{"pageNumber":"3656","pageRowStart":"91375","pageSize":"25","recordCount":185279,"records":[{"id":70020009,"text":"70020009 - 1997 - Improved method for producing catalytic carbon and the potential for increasing its use in commercial applications","interactions":[],"lastModifiedDate":"2023-12-16T01:08:58.573664","indexId":"70020009","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1513,"text":"Energy and Fuels","active":true,"publicationSubtype":{"id":10}},"title":"Improved method for producing catalytic carbon and the potential for increasing its use in commercial applications","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Chemical Society","issn":"08870624","usgsCitation":"Kruse, C., Lizzio, A., DeBarr, J., and Feizoulof, C., 1997, Improved method for producing catalytic carbon and the potential for increasing its use in commercial applications: Energy and Fuels, v. 11, no. 2, p. 260-266.","productDescription":"7 p.","startPage":"260","endPage":"266","numberOfPages":"7","costCenters":[],"links":[{"id":227860,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a395ce4b0c8380cd618c6","contributors":{"authors":[{"text":"Kruse, C.W.","contributorId":52333,"corporation":false,"usgs":true,"family":"Kruse","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":384694,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lizzio, A.A.","contributorId":70937,"corporation":false,"usgs":true,"family":"Lizzio","given":"A.A.","email":"","affiliations":[],"preferred":false,"id":384695,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeBarr, J.A.","contributorId":20078,"corporation":false,"usgs":true,"family":"DeBarr","given":"J.A.","affiliations":[],"preferred":false,"id":384693,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Feizoulof, C.A.","contributorId":80437,"corporation":false,"usgs":true,"family":"Feizoulof","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":384696,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70019238,"text":"70019238 - 1997 - Resolution of fault slip along the 470-km-long rupture of the great 1906 San Francisco earthquake and its implications","interactions":[],"lastModifiedDate":"2024-09-30T13:25:39.833874","indexId":"70019238","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Resolution of fault slip along the 470-km-long rupture of the great 1906 San Francisco earthquake and its implications","docAbstract":"Data from all available triangulation networks affected by the 1906 earthquake have been combined to assess the trade-off between slip resolution and its uncertainty and to construct a conservative image of coseismic slip along the rupture. Because of varying network aperture and station density, slip resolution is very uneven. Although slip is determined within uncertainties of ??1.0 m along 60% of the fault, constraints are poor on the remaining, mostly offshore portions of the rupture. Slip decreases from maxima of 8.6 and 7.5 m at Shelter Cove and Tomales Bay to 4.5 m near Mount Tamalpais and 2.7 m at Loma Prieta. The geodetically derived slip distribution is in poor agreement with estimates based on analysis of S wave seismograms, probably because these waves register only 20-30% of the total seismic moment obtained from longer-period surface waves. Consideration of a range of fault geometries for 1906 slip near Loma Prieta indicates right-lateral motions lie between 2.3 and 3.1 m. These values are considerably greater than the 1.5 m of measured surface slip on which several assessments of high earthquake hazard for this fault segment were based. This factor, along with the absence of 1989 slippage where 1906 surface slip was used to make the forecasts, casts doubt on some claims of success in predicting the 1989 M = 6.9 Loma Prieta earthquake.","language":"English","publisher":"American Geophysical Union","doi":"10.1029/96JB03486","issn":"01480227","usgsCitation":"Thatcher, W., Marshall, G., and Lisowski, M., 1997, Resolution of fault slip along the 470-km-long rupture of the great 1906 San Francisco earthquake and its implications: Journal of Geophysical Research B: Solid Earth, v. 102, no. B3, p. 5353-5367, https://doi.org/10.1029/96JB03486.","productDescription":"15 p.","startPage":"5353","endPage":"5367","numberOfPages":"15","costCenters":[],"links":[{"id":479941,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/96jb03486","text":"Publisher Index Page"},{"id":226419,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"102","issue":"B3","noUsgsAuthors":false,"publicationDate":"1997-03-10","publicationStatus":"PW","scienceBaseUri":"505aa9d4e4b0c8380cd85fc9","contributors":{"authors":[{"text":"Thatcher, W.","contributorId":32669,"corporation":false,"usgs":true,"family":"Thatcher","given":"W.","email":"","affiliations":[],"preferred":false,"id":382107,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marshall, G.","contributorId":21292,"corporation":false,"usgs":true,"family":"Marshall","given":"G.","email":"","affiliations":[],"preferred":false,"id":382106,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lisowski, M.","contributorId":70381,"corporation":false,"usgs":true,"family":"Lisowski","given":"M.","email":"","affiliations":[],"preferred":false,"id":382108,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70019926,"text":"70019926 - 1997 - A self-modifying cellular automaton model of historical urbanization in the San Francisco Bay area","interactions":[],"lastModifiedDate":"2017-04-07T15:01:56","indexId":"70019926","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1526,"text":"Environment and Planning B: Planning and Design","active":true,"publicationSubtype":{"id":10}},"title":"A self-modifying cellular automaton model of historical urbanization in the San Francisco Bay area","docAbstract":"In this paper we describe a cellular automaton (CA) simulation model developed to predict urban growth as part of a project for estimating the regional and broader impact of urbanization on the San Francisco Bay area's climate. The rules of the model are more complex than those of a typical CA and involve the use of multiple data sources, including topography, road networks, and existing settlement distributions, and their modification over time. In addition, the control parameters of the model are allowed to self-modify: that is, the CA adapts itself to the circumstances it generates, in particular, during periods of rapid growth or stagnation. In addition, the model was written to allow the accumulation of probabilistic estimates based on Monte Carlo methods. Calibration of the model has been accomplished by the use of historical maps to compare model predictions of urbanization, based solely upon the distribution in year 1900, with observed data for years 1940, 1954, 1962, 1974, and 1990. The complexity of this model has made calibration a particularly demanding step. Lessons learned about the methods, measures, and strategies developed to calibrate the model may be of use in other environmental modeling contexts. With the calibration complete, the model is being used to generate a set of future scenarios for the San Francisco Bay area along with their probabilities based on the Monte Carlo version of the model. Animated dynamic mapping of the simulations will be used to allow visualization of the impact of future urban growth.","language":"English","publisher":"SAGE","doi":"10.1068/b240247","issn":"02658135","usgsCitation":"Clarke, K., Hoppen, S., and Gaydos, L., 1997, A self-modifying cellular automaton model of historical urbanization in the San Francisco Bay area: Environment and Planning B: Planning and Design, v. 24, no. 2, p. 247-261, https://doi.org/10.1068/b240247.","productDescription":"15 p.","startPage":"247","endPage":"261","numberOfPages":"15","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":227695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e584e4b0c8380cd46dad","contributors":{"authors":[{"text":"Clarke, K.C.","contributorId":55980,"corporation":false,"usgs":true,"family":"Clarke","given":"K.C.","affiliations":[],"preferred":false,"id":384403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoppen, S.","contributorId":8239,"corporation":false,"usgs":true,"family":"Hoppen","given":"S.","affiliations":[],"preferred":false,"id":384402,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gaydos, L.","contributorId":101015,"corporation":false,"usgs":true,"family":"Gaydos","given":"L.","email":"","affiliations":[],"preferred":false,"id":384404,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70019966,"text":"70019966 - 1997 - Variability in perceived satisfaction of reservoir management objectives","interactions":[],"lastModifiedDate":"2024-05-23T14:34:00.871768","indexId":"70019966","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2501,"text":"Journal of Water Resources Planning and Management","active":true,"publicationSubtype":{"id":10}},"title":"Variability in perceived satisfaction of reservoir management objectives","docAbstract":"<p><span>Fuzzy set theory provides a useful model to address imprecision in interpreting linguistically described objectives for reservoir management. Fuzzy membership functions can be used to represent degrees of objective satisfaction for different values of management variables. However, lack of background information, differing experiences and qualifications, and complex interactions of influencing factors can contribute to significant variability among membership functions derived from surveys of multiple experts. In the present study, probabilistic membership functions are used to model variability in experts' perceptions of satisfaction of objectives for hydropower generation, fish habitat, kayaking, rafting, and scenery preservation on the Green River through operations of Flaming Gorge Dam. Degree of variability in experts' perceptions differed among objectives but resulted in substantial uncertainty in estimation of optimal reservoir releases.</span></p>","language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0733-9496(1997)123:3(147)","issn":"07339496","usgsCitation":"Owen, W., Gates, T., and Flug, M., 1997, Variability in perceived satisfaction of reservoir management objectives: Journal of Water Resources Planning and Management, v. 123, no. 3, p. 147-153, https://doi.org/10.1061/(ASCE)0733-9496(1997)123:3(147).","productDescription":"7 p.","startPage":"147","endPage":"153","numberOfPages":"7","costCenters":[],"links":[{"id":227778,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"123","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc12de4b08c986b32a488","contributors":{"authors":[{"text":"Owen, W.J.","contributorId":11349,"corporation":false,"usgs":true,"family":"Owen","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":384521,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gates, T.K.","contributorId":33074,"corporation":false,"usgs":true,"family":"Gates","given":"T.K.","email":"","affiliations":[],"preferred":false,"id":384522,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flug, M.","contributorId":57419,"corporation":false,"usgs":true,"family":"Flug","given":"M.","affiliations":[],"preferred":false,"id":384523,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70020179,"text":"70020179 - 1997 - Evaluation of field and laboratory research on scour at bridge piers in the United States","interactions":[],"lastModifiedDate":"2012-03-12T17:20:15","indexId":"70020179","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Evaluation of field and laboratory research on scour at bridge piers in the United States","docAbstract":"The Federal Highway Administration sponsored a laboratory research at Colorado State University and field data collection with the US Geological Survey, to evaluate the effects of bed material on the depth of scour. Correction factors are compared to include the effect of bed material in the HEC-18 equation. The HEC-18 equation tends to overpredict the observed scour for streams with coarse bed material. The field-based correction factor K4 causes underprediction associated with data collected from other countries.","largerWorkTitle":"Proceedings, Congress of the International Association of Hydraulic Research, IAHR","conferenceTitle":"Proceedings of the 1997 27th Congress of the International Association of Hydraulic Research, IAHR. Part C","conferenceDate":"10 August 1997 through 15 August 1997","conferenceLocation":"San Francisco, CA, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, United States","usgsCitation":"Mueller, D.S., and Jones, J.S., 1997, Evaluation of field and laboratory research on scour at bridge piers in the United States, <i>in</i> Proceedings, Congress of the International Association of Hydraulic Research, IAHR, v. A, San Francisco, CA, USA, 10 August 1997 through 15 August 1997, p. 135-140.","startPage":"135","endPage":"140","numberOfPages":"6","costCenters":[],"links":[{"id":231162,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"A","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0c73e4b0c8380cd52b5a","contributors":{"authors":[{"text":"Mueller, David S. dmueller@usgs.gov","contributorId":1499,"corporation":false,"usgs":true,"family":"Mueller","given":"David","email":"dmueller@usgs.gov","middleInitial":"S.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":385286,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, J. Sterling","contributorId":92814,"corporation":false,"usgs":true,"family":"Jones","given":"J.","email":"","middleInitial":"Sterling","affiliations":[],"preferred":false,"id":385287,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70019665,"text":"70019665 - 1997 - Active faults of the Baikal depression","interactions":[],"lastModifiedDate":"2012-03-12T17:19:19","indexId":"70019665","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1097,"text":"Bulletin des Centres de Recherches Elf Exploration Production","active":true,"publicationSubtype":{"id":10}},"title":"Active faults of the Baikal depression","docAbstract":"The Baikal depression occupies a central position in the system of the basins of the Baikal Rift Zone and corresponds to the nucleus from which the continental lithosphere began to open. For different reasons, the internal structure of the Lake Baikal basin remained unknown for a long time. In this article, we present for the first time a synthesis of the data concerning the structure of the sedimentary section beneath Lake Baikal, which were obtained by complex seismic and structural investigations, conducted mainly from 1989 to 1992. We make a brief description of the most interesting seismic profiles which provide a rough idea of a sedimentary unit structure, present a detailed structural interpretation and show the relationship between active faults in the lake, heat flow anomalies and recent hydrothermalism.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin des Centres de Recherches Elf Exploration Production","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03962687","usgsCitation":"Levi, K., Miroshnichenko, A., San’kov, V.A., Babushkin, S., Larkin, G., Badardinov, A., Wong, H., Colman, S., and Delvaux, D., 1997, Active faults of the Baikal depression: Bulletin des Centres de Recherches Elf Exploration Production, v. 21, no. 2, p. 399-434.","startPage":"399","endPage":"434","numberOfPages":"36","costCenters":[],"links":[{"id":228089,"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":"5059e6abe4b0c8380cd4758e","contributors":{"authors":[{"text":"Levi, K.G.","contributorId":86506,"corporation":false,"usgs":true,"family":"Levi","given":"K.G.","email":"","affiliations":[],"preferred":false,"id":383495,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miroshnichenko, A.I.","contributorId":45849,"corporation":false,"usgs":true,"family":"Miroshnichenko","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":383491,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"San’kov, V. A.","contributorId":54752,"corporation":false,"usgs":true,"family":"San’kov","given":"V.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":383492,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Babushkin, S.M.","contributorId":90054,"corporation":false,"usgs":true,"family":"Babushkin","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":383496,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Larkin, G.V.","contributorId":37487,"corporation":false,"usgs":true,"family":"Larkin","given":"G.V.","email":"","affiliations":[],"preferred":false,"id":383489,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Badardinov, A.A.","contributorId":41165,"corporation":false,"usgs":true,"family":"Badardinov","given":"A.A.","affiliations":[],"preferred":false,"id":383490,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wong, H.K.","contributorId":102652,"corporation":false,"usgs":true,"family":"Wong","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":383497,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Colman, S.","contributorId":63553,"corporation":false,"usgs":true,"family":"Colman","given":"S.","affiliations":[],"preferred":false,"id":383493,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Delvaux, D.","contributorId":76082,"corporation":false,"usgs":true,"family":"Delvaux","given":"D.","email":"","affiliations":[],"preferred":false,"id":383494,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70019223,"text":"70019223 - 1997 - Modeling saltwater upconing in a freshwater aquifer in south-central Kansas","interactions":[],"lastModifiedDate":"2012-03-12T17:19:16","indexId":"70019223","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Modeling saltwater upconing in a freshwater aquifer in south-central Kansas","docAbstract":"The Great Bend Prairie freshwater alluvial aquifer in south-central Kansas overlies a bedrock brine aquifer of Permian age. The continuous extraction of freshwater mainly for irrigation in this area has accelerated the upward movement of the saltwater, resulting in the deterioration of water quality. Predicting saltwater upconing is critical for maintaining a long-term supply of water of good quality to the Groundwater Management District No. 5. This paper uses a numerical model to predict the effect of saltwater upconing on the salinity of pumped water. A sensitivity analysis was conducted for estimating the effects of uncertainties in model parameters on the numerical results. The most important factors affecting the salinity of discharged water are found to be the location and nature of clay layers in the aquifer, the pumping rate, the location of the well screen, and the hydraulic conductivities of the medium. The effect of uncertainties in aquifer porosity and dispersivity on salinity is appreciable but not substantial, whereas that of recharge from precipitation in the study area is relatively insignificant. In addition, a numerical model based on the field conditions observed at the Siefkes site was constructed and calibrated to reproduce and project the variation of measured water levels and discharged groundwater concentration. Finally, a number of practical management recommendations based on this study are presented.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier Sci B.V.","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/S0022-1694(97)00048-6","issn":"00221694","usgsCitation":"Ma, T., Sophocleous, M., Yu, Y., and Buddemeier, R., 1997, Modeling saltwater upconing in a freshwater aquifer in south-central Kansas: Journal of Hydrology, v. 201, no. 1-4, p. 120-137, https://doi.org/10.1016/S0022-1694(97)00048-6.","startPage":"120","endPage":"137","numberOfPages":"18","costCenters":[],"links":[{"id":205808,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0022-1694(97)00048-6"},{"id":226913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"201","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5c25e4b0c8380cd6fa8c","contributors":{"authors":[{"text":"Ma, T.-S.","contributorId":67232,"corporation":false,"usgs":true,"family":"Ma","given":"T.-S.","email":"","affiliations":[],"preferred":false,"id":382047,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sophocleous, M.","contributorId":13373,"corporation":false,"usgs":true,"family":"Sophocleous","given":"M.","email":"","affiliations":[],"preferred":false,"id":382046,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yu, Y.-S.","contributorId":98892,"corporation":false,"usgs":true,"family":"Yu","given":"Y.-S.","email":"","affiliations":[],"preferred":false,"id":382049,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Buddemeier, R. W.","contributorId":86492,"corporation":false,"usgs":true,"family":"Buddemeier","given":"R. W.","affiliations":[],"preferred":false,"id":382048,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70019142,"text":"70019142 - 1997 - Occurrence of MTBE and tert-butyl alcohol in a gasoline-contaminated aquifer","interactions":[],"lastModifiedDate":"2012-03-12T17:19:16","indexId":"70019142","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":610,"text":"ACS Division of Environmental Chemistry, Preprints","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence of MTBE and tert-butyl alcohol in a gasoline-contaminated aquifer","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"ACS Division of Environmental Chemistry, Preprints","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00933066","usgsCitation":"Landmeyer, J., Pankow, J.F., and Church, C., 1997, Occurrence of MTBE and tert-butyl alcohol in a gasoline-contaminated aquifer: ACS Division of Environmental Chemistry, Preprints, v. 37, no. 1, p. 413-415.","startPage":"413","endPage":"415","numberOfPages":"3","costCenters":[],"links":[{"id":226408,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6b9fe4b0c8380cd747d9","contributors":{"authors":[{"text":"Landmeyer, J. E.","contributorId":91140,"corporation":false,"usgs":true,"family":"Landmeyer","given":"J. E.","affiliations":[],"preferred":false,"id":381793,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pankow, J. F.","contributorId":20917,"corporation":false,"usgs":true,"family":"Pankow","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":381791,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Church, C.D.","contributorId":55583,"corporation":false,"usgs":true,"family":"Church","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":381792,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70019349,"text":"70019349 - 1997 - Distribution of MTBE in ground water in New England by aquifer type and land use","interactions":[],"lastModifiedDate":"2012-03-12T17:19:11","indexId":"70019349","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":610,"text":"ACS Division of Environmental Chemistry, Preprints","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of MTBE in ground water in New England by aquifer type and land use","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"ACS Division of Environmental Chemistry, Preprints","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00933066","usgsCitation":"Grady, S.J., 1997, Distribution of MTBE in ground water in New England by aquifer type and land use: ACS Division of Environmental Chemistry, Preprints, v. 37, no. 1, p. 392-394.","startPage":"392","endPage":"394","numberOfPages":"3","costCenters":[],"links":[{"id":226832,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a02b4e4b0c8380cd50183","contributors":{"authors":[{"text":"Grady, S. J.","contributorId":69962,"corporation":false,"usgs":true,"family":"Grady","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":382425,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70019850,"text":"70019850 - 1997 - A growth form method for describing browse condition","interactions":[],"lastModifiedDate":"2012-03-12T17:19:17","indexId":"70019850","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3230,"text":"Rangelands","active":true,"publicationSubtype":{"id":10}},"title":"A growth form method for describing browse condition","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Rangelands","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"01900528","usgsCitation":"Keigley, R., 1997, A growth form method for describing browse condition: Rangelands, v. 19, no. 3, p. 26-29.","startPage":"26","endPage":"29","numberOfPages":"4","costCenters":[],"links":[{"id":227893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e40fe4b0c8380cd463b4","contributors":{"authors":[{"text":"Keigley, R.B.","contributorId":85115,"corporation":false,"usgs":true,"family":"Keigley","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":384160,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70019346,"text":"70019346 - 1997 - Comment on \"The 1946 Hispaniola earthquake and the tectonics of the North America-Caribbean plate boundary zone, northeastern Hispaniola\"","interactions":[],"lastModifiedDate":"2024-09-30T14:21:44.212717","indexId":"70019346","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Comment on \"The 1946 Hispaniola earthquake and the tectonics of the North America-Caribbean plate boundary zone, northeastern Hispaniola\"","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/96JB00648","issn":"01480227","usgsCitation":"Dolan, J., and Wald, D., 1997, Comment on \"The 1946 Hispaniola earthquake and the tectonics of the North America-Caribbean plate boundary zone, northeastern Hispaniola\": Journal of Geophysical Research B: Solid Earth, v. 102, no. B1, p. 785-792, https://doi.org/10.1029/96JB00648.","productDescription":"8 p.","startPage":"785","endPage":"792","numberOfPages":"8","costCenters":[],"links":[{"id":226829,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"102","issue":"B1","noUsgsAuthors":false,"publicationDate":"1997-01-10","publicationStatus":"PW","scienceBaseUri":"5059f7e8e4b0c8380cd4cd8b","contributors":{"authors":[{"text":"Dolan, J.F.","contributorId":64813,"corporation":false,"usgs":true,"family":"Dolan","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":382420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wald, D.J. 0000-0002-1454-4514","orcid":"https://orcid.org/0000-0002-1454-4514","contributorId":43809,"corporation":false,"usgs":true,"family":"Wald","given":"D.J.","affiliations":[],"preferred":false,"id":382417,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70019454,"text":"70019454 - 1997 - Applications of the 190Pt-186Os isotope system to geochemistry and cosmochemistry","interactions":[],"lastModifiedDate":"2023-12-15T00:18:30.721831","indexId":"70019454","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Applications of the <sup>190</sup>Pt-<sup>186</sup>Os isotope system to geochemistry and cosmochemistry","title":"Applications of the 190Pt-186Os isotope system to geochemistry and cosmochemistry","docAbstract":"<p><span>Platinum is fractionated from osmium primarily as a consequence of processes involving sulfide and metal crystallization. Consequently, the&nbsp;</span><sup>190</sup><span>Pt</span><sup>186</sup><span>Os isotope system (</span><sup>190</sup><span>Pt →&nbsp;</span><sup>186</sup><span>Os + α) shows promise for dating some types of magmatic sulfide ores and evolved iron meteorites. The first&nbsp;</span><sup>190</sup><span>Pt&nbsp;</span><sup>186</sup><span>Os isochrons are presented here for ores from the ca. 251 Ma Noril'sk, Siberia plume, and for group IIAB magmatic iron meteorites. Given the known age of the Noril'sk system, a decay constant for&nbsp;</span><sup>190</sup><span>Pt is determined to be 1.542 × 10</span><sup>−12</sup><span>a</span><sup>−1</sup><span>, with ±1% uncertainty. The isochron generated for the IIAB irons is consistent with this decay constant and the known age of the group. The&nbsp;</span><sup>186</sup><span>Os/</span><sup>188</sup><span>Os ratios of presumably young, mantle-derived osmiridiums and also the carbonaceous chondrite Allende were measured to high-precision to constrain the composition of the modern upper mantle. These compositions overlap, indicating that the upper mantle is chondritic within the level of resolution now available. Our best estimate for this&nbsp;</span><sup>186</sup><span>Os/</span><sup>188</sup><span>Os ratio is 0.119834 ± 2 (2σ</span><sub><i>M</i></sub><span>). The&nbsp;</span><sup>190</sup><span>Pt/</span><sup>186</sup><span>Os ratios determined for six enstatite chondrites average 0.001659 ± 75, which is very similar to published values for carbonaceous chondrites. Using this ratio and the presumed composition of the modern upper mantle and chondrites, a solar system initial&nbsp;</span><sup>186</sup><span>Os/</span><sup>188</sup><span>Os ratio of 0.119820 is calculated. In comparison to the modern upper mantle composition, the&nbsp;</span><sup>186</sup><span>Os/</span><sup>188</sup><span>Os ratio of the Noril'sk plume was approximately 0.012% enriched in&nbsp;</span><sup>186</sup><span>Os. Possible reasons for this heterogeneity include the recycling of Pt-rich crust into the mantle source of the plume and derivation of the osmium from the outer core. Derivation of the osmium from the outer core is our favored model.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0016-7037(97)00270-6","issn":"00167037","usgsCitation":"Walker, R., Morgan, J.W., Beary, E., Smoliar, M., Czamanske, G., and Horan, M., 1997, Applications of the 190Pt-186Os isotope system to geochemistry and cosmochemistry: Geochimica et Cosmochimica Acta, v. 61, no. 22, p. 4799-4807, https://doi.org/10.1016/S0016-7037(97)00270-6.","productDescription":"9 p.","startPage":"4799","endPage":"4807","costCenters":[],"links":[{"id":226791,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"61","issue":"22","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eccae4b0c8380cd494ba","contributors":{"authors":[{"text":"Walker, R.J.","contributorId":105859,"corporation":false,"usgs":true,"family":"Walker","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":382791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, J. W.","contributorId":92384,"corporation":false,"usgs":true,"family":"Morgan","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":382789,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beary, E.S.","contributorId":29967,"corporation":false,"usgs":true,"family":"Beary","given":"E.S.","affiliations":[],"preferred":false,"id":382787,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smoliar, M.I.","contributorId":96843,"corporation":false,"usgs":true,"family":"Smoliar","given":"M.I.","email":"","affiliations":[],"preferred":false,"id":382790,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Czamanske, G.K.","contributorId":26300,"corporation":false,"usgs":true,"family":"Czamanske","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":382786,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Horan, M.F.","contributorId":75282,"corporation":false,"usgs":true,"family":"Horan","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":382788,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70020045,"text":"70020045 - 1997 - Comparison of phytoplankton succession in two lakes of different mixing regimes","interactions":[],"lastModifiedDate":"2012-03-12T17:19:19","indexId":"70020045","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":883,"text":"Archiv fur Hydrobiologie","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of phytoplankton succession in two lakes of different mixing regimes","docAbstract":"The influence of frequent water-column mixing on phytoplankton succession and species composition was studied by comparing plankton dynamics in two lakes (Lake Opinicon and Upper Rock Lake) which have similar water chemistry, but differ widely in their basin morphometries: Opinicon is shallow and frequently-mixed during the ice-free season, whereas nearby Upper Rock is deep and dimictic. The species composition and the seasonal succession of phytoplankton were broadly similar in both lakes over the three years of study. The spring phytoplankton in both lakes consisted of diatoms that were replaced in the summer and fall by cyanobacteria. Diatom peaks in Opinicon preceded similar peaks in Upper Rock. Loss of diatoms from the phytoplankton in Upper Rock appeared to be related to sedimentation; in contrast, zooplankton herbivory may have resulted, partly, in loss of diatoms in Opinicon. Lightly-silicified and spindle-shaped diatoms (Rhizosolenia and single-celled Fragilaria) were more abundant in the dimictic lake, whereas heavily-silicified diatoms (Aulacoseira) were more abundant in the frequently-mixed lake. Zooplankton taxa and their seasonal patterns were similar in both lakes, but populations were considerably denser in the frequently-mixed lake. The results of canonical correspondence analysis and detrended correspondence analysis (multivariate ordination techniques) indicated that, although phytoplankton growth was influenced by similar physical and chemical variables in both lakes, the influence of chemical variables was stronger in Upper Rock. A frequently-mixed system, such as Lake Opinicon, appeared to provide a similar environment for plankton development to a well-mixed epilimnion of a typical dimictic lake, such as Upper Rock Lake.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Archiv fur Hydrobiologie","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00039136","usgsCitation":"Agbeti, M., Kingston, J., Smol, J.P., and Watters, C., 1997, Comparison of phytoplankton succession in two lakes of different mixing regimes: Archiv fur Hydrobiologie, v. 140, no. 1, p. 37-69.","startPage":"37","endPage":"69","numberOfPages":"33","costCenters":[],"links":[{"id":227782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"140","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f881e4b0c8380cd4d152","contributors":{"authors":[{"text":"Agbeti, M.D.","contributorId":47104,"corporation":false,"usgs":true,"family":"Agbeti","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":384816,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kingston, J.C.","contributorId":80276,"corporation":false,"usgs":true,"family":"Kingston","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":384817,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smol, J. P.","contributorId":21298,"corporation":false,"usgs":false,"family":"Smol","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":384814,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Watters, C.","contributorId":32313,"corporation":false,"usgs":true,"family":"Watters","given":"C.","email":"","affiliations":[],"preferred":false,"id":384815,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70020056,"text":"70020056 - 1997 - The effect of drought on Engelmann prickly pear (cactaceae: Opuntia engelmannii) fruit and seed production","interactions":[],"lastModifiedDate":"2012-03-12T17:19:19","indexId":"70020056","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3451,"text":"Southwestern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"The effect of drought on Engelmann prickly pear (cactaceae: Opuntia engelmannii) fruit and seed production","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Southwestern Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00384909","usgsCitation":"Bowers, J.E., 1997, The effect of drought on Engelmann prickly pear (cactaceae: Opuntia engelmannii) fruit and seed production: Southwestern Naturalist, v. 42, no. 2, p. 240-242.","startPage":"240","endPage":"242","numberOfPages":"3","costCenters":[],"links":[{"id":227952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bab23e4b08c986b322c52","contributors":{"authors":[{"text":"Bowers, Janice E.","contributorId":18119,"corporation":false,"usgs":true,"family":"Bowers","given":"Janice","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":384848,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70019859,"text":"70019859 - 1997 - Sedimentary phosphorus cycling and a phosphorus mass balance for the Green Bay (Lake Michigan) ecosystem","interactions":[],"lastModifiedDate":"2018-02-06T12:21:35","indexId":"70019859","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Sedimentary phosphorus cycling and a phosphorus mass balance for the Green Bay (Lake Michigan) ecosystem","docAbstract":"The tributaries of Green Bay have long been recognized as major sources of phosphorus in the Lake Michigan basin. The status of Green Bay as a sink or source of phosphorus for Lake Michigan proper has been less well defined. The bay receives nearly 70% of its annual load of phosphorus (700 metric tons (t)??year-1) from a single source: the Fox River. Most of this phosphorus is deposited in sediments accumulating at rates that reach 160 mg??cm-2??year-1 with an average of 20 mg??cm-2 year-1. The phosphorus content of these sediments varies from <5 to >70 ??mol??g-1. Deposition is highly focused, with ???0% of the total sediment accumulation and at least 80% of the phosphorus burial occurring within 20% of the surface area of the bay. Diagenetic and stoichiometric models of phosphorus cycling imply that >80% of the phosphorus deposited is permanently buried. External phosphorus loading to the bay is combined with sediment fluxes of phophorus to arrive at a simple phosphorus budget. Green Bay acts as an efficient nutrient trap, with the sediments retaining an estimated 70-90% of the external phosphorus inputs before flowing into Lake Michigan.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Fisheries and Aquatic Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1139/cjfas-54-1-10","issn":"0706652X","usgsCitation":"Val, K.J., Edgington, D., Sager, P., and Robertson, D.M., 1997, Sedimentary phosphorus cycling and a phosphorus mass balance for the Green Bay (Lake Michigan) ecosystem: Canadian Journal of Fisheries and Aquatic Sciences, v. 54, no. 1, p. 10-26, https://doi.org/10.1139/cjfas-54-1-10.","startPage":"10","endPage":"26","numberOfPages":"17","costCenters":[],"links":[{"id":228023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":206040,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1139/cjfas-54-1-10"}],"volume":"54","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8a2ee4b08c986b317095","contributors":{"authors":[{"text":"Val, Klump J.","contributorId":41164,"corporation":false,"usgs":true,"family":"Val","given":"Klump","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":384186,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edgington, D.N.","contributorId":14587,"corporation":false,"usgs":true,"family":"Edgington","given":"D.N.","email":"","affiliations":[],"preferred":false,"id":384184,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sager, P.E.","contributorId":61974,"corporation":false,"usgs":true,"family":"Sager","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":384187,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robertson, Dale M. 0000-0001-6799-0596 dzrobert@usgs.gov","orcid":"https://orcid.org/0000-0001-6799-0596","contributorId":150760,"corporation":false,"usgs":true,"family":"Robertson","given":"Dale","email":"dzrobert@usgs.gov","middleInitial":"M.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":384185,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70019742,"text":"70019742 - 1997 - Microorganisms as tracers in groundwater injection and recovery experiments: A review","interactions":[],"lastModifiedDate":"2019-02-13T16:26:42","indexId":"70019742","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1621,"text":"FEMS Microbiology Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Microorganisms as tracers in groundwater injection and recovery experiments: A review","docAbstract":"Modern day injection and recovery techniques designed to examine the transport behavior of microorganisms in groundwater have evolved from experiments conducted in the late 1800s, in which bacteria that form red or yellow pigments were used to trace flow paths through karst and fractured- rock aquifers. A number of subsequent groundwater hydrology studies employed bacteriophage that can be injected into aquifers at very high concentrations (e g., 1013 phage ml-1) and monitored through many log units of dilution to follow groundwater flow paths for great distances, particularly in karst terrain. Starting in the 1930s, microbial indicators of fecal contamination (particularly coliform bacteria and their coliphages) were employed as tracers to determine potential migration of pathogens in groundwater. Several injection and recovery experiments performed in the 1990s employed indigenous groundwater microorganisms (both cultured and uncultured) that are better able to survive under in situ conditions. Better methods for labeling native bacteria (e.g by stable isotope labeling or inserting genetic markers; such as the ability to cause ice nucleation) are being developed that will not compromise the organisms' viability during the experimental time course.","language":"English","publisher":"Oxford","doi":"10.1016/S0168-6445(97)00026-0","issn":"01686445","usgsCitation":"Harvey, R., 1997, Microorganisms as tracers in groundwater injection and recovery experiments: A review: FEMS Microbiology Reviews, v. 20, no. 3-4, p. 461-472, https://doi.org/10.1016/S0168-6445(97)00026-0.","productDescription":"12 p.","startPage":"461","endPage":"472","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":479976,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/s0168-6445(97)00026-0","text":"Publisher Index Page"},{"id":228056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":206046,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0168-6445(97)00026-0"}],"volume":"20","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a568be4b0c8380cd6d67a","contributors":{"authors":[{"text":"Harvey, R.W. 0000-0002-2791-8503","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":11757,"corporation":false,"usgs":true,"family":"Harvey","given":"R.W.","affiliations":[],"preferred":false,"id":383762,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70019768,"text":"70019768 - 1997 - Experimental design for estimating parameters of rate-limited mass transfer: Analysis of stream tracer studies","interactions":[],"lastModifiedDate":"2019-02-04T10:46:05","indexId":"70019768","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","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":"Experimental design for estimating parameters of rate-limited mass transfer: Analysis of stream tracer studies","docAbstract":"<p><span>Tracer experiments are valuable tools for analyzing the transport characteristics of streams and their interactions with shallow groundwater. The focus of this work is the design of tracer studies in high-gradient stream systems subject to advection, dispersion, groundwater inflow, and exchange between the active channel and zones in surface or subsurface water where flow is stagnant or slow moving. We present a methodology for (1) evaluating and comparing alternative stream tracer experiment designs and (2) identifying those combinations of stream transport properties that pose limitations to parameter estimation and therefore a challenge to tracer test design. The methodology uses the concept of global parameter uncertainty analysis, which couples solute transport simulation with parameter uncertainty analysis in a Monte Carlo framework. Two general conclusions resulted from this work. First, the solute injection and sampling strategy has an important effect on the reliability of transport parameter estimates. We found that constant injection with sampling through concentration rise, plateau, and fall provided considerably more reliable parameter estimates than a pulse injection across the spectrum of transport scenarios likely encountered in high-gradient streams. Second, for a given tracer test design, the uncertainties in mass transfer and storage-zone parameter estimates are strongly dependent on the experimental Damkohler number,&nbsp;</span><i>DaI</i><span>, which is a dimensionless combination of the rates of exchange between the stream and storage zones, the stream-water velocity, and the stream reach length of the experiment. Parameter uncertainties are lowest at<span>&nbsp;</span></span><i>DaI</i><span><span>&nbsp;</span>values on the order of 1.0. When<span>&nbsp;</span></span><i>DaI</i><span><span>&nbsp;</span>values are much less than 1.0 (owing to high velocity, long exchange timescale, and/or short reach length), parameter uncertainties are high because only a small amount of tracer interacts with storage zones in the reach. For the opposite conditions (</span><i>DaI</i><span><span>&nbsp;</span>≫ 1.0), solute exchange rates are fast relative to stream-water velocity and all solute is exchanged with the storage zone over the experimental reach. As<span>&nbsp;</span></span><i>DaI</i><span><span>&nbsp;</span>increases, tracer dispersion caused by hyporheic exchange eventually reaches an equilibrium condition and storage-zone exchange parameters become essentially nonidentifiable.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/97WR01067","usgsCitation":"Wagner, B.J., and Harvey, J.W., 1997, Experimental design for estimating parameters of rate-limited mass transfer: Analysis of stream tracer studies: Water Resources Research, v. 33, no. 7, p. 1731-1741, https://doi.org/10.1029/97WR01067.","productDescription":"11 p.","startPage":"1731","endPage":"1741","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":479977,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/97wr01067","text":"Publisher Index Page"},{"id":227845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0dc5e4b0c8380cd531ad","contributors":{"authors":[{"text":"Wagner, Brian J. bjwagner@usgs.gov","contributorId":427,"corporation":false,"usgs":true,"family":"Wagner","given":"Brian","email":"bjwagner@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":383847,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harvey, Judson W. 0000-0002-2654-9873 jwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2654-9873","contributorId":1796,"corporation":false,"usgs":true,"family":"Harvey","given":"Judson","email":"jwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":383848,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70019770,"text":"70019770 - 1997 - Wind assistance: A requirement for migration of shorebirds?","interactions":[],"lastModifiedDate":"2017-03-16T12:39:51","indexId":"70019770","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Wind assistance: A requirement for migration of shorebirds?","docAbstract":"<p>We investigated the importance of wind-assisted flight for northward (spring) migration by Western Sandpipers (<i>Calidris mauri</i>) along the Pacific Coast of North America. Using current models of energy costs of flight and recent data on the phenology of migration, we estimated the energy (fat) requirements for migration in calm winds and with wind-assisted flight for different rates of fat deposition: (1) a variable rate, assuming that birds deposit the minimum amount of fat required to reach the next stopover site; (2) a constant maximum rate of 1.0 g/day; and (3) a lower constant rate of 0.4 g/day. We tested these models by comparing conservative estimates of predicted body mass along the migration route with empirical data on body mass of Western Sandpipers at different stopover sites and upon arrival at the breeding grounds. In calm conditions, birds would have to deposit unrealistically high amounts of fat (up to 330% of observed values) to maintain body mass above absolute lean mass values. Fat-deposition rates of 1.0 g/day and 0.4 g/day, in calm conditions, resulted in a steady decline in body mass along the migration route, with predicted body masses on arrival in Alaska of only 60% (13.6 g) and 26% (5.9 g) of average lean mass (22.7 g). Conversely, birds migrating with wind assistance would be able to complete migration with fat-deposition rates as low as 0.4 g/day, similar to values reported for this size bird from field studies. Our results extend the conclusion of the importance of winds for large, long-distance migrants to a small, short-distance migrant. We suggest that the migratory decisions of birds are more strongly influenced by the frequency and duration of winds aloft, i.e. by events during the flight phase, than by events during the stopover phase of migration, such as fat-deposition rate, that have been the focus of much recent migration theory.</p>","language":"English","publisher":"American Ornithological Society","doi":"10.2307/4089246","issn":"00048038","usgsCitation":"Butler, R.W., Williams, T., Warnock, N., and Bishop, M.A., 1997, Wind assistance: A requirement for migration of shorebirds?: The Auk, v. 114, no. 3, p. 456-466, https://doi.org/10.2307/4089246.","productDescription":"11 p.","startPage":"456","endPage":"466","costCenters":[],"links":[{"id":480032,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/4089246","text":"Publisher Index Page"},{"id":227886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"114","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd11ee4b08c986b32f23e","contributors":{"authors":[{"text":"Butler, Robert W.","contributorId":67444,"corporation":false,"usgs":false,"family":"Butler","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":383853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Tony D.","contributorId":89813,"corporation":false,"usgs":true,"family":"Williams","given":"Tony D.","affiliations":[],"preferred":false,"id":383852,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Warnock, Nils","contributorId":64534,"corporation":false,"usgs":false,"family":"Warnock","given":"Nils","email":"","affiliations":[],"preferred":false,"id":383854,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bishop, Mary Anne","contributorId":10698,"corporation":false,"usgs":true,"family":"Bishop","given":"Mary","email":"","middleInitial":"Anne","affiliations":[],"preferred":false,"id":383855,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70019544,"text":"70019544 - 1997 - Introduction to ecology and management of potamodromous salmonids","interactions":[],"lastModifiedDate":"2017-11-16T19:47:44","indexId":"70019544","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Introduction to ecology and management of potamodromous salmonids","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8675-17.4.1027","usgsCitation":"Gresswell, R., 1997, Introduction to ecology and management of potamodromous salmonids: North American Journal of Fisheries Management, v. 17, no. 4, p. 1027-1028, https://doi.org/10.1577/1548-8675-17.4.1027.","productDescription":"2 p.","startPage":"1027","endPage":"1028","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":228160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"4","noUsgsAuthors":false,"publicationDate":"1997-11-01","publicationStatus":"PW","scienceBaseUri":"505a3debe4b0c8380cd6394a","contributors":{"authors":[{"text":"Gresswell, R. E.","contributorId":38084,"corporation":false,"usgs":true,"family":"Gresswell","given":"R. E.","affiliations":[],"preferred":false,"id":383119,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014842,"text":"1014842 - 1997 - Mercury concentrations in Maine sport fishes","interactions":[],"lastModifiedDate":"2026-03-25T15:41:35.497192","indexId":"1014842","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Mercury concentrations in Maine sport fishes","docAbstract":"<p><span>To assess mercury contamination of fish in Maine, fish were collected from 120 randomly selected lakes. The collection goal for each lake was five fish of the single most common sport fish species within the size range commonly harvested by anglers. Skinless, boneless fillets of fish from each lake were composited, homogenized, and analyzed for total mercury. The two most abundant species, brook trout&nbsp;</span><i>Salvelinus fontinalis</i><span>&nbsp;and smallmouth bass&nbsp;</span><i>Micropterus dolomieu</i><span>, were also analyzed individually. The composite fish analyses indicate high concentrations of mercury, particularly in large and long‐lived nonsalmonid species. Chain pickerel&nbsp;</span><i>Esox niger</i><span>, smallmouth bass, largemouth bass&nbsp;</span><i>Micropterus salmoides</i><span>, and white perch&nbsp;</span><i>Morone americana</i><span>&nbsp;had the highest average mercury concentrations, and brook trout and yellow perch&nbsp;</span><i>Perca flavescens</i><span>&nbsp;had the lowest. The mean species composite mercury concentration was positively correlated with a factor incorporating the average size and age of the fish. Lakes containing fish with high mercury concentrations were not clustered near known industrial or population centers but were commonest in the area within 150 km of the seacoast, reflecting the geographical distribution of species that contained higher mercury concentrations. Stocked and wild brook trout were not different in length or weight, but wild fish were older and had higher mercury concentrations. Fish populations maintained by frequent introductions of hatchery‐produced fish and subject to high angler exploitation rates may consist of younger fish with lower exposure to environmental mercury and thus contain lower concentrations than wild populations.</span></p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1997)126<0144:MCIMSF>2.3.CO;2","usgsCitation":"Stafford, C., and Haines, T., 1997, Mercury concentrations in Maine sport fishes: Transactions of the American Fisheries Society, v. 126, no. 1, p. 144-152, https://doi.org/10.1577/1548-8659(1997)126<0144:MCIMSF>2.3.CO;2.","productDescription":"9 p.","startPage":"144","endPage":"152","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131577,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70020188,"text":"70020188 - 1997 - Gas hydrates in the Messoyakha gas field of the West Siberian Basin - a re-examination of the geologic evidence","interactions":[],"lastModifiedDate":"2012-03-12T17:20:19","indexId":"70020188","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Gas hydrates in the Messoyakha gas field of the West Siberian Basin - a re-examination of the geologic evidence","docAbstract":"The amount of natural gas within the gas hydrate accumulations of the world is believed to greatly exceed the volume of known conventional natural gas reserves. The hydrocarbon production history of the Russian Messoyakha field, located in the West Siberian Basin, has been used as evidence that gas hydrates are an immediate source of natural gas that can be produced by conventional means. Re-examination of available geologic, geochemical, and hydrocarbon production data suggests, however, that gas hydrates may not have contributed to gas production in the Messoyakha field. More field and laboratory studies are needed to assess the historical contribution of gas hydrate production in the Messoyakha field.","largerWorkTitle":"Proceedings of the International Offshore and Polar Engineering Conference","conferenceTitle":"Proceedings of the 1997 7th International Offshore and Polar Engineering Conference. Part 3 (of 4)","conferenceDate":"25 May 1997 through 30 May 1997","conferenceLocation":"Honolulu, HI, USA","language":"English","publisher":"Int Soc of Offshore and Polar Engineerns (ISOPE)","publisherLocation":"Golden, CO, United States","usgsCitation":"Collett, T.S., and Ginsburg, G.D., 1997, Gas hydrates in the Messoyakha gas field of the West Siberian Basin - a re-examination of the geologic evidence, <i>in</i> Proceedings of the International Offshore and Polar Engineering Conference, v. 1, Honolulu, HI, USA, 25 May 1997 through 30 May 1997, p. 96-103.","startPage":"96","endPage":"103","numberOfPages":"8","costCenters":[],"links":[{"id":231319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14d4e4b0c8380cd54bb4","contributors":{"editors":[{"text":"Chung J.S.Kim C.H.Olagnon M.Naito S.","contributorId":128386,"corporation":true,"usgs":false,"organization":"Chung J.S.Kim C.H.Olagnon M.Naito S.","id":536462,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Collett, Timothy S. 0000-0002-7598-4708 tcollett@usgs.gov","orcid":"https://orcid.org/0000-0002-7598-4708","contributorId":1698,"corporation":false,"usgs":true,"family":"Collett","given":"Timothy","email":"tcollett@usgs.gov","middleInitial":"S.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":385311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ginsburg, Gabriel D.","contributorId":7036,"corporation":false,"usgs":true,"family":"Ginsburg","given":"Gabriel","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":385312,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70019569,"text":"70019569 - 1997 - Springs and seeps of colonial National Historical Park: Groundwater study will help analyze off-site impacts to park ecosystem","interactions":[],"lastModifiedDate":"2012-03-12T17:19:20","indexId":"70019569","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3014,"text":"Park Science","active":true,"publicationSubtype":{"id":10}},"title":"Springs and seeps of colonial National Historical Park: Groundwater study will help analyze off-site impacts to park ecosystem","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Park Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"07359462","usgsCitation":"Focazio, M., 1997, Springs and seeps of colonial National Historical Park: Groundwater study will help analyze off-site impacts to park ecosystem: Park Science, v. 17, no. 2, p. 12-13.","startPage":"12","endPage":"13","numberOfPages":"2","costCenters":[],"links":[{"id":227918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9630e4b08c986b31b357","contributors":{"authors":[{"text":"Focazio, M.","contributorId":45848,"corporation":false,"usgs":true,"family":"Focazio","given":"M.","affiliations":[],"preferred":false,"id":383202,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70019677,"text":"70019677 - 1997 - The sandflat habitat: Scaling from experiments to conclusions","interactions":[],"lastModifiedDate":"2017-03-07T16:40:24","indexId":"70019677","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The sandflat habitat: Scaling from experiments to conclusions","docAbstract":"<p>Ecological systems are characterised by spatial and temporal variations in the density of organisms and resources, and in the intensity of processes which affect them (e.g. Watt, 1947, Dayton, 1971, Addicot et al., 1987, Kolasa and Pickett, 1991 and Giller et al., 1994). This heterogeneity represents both a difficulty for field study design and statistical testing, and a challenge to describe the spatial structuring of populations, communities and ecosystems (Legendre, 1993). Patterns in ecological and environmental variables are fundamental to developing hypotheses and in designing subsequent field studies, because they determine the spatial and temporal scales of study. Spatial and/or temporal patterns also provide useful stepping stones for addressing issues of scale. Patterns apparent at one scale can collapse to noise when viewed from other scales, indicating that patterns, processes and our perceptions vary in a scale-dependent manner. 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,{"id":1004005,"text":"1004005 - 1997 - Nested taxa-area curves for eastern United States floras","interactions":[],"lastModifiedDate":"2015-05-04T13:14:59","indexId":"1004005","displayToPublicDate":"1997-01-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3297,"text":"Rhodora","active":true,"publicationSubtype":{"id":10}},"title":"Nested taxa-area curves for eastern United States floras","docAbstract":"<p>The slopes of log-log species-area curves have been studied extensively and found to be influenced by the range of areas under study. Two such studies of eastern United States floras have yielded species-area curve slopes which differ by more than 100%: 0.251 and 0.113. The first slope may be too steep because the flora of the world was included, and both may be too steep because noncontiguous areas were used. These two hypotheses were tested using a set of nested floras centered in Ohio and continuing up to the flora of the world. The results suggest that this set of eastern United States floras produces a log-log species-area curve with a slope of approximately 0.20 with the flora of the world excluded, and regardless of whether or not the floras are from nested areas. Genera- and family-area curves are less steep than species-area curves and show similar patterns. Taxa ratio curves also increase with area, with the species/family ratio showing the steepest slope.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Rhodora","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Bennett, J.P., 1997, Nested taxa-area curves for eastern United States floras: Rhodora, v. 99, no. 899, p. 241-251.","productDescription":"p. 241-251","startPage":"241","endPage":"251","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":129651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Ohio","otherGeospatial":"Hopewell Culture National Historic Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.00617218017578,\n              39.382742911429034\n            ],\n            [\n              -83.00110816955566,\n              39.39023900346479\n            ],\n            [\n              -82.99080848693848,\n              39.39156566154972\n            ],\n            [\n              -82.97896385192871,\n              39.39421890204694\n            ],\n            [\n              -82.97475814819336,\n              39.38479944160311\n            ],\n            [\n              -82.9738998413086,\n              39.38115071741885\n            ],\n            [\n              -82.97518730163574,\n              39.37849698002401\n            ],\n            [\n              -82.98969268798828,\n              39.37969117433663\n            ],\n            [\n              -82.99818992614746,\n              39.37517966640772\n            ],\n            [\n              -83.00256729125977,\n              39.3775018024908\n            ],\n            [\n              -83.00617218017578,\n              39.38234486633152\n            ],\n            [\n              -83.00617218017578,\n              39.382742911429034\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"99","issue":"899","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697cc4","contributors":{"authors":[{"text":"Bennett, J. P.","contributorId":52103,"corporation":false,"usgs":true,"family":"Bennett","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":314909,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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