FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W374684669> ?p ?o ?g. }

• W374684669 endingPage "134" @default.
• W374684669 startingPage "127" @default.
• W374684669 abstract "Difficulty in characterizing the fracture-rock matrix system, its hydraulic properties and connectivity at resolutions have led to the development of different conceptual models of fractured rocks. Over the last several decades, considerable effort has gone into creating maps of subsurface heterogeneity in hydraulic conductivity (K) and specific storage (Ss) of fractured rocks. In the unsaturated zone, maps of permeability (k) and porosity (ϕ) may also be obtained with pneumatic tests. Traditionally, numerous single-hole tests are conducted at successive intervals along boreholes to obtain information on such variability. If data from multiple test intervals in several boreholes are available, then they are amenable to geostatistical analysis. However, at some field sites, boreholes are sufficiently far apart that could lead to difficulties in conducting traditional geostatistical analysis as single-hole tests do not directly provide information on connectivity between boreholes. Recent research in the characterization of both unconsolidated and fractured rocks through synthetic, laboratory and field studies has shown that hydraulic tomography (HT) and pneumatic tomography (PT) are very promising approaches in characterizing subsurface heterogeneity. This is due to the fact that both HT and PT rely on multiple pumping or injection tests to generate signals that are detected in neighbouring monitoring intervals. In this paper, I discuss lessons learned from the various studies published in the literature on HT and PT in fractured rocks. In particular, some lessons learned include that: 1) both techniques allow for the mapping of heterogeneity between boreholes; 2) they are applicable at large scales as long as reliable drawdown signals can be detected; 3) PT has shown that improved mapping of heterogeneity leads to the suppression of scale effect in flow properties; 4) both techniques can map the connectivity of flow properties; and 5) improved mapping of heterogeneity and connectivity may lead to improved transport predictions. Overall, HT and PT both appear to provide the most reliable maps of subsurface heterogeneity in fractured rocks, but improvements can be made. Future research needs resulting from these lessons are also briefly discussed." @default.
• W374684669 created "2016-06-24" @default.
• W374684669 creator A5005758499 @default.
• W374684669 date "2015-01-01" @default.
• W374684669 modified "2023-10-18" @default.
• W374684669 title "Lessons Learned from Hydraulic and Pneumatic Tomography in Fractured Rocks" @default.
• W374684669 cites W1481878801 @default.
• W374684669 cites W1485943595 @default.
• W374684669 cites W1486816089 @default.
• W374684669 cites W1494298856 @default.
• W374684669 cites W1535664136 @default.
• W374684669 cites W1556099588 @default.
• W374684669 cites W1566989920 @default.
• W374684669 cites W1581594141 @default.
• W374684669 cites W1585742548 @default.
• W374684669 cites W1593429003 @default.
• W374684669 cites W1597239557 @default.
• W374684669 cites W1610967235 @default.
• W374684669 cites W1613997427 @default.
• W374684669 cites W1619556709 @default.
• W374684669 cites W1645383175 @default.
• W374684669 cites W1650350869 @default.
• W374684669 cites W1652531989 @default.
• W374684669 cites W1657819877 @default.
• W374684669 cites W1824614064 @default.
• W374684669 cites W1857393746 @default.
• W374684669 cites W1966773213 @default.
• W374684669 cites W1969363361 @default.
• W374684669 cites W1971408786 @default.
• W374684669 cites W1976003395 @default.
• W374684669 cites W1978305759 @default.
• W374684669 cites W1984803607 @default.
• W374684669 cites W1993792217 @default.
• W374684669 cites W2006087805 @default.
• W374684669 cites W2011209109 @default.
• W374684669 cites W2011340235 @default.
• W374684669 cites W2027852097 @default.
• W374684669 cites W2037938620 @default.
• W374684669 cites W2046249551 @default.
• W374684669 cites W2047040515 @default.
• W374684669 cites W2048802840 @default.
• W374684669 cites W2050067291 @default.
• W374684669 cites W2052379270 @default.
• W374684669 cites W2054618741 @default.
• W374684669 cites W2056416998 @default.
• W374684669 cites W2059164460 @default.
• W374684669 cites W2073132281 @default.
• W374684669 cites W2098981021 @default.
• W374684669 cites W2102351622 @default.
• W374684669 cites W2122691590 @default.
• W374684669 cites W2137635323 @default.
• W374684669 cites W2149165195 @default.
• W374684669 cites W2149276484 @default.
• W374684669 cites W2154653682 @default.
• W374684669 cites W2159645814 @default.
• W374684669 cites W3122643305 @default.
• W374684669 doi "https://doi.org/10.1016/j.proenv.2015.04.018" @default.
• W374684669 hasPublicationYear "2015" @default.
• W374684669 type Work @default.
• W374684669 sameAs 374684669 @default.
• W374684669 citedByCount "4" @default.
• W374684669 countsByYear W3746846692019 @default.
• W374684669 countsByYear W3746846692020 @default.
• W374684669 crossrefType "journal-article" @default.
• W374684669 hasAuthorship W374684669A5005758499 @default.
• W374684669 hasBestOaLocation W3746846691 @default.
• W374684669 hasConcept C120882062 @default.
• W374684669 hasConcept C127313418 @default.
• W374684669 hasConcept C150560799 @default.
• W374684669 hasConcept C159390177 @default.
• W374684669 hasConcept C159750122 @default.
• W374684669 hasConcept C187320778 @default.
• W374684669 hasConcept C2779096232 @default.
• W374684669 hasConcept C41625074 @default.
• W374684669 hasConcept C54355233 @default.
• W374684669 hasConcept C5900021 @default.
• W374684669 hasConcept C63184880 @default.
• W374684669 hasConcept C78762247 @default.
• W374684669 hasConcept C86803240 @default.
• W374684669 hasConceptScore W374684669C120882062 @default.
• W374684669 hasConceptScore W374684669C127313418 @default.
• W374684669 hasConceptScore W374684669C150560799 @default.
• W374684669 hasConceptScore W374684669C159390177 @default.
• W374684669 hasConceptScore W374684669C159750122 @default.
• W374684669 hasConceptScore W374684669C187320778 @default.
• W374684669 hasConceptScore W374684669C2779096232 @default.
• W374684669 hasConceptScore W374684669C41625074 @default.
• W374684669 hasConceptScore W374684669C54355233 @default.
• W374684669 hasConceptScore W374684669C5900021 @default.
• W374684669 hasConceptScore W374684669C63184880 @default.
• W374684669 hasConceptScore W374684669C78762247 @default.
• W374684669 hasConceptScore W374684669C86803240 @default.
• W374684669 hasLocation W3746846691 @default.
• W374684669 hasOpenAccess W374684669 @default.
• W374684669 hasPrimaryLocation W3746846691 @default.
• W374684669 hasRelatedWork W1998180939 @default.
• W374684669 hasRelatedWork W1999934806 @default.
• W374684669 hasRelatedWork W2034459683 @default.

• next