Loading…
Stability properties of a crack inverse problem in half space
We show in this paper a Lipschitz stability result for a crack inverse problem in half space. The direct problem is a Laplace equation with zero Neumann condition on the top boundary. The forcing term is a discontinuity across the crack. This formulation can be related to geological faults in elasti...
Saved in:
Published in: | Mathematical methods in the applied sciences 2021-09, Vol.44 (14), p.11498-11513 |
---|---|
Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
cited_by | cdi_FETCH-LOGICAL-c2939-8284b07c9cbecfbc8d8f9f96f9d5935c9ede9055dac5eef358499179f7ed77a63 |
---|---|
cites | cdi_FETCH-LOGICAL-c2939-8284b07c9cbecfbc8d8f9f96f9d5935c9ede9055dac5eef358499179f7ed77a63 |
container_end_page | 11513 |
container_issue | 14 |
container_start_page | 11498 |
container_title | Mathematical methods in the applied sciences |
container_volume | 44 |
creator | Volkov, Darko Jiang, Yulong |
description | We show in this paper a Lipschitz stability result for a crack inverse problem in half space. The direct problem is a Laplace equation with zero Neumann condition on the top boundary. The forcing term is a discontinuity across the crack. This formulation can be related to geological faults in elastic media or to irrotational incompressible flows in a half space minus an inner wall. The direct problem is well posed in an appropriate functional space. We study the related inverse problem where the jump across the crack is unknown, and more importantly, the geometry and the location of the crack are unknown. The data for the inverse problem are of Dirichlet type over a portion of the top boundary. We prove that this inverse problem is uniquely solvable under some assumptions on the geometry of the crack. The highlight of this paper is showing a stability result for this inverse problem. Assuming that the crack is planar, we show that reconstructing the plane containing the crack is Lipschitz stable despite the fact that the forcing term for the underlying PDE is unknown. This uniform stability result holds under the assumption that the forcing term is bounded above and the Dirichlet data are bounded below away from zero in appropriate norms. |
doi_str_mv | 10.1002/mma.7509 |
format | article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2560492781</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2560492781</sourcerecordid><originalsourceid>FETCH-LOGICAL-c2939-8284b07c9cbecfbc8d8f9f96f9d5935c9ede9055dac5eef358499179f7ed77a63</originalsourceid><addsrcrecordid>eNp10E1PwzAMBuAIgcQYSPyESFy4dDhp09QHDtPEl7SJA3CO0tQRHe1akg60f0_HuHKyLD-yrZexSwEzASBv2tbOtAI8YhMBiInIdH7MJiA0JJkU2Sk7i3ENAIUQcsJuXwZb1k097Hgfup7CUFPkneeWu2DdB683XxQi7adlQ-3Y83fbeB576-icnXjbRLr4q1P2dn_3unhMls8PT4v5MnESU0wKWWQlaIeuJOdLV1SFR4-5x0phqhxSRQhKVdYpIp-qIkMUGr2mSmubp1N2ddg7fvG5pTiYdbcNm_GkkSqHDKUuxKiuD8qFLsZA3vShbm3YGQFmH44ZwzH7cEaaHOh33dDuX2dWq_mv_wH-ZGU_</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2560492781</pqid></control><display><type>article</type><title>Stability properties of a crack inverse problem in half space</title><source>Wiley</source><creator>Volkov, Darko ; Jiang, Yulong</creator><creatorcontrib>Volkov, Darko ; Jiang, Yulong</creatorcontrib><description>We show in this paper a Lipschitz stability result for a crack inverse problem in half space. The direct problem is a Laplace equation with zero Neumann condition on the top boundary. The forcing term is a discontinuity across the crack. This formulation can be related to geological faults in elastic media or to irrotational incompressible flows in a half space minus an inner wall. The direct problem is well posed in an appropriate functional space. We study the related inverse problem where the jump across the crack is unknown, and more importantly, the geometry and the location of the crack are unknown. The data for the inverse problem are of Dirichlet type over a portion of the top boundary. We prove that this inverse problem is uniquely solvable under some assumptions on the geometry of the crack. The highlight of this paper is showing a stability result for this inverse problem. Assuming that the crack is planar, we show that reconstructing the plane containing the crack is Lipschitz stable despite the fact that the forcing term for the underlying PDE is unknown. This uniform stability result holds under the assumption that the forcing term is bounded above and the Dirichlet data are bounded below away from zero in appropriate norms.</description><identifier>ISSN: 0170-4214</identifier><identifier>EISSN: 1099-1476</identifier><identifier>DOI: 10.1002/mma.7509</identifier><language>eng</language><publisher>Freiburg: Wiley Subscription Services, Inc</publisher><subject>Computational fluid dynamics ; Dirichlet problem ; Elastic media ; Fluid flow ; Geological faults ; Incompressible flow ; integral equation ; Inverse problems ; inverse problems for PDEs ; Laplace equation ; Norms ; Stability</subject><ispartof>Mathematical methods in the applied sciences, 2021-09, Vol.44 (14), p.11498-11513</ispartof><rights>2021 John Wiley & Sons, Ltd.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2939-8284b07c9cbecfbc8d8f9f96f9d5935c9ede9055dac5eef358499179f7ed77a63</citedby><cites>FETCH-LOGICAL-c2939-8284b07c9cbecfbc8d8f9f96f9d5935c9ede9055dac5eef358499179f7ed77a63</cites><orcidid>0000-0001-9203-9583</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,778,782,27911,27912</link.rule.ids></links><search><creatorcontrib>Volkov, Darko</creatorcontrib><creatorcontrib>Jiang, Yulong</creatorcontrib><title>Stability properties of a crack inverse problem in half space</title><title>Mathematical methods in the applied sciences</title><description>We show in this paper a Lipschitz stability result for a crack inverse problem in half space. The direct problem is a Laplace equation with zero Neumann condition on the top boundary. The forcing term is a discontinuity across the crack. This formulation can be related to geological faults in elastic media or to irrotational incompressible flows in a half space minus an inner wall. The direct problem is well posed in an appropriate functional space. We study the related inverse problem where the jump across the crack is unknown, and more importantly, the geometry and the location of the crack are unknown. The data for the inverse problem are of Dirichlet type over a portion of the top boundary. We prove that this inverse problem is uniquely solvable under some assumptions on the geometry of the crack. The highlight of this paper is showing a stability result for this inverse problem. Assuming that the crack is planar, we show that reconstructing the plane containing the crack is Lipschitz stable despite the fact that the forcing term for the underlying PDE is unknown. This uniform stability result holds under the assumption that the forcing term is bounded above and the Dirichlet data are bounded below away from zero in appropriate norms.</description><subject>Computational fluid dynamics</subject><subject>Dirichlet problem</subject><subject>Elastic media</subject><subject>Fluid flow</subject><subject>Geological faults</subject><subject>Incompressible flow</subject><subject>integral equation</subject><subject>Inverse problems</subject><subject>inverse problems for PDEs</subject><subject>Laplace equation</subject><subject>Norms</subject><subject>Stability</subject><issn>0170-4214</issn><issn>1099-1476</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp10E1PwzAMBuAIgcQYSPyESFy4dDhp09QHDtPEl7SJA3CO0tQRHe1akg60f0_HuHKyLD-yrZexSwEzASBv2tbOtAI8YhMBiInIdH7MJiA0JJkU2Sk7i3ENAIUQcsJuXwZb1k097Hgfup7CUFPkneeWu2DdB683XxQi7adlQ-3Y83fbeB576-icnXjbRLr4q1P2dn_3unhMls8PT4v5MnESU0wKWWQlaIeuJOdLV1SFR4-5x0phqhxSRQhKVdYpIp-qIkMUGr2mSmubp1N2ddg7fvG5pTiYdbcNm_GkkSqHDKUuxKiuD8qFLsZA3vShbm3YGQFmH44ZwzH7cEaaHOh33dDuX2dWq_mv_wH-ZGU_</recordid><startdate>20210930</startdate><enddate>20210930</enddate><creator>Volkov, Darko</creator><creator>Jiang, Yulong</creator><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TB</scope><scope>8FD</scope><scope>FR3</scope><scope>JQ2</scope><scope>KR7</scope><orcidid>https://orcid.org/0000-0001-9203-9583</orcidid></search><sort><creationdate>20210930</creationdate><title>Stability properties of a crack inverse problem in half space</title><author>Volkov, Darko ; Jiang, Yulong</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2939-8284b07c9cbecfbc8d8f9f96f9d5935c9ede9055dac5eef358499179f7ed77a63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Computational fluid dynamics</topic><topic>Dirichlet problem</topic><topic>Elastic media</topic><topic>Fluid flow</topic><topic>Geological faults</topic><topic>Incompressible flow</topic><topic>integral equation</topic><topic>Inverse problems</topic><topic>inverse problems for PDEs</topic><topic>Laplace equation</topic><topic>Norms</topic><topic>Stability</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Volkov, Darko</creatorcontrib><creatorcontrib>Jiang, Yulong</creatorcontrib><collection>CrossRef</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>ProQuest Computer Science Collection</collection><collection>Civil Engineering Abstracts</collection><jtitle>Mathematical methods in the applied sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Volkov, Darko</au><au>Jiang, Yulong</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Stability properties of a crack inverse problem in half space</atitle><jtitle>Mathematical methods in the applied sciences</jtitle><date>2021-09-30</date><risdate>2021</risdate><volume>44</volume><issue>14</issue><spage>11498</spage><epage>11513</epage><pages>11498-11513</pages><issn>0170-4214</issn><eissn>1099-1476</eissn><abstract>We show in this paper a Lipschitz stability result for a crack inverse problem in half space. The direct problem is a Laplace equation with zero Neumann condition on the top boundary. The forcing term is a discontinuity across the crack. This formulation can be related to geological faults in elastic media or to irrotational incompressible flows in a half space minus an inner wall. The direct problem is well posed in an appropriate functional space. We study the related inverse problem where the jump across the crack is unknown, and more importantly, the geometry and the location of the crack are unknown. The data for the inverse problem are of Dirichlet type over a portion of the top boundary. We prove that this inverse problem is uniquely solvable under some assumptions on the geometry of the crack. The highlight of this paper is showing a stability result for this inverse problem. Assuming that the crack is planar, we show that reconstructing the plane containing the crack is Lipschitz stable despite the fact that the forcing term for the underlying PDE is unknown. This uniform stability result holds under the assumption that the forcing term is bounded above and the Dirichlet data are bounded below away from zero in appropriate norms.</abstract><cop>Freiburg</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1002/mma.7509</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0001-9203-9583</orcidid></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0170-4214 |
ispartof | Mathematical methods in the applied sciences, 2021-09, Vol.44 (14), p.11498-11513 |
issn | 0170-4214 1099-1476 |
language | eng |
recordid | cdi_proquest_journals_2560492781 |
source | Wiley |
subjects | Computational fluid dynamics Dirichlet problem Elastic media Fluid flow Geological faults Incompressible flow integral equation Inverse problems inverse problems for PDEs Laplace equation Norms Stability |
title | Stability properties of a crack inverse problem in half space |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-15T16%3A54%3A04IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Stability%20properties%20of%20a%20crack%20inverse%20problem%20in%20half%20space&rft.jtitle=Mathematical%20methods%20in%20the%20applied%20sciences&rft.au=Volkov,%20Darko&rft.date=2021-09-30&rft.volume=44&rft.issue=14&rft.spage=11498&rft.epage=11513&rft.pages=11498-11513&rft.issn=0170-4214&rft.eissn=1099-1476&rft_id=info:doi/10.1002/mma.7509&rft_dat=%3Cproquest_cross%3E2560492781%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c2939-8284b07c9cbecfbc8d8f9f96f9d5935c9ede9055dac5eef358499179f7ed77a63%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2560492781&rft_id=info:pmid/&rfr_iscdi=true |