Matches in SemOpenAlex for { <https://semopenalex.org/work/W2034283798> ?p ?o ?g. }
- W2034283798 endingPage "1558" @default.
- W2034283798 startingPage "1547" @default.
- W2034283798 abstract "Resistivity and induced polarization (IP) measurements (0.1–1000 Hz) were made on clay‐free unconsolidated sediments from a sandy, alluvial aquifer in the Kansas River floodplain. The sensitivity of imaginary conductivity σ″, a fundamental IP measurement, to lithological parameters, fluid conductivity, and degree of saturation was assessed. The previously reported power law dependence of IP on surface area and grain size is clearly observed despite the narrow lithologic range encountered in this unconsolidated sedimentary sequence. The grain‐size σ″ relationship is effectively frequency independent between 0.1 and 100 Hz but depends on the representative grain diameter used. For the sediments examined here, d 90 , the grain diameter of the coarsest sediments in a sample, is well correlated with σ″. The distribution of the internal surface in the well‐sorted, sandy sediments investigated here is such that most of the sample weight is likely required to account for the majority of the internal surface. We find the predictive capability of the Börner model for hydraulic conductivity (K)estimation from IP measurements is limited when applied to this narrow lithologic range. The relatively weak dependence of σ″ on fluid conductivity (σ w ) observed for these sediments when saturated with an NaCl solution (0.06–10 S/m) is consistent with competing effects of surface charge density and surface ionic mobility on σ″ as previously inferred for sandstone. Importantly, IP parameters are a function of saturation and exhibit hysteretic behavior over a drainage and imbibition cycle. However, σ″ is less dependent than the real conductivity σ′ on saturation. In the case of evaporative drying, the σ″ saturation exponent is approximately half of the σ′ exponent. Crosshole IP imaging illustrates the potential for lithologic discrimination of unconsolidated sediments. A fining‐upward sequence correlates with an upward increase in normalized chargeability M n , a field IP parameter proportional to σ″. The hydraulic conductivity distribution obtained from the Börner model discriminates a hydraulically conductive sand–gravel from overlying medium sand." @default.
- W2034283798 created "2016-06-24" @default.
- W2034283798 creator A5001777851 @default.
- W2034283798 creator A5003060932 @default.
- W2034283798 date "2003-09-01" @default.
- W2034283798 modified "2023-09-27" @default.
- W2034283798 title "Controls on induced polarization in sandy unconsolidated sediments and application to aquifer characterization" @default.
- W2034283798 cites W1976730797 @default.
- W2034283798 cites W1979084365 @default.
- W2034283798 cites W1982307786 @default.
- W2034283798 cites W1983929161 @default.
- W2034283798 cites W1995921923 @default.
- W2034283798 cites W1999684187 @default.
- W2034283798 cites W2000295358 @default.
- W2034283798 cites W2002194678 @default.
- W2034283798 cites W2007188064 @default.
- W2034283798 cites W2008982771 @default.
- W2034283798 cites W2011757174 @default.
- W2034283798 cites W2012712793 @default.
- W2034283798 cites W2015234009 @default.
- W2034283798 cites W2031401646 @default.
- W2034283798 cites W2051699790 @default.
- W2034283798 cites W2059072408 @default.
- W2034283798 cites W2074090534 @default.
- W2034283798 cites W2074297536 @default.
- W2034283798 cites W2086215685 @default.
- W2034283798 cites W2100524267 @default.
- W2034283798 cites W2104694724 @default.
- W2034283798 cites W2105371752 @default.
- W2034283798 cites W2105893200 @default.
- W2034283798 cites W2113075737 @default.
- W2034283798 cites W2113476080 @default.
- W2034283798 cites W2117741254 @default.
- W2034283798 cites W2119934871 @default.
- W2034283798 cites W2127013476 @default.
- W2034283798 cites W2134029612 @default.
- W2034283798 cites W2146801751 @default.
- W2034283798 cites W2147796951 @default.
- W2034283798 cites W2493661768 @default.
- W2034283798 cites W2503439741 @default.
- W2034283798 cites W4252093097 @default.
- W2034283798 doi "https://doi.org/10.1190/1.1620628" @default.
- W2034283798 hasPublicationYear "2003" @default.
- W2034283798 type Work @default.
- W2034283798 sameAs 2034283798 @default.
- W2034283798 citedByCount "118" @default.
- W2034283798 countsByYear W20342837982012 @default.
- W2034283798 countsByYear W20342837982013 @default.
- W2034283798 countsByYear W20342837982014 @default.
- W2034283798 countsByYear W20342837982015 @default.
- W2034283798 countsByYear W20342837982016 @default.
- W2034283798 countsByYear W20342837982017 @default.
- W2034283798 countsByYear W20342837982018 @default.
- W2034283798 countsByYear W20342837982019 @default.
- W2034283798 countsByYear W20342837982020 @default.
- W2034283798 countsByYear W20342837982021 @default.
- W2034283798 countsByYear W20342837982022 @default.
- W2034283798 countsByYear W20342837982023 @default.
- W2034283798 crossrefType "journal-article" @default.
- W2034283798 hasAuthorship W2034283798A5001777851 @default.
- W2034283798 hasAuthorship W2034283798A5003060932 @default.
- W2034283798 hasConcept C100701293 @default.
- W2034283798 hasConcept C114614502 @default.
- W2034283798 hasConcept C114793014 @default.
- W2034283798 hasConcept C119599485 @default.
- W2034283798 hasConcept C122792734 @default.
- W2034283798 hasConcept C127313418 @default.
- W2034283798 hasConcept C127413603 @default.
- W2034283798 hasConcept C131540310 @default.
- W2034283798 hasConcept C147789679 @default.
- W2034283798 hasConcept C159390177 @default.
- W2034283798 hasConcept C159750122 @default.
- W2034283798 hasConcept C17409809 @default.
- W2034283798 hasConcept C185592680 @default.
- W2034283798 hasConcept C187320778 @default.
- W2034283798 hasConcept C192191005 @default.
- W2034283798 hasConcept C199289684 @default.
- W2034283798 hasConcept C2778409621 @default.
- W2034283798 hasConcept C33923547 @default.
- W2034283798 hasConcept C5900021 @default.
- W2034283798 hasConcept C59822182 @default.
- W2034283798 hasConcept C63184880 @default.
- W2034283798 hasConcept C6494504 @default.
- W2034283798 hasConcept C69990965 @default.
- W2034283798 hasConcept C75622301 @default.
- W2034283798 hasConcept C76177295 @default.
- W2034283798 hasConcept C85292911 @default.
- W2034283798 hasConcept C86803240 @default.
- W2034283798 hasConcept C9930424 @default.
- W2034283798 hasConceptScore W2034283798C100701293 @default.
- W2034283798 hasConceptScore W2034283798C114614502 @default.
- W2034283798 hasConceptScore W2034283798C114793014 @default.
- W2034283798 hasConceptScore W2034283798C119599485 @default.
- W2034283798 hasConceptScore W2034283798C122792734 @default.
- W2034283798 hasConceptScore W2034283798C127313418 @default.
- W2034283798 hasConceptScore W2034283798C127413603 @default.
- W2034283798 hasConceptScore W2034283798C131540310 @default.
- W2034283798 hasConceptScore W2034283798C147789679 @default.