A crack in the homogeneous half plane interacting with a crack at the interface between the nonhomogeneous coating and the homogeneous half-plane

Theotokoglou, EE; Paulino, GH

dc.contributor.author	Theotokoglou, EE	en
dc.contributor.author	Paulino, GH	en
dc.date.accessioned	2014-03-01T01:21:42Z
dc.date.available	2014-03-01T01:21:42Z
dc.date.issued	2005	en
dc.identifier.issn	0376-9429	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/16332
dc.subject	Coordinate System	en
dc.subject	Fundamental Solution	en
dc.subject	Integral Transforms	en
dc.subject	Shear Modulus	en
dc.subject	Stress Field	en
dc.subject.classification	Mechanics	en
dc.subject.other	Coatings	en
dc.subject.other	Elastic moduli	en
dc.subject.other	Fourier transforms	en
dc.subject.other	Fracture mechanics	en
dc.subject.other	Integral equations	en
dc.subject.other	Interfaces (materials)	en
dc.subject.other	Problem solving	en
dc.subject.other	Strain	en
dc.subject.other	Stresses	en
dc.subject.other	Elastic coating	en
dc.subject.other	Fourier integral transform method	en
dc.subject.other	Homogeneous half plane	en
dc.subject.other	Local coordinate systems	en
dc.subject.other	Nonhomogeneous coating	en
dc.subject.other	Plane stress conditions	en
dc.subject.other	Structural coordinate system	en
dc.subject.other	Cracks	en
dc.title	A crack in the homogeneous half plane interacting with a crack at the interface between the nonhomogeneous coating and the homogeneous half-plane	en
heal.type	journalArticle	en
heal.identifier.primary	10.1007/s10704-005-0635-1	en
heal.identifier.secondary	http://dx.doi.org/10.1007/s10704-005-0635-1	en
heal.language	English	en
heal.publicationDate	2005	en
heal.abstract	A fundamental solution is established for a crack in a homogeneous half-plane interacting with a crack at the interface between the homogeneous elastic half-plane and the nonhomogeneous elastic coating in which the shear modulus varies exponentially with one coordinate. The problem is solved under plane strain or generalized plane stress conditions using the Fourier integral transform method. The stress field in the homogeneous half plane is evaluated by the superposition of two states of stresses, one of which is associated with a local coordinate system in the infinite fractured plate, while the other one in the infinite half plane defined in a structural coordinate system. © Springer 2005.	en
heal.publisher	SPRINGER	en
heal.journalName	International Journal of Fracture	en
dc.identifier.doi	10.1007/s10704-005-0635-1	en
dc.identifier.isi	ISI:000231954600006	en
dc.identifier.volume	134	en
dc.identifier.issue	1	en
dc.identifier.spage	L11	en
dc.identifier.epage	L18	en