Skip to main content Accessibility help
×
Hostname: page-component-78c5997874-fbnjt Total loading time: 0 Render date: 2024-11-10T08:22:47.109Z Has data issue: false hasContentIssue false

1 - Introduction to Static and Dynamic High-Pressure Mineral Physics

Published online by Cambridge University Press:  03 August 2023

Yingwei Fei
Affiliation:
Carnegie Institution of Washington, Washington DC
Michael J. Walter
Affiliation:
Carnegie Institution of Washington, Washington DC
Get access

Summary

In October of 2018, a group of scientists gathered at the Broad Branch Road campus of the Carnegie Institution for Science to celebrate 50 years of high-pressure research by Ho-Kwang “Dave” Mao at the Geophysical Laboratory. The celebration highlighted the growth of high-pressure mineral physics over the last half century, which has matured into a vibrant discipline in the physical sciences because of its intimate connections to Earth and planetary sciences, solid-state physics, and materials science. Dave’s impact in high-pressure research for over a half a century has been immense, with a history of innovation and discovery spanning from the Earth and planetary sciences to fundamental materials physics. Dave has always been an intrepid pioneer in high-pressure science, and together with his numerous colleagues and collaborators across the world he has driven the field to ever higher pressures and temperatures, guided the community in adopting and adapting a spectrum of new technologies for in situ interrogation of samples at extreme conditions, and relentlessly explored the materials that make up the deep interiors of planets. In this volume, we assemble 15 chapters from authors who have worked with, been inspired by, or mentored by Dave over his amazing career, spanning a range of subjects that covers the entire field of high-pressure mineral physics.

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2022

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Badding, J. V., Hemley, R. J., Mao, H. K. (1991). High-pressure chemistry of hydrogen in metals – in situ study of iron hydride. Science, 253, 421424.Google Scholar
Badro, J., Struzhkin, V. V., Shu, J., et al. (1999). Magnetism in FeO at megabar pressures from X-ray emission spectroscopy. Physical Review Letters, 83, 4101.Google Scholar
Bell, P., Yagi, T., Mao, H. (1979). Iron-magnesium distribution coefficients between spinel [(Mg, Fe) 2SiO4], magnesiowüstite [(Mg, Fe) O], and perovskite [(Mg, Fe) SiO3]. Year Book Carnegie Institute Washington, 78, 618621.Google Scholar
Chen, X.-J., Wang, J.-L., Struzhkin, V. V., Mao, H.-k., Hemley, R. J., Lin, H.-Q. (2008). Superconducting behavior in compressed solid SiH 4 with a layered structure. Physical Review Letters, 101, 077002.Google Scholar
Duffy, T. S., Hemley, R. J., Mao, H. K. (1995). Equation of state and shear-strength at multimegabar pressures – magnesium-oxide to 227GPa. Physical Review Letters, 74, 13711374.Google Scholar
Eremets, M. I., Struzhkin, V. W., Mao, H. K., Hemley, R. J. (2001). Superconductivity in boron. Science, 293, 272274.CrossRefGoogle ScholarPubMed
Fei, Y. W., Mao, H. K. (1994). In-situ determination of the NiAs phase of FeO at high-pressure and temperature. Science, 266, 16781680.Google Scholar
Goncharov, A. F., Kong, L., Mao, H.-k. (2019). High-pressure integrated synchrotron infrared spectroscopy system at the Shanghai Synchrotron Radiation Facility. Review of Scientific Instruments, 90, 093905.CrossRefGoogle ScholarPubMed
Goncharov, A. F., Struzhkin, V. V., Somayazulu, M. S., Hemley, R. J., Mao, H. K. (1996). Compression of ice to 210 gigapascals: infrared evidence for a symmetric hydrogen-bonded phase. Science, 273, 218220.CrossRefGoogle ScholarPubMed
Gregoryanz, E., Goncharov, A. F., Matsuishi, K., Mao, H., Hemley, R. J. (2003). Raman spectroscopy of hot dense hydrogen. Physical Review Letters, 90(17).Google Scholar
Gregoryanz, E., Goncharov, A. F., Sanloup, C., Somayazulu, M., Mao, H.-k., Hemley, R. J. (2007). High P-T transformations of nitrogen to 170 GPa. Journal of Chemical Physics, 126, 184505.CrossRefGoogle Scholar
Hemley, R. J., Mao, H.-k. (1988). Phase-transition in solid molecular-hydrogen at ultrahigh pressures. Physical Review Letters, 61, 857860.CrossRefGoogle ScholarPubMed
Hemley, R. J., Mao, H.-k., Struzhkin, V. V. (2005). Synchrotron radiation and high pressure: new light on materials under extreme conditions. Journal of Synchrotron Radiation, 12, 135154.Google Scholar
Hirose, K., Fei, Y. W., Ma, Y. Z., Mao, H. K. (1999). The fate of subducted basaltic crust in the Earth’s lower mantle. Nature, 397, 5356.Google Scholar
Hu, Q. Y., Kim, D. Y., Yang, W. G., et al. (2016). FeO2 and FeOOH under deep lower-mantle conditions and Earth’s oxygen-hydrogen cycles. Nature, 534, 241244.CrossRefGoogle ScholarPubMed
Jephcoat, A. P., Mao, H. K., Bell, P. M. (1986). Static compression of iron to 78-GPa with rare-gas solids as pressure-transmitting media. Journal of Geophysical Research – Solid Earth and Planets, 91, 46774684.CrossRefGoogle Scholar
Ji, C., Li, B., Liu, W., et al. (2019). Ultrahigh-pressure isostructural electronic transitions in hydrogen. Nature, 573, 558562.Google Scholar
Li, J., Struzhkin, V. V., Mao, H. K., et al. (2004). Electronic spin state of iron in lower mantle perovskite. Proceedings of the National Academy of Sciences of the United States of America, 101, 1402714030.Google Scholar
Lin, J. F., Struzhkin, V. V., Jacobsen, S. D., et al. (2005). Spin transition of iron in magnesiowustite in the Earth’s lower mantle. Nature, 436, 377380.CrossRefGoogle ScholarPubMed
Lin, Y. H., Hu, Q. Y., Meng, Y., Walter, M., Mao, H. K. (2020). Evidence for the stability of ultrahydrous stishovite in Earth’s lower mantle. Proceedings of the National Academy of Sciences of the United States of America, 117, 184189.CrossRefGoogle ScholarPubMed
Liu, J., Hu, Q. Y., Bi, W. L., et al. (2019). Altered chemistry of oxygen and iron under deep Earth conditions. Nature Communications, 10(1), 18.Google Scholar
Liu, J., Hu, Q. Y., Kim, , et al. (2017). Hydrogen-bearing iron peroxide and the origin of ultralow-velocity zones. Nature, 551, 494497.Google Scholar
Liu, L. G. (1976). Orthorhombic perovskite phases observed in olivine, pyroxene and garnet at high-pressures and temperatures. Physics of the Earth and Planetary Interiors, 11, 289298.Google Scholar
Loubeyre, P., LeToullec, R., Hausermann, D., et al. (1996). X-ray diffraction and equation of state of hydrogen at megabar pressures. Nature, 383, 702704.Google Scholar
Mao, H. K., Bassett, W. A., Takahash, T. (1967). Effect of pressure on crystal structure and lattice parameters of iron up to 300 kbar. Journal of Applied Physics, 38, 274276.Google Scholar
Mao, H. K., Bell, P. M. (1978). High-pressure physics – sustained static generation of 1.36 to 1.72 megabars. Science, 200, 11451147.CrossRefGoogle ScholarPubMed
Mao, H. K., Bell, P. M. (1979). Equations of state of MgO and epsilon-Fe under static pressure conditions. Journal of Geophysical Research, 84, 45334536.Google Scholar
Mao, H. K., Bell, P. M., Shaner, J. W., Steinberg, D. J. (1978). Specific volume measurements of Cu, Mo, Pd, and Ag and calibration of ruby r1 fluorescence pressure gauge from 0.06 to 1 Mbar. Journal of Applied Physics, 49, 32763283.Google Scholar
Mao, H.-k., Chen, B., Chen, J., et al. (2016). Recent advances in high-pressure science and technology. Matter and Radiation at Extremes, 1, 5975.Google Scholar
Mao, H. K., Chen, L. C., Hemley, R. J., Jephcoat, A. P., Wu, Y., Bassett, W. A. (1989). Stability and equation of state of CaSio3-perovskite to 134-GPa. Journal of Geophysical Research – Solid Earth and Planets, 94, 1788917894.Google Scholar
Mao, H. K., Hemley, R. J. (1994). Ultrahigh-pressure transitions in solid hydrogen. Reviews of Modern Physics, 66, 671692.CrossRefGoogle Scholar
Mao, H.-k., Hemley, R. J. (1996). Energy dispersive X-ray diffraction of micro-crystals at ultrahigh pressures. International Journal of High Pressure Research, 14, 257267.CrossRefGoogle Scholar
Mao, H. K., Hemley, R. J., Wu, Y., et al. (1988a). High-pressure phase-diagram and equation of state of solid helium from single-crystal X-ray-diffraction to 23.3-GPa. Physical Review Letters, 60, 26492652.Google Scholar
Mao, H. K., Hu, Q. Y., Yang, L. X., et al. (2017). When water meets iron at Earth’s core-mantle boundary. National Science Review, 4, 870878.Google Scholar
Mao, H. K., Jephcoat, A. P., Hemley, R. J., et al. (1988b). Synchrotron X-ray-diffraction measurements of single-crystal hydrogen to 26.5 gigapascals. Science, 239, 11311134.Google Scholar
Mao, H.-k., Kao, C., Hemley, R. J. (2001a). Inelastic X-ray scattering at ultrahigh pressures. Journal of Physics: Condensed Matter, 13, 7847.Google Scholar
Mao, H. K., Shen, G. Y., Hemley, R. J. (1997). Multivariable dependence of Fe–Mg partitioning in the lower mantle. Science, 278, 20982100.Google Scholar
Mao, H. K., Shu, J. F., Shen, G. Y., Hemley, R. J., Li, B. S., Singh, A. K. (1998). Elasticity and rheology of iron above 220 GPa and the nature of the Earth’s inner core. Nature, 396, 741743.CrossRefGoogle Scholar
Mao, H. K., Takahashi, T., Bassett, W. A., Kinsland, G. L., Merrill, L. (1974). Isothermal compression of magnetite to 320 kbar and pressure-induced phase-transformation. Journal of Geophysical Research, 79, 11651170.CrossRefGoogle Scholar
Mao, H. K., Wu, Y., Chen, L. C., Shu, J. F., Jephcoat, A. P. (1990). Static compression of iron to 300 GPa and Fe0.8Ni0.2 alloy to 260 GPa – implications for composition of the core. Journal of Geophysical Research-Solid Earth and Planets, 95, 2173721742.Google Scholar
Mao, H. K., Xu, J., Bell, P. M. (1986). Calibration of the ruby pressure gauge to 800-kbar under quasi-hydrostatic conditions. Journal of Geophysical Research-Solid Earth and Planets, 91, 46734676.Google Scholar
Mao, H. K., Xu, J., Struzhkin, V. V., et al. (2001b). Phonon density of states of iron up to 153 gigapascals. Science, 292, 914916.Google Scholar
Mao, W. L., Mao, H.-k., Meng, Y., et al. (2006a). X-ray–induced dissociation of H2O and formation of an O2–H2 alloy at high pressure. Science, 314, 636638.Google Scholar
Mao, W. L., Mao, H.-k., Sturhahn, W., et al. (2006b). Iron-rich post-perovskite and the origin of ultralow-velocity zones. Science, 312, 564565.Google Scholar
Meng, Y., Mao, H.-k., Eng, P. J., et al. (2004). The formation of sp(3) bonding in compressed BN. Nature Materials, 3, 111114.Google Scholar
Merkel, S., Wenk, H. R., Shu, J. F., et al. (2002). Deformation of polycrystalline MgO at pressures of the lower mantle. Journal of Geophysical Research – Solid Earth, 107, (B11), ECV 3.1EVC3.17.Google Scholar
Piermarini, G. J. (2001). High pressure X-ray crystallography with the diamond cell at NIST/NBS. Journal of Research of the National Institute of Standards and Technology, 106, 889920.Google Scholar
Saxena, S., Dubrovinsky, L., Häggkvist, P., Cerenius, Y., Shen, G., Mao, H. (1995). Synchrotron X-ray study of iron at high pressure and temperature. Science, 269, 17031704.Google Scholar
Sharma, S. K., Mao, H. K., Bell, P. M. (1980). Raman measurements of hydrogen in the pressure range 0.2–630 kbar at room-temperature. Physical Review Letters, 44, 886888.Google Scholar
Shen, G., Mao, H.-k., Hemley, R. J. (1996). Laser-heated diamond anvil cell technique: double-sided heating with multimode Nd: YAG laser. Computer, 1, L2.Google Scholar
Shen, G., Wang, L., Ferry, R., Mao, H.-k., Hemley, R. J. (2010). A portable laser heating microscope for high pressure research. Journal of Physics: Conference Series, 215, 012191.Google Scholar
Shen, G. Y., Mao, H. K. (2017). High-pressure studies with X-rays using diamond anvil cells. Reports on Progress in Physics, 80, 153.Google Scholar
Shen, G. Y., Mao, H. K., Hemley, R. J., Duffy, T. S., Rivers, M. L. (1998). Melting and crystal structure of iron at high pressures and temperatures. Geophysical Research Letters, 25, 373376.Google Scholar
Shieh, S. R., Mao, H. K., Hemley, R. J., Ming, L. C. (1998). Decomposition of phase D in the lower mantle and the fate of dense hydrous silicates in subducting slabs. Earth and Planetary Science Letters, 159, 1323.Google Scholar
Somayazulu, M., Dera, P., Goncharov, A. F., et al. (2010). Pressure-induced bonding and compound formation in xenon–hydrogen solids. Nature Chemistry, 2, 5053.Google Scholar
Stixrude, L., Hemley, R. J., Fei, Y., Mao, H. K. (1992). Thermoelasticity of silicate perovskite and magnesiowustite and stratification of the Earth’s mantle. Science, 257, 10991101.Google Scholar
Vos, W. L., Finger, L. W., Hemley, R. J., Mao, H. K. (1993). Novel H2-H2O clathrates at high-pressures. Physical Review Letters, 71, 31503153.Google Scholar
Wang, Y., Ying, J., Zhou, Z., et al. (2018). Emergent superconductivity in an iron-based honeycomb lattice initiated by pressure-driven spin-crossover. Nature Communications, 9, 17.Google Scholar
Yagi, T., Bell, P., Mao, H. (1979). Phase relations in the system MgO-FeO-SiO2 between 150 and 700 kbar at 1000 C. Year Book Carnegie Institute Washington, 78, 614618.Google Scholar
Yagi, T., Mao, H. K., Bell, P.M. (1978). Structure and crystal-chemistry of perovskite-type MgSiO3. Physics and Chemistry of Minerals, 3, 97110.Google Scholar
Yoshimura, Y., Stewart, S. T., Somayazulu, M., Mao, H.-k., Hemley, R. J. (2006). High-pressure X-ray diffraction and Raman spectroscopy of ice VIII. Journal of Chemical Physics, 124, 024502.Google Scholar
Zeng, Z., Yang, L., Zeng, Q., et al. (2017). Synthesis of quenchable amorphous diamond. Nature Communications, 8, 17.Google Scholar
Zha, C. S., Mao, H. K., Hemley, R. J. (2000). Elasticity of MgO and a primary pressure scale to 55 GPa. Proceedings of the National Academy of Sciences of the United States of America, 97, 1349413499.Google Scholar
Zhang, L., Yuan, H. S., Meng, Y., Mao, H. K. (2018). Discovery of a hexagonal ultradense hydrous phase in (Fe,Al)OOH. Proceedings of the National Academy of Sciences of the United States of America, 115, 29082911.Google Scholar
Zhao, J., Sturhahn, W., Lin, J.-f., Shen, G., Alp, E. E., Mao, H.-k. (2004). Nuclear resonant scattering at high pressure and high temperature. High Pressure Research, 24, 447457.Google Scholar
Zhou, Y., Wu, J., Ning, W., et al. (2016). Pressure-induced superconductivity in a three-dimensional topological material ZrTe5. Proceedings of the National Academy of Sciences, 113, 29042909.Google Scholar
Zhu, J., Zhang, J., Kong, P., et al. (2013). Superconductivity in topological insulator Sb2Te3 induced by pressure. Scientific Reports, 3, 16.Google Scholar

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×