FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1974423986> ?p ?o ?g. }

• W1974423986 abstract "Abstract The efficiency of hydraulic fractures largely determines the economics of tight sands and gas shale reservoirs. Efficiency is defined by the fracture conductivity which results from the stimulation treatment. This is a function of fracture half length and height. Independent measures of fracture length and height, and containment provide prime data in evaluating stimulation treatments. Downhole or surface microseismic monitoring produce spatial distributions of microseismic events associated with hydraulic fracturing. These distributions provide the constraints on fracture length, height and containment. Most commercial product offerings ignore uncertainty in locations and biases produced by limited observation arrays. We examine these uncertainties and biases through an analysis of a simulation of event locations and sensor arrays. In addition, we investigate the errors produced by ignoring velocity anisotropy characteristic of gas shale. We studied a set of synthetic microseisms locations. Simulations results demonstrate that mapping fracturing geometry with subsurface sensor arrays requires at least two observation wells (not a common field practice); this minimizes the geometry bias generated when only one observation well is used. One of the two observation wells should be aligned in the direction of the fracture azimuth. Failure to do so results in underestimation of the fracture half-length by approximately 10%. This requires knowledge of the prevailing in-situ stresses directions prior to stimulation. Downhole sensors should be located at the same depth of the fractured formation to avoid errors in fracture height estimation which can be as much as 50%. Velocity anisotropy has a minimal influence on uncertainty in event locations when subsurface sensor arrays are modeled with horizontal velocities. Surface sensor arrays can lead to underestimation of the fracture half-length in the order of 30% to 40% depending on the anisotropy effect whereas fracture height estimation error can be as much as 4%. Analysis of surface sensors arrays which avoid production shutdowns, reveals fracture half-lengths can be underestimated by about 17% to 31% depending on the velocity anisotropy. Uncertainty in event locations using only the vertical velocity in an anisotropic velocity field reduces with increasing depth as expected. Recent analysis of spatial distributions of microseismic activity for effective permeability and diffusion coefficients requires improved location accuracy and estimations of uncertainty." @default.
• W1974423986 created "2016-06-24" @default.
• W1974423986 creator A5003675637 @default.
• W1974423986 creator A5055140146 @default.
• W1974423986 creator A5055702459 @default.
• W1974423986 date "2010-11-02" @default.
• W1974423986 modified "2023-09-24" @default.
• W1974423986 title "Estimation Of Uncertainty In Microseismic Event Location Associated With Hydraulic Fracturing" @default.
• W1974423986 cites W1616123453 @default.
• W1974423986 cites W1964099543 @default.
• W1974423986 cites W1965012705 @default.
• W1974423986 cites W1966402044 @default.
• W1974423986 cites W1966992696 @default.
• W1974423986 cites W1967927266 @default.
• W1974423986 cites W1974911972 @default.
• W1974423986 cites W1977150888 @default.
• W1974423986 cites W1979431056 @default.
• W1974423986 cites W1980898553 @default.
• W1974423986 cites W1987826796 @default.
• W1974423986 cites W2001045038 @default.
• W1974423986 cites W2003688962 @default.
• W1974423986 cites W2012285328 @default.
• W1974423986 cites W2012945668 @default.
• W1974423986 cites W2016090815 @default.
• W1974423986 cites W2018709669 @default.
• W1974423986 cites W2022110266 @default.
• W1974423986 cites W2022523637 @default.
• W1974423986 cites W2031321880 @default.
• W1974423986 cites W2033533622 @default.
• W1974423986 cites W2035202592 @default.
• W1974423986 cites W2039402439 @default.
• W1974423986 cites W2043965640 @default.
• W1974423986 cites W2044294713 @default.
• W1974423986 cites W2044642615 @default.
• W1974423986 cites W2049002746 @default.
• W1974423986 cites W2052227211 @default.
• W1974423986 cites W2053086953 @default.
• W1974423986 cites W2056956197 @default.
• W1974423986 cites W2060375287 @default.
• W1974423986 cites W2063115515 @default.
• W1974423986 cites W2065401080 @default.
• W1974423986 cites W2068554305 @default.
• W1974423986 cites W2072229499 @default.
• W1974423986 cites W2077991017 @default.
• W1974423986 cites W2078025631 @default.
• W1974423986 cites W2086074638 @default.
• W1974423986 cites W2086680719 @default.
• W1974423986 cites W2098274171 @default.
• W1974423986 cites W2099105138 @default.
• W1974423986 cites W2140993886 @default.
• W1974423986 cites W2148741352 @default.
• W1974423986 cites W2320040430 @default.
• W1974423986 cites W2433534058 @default.
• W1974423986 cites W2488112834 @default.
• W1974423986 cites W3015979381 @default.
• W1974423986 cites W3135166342 @default.
• W1974423986 cites W579387256 @default.
• W1974423986 cites W591303395 @default.
• W1974423986 cites W649559325 @default.
• W1974423986 cites W2255069485 @default.
• W1974423986 cites W29337337 @default.
• W1974423986 doi "https://doi.org/10.2118/135325-ms" @default.
• W1974423986 hasPublicationYear "2010" @default.
• W1974423986 type Work @default.
• W1974423986 sameAs 1974423986 @default.
• W1974423986 citedByCount "7" @default.
• W1974423986 countsByYear W19744239862013 @default.
• W1974423986 countsByYear W19744239862014 @default.
• W1974423986 countsByYear W19744239862016 @default.
• W1974423986 countsByYear W19744239862018 @default.
• W1974423986 countsByYear W19744239862020 @default.
• W1974423986 crossrefType "proceedings-article" @default.
• W1974423986 hasAuthorship W1974423986A5003675637 @default.
• W1974423986 hasAuthorship W1974423986A5055140146 @default.
• W1974423986 hasAuthorship W1974423986A5055702459 @default.
• W1974423986 hasConcept C121332964 @default.
• W1974423986 hasConcept C127313418 @default.
• W1974423986 hasConcept C127413603 @default.
• W1974423986 hasConcept C165205528 @default.
• W1974423986 hasConcept C201995342 @default.
• W1974423986 hasConcept C2779096232 @default.
• W1974423986 hasConcept C2779662365 @default.
• W1974423986 hasConcept C2994384808 @default.
• W1974423986 hasConcept C41008148 @default.
• W1974423986 hasConcept C62520636 @default.
• W1974423986 hasConcept C7266685 @default.
• W1974423986 hasConcept C78762247 @default.
• W1974423986 hasConcept C96250715 @default.
• W1974423986 hasConceptScore W1974423986C121332964 @default.
• W1974423986 hasConceptScore W1974423986C127313418 @default.
• W1974423986 hasConceptScore W1974423986C127413603 @default.
• W1974423986 hasConceptScore W1974423986C165205528 @default.
• W1974423986 hasConceptScore W1974423986C201995342 @default.
• W1974423986 hasConceptScore W1974423986C2779096232 @default.
• W1974423986 hasConceptScore W1974423986C2779662365 @default.
• W1974423986 hasConceptScore W1974423986C2994384808 @default.
• W1974423986 hasConceptScore W1974423986C41008148 @default.
• W1974423986 hasConceptScore W1974423986C62520636 @default.
• W1974423986 hasConceptScore W1974423986C7266685 @default.
• W1974423986 hasConceptScore W1974423986C78762247 @default.

• next