FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2090785895> ?p ?o ?g. }

• W2090785895 endingPage "no" @default.
• W2090785895 startingPage "no" @default.
• W2090785895 abstract "Salt water intrusion models are commonly used to support groundwater resource management in coastal aquifers. Concentration data used for model calibration are often sparse and limited in spatial extent. With airborne and ground-based electromagnetic surveys, electrical resistivity models can be obtained to provide high-resolution three-dimensional models of subsurface resistivity variations that can be related to geology and salt concentrations on a regional scale. Several previous studies have calibrated salt water intrusion models with geophysical data, but are typically limited to the use of the inverted electrical resistivity models without considering the measured geophysical data directly. This induces a number of errors related to inconsistent scales between the geophysical and hydrologic models and the applied regularization constraints in the geophysical inversion. To overcome these errors, we perform a coupled hydrogeophysical inversion (CHI) in which we use a salt water intrusion model to interpret the geophysical data and guide the geophysical inversion. We refer to this methodology as a Coupled Hydrogeophysical Inversion-State (CHI-S), in which simulated salt concentrations are transformed to an electrical resistivity model, after which a geophysical forward response is calculated and compared with the measured geophysical data. This approach was applied for a field site in Santa Cruz County, California, where a time-domain electromagnetic (TDEM) dataset was collected. For this location, a simple two-dimensional cross-sectional salt water intrusion model was developed, for which we estimated five uniform aquifer properties, incorporating the porosity that was also part of the employed petrophysical relationship. In addition, one geophysical parameter was estimated. The six parameters could be resolved well by fitting more than 300 apparent resistivities that were comprised by the TDEM dataset. Except for three sounding locations, all the TDEM data could be fitted close to a root-mean-square error of 1. Possible explanations for the poor fit of these soundings are the assumption of spatial uniformity, fixed boundary conditions and the neglecting of 3D effects in the groundwater model and the TDEM forward responses." @default.
• W2090785895 created "2016-06-24" @default.
• W2090785895 creator A5003233325 @default.
• W2090785895 creator A5016159634 @default.
• W2090785895 creator A5037075253 @default.
• W2090785895 creator A5050423884 @default.
• W2090785895 creator A5057504959 @default.
• W2090785895 creator A5071711632 @default.
• W2090785895 date "2012-08-01" @default.
• W2090785895 modified "2023-10-18" @default.
• W2090785895 title "Calibrating a Salt Water Intrusion Model with Time-Domain Electromagnetic Data" @default.
• W2090785895 cites W126688294 @default.
• W2090785895 cites W1603070741 @default.
• W2090785895 cites W1643119064 @default.
• W2090785895 cites W1968675537 @default.
• W2090785895 cites W1975152865 @default.
• W2090785895 cites W1976003395 @default.
• W2090785895 cites W1976078677 @default.
• W2090785895 cites W1981325185 @default.
• W2090785895 cites W1998742682 @default.
• W2090785895 cites W2004273647 @default.
• W2090785895 cites W2008551877 @default.
• W2090785895 cites W2018570871 @default.
• W2090785895 cites W2021339940 @default.
• W2090785895 cites W2021984446 @default.
• W2090785895 cites W2023236756 @default.
• W2090785895 cites W2041436028 @default.
• W2090785895 cites W2044676352 @default.
• W2090785895 cites W2049116044 @default.
• W2090785895 cites W2065182477 @default.
• W2090785895 cites W2079098033 @default.
• W2090785895 cites W2082574589 @default.
• W2090785895 cites W2098704745 @default.
• W2090785895 cites W2115894759 @default.
• W2090785895 cites W2119995368 @default.
• W2090785895 cites W2119998244 @default.
• W2090785895 cites W2126865599 @default.
• W2090785895 cites W2129622983 @default.
• W2090785895 cites W2133846178 @default.
• W2090785895 cites W2137988860 @default.
• W2090785895 cites W2143124469 @default.
• W2090785895 cites W21570526 @default.
• W2090785895 cites W2159260396 @default.
• W2090785895 doi "https://doi.org/10.1111/j.1745-6584.2012.00974.x" @default.
• W2090785895 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/22891736" @default.
• W2090785895 hasPublicationYear "2012" @default.
• W2090785895 type Work @default.
• W2090785895 sameAs 2090785895 @default.
• W2090785895 citedByCount "16" @default.
• W2090785895 countsByYear W20907858952013 @default.
• W2090785895 countsByYear W20907858952014 @default.
• W2090785895 countsByYear W20907858952015 @default.
• W2090785895 countsByYear W20907858952016 @default.
• W2090785895 countsByYear W20907858952017 @default.
• W2090785895 countsByYear W20907858952018 @default.
• W2090785895 countsByYear W20907858952020 @default.
• W2090785895 countsByYear W20907858952021 @default.
• W2090785895 countsByYear W20907858952022 @default.
• W2090785895 countsByYear W20907858952023 @default.
• W2090785895 crossrefType "journal-article" @default.
• W2090785895 hasAuthorship W2090785895A5003233325 @default.
• W2090785895 hasAuthorship W2090785895A5016159634 @default.
• W2090785895 hasAuthorship W2090785895A5037075253 @default.
• W2090785895 hasAuthorship W2090785895A5050423884 @default.
• W2090785895 hasAuthorship W2090785895A5057504959 @default.
• W2090785895 hasAuthorship W2090785895A5071711632 @default.
• W2090785895 hasConcept C109007969 @default.
• W2090785895 hasConcept C114793014 @default.
• W2090785895 hasConcept C119599485 @default.
• W2090785895 hasConcept C127313418 @default.
• W2090785895 hasConcept C127413603 @default.
• W2090785895 hasConcept C132594454 @default.
• W2090785895 hasConcept C159390177 @default.
• W2090785895 hasConcept C174091901 @default.
• W2090785895 hasConcept C187320778 @default.
• W2090785895 hasConcept C1893757 @default.
• W2090785895 hasConcept C24326235 @default.
• W2090785895 hasConcept C2780103101 @default.
• W2090785895 hasConcept C2909720056 @default.
• W2090785895 hasConcept C46293882 @default.
• W2090785895 hasConcept C60591178 @default.
• W2090785895 hasConcept C6648577 @default.
• W2090785895 hasConcept C69990965 @default.
• W2090785895 hasConcept C75622301 @default.
• W2090785895 hasConcept C76177295 @default.
• W2090785895 hasConcept C8058405 @default.
• W2090785895 hasConceptScore W2090785895C109007969 @default.
• W2090785895 hasConceptScore W2090785895C114793014 @default.
• W2090785895 hasConceptScore W2090785895C119599485 @default.
• W2090785895 hasConceptScore W2090785895C127313418 @default.
• W2090785895 hasConceptScore W2090785895C127413603 @default.
• W2090785895 hasConceptScore W2090785895C132594454 @default.
• W2090785895 hasConceptScore W2090785895C159390177 @default.
• W2090785895 hasConceptScore W2090785895C174091901 @default.
• W2090785895 hasConceptScore W2090785895C187320778 @default.
• W2090785895 hasConceptScore W2090785895C1893757 @default.
• W2090785895 hasConceptScore W2090785895C24326235 @default.
• W2090785895 hasConceptScore W2090785895C2780103101 @default.

• next