Dynamic interpretation of the orientation relationships arising upon the α–ε–γ martensitic transformation via the transformation of {112}α planes
Abstract In this work, we have considered different variants of the formation of martensite crystals upon the α–ε transformation caused by the deformation of planes {112}α that leads to the symmetry of atomic arrangement typical of the basal planes {0001} ε of the ε phase within the dynamic theory o...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kashchenko, M. P. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2015 |
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| Übergeordnetes Werk: |
Enthalten in: The physics of metals and metallography - Pleiades Publishing, 1957, 116(2015), 10 vom: Okt., Seite 967-978 |
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| Übergeordnetes Werk: |
volume:116 ; year:2015 ; number:10 ; month:10 ; pages:967-978 |
| Links: |
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| DOI / URN: |
10.1134/S0031918X15100075 |
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OLC2060536510 |
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| 520 | |a Abstract In this work, we have considered different variants of the formation of martensite crystals upon the α–ε transformation caused by the deformation of planes {112}α that leads to the symmetry of atomic arrangement typical of the basal planes {0001} ε of the ε phase within the dynamic theory of martensitic transformations. It has been shown that there are dislocation nucleation centers that facilitate the start of the wave process responsible for the initiation of this deformation. The relatively rarely observed parallelism of three planes of different phases, namely, {112}α || {0001}ε || {112}γ, is interpreted as a consequence of the rapidly arising unstable intermediate state, which leads to the formation of coherently matched crystals of the γ and ε phases. The opportunity of the existence of the lattice parameter $${a_{{\varepsilon _2}}}$$ that exceeds the lattice parameter of the α phase is noted. | ||
| 650 | 4 | |a martensitic α–ε transformation | |
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| 700 | 1 | |a Chashchina, V. G. |4 aut | |
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10.1134/S0031918X15100075 doi (DE-627)OLC2060536510 (DE-He213)S0031918X15100075-p DE-627 ger DE-627 rakwb eng 530 VZ Kashchenko, M. P. verfasserin aut Dynamic interpretation of the orientation relationships arising upon the α–ε–γ martensitic transformation via the transformation of {112}α planes 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract In this work, we have considered different variants of the formation of martensite crystals upon the α–ε transformation caused by the deformation of planes {112}α that leads to the symmetry of atomic arrangement typical of the basal planes {0001} ε of the ε phase within the dynamic theory of martensitic transformations. It has been shown that there are dislocation nucleation centers that facilitate the start of the wave process responsible for the initiation of this deformation. The relatively rarely observed parallelism of three planes of different phases, namely, {112}α || {0001}ε || {112}γ, is interpreted as a consequence of the rapidly arising unstable intermediate state, which leads to the formation of coherently matched crystals of the γ and ε phases. The opportunity of the existence of the lattice parameter $${a_{{\varepsilon _2}}}$$ that exceeds the lattice parameter of the α phase is noted. martensitic α–ε transformation dynamic theory material orientational relationships Chashchina, V. G. aut Enthalten in The physics of metals and metallography Pleiades Publishing, 1957 116(2015), 10 vom: Okt., Seite 967-978 (DE-627)129504009 (DE-600)208858-7 (DE-576)014907313 0031-918X nnns volume:116 year:2015 number:10 month:10 pages:967-978 https://doi.org/10.1134/S0031918X15100075 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY GBV_ILN_70 AR 116 2015 10 10 967-978 |
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10.1134/S0031918X15100075 doi (DE-627)OLC2060536510 (DE-He213)S0031918X15100075-p DE-627 ger DE-627 rakwb eng 530 VZ Kashchenko, M. P. verfasserin aut Dynamic interpretation of the orientation relationships arising upon the α–ε–γ martensitic transformation via the transformation of {112}α planes 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract In this work, we have considered different variants of the formation of martensite crystals upon the α–ε transformation caused by the deformation of planes {112}α that leads to the symmetry of atomic arrangement typical of the basal planes {0001} ε of the ε phase within the dynamic theory of martensitic transformations. It has been shown that there are dislocation nucleation centers that facilitate the start of the wave process responsible for the initiation of this deformation. The relatively rarely observed parallelism of three planes of different phases, namely, {112}α || {0001}ε || {112}γ, is interpreted as a consequence of the rapidly arising unstable intermediate state, which leads to the formation of coherently matched crystals of the γ and ε phases. The opportunity of the existence of the lattice parameter $${a_{{\varepsilon _2}}}$$ that exceeds the lattice parameter of the α phase is noted. martensitic α–ε transformation dynamic theory material orientational relationships Chashchina, V. G. aut Enthalten in The physics of metals and metallography Pleiades Publishing, 1957 116(2015), 10 vom: Okt., Seite 967-978 (DE-627)129504009 (DE-600)208858-7 (DE-576)014907313 0031-918X nnns volume:116 year:2015 number:10 month:10 pages:967-978 https://doi.org/10.1134/S0031918X15100075 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY GBV_ILN_70 AR 116 2015 10 10 967-978 |
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10.1134/S0031918X15100075 doi (DE-627)OLC2060536510 (DE-He213)S0031918X15100075-p DE-627 ger DE-627 rakwb eng 530 VZ Kashchenko, M. P. verfasserin aut Dynamic interpretation of the orientation relationships arising upon the α–ε–γ martensitic transformation via the transformation of {112}α planes 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract In this work, we have considered different variants of the formation of martensite crystals upon the α–ε transformation caused by the deformation of planes {112}α that leads to the symmetry of atomic arrangement typical of the basal planes {0001} ε of the ε phase within the dynamic theory of martensitic transformations. It has been shown that there are dislocation nucleation centers that facilitate the start of the wave process responsible for the initiation of this deformation. The relatively rarely observed parallelism of three planes of different phases, namely, {112}α || {0001}ε || {112}γ, is interpreted as a consequence of the rapidly arising unstable intermediate state, which leads to the formation of coherently matched crystals of the γ and ε phases. The opportunity of the existence of the lattice parameter $${a_{{\varepsilon _2}}}$$ that exceeds the lattice parameter of the α phase is noted. martensitic α–ε transformation dynamic theory material orientational relationships Chashchina, V. G. aut Enthalten in The physics of metals and metallography Pleiades Publishing, 1957 116(2015), 10 vom: Okt., Seite 967-978 (DE-627)129504009 (DE-600)208858-7 (DE-576)014907313 0031-918X nnns volume:116 year:2015 number:10 month:10 pages:967-978 https://doi.org/10.1134/S0031918X15100075 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY GBV_ILN_70 AR 116 2015 10 10 967-978 |
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10.1134/S0031918X15100075 doi (DE-627)OLC2060536510 (DE-He213)S0031918X15100075-p DE-627 ger DE-627 rakwb eng 530 VZ Kashchenko, M. P. verfasserin aut Dynamic interpretation of the orientation relationships arising upon the α–ε–γ martensitic transformation via the transformation of {112}α planes 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract In this work, we have considered different variants of the formation of martensite crystals upon the α–ε transformation caused by the deformation of planes {112}α that leads to the symmetry of atomic arrangement typical of the basal planes {0001} ε of the ε phase within the dynamic theory of martensitic transformations. It has been shown that there are dislocation nucleation centers that facilitate the start of the wave process responsible for the initiation of this deformation. The relatively rarely observed parallelism of three planes of different phases, namely, {112}α || {0001}ε || {112}γ, is interpreted as a consequence of the rapidly arising unstable intermediate state, which leads to the formation of coherently matched crystals of the γ and ε phases. The opportunity of the existence of the lattice parameter $${a_{{\varepsilon _2}}}$$ that exceeds the lattice parameter of the α phase is noted. martensitic α–ε transformation dynamic theory material orientational relationships Chashchina, V. G. aut Enthalten in The physics of metals and metallography Pleiades Publishing, 1957 116(2015), 10 vom: Okt., Seite 967-978 (DE-627)129504009 (DE-600)208858-7 (DE-576)014907313 0031-918X nnns volume:116 year:2015 number:10 month:10 pages:967-978 https://doi.org/10.1134/S0031918X15100075 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY GBV_ILN_70 AR 116 2015 10 10 967-978 |
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10.1134/S0031918X15100075 doi (DE-627)OLC2060536510 (DE-He213)S0031918X15100075-p DE-627 ger DE-627 rakwb eng 530 VZ Kashchenko, M. P. verfasserin aut Dynamic interpretation of the orientation relationships arising upon the α–ε–γ martensitic transformation via the transformation of {112}α planes 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract In this work, we have considered different variants of the formation of martensite crystals upon the α–ε transformation caused by the deformation of planes {112}α that leads to the symmetry of atomic arrangement typical of the basal planes {0001} ε of the ε phase within the dynamic theory of martensitic transformations. It has been shown that there are dislocation nucleation centers that facilitate the start of the wave process responsible for the initiation of this deformation. The relatively rarely observed parallelism of three planes of different phases, namely, {112}α || {0001}ε || {112}γ, is interpreted as a consequence of the rapidly arising unstable intermediate state, which leads to the formation of coherently matched crystals of the γ and ε phases. The opportunity of the existence of the lattice parameter $${a_{{\varepsilon _2}}}$$ that exceeds the lattice parameter of the α phase is noted. martensitic α–ε transformation dynamic theory material orientational relationships Chashchina, V. G. aut Enthalten in The physics of metals and metallography Pleiades Publishing, 1957 116(2015), 10 vom: Okt., Seite 967-978 (DE-627)129504009 (DE-600)208858-7 (DE-576)014907313 0031-918X nnns volume:116 year:2015 number:10 month:10 pages:967-978 https://doi.org/10.1134/S0031918X15100075 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY GBV_ILN_70 AR 116 2015 10 10 967-978 |
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Dynamic interpretation of the orientation relationships arising upon the α–ε–γ martensitic transformation via the transformation of {112}α planes |
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Abstract In this work, we have considered different variants of the formation of martensite crystals upon the α–ε transformation caused by the deformation of planes {112}α that leads to the symmetry of atomic arrangement typical of the basal planes {0001} ε of the ε phase within the dynamic theory of martensitic transformations. It has been shown that there are dislocation nucleation centers that facilitate the start of the wave process responsible for the initiation of this deformation. The relatively rarely observed parallelism of three planes of different phases, namely, {112}α || {0001}ε || {112}γ, is interpreted as a consequence of the rapidly arising unstable intermediate state, which leads to the formation of coherently matched crystals of the γ and ε phases. The opportunity of the existence of the lattice parameter $${a_{{\varepsilon _2}}}$$ that exceeds the lattice parameter of the α phase is noted. © Pleiades Publishing, Ltd. 2015 |
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Abstract In this work, we have considered different variants of the formation of martensite crystals upon the α–ε transformation caused by the deformation of planes {112}α that leads to the symmetry of atomic arrangement typical of the basal planes {0001} ε of the ε phase within the dynamic theory of martensitic transformations. It has been shown that there are dislocation nucleation centers that facilitate the start of the wave process responsible for the initiation of this deformation. The relatively rarely observed parallelism of three planes of different phases, namely, {112}α || {0001}ε || {112}γ, is interpreted as a consequence of the rapidly arising unstable intermediate state, which leads to the formation of coherently matched crystals of the γ and ε phases. The opportunity of the existence of the lattice parameter $${a_{{\varepsilon _2}}}$$ that exceeds the lattice parameter of the α phase is noted. © Pleiades Publishing, Ltd. 2015 |
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Abstract In this work, we have considered different variants of the formation of martensite crystals upon the α–ε transformation caused by the deformation of planes {112}α that leads to the symmetry of atomic arrangement typical of the basal planes {0001} ε of the ε phase within the dynamic theory of martensitic transformations. It has been shown that there are dislocation nucleation centers that facilitate the start of the wave process responsible for the initiation of this deformation. The relatively rarely observed parallelism of three planes of different phases, namely, {112}α || {0001}ε || {112}γ, is interpreted as a consequence of the rapidly arising unstable intermediate state, which leads to the formation of coherently matched crystals of the γ and ε phases. The opportunity of the existence of the lattice parameter $${a_{{\varepsilon _2}}}$$ that exceeds the lattice parameter of the α phase is noted. © Pleiades Publishing, Ltd. 2015 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2060536510</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230401091450.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2015 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1134/S0031918X15100075</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2060536510</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)S0031918X15100075-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">530</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Kashchenko, M. P.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Dynamic interpretation of the orientation relationships arising upon the α–ε–γ martensitic transformation via the transformation of {112}α planes</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Pleiades Publishing, Ltd. 2015</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract In this work, we have considered different variants of the formation of martensite crystals upon the α–ε transformation caused by the deformation of planes {112}α that leads to the symmetry of atomic arrangement typical of the basal planes {0001} ε of the ε phase within the dynamic theory of martensitic transformations. It has been shown that there are dislocation nucleation centers that facilitate the start of the wave process responsible for the initiation of this deformation. The relatively rarely observed parallelism of three planes of different phases, namely, {112}α || {0001}ε || {112}γ, is interpreted as a consequence of the rapidly arising unstable intermediate state, which leads to the formation of coherently matched crystals of the γ and ε phases. The opportunity of the existence of the lattice parameter $${a_{{\varepsilon _2}}}$$ that exceeds the lattice parameter of the α phase is noted.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">martensitic α–ε transformation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">dynamic theory</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">material orientational relationships</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Chashchina, V. G.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">The physics of metals and metallography</subfield><subfield code="d">Pleiades Publishing, 1957</subfield><subfield code="g">116(2015), 10 vom: Okt., Seite 967-978</subfield><subfield code="w">(DE-627)129504009</subfield><subfield code="w">(DE-600)208858-7</subfield><subfield code="w">(DE-576)014907313</subfield><subfield code="x">0031-918X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:116</subfield><subfield code="g">year:2015</subfield><subfield code="g">number:10</subfield><subfield code="g">month:10</subfield><subfield code="g">pages:967-978</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1134/S0031918X15100075</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-TEC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">116</subfield><subfield code="j">2015</subfield><subfield code="e">10</subfield><subfield code="c">10</subfield><subfield code="h">967-978</subfield></datafield></record></collection>
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