FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1995497761> ?p ?o ?g. }

• W1995497761 endingPage "927" @default.
• W1995497761 startingPage "918" @default.
• W1995497761 abstract "In order to evaluate the applicability of the magnetic resonance sounding method (MRS) in the Danish context and its accuracy in estimating the hydraulic conductivity of different sedimentary aquifers, three MRS campaigns were conducted in Denmark between 2003 and 2007. In total, 12 sites were investigated. At two sites, it was impossible to measure with MRS due to the high level of ambient electromagnetic noise. For the present study, MRS results from 10 investigated sites throughout Denmark are used. A simplified classification of the grain-size within the investigated aquifers was established, based on a geological description of available borehole data. MRS-obtained parameters, water content (θMRS) and decay time (T1), as well as normalised values of the MRS hydraulic conductivity estimator (KMRSn), from 23 MRS stations were compared with the aquifer class defined by geological description of adjacent boreholes. The comparison revealed a qualitative correlation. Moreover, KMRSn results revealed variations in the hydraulic conductivity within the investigated areas. The observed variations may suggest preferential locations for water- supply boreholes. Further MRS measurements close to boreholes with detailed grain-size analyses and pumping tests are required for a more quantitative estimation. Pour évaluer l’application de la résonance magnétique des protons (RMP) au contexte danois, ainsi que la précision de la méthode à estimer la conductivité hydraulique des différents aquifères sédimentaires, trois campagnes RMP ont été réalisées au Danemark entre 2003 et 2007. Douze sites, au total, ont été étudiés. Sur deux sites, il a été impossible de mesurer avec la RMP à cause du bruit électromagnétique ambiant. Pour cette étude, les résultats RMP obtenus à partir de dix sites autour du Danemark sont utilisés. Une classification simplifiée des formations aquifères selon la taille des grains a été d’abord établie, basée sur la description géologique des forages disponibles. Les paramètres RMP obtenus, teneur en eau (θMRS) et temps de décroissance (T1), ainsi que les valeurs normalisées de l’estimateur de la conductivité hydraulique (KMRSn), de 23 stations RMP, ont été comparés avec les classes des aquifères, définies à partir de la description géologique de forages voisins. La comparaison révèle une corrélation qualitative. En outre, les résultats KMRSn révèlent des variations de la conductivité hydraulique dans les sites étudiés. Ces variations peuvent permettre de proposer des emplacements préférentiels pour l’implantation de forages d’eau. Pour une estimation plus quantitative, des mesures supplémentaires RMP à proximité de forages ayant fait l’objet d’analyses granulométriques détaillées et d’essais de pompage sont nécessaires." @default.
• W1995497761 created "2016-06-24" @default.
• W1995497761 creator A5012213964 @default.
• W1995497761 creator A5057259838 @default.
• W1995497761 creator A5066407315 @default.
• W1995497761 creator A5075393824 @default.
• W1995497761 date "2009-10-01" @default.
• W1995497761 modified "2023-10-01" @default.
• W1995497761 title "Investigation of sedimentary aquifers in Denmark using the magnetic resonance sounding method (MRS)" @default.
• W1995497761 cites W2021511018 @default.
• W1995497761 cites W2023259268 @default.
• W1995497761 cites W2029072607 @default.
• W1995497761 cites W2030004709 @default.
• W1995497761 cites W2046205922 @default.
• W1995497761 cites W2048057485 @default.
• W1995497761 cites W2055103535 @default.
• W1995497761 cites W2061327125 @default.
• W1995497761 cites W2090465752 @default.
• W1995497761 cites W2123390718 @default.
• W1995497761 cites W2130456298 @default.
• W1995497761 cites W2135782256 @default.
• W1995497761 cites W2161883140 @default.
• W1995497761 doi "https://doi.org/10.1016/j.crte.2009.07.007" @default.
• W1995497761 hasPublicationYear "2009" @default.
• W1995497761 type Work @default.
• W1995497761 sameAs 1995497761 @default.
• W1995497761 citedByCount "18" @default.
• W1995497761 countsByYear W19954977612012 @default.
• W1995497761 countsByYear W19954977612013 @default.
• W1995497761 countsByYear W19954977612014 @default.
• W1995497761 countsByYear W19954977612018 @default.
• W1995497761 countsByYear W19954977612019 @default.
• W1995497761 countsByYear W19954977612020 @default.
• W1995497761 countsByYear W19954977612022 @default.
• W1995497761 countsByYear W19954977612023 @default.
• W1995497761 crossrefType "journal-article" @default.
• W1995497761 hasAuthorship W1995497761A5012213964 @default.
• W1995497761 hasAuthorship W1995497761A5057259838 @default.
• W1995497761 hasAuthorship W1995497761A5066407315 @default.
• W1995497761 hasAuthorship W1995497761A5075393824 @default.
• W1995497761 hasConcept C111368507 @default.
• W1995497761 hasConcept C114793014 @default.
• W1995497761 hasConcept C127313418 @default.
• W1995497761 hasConcept C150560799 @default.
• W1995497761 hasConcept C151730666 @default.
• W1995497761 hasConcept C159390177 @default.
• W1995497761 hasConcept C159750122 @default.
• W1995497761 hasConcept C17409809 @default.
• W1995497761 hasConcept C187320778 @default.
• W1995497761 hasConcept C192191005 @default.
• W1995497761 hasConcept C199289684 @default.
• W1995497761 hasConcept C2779343474 @default.
• W1995497761 hasConcept C55510283 @default.
• W1995497761 hasConcept C63184880 @default.
• W1995497761 hasConcept C6494504 @default.
• W1995497761 hasConcept C75622301 @default.
• W1995497761 hasConcept C76177295 @default.
• W1995497761 hasConceptScore W1995497761C111368507 @default.
• W1995497761 hasConceptScore W1995497761C114793014 @default.
• W1995497761 hasConceptScore W1995497761C127313418 @default.
• W1995497761 hasConceptScore W1995497761C150560799 @default.
• W1995497761 hasConceptScore W1995497761C151730666 @default.
• W1995497761 hasConceptScore W1995497761C159390177 @default.
• W1995497761 hasConceptScore W1995497761C159750122 @default.
• W1995497761 hasConceptScore W1995497761C17409809 @default.
• W1995497761 hasConceptScore W1995497761C187320778 @default.
• W1995497761 hasConceptScore W1995497761C192191005 @default.
• W1995497761 hasConceptScore W1995497761C199289684 @default.
• W1995497761 hasConceptScore W1995497761C2779343474 @default.
• W1995497761 hasConceptScore W1995497761C55510283 @default.
• W1995497761 hasConceptScore W1995497761C63184880 @default.
• W1995497761 hasConceptScore W1995497761C6494504 @default.
• W1995497761 hasConceptScore W1995497761C75622301 @default.
• W1995497761 hasConceptScore W1995497761C76177295 @default.
• W1995497761 hasIssue "10-11" @default.
• W1995497761 hasLocation W19954977611 @default.
• W1995497761 hasOpenAccess W1995497761 @default.
• W1995497761 hasPrimaryLocation W19954977611 @default.
• W1995497761 hasRelatedWork W2008745676 @default.
• W1995497761 hasRelatedWork W2033987489 @default.
• W1995497761 hasRelatedWork W2057030403 @default.
• W1995497761 hasRelatedWork W2086342990 @default.
• W1995497761 hasRelatedWork W2129214965 @default.
• W1995497761 hasRelatedWork W2563824525 @default.
• W1995497761 hasRelatedWork W2787030420 @default.
• W1995497761 hasRelatedWork W2923778803 @default.
• W1995497761 hasRelatedWork W2964752161 @default.
• W1995497761 hasRelatedWork W3017031929 @default.
• W1995497761 hasVolume "341" @default.
• W1995497761 isParatext "false" @default.
• W1995497761 isRetracted "false" @default.
• W1995497761 magId "1995497761" @default.
• W1995497761 workType "article" @default.