| CONDENSED MATTER: STRUCTURAL, MECHANICAL, AND THERMAL PROPERTIES |
Prev
Next
|
|
|
In situ study of calcite-III dimorphism using dynamic diamond anvil cell |
| Xia Zhao(赵霞)1,2, Sheng-Hua Mei(梅升华)1,†, Zhi Zheng(郑直)1, Yue Gao(高悦)1,2, Jiang-Zhi Chen(陈姜智)1, Yue-Gao Liu(刘月高)1, Jian-Guo Sun(孙建国)3, Yan Li(李艳)1,2, and Jian-Hui Sun(孙建辉)1 |
1 CAS Key Laboratory for Experimental Study under Deep-sea Extreme Conditions, Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences(CAS), Sanya 572000, China;
2 University of Chinese Academy of Sciences, Beijing 100049, China;
3 Department of Mechanical Engineering, National University of Singapore(NUS), Singapore 117575, Singapore |
|
|
|
|
Abstract The phase transitions among the high-pressure polymorphic forms of CaCO3 (cc-I, cc-II, cc-III, and cc-IIIb) are investigated by dynamic diamond anvil cell (dDAC) and in situ Raman spectroscopy. Experiments are carried out at room temperature and high pressures up to 12.8 GPa with the pressurizing rate varying from 0.006 GPa/s to 0.056 GPa/s. In situ observation shows that with the increase of pressure, calcite transforms from cc-I to cc-II at ～ 1.5 GPa and from cc-II to cc-III at ～ 2.5 GPa, and transitions are independent of the pressurizing rate. Further, as the pressure continues to increase, the cc-IIIb begins to appear and coexists with cc-III within a pressure range that is inversely proportional to the pressurizing rate. At the pressurizing rates of 0.006, 0.012, 0.021, and 0.056 GPa/s, the coexistence pressure ranges of cc-III and cc-IIIb are 2.8 GPa-9.8 GPa, 3.1 GPa-6.9 GPa, 2.7 GPa-6.0 GPa, and 2.8 GPa-4.5 GPa, respectively. The dependence of the coexistence on the pressurizing rate may result from the influence of pressurizing rate on the activation process of transition by reducing the energy barrier. The higher the pressurizing rate, the lower the energy barrier is, and the easier it is to pull the system out of the coexistence state. The results of this in situ study provide new insights into the understanding of the phase transition of calcite.
|
Received: 09 December 2021
Revised: 21 March 2022
Accepted manuscript online: 28 March 2022
|
|
PACS:
|
62.50.-p
|
(High-pressure effects in solids and liquids)
|
| |
33.20.Fb
|
(Raman and Rayleigh spectra (including optical scattering) ?)
|
| |
47.80.Fg
|
(Pressure and temperature measurements)
|
| |
91.65.-n
|
(Mineralogy and petrology)
|
|
| Fund: Project supported by the Fund from the Chinese Academy of Sciences (Grant No. QYZDY-SSW-DQC029) and the National Natural Science Foundation of China (Grant No. 41674097). |
Corresponding Authors:
Sheng-Hua Mei
E-mail: mei@idsse.ac.cn
|
Cite this article:
Xia Zhao(赵霞), Sheng-Hua Mei(梅升华), Zhi Zheng(郑直), Yue Gao(高悦), Jiang-Zhi Chen(陈姜智), Yue-Gao Liu(刘月高), Jian-Guo Sun(孙建国), Yan Li(李艳), and Jian-Hui Sun(孙建辉) In situ study of calcite-III dimorphism using dynamic diamond anvil cell 2022 Chin. Phys. B 31 096201
|
[1] Dasgupta R and Hirschmann M M 2010 Earth and Planetary Science Letters 298 1
[2] Merlini M, Hanfland M and Crichton W A 2012 Earth and Planetary Science Letters 333 265
[3] Liu Y, Li W, Lu X, Liu Y, Ruan B and Liu X 2017 Ore Geology Reviews 91 419
[4] Zhang Z W, Wang Y L, Qian B, Liu Y G, Zhang D Y, Lu P R and Dong J 2018 Ore Geology Reviews 96 236
[5] Suito K, Namba J, Horikawa T, Taniguchi Y, Sakurai N, Kobayashi M, Onodera A, Shimomura O and Kikegawa T 2001 American Mineralogist 86 997
[6] Hagiya K, Matsui M, Kimura Y and Akahama Y 2005 Journal of Mineralogical and Petrological Sciences 100 31
[7] Catalli K and Williams Q 2005 American Mineralogist 90 1679
[8] Ono S, Kikegawa T and Ohishi Y 2007 American Mineralogist 92 1246
[9] Oganov A R, Glass C W and Ono S 2006 Earth and Planetary Science Letters 241 95
[10] Oganov A R, Ono S, Ma Y, Glass C W and Garcia A 2008 Earth and Planetary Science Letters 273 38
[11] Gavryushkin P N, Martirosyan N S, Inerbaev T M, Popov Z I, Rashchenko S V, Likhacheva A Y, Lobanov S S, Goncharov A F, Prakapenka V B and Litasov K D 2017 Crystal Growth and Design 17 6291
[12] Li X, Zhang Z, Lin J F, Ni H, Prakapenka V B and Mao Z 2018 Geophysical Research Letters 45 1355
[13] Kushiro I 1975 Earth and Planetary Science Letters 28 116
[14] Ague J J and Nicolescu S 2014 Nature Geoscience 7 355
[15] Kaminsky F, Matzel J, Jacobsen B, Hutcheon I and Wirth R 2016 Mineralogy and Petrology 110 379
[16] Wirth R, Kaminsky F, Matsyuk S and Schreiber A 2009 Earth and Planetary Science Letters 286 292
[17] Nestola F, Korolev N, Kopylova M, Rotiroti N, Pearson D G, Pamato M G, Alvaro M, Peruzzo L, Gurney J J, Moore A E and Davidson J 2018 Nature 555 237
[18] Hou M, Zhang Q, Tao R, Liu H, Kono Y, Mao H K, Yang W, Chen B and Fei Y 2019 Nat. Commun. 10 1963
[19] Hacker B R, Kirby S H and Bohlen S R 1992 Science 258 110
[20] Liu L G and Mernagh T P 1990 American Mineralogist 75 801
[21] Merlini M, Crichton W A, Chantel J, Guignard J and Poli S 2014 Mineralogical Magazine 78 225
[22] Pippinger T, Miletich R, Merlini M, Lotti P, Schouwink P, Yagi T, Crichton W A and Hanfland M 2014 Physics and Chemistry of Minerals 42 29
[23] Belkofsi R, Adjaoud O and Belabbas I 2018 Modelling and Simulation in Materials Science and Engineering 26 065004
[24] Koch-Mueller M, Jahn S, Birkholz N, Ritter E and Schade U 2016 Physics and Chemistry of Minerals 43 545
[25] Yuan X, Gao C and Gao J 2019 Mineralogical Magazine 83 191
[26] Beaussier S J, Gerya T V and Burg J P 2019 Tectonophysics 763 1
[27] Hynes A 1987 Precambrian Research 36 189
[28] Choe H and Dyment J 2021 Eaeth and Planetary Science Letters 561 116787
[29] Choe H and Dyment J 2020 Geophysical Research Letters 47 e2019GL085975
[30] Tao R, Zhang L and Zhang L 2020 Geoscience Frontiers 11 915
[31] Audetat A, Pettke T and Dolejs D 2004 Lithos 72 147
[32] Katz S and Schock R N 1968 American Mineralogist 53 1910
[33] Cifrulak S D 1970 American Mineralogist 55 815
[34] Fong M Y and Nicol M 1971 J. Chem. Phys. 54 579
[35] Adams D M and Pogson M 1988 Spectrochimica Acta Part A:Molecular Spectroscopy 44 745
[36] Williams Q, Collerson B and Knittle E 1992 American Mineralogist 77 1158
[37] Gillet P, Biellmann C, Reynard B and McMillan P 1993 Physics and Chemistry of Minerals 20 1
[38] Wang S and Zheng H 2011 Spectroscopy and Spectral Analysis 31 2117
[39] Bayarjargal L, Fruhner C J, Schrodt N and Winkler B 2018 Physics of the Earth and Planetary Interiors 281 31
[40] Fu W and Yuan X 2019 Spectroscope and Spectral Analysis 39 2053 (in Chinese)
[41] Bischoff W D, Sharma S K and Mackenzie F T 1985 American Mineralogist 70 581
[42] Merrill L and Bassett W A 1975 Acta Crystallographica Section B:Structural Crystallography and Crystal Chemistry 31 343
[43] Ono S, Kikegawa T, Ohishi Y and Tsuchiya J 2005 American Mineralogist 90 667
[44] Yuan C, Zhang X, Zhou L, Li H, Feng S, Yang K and Zhu X 2021 Journal of Molecular Liquids 328 115444
[45] Lin C, Smith J S, Sinogeikin S V, Park C, Kono Y, Kenney-Benson C, Rod E and Shen G 2016 J. Appl. Phys. 119 045902
[46] Chen J Y, Kim M, Yoo C S, Liermann H P and Evans W 2014 J. Phys.:Conf. Ser. 500 142006
[47] Velisavljevic N, Sinogeikin S, Saavedra R, Chellappa R S, Rothkirch A, Dattelbaum D M, Konopkova Z, Liermann H P, Bishop M, Tsoi G M and Vohra Y K 2014 J. Phys.:Conf. Ser. 500 032020
[48] Chen J Y and Yoo C S 2011 Proc. Natl. Acad. Sci. USA 108 7685
[49] Mao H K and Bell P M 1978 Science 200 1145
[50] Monkhorst H J and Pack J D 1976 Phys. Rev. B 13 5188
[51] Jamieson J C 1957 Journal of Geology 65 334
[52] Bridgman P W 1939 American Journal of Science 237 7
[53] Lin C and Tse J S 2021 J. Phys. Chem. Lett. 12 8024 |
| No Suggested Reading articles found! |
|
|
Viewed |
|
|
|
Full text
|
|
|
|
|
Abstract
|
|
|
|
|
Cited |
|
|
|
|
Altmetric
|
|
blogs
Facebook pages
Wikipedia page
Google+ users
|
Online attention
Altmetric calculates a score based on the online attention an article receives. Each coloured thread in the circle represents a different type of online attention. The number in the centre is the Altmetric score. Social media and mainstream news media are the main sources that calculate the score. Reference managers such as Mendeley are also tracked but do not contribute to the score. Older articles often score higher because they have had more time to get noticed. To account for this, Altmetric has included the context data for other articles of a similar age.
View more on Altmetrics
|
|
|
