THE REPRESENTER METHOD FOR TWO-PHASE FLOW IN POROUS MEDIA

dc.contributor.authorBaird J.
dc.contributor.authorDawson C.
dc.date.accessioned2026-06-04T15:31:49Z
dc.date.issued2007
dc.description.abstractThe representer method is applied to a one-dimensional two-phase flow model in porous media; capillary pressure and gravity are neglected. The Euler–Lagrange equations must be linearized, and one such linearization is presented here. The representer method is applied to the linear system iteratively until convergence, though a rigorous proof of convergence is out of reach. The linearization chosen is easy to calculate but does not converge for certain weights; however, a simple damping restores convergence at the cost of extra iterations. Numerical experiments are performed that illustrate the method, and quick comparison to the ensemble Kalman smoother is made.
dc.identifierhttps://elibrary.ru/item.asp?id=51152359
dc.identifier.citationComputational Geosciences, 2007, 11, 3, 235-248
dc.identifier.doi10.1007/s10596-007-9048-8
dc.identifier.issn1420-0597
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/53127
dc.subjectREPRESENTER METHOD
dc.subjectTWO-PHASE FLOW
dc.subjectPOROUS MEDIA
dc.subjectENSEMBLE KALMAN SMOOTHER
dc.titleTHE REPRESENTER METHOD FOR TWO-PHASE FLOW IN POROUS MEDIA
dc.typeСтатья

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