FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022797858> ?p ?o ?g. }

• W2022797858 abstract "American Institute of Mining, Metallurgical, and Petroleum Engineers, Inc. Discussion of this paper is invited. Three copies of any discussion should be sent to the Society of Petroleum Engineers office. Such discussion may be presented at the above meeting and, with the paper, may be considered for publication in one of the two SPE magazines. Abstract For many years hydraulic fracturing has been used as a stimulation tool for oil and gas reservoirs. Hydraulic fracturing has also been developed as a method to measure in situ stresses. The correspondence between the measured fluid pressures and the in situ stresses has been studied and is fairly well understood. The characteristics of the fractures created by hydraulic fracturing are not understood. Information about the fractures at the wellbore can be obtained by a number of techniques but knowledge of the fractures behavior away from the well is very limited. The fracture behavior may determine either the stress direction for a stress measurement or the difference between a good or bad stimulation job. To better understand the hydraulic fracture technique, experiments were performed in a tuff formation in Rainier Mesa performed in a tuff formation in Rainier Mesa at the Nevada Test Site. The purpose of the experiments was to determine the stresses in the mesa; and, to examine the fracture behavior produced by the hydraulic fracture technique. Hydraulic fracturing was performed in both vertical and horizontal performed in both vertical and horizontal boreholes with a maximum overburden of 1490 ft. All experiments were done in the vicinity of an existing tunnel complex but sufficiently remote to avoid unwanted boundary effects. The stresses were determined from the hydraulic fracture data using the theory of Fairhurst and Haimson. The maximum horizontal, vertical and minimum horizontal principal stresses for 1365 ft. of overburden principal stresses for 1365 ft. of overburden were 1788 psi, 1183 psi, and 1015 Psi, respectively. A number of the fractures produced during the tests were mapped by produced during the tests were mapped by mining from the tunnel complex and physically examining the fractured formation. physically examining the fractured formation. Dyed water was used for all the holes drilled in the tunnel complex. Dyed cement grouts were used to tag the fractures formed in a 1365 ft. deep hole from the top of the mesa. Two fracture jobs were performed at two locations in the vertical hole using yellow and red grouts. These fractures were essentially vertical and parallel." @default.
• W2022797858 created "2016-06-24" @default.
• W2022797858 creator A5031400858 @default.
• W2022797858 creator A5066123715 @default.
• W2022797858 date "1975-09-28" @default.
• W2022797858 modified "2023-09-27" @default.
• W2022797858 title "Physical Observations and Mapping of Cracks Resulting from Hydraulic Fracturing In Situ Stress Measurements" @default.
• W2022797858 doi "https://doi.org/10.2118/5542-ms" @default.
• W2022797858 hasPublicationYear "1975" @default.
• W2022797858 type Work @default.
• W2022797858 sameAs 2022797858 @default.
• W2022797858 citedByCount "12" @default.
• W2022797858 countsByYear W20227978582013 @default.
• W2022797858 countsByYear W20227978582016 @default.
• W2022797858 crossrefType "proceedings-article" @default.
• W2022797858 hasAuthorship W2022797858A5031400858 @default.
• W2022797858 hasAuthorship W2022797858A5066123715 @default.
• W2022797858 hasConcept C127313418 @default.
• W2022797858 hasConcept C138885662 @default.
• W2022797858 hasConcept C150560799 @default.
• W2022797858 hasConcept C151730666 @default.
• W2022797858 hasConcept C183250156 @default.
• W2022797858 hasConcept C187320778 @default.
• W2022797858 hasConcept C191897082 @default.
• W2022797858 hasConcept C192562407 @default.
• W2022797858 hasConcept C21036866 @default.
• W2022797858 hasConcept C2777201227 @default.
• W2022797858 hasConcept C2779096232 @default.
• W2022797858 hasConcept C2779538338 @default.
• W2022797858 hasConcept C2780952559 @default.
• W2022797858 hasConcept C41895202 @default.
• W2022797858 hasConcept C43369102 @default.
• W2022797858 hasConcept C548895740 @default.
• W2022797858 hasConcept C78762247 @default.
• W2022797858 hasConcept C81803558 @default.
• W2022797858 hasConcept C9677107 @default.
• W2022797858 hasConceptScore W2022797858C127313418 @default.
• W2022797858 hasConceptScore W2022797858C138885662 @default.
• W2022797858 hasConceptScore W2022797858C150560799 @default.
• W2022797858 hasConceptScore W2022797858C151730666 @default.
• W2022797858 hasConceptScore W2022797858C183250156 @default.
• W2022797858 hasConceptScore W2022797858C187320778 @default.
• W2022797858 hasConceptScore W2022797858C191897082 @default.
• W2022797858 hasConceptScore W2022797858C192562407 @default.
• W2022797858 hasConceptScore W2022797858C21036866 @default.
• W2022797858 hasConceptScore W2022797858C2777201227 @default.
• W2022797858 hasConceptScore W2022797858C2779096232 @default.
• W2022797858 hasConceptScore W2022797858C2779538338 @default.
• W2022797858 hasConceptScore W2022797858C2780952559 @default.
• W2022797858 hasConceptScore W2022797858C41895202 @default.
• W2022797858 hasConceptScore W2022797858C43369102 @default.
• W2022797858 hasConceptScore W2022797858C548895740 @default.
• W2022797858 hasConceptScore W2022797858C78762247 @default.
• W2022797858 hasConceptScore W2022797858C81803558 @default.
• W2022797858 hasConceptScore W2022797858C9677107 @default.
• W2022797858 hasLocation W20227978581 @default.
• W2022797858 hasOpenAccess W2022797858 @default.
• W2022797858 hasPrimaryLocation W20227978581 @default.
• W2022797858 hasRelatedWork W2022797858 @default.
• W2022797858 hasRelatedWork W2025679555 @default.
• W2022797858 hasRelatedWork W2063266203 @default.
• W2022797858 hasRelatedWork W2091880458 @default.
• W2022797858 hasRelatedWork W2092283179 @default.
• W2022797858 hasRelatedWork W3023621856 @default.
• W2022797858 hasRelatedWork W3096967538 @default.
• W2022797858 hasRelatedWork W4244093355 @default.
• W2022797858 hasRelatedWork W2522472209 @default.
• W2022797858 hasRelatedWork W2625916794 @default.
• W2022797858 isParatext "false" @default.
• W2022797858 isRetracted "false" @default.
• W2022797858 magId "2022797858" @default.
• W2022797858 workType "article" @default.