SCHOOL OF EARTH AND SPACE SCIENCES, Peking University

Research Area

DATE：2018-05-24

Infomation
Name:	Qiong Liu
Title:	Associate Professor
Phone:	010-62767639
Position:	Rm 3303, 5 Yiheyuan Rd.Haidian District, Beijing, 100871, China
Email:	qiong.liu@pku.edu.cn

ACADEMIC APPOINTMENTS
2000.09--2005.08	Ph.D.	Geology, University of Michigan, Ann Arbor, USA
1994.09--2000.07	Ph.D	Mineralogy, Petrology, and Geochemistry, China University of Geosciences, Beijing
1990.09--1994.07	B.S.	Mineral Deposits Geology, China University of Geosciences, Wuhan

PROFESSIONAL PREPARATION
2009.04--to now	Associate Professor, School of Earth and Space Sciences, Peking University
2014.09--to now	Adjunct Associate Professor, China University of Geosciences, Beijing
2010.10--2011.02	Visiting Scholar, Geophysical Laboratory, Carnegie Institution of Washington
2007.03--2009.03	Postdoctoral Research Associate, Mineral Physics Institute, Stony Brook University
2005.09--2007.02	Postdoctoral Researcher, University of Michigan, Ann Arbor
1998.09--2005.08	Research Assistant, University of Michigan, Ann Arbor
1994.09--1998.08	Research Assistant, China University of Geosciences, Beijing, China

AWARDS AND FELLOWSHIPS
no record

RECENT COURSES TAUGHT
Instructor, Peking University, Beijing, China Fall 2009-2016 Geochemistry Seminar, Introduction to Cosmochemistry Winter 2011-2014, Fall 2015-2016 High Temperature and High Pressure Material Sciences Fall 2011-2016 Geochemical Data Interpretation Winter 2016 Synchrotron Radiation and its Applications in Geosciences

CURRENT PROFESSIONAL ACTIVITIES
Adjunct Associate Professor, China University of Geosciences (Beijing)

EXTERNAL RESEARCH GRANT HISTORY
Elastic Velocities of Dense Hydrous Magnesium Silicate (DHMS) under Subduction and Mantle Transition Zone conditions and Implications for Water Storage and Circulation, Natural Science Foundation of China，Co-PI, 2016/1 – 2020/12 Deep carbon cycle in the subduction zone: Petrological observation and high-temperature and high-pressure experimental simulation，Natural Science Foundation of China，Co-PI, 2016/1 – 2020/12 The phase and chemical changes of carbon-bearing fluids and minerals in the Earth's deep interior, Natural Science Foundation of China，Co-PI, 2011/1 – 2014/12 Ultrasonic studies on molten olivine solid solution, Natural Science Foundation of China，PI, 2010/1 – 2012/12 Scott Turner Award (2000, 2002, 2003), University of Michigan

EXTERNAL RESEARCH GRANT HISTORY

Elastic Velocities of Dense Hydrous Magnesium Silicate (DHMS) under Subduction and Mantle Transition Zone conditions and Implications for Water Storage and Circulation, Natural Science Foundation of China，Co-PI, 2016/1 – 2020/12
Deep carbon cycle in the subduction zone: Petrological observation and high-temperature and high-pressure experimental simulation，Natural Science Foundation of China，Co-PI, 2016/1 – 2020/12
The phase and chemical changes of carbon-bearing fluids and minerals in the Earth's deep interior, Natural Science Foundation of China，Co-PI, 2011/1 – 2014/12
Ultrasonic studies on molten olivine solid solution, Natural Science Foundation of China，PI, 2010/1 – 2012/12
Scott Turner Award (2000, 2002, 2003), University of Michigan

REFEREED PUBLICATIONS
Nie S., Liu Y., Liu Q., Wang M., and Wang H. (2017) Phase transitions and thermal expansion of BaCO3 and SrCO3 up to 1413 K, European Journal of Mineralogy, 29, 433-443, DOI: 10.1127/ejm/2017/0029-2612. Wang M., Liu Q., Inoue T., Li B., Pottish S., Wood J., Yang C., and Tao R. (2016) The K2CO3 fusion curve revisited: New experiments at pressures up to 12 GPa, Journal of Mineralogical and Petrological Sciences, 111, 241-251. Wang M., Liu Q., Nie S., Li B., Wu Y., Gao J., Wei X., and Wu X. (2015) High-pressure Phase transitions and compressibilities of aragonite-structure carbonates: SrCO3 and BaCO3, Physics and Chemistry of Minerals, 42, 517-527, doi: 10.1007/s00269-015-0740-2. Tao R., Zhang L., Fei Y., and Liu Q. (2014) The effect of Fe on the stability of dolomite at high pressure: Experimental study and petrological observation in eclogite from southwestern Tianshan, China. Geochimica et Cosmochimica Acta, 143, 253-267. Thomas, C. W., Liu Q., C. Agee B., Asimow P. D., and Lange R. A. (2012) Multi-technique equation of state for Fe2SiO4 melt and the density of Fe-bearing silicate melts from 0 to 161 GPa, Journal of Geophysical Research, 117, B10206, doi:10.1029/2012JB009403. Liu Q., Liu W., Whitaker, M. L., Wang L., and Li B. (2010) In situ ultrasonic velocity measurements across the olivine-spinel transformation in Fe2SiO4 . American Mineralogist, 95, 1000-1005. Liu Q., Liu W., Whitaker M. L., Wang L., and Li B. (2008) Compressional and shear wave velocities of Fe2SiO4 spinel at high pressure and high temperature. High Pressure Research, 28, 405-413. Liu Q., Lange R.A., and Ai Y.H. (2007) Acoustic velocity measurements on Na2O-TiO2-SiO2 liquids: Evidence for a highly compressible TiO2 component related to five-coordinated Ti. Geochimica et Cosmochimica Acta, 71, 4314-4326. Liu Q., Tenner T., and Lange R.A. (2007) Do carbonate liquids become denser than silicate liquids at pressure? Constraints from the fusion curve of K2CO3 to 3.2 GPa. Contributions to Mineralogy and Petrology, 153, 55-66. Liu Q. and Lange R.A. (2006) The partial molar volume of Fe2O3 in alkali silicate melts: Evidence for an average Fe3+ coordination number near five. American Mineralogist, 91, 385-393. Liu Q. and Lange R.A. (2003) The density of natrocarbonatite liquids: new measurements and the partial molar volume of the CaCO3 component. Contributions to Mineralogy and Petrology, 146, 370-381. Liu Q. and Lange R.A. (2001) The partial molar volume and thermal expansivity of TiO2 in alkali silicate liquids: systematic variation with Ti coordination. Geochimica et Cosmochimica Acta, 65, 2379-2393.

REFEREED PUBLICATIONS

Nie S., Liu Y., Liu Q., Wang M., and Wang H. (2017) Phase transitions and thermal expansion of BaCO3 and SrCO3 up to 1413 K, European Journal of Mineralogy, 29, 433-443, DOI: 10.1127/ejm/2017/0029-2612.
Wang M., Liu Q., Inoue T., Li B., Pottish S., Wood J., Yang C., and Tao R. (2016) The K2CO3 fusion curve revisited: New experiments at pressures up to 12 GPa, Journal of Mineralogical and Petrological Sciences, 111, 241-251.
Wang M., Liu Q., Nie S., Li B., Wu Y., Gao J., Wei X., and Wu X. (2015) High-pressure Phase transitions and compressibilities of aragonite-structure carbonates: SrCO3 and BaCO3, Physics and Chemistry of Minerals, 42, 517-527, doi: 10.1007/s00269-015-0740-2.
Tao R., Zhang L., Fei Y., and Liu Q. (2014) The effect of Fe on the stability of dolomite at high pressure: Experimental study and petrological observation in eclogite from southwestern Tianshan, China. Geochimica et Cosmochimica Acta, 143, 253-267.
Thomas, C. W., Liu Q., C. Agee B., Asimow P. D., and Lange R. A. (2012) Multi-technique equation of state for Fe2SiO4 melt and the density of Fe-bearing silicate melts from 0 to 161 GPa, Journal of Geophysical Research, 117, B10206, doi:10.1029/2012JB009403.
Liu Q., Liu W., Whitaker, M. L., Wang L., and Li B. (2010) In situ ultrasonic velocity measurements across the olivine-spinel transformation in Fe2SiO4 . American Mineralogist, 95, 1000-1005.
Liu Q., Liu W., Whitaker M. L., Wang L., and Li B. (2008) Compressional and shear wave velocities of Fe2SiO4 spinel at high pressure and high temperature. High Pressure Research, 28, 405-413.
Liu Q., Lange R.A., and Ai Y.H. (2007) Acoustic velocity measurements on Na2O-TiO2-SiO2 liquids: Evidence for a highly compressible TiO2 component related to five-coordinated Ti. Geochimica et Cosmochimica Acta, 71, 4314-4326.
Liu Q., Tenner T., and Lange R.A. (2007) Do carbonate liquids become denser than silicate liquids at pressure? Constraints from the fusion curve of K2CO3 to 3.2 GPa. Contributions to Mineralogy and Petrology, 153, 55-66.
Liu Q. and Lange R.A. (2006) The partial molar volume of Fe2O3 in alkali silicate melts: Evidence for an average Fe3+ coordination number near five. American Mineralogist, 91, 385-393.
Liu Q. and Lange R.A. (2003) The density of natrocarbonatite liquids: new measurements and the partial molar volume of the CaCO3 component. Contributions to Mineralogy and Petrology, 146, 370-381.
Liu Q. and Lange R.A. (2001) The partial molar volume and thermal expansivity of TiO2 in alkali silicate liquids: systematic variation with Ti coordination. Geochimica et Cosmochimica Acta, 65, 2379-2393.