FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1945573259> ?p ?o ?g. }

• W1945573259 abstract "First posted August 6, 2015 For additional information, contact: Director, Crustal Geophysics and Geochemistry Science Center U.S. Geological Survey Box 25046, MS 964 Denver, CO 80225http://crustal.usgs.gov/ In 2010, Utah Department of Environmental Quality (DEQ) Division of Water Quality (UDWQ, 2010) determined that water quality in Pariette Draw was in violation of Federal and State water quality criteria for total dissolved solids (TDS), selenium (Se), and boron (B). The measure of total dissolved solids is the sum of all the major ion concentrations in solution and in this case, the dominant ions are sodium (Na) and sulfate (SO4), which can form salts like thenardite (Na2SO4) and mirabilite (Na2SO4⋅H2O). The Utah Department of Environmental Quality (2010) classified the contamination as natural background and from nonpoint sources related to regional lithology and irrigation practices. Although the daily loads of the constituents of concern and water chemistry have been characterized for parts of the watershed, little is known about the controls that bedrock and soil mineralogy have on salt, Se, and B storage and the water-rock interactions that influence the mobility of these components in ground and surface waters. Studies in the Uncompahgre River watershed in Colorado by Tuttle and others (2014a, 2014b) show that salt derived from weathering of shale in a semiarid climate is stored in a variety of minerals that contribute solutes to runoff and surface waters based on a complex set of conditions such as water availability, geomorphic position (for example, topography controls the depth of salt accumulation in soils), water-table fluctuations, redox conditions, mineral dissolution kinetics, ion-exchange reactions, and secondary mineral formation. Elements like Se and B commonly reside in soluble salt phases, so knowledge of the behavior of salt minerals also sheds light on the behavior of associated contaminants. The goal of this study was to establish a process-based understanding of salt, Se, and B behavior to address whether these contaminants can be better managed, or if uncontrollable natural processes will overwhelm any attempts to bring Pariette Draw into compliance with respect to recently established total maximum daily limits (TMDLs). We collected data to refine our knowledge about the role of rock weathering and soil formation in the transport and storage of salt in the watershed and to show how salt is cycled under irrigated and natural conditions. Our approach was to sample rock, soils, and sediment on irrigated and natural terrain for mineralogical analysis to determine the residence of salt and associated Se and B, classify minerals as primary (related to rock formation) or secondary weathering products, and characterize mineral dissolution kinetics. Mineral and chemical analyses and selective extractions of rocks and soils provide useful information in understanding solute movement and mineral dissolution/ formation. The resulting data are critical in determining residence of salt, Se, and B in weathered rock and soil and understanding the mobility during water-rock-soil interactions. This report summarizes our methods for sample and data collection and tabulates the mineral, chemical, and isotopic data collected." @default.
• W1945573259 created "2016-06-24" @default.
• W1945573259 creator A5018083581 @default.
• W1945573259 creator A5075280069 @default.
• W1945573259 creator A5087164465 @default.
• W1945573259 date "2015-01-01" @default.
• W1945573259 modified "2023-09-27" @default.
• W1945573259 title "Results of mineral, chemical, and sulfate isotopic analyses of water, soil, rocks, and soil extracts from the Pariette Draw Watershed, Uinta Basin, Utah" @default.
• W1945573259 doi "https://doi.org/10.3133/ofr20151132" @default.
• W1945573259 hasPublicationYear "2015" @default.
• W1945573259 type Work @default.
• W1945573259 sameAs 1945573259 @default.
• W1945573259 citedByCount "0" @default.
• W1945573259 crossrefType "journal-article" @default.
• W1945573259 hasAuthorship W1945573259A5018083581 @default.
• W1945573259 hasAuthorship W1945573259A5075280069 @default.
• W1945573259 hasAuthorship W1945573259A5087164465 @default.
• W1945573259 hasBestOaLocation W19455732591 @default.
• W1945573259 hasConcept C114793014 @default.
• W1945573259 hasConcept C119857082 @default.
• W1945573259 hasConcept C122792734 @default.
• W1945573259 hasConcept C126645576 @default.
• W1945573259 hasConcept C127313418 @default.
• W1945573259 hasConcept C129360787 @default.
• W1945573259 hasConcept C137527640 @default.
• W1945573259 hasConcept C150547873 @default.
• W1945573259 hasConcept C159390177 @default.
• W1945573259 hasConcept C159750122 @default.
• W1945573259 hasConcept C17409809 @default.
• W1945573259 hasConcept C178790620 @default.
• W1945573259 hasConcept C185592680 @default.
• W1945573259 hasConcept C187320778 @default.
• W1945573259 hasConcept C18903297 @default.
• W1945573259 hasConcept C205649164 @default.
• W1945573259 hasConcept C2778343803 @default.
• W1945573259 hasConcept C2780797713 @default.
• W1945573259 hasConcept C39432304 @default.
• W1945573259 hasConcept C40724407 @default.
• W1945573259 hasConcept C41008148 @default.
• W1945573259 hasConcept C50477045 @default.
• W1945573259 hasConcept C58640448 @default.
• W1945573259 hasConcept C76177295 @default.
• W1945573259 hasConcept C76886044 @default.
• W1945573259 hasConcept C8625798 @default.
• W1945573259 hasConcept C86803240 @default.
• W1945573259 hasConcept C87717796 @default.
• W1945573259 hasConceptScore W1945573259C114793014 @default.
• W1945573259 hasConceptScore W1945573259C119857082 @default.
• W1945573259 hasConceptScore W1945573259C122792734 @default.
• W1945573259 hasConceptScore W1945573259C126645576 @default.
• W1945573259 hasConceptScore W1945573259C127313418 @default.
• W1945573259 hasConceptScore W1945573259C129360787 @default.
• W1945573259 hasConceptScore W1945573259C137527640 @default.
• W1945573259 hasConceptScore W1945573259C150547873 @default.
• W1945573259 hasConceptScore W1945573259C159390177 @default.
• W1945573259 hasConceptScore W1945573259C159750122 @default.
• W1945573259 hasConceptScore W1945573259C17409809 @default.
• W1945573259 hasConceptScore W1945573259C178790620 @default.
• W1945573259 hasConceptScore W1945573259C185592680 @default.
• W1945573259 hasConceptScore W1945573259C187320778 @default.
• W1945573259 hasConceptScore W1945573259C18903297 @default.
• W1945573259 hasConceptScore W1945573259C205649164 @default.
• W1945573259 hasConceptScore W1945573259C2778343803 @default.
• W1945573259 hasConceptScore W1945573259C2780797713 @default.
• W1945573259 hasConceptScore W1945573259C39432304 @default.
• W1945573259 hasConceptScore W1945573259C40724407 @default.
• W1945573259 hasConceptScore W1945573259C41008148 @default.
• W1945573259 hasConceptScore W1945573259C50477045 @default.
• W1945573259 hasConceptScore W1945573259C58640448 @default.
• W1945573259 hasConceptScore W1945573259C76177295 @default.
• W1945573259 hasConceptScore W1945573259C76886044 @default.
• W1945573259 hasConceptScore W1945573259C8625798 @default.
• W1945573259 hasConceptScore W1945573259C86803240 @default.
• W1945573259 hasConceptScore W1945573259C87717796 @default.
• W1945573259 hasLocation W19455732591 @default.
• W1945573259 hasOpenAccess W1945573259 @default.
• W1945573259 hasPrimaryLocation W19455732591 @default.
• W1945573259 hasRelatedWork W1535395247 @default.
• W1945573259 hasRelatedWork W2055705976 @default.
• W1945573259 hasRelatedWork W2146657169 @default.
• W1945573259 hasRelatedWork W2276323009 @default.
• W1945573259 hasRelatedWork W2392512544 @default.
• W1945573259 hasRelatedWork W2521692511 @default.
• W1945573259 hasRelatedWork W2887370619 @default.
• W1945573259 hasRelatedWork W3034477078 @default.
• W1945573259 hasRelatedWork W3147246668 @default.
• W1945573259 hasRelatedWork W760098785 @default.
• W1945573259 isParatext "false" @default.
• W1945573259 isRetracted "false" @default.
• W1945573259 magId "1945573259" @default.
• W1945573259 workType "article" @default.