study area, sequences of glaciolacustrine deposits and meltwater drainage channels indicate progressive northward recession of the glacier margin. Radiocarbon dates from nearby New England and Québec suggest that the ice sheet withdrew from this part of the White Mountains between about 12 500 and 12 000&nbsp;</span><sup>14</sup><span>&nbsp;C yr BP. We attribute the Littleton- Bethlehem Readvance to a brief climatic cooling during Older Dyas time, close to 12,000 BP.</span></p>","language":"English","publisher":"Les Presses de l'Université de Montréal","doi":"10.7202/004882ar","usgsCitation":"Thompson, W.B., Fowler, B.K., and Dorion, C.C., 1999, Deglaciation of the northwestern White Mountains, New Hampshire: Geographie Physique et Quaternaire, v. 53, no. 1, p. 59-77, https://doi.org/10.7202/004882ar.","productDescription":"19 p.","startPage":"59","endPage":"77","numberOfPages":"19","costCenters":[],"links":[{"id":479509,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.7202/004882ar","text":"External Repository"},{"id":230887,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Hampshire","otherGeospatial":"White Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.03243018820368,\n              44.504681864058426\n            ],\n            [\n              -72.05787655312217,\n              44.504681864058426\n            ],\n            [\n              -72.05787655312217,\n              44.13794517845437\n            ],\n            [\n              -71.03243018820368,\n              44.13794517845437\n            ],\n            [\n              -71.03243018820368,\n              44.504681864058426\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"53","issue":"1","noUsgsAuthors":false,"publicationDate":"2002-10-02","publicationStatus":"PW","scienceBaseUri":"5059fe53e4b0c8380cd4ec8b","contributors":{"authors":[{"text":"Thompson, Woodrow B.","contributorId":67482,"corporation":false,"usgs":true,"family":"Thompson","given":"Woodrow","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":392098,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fowler, Brian K.","contributorId":83975,"corporation":false,"usgs":true,"family":"Fowler","given":"Brian","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":392096,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dorion, C. C.","contributorId":93236,"corporation":false,"usgs":true,"family":"Dorion","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":392097,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70021969,"text":"70021969 - 1999 - Application of geologic map information to water quality issues in the southern part of the Chesapeake Bay watershed, Maryland and Virginia, eastern United States","interactions":[],"lastModifiedDate":"2012-03-12T17:19:55","indexId":"70021969","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Application of geologic map information to water quality issues in the southern part of the Chesapeake Bay watershed, Maryland and Virginia, eastern United States","docAbstract":"Geologic map units contain much information about the mineralogy, chemistry, and physical attributes of the rocks mapped. This paper presents information from regional-scale geologic maps in Maryland and Virginia, which are in the southern part of the Chesapeake Bay watershed in the eastern United States. The geologic map information is discussed and analyzed in relation to water chemistry data from shallow wells and stream reaches in the area. Two environmental problems in the Chesapeake Bay watershed are used as test examples. The problems, high acidity and high nitrate concentrations in streams and rivers, tend to be mitigated by some rock and sediment types and not by others. Carbonate rocks (limestone, dolomite, and carbonate-cemented rocks) have the greatest capacity to neutralize acidic ground water and surface water in contact with them. Rocks and sediments having high carbon or sulfur contents (such as peat and black shale) potentially contribute the most toward denitrification of ground water and surface water in contact with them. Rocks and sediments that are composed mostly of quartz, feldspar, and light-colored clay (rocks such as granite and sandstone, sediments such as sand and gravel) tend not to alter the chemistry of waters that are in contact with them. The testing of relationships between regionally mapped geologic units and water chemistry is in a preliminary stage, and initial results are encouraging.Geologic map units contain much information about the mineralogy, chemistry, and physical attributes of the rocks mapped. This paper presents information from regional-scale geologic maps in Maryland and Virginia, which are in the southern part of the Chesapeake Bay watershed in the eastern United States. The geologic map information is discussed and analyzed in relation to water chemistry data from shallow wells and stream reaches in the area. Two environmental problems in the Chesapeake Bay watershed are used as test examples. The problems, high acidity and high nitrate concentrations in streams and rivers, tend to be mitigated by some rock and sediment types and not by others. Carbonate rocks (limestone, dolomite, and carbonate-cemented rocks) have the greatest capacity to neutralize acidic ground water and surface water in contact with them. Rocks and sediments having high carbon or sulfur contents (such as peat and black shale) potentially contribute the most toward denitrification of ground water and surface water in contact with them. Rocks and sediments that are composed mostly of quartz, feldspar, and light-colored clay (rocks such as granite and sandstone, sediments such as sand and gravel) tend not to alter the chemistry of waters that are in contact with them. The testing of relationships between regionally mapped geologic units and water chemistry is in a preliminary stage, and initial results are encouraging.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geochemical Exploration","largerWorkSubtype":{"id":10,"text":"Journal Article"},"conferenceTitle":"Proceedings of the 4th International Symposium on Environmental Geochemistry ISEG. Pt 1 (of 2)","conferenceDate":"5 October 1997 through 10 October 1997","conferenceLocation":"Vail, CO, USA","language":"English","publisher":"Elsevier Sci B.V.","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/S0375-6742(98)00043-0","issn":"03756742","usgsCitation":"McCartan, L., Peper, J., Bachman, L., and Horton, J.W., 1999, Application of geologic map information to water quality issues in the southern part of the Chesapeake Bay watershed, Maryland and Virginia, eastern United States: Journal of Geochemical Exploration, v. 64, no. 1-3 -3 pt 1, p. 355-376, https://doi.org/10.1016/S0375-6742(98)00043-0.","startPage":"355","endPage":"376","numberOfPages":"22","costCenters":[],"links":[{"id":206207,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0375-6742(98)00043-0"},{"id":229122,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"64","issue":"1-3 -3 pt 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ec9fe4b0c8380cd493b2","contributors":{"authors":[{"text":"McCartan, L.","contributorId":55153,"corporation":false,"usgs":true,"family":"McCartan","given":"L.","affiliations":[],"preferred":false,"id":391897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peper, J. D.","contributorId":29387,"corporation":false,"usgs":true,"family":"Peper","given":"J. D.","affiliations":[],"preferred":false,"id":391895,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bachman, L. J.","contributorId":47760,"corporation":false,"usgs":true,"family":"Bachman","given":"L. J.","affiliations":[],"preferred":false,"id":391896,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Horton, J. Wright Jr. 0000-0001-6756-6365 whorton@usgs.gov","orcid":"https://orcid.org/0000-0001-6756-6365","contributorId":81184,"corporation":false,"usgs":true,"family":"Horton","given":"J.","suffix":"Jr.","email":"whorton@usgs.gov","middleInitial":"Wright","affiliations":[],"preferred":false,"id":391898,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70022030,"text":"70022030 - 1999 - The Bear Brook Watershed, Maine (BBWM), USA","interactions":[],"lastModifiedDate":"2012-03-12T17:19:43","indexId":"70022030","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1552,"text":"Environmental Monitoring and Assessment","onlineIssn":"1573-2959","printIssn":"0167-6369","active":true,"publicationSubtype":{"id":10}},"title":"The Bear Brook Watershed, Maine (BBWM), USA","docAbstract":"The Bear Brook Watershed Manipulation project in Maine is a paired calibrated watershed study funded by the U.S. EPA. The research program is evaluating whole ecosystem response to elevated inputs of acidifying chemicals. The consists of a 2.5 year calibration period (1987-1989), nine years of chemical additions of (NH4)2SO4 (15N- and 34S-enriched for several years) to West Bear watershed (1989-1998), followed by a recovery period. The other watershed, East Bear, serves as a reference. Dosing is in six equal treatments/yr of 1800 eq SO4 and NH4/ha/yr, a 200% increase over 1988 loading (wet plus dry) for SO4 300% for N (wet NO3 + NH4). The experimental and reference watersheds are forested with mixed hard- and softwoods, and have thin acidic soils, areas of 10.2 and 10.7 ha and relief of 210 m. Thin till of variable composition is underlain by metasedimentary pelitic rocks and calc-silicate gneiss intruded by granite dikes and sills. For the period 1987-1995, precipitation averaged 1.4 m/yr, had a mean pH of 4.5, with SO4, NO3, and NH4 concentrations of 26, 14, and 7 ??eq/L, respectively. The nearly perrenial streams draining each watershed have discharges ranging from 0 (East Bear stops flowing for one to two months per year) to 150 L/sec. Prior to manipulation, East Bear and West Bear had a volume weighted annual mean pH of approximately 5.4, alkalinity = 0 to 4 ??eq/L, total base cations = 184 ??eq/L (sea-salt corrected = 118 ??eq/L), and SO4 = 100 to 111 ??eq/L. Nitrate ranged from 0 to 30 ??eq/L with an annual mean of 6 to 25 ??eq/L; dissolved organic carbon (DOC) ranged from 1 to 7 mg/L but was typically less than 3. Episodic acidification occurred at high discharge and was caused by dilution of cations, slightly increased DOC, significantly higher NO3, and the sea-salt effect. Depressions in pH were accompanied by increases in inorganic Al. The West Bear catchment responded to the chemical additions with increased export of base cations, Al, SO4, NO3, and decreased pH, ANC, and DOC. Silica remained relatively constant. Neutralization of the acidifying chemicals occurred dominantly by cation desorption and mobilization of Al.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Monitoring and Assessment","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Kluwer Academic Publishers","publisherLocation":"Dordrecht, Netherlands","doi":"10.1023/A:1006115011381","issn":"01676369","usgsCitation":"Norton, S., Kahl, J., Fernandez, I., Haines, T., Rustad, L., Nodvin, S., Scofield, J., Strickland, T., Erickson, H., Wigington, P., and Lee, J., 1999, The Bear Brook Watershed, Maine (BBWM), USA: Environmental Monitoring and Assessment, v. 55, no. 1, p. 7-51, https://doi.org/10.1023/A:1006115011381.","startPage":"7","endPage":"51","numberOfPages":"45","costCenters":[],"links":[{"id":206831,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/A:1006115011381"},{"id":230886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba698e4b08c986b3211fe","contributors":{"authors":[{"text":"Norton, S.","contributorId":45671,"corporation":false,"usgs":true,"family":"Norton","given":"S.","affiliations":[],"preferred":false,"id":392091,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kahl, J.","contributorId":32486,"corporation":false,"usgs":true,"family":"Kahl","given":"J.","affiliations":[],"preferred":false,"id":392088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fernandez, I.","contributorId":33881,"corporation":false,"usgs":true,"family":"Fernandez","given":"I.","affiliations":[],"preferred":false,"id":392089,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Haines, T.","contributorId":12401,"corporation":false,"usgs":true,"family":"Haines","given":"T.","email":"","affiliations":[],"preferred":false,"id":392085,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rustad, L.","contributorId":98687,"corporation":false,"usgs":true,"family":"Rustad","given":"L.","affiliations":[],"preferred":false,"id":392095,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Nodvin, S.","contributorId":67686,"corporation":false,"usgs":true,"family":"Nodvin","given":"S.","email":"","affiliations":[],"preferred":false,"id":392093,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Scofield, J.","contributorId":17187,"corporation":false,"usgs":true,"family":"Scofield","given":"J.","email":"","affiliations":[],"preferred":false,"id":392086,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Strickland, T.","contributorId":68918,"corporation":false,"usgs":true,"family":"Strickland","given":"T.","email":"","affiliations":[],"preferred":false,"id":392094,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Erickson, H.","contributorId":41177,"corporation":false,"usgs":true,"family":"Erickson","given":"H.","email":"","affiliations":[],"preferred":false,"id":392090,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Wigington, P. Jr.","contributorId":18928,"corporation":false,"usgs":true,"family":"Wigington","given":"P.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":392087,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Lee, J.","contributorId":58596,"corporation":false,"usgs":true,"family":"Lee","given":"J.","affiliations":[],"preferred":false,"id":392092,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70022029,"text":"70022029 - 1999 - Spatial and temporal patterns of nonindigenous fish introductions in the United States","interactions":[],"lastModifiedDate":"2016-01-05T09:38:30","indexId":"70022029","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1657,"text":"Fisheries","onlineIssn":"1548-8446","printIssn":"0363-2415","active":true,"publicationSubtype":{"id":10}},"title":"Spatial and temporal patterns of nonindigenous fish introductions in the United States","docAbstract":"<p>In 1978 biologists in Gainesville, Florida, began compiling records on the distribution and status of nonindigenous fishes known in U.S. inland waters. The database, now in electronic format, currently contains approximately 17,000 records representing more than 500 nonindigenous fish taxa (i.e., species, hybrids, and unidentified forms). Of these taxa, 317 (61%) are native to the United States but have been introduced by humans into U.S. drainages outside their natural geographic ranges; 185 (35%) are fishes introduced from foreign countries; and 22 (4%) are hybrids. Of the introduced foreign fish taxa, 71 (38%) are species that have established (i.e., reproducing) or possibly established populations in open U.S. waters. The database is a useful tool for natural resource managers and other decision makers. Although we periodically revise records and constantly enter new ones, our database is fairly updated; thus, we are able to more thoroughly analyze patterns of introduction and the spread of nonindigenous fishes within the United States. Moreover, information gaps exposed by the data set should serve to stimulate and guide future research on nonindigenous fishes. This paper introduces our database and provides an overview of temporal and spatial patterns of nonindigenous fish distributions in U.S. inland waters.</p>","language":"English","publisher":"Elsevier","doi":"10.1577/1548-8446(1999)024<0016:SATPON>2.0.CO;2","issn":"03632415","usgsCitation":"Nico, L., and Fuller, P., 1999, Spatial and temporal patterns of nonindigenous fish introductions in the United States: Fisheries, v. 24, no. 1, p. 16-27, https://doi.org/10.1577/1548-8446(1999)024<0016:SATPON>2.0.CO;2.","productDescription":"12 p.","startPage":"16","endPage":"27","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":230849,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9441e4b08c986b31a977","contributors":{"authors":[{"text":"Nico, L.G. 0000-0002-4488-7737","orcid":"https://orcid.org/0000-0002-4488-7737","contributorId":83052,"corporation":false,"usgs":true,"family":"Nico","given":"L.G.","affiliations":[],"preferred":false,"id":392084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fuller, P.L. 0000-0002-9389-9144","orcid":"https://orcid.org/0000-0002-9389-9144","contributorId":68245,"corporation":false,"usgs":true,"family":"Fuller","given":"P.L.","affiliations":[],"preferred":false,"id":392083,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000484,"text":"1000484 - 1999 - A list of Michigan Corixidae (Hemiptera) with four new state records from the Great Lakes of Michigan","interactions":[],"lastModifiedDate":"2016-04-04T10:56:10","indexId":"1000484","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1520,"text":"Entomological News","active":true,"publicationSubtype":{"id":10}},"title":"A list of Michigan Corixidae (Hemiptera) with four new state records from the Great Lakes of Michigan","docAbstract":"<p><i>Corisella tarsalis</i>, <i>Sigara lineata</i>, <i>Trichocorixa borealis</i>, and <i>Trichocorixa kanza</i> were recently identified from Michigan and constitute new state records. These four species were collected from two of the Great Lakes or their connecting rivers and increase the number of corixids for Michigan to 47 species. We newly report the genus <i>Corisella</i> for Michigan. Although most abundant in the western United States and Canada, scattered <i>Corisella</i> records in the Midwest (Wisconsin, Ohio and Ontario, Canada) indicated there was a good probability of its occurrence in Michigan. Finally, we provide an updated list of Michigan Corixidae.</p>","language":"English","usgsCitation":"Chordas, S.W., and Hudson, P.L., 1999, A list of Michigan Corixidae (Hemiptera) with four new state records from the Great Lakes of Michigan: Entomological News, v. 110, no. 4, p. 246-250.","productDescription":"5 p.","startPage":"246","endPage":"250","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":130319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266609,"type":{"id":11,"text":"Document"},"url":"https://biostor.org/reference/76587"}],"volume":"110","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae322","contributors":{"authors":[{"text":"Chordas, Stephen W. III","contributorId":87089,"corporation":false,"usgs":true,"family":"Chordas","given":"Stephen","suffix":"III","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":308610,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudson, Patrick L. 0000-0002-7646-443X phudson@usgs.gov","orcid":"https://orcid.org/0000-0002-7646-443X","contributorId":5616,"corporation":false,"usgs":true,"family":"Hudson","given":"Patrick","email":"phudson@usgs.gov","middleInitial":"L.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":308609,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70021970,"text":"70021970 - 1999 - Six-egg clutches of the Mountain Plover, Charadrius montanus","interactions":[],"lastModifiedDate":"2023-11-13T12:54:39.779271","indexId":"70021970","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1163,"text":"Canadian Field-Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Six-egg clutches of the Mountain Plover, Charadrius montanus","docAbstract":"Three six-egg clutches of the Mountain Plover (Charadrius montanus) represent the largest clutch size ever reported for this declining Great Plains shorebird. Clutch size in this species is normally three eggs, and six-egg clutches probably represent the laying of a second clutch in the nest by the same female.","language":"English","publisher":"Ottawa Field-Naturalists' Club","issn":"00083550","usgsCitation":"Dinsmore, S., and Knopf, F., 1999, Six-egg clutches of the Mountain Plover, Charadrius montanus: Canadian Field-Naturalist, v. 113, no. 3, p. 516-517.","productDescription":"2 p.","startPage":"516","endPage":"517","numberOfPages":"2","costCenters":[],"links":[{"id":229608,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":422526,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.biodiversitylibrary.org/part/358625"}],"volume":"113","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9107e4b08c986b319734","contributors":{"authors":[{"text":"Dinsmore, S.J.","contributorId":85114,"corporation":false,"usgs":true,"family":"Dinsmore","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":391900,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knopf, F.L.","contributorId":26998,"corporation":false,"usgs":true,"family":"Knopf","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":391899,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70022013,"text":"70022013 - 1999 - Recrystallization and anatexis along the plutonic-volcanic contact of the Turkey Creek caldera, Arizona","interactions":[],"lastModifiedDate":"2023-12-19T12:58:10.219537","indexId":"70022013","displayToPublicDate":"1999-01-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Recrystallization and anatexis along the plutonic-volcanic contact of the Turkey Creek caldera, Arizona","docAbstract":"<p>Unusual geologic and geochemical relations are preserved along the contact between intracaldera tuff and a resurgent intrusion within the 26.9 Ma Turkey Creek caldera of southeast Arizona. Thick intracaldera tuff is weakly argillically altered throughout, except in zones within several hundred meters of its contact with the resurgent intrusion, where the groundmass of the tuff has been variably converted to granophyre and unaltered sanidine phenocrysts are present. Dikes of similarly granophyric material originate at the tuff-resurgent intrusion contact and intrude overlying intracaldera megabreccia and tuff. Field relations indicate that the resurgent intrusion is a laccolith and that it caused local partial melting of adjacent intracaldera tuff. Geochemical and petrographic relations indicate that small volumes of partially melted intracaldera tuff assimilated and mixed with dacite of the resurgent intrusion along their contact, resulting in rocks that have petrographic and compositional characteristics transitional between those of tuff and dacite. Some of this variably contaminated, second-generation magma coalesced, was mobilized, and was intruded into overlying intracaldera rocks.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1999)111<0143:RAAATP>2.3.CO;2","issn":"00167606","usgsCitation":"Bray, D., and Pallister, J., 1999, Recrystallization and anatexis along the plutonic-volcanic contact of the Turkey Creek caldera, Arizona: Geological Society of America Bulletin, v. 111, no. 1, p. 143-153, https://doi.org/10.1130/0016-7606(1999)111<0143:RAAATP>2.3.CO;2.","productDescription":"11 p.","startPage":"143","endPage":"153","numberOfPages":"11","costCenters":[],"links":[{"id":230511,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Turkey Creek caldera","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -109.9244036605549,\n              32.5000106686156\n            ],\n            [\n              -109.9244036605549,\n              31.437545697056535\n            ],\n            [\n              -109.13338803555492,\n              31.437545697056535\n            ],\n            [\n              -109.13338803555492,\n              32.5000106686156\n            ],\n            [\n              -109.9244036605549,\n              32.5000106686156\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"111","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a359e4b0e8fec6cdb837","contributors":{"authors":[{"text":"Bray, du","contributorId":28749,"corporation":false,"usgs":true,"family":"Bray","given":"du","email":"","affiliations":[],"preferred":false,"id":392037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pallister, J.S.","contributorId":46534,"corporation":false,"usgs":true,"family":"Pallister","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":392038,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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