Extrapolation and phase correction of non-uniformly broadened signals
•A numerical method for restoration of heterogeneously broadened NMR-signals is proposed.•The method can be used as an automatic phase-corrector and a low-pass filter.•We propose a fast MRI-protocol with zero echo time, based on the method. The initial part of FID-signals cannot always be acquired e...
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Veröffentlicht in: | Journal of magnetic resonance (1997) 2013-08, Vol.233, p.64-73 |
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container_title | Journal of magnetic resonance (1997) |
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creator | Rodts, Stéphane Bytchenkoff, Dimitri |
description | •A numerical method for restoration of heterogeneously broadened NMR-signals is proposed.•The method can be used as an automatic phase-corrector and a low-pass filter.•We propose a fast MRI-protocol with zero echo time, based on the method.
The initial part of FID-signals cannot always be acquired experimentally. This is particularly true for signals characterised by strong inhomogeneous broadening, such as those in porous materials, e.g. cements, soils and rocks, those measured by portable NMR-apparatus, or EPR-signals. Here we report on a numerical method we designed to extrapolate those initial missing parts, i.e. to retrieve their amplitude and phase. Should the entire signal be available from an experiment, the algorithm can still be used as an automatic phase-corrector and a low-pass filter. The method is based on the use of cardinal series, applies to any oversampled signals and requires no prior knowledge of the system under study. We show that the method can also be used to restore entire one-dimensional MRI-data sets from those in which less than half of the k-space was sampled, thus not only potentially allowing to speed up data acquisition – when extended to two or three dimensions, but also to circumvent phase-distortions usually encountered when exploring the k-space near its origin. |
doi_str_mv | 10.1016/j.jmr.2013.05.003 |
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The initial part of FID-signals cannot always be acquired experimentally. This is particularly true for signals characterised by strong inhomogeneous broadening, such as those in porous materials, e.g. cements, soils and rocks, those measured by portable NMR-apparatus, or EPR-signals. Here we report on a numerical method we designed to extrapolate those initial missing parts, i.e. to retrieve their amplitude and phase. Should the entire signal be available from an experiment, the algorithm can still be used as an automatic phase-corrector and a low-pass filter. The method is based on the use of cardinal series, applies to any oversampled signals and requires no prior knowledge of the system under study. We show that the method can also be used to restore entire one-dimensional MRI-data sets from those in which less than half of the k-space was sampled, thus not only potentially allowing to speed up data acquisition – when extended to two or three dimensions, but also to circumvent phase-distortions usually encountered when exploring the k-space near its origin.</description><identifier>ISSN: 1090-7807</identifier><identifier>EISSN: 1096-0856</identifier><identifier>DOI: 10.1016/j.jmr.2013.05.003</identifier><identifier>PMID: 23735873</identifier><language>eng</language><publisher>United States: Elsevier Inc</publisher><subject>Bayesian ; Cardinal series ; Cements ; Computer Science ; Engineering Sciences ; Extrapolation ; Low pass filters ; Materials ; MRI ; Origins ; Oversampling ; Phase-correction ; Porous ; Porous materials ; Rocks ; Signal and Image processing ; Soils ; Three dimensional</subject><ispartof>Journal of magnetic resonance (1997), 2013-08, Vol.233, p.64-73</ispartof><rights>2013 Elsevier Inc.</rights><rights>Copyright © 2013 Elsevier Inc. All rights reserved.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c420t-26bb78435b6775e521434751c121fb9dc16e128eb7f8e99ce3538f9c1800fb6e3</citedby><cites>FETCH-LOGICAL-c420t-26bb78435b6775e521434751c121fb9dc16e128eb7f8e99ce3538f9c1800fb6e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S1090780713001134$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,314,776,780,881,3536,27902,27903,65308</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/23735873$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink><backlink>$$Uhttps://enpc.hal.science/hal-00946099$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Rodts, Stéphane</creatorcontrib><creatorcontrib>Bytchenkoff, Dimitri</creatorcontrib><title>Extrapolation and phase correction of non-uniformly broadened signals</title><title>Journal of magnetic resonance (1997)</title><addtitle>J Magn Reson</addtitle><description>•A numerical method for restoration of heterogeneously broadened NMR-signals is proposed.•The method can be used as an automatic phase-corrector and a low-pass filter.•We propose a fast MRI-protocol with zero echo time, based on the method.
The initial part of FID-signals cannot always be acquired experimentally. This is particularly true for signals characterised by strong inhomogeneous broadening, such as those in porous materials, e.g. cements, soils and rocks, those measured by portable NMR-apparatus, or EPR-signals. Here we report on a numerical method we designed to extrapolate those initial missing parts, i.e. to retrieve their amplitude and phase. Should the entire signal be available from an experiment, the algorithm can still be used as an automatic phase-corrector and a low-pass filter. The method is based on the use of cardinal series, applies to any oversampled signals and requires no prior knowledge of the system under study. We show that the method can also be used to restore entire one-dimensional MRI-data sets from those in which less than half of the k-space was sampled, thus not only potentially allowing to speed up data acquisition – when extended to two or three dimensions, but also to circumvent phase-distortions usually encountered when exploring the k-space near its origin.</description><subject>Bayesian</subject><subject>Cardinal series</subject><subject>Cements</subject><subject>Computer Science</subject><subject>Engineering Sciences</subject><subject>Extrapolation</subject><subject>Low pass filters</subject><subject>Materials</subject><subject>MRI</subject><subject>Origins</subject><subject>Oversampling</subject><subject>Phase-correction</subject><subject>Porous</subject><subject>Porous materials</subject><subject>Rocks</subject><subject>Signal and Image processing</subject><subject>Soils</subject><subject>Three dimensional</subject><issn>1090-7807</issn><issn>1096-0856</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNqFkU1v1DAQhiMEoh_wA7igHOGQMGPHsS1OVbW0lVbqBc6W40yoV4m92LsV_fd4u22P9DSj0TOvRvNU1SeEFgH7b5t2s6SWAfIWRAvA31SnCLpvQIn-7WMPjVQgT6qznDcAiELC--qEccmFkvy0Wq3-7pLdxtnufAy1DWO9vbOZahdTIvc4jFMdYmj2wU8xLfNDPaRoRwo01tn_DnbOH6p3Uyn08ameV79-rH5eXjfr26uby4t14zoGu4b1wyBVx8XQSylIMOx4JwU6ZDgNenTYEzJFg5wUae2IC64m7VABTENP_Lz6esy9s7PZJr_Y9GCi9eb6Ym0OMwDd9aD1PRb2y5HdpvhnT3lnFp8dzbMNFPfZoNScKdYL_Trald9q1SErKB5Rl2LOiaaXMxDMQYrZmCLFHKQYEOUgXnY-P8Xvh4XGl41nCwX4fgSo_O7eUzLZeQqORn9wYMbo_xP_D6ErmuE</recordid><startdate>20130801</startdate><enddate>20130801</enddate><creator>Rodts, Stéphane</creator><creator>Bytchenkoff, Dimitri</creator><general>Elsevier Inc</general><general>Elsevier</general><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope><scope>7U5</scope><scope>8FD</scope><scope>L7M</scope><scope>1XC</scope></search><sort><creationdate>20130801</creationdate><title>Extrapolation and phase correction of non-uniformly broadened signals</title><author>Rodts, Stéphane ; Bytchenkoff, Dimitri</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c420t-26bb78435b6775e521434751c121fb9dc16e128eb7f8e99ce3538f9c1800fb6e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Bayesian</topic><topic>Cardinal series</topic><topic>Cements</topic><topic>Computer Science</topic><topic>Engineering Sciences</topic><topic>Extrapolation</topic><topic>Low pass filters</topic><topic>Materials</topic><topic>MRI</topic><topic>Origins</topic><topic>Oversampling</topic><topic>Phase-correction</topic><topic>Porous</topic><topic>Porous materials</topic><topic>Rocks</topic><topic>Signal and Image processing</topic><topic>Soils</topic><topic>Three dimensional</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Rodts, Stéphane</creatorcontrib><creatorcontrib>Bytchenkoff, Dimitri</creatorcontrib><collection>PubMed</collection><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Technology Research Database</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Journal of magnetic resonance (1997)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Rodts, Stéphane</au><au>Bytchenkoff, Dimitri</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Extrapolation and phase correction of non-uniformly broadened signals</atitle><jtitle>Journal of magnetic resonance (1997)</jtitle><addtitle>J Magn Reson</addtitle><date>2013-08-01</date><risdate>2013</risdate><volume>233</volume><spage>64</spage><epage>73</epage><pages>64-73</pages><issn>1090-7807</issn><eissn>1096-0856</eissn><abstract>•A numerical method for restoration of heterogeneously broadened NMR-signals is proposed.•The method can be used as an automatic phase-corrector and a low-pass filter.•We propose a fast MRI-protocol with zero echo time, based on the method.
The initial part of FID-signals cannot always be acquired experimentally. This is particularly true for signals characterised by strong inhomogeneous broadening, such as those in porous materials, e.g. cements, soils and rocks, those measured by portable NMR-apparatus, or EPR-signals. Here we report on a numerical method we designed to extrapolate those initial missing parts, i.e. to retrieve their amplitude and phase. Should the entire signal be available from an experiment, the algorithm can still be used as an automatic phase-corrector and a low-pass filter. The method is based on the use of cardinal series, applies to any oversampled signals and requires no prior knowledge of the system under study. We show that the method can also be used to restore entire one-dimensional MRI-data sets from those in which less than half of the k-space was sampled, thus not only potentially allowing to speed up data acquisition – when extended to two or three dimensions, but also to circumvent phase-distortions usually encountered when exploring the k-space near its origin.</abstract><cop>United States</cop><pub>Elsevier Inc</pub><pmid>23735873</pmid><doi>10.1016/j.jmr.2013.05.003</doi><tpages>10</tpages></addata></record> |
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subjects | Bayesian Cardinal series Cements Computer Science Engineering Sciences Extrapolation Low pass filters Materials MRI Origins Oversampling Phase-correction Porous Porous materials Rocks Signal and Image processing Soils Three dimensional |
title | Extrapolation and phase correction of non-uniformly broadened signals |
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