Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3
Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at high pressure using diamond anvil cells at room temperature. Pressure dependence of Raman peaks assignable to the symmetric stretching vibration modes of...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Maruyama, Koji [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2017 |
|---|
| Rechteinformationen: |
Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. |
|---|
| Schlagwörter: |
|---|
| Übergeordnetes Werk: |
Enthalten in: Journal of Raman spectroscopy - Chichester [u.a.] : Wiley, 1973, 48(2017), 11, Seite 1449-1453 |
|---|---|
| Übergeordnetes Werk: |
volume:48 ; year:2017 ; number:11 ; pages:1449-1453 |
| Links: |
|---|
| DOI / URN: |
10.1002/jrs.5162 |
|---|
| Katalog-ID: |
OLC1998935590 |
|---|
| LEADER | 01000caa a2200265 4500 | ||
|---|---|---|---|
| 001 | OLC1998935590 | ||
| 003 | DE-627 | ||
| 005 | 20230516175941.0 | ||
| 007 | tu | ||
| 008 | 171228s2017 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1002/jrs.5162 |2 doi | |
| 028 | 5 | 2 | |a PQ20171228 |
| 035 | |a (DE-627)OLC1998935590 | ||
| 035 | |a (DE-599)GBVOLC1998935590 | ||
| 035 | |a (PRQ)p1312-ae683b2b55fe27692633fb098fa8a1f252860141bcf1696da17f9142e78fe10a3 | ||
| 035 | |a (KEY)0047158520170000048001101449pressureinducedphasetransitionsofvateriteametastab | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 540 |q DE-600 |
| 084 | |a 35.25 |2 bkl | ||
| 084 | |a 33.07 |2 bkl | ||
| 100 | 1 | |a Maruyama, Koji |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3 |
| 264 | 1 | |c 2017 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 520 | |a Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at high pressure using diamond anvil cells at room temperature. Pressure dependence of Raman peaks assignable to the symmetric stretching vibration modes of carbonate ion indicated the phase transitions of vaterite. At 4.3 GPa, vaterite (vaterite I) transformed to a high‐pressure form of vaterite (vaterite II). With increasing pressure, a part of vaterite II gradually transformed to calcite III, and the remainder of vaterite II transformed to another new phase (vaterite III). The phase transition from vaterite II to calcite III was irreversible, and calcite III back‐transformed to calcite I during decompression. Moreover, at the pressures higher than 13.1 GPa, several diffraction spots were observed on an imaging plate, indicating another phase transition from vaterite III to a phase having coarse grains (vaterite IV). Our results indicate that vaterite undergoes more complex phase transitions at high pressure than other polymorphs of calcium carbonate, calcite, and aragonite. These phase transitions of vaterite will open a window to understanding phase transitions of metastable minerals at high pressure. Copyright © 2017 John Wiley & Sons, Ltd. Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at room temperature. At 4.3 GPa, vaterite transformed to vaterite II. With increasing pressure, a part of vaterite II transformed to calcite III, and the remainder of vaterite II transformed to vaterite III. The phase transition from vaterite II to calcite III was irreversible. At pressures higher than 13.1 GPa, another phase transition from vaterite III to vaterite IV was found. | ||
| 540 | |a Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. | ||
| 650 | 4 | |a phase transition | |
| 650 | 4 | |a calcium carbonate | |
| 650 | 4 | |a high pressure | |
| 650 | 4 | |a calcite | |
| 650 | 4 | |a vaterite | |
| 650 | 4 | |a Vibration mode | |
| 650 | 4 | |a Decompression | |
| 650 | 4 | |a Calcium | |
| 650 | 4 | |a High pressure | |
| 650 | 4 | |a Phase transformations | |
| 650 | 4 | |a Calcite | |
| 650 | 4 | |a Diamonds | |
| 650 | 4 | |a X-ray diffraction | |
| 650 | 4 | |a Aragonite | |
| 650 | 4 | |a Diffraction patterns | |
| 650 | 4 | |a Phase transitions | |
| 650 | 4 | |a Raman spectroscopy | |
| 650 | 4 | |a Calcium carbonate | |
| 650 | 4 | |a Spots | |
| 650 | 4 | |a Raman spectra | |
| 650 | 4 | |a Diamond anvil cells | |
| 650 | 4 | |a Vibration | |
| 650 | 4 | |a Metastable phases | |
| 650 | 4 | |a Phase transition | |
| 650 | 4 | |a Pressure dependence | |
| 650 | 4 | |a Diffraction | |
| 650 | 4 | |a Pressure | |
| 650 | 4 | |a Minerals | |
| 700 | 1 | |a Kagi, Hiroyuki |4 oth | |
| 700 | 1 | |a Komatsu, Kazuki |4 oth | |
| 700 | 1 | |a Yoshino, Toru |4 oth | |
| 700 | 1 | |a Nakano, Satoshi |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |t Journal of Raman spectroscopy |d Chichester [u.a.] : Wiley, 1973 |g 48(2017), 11, Seite 1449-1453 |w (DE-627)129391832 |w (DE-600)184918-9 |w (DE-576)014776979 |x 0377-0486 |7 nnns |
| 773 | 1 | 8 | |g volume:48 |g year:2017 |g number:11 |g pages:1449-1453 |
| 856 | 4 | 1 | |u http://dx.doi.org/10.1002/jrs.5162 |3 Volltext |
| 856 | 4 | 2 | |u http://onlinelibrary.wiley.com/doi/10.1002/jrs.5162/abstract |
| 856 | 4 | 2 | |u https://search.proquest.com/docview/1967712082 |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-PHY | ||
| 912 | |a SSG-OLC-CHE | ||
| 912 | |a SSG-OLC-PHA | ||
| 912 | |a SSG-OLC-DE-84 | ||
| 912 | |a GBV_ILN_70 | ||
| 936 | b | k | |a 35.25 |q AVZ |
| 936 | b | k | |a 33.07 |q AVZ |
| 951 | |a AR | ||
| 952 | |d 48 |j 2017 |e 11 |h 1449-1453 | ||
| author_variant |
k m km |
|---|---|
| matchkey_str |
article:03770486:2017----::rsuenuepaerniinovtrtaeat |
| hierarchy_sort_str |
2017 |
| bklnumber |
35.25 33.07 |
| publishDate |
2017 |
| allfields |
10.1002/jrs.5162 doi PQ20171228 (DE-627)OLC1998935590 (DE-599)GBVOLC1998935590 (PRQ)p1312-ae683b2b55fe27692633fb098fa8a1f252860141bcf1696da17f9142e78fe10a3 (KEY)0047158520170000048001101449pressureinducedphasetransitionsofvateriteametastab DE-627 ger DE-627 rakwb eng 540 DE-600 35.25 bkl 33.07 bkl Maruyama, Koji verfasserin aut Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at high pressure using diamond anvil cells at room temperature. Pressure dependence of Raman peaks assignable to the symmetric stretching vibration modes of carbonate ion indicated the phase transitions of vaterite. At 4.3 GPa, vaterite (vaterite I) transformed to a high‐pressure form of vaterite (vaterite II). With increasing pressure, a part of vaterite II gradually transformed to calcite III, and the remainder of vaterite II transformed to another new phase (vaterite III). The phase transition from vaterite II to calcite III was irreversible, and calcite III back‐transformed to calcite I during decompression. Moreover, at the pressures higher than 13.1 GPa, several diffraction spots were observed on an imaging plate, indicating another phase transition from vaterite III to a phase having coarse grains (vaterite IV). Our results indicate that vaterite undergoes more complex phase transitions at high pressure than other polymorphs of calcium carbonate, calcite, and aragonite. These phase transitions of vaterite will open a window to understanding phase transitions of metastable minerals at high pressure. Copyright © 2017 John Wiley & Sons, Ltd. Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at room temperature. At 4.3 GPa, vaterite transformed to vaterite II. With increasing pressure, a part of vaterite II transformed to calcite III, and the remainder of vaterite II transformed to vaterite III. The phase transition from vaterite II to calcite III was irreversible. At pressures higher than 13.1 GPa, another phase transition from vaterite III to vaterite IV was found. Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. phase transition calcium carbonate high pressure calcite vaterite Vibration mode Decompression Calcium High pressure Phase transformations Calcite Diamonds X-ray diffraction Aragonite Diffraction patterns Phase transitions Raman spectroscopy Calcium carbonate Spots Raman spectra Diamond anvil cells Vibration Metastable phases Phase transition Pressure dependence Diffraction Pressure Minerals Kagi, Hiroyuki oth Komatsu, Kazuki oth Yoshino, Toru oth Nakano, Satoshi oth Enthalten in Journal of Raman spectroscopy Chichester [u.a.] : Wiley, 1973 48(2017), 11, Seite 1449-1453 (DE-627)129391832 (DE-600)184918-9 (DE-576)014776979 0377-0486 nnns volume:48 year:2017 number:11 pages:1449-1453 http://dx.doi.org/10.1002/jrs.5162 Volltext http://onlinelibrary.wiley.com/doi/10.1002/jrs.5162/abstract https://search.proquest.com/docview/1967712082 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-PHA SSG-OLC-DE-84 GBV_ILN_70 35.25 AVZ 33.07 AVZ AR 48 2017 11 1449-1453 |
| spelling |
10.1002/jrs.5162 doi PQ20171228 (DE-627)OLC1998935590 (DE-599)GBVOLC1998935590 (PRQ)p1312-ae683b2b55fe27692633fb098fa8a1f252860141bcf1696da17f9142e78fe10a3 (KEY)0047158520170000048001101449pressureinducedphasetransitionsofvateriteametastab DE-627 ger DE-627 rakwb eng 540 DE-600 35.25 bkl 33.07 bkl Maruyama, Koji verfasserin aut Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at high pressure using diamond anvil cells at room temperature. Pressure dependence of Raman peaks assignable to the symmetric stretching vibration modes of carbonate ion indicated the phase transitions of vaterite. At 4.3 GPa, vaterite (vaterite I) transformed to a high‐pressure form of vaterite (vaterite II). With increasing pressure, a part of vaterite II gradually transformed to calcite III, and the remainder of vaterite II transformed to another new phase (vaterite III). The phase transition from vaterite II to calcite III was irreversible, and calcite III back‐transformed to calcite I during decompression. Moreover, at the pressures higher than 13.1 GPa, several diffraction spots were observed on an imaging plate, indicating another phase transition from vaterite III to a phase having coarse grains (vaterite IV). Our results indicate that vaterite undergoes more complex phase transitions at high pressure than other polymorphs of calcium carbonate, calcite, and aragonite. These phase transitions of vaterite will open a window to understanding phase transitions of metastable minerals at high pressure. Copyright © 2017 John Wiley & Sons, Ltd. Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at room temperature. At 4.3 GPa, vaterite transformed to vaterite II. With increasing pressure, a part of vaterite II transformed to calcite III, and the remainder of vaterite II transformed to vaterite III. The phase transition from vaterite II to calcite III was irreversible. At pressures higher than 13.1 GPa, another phase transition from vaterite III to vaterite IV was found. Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. phase transition calcium carbonate high pressure calcite vaterite Vibration mode Decompression Calcium High pressure Phase transformations Calcite Diamonds X-ray diffraction Aragonite Diffraction patterns Phase transitions Raman spectroscopy Calcium carbonate Spots Raman spectra Diamond anvil cells Vibration Metastable phases Phase transition Pressure dependence Diffraction Pressure Minerals Kagi, Hiroyuki oth Komatsu, Kazuki oth Yoshino, Toru oth Nakano, Satoshi oth Enthalten in Journal of Raman spectroscopy Chichester [u.a.] : Wiley, 1973 48(2017), 11, Seite 1449-1453 (DE-627)129391832 (DE-600)184918-9 (DE-576)014776979 0377-0486 nnns volume:48 year:2017 number:11 pages:1449-1453 http://dx.doi.org/10.1002/jrs.5162 Volltext http://onlinelibrary.wiley.com/doi/10.1002/jrs.5162/abstract https://search.proquest.com/docview/1967712082 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-PHA SSG-OLC-DE-84 GBV_ILN_70 35.25 AVZ 33.07 AVZ AR 48 2017 11 1449-1453 |
| allfields_unstemmed |
10.1002/jrs.5162 doi PQ20171228 (DE-627)OLC1998935590 (DE-599)GBVOLC1998935590 (PRQ)p1312-ae683b2b55fe27692633fb098fa8a1f252860141bcf1696da17f9142e78fe10a3 (KEY)0047158520170000048001101449pressureinducedphasetransitionsofvateriteametastab DE-627 ger DE-627 rakwb eng 540 DE-600 35.25 bkl 33.07 bkl Maruyama, Koji verfasserin aut Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at high pressure using diamond anvil cells at room temperature. Pressure dependence of Raman peaks assignable to the symmetric stretching vibration modes of carbonate ion indicated the phase transitions of vaterite. At 4.3 GPa, vaterite (vaterite I) transformed to a high‐pressure form of vaterite (vaterite II). With increasing pressure, a part of vaterite II gradually transformed to calcite III, and the remainder of vaterite II transformed to another new phase (vaterite III). The phase transition from vaterite II to calcite III was irreversible, and calcite III back‐transformed to calcite I during decompression. Moreover, at the pressures higher than 13.1 GPa, several diffraction spots were observed on an imaging plate, indicating another phase transition from vaterite III to a phase having coarse grains (vaterite IV). Our results indicate that vaterite undergoes more complex phase transitions at high pressure than other polymorphs of calcium carbonate, calcite, and aragonite. These phase transitions of vaterite will open a window to understanding phase transitions of metastable minerals at high pressure. Copyright © 2017 John Wiley & Sons, Ltd. Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at room temperature. At 4.3 GPa, vaterite transformed to vaterite II. With increasing pressure, a part of vaterite II transformed to calcite III, and the remainder of vaterite II transformed to vaterite III. The phase transition from vaterite II to calcite III was irreversible. At pressures higher than 13.1 GPa, another phase transition from vaterite III to vaterite IV was found. Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. phase transition calcium carbonate high pressure calcite vaterite Vibration mode Decompression Calcium High pressure Phase transformations Calcite Diamonds X-ray diffraction Aragonite Diffraction patterns Phase transitions Raman spectroscopy Calcium carbonate Spots Raman spectra Diamond anvil cells Vibration Metastable phases Phase transition Pressure dependence Diffraction Pressure Minerals Kagi, Hiroyuki oth Komatsu, Kazuki oth Yoshino, Toru oth Nakano, Satoshi oth Enthalten in Journal of Raman spectroscopy Chichester [u.a.] : Wiley, 1973 48(2017), 11, Seite 1449-1453 (DE-627)129391832 (DE-600)184918-9 (DE-576)014776979 0377-0486 nnns volume:48 year:2017 number:11 pages:1449-1453 http://dx.doi.org/10.1002/jrs.5162 Volltext http://onlinelibrary.wiley.com/doi/10.1002/jrs.5162/abstract https://search.proquest.com/docview/1967712082 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-PHA SSG-OLC-DE-84 GBV_ILN_70 35.25 AVZ 33.07 AVZ AR 48 2017 11 1449-1453 |
| allfieldsGer |
10.1002/jrs.5162 doi PQ20171228 (DE-627)OLC1998935590 (DE-599)GBVOLC1998935590 (PRQ)p1312-ae683b2b55fe27692633fb098fa8a1f252860141bcf1696da17f9142e78fe10a3 (KEY)0047158520170000048001101449pressureinducedphasetransitionsofvateriteametastab DE-627 ger DE-627 rakwb eng 540 DE-600 35.25 bkl 33.07 bkl Maruyama, Koji verfasserin aut Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at high pressure using diamond anvil cells at room temperature. Pressure dependence of Raman peaks assignable to the symmetric stretching vibration modes of carbonate ion indicated the phase transitions of vaterite. At 4.3 GPa, vaterite (vaterite I) transformed to a high‐pressure form of vaterite (vaterite II). With increasing pressure, a part of vaterite II gradually transformed to calcite III, and the remainder of vaterite II transformed to another new phase (vaterite III). The phase transition from vaterite II to calcite III was irreversible, and calcite III back‐transformed to calcite I during decompression. Moreover, at the pressures higher than 13.1 GPa, several diffraction spots were observed on an imaging plate, indicating another phase transition from vaterite III to a phase having coarse grains (vaterite IV). Our results indicate that vaterite undergoes more complex phase transitions at high pressure than other polymorphs of calcium carbonate, calcite, and aragonite. These phase transitions of vaterite will open a window to understanding phase transitions of metastable minerals at high pressure. Copyright © 2017 John Wiley & Sons, Ltd. Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at room temperature. At 4.3 GPa, vaterite transformed to vaterite II. With increasing pressure, a part of vaterite II transformed to calcite III, and the remainder of vaterite II transformed to vaterite III. The phase transition from vaterite II to calcite III was irreversible. At pressures higher than 13.1 GPa, another phase transition from vaterite III to vaterite IV was found. Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. phase transition calcium carbonate high pressure calcite vaterite Vibration mode Decompression Calcium High pressure Phase transformations Calcite Diamonds X-ray diffraction Aragonite Diffraction patterns Phase transitions Raman spectroscopy Calcium carbonate Spots Raman spectra Diamond anvil cells Vibration Metastable phases Phase transition Pressure dependence Diffraction Pressure Minerals Kagi, Hiroyuki oth Komatsu, Kazuki oth Yoshino, Toru oth Nakano, Satoshi oth Enthalten in Journal of Raman spectroscopy Chichester [u.a.] : Wiley, 1973 48(2017), 11, Seite 1449-1453 (DE-627)129391832 (DE-600)184918-9 (DE-576)014776979 0377-0486 nnns volume:48 year:2017 number:11 pages:1449-1453 http://dx.doi.org/10.1002/jrs.5162 Volltext http://onlinelibrary.wiley.com/doi/10.1002/jrs.5162/abstract https://search.proquest.com/docview/1967712082 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-PHA SSG-OLC-DE-84 GBV_ILN_70 35.25 AVZ 33.07 AVZ AR 48 2017 11 1449-1453 |
| allfieldsSound |
10.1002/jrs.5162 doi PQ20171228 (DE-627)OLC1998935590 (DE-599)GBVOLC1998935590 (PRQ)p1312-ae683b2b55fe27692633fb098fa8a1f252860141bcf1696da17f9142e78fe10a3 (KEY)0047158520170000048001101449pressureinducedphasetransitionsofvateriteametastab DE-627 ger DE-627 rakwb eng 540 DE-600 35.25 bkl 33.07 bkl Maruyama, Koji verfasserin aut Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at high pressure using diamond anvil cells at room temperature. Pressure dependence of Raman peaks assignable to the symmetric stretching vibration modes of carbonate ion indicated the phase transitions of vaterite. At 4.3 GPa, vaterite (vaterite I) transformed to a high‐pressure form of vaterite (vaterite II). With increasing pressure, a part of vaterite II gradually transformed to calcite III, and the remainder of vaterite II transformed to another new phase (vaterite III). The phase transition from vaterite II to calcite III was irreversible, and calcite III back‐transformed to calcite I during decompression. Moreover, at the pressures higher than 13.1 GPa, several diffraction spots were observed on an imaging plate, indicating another phase transition from vaterite III to a phase having coarse grains (vaterite IV). Our results indicate that vaterite undergoes more complex phase transitions at high pressure than other polymorphs of calcium carbonate, calcite, and aragonite. These phase transitions of vaterite will open a window to understanding phase transitions of metastable minerals at high pressure. Copyright © 2017 John Wiley & Sons, Ltd. Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at room temperature. At 4.3 GPa, vaterite transformed to vaterite II. With increasing pressure, a part of vaterite II transformed to calcite III, and the remainder of vaterite II transformed to vaterite III. The phase transition from vaterite II to calcite III was irreversible. At pressures higher than 13.1 GPa, another phase transition from vaterite III to vaterite IV was found. Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. phase transition calcium carbonate high pressure calcite vaterite Vibration mode Decompression Calcium High pressure Phase transformations Calcite Diamonds X-ray diffraction Aragonite Diffraction patterns Phase transitions Raman spectroscopy Calcium carbonate Spots Raman spectra Diamond anvil cells Vibration Metastable phases Phase transition Pressure dependence Diffraction Pressure Minerals Kagi, Hiroyuki oth Komatsu, Kazuki oth Yoshino, Toru oth Nakano, Satoshi oth Enthalten in Journal of Raman spectroscopy Chichester [u.a.] : Wiley, 1973 48(2017), 11, Seite 1449-1453 (DE-627)129391832 (DE-600)184918-9 (DE-576)014776979 0377-0486 nnns volume:48 year:2017 number:11 pages:1449-1453 http://dx.doi.org/10.1002/jrs.5162 Volltext http://onlinelibrary.wiley.com/doi/10.1002/jrs.5162/abstract https://search.proquest.com/docview/1967712082 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-PHA SSG-OLC-DE-84 GBV_ILN_70 35.25 AVZ 33.07 AVZ AR 48 2017 11 1449-1453 |
| language |
English |
| source |
Enthalten in Journal of Raman spectroscopy 48(2017), 11, Seite 1449-1453 volume:48 year:2017 number:11 pages:1449-1453 |
| sourceStr |
Enthalten in Journal of Raman spectroscopy 48(2017), 11, Seite 1449-1453 volume:48 year:2017 number:11 pages:1449-1453 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
phase transition calcium carbonate high pressure calcite vaterite Vibration mode Decompression Calcium High pressure Phase transformations Calcite Diamonds X-ray diffraction Aragonite Diffraction patterns Phase transitions Raman spectroscopy Calcium carbonate Spots Raman spectra Diamond anvil cells Vibration Metastable phases Phase transition Pressure dependence Diffraction Pressure Minerals |
| dewey-raw |
540 |
| isfreeaccess_bool |
false |
| container_title |
Journal of Raman spectroscopy |
| authorswithroles_txt_mv |
Maruyama, Koji @@aut@@ Kagi, Hiroyuki @@oth@@ Komatsu, Kazuki @@oth@@ Yoshino, Toru @@oth@@ Nakano, Satoshi @@oth@@ |
| publishDateDaySort_date |
2017-01-01T00:00:00Z |
| hierarchy_top_id |
129391832 |
| dewey-sort |
3540 |
| id |
OLC1998935590 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC1998935590</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230516175941.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">171228s2017 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1002/jrs.5162</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20171228</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1998935590</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1998935590</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)p1312-ae683b2b55fe27692633fb098fa8a1f252860141bcf1696da17f9142e78fe10a3</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0047158520170000048001101449pressureinducedphasetransitionsofvateriteametastab</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">540</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">35.25</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">33.07</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Maruyama, Koji</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</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="520" ind1=" " ind2=" "><subfield code="a">Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at high pressure using diamond anvil cells at room temperature. Pressure dependence of Raman peaks assignable to the symmetric stretching vibration modes of carbonate ion indicated the phase transitions of vaterite. At 4.3 GPa, vaterite (vaterite I) transformed to a high‐pressure form of vaterite (vaterite II). With increasing pressure, a part of vaterite II gradually transformed to calcite III, and the remainder of vaterite II transformed to another new phase (vaterite III). The phase transition from vaterite II to calcite III was irreversible, and calcite III back‐transformed to calcite I during decompression. Moreover, at the pressures higher than 13.1 GPa, several diffraction spots were observed on an imaging plate, indicating another phase transition from vaterite III to a phase having coarse grains (vaterite IV). Our results indicate that vaterite undergoes more complex phase transitions at high pressure than other polymorphs of calcium carbonate, calcite, and aragonite. These phase transitions of vaterite will open a window to understanding phase transitions of metastable minerals at high pressure. Copyright © 2017 John Wiley & Sons, Ltd. Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at room temperature. At 4.3 GPa, vaterite transformed to vaterite II. With increasing pressure, a part of vaterite II transformed to calcite III, and the remainder of vaterite II transformed to vaterite III. The phase transition from vaterite II to calcite III was irreversible. At pressures higher than 13.1 GPa, another phase transition from vaterite III to vaterite IV was found.</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">phase transition</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">calcium carbonate</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">high pressure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">calcite</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">vaterite</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Vibration mode</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Decompression</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Calcium</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">High pressure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Phase transformations</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Calcite</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Diamonds</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">X-ray diffraction</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Aragonite</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Diffraction patterns</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Phase transitions</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Raman spectroscopy</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Calcium carbonate</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Spots</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Raman spectra</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Diamond anvil cells</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Vibration</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Metastable phases</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Phase transition</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Pressure dependence</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Diffraction</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Pressure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Minerals</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kagi, Hiroyuki</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Komatsu, Kazuki</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Yoshino, Toru</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Nakano, Satoshi</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of Raman spectroscopy</subfield><subfield code="d">Chichester [u.a.] : Wiley, 1973</subfield><subfield code="g">48(2017), 11, Seite 1449-1453</subfield><subfield code="w">(DE-627)129391832</subfield><subfield code="w">(DE-600)184918-9</subfield><subfield code="w">(DE-576)014776979</subfield><subfield code="x">0377-0486</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:48</subfield><subfield code="g">year:2017</subfield><subfield code="g">number:11</subfield><subfield code="g">pages:1449-1453</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1002/jrs.5162</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://onlinelibrary.wiley.com/doi/10.1002/jrs.5162/abstract</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://search.proquest.com/docview/1967712082</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-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-CHE</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">35.25</subfield><subfield code="q">AVZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">33.07</subfield><subfield code="q">AVZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">48</subfield><subfield code="j">2017</subfield><subfield code="e">11</subfield><subfield code="h">1449-1453</subfield></datafield></record></collection>
|
| author |
Maruyama, Koji |
| spellingShingle |
Maruyama, Koji ddc 540 bkl 35.25 bkl 33.07 misc phase transition misc calcium carbonate misc high pressure misc calcite misc vaterite misc Vibration mode misc Decompression misc Calcium misc High pressure misc Phase transformations misc Calcite misc Diamonds misc X-ray diffraction misc Aragonite misc Diffraction patterns misc Phase transitions misc Raman spectroscopy misc Calcium carbonate misc Spots misc Raman spectra misc Diamond anvil cells misc Vibration misc Metastable phases misc Phase transition misc Pressure dependence misc Diffraction misc Pressure misc Minerals Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3 |
| authorStr |
Maruyama, Koji |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)129391832 |
| format |
Article |
| dewey-ones |
540 - Chemistry & allied sciences |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0377-0486 |
| topic_title |
540 DE-600 35.25 bkl 33.07 bkl Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3 phase transition calcium carbonate high pressure calcite vaterite Vibration mode Decompression Calcium High pressure Phase transformations Calcite Diamonds X-ray diffraction Aragonite Diffraction patterns Phase transitions Raman spectroscopy Calcium carbonate Spots Raman spectra Diamond anvil cells Vibration Metastable phases Phase transition Pressure dependence Diffraction Pressure Minerals |
| topic |
ddc 540 bkl 35.25 bkl 33.07 misc phase transition misc calcium carbonate misc high pressure misc calcite misc vaterite misc Vibration mode misc Decompression misc Calcium misc High pressure misc Phase transformations misc Calcite misc Diamonds misc X-ray diffraction misc Aragonite misc Diffraction patterns misc Phase transitions misc Raman spectroscopy misc Calcium carbonate misc Spots misc Raman spectra misc Diamond anvil cells misc Vibration misc Metastable phases misc Phase transition misc Pressure dependence misc Diffraction misc Pressure misc Minerals |
| topic_unstemmed |
ddc 540 bkl 35.25 bkl 33.07 misc phase transition misc calcium carbonate misc high pressure misc calcite misc vaterite misc Vibration mode misc Decompression misc Calcium misc High pressure misc Phase transformations misc Calcite misc Diamonds misc X-ray diffraction misc Aragonite misc Diffraction patterns misc Phase transitions misc Raman spectroscopy misc Calcium carbonate misc Spots misc Raman spectra misc Diamond anvil cells misc Vibration misc Metastable phases misc Phase transition misc Pressure dependence misc Diffraction misc Pressure misc Minerals |
| topic_browse |
ddc 540 bkl 35.25 bkl 33.07 misc phase transition misc calcium carbonate misc high pressure misc calcite misc vaterite misc Vibration mode misc Decompression misc Calcium misc High pressure misc Phase transformations misc Calcite misc Diamonds misc X-ray diffraction misc Aragonite misc Diffraction patterns misc Phase transitions misc Raman spectroscopy misc Calcium carbonate misc Spots misc Raman spectra misc Diamond anvil cells misc Vibration misc Metastable phases misc Phase transition misc Pressure dependence misc Diffraction misc Pressure misc Minerals |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| author2_variant |
h k hk k k kk t y ty s n sn |
| hierarchy_parent_title |
Journal of Raman spectroscopy |
| hierarchy_parent_id |
129391832 |
| dewey-tens |
540 - Chemistry |
| hierarchy_top_title |
Journal of Raman spectroscopy |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)129391832 (DE-600)184918-9 (DE-576)014776979 |
| title |
Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3 |
| ctrlnum |
(DE-627)OLC1998935590 (DE-599)GBVOLC1998935590 (PRQ)p1312-ae683b2b55fe27692633fb098fa8a1f252860141bcf1696da17f9142e78fe10a3 (KEY)0047158520170000048001101449pressureinducedphasetransitionsofvateriteametastab |
| title_full |
Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3 |
| author_sort |
Maruyama, Koji |
| journal |
Journal of Raman spectroscopy |
| journalStr |
Journal of Raman spectroscopy |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2017 |
| contenttype_str_mv |
txt |
| container_start_page |
1449 |
| author_browse |
Maruyama, Koji |
| container_volume |
48 |
| class |
540 DE-600 35.25 bkl 33.07 bkl |
| format_se |
Aufsätze |
| author-letter |
Maruyama, Koji |
| doi_str_mv |
10.1002/jrs.5162 |
| dewey-full |
540 |
| title_sort |
pressure‐induced phase transitions of vaterite, a metastable phase of caco3 |
| title_auth |
Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3 |
| abstract |
Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at high pressure using diamond anvil cells at room temperature. Pressure dependence of Raman peaks assignable to the symmetric stretching vibration modes of carbonate ion indicated the phase transitions of vaterite. At 4.3 GPa, vaterite (vaterite I) transformed to a high‐pressure form of vaterite (vaterite II). With increasing pressure, a part of vaterite II gradually transformed to calcite III, and the remainder of vaterite II transformed to another new phase (vaterite III). The phase transition from vaterite II to calcite III was irreversible, and calcite III back‐transformed to calcite I during decompression. Moreover, at the pressures higher than 13.1 GPa, several diffraction spots were observed on an imaging plate, indicating another phase transition from vaterite III to a phase having coarse grains (vaterite IV). Our results indicate that vaterite undergoes more complex phase transitions at high pressure than other polymorphs of calcium carbonate, calcite, and aragonite. These phase transitions of vaterite will open a window to understanding phase transitions of metastable minerals at high pressure. Copyright © 2017 John Wiley & Sons, Ltd. Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at room temperature. At 4.3 GPa, vaterite transformed to vaterite II. With increasing pressure, a part of vaterite II transformed to calcite III, and the remainder of vaterite II transformed to vaterite III. The phase transition from vaterite II to calcite III was irreversible. At pressures higher than 13.1 GPa, another phase transition from vaterite III to vaterite IV was found. |
| abstractGer |
Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at high pressure using diamond anvil cells at room temperature. Pressure dependence of Raman peaks assignable to the symmetric stretching vibration modes of carbonate ion indicated the phase transitions of vaterite. At 4.3 GPa, vaterite (vaterite I) transformed to a high‐pressure form of vaterite (vaterite II). With increasing pressure, a part of vaterite II gradually transformed to calcite III, and the remainder of vaterite II transformed to another new phase (vaterite III). The phase transition from vaterite II to calcite III was irreversible, and calcite III back‐transformed to calcite I during decompression. Moreover, at the pressures higher than 13.1 GPa, several diffraction spots were observed on an imaging plate, indicating another phase transition from vaterite III to a phase having coarse grains (vaterite IV). Our results indicate that vaterite undergoes more complex phase transitions at high pressure than other polymorphs of calcium carbonate, calcite, and aragonite. These phase transitions of vaterite will open a window to understanding phase transitions of metastable minerals at high pressure. Copyright © 2017 John Wiley & Sons, Ltd. Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at room temperature. At 4.3 GPa, vaterite transformed to vaterite II. With increasing pressure, a part of vaterite II transformed to calcite III, and the remainder of vaterite II transformed to vaterite III. The phase transition from vaterite II to calcite III was irreversible. At pressures higher than 13.1 GPa, another phase transition from vaterite III to vaterite IV was found. |
| abstract_unstemmed |
Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at high pressure using diamond anvil cells at room temperature. Pressure dependence of Raman peaks assignable to the symmetric stretching vibration modes of carbonate ion indicated the phase transitions of vaterite. At 4.3 GPa, vaterite (vaterite I) transformed to a high‐pressure form of vaterite (vaterite II). With increasing pressure, a part of vaterite II gradually transformed to calcite III, and the remainder of vaterite II transformed to another new phase (vaterite III). The phase transition from vaterite II to calcite III was irreversible, and calcite III back‐transformed to calcite I during decompression. Moreover, at the pressures higher than 13.1 GPa, several diffraction spots were observed on an imaging plate, indicating another phase transition from vaterite III to a phase having coarse grains (vaterite IV). Our results indicate that vaterite undergoes more complex phase transitions at high pressure than other polymorphs of calcium carbonate, calcite, and aragonite. These phase transitions of vaterite will open a window to understanding phase transitions of metastable minerals at high pressure. Copyright © 2017 John Wiley & Sons, Ltd. Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at room temperature. At 4.3 GPa, vaterite transformed to vaterite II. With increasing pressure, a part of vaterite II transformed to calcite III, and the remainder of vaterite II transformed to vaterite III. The phase transition from vaterite II to calcite III was irreversible. At pressures higher than 13.1 GPa, another phase transition from vaterite III to vaterite IV was found. |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-PHA SSG-OLC-DE-84 GBV_ILN_70 |
| container_issue |
11 |
| title_short |
Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3 |
| url |
http://dx.doi.org/10.1002/jrs.5162 http://onlinelibrary.wiley.com/doi/10.1002/jrs.5162/abstract https://search.proquest.com/docview/1967712082 |
| remote_bool |
false |
| author2 |
Kagi, Hiroyuki Komatsu, Kazuki Yoshino, Toru Nakano, Satoshi |
| author2Str |
Kagi, Hiroyuki Komatsu, Kazuki Yoshino, Toru Nakano, Satoshi |
| ppnlink |
129391832 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth oth oth oth |
| doi_str |
10.1002/jrs.5162 |
| up_date |
2024-07-04T06:01:52.264Z |
| _version_ |
1803627174051184640 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC1998935590</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230516175941.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">171228s2017 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1002/jrs.5162</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20171228</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1998935590</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1998935590</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)p1312-ae683b2b55fe27692633fb098fa8a1f252860141bcf1696da17f9142e78fe10a3</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0047158520170000048001101449pressureinducedphasetransitionsofvateriteametastab</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">540</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">35.25</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">33.07</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Maruyama, Koji</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO3</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</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="520" ind1=" " ind2=" "><subfield code="a">Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at high pressure using diamond anvil cells at room temperature. Pressure dependence of Raman peaks assignable to the symmetric stretching vibration modes of carbonate ion indicated the phase transitions of vaterite. At 4.3 GPa, vaterite (vaterite I) transformed to a high‐pressure form of vaterite (vaterite II). With increasing pressure, a part of vaterite II gradually transformed to calcite III, and the remainder of vaterite II transformed to another new phase (vaterite III). The phase transition from vaterite II to calcite III was irreversible, and calcite III back‐transformed to calcite I during decompression. Moreover, at the pressures higher than 13.1 GPa, several diffraction spots were observed on an imaging plate, indicating another phase transition from vaterite III to a phase having coarse grains (vaterite IV). Our results indicate that vaterite undergoes more complex phase transitions at high pressure than other polymorphs of calcium carbonate, calcite, and aragonite. These phase transitions of vaterite will open a window to understanding phase transitions of metastable minerals at high pressure. Copyright © 2017 John Wiley & Sons, Ltd. Pressure‐induced phase transitions of vaterite, a metastable phase of CaCO 3 , were observed from Raman spectra and X‐ray diffraction patterns at room temperature. At 4.3 GPa, vaterite transformed to vaterite II. With increasing pressure, a part of vaterite II transformed to calcite III, and the remainder of vaterite II transformed to vaterite III. The phase transition from vaterite II to calcite III was irreversible. At pressures higher than 13.1 GPa, another phase transition from vaterite III to vaterite IV was found.</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">phase transition</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">calcium carbonate</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">high pressure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">calcite</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">vaterite</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Vibration mode</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Decompression</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Calcium</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">High pressure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Phase transformations</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Calcite</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Diamonds</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">X-ray diffraction</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Aragonite</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Diffraction patterns</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Phase transitions</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Raman spectroscopy</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Calcium carbonate</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Spots</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Raman spectra</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Diamond anvil cells</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Vibration</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Metastable phases</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Phase transition</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Pressure dependence</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Diffraction</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Pressure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Minerals</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kagi, Hiroyuki</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Komatsu, Kazuki</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Yoshino, Toru</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Nakano, Satoshi</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of Raman spectroscopy</subfield><subfield code="d">Chichester [u.a.] : Wiley, 1973</subfield><subfield code="g">48(2017), 11, Seite 1449-1453</subfield><subfield code="w">(DE-627)129391832</subfield><subfield code="w">(DE-600)184918-9</subfield><subfield code="w">(DE-576)014776979</subfield><subfield code="x">0377-0486</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:48</subfield><subfield code="g">year:2017</subfield><subfield code="g">number:11</subfield><subfield code="g">pages:1449-1453</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1002/jrs.5162</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://onlinelibrary.wiley.com/doi/10.1002/jrs.5162/abstract</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://search.proquest.com/docview/1967712082</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-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-CHE</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">35.25</subfield><subfield code="q">AVZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">33.07</subfield><subfield code="q">AVZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">48</subfield><subfield code="j">2017</subfield><subfield code="e">11</subfield><subfield code="h">1449-1453</subfield></datafield></record></collection>
|
| score |
7.400591 |