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contributor authorD. A. Mendelsohn
date accessioned2017-05-08T23:17:33Z
date available2017-05-08T23:17:33Z
date copyrightSeptember, 1984
date issued1984
identifier issn0195-0738
identifier otherJERTD2-26400#369_1.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/98295
description abstractThis is Part I of a two-part paper which reviews in depth the literature on the modeling of the propagation of large hydraulic fractures in underground rock formations. Part I presents a general formulation of the problem, its geometry and only the most fundamental and unrestrictive physical assumptions. The two basic two-dimensional models of constant height (rectangular) fractures which formed the core of modeling efforts from 1960 through the late 1970’s are discussed in detail followed by a brief review of the effects of fluid diffusion in the fractured medium on crack propagation. The recent field and laboratory observations which have shown that nonrectangular fractures can occur quite often are discussed, as are their impact on the modeling effort, specifically the need for three-dimensional models of crack propagation in layered environments. Part II of the paper deals with the three-dimensional modeling efforts and some fundamental crack and fracture mechanics problems related to the vertical growth of a hydraulic fracture.
publisherThe American Society of Mechanical Engineers (ASME)
titleA Review of Hydraulic Fracture Modeling—Part I: General Concepts, 2D Models, Motivation for 3D Modeling
typeJournal Paper
journal volume106
journal issue3
journal titleJournal of Energy Resources Technology
identifier doi10.1115/1.3231067
journal fristpage369
journal lastpage376
identifier eissn1528-8994
keywordsFracture (Process)
keywordsModeling
keywordsThree-dimensional modeling
keywordsCrack propagation
keywordsGeometry
keywordsRocks
keywordsThree-dimensional models
keywordsFracture mechanics
keywordsDiffusion (Physics) AND Fluids
treeJournal of Energy Resources Technology:;1984:;volume( 106 ):;issue: 003
contenttypeFulltext


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