{"pageNumber":"2191","pageRowStart":"54750","pageSize":"25","recordCount":184553,"records":[{"id":70033108,"text":"70033108 - 2008 - Enabling global collaboration in the geosciences","interactions":[],"lastModifiedDate":"2012-03-12T17:21:37","indexId":"70033108","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Enabling global collaboration in the geosciences","docAbstract":"[No abstract available]","largerWorkTitle":"Eos","language":"English","issn":"00963","usgsCitation":"Klump, J., Allison, L., Asch, K., Fox, P., Gundersen, L., Jackson, I., Loewe, P., Snyder, W., and Ritschel, B., 2008, Enabling global collaboration in the geosciences, <i>in</i> Eos, v. 89, no. 49, p. 503-504.","startPage":"503","endPage":"504","numberOfPages":"2","costCenters":[],"links":[{"id":241120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"49","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0918e4b0c8380cd51ddc","contributors":{"authors":[{"text":"Klump, J.","contributorId":101527,"corporation":false,"usgs":true,"family":"Klump","given":"J.","affiliations":[],"preferred":false,"id":439407,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allison, L.","contributorId":51611,"corporation":false,"usgs":true,"family":"Allison","given":"L.","affiliations":[],"preferred":false,"id":439402,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Asch, K.","contributorId":57732,"corporation":false,"usgs":true,"family":"Asch","given":"K.","email":"","affiliations":[],"preferred":false,"id":439403,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fox, P.","contributorId":59213,"corporation":false,"usgs":true,"family":"Fox","given":"P.","email":"","affiliations":[],"preferred":false,"id":439405,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gundersen, L.","contributorId":58903,"corporation":false,"usgs":true,"family":"Gundersen","given":"L.","email":"","affiliations":[],"preferred":false,"id":439404,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jackson, I.","contributorId":89752,"corporation":false,"usgs":true,"family":"Jackson","given":"I.","email":"","affiliations":[],"preferred":false,"id":439406,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Loewe, P.","contributorId":47253,"corporation":false,"usgs":true,"family":"Loewe","given":"P.","email":"","affiliations":[],"preferred":false,"id":439401,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Snyder, W.S.","contributorId":107428,"corporation":false,"usgs":true,"family":"Snyder","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":439408,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Ritschel, B.","contributorId":43634,"corporation":false,"usgs":true,"family":"Ritschel","given":"B.","email":"","affiliations":[],"preferred":false,"id":439400,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70033455,"text":"70033455 - 2008 - Seasonal habitat use of brook trout and juvenile Atlantic Salmon in a Tributary of Lake Ontario","interactions":[],"lastModifiedDate":"2015-11-24T13:11:33","indexId":"70033455","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2898,"text":"Northeastern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal habitat use of brook trout and juvenile Atlantic Salmon in a Tributary of Lake Ontario","docAbstract":"<p><span>The seasonal habitat use of&nbsp;</span><i>Salvelinus fontinalis</i><span>&nbsp;(Brook Trout) and sub-yearling&nbsp;</span><i>Salmo salar&nbsp;</i><span>(Atlantic Salmon) was examined in Hart Brook, a tributary of Lake Ontario. Fish habitat use and available habitat were examined during summer and autumn. Interspecific differences in habitat use occurred as well as intraspecific seasonal differences. Overyearling Brook Trout were more selective in their habitat preferences than subyearling Brook Trout or juvenile Atlantic Salmon. Depth and the amount of cover were significantly different among the three fish groups. Salmon occupied faster and shallower water than either age group of trout. Atlantic Salmon were also associated with larger-sized substrate materials than either trout age group, and salmon occurred in habitats with less cover than trout. Overyearling Brook Trout occupied deeper water with more cover than subyearling trout. All three salmonid groups occupied areas with more cover in autumn compared to summer. In autumn, subyearling Brook Trout used deeper areas than they had in the summer. In Hart Brook, the habitat of subyearling Atlantic Salmon can be generally characterized as riffles, the habitat of overyearling Brook Trout was deep pools with extensive cover (35%), and that of subyearling trout was any area with moderate flow and at least 20% cover. As efforts proceed to reintroduce Atlantic Salmon in Lake Ontario, further research is needed to ensure the conservation of Brook Trout populations.</span></p>","language":"English","publisher":"Humboldt Field Research Institute","publisherLocation":"Steuben, ME","doi":"10.1656/1092-6194-15.3.363","issn":"10926194","usgsCitation":"Johnson, J.H., 2008, Seasonal habitat use of brook trout and juvenile Atlantic Salmon in a Tributary of Lake Ontario: Northeastern Naturalist, v. 15, no. 3, p. 363-374, https://doi.org/10.1656/1092-6194-15.3.363.","productDescription":"12 p.","startPage":"363","endPage":"374","numberOfPages":"12","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":241883,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Hart Brook, Lake Ontario","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.1,\n              43.8\n            ],\n            [\n              -76.1,\n              43.85\n            ],\n            [\n              -76,\n              43.85\n            ],\n            [\n              -76,\n              43.8\n            ],\n            [\n              -76.1,\n              43.8\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b88afe4b08c986b316ae3","contributors":{"authors":[{"text":"Johnson, James H. 0000-0002-5619-3871 jhjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-5619-3871","contributorId":389,"corporation":false,"usgs":true,"family":"Johnson","given":"James","email":"jhjohnson@usgs.gov","middleInitial":"H.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":440936,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70033205,"text":"70033205 - 2008 - An evaluation of the precision of fin ray, otolith, and scale age determinations for brook trout","interactions":[],"lastModifiedDate":"2012-03-12T17:21:38","indexId":"70033205","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","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":"An evaluation of the precision of fin ray, otolith, and scale age determinations for brook trout","docAbstract":"The ages of brook trout Salvelinus fontinalis are typically estimated using scales despite a lack of research documenting the effectiveness of this technique. The use of scales is often preferred because it is nonlethal and is believed to require less effort than alternative methods. To evaluate the relative effectiveness of different age estimation methodologies for brook trout, we measured the precision and processing times of scale, sagittal otolith, and pectoral fin ray age estimation techniques. Three independent readers, age bias plots, coefficients of variation (CV = 100 x SD/mean), and percent agreement (PA) were used to measure within-reader, among-structure bias and within-structure, among-reader precision. Bias was generally minimal; however, the age estimates derived from scales tended to be lower than those derived from otoliths within older (age > 2) cohorts. Otolith, fin ray, and scale age estimates were within 1 year of each other for 95% of the comparisons. The measures of precision for scales (CV = 6.59; PA = 82.30) and otoliths (CV = 7.45; PA = 81.48) suggest higher agreement between these structures than with fin rays (CV = 11.30; PA = 65.84). The mean per-sample processing times were lower for scale (13.88 min) and otolith techniques (12.23 min) than for fin ray techniques (22.68 min). The comparable processing times of scales and otoliths contradict popular belief and are probably a result of the high proportion of regenerated scales within samples and the ability to infer age from whole (as opposed to sectioned) otoliths. This research suggests that while scales produce age estimates rivaling those of otoliths for younger (age > 3) cohorts, they may be biased within older cohorts and therefore should be used with caution. ?? Copyright by the American Fisheries Society 2008.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Fisheries Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/M07-187.1","issn":"02755","usgsCitation":"Stolarski, J., and Hartman, K., 2008, An evaluation of the precision of fin ray, otolith, and scale age determinations for brook trout: North American Journal of Fisheries Management, v. 28, no. 6, p. 1790-1795, https://doi.org/10.1577/M07-187.1.","startPage":"1790","endPage":"1795","numberOfPages":"6","costCenters":[],"links":[{"id":213429,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/M07-187.1"},{"id":241054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"6","noUsgsAuthors":false,"publicationDate":"2008-12-01","publicationStatus":"PW","scienceBaseUri":"5059ea58e4b0c8380cd487ce","contributors":{"authors":[{"text":"Stolarski, J.T.","contributorId":96487,"corporation":false,"usgs":true,"family":"Stolarski","given":"J.T.","affiliations":[],"preferred":false,"id":439828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hartman, K.J.","contributorId":64007,"corporation":false,"usgs":true,"family":"Hartman","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":439827,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70033109,"text":"70033109 - 2008 - A soil burn severity index for understanding soil-fire relations in tropical forests","interactions":[],"lastModifiedDate":"2017-11-17T11:33:02","indexId":"70033109","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"A soil burn severity index for understanding soil-fire relations in tropical forests","docAbstract":"Methods for evaluating the impact of fires within tropical forests are needed as fires become more frequent and human populations and demands on forests increase. Short- and long-term fire effects on soils are determined by the prefire, fire, and postfire environments. We placed these components within a fire-disturbance continuum to guide our literature synthesis and develop an integrated soil burn severity index. The soil burn severity index provides a set of indicators that reflect the range of conditions present after a fire. The index consists of seven levels, an unburned level and six other levels that describe a range of postfire soil conditions. We view this index as a tool for understanding the effects of fires on the forest floor, with the realization that as new information is gained, the index may be modified as warranted. ?? Royal Swedish Academy of Sciences 2008.","largerWorkTitle":"Ambio","language":"English","issn":"00447","usgsCitation":"Jain, T., Gould, W., Graham, R., Pilliod, D., Lentile, L., and Gonzalez, G., 2008, A soil burn severity index for understanding soil-fire relations in tropical forests, <i>in</i> Ambio, v. 37, no. 7-8, p. 563-568.","startPage":"563","endPage":"568","numberOfPages":"6","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":241121,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"7-8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e59be4b0c8380cd46e7e","contributors":{"authors":[{"text":"Jain, T.B.","contributorId":38368,"corporation":false,"usgs":true,"family":"Jain","given":"T.B.","email":"","affiliations":[],"preferred":false,"id":439410,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gould, W.A.","contributorId":42433,"corporation":false,"usgs":true,"family":"Gould","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":439411,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Graham, R.T.","contributorId":88159,"corporation":false,"usgs":true,"family":"Graham","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":439414,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pilliod, D. S.","contributorId":45259,"corporation":false,"usgs":false,"family":"Pilliod","given":"D. S.","affiliations":[],"preferred":false,"id":439412,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lentile, L.B.","contributorId":18582,"corporation":false,"usgs":true,"family":"Lentile","given":"L.B.","affiliations":[],"preferred":false,"id":439409,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gonzalez, G.","contributorId":47174,"corporation":false,"usgs":true,"family":"Gonzalez","given":"G.","email":"","affiliations":[],"preferred":false,"id":439413,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70033203,"text":"70033203 - 2008 - Influences of organic matter and calcification rate on trace elements in aragonitic estuarine bivalve shells","interactions":[],"lastModifiedDate":"2018-10-24T09:43:47","indexId":"70033203","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Influences of organic matter and calcification rate on trace elements in aragonitic estuarine bivalve shells","docAbstract":"<div id=\"abstracts\" class=\"Abstracts\"><div id=\"aep-abstract-id12\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id13\"><p>A suite of elements (B, Na, Mg, S, K, Ca, V, Mn, Cr, Sr, and Ba) was measured in aragonitic shells of the estuarine bivalve<span>&nbsp;</span><i>Corbula amurensis</i>, the Asian clam, using the Sensitive High-Resolution Ion MicroProbe with Reverse Geometry (SHRIMP RG). Our initial intent was to explore potential geochemical proxy relationships between shell chemistry and salinity (freshwater inflow) in northern San Francisco Bay (SFB). In the course of this study we observed variations in shell trace element to calcium ([M]/Ca) ratios that could only be attributed to internal biological processes. This paper discusses the nature and sources of internal trace element variability in<span>&nbsp;</span><i>C. amurensis</i><span>&nbsp;</span>shells related to the shell organic fraction and shell calcification rates. The average organic content of whole<span>&nbsp;</span><i>C. amurensis</i><span>&nbsp;</span>shells is 19%. After treating whole powdered shells with an oxidative cleaning procedure to remove organic matter, shells contained on average 33% less total Mg and 78% less total Mn. Within our analytical uncertainty, Sr and Ba contents were unchanged by the removal of organic matter. These results show that aragonitic<span>&nbsp;</span><i>C. amurensis</i><span>&nbsp;</span>shells have a large component of non-lattice-bound Mg and Mn that probably contribute to the dissimilarity of [M]/Ca profiles among five same-sized shells. Non-lattice-bound trace elements could complicate the development and application of geochemical proxy relationships in bivalve shells. Because B, Ba and Sr occur exclusively in shell aragonite, they are good candidates for external proxy relationships. [M]/Ca ratios were significantly different in prismatic and nacreous aragonite and in two valves of the same shell that had different crystal growth rates. Some part of these differences can be attributed to non-lattice-bound trace elements associated with the organic fraction. The differences in [M]/Ca ratios were also consistent with the calcification rate-dependent ion transport model developed by Carré et al. [Carré M., Bentaleb I., Bruguier O., Ordinola E., Barrett N. T. and Fontugne M. (2006) Calcification rate influence on trace element concentrations in aragonitic bivalve shells: evidences and mechanisms.<span>&nbsp;</span><i>Geochim. Cosmochim. Acta</i><strong>70</strong>, 4906–4920] which predicts that [M]/Ca ratios increase as calcification rates increase and Ca<sup>2+</sup><span>&nbsp;</span>channel specificity decreases. This result, in combination with the possibility that there were ontogenetic variations in growth rates among individuals younger than 2 years, underscores the need to develop an independent age model for<span>&nbsp;</span><i>C. amurensis</i><span>&nbsp;</span>shells. If growth-rate effects on lattice-bound [M]/Ca ratios can be constrained, it may yet be possible to develop high-resolution geochemical proxies for external solution chemistry in low-salinity regions of SFB.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/j.gca.2008.09.003","issn":"00167","usgsCitation":"Takesue, R., Bacon, C., and Thompson, J., 2008, Influences of organic matter and calcification rate on trace elements in aragonitic estuarine bivalve shells: Geochimica et Cosmochimica Acta, v. 72, no. 22, p. 5431-5445, https://doi.org/10.1016/j.gca.2008.09.003.","productDescription":"15 p.","startPage":"5431","endPage":"5445","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":241018,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213395,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.gca.2008.09.003"}],"volume":"72","issue":"22","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3ba3e4b0c8380cd6270a","contributors":{"authors":[{"text":"Takesue, R.K.","contributorId":21645,"corporation":false,"usgs":true,"family":"Takesue","given":"R.K.","affiliations":[],"preferred":false,"id":439820,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bacon, C. R. 0000-0002-2165-5618","orcid":"https://orcid.org/0000-0002-2165-5618","contributorId":21522,"corporation":false,"usgs":true,"family":"Bacon","given":"C. R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":439819,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, J.K.","contributorId":103300,"corporation":false,"usgs":true,"family":"Thompson","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":439821,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70033767,"text":"70033767 - 2008 - Food web dynamics in a seasonally varying wetland","interactions":[],"lastModifiedDate":"2012-03-12T17:21:31","indexId":"70033767","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2699,"text":"Mathematical Biosciences and Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Food web dynamics in a seasonally varying wetland","docAbstract":"A spatially explicit model is developed to simulate the small fish community and its underlying food web, in the freshwater marshes of the Everglades. The community is simplified to a few small fish species feeding on periphyton and invertebrates. Other compartments are detritus, crayfish, and a piscivorous fish species. This unit food web model is applied to each of the 10,000 spatial cells on a 100 x 100 pixel landscape. Seasonal variation in water level is assumed and rules are assigned for fish movement in response to rising and falling water levels, which can cause many spatial cells to alternate between flooded and dry conditions. It is shown that temporal variations of water level on a spatially heterogeneous landscape can maintain at least three competing fish species. In addition, these environmental factors can strongly affect the temporal variation of the food web caused by top-down control from the piscivorous fish.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mathematical Biosciences and Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.3934/mbe.2008.5.877","issn":"15471","usgsCitation":"DeAngelis, D., Trexler, J., and Donalson, D., 2008, Food web dynamics in a seasonally varying wetland: Mathematical Biosciences and Engineering, v. 5, no. 4, p. 877-887, https://doi.org/10.3934/mbe.2008.5.877.","startPage":"877","endPage":"887","numberOfPages":"11","costCenters":[],"links":[{"id":476646,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3934/mbe.2008.5.877","text":"Publisher Index Page"},{"id":214234,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3934/mbe.2008.5.877"},{"id":241934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a12e6e4b0c8380cd54435","contributors":{"authors":[{"text":"DeAngelis, D.L. 0000-0002-1570-4057","orcid":"https://orcid.org/0000-0002-1570-4057","contributorId":32470,"corporation":false,"usgs":true,"family":"DeAngelis","given":"D.L.","affiliations":[],"preferred":false,"id":442359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trexler, J.C.","contributorId":23108,"corporation":false,"usgs":true,"family":"Trexler","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":442358,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Donalson, D.D.","contributorId":69793,"corporation":false,"usgs":true,"family":"Donalson","given":"D.D.","affiliations":[],"preferred":false,"id":442360,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70033197,"text":"70033197 - 2008 - The utility of gravity and water-level monitoring at alluvial aquifer wells in southern Arizona","interactions":[],"lastModifiedDate":"2012-03-12T17:21:34","indexId":"70033197","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"The utility of gravity and water-level monitoring at alluvial aquifer wells in southern Arizona","docAbstract":"Coincident monitoring of gravity and water levels at 39 wells in southern Arizona indicate that water-level change might not be a reliable indicator of aquifer-storage change for alluvial aquifer systems. One reason is that water levels in wells that are screened across single or multiple aquifers might not represent the hydraulic head and storage change in a local unconfined aquifer. Gravity estimates of aquifer-storage change can be approximated as a one-dimensional feature except near some withdrawal wells and recharge sources. The aquifer storage coefficient is estimated by the linear regression slope of storage change (estimated using gravity methods) and water-level change. Nonaquifer storage change that does not percolate to the aquifer can be significant, greater than 3 ??Gal, when water is held in the root zone during brief periods following extreme rates of precipitation. Monitor-ing of storage change using gravity methods at wells also can improve understanding of local hydrogeologic conditions. In the study area, confined aquifer conditions are likely at three wells where large water-level variations were accompanied by little gravity change. Unconfined conditions were indicated at 15 wells where significant water-level and gravity change were positively linearly correlated. Good positive linear correlations resulted in extremely large specific-yield values, greater than 0.35, at seven wells where it is likely that significant ephemeral streamflow infiltration resulted in unsaturated storage change. Poor or negative linear correlations indicate the occurrence of confined, multiple, or perched aquifers. Monitoring of a multiple compressible aquifer system at one well resulted in negative correlation of rising water levels and subsidence-corrected gravity change, which suggests that water-level trends at the well are not a good indicatior of overall storage change. ?? 2008 Society of Exploration Geophysicists. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geophysics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1190/1.2978166","issn":"00168","usgsCitation":"Pool, D.R., 2008, The utility of gravity and water-level monitoring at alluvial aquifer wells in southern Arizona: Geophysics, v. 73, no. 6, https://doi.org/10.1190/1.2978166.","costCenters":[],"links":[{"id":213309,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1190/1.2978166"},{"id":240921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"73","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb1a5e4b08c986b32538d","contributors":{"authors":[{"text":"Pool, D. R.","contributorId":75581,"corporation":false,"usgs":true,"family":"Pool","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":439785,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70033461,"text":"70033461 - 2008 - NMR and mass spectrometry of phosphorus in wetlands","interactions":[],"lastModifiedDate":"2012-03-12T17:21:33","indexId":"70033461","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1594,"text":"European Journal of Soil Science","active":true,"publicationSubtype":{"id":10}},"title":"NMR and mass spectrometry of phosphorus in wetlands","docAbstract":"There is at present little information on the long-term stability of phosphorus sequestered in wetlands. Phosphorus sequestered during high loading periods may be relatively unstable and easily remobilized following changes in nutrient status or hydrological regime, but the chemical forms of sequestered phosphorus that do remobilize are largely unknown at this time. A lack of suitable analytical techniques has contributed to this dearth of knowledge regarding the stability of soil organic phosphorus. We analysed phosphorus in soils from the 'head' of Rescue Strand tree island and an adjacent marsh in the Florida Everglades by 31P nuclear magnetic resonance (NMR) spectroscopy and high-resolution mass spectrometry. Tree islands are important areas of biodiversity within the Everglades and offer a unique opportunity to study phosphorus sequestration because they are exposed to large phosphorus loads and appear to be natural nutrient sinks. The 31P NMR profiling of extracts from surface and sediment samples in the tree island indicates that phosphorus input to Rescue Strand tree island soils is mostly in the form of inorganic ortho-phosphate and is either refractory when deposited or rapidly recycled by the native vegetation into a stable phosphorus pool largely resistant to re-utilization by plants or microbes. Mass spectrometry revealed the presence of inositol hexakisphosphate, a common organic monophosphate ester not previously observed in Everglades' soils. ?? 2008 The Authors.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"European Journal of Soil Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1365-2389.2007.01008.x","issn":"13510754","usgsCitation":"El-Rifai, H., Heerboth, M., Gedris, T., Newman, S., Orem, W., and Cooper, W., 2008, NMR and mass spectrometry of phosphorus in wetlands: European Journal of Soil Science, v. 59, no. 3, p. 517-525, https://doi.org/10.1111/j.1365-2389.2007.01008.x.","startPage":"517","endPage":"525","numberOfPages":"9","costCenters":[],"links":[{"id":214246,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-2389.2007.01008.x"},{"id":241946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","issue":"3","noUsgsAuthors":false,"publicationDate":"2008-02-04","publicationStatus":"PW","scienceBaseUri":"505a6147e4b0c8380cd718b9","contributors":{"authors":[{"text":"El-Rifai, H.","contributorId":34733,"corporation":false,"usgs":true,"family":"El-Rifai","given":"H.","email":"","affiliations":[],"preferred":false,"id":440963,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heerboth, M.","contributorId":73024,"corporation":false,"usgs":true,"family":"Heerboth","given":"M.","email":"","affiliations":[],"preferred":false,"id":440965,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gedris, T.E.","contributorId":77752,"corporation":false,"usgs":true,"family":"Gedris","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":440966,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Newman, S.","contributorId":7678,"corporation":false,"usgs":true,"family":"Newman","given":"S.","affiliations":[],"preferred":false,"id":440962,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Orem, W. 0000-0003-4990-0539","orcid":"https://orcid.org/0000-0003-4990-0539","contributorId":87335,"corporation":false,"usgs":true,"family":"Orem","given":"W.","affiliations":[],"preferred":false,"id":440967,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cooper, W.T.","contributorId":40437,"corporation":false,"usgs":true,"family":"Cooper","given":"W.T.","email":"","affiliations":[],"preferred":false,"id":440964,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70176273,"text":"70176273 - 2008 - Vision of a cyberinfrastructure for nonnative, invasive species management","interactions":[],"lastModifiedDate":"2018-10-11T15:57:23","indexId":"70176273","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":997,"text":"BioScience","active":true,"publicationSubtype":{"id":10}},"title":"Vision of a cyberinfrastructure for nonnative, invasive species management","docAbstract":"<p><span>Although the quantity of data on the location, status, and management of invasive species is ever increasing, invasive species data sets are often difficult to obtain and integrate. A cyberinfrastructure for such information could make these data available for Internet users. The data can be used to create regional watch lists, to send e-mail alerts when a new species enters a region, to construct models of species' current and future distributions, and to inform management. Although the exchange of environmental data over the Internet in the form of raster data is maturing, and the exchange of species occurrence data is developing quickly, there is room for improvement. In this article, we present a vision for a comprehensive invasive species cyberinfrastructure that is capable of accessing data effectively, creating models of invasive species spread, and distributing this information.</span></p>","language":"English","publisher":"Oxford Journals","doi":"10.1641/B580312","usgsCitation":"Graham, J., Simpson, A., Crall, A.W., Jarnevich, C.S., Newman, G., and Stohlgren, T.J., 2008, Vision of a cyberinfrastructure for nonnative, invasive species management: BioScience, v. 58, no. 3, p. 263-268, https://doi.org/10.1641/B580312.","productDescription":"6 p.","startPage":"263","endPage":"268","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true},{"id":37226,"text":"Core Science Analytics, Synthesis, and Libraries","active":true,"usgs":true}],"links":[{"id":476833,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1641/b580312","text":"Publisher Index Page"},{"id":328288,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57cfe8c0e4b04836416a0e5e","contributors":{"authors":[{"text":"Graham, Jim","contributorId":37608,"corporation":false,"usgs":true,"family":"Graham","given":"Jim","email":"","affiliations":[],"preferred":false,"id":748324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simpson, Annie 0000-0001-8338-5134 asimpson@usgs.gov","orcid":"https://orcid.org/0000-0001-8338-5134","contributorId":127,"corporation":false,"usgs":true,"family":"Simpson","given":"Annie","email":"asimpson@usgs.gov","affiliations":[{"id":208,"text":"Core Science Analytics and Synthesis","active":true,"usgs":true}],"preferred":true,"id":748325,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crall, Alycia W.","contributorId":60123,"corporation":false,"usgs":true,"family":"Crall","given":"Alycia","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":748326,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jarnevich, Catherine S. 0000-0002-9699-2336 jarnevichc@usgs.gov","orcid":"https://orcid.org/0000-0002-9699-2336","contributorId":3424,"corporation":false,"usgs":true,"family":"Jarnevich","given":"Catherine","email":"jarnevichc@usgs.gov","middleInitial":"S.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":748327,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Newman, Greg","contributorId":22636,"corporation":false,"usgs":true,"family":"Newman","given":"Greg","affiliations":[],"preferred":false,"id":748328,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stohlgren, Thomas J. 0000-0001-9696-4450 stohlgrent@usgs.gov","orcid":"https://orcid.org/0000-0001-9696-4450","contributorId":2902,"corporation":false,"usgs":true,"family":"Stohlgren","given":"Thomas","email":"stohlgrent@usgs.gov","middleInitial":"J.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":748329,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70009719,"text":"70009719 - 2008 - Introduction to the U.S. Geological Survey National Water-Quality Assessment (NAWQA) of ground-water quality trends and comparison to other national programs","interactions":[],"lastModifiedDate":"2012-03-12T17:18:22","indexId":"70009719","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Introduction to the U.S. Geological Survey National Water-Quality Assessment (NAWQA) of ground-water quality trends and comparison to other national programs","docAbstract":"Assessment of temporal trends in national ground-water quality networks are rarely published in scientific journals. This is partly due to the fact that long-term data from these types of networks are uncommon and because many national monitoring networks are not driven by hypotheses that can be easily incorporated into scientific research. The U.S. Geological Survey (USGS) National Water-Quality Assessment Program (NAWQA) since 1991 has to date (2006) concentrated on occurrence of contaminants because sufficient data for trend analysis is only just becoming available. This paper introduces the first set of trend assessments from NAWQA and provides an assessment of the success of the program. On a national scale, nitrate concentrations in ground water have generally increased from 1988 to 2004, but trends in pesticide concentrations are less apparent. Regionally, the studies showed high nitrate concentrations and frequent pesticide detections are linked to agricultural use of fertilizers and pesticides. Most of these areas showed increases in nitrate concentration within the last decade, and these increases are associated with oxic-geochemical conditions and well-drained soils. The current NAWQA plan for collecting data to define trends needs to be constantly reevaluated to determine if the approach fulfills the expected outcome. To assist this evaluation, a comparison of NAWQA to other national ground-water quality programs was undertaken. The design and spatial extent of each national program depend on many factors, including current and long-term budgets, purpose of the program, size of the country, and diversity of aquifer types. Comparison of NAWQA to nine other national programs shows a great diversity in program designs, but indicates that different approaches can achieve similar and equally important goals. Copyright ?? 2008 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America. All rights reserved.","largerWorkTitle":"Journal of Environmental Quality","language":"English","doi":"10.2134/jeq2008.0049","issn":"00472425","usgsCitation":"Rosen, M.R., and Lapham, W., 2008, Introduction to the U.S. Geological Survey National Water-Quality Assessment (NAWQA) of ground-water quality trends and comparison to other national programs, <i>in</i> Journal of Environmental Quality, v. 37, no. SUPPL. 5, https://doi.org/10.2134/jeq2008.0049.","costCenters":[],"links":[{"id":476774,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2134/jeq2008.0049","text":"Publisher Index Page"},{"id":219327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":204937,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2134/jeq2008.0049"}],"volume":"37","issue":"SUPPL. 5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3dfae4b0c8380cd639db","contributors":{"authors":[{"text":"Rosen, Michael R.","contributorId":43096,"corporation":false,"usgs":true,"family":"Rosen","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":356948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lapham, W.W.","contributorId":36583,"corporation":false,"usgs":true,"family":"Lapham","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":356947,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1004088,"text":"1004088 - 2008 - Distribution and morphology of growth anomalies in Acropora from the Indo-Pacific","interactions":[],"lastModifiedDate":"2018-02-20T15:02:00","indexId":"1004088","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1396,"text":"Diseases of Aquatic Organisms","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Distribution and morphology of growth anomalies in <i>Acropora</i> from the Indo-Pacific","title":"Distribution and morphology of growth anomalies in Acropora from the Indo-Pacific","docAbstract":"<p><span>We assessed the distribution and prevalence of growth anomalies (GAs) in&nbsp;</span><i>Acropora</i><span><span>&nbsp;</span>from French Frigate Shoals (Hawaii, USA), Johnston Atoll and Tutuila (American Samoa), developed a nomenclature for gross morphology, characterized GAs at the cellular level and obtained preliminary indices of their spatial patterns and progression within coral colonies.<span>&nbsp;</span></span><i>Acropora</i><span><span>&nbsp;</span>GAs were found in all 3 regions, but the distribution, variety and prevalence of<span>&nbsp;</span></span><i>Acropora</i><span><span>&nbsp;</span>GAs was highest in American Samoa. GAs were grouped into 7 gross morphologies (exophytic, bosselated, crateriform, nodular, vermiform, fimbriate or annular). On histology, GAs consisted of hyperplastic basal body wall (calicodermis, mesoglea and gastrodermis apposed to skeleton) with 3 distinct patterns of necrosis. There was no evidence of anaplasia or mitotic figures (common but not necessarily required morphologic indicators of neoplasia). Compared to normal tissues, GAs had significantly fewer polyps, zooxanthellae within the gastrodermis of the coenenchyme, mesenterial filaments and gonads but significantly more necrosis. On 2 colonies with GAs monitored at 2 points over 11 mo, numbers of GAs per colony increased from 0.9 to 3 times the original number seen, and significant clustering of GAs occurred within colonies. The evidence of GAs being true neoplasias (tumors) is mixed, so a cautionary approach is urged in use of morphologic terminology.</span></p>","language":"English","publisher":"Inter-Research","doi":"10.3354/dao01881","usgsCitation":"Work, T.M., Aeby, G.S., and Coles, S.L., 2008, Distribution and morphology of growth anomalies in Acropora from the Indo-Pacific: Diseases of Aquatic Organisms, v. 78, no. 3, p. 255-264, https://doi.org/10.3354/dao01881.","productDescription":"10 p.","startPage":"255","endPage":"264","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":486899,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/dao01881","text":"Publisher Index Page"},{"id":135802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawai'i","otherGeospatial":"American Samoa","volume":"78","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495c7","contributors":{"authors":[{"text":"Work, Thierry M. 0000-0002-4426-9090","orcid":"https://orcid.org/0000-0002-4426-9090","contributorId":34078,"corporation":false,"usgs":true,"family":"Work","given":"Thierry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":315147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aeby, Greta S.","contributorId":64783,"corporation":false,"usgs":false,"family":"Aeby","given":"Greta","email":"","middleInitial":"S.","affiliations":[{"id":13394,"text":"Hawai‘i Institute of Marine Biology","active":true,"usgs":false}],"preferred":false,"id":315149,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coles, Steve L.","contributorId":172257,"corporation":false,"usgs":false,"family":"Coles","given":"Steve","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":315148,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70009709,"text":"70009709 - 2008 - Using open hole and cased-hole resistivity logs to monitor gas hydrate dissociation during a thermal test in the mallik 5L-38 research well, Mackenzie Delta, Canada","interactions":[],"lastModifiedDate":"2012-03-12T17:18:24","indexId":"70009709","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Using open hole and cased-hole resistivity logs to monitor gas hydrate dissociation during a thermal test in the mallik 5L-38 research well, Mackenzie Delta, Canada","docAbstract":"Gas hydrates, which are naturally occurring ice-like combinations of gas and water, have the potential to provide vast amounts of natural gas from the world's oceans and polar regions. However, producing gas economically from hydrates entails major technical challenges. Proposed recovery methods such as dissociating or melting gas hydrates by heating or depressurization are currently being tested. One such test was conducted in northern Canada by the partners in the Mallik 2002 Gas Hydrate Production Research Well Program. This paper describes how resistivity logs were used to determine the size of the annular region of gas hydrate dissociation that occurred around the wellbore during the thermal test in the Mallik 5L-38 well. An open-hole logging suite, run prior to the thermal test, included array induction, array laterolog, nuclear magnetic resonance and 1.1-GHz electromagnetic propagation logs. The reservoir saturation tool was run both before and after the thermal test to monitor formation changes. A cased-hole formation resistivity log was run after the test.Baseline resistivity values in each formation layer (Rt) were established from the deep laterolog data. The resistivity in the region of gas hydrate dissociation near the wellbore (Rxo) was determined from electromagnetic propagation and reservoir saturation tool measurements. The radius of hydrate dissociation as a function of depth was then determined by means of iterative forward modeling of cased-hole formation resistivity tool response. The solution was obtained by varying the modeled dissociation radius until the modeled log overlaid the field log. Pretest gas hydrate production computer simulations had predicted that dissociation would take place at a uniform radius over the 13-ft test interval. However, the post-test resistivity modeling showed that this was not the case. The resistivity-derived dissociation radius was greatest near the outlet of the pipe that circulated hot water in the wellbore, where the highest temperatures were recorded. The radius was smallest near the center of the test interval, where a conglomerate section with low values of porosity and permeability inhibited dissociation. The free gas volume calculated from the resistivity-derived dissociation radii yielded a value within 20 per cent of surface gauge measurements. These results show that the inversion of resistivity measurements holds promise for use in future gas hydrate monitoring. ?? 2008 Society of Petrophysicists and Well Log Analysts. All rights reserved.","largerWorkTitle":"Petrophysics","language":"English","issn":"15299074","usgsCitation":"Anderson, B., Collett, T.S., Lewis, R., and Dubourg, I., 2008, Using open hole and cased-hole resistivity logs to monitor gas hydrate dissociation during a thermal test in the mallik 5L-38 research well, Mackenzie Delta, Canada, <i>in</i> Petrophysics, v. 49, no. 3, p. 285-294.","startPage":"285","endPage":"294","numberOfPages":"10","costCenters":[],"links":[{"id":219103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc08ae4b08c986b32a1a9","contributors":{"authors":[{"text":"Anderson, B.I.","contributorId":41133,"corporation":false,"usgs":true,"family":"Anderson","given":"B.I.","email":"","affiliations":[],"preferred":false,"id":356903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collett, T. S. 0000-0002-7598-4708","orcid":"https://orcid.org/0000-0002-7598-4708","contributorId":86342,"corporation":false,"usgs":true,"family":"Collett","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":356904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lewis, R.E.","contributorId":31735,"corporation":false,"usgs":true,"family":"Lewis","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":356902,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dubourg, I.","contributorId":101000,"corporation":false,"usgs":true,"family":"Dubourg","given":"I.","email":"","affiliations":[],"preferred":false,"id":356905,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010005,"text":"70010005 - 2008 - Understanding slow slip, tremor, and quakes","interactions":[],"lastModifiedDate":"2012-03-12T17:18:22","indexId":"70010005","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Understanding slow slip, tremor, and quakes","docAbstract":"[No abstract available]","largerWorkTitle":"Eos","language":"English","issn":"00963941","usgsCitation":"Gomberg, J., Trehu, A., Roeloffs, E., and Dragert, H., 2008, Understanding slow slip, tremor, and quakes, <i>in</i> Eos, v. 89, no. 34.","startPage":"315","costCenters":[],"links":[{"id":218926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"34","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc5ae4b08c986b328b9f","contributors":{"authors":[{"text":"Gomberg, J.","contributorId":95994,"corporation":false,"usgs":true,"family":"Gomberg","given":"J.","email":"","affiliations":[],"preferred":false,"id":357650,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trehu, A.M.","contributorId":90754,"corporation":false,"usgs":true,"family":"Trehu","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":357649,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roeloffs, E.","contributorId":21680,"corporation":false,"usgs":true,"family":"Roeloffs","given":"E.","email":"","affiliations":[],"preferred":false,"id":357648,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dragert, H.","contributorId":8612,"corporation":false,"usgs":true,"family":"Dragert","given":"H.","affiliations":[],"preferred":false,"id":357647,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70009708,"text":"70009708 - 2008 - Prey of nesting ospreys on the Willamette and Columbia Rivers, Oregon and Washington","interactions":[],"lastModifiedDate":"2026-01-07T17:25:54.218161","indexId":"70009708","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2900,"text":"Northwest Science","onlineIssn":"2161-9859","printIssn":"0029-344X","active":true,"publicationSubtype":{"id":10}},"title":"Prey of nesting ospreys on the Willamette and Columbia Rivers, Oregon and Washington","docAbstract":"<p><span>To more effectively use ospreys as a biomonitoring tool and to better assess contaminant pathways, the diet of nesting ospreys (</span><span class=\"genus-species\">Pandion haliaetus</span><span>) was studied along the lower Columbia and upper mainstem Willamette rivers by evaluating prey remains collected from wire baskets constructed under artificial feeding perches installed near nest sites and from the ground beneath natural feeding perches and nests. Prey remains from 1997–2004 on the Columbia River and 1993 (previously published) and 2001 on the Willamette River were evaluated and compared. Largescale suckers (</span><span class=\"genus-species\">Catostomus macrocheilus</span><span>) were the predominate fish species identified in collections from the Columbia River (61.5% [84.3% biomass]) and Willamette River (76.0% [92.7% biomass]). Prey fish diversity, when based only on ground collections, was higher in the Columbia (2.45) than the Willamette river (1.92) (</span><i>P</i><span>&nbsp;= 0.038). Prey fish diversity in collections from the Willamette River did not differ between this study (2001) and previous study (1993) (</span><i>P</i><span>&nbsp;= 0.62). Fish bones recovered in wire baskets are likely more representative of osprey diet compared to bones recovered from the ground, because prey diversity was higher among basket samples compared to ground collections (wire basket diversity = 5.25 vs. ground collection diversity = 2.45,&nbsp;</span><i>P</i><span>&nbsp;= 0.011). Soft-boned salmonids (</span><span class=\"genus-species\">Oncorhynchus</span><span>&nbsp;</span><i>spp.</i><span>), American shad (</span><span class=\"genus-species\">Alosa sapidissima</span><span>), and mountain whitefish (</span><span class=\"genus-species\">Prosopium williamsoni</span><span>) were probably underrepresented in collections obtained from the ground. Study results suggest that baskets provide a better method for assessing osprey diet than other indirect methods. These findings augment available osprey food-habits information and provide additional biological and ecological information to better assess potential impacts of various environmental contaminants on nesting ospreys.</span></p>","language":"English","publisher":"BioOne","doi":"10.3955/0029-344X-82.3.229","issn":"0029344X","usgsCitation":"Johnson, B.L., Kaiser, J.L., Henny, C.J., and Grove, R.A., 2008, Prey of nesting ospreys on the Willamette and Columbia Rivers, Oregon and Washington: Northwest Science, v. 82, no. 3, p. 229-236, https://doi.org/10.3955/0029-344X-82.3.229.","productDescription":"8 p.","startPage":"229","endPage":"236","numberOfPages":"8","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":219102,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, 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 \"}}]}","volume":"82","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8b7fe4b0c8380cd7e27b","contributors":{"authors":[{"text":"Johnson, Branden L. 0000-0002-8018-6452 branden_johnson@usgs.gov","orcid":"https://orcid.org/0000-0002-8018-6452","contributorId":257446,"corporation":false,"usgs":true,"family":"Johnson","given":"Branden","email":"branden_johnson@usgs.gov","middleInitial":"L.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":356901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaiser, J. L.","contributorId":27602,"corporation":false,"usgs":true,"family":"Kaiser","given":"J.","middleInitial":"L.","affiliations":[],"preferred":false,"id":356900,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Henny, Charles J.","contributorId":12578,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":356899,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grove, R. A.","contributorId":6546,"corporation":false,"usgs":false,"family":"Grove","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":356898,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010003,"text":"70010003 - 2008 - Decadal-scale changes of pesticides in ground water of the United States, 1993-2003","interactions":[],"lastModifiedDate":"2012-03-12T17:18:21","indexId":"70010003","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Decadal-scale changes of pesticides in ground water of the United States, 1993-2003","docAbstract":"Pesticide data for ground water sampled across the United States between 1993-1995 and 2001-2003 by the U.S. Geological Survey National Water-Quality Assessment Program were evaluated for trends in detection frequency and concentration. The data analysis evaluated samples collected from a total of 362 wells located in 12 local well networks characterizing shallow ground water in agricultural areas and six local well networks characterizing the drinking water resource in areas of variable land use. Each well network was sampled once during 1993-1995 and once during 2001-2003. The networks provide an overview of conditions across a wide range of hydrogeologic settings and in major agricultural areas that vary in dominant crop type and pesticide use. Of about 80 pesticide compounds analyzed, only six compounds were detected in ground water from at least 10 wells during both sampling events. These compounds were the triazine herbicides atrazine, simazine, and prometon; the acetanilide herbicide metolachlor; the urea herbicide tebuthiuron; and an atrazine degradate, deethylatrazine (DEA). Observed concentrations of these compounds generally were <0.12 ??g L-1. At individual wells, changes in concentrations typically were <0.02 ??g L-1. Data analysis incorporated adjustments for changes in laboratory recovery as assessed through laboratory spikes. In wells yielding detectable concentrations of atrazine, DEA, and prometon, concentrations were significantly lower (?? = 0.1) in 2001-2003 than in 1993-1995, whereas detection frequency of these compounds did not change significantly. Trends in atrazine concentrations at shallow wells in agricultural areas were found to be consistent overall with recent atrazine use data. Copyright ?? 2008 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America. All rights reserved.","largerWorkTitle":"Journal of Environmental Quality","language":"English","doi":"10.2134/jeq2007.0054","issn":"00472425","usgsCitation":"Bexfield, L.M., 2008, Decadal-scale changes of pesticides in ground water of the United States, 1993-2003, <i>in</i> Journal of Environmental Quality, v. 37, no. SUPPL. 5, https://doi.org/10.2134/jeq2007.0054.","costCenters":[],"links":[{"id":204896,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2134/jeq2007.0054"},{"id":218924,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"SUPPL. 5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe00e4b0c8380cd4ea6f","contributors":{"authors":[{"text":"Bexfield, L. M.","contributorId":36593,"corporation":false,"usgs":true,"family":"Bexfield","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":357643,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009711,"text":"70009711 - 2008 - Efficacy of PIT tags for tracking the terrestrial anurans Rana pipiens and rana sylvatica","interactions":[],"lastModifiedDate":"2017-11-06T09:45:39","indexId":"70009711","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1898,"text":"Herpetological Review","active":true,"publicationSubtype":{"id":10}},"title":"Efficacy of PIT tags for tracking the terrestrial anurans Rana pipiens and rana sylvatica","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Herpetological Review","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0018084X","usgsCitation":"Blomquist, S.M., Zydlewski, J.D., and Hunter, M., 2008, Efficacy of PIT tags for tracking the terrestrial anurans Rana pipiens and rana sylvatica: Herpetological Review, v. 39, no. 2, p. 174-179.","startPage":"174","endPage":"179","numberOfPages":"6","costCenters":[],"links":[{"id":219178,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0855e4b0c8380cd51a9c","contributors":{"authors":[{"text":"Blomquist, S. M.","contributorId":103409,"corporation":false,"usgs":false,"family":"Blomquist","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":356925,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zydlewski, Joseph D. 0000-0002-2255-2303 jzydlewski@usgs.gov","orcid":"https://orcid.org/0000-0002-2255-2303","contributorId":2004,"corporation":false,"usgs":true,"family":"Zydlewski","given":"Joseph","email":"jzydlewski@usgs.gov","middleInitial":"D.","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true},{"id":365,"text":"Leetown Science Center","active":true,"usgs":true},{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":false,"id":356923,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hunter, M.L. Jr.","contributorId":91619,"corporation":false,"usgs":true,"family":"Hunter","given":"M.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":356924,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70009717,"text":"70009717 - 2008 - Regional nitrate and pesticide trends in ground water in the eastern San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2018-09-13T14:31:08","indexId":"70009717","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Regional nitrate and pesticide trends in ground water in the eastern San Joaquin Valley, California","docAbstract":"Protection of ground water for present and future use requires monitoring and understanding of the mechanisms controlling long-term quality of ground water. In this study, spatial and temporal trends in concentrations of nitrate and pesticides in ground water in the eastern San Joaquin Valley, California, were evaluated to determine the long-term effects of agricultural and urban development on regional ground-water quality. Trends in concentrations of nitrate, the nematocide 1,2-dibromo-3-chloropropane, and the herbicide simazine during the last two decades are generally consistent with known nitrogen fertilizer and pesticide use and with the position of the well networks in the regional ground-water flow system. Concentrations of nitrate and pesticides are higher in the shallow part of the aquifer system where domestic wells are typically screened, whereas concentrations are lower in the deep part of the aquifer system where public-supply wells are typically screened. Attenuation processes do not seem to significantly affect concentrations. Historical data indicate that concentrations of nitrate have increased since the 1950s in the shallow and deep parts of the aquifer system. Concentrations of nitrate and detection of pesticides in the deep part of the aquifer system will likely increase as the proportion of highly affected water contributed to these wells increases with time. Because of the time of travel between the water table and the deep part of the aquifer system, current concentrations in public-supply wells likely reflect the effects of 40- to 50-yr-old management practices. Copyright ?? 2008 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America. All rights reserved.","largerWorkTitle":"Journal of Environmental Quality","language":"English","doi":"10.2134/jeq2007.0061","issn":"00472425","usgsCitation":"Burow, K., Shelton, J.L., and Dubrovsky, N., 2008, Regional nitrate and pesticide trends in ground water in the eastern San Joaquin Valley, California, <i>in</i> Journal of Environmental Quality, v. 37, no. SUPPL. 5, https://doi.org/10.2134/jeq2007.0061.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":219325,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":204935,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2134/jeq2007.0061"}],"volume":"37","issue":"SUPPL. 5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a53de4b0e8fec6cdbdac","contributors":{"authors":[{"text":"Burow, K.R. 0000-0001-6006-6667","orcid":"https://orcid.org/0000-0001-6006-6667","contributorId":48283,"corporation":false,"usgs":true,"family":"Burow","given":"K.R.","affiliations":[],"preferred":false,"id":356942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shelton, James L.","contributorId":85319,"corporation":false,"usgs":false,"family":"Shelton","given":"James","email":"","middleInitial":"L.","affiliations":[{"id":13267,"text":"Warnell School of Forestry and Natural Resources, University of Georgia","active":true,"usgs":false}],"preferred":false,"id":356943,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dubrovsky, N. M.","contributorId":48199,"corporation":false,"usgs":true,"family":"Dubrovsky","given":"N. M.","affiliations":[],"preferred":false,"id":356941,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70191954,"text":"70191954 - 2008 - Instream flow assessment of streams draining the Arbuckle-Simpson Aquifer","interactions":[],"lastModifiedDate":"2018-01-25T14:38:19","indexId":"70191954","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Instream flow assessment of streams draining the Arbuckle-Simpson Aquifer","docAbstract":"<p>The availability of high quality water is critical to both humans and ecosystems. A recent proposal was made by rapidly expanding municipalities in central Oklahoma to begin transferring groundwater from the Arbuckle-Simpson aquifer, a sensitive sole-source aquifer in south-central Oklahoma. Concerned citizens and municipalities living on and getting their drinking water from the Arbuckle-Simpson lobbied the legislature to pass a temporary moratorium on groundwater transfer to allow for a comprehensive study of the aquifer and its ecosystems. We conducted an instream flow assessment using Physical Habitat Simulation (PHABSIM) on springs and streams with four spring-dependent species: two minnows, southern redbelly dace (Phoxinus erthyrogaster) and redspot chub (Nocomis asper); and two darters, least darter (Etheostoma microperca) and orangethroat darter (Etheostoma spectabile). Spring habitats are unique compared to other river habitats because they have constant flow and temperature, small and isolated habitat patches, and a general lack of predators. </p><p>Our study sites included two spring-fed streams, one larger stream with high groundwater inputs, and a river with both groundwater and surface water inputs that is adjacent to the small spring-fed streams. These habitats meet the criteria for groundwater dependent ecosystems because they would not exist without the surface expression of groundwater. A total of 99 transects in all four sites were surveyed for channel elevation, and three sets of water surface elevation and water velocity were measured. Habitat suitability criteria were derived for the species at each site using nonparametric confidence limits based on underwater observations made by snorkelers. Simulations of flow were focused on declines in discharge, which is the expected effect of the proposed groundwater diversion. </p><p>Our results show that only a small proportion of the total available area in each habitat is considered to be preferred habitat (Weighted Usable Area [WUA]) by the four target species. In the spring habitats, a maximum of 10% of the total area is preferred habitat and that dropped to as little as 3% with decreased flows. The quantity of WUA decreased when lower discharges were simulated for all the target species. Declines in the small amount of habitat that is already available would likely degrade these populations of fishes. In the larger river habitat, the highest WUA occurred at the lowest discharge, which leads us to conclude that in the event of dewatering of the spring habitats, the river should provide some refuge habitat for spring dependent species. </p><p>Based on the findings of this study, groundwater removal from the aquifer near springs may have adverse impacts on fish habitat availability for spring dependent fish populations if seasonal trends in spring discharge are not maintained (higher in winter and lower in late summer). Quantifying the relationship of streamflow between gaged and ungaged springs in the Arbuckle-Simpson is a possible method to monitor and maintain flows in springs. </p>","language":"English","usgsCitation":"Seilheimer, T.S., and Fisher, W.L., 2008, Instream flow assessment of streams draining the Arbuckle-Simpson Aquifer, 49 p.","productDescription":"49 p.","ipdsId":"IP-009159","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":350624,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350623,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.owrb.ok.gov/studies/groundwater/arbuckle_simpson/pdf/Arbuckle-SimpsonInstreamFlow.pdf"}],"publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a6afacae4b06e28e9c9a92a","contributors":{"authors":[{"text":"Seilheimer, Titus S.","contributorId":50772,"corporation":false,"usgs":true,"family":"Seilheimer","given":"Titus","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":725828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, William L. wfisher@usgs.gov","contributorId":1229,"corporation":false,"usgs":true,"family":"Fisher","given":"William","email":"wfisher@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":713778,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003972,"text":"1003972 - 2008 - Cutaneous and diphtheritic avian poxvirus infection in a nestling Southern Giant Petrel (Macronectes giganteus) from Antarctica","interactions":[],"lastModifiedDate":"2023-10-20T15:15:15.551683","indexId":"1003972","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3093,"text":"Polar Biology","active":true,"publicationSubtype":{"id":10}},"title":"Cutaneous and diphtheritic avian poxvirus infection in a nestling Southern Giant Petrel (Macronectes giganteus) from Antarctica","docAbstract":"<p><span>The Southern giant petrel (</span><i>Macronectes giganteus</i><span>) is declining over much of its range and currently is listed as vulnerable to extinction by the International Union for the Conservation of Nature (IUCN). Island-specific breeding colonies near Palmer Station, Antarctica, have been monitored for over 30&nbsp;years, and because this population continues to increase, it is critically important to conservation. In austral summer 2004, six diseased giant petrel chicks were observed in four of these colonies. Diseased chicks were 6–9&nbsp;weeks old and had multiple proliferative nodules on their bills and skin. One severely affected chick was found dead on the nest and was salvaged for necropsy. Histopathological examination of nodules from the dead chick revealed epithelial cell hyperplasia and hypertrophy with numerous eosinophilic intracytoplasmic inclusions (Böllinger bodies). A poxvirus was isolated from multiple nodules. Poxviral infection has not been reported in this species, and the reason for its emergence and its potential impact on the population are not yet known.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s00300-007-0390-z","usgsCitation":"Shearn-Bochsler, V., Green, D.E., Converse, K.A., Docherty, D.E., Thiel, T., Geisz, H., Fraser, W., and Patterson-Fraser, D.L., 2008, Cutaneous and diphtheritic avian poxvirus infection in a nestling Southern Giant Petrel (Macronectes giganteus) from Antarctica: Polar Biology, v. 31, no. 5, p. 569-573, https://doi.org/10.1007/s00300-007-0390-z.","productDescription":"5 p.","startPage":"569","endPage":"573","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":422013,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Antarctica: Palmer Station","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -64.07432556152342,\n              -64.74264817735076\n            ],\n            [\n              -64.00909423828125,\n              -64.74689607086069\n            ],\n            [\n              -63.98128509521485,\n              -64.75407202924025\n            ],\n            [\n              -63.95347595214844,\n              -64.76358821744012\n            ],\n            [\n              -63.94969940185546,\n              -64.77339370305394\n            ],\n            [\n              -63.94729614257812,\n              -64.78304935691033\n            ],\n            [\n              -63.95759582519532,\n              -64.79767255432083\n            ],\n            [\n              -63.97819519042968,\n              -64.81038828842998\n            ],\n            [\n              -64.0396499633789,\n              -64.817547383571\n            ],\n            [\n              -64.13887023925781,\n              -64.81082665504367\n            ],\n            [\n              -64.1550064086914,\n              -64.80264263569762\n            ],\n            [\n              -64.15225982666014,\n              -64.79211667318563\n            ],\n            [\n              -64.14676666259766,\n              -64.77558847319227\n            ],\n            [\n              -64.13440704345703,\n              -64.7612460821597\n            ],\n            [\n              -64.11003112792969,\n              -64.75260770270529\n            ],\n            [\n              -64.07432556152342,\n              -64.74264817735076\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"31","issue":"5","noUsgsAuthors":false,"publicationDate":"2007-11-20","publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ec2d","contributors":{"authors":[{"text":"Shearn-Bochsler, Valerie","contributorId":43322,"corporation":false,"usgs":true,"family":"Shearn-Bochsler","given":"Valerie","affiliations":[],"preferred":false,"id":314781,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, David Earl","contributorId":106052,"corporation":false,"usgs":true,"family":"Green","given":"David","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":314788,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Converse, K. A.","contributorId":81436,"corporation":false,"usgs":true,"family":"Converse","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":314784,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Docherty, D. E.","contributorId":83469,"corporation":false,"usgs":true,"family":"Docherty","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":314785,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Thiel, T.","contributorId":80241,"corporation":false,"usgs":true,"family":"Thiel","given":"T.","email":"","affiliations":[],"preferred":false,"id":314783,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Geisz, H.N.","contributorId":58615,"corporation":false,"usgs":true,"family":"Geisz","given":"H.N.","email":"","affiliations":[],"preferred":false,"id":314782,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Fraser, William R.","contributorId":94277,"corporation":false,"usgs":true,"family":"Fraser","given":"William R.","affiliations":[],"preferred":false,"id":314787,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Patterson-Fraser, Donna L.","contributorId":84726,"corporation":false,"usgs":true,"family":"Patterson-Fraser","given":"Donna","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":314786,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70033556,"text":"70033556 - 2008 - Infrared (0.83–5.1 μm)  photometry of Phoebe from the <i>Cassini</i> Visual Infrared Mapping Spectrometer","interactions":[],"lastModifiedDate":"2015-04-01T13:21:32","indexId":"70033556","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Infrared (0.83–5.1 μm)  photometry of Phoebe from the <i>Cassini</i> Visual Infrared Mapping Spectrometer","docAbstract":"<p>Three weeks prior to the commencement of <i>Cassini's &nbsp;</i> 4 year tour of the saturnian system, the spacecraft executed a close flyby of the outer satellite Phoebe. The infrared channel of the Visual Infrared Mapping Spectrometer (VIMS) obtained images of reflected light over the 0.83&ndash;5.1 &mu;m spectral range with an average spectral resolution of 16.5 nm, spatial resolution up to 2 km, and over a range of solar phase angles not observed before. These images have been analyzed to derive fundamental photometric parameters including the phase curve and phase integral, spectral geometric albedo, bolometric Bond albedo, and the single scattering albedo. Physical properties of the surface, including macroscopic roughness and the single particle phase function, have also been characterized. Maps of normal reflectance show the existence of two major albedo regimes in the infrared, with gradations between the two regimes and much terrain with substantially higher albedos. The phase integral of Phoebe is <span id=\"mmlsi1\" class=\"mathmlsrc\"><span class=\"formulatext stixSupport mathImg\" title=\"Click to view the MathML source\" data-mathurl=\"/science?_ob=MathURL&amp;_method=retrieve&amp;_eid=1-s2.0-S0019103507004642&amp;_mathId=si1.gif&amp;_user=111111111&amp;_pii=S0019103507004642&amp;_rdoc=1&amp;_issn=00191035&amp;md5=dcfb10a036b31bfb4cf4da39c0b0bfff\">0.29&plusmn;0.03</span><span class=\"mathContainer hidden\"><span class=\"mathCode\">0.29&plusmn;0.03</span></span></span>, with no significant wavelength dependence. The bolometric Bond albedo is <span id=\"mmlsi2\" class=\"mathmlsrc\"><span class=\"formulatext stixSupport mathImg\" title=\"Click to view the MathML source\" data-mathurl=\"/science?_ob=MathURL&amp;_method=retrieve&amp;_eid=1-s2.0-S0019103507004642&amp;_mathId=si2.gif&amp;_user=111111111&amp;_pii=S0019103507004642&amp;_rdoc=1&amp;_issn=00191035&amp;md5=d6f43e2b738181e6c5c1c3e99c81334e\">0.023&plusmn;007</span><span class=\"mathContainer hidden\"><span class=\"mathCode\">0.023&plusmn;007</span></span></span>. We find that the surface of Phoebe is rough, with a mean slope angle of 33&deg;. The satellite's surface has a substantial forward scattering component, suggesting that its surface is dusty, perhaps from a history of outgassing. The spectrum of Phoebe is best matched by a composition including water ice, amorphous carbon, iron-bearing minerals, carbon dioxide, and Triton tholin. The characteristics of Phoebe suggest that it originated outside the saturnian system, perhaps in the Kuiper Belt, and was captured on its journey inward, as suggested by <span id=\"bbib032\"><a id=\"ancbbib032\" class=\"intra_ref\" href=\"http://www.sciencedirect.com/science/article/pii/S0019103507004642#bib032\">Johnson and Lunine (2005)</a></span>.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.icarus.2007.09.014","issn":"00191035","usgsCitation":"Buratti, B.J., Soderlund, K., Bauer, J., Mosher, J.A., Hicks, M., Simonelli, D., Jaumann, R., Clark, R.N., Brown, R.H., Cruikshank, D.P., and Momary, T., 2008, Infrared (0.83–5.1 μm)  photometry of Phoebe from the <i>Cassini</i> Visual Infrared Mapping Spectrometer: Icarus, v. 193, no. 2, p. 309-322, https://doi.org/10.1016/j.icarus.2007.09.014.","productDescription":"14 p.","startPage":"309","endPage":"322","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":242282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214547,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.icarus.2007.09.014"}],"otherGeospatial":"Phoebe","volume":"193","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3bbde4b0c8380cd627dd","contributors":{"authors":[{"text":"Buratti, B. J.","contributorId":69280,"corporation":false,"usgs":false,"family":"Buratti","given":"B.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":441428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Soderlund, K.","contributorId":80883,"corporation":false,"usgs":true,"family":"Soderlund","given":"K.","email":"","affiliations":[],"preferred":false,"id":441429,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bauer, J.","contributorId":85400,"corporation":false,"usgs":true,"family":"Bauer","given":"J.","affiliations":[],"preferred":false,"id":441431,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mosher, J. A.","contributorId":34605,"corporation":false,"usgs":false,"family":"Mosher","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":441425,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hicks, M.D.","contributorId":7045,"corporation":false,"usgs":true,"family":"Hicks","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":441422,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Simonelli, D.P.","contributorId":42373,"corporation":false,"usgs":true,"family":"Simonelli","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":441426,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Jaumann, R.","contributorId":81232,"corporation":false,"usgs":false,"family":"Jaumann","given":"R.","email":"","affiliations":[],"preferred":false,"id":441430,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Clark, R. N.","contributorId":6568,"corporation":false,"usgs":true,"family":"Clark","given":"R.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":441421,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Brown, R. H.","contributorId":19931,"corporation":false,"usgs":false,"family":"Brown","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":441424,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Cruikshank, D. P.","contributorId":51434,"corporation":false,"usgs":false,"family":"Cruikshank","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":441427,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Momary, T.","contributorId":17415,"corporation":false,"usgs":true,"family":"Momary","given":"T.","affiliations":[],"preferred":false,"id":441423,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70032051,"text":"70032051 - 2008 - The effect of acid rain and altitude on concentration, δ34S, and δ18O of sulfate in the water from Sudety Mountains, Poland","interactions":[],"lastModifiedDate":"2015-04-02T12:53:31","indexId":"70032051","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"The effect of acid rain and altitude on concentration, δ34S, and δ18O of sulfate in the water from Sudety Mountains, Poland","docAbstract":"<p id=\"\">The analyses of sulfate content,&nbsp;<i>&delta;</i><sup>34</sup>S and&nbsp;<i>&delta;</i><sup>18</sup>O of dissolved sulfate, and&nbsp;<i>&delta;</i><sup>18</sup>O of water were carried out in a 14&nbsp;km<sup>2</sup>&nbsp;crystalline massif located in the Sudety Mountains (SW Poland) to 1) assess the amount of the sulfate delivered to the surface and groundwater systems by modern atmospheric precipitation, 2) determine the effect of altitude on these parameters, and 3) investigate their seasonal variations. In April and November of 2002, August 2003, and March and September of 2005, samples of water were collected from springs and streams of the massif. During these seasons, sulfate contents and&nbsp;<i>&delta;</i><sup>18</sup>O(SO<sub>4</sub><sup>2&minus;</sup>) values varied from 5.80 to 18.00&nbsp;mg/l and from 3.96 to 8.23&permil;, respectively, showing distinctively higher values of<i>&delta;</i><sup>18</sup>O(SO<sub>4</sub><sup>2&minus;</sup>) in wet seasons. The&nbsp;<i>&delta;</i><sup>34</sup>S(SO<sub>4</sub><sup>2&minus;</sup>) values had a relatively narrow range from 4.09 to 5.28&permil; and were similar to those reported for organic matter in soil and the canopy throughfall in the Sudety Mountains.</p>\n<p id=\"\">Sulfate content,&nbsp;<i>&delta;</i><sup>34</sup>S(SO<sub>4</sub><sup>2&minus;</sup>),&nbsp;<i>&delta;</i><sup>18</sup>O(SO<sub>4</sub><sup>2&minus;</sup>), and &delta;<sup>18</sup>O(H<sub>2</sub>O) values revealed a remarkable dependence on the altitude. The calculated altitude effects for five season averages of these parameters were &minus;&nbsp;1.00&nbsp;mg/l/100&nbsp;m, &minus;&nbsp;0.18&permil;/100&nbsp;m, &minus;&nbsp;0.27&permil;/100&nbsp;m, and &minus;&nbsp;0.17&permil;/100&nbsp;m, respectively. This dependence on the altitude resulted mainly from the mixing of sulfates of different origins such as anthropogenic sulfate, sulfate produced in the soil within the weathered zone of the massif, and that one from the tree canopy. The oxygen isotope mass balance indicates that, in the study area, about one third of the sulfate delivered to the surface and groundwater by modern precipitation comes from anthropogenic pollution. Further interaction of meteoric water within the weathered rocks causes a continuous decrease of &delta;<sup>18</sup>O(SO<sub>4</sub><sup>2&minus;</sup>) values resulting from biological transformation of the sulfate due to plant vegetation and decomposition of organic matter.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.chemgeo.2007.11.006","issn":"00092541","usgsCitation":"Szynkiewicz, A., Modelska, M., Jedrysek, M.O., and Mastalerz, M., 2008, The effect of acid rain and altitude on concentration, δ34S, and δ18O of sulfate in the water from Sudety Mountains, Poland: Chemical Geology, v. 249, no. 1-2, p. 36-51, https://doi.org/10.1016/j.chemgeo.2007.11.006.","productDescription":"16 p.","startPage":"36","endPage":"51","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":242466,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214717,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2007.11.006"}],"country":"Poland","otherGeospatial":"Sudety Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              16.5234375,\n              50.04302974380058\n            ],\n            [\n              16.5234375,\n              50.44351305245805\n            ],\n            [\n              16.864013671875,\n              50.44351305245805\n            ],\n            [\n              16.864013671875,\n              50.04302974380058\n            ],\n            [\n              16.5234375,\n              50.04302974380058\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"249","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bab13e4b08c986b322bd4","contributors":{"authors":[{"text":"Szynkiewicz, Anna","contributorId":39599,"corporation":false,"usgs":true,"family":"Szynkiewicz","given":"Anna","email":"","affiliations":[],"preferred":false,"id":434321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Modelska, Magdalena","contributorId":64045,"corporation":false,"usgs":true,"family":"Modelska","given":"Magdalena","email":"","affiliations":[],"preferred":false,"id":434322,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jedrysek, Mariusz Orion","contributorId":94513,"corporation":false,"usgs":true,"family":"Jedrysek","given":"Mariusz","email":"","middleInitial":"Orion","affiliations":[],"preferred":false,"id":434324,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mastalerz, Maria","contributorId":105788,"corporation":false,"usgs":false,"family":"Mastalerz","given":"Maria","affiliations":[{"id":17608,"text":"Indiana Univesity","active":true,"usgs":false}],"preferred":false,"id":434323,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70032046,"text":"70032046 - 2008 - Chlorinated, brominated, and perfluorinated compounds, polycyclic aromatic hydrocarbons and trace elements in livers of sea otters from California, Washington, and Alaska (USA), and Kamchatka (Russia)","interactions":[],"lastModifiedDate":"2023-10-24T10:55:08.36997","indexId":"70032046","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2259,"text":"Journal of Environmental Monitoring","active":true,"publicationSubtype":{"id":10}},"title":"Chlorinated, brominated, and perfluorinated compounds, polycyclic aromatic hydrocarbons and trace elements in livers of sea otters from California, Washington, and Alaska (USA), and Kamchatka (Russia)","docAbstract":"<p>Concentrations of organochlorine pesticides (DDTs, HCHs, and chlordanes), polychlorinated biphenyls (PCBs), polybrominated diphenyl ethers (PBDEs), polycyclic aromatic hydrocarbons (PAHs), perfluorinated compounds (PFCs), and 20 trace elements were determined in livers of 3- to 5-year old stranded sea otters collected from the coastal waters of California, Washington, and Alaska (USA) and from Kamchatka (Russia). Concentrations of organochlorine pesticides, PCBs, and PBDEs were high in sea otters collected from the California coast. Concentrations of DDTs were 10-fold higher in California sea otters than in otters from other locations; PCB concentrations were 5-fold higher, and PBDE concentrations were 2-fold higher, in California sea otters than in otters from other locations. Concentrations of PAHs were higher in sea otters from Prince William Sound than in sea otters from other locations. Concentrations of several trace elements were elevated in sea otters collected from California and Prince William Sound. Elevated concentrations of Mn and Zn in sea otters from California and Prince William Sound were indicative of oxidative stress-related injuries in these two populations. Concentrations of all of the target compounds, including trace elements, that were analyzed in sea otters from Kamchatka were lower than those found from the US coastal locations.&nbsp;</p>","language":"English","publisher":"Royal Society of Chemistry","doi":"10.1039/b718596k","issn":"14640325","usgsCitation":"Kannan, K., Moon, H., Yun, S., Agusa, T., Thomas, N., and Tanabe, S., 2008, Chlorinated, brominated, and perfluorinated compounds, polycyclic aromatic hydrocarbons and trace elements in livers of sea otters from California, Washington, and Alaska (USA), and Kamchatka (Russia): Journal of Environmental Monitoring, v. 10, no. 4, p. 552-558, https://doi.org/10.1039/b718596k.","productDescription":"7 p.","startPage":"552","endPage":"558","numberOfPages":"7","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-008083","costCenters":[{"id":456,"text":"National Wildlife Health 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T.","contributorId":60605,"corporation":false,"usgs":true,"family":"Agusa","given":"T.","email":"","affiliations":[],"preferred":false,"id":434300,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Thomas, N. J. 0000-0002-0161-0391","orcid":"https://orcid.org/0000-0002-0161-0391","contributorId":49731,"corporation":false,"usgs":true,"family":"Thomas","given":"N. J.","affiliations":[],"preferred":false,"id":434298,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tanabe, S.","contributorId":93005,"corporation":false,"usgs":true,"family":"Tanabe","given":"S.","email":"","affiliations":[],"preferred":false,"id":434302,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70031826,"text":"70031826 - 2008 - Storm-driven sediment transport in Massachusetts Bay","interactions":[],"lastModifiedDate":"2017-09-27T14:46:01","indexId":"70031826","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1333,"text":"Continental Shelf Research","active":true,"publicationSubtype":{"id":10}},"title":"Storm-driven sediment transport in Massachusetts Bay","docAbstract":"Massachusetts Bay is a semi-enclosed embayment in the western Gulf of Maine about 50 km wide and 100 km long. Bottom sediment resuspension is controlled predominately by storm-induced surface waves and transport by the tidal- and wind-driven circulation. Because the Bay is open to the northeast, winds from the northeast ('Northeasters') generate the largest surface waves and are thus the most effective in resuspending sediments. The three-dimensional oceanographic circulation model Regional Ocean Modeling System (ROMS) is used to explore the resuspension, transport, and deposition of sediment caused by Northeasters. The model transports multiple sediment classes and tracks the evolution of a multilevel sediment bed. The surficial sediment characteristics of the bed are coupled to one of several bottom-boundary layer modules that calculate enhanced bottom roughness due to wave-current interaction. The wave field is calculated from the model Simulating WAves Nearshore (SWAN). Two idealized simulations were carried out to explore the effects of Northeasters on the transport and fate of sediments. In one simulation, an initially spatially uniform bed of mixed sediments exposed to a series of Northeasters evolved to a pattern similar to the existing surficial sediment distribution. A second set of simulations explored sediment-transport pathways caused by storms with winds from the northeast quadrant by simulating release of sediment at selected locations. Storms with winds from the north cause transport southward along the western shore of Massachusetts Bay, while storms with winds from the east and southeast drive northerly nearshore flow. The simulations show that Northeasters can effectively transport sediments from Boston Harbor and the area offshore of the harbor to the southeast into Cape Cod Bay and offshore into Stellwagen Basin. This transport pattern is consistent with Boston Harbor as the source of silver found in the surficial sediments of Cape Cod Bay and Stellwagen Basin.","language":"English","publisher":"Elsevier","doi":"10.1016/j.csr.2007.08.008","issn":"02784343","usgsCitation":"Warner, J., Butman, B., and Dalyander, P., 2008, Storm-driven sediment transport in Massachusetts Bay: Continental Shelf Research, v. 28, no. 2, p. 257-282, https://doi.org/10.1016/j.csr.2007.08.008.","productDescription":"26 p.","startPage":"257","endPage":"282","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":476821,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/1912/2103","text":"External Repository"},{"id":242650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod Bay, Gulf of Maine, Massachusetts Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71,\n              41.590796851056005\n            ],\n            [\n              -69.89501953125,\n              41.590796851056005\n            ],\n            [\n              -69.89501953125,\n              42.924251753870685\n            ],\n            [\n              -71,\n              42.924251753870685\n            ],\n            [\n              -71,\n              41.590796851056005\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"28","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b987de4b08c986b31c061","contributors":{"authors":[{"text":"Warner, J.C.","contributorId":46644,"corporation":false,"usgs":true,"family":"Warner","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":433302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butman, B.","contributorId":85580,"corporation":false,"usgs":true,"family":"Butman","given":"B.","email":"","affiliations":[],"preferred":false,"id":433304,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dalyander, P.S. 0000-0001-9583-0872","orcid":"https://orcid.org/0000-0001-9583-0872","contributorId":68968,"corporation":false,"usgs":true,"family":"Dalyander","given":"P.S.","affiliations":[],"preferred":false,"id":433303,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031987,"text":"70031987 - 2008 - Assessment of crop growth and soil water modules in SWAT2000 using extensive field experiment data in an irrigation district of the Yellow River Basin","interactions":[],"lastModifiedDate":"2012-03-12T17:21:28","indexId":"70031987","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","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":"Assessment of crop growth and soil water modules in SWAT2000 using extensive field experiment data in an irrigation district of the Yellow River Basin","docAbstract":"SWAT, a physically-based, hydrological model simulates crop growth, soil water and groundwater movement, and transport of sediment and nutrients at both the process and watershed scales. While the different versions of SWAT have been widely used throughout the world for agricultural and water resources applications, little has been done to test the performance, variability, and transferability of the parameters in the crop growth, soil water, and groundwater modules in an integrated way with multiple sets of field experimental data at the process scale. Using an multiple years of field experimental data of winter wheat (Triticum aestivum L.) in the irrigation district of the Yellow River Basin, this paper assesses the performance of the plant-soil-groundwater modules and the variability and transferability of SWAT2000. Comparison of the simulated results by SWAT to the observations showed that SWAT performed quite unsatisfactorily in LAI predictions during the senescence stage, in yield predictions, and in soil-water estimation under dry soil-profile conditions. The unsatisfactory performance in LAI prediction might be attributed to over-simplified senescence modeling; in yield prediction to the improper computation of the harvest index; and in soil water under dry conditions to the exclusion of groundwater evaporation from the soil water balance in SWAT. In this paper, improvements in crop growth, soil water, and groundwater modules in SWAT were implemented. The saturated soil profile was coupled to the oscillating groundwater table. A variable evaporation coefficient taking into account soil water deficit index, groundwater depth, and crop root depth was used to replace the fixed coefficient in computing groundwater evaporation. The soil water balance included the groundwater evaporation. The modifications improved simulations of crop evapotranspiration and biomass as well as soil water dynamics under dry soil-profile conditions. The evaluation shows that the crop growth and soil water components of SWAT could be further refined to better simulate the hydrology of agricultural watersheds. ?? 2008 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jhydrol.2008.01.003","issn":"00221694","usgsCitation":"Luo, Y., He, C., Sophocleous, M., Yin, Z., Hongrui, R., and Ouyang, Z., 2008, Assessment of crop growth and soil water modules in SWAT2000 using extensive field experiment data in an irrigation district of the Yellow River Basin: Journal of Hydrology, v. 352, no. 1-2, p. 139-156, https://doi.org/10.1016/j.jhydrol.2008.01.003.","startPage":"139","endPage":"156","numberOfPages":"18","costCenters":[],"links":[{"id":242495,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214745,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhydrol.2008.01.003"}],"volume":"352","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ee2ae4b0c8380cd49bd3","contributors":{"authors":[{"text":"Luo, Y.","contributorId":28417,"corporation":false,"usgs":true,"family":"Luo","given":"Y.","email":"","affiliations":[],"preferred":false,"id":434006,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"He, C.","contributorId":76951,"corporation":false,"usgs":true,"family":"He","given":"C.","email":"","affiliations":[],"preferred":false,"id":434009,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sophocleous, M.","contributorId":13373,"corporation":false,"usgs":true,"family":"Sophocleous","given":"M.","email":"","affiliations":[],"preferred":false,"id":434005,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yin, Z.","contributorId":108077,"corporation":false,"usgs":true,"family":"Yin","given":"Z.","email":"","affiliations":[],"preferred":false,"id":434010,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hongrui, R.","contributorId":34340,"corporation":false,"usgs":true,"family":"Hongrui","given":"R.","email":"","affiliations":[],"preferred":false,"id":434008,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ouyang, Z.","contributorId":28815,"corporation":false,"usgs":true,"family":"Ouyang","given":"Z.","email":"","affiliations":[],"preferred":false,"id":434007,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70031951,"text":"70031951 - 2008 - Palila (Loxioides bailleui) fledgling fed by Hawai'i 'Amakihi (Hemignathus virens)","interactions":[],"lastModifiedDate":"2012-03-12T17:21:27","indexId":"70031951","displayToPublicDate":"2008-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3784,"text":"Wilson Journal of Ornithology","active":true,"publicationSubtype":{"id":10}},"title":"Palila (Loxioides bailleui) fledgling fed by Hawai'i 'Amakihi (Hemignathus virens)","docAbstract":"We observed an adult male Hawai'i 'Amakihi (Hemignathus virens) repeatedly feed a fledgling Palila (Loxioides bailleui). We observed 16-19 food provisions during 14 hrs of observation between 21 and 29 June 2006. The presumed biological parents were frequently seen nearby, but adult Palila were not observed feeding the fledgling.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wilson Journal of Ornithology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1676/07-070.1","issn":"15594491","usgsCitation":"Farmer, C., Frederick, B., Banko, P., Stephens, R., and Snow, C., 2008, Palila (Loxioides bailleui) fledgling fed by Hawai'i 'Amakihi (Hemignathus virens): Wilson Journal of Ornithology, v. 120, no. 2, p. 416-418, https://doi.org/10.1676/07-070.1.","startPage":"416","endPage":"418","numberOfPages":"3","costCenters":[],"links":[{"id":242493,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214743,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1676/07-070.1"}],"volume":"120","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7477e4b0c8380cd7766b","contributors":{"authors":[{"text":"Farmer, C.","contributorId":20995,"corporation":false,"usgs":true,"family":"Farmer","given":"C.","affiliations":[],"preferred":false,"id":433852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frederick, B.A.","contributorId":94119,"corporation":false,"usgs":true,"family":"Frederick","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":433854,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Banko, P.C. 0000-0002-6035-9803","orcid":"https://orcid.org/0000-0002-6035-9803","contributorId":99531,"corporation":false,"usgs":true,"family":"Banko","given":"P.C.","affiliations":[],"preferred":false,"id":433855,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stephens, R.M.","contributorId":103482,"corporation":false,"usgs":true,"family":"Stephens","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":433856,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Snow, C.W.","contributorId":32743,"corporation":false,"usgs":true,"family":"Snow","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":433853,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
]}