Frank Donald Stacey (21 August 1929,
Essex, UK) is an English-born Australian geophysicist, known for his research on
rock magnetism[1] and application of thermodynamics to understanding the
Earth's core and
mantle.[2][3][1]
Education and career
At the
University of London, Stacey graduated with a B.Sc. in 1950 and a Ph.D. in 1953. As a postdoc, he was from 1953 to 1956 a research fellow at the
University of British Columbia in
Vancouver. From 1961 to 1964 he was a
Royal Society Gassiot Fellow in Geomagnetism at the
Meteorological Office Research Unit of the
University of Cambridge.[4] Near the beginning of his career he published several papers in The Philosophical Magazine.[5][6][7][8] He was a Reader in Physics at the
University of Queensland from 1964 to 1971[4] — during those years he wrote the first three editions of Physics of the Earth.[9] (In 1988 a fourth edition was published with Paul McEwan Davis as co-author.[9]) In 1968 Stacey received his D.Sc. from the University of London. From 1971 to 1990 he was a professor of Applied Physics at the University of Queensland.[4] He was appointed to visiting lectureships in several different countries. In 1997 he joined the
Australian Government agency
CSIRO Exploration and Mining.[9]
Louis Néel’s 1955 paper Some theoretical aspects of rock-magnetism[10] inspired Stacey to generalize Néel's single-domain theory for magnetic
grains to multi-domained grains. In the theory of
remanence for
igneous rocks, Stacey introduced the concept of pseudo-single domain for magnetic grains which are small and multi-domained.[1][11] He did research on scientifically describing
rock fabric using
magnetic anisotropy[1][12] and predicting earthquakes and volcanic eruptions using
piezomagnetism.[1][13][14] With several colleagues, Stacey investigated possible failures of Newton's law of gravity.[15][16][17][18][19][20]
Using a lattice dynamical formulation for the
Grüneisen parameter, he developed a new
equation of state for high pressures with applications to materials in the Earth's core and lower mantle.[1][21] His book Physics of the Earth became a widely used, standard textbook and was the first geophysics textbook to comprehensively deal with solid Earth geophysics.[1]
Stacey, Frank D. (1998). "Thermoelasticity of a mineral composite and a reconsideration of lower mantle properties". Physics of the Earth and Planetary Interiors. 106 (3–4): 219–236.
Bibcode:
1998PEPI..106..219S.
doi:
10.1016/S0031-9201(98)00084-3.
Stacey, Frank D.; Anderson, Orson L. (2001). "Electrical and thermal conductivities of Fe–Ni–Si alloy under core conditions". Physics of the Earth and Planetary Interiors. 124 (3–4): 153–162.
Bibcode:
2001PEPI..124..153S.
doi:
10.1016/S0031-9201(01)00186-8.
Stacey, F.D.; Davis, P.M. (2004). "High pressure equations of state with applications to the lower mantle and core". Physics of the Earth and Planetary Interiors. 142 (3–4): 137–184.
Bibcode:
2004PEPI..142..137S.
doi:
10.1016/j.pepi.2004.02.003.
Stacey, F.D.; Loper, D.E. (2007). "A revised estimate of the conductivity of iron alloy at high pressure and implications for the core energy balance". Physics of the Earth and Planetary Interiors. 161 (1–2): 13–18.
Bibcode:
2007PEPI..161...13S.
doi:
10.1016/j.pepi.2006.12.001.
Stacey, Frank D.; Hodgkinson, Jane H. (2019). "Thermodynamics with the Grüneisen parameter: Fundamentals and applications to high pressure physics and geophysics". Physics of the Earth and Planetary Interiors. 286: 42–68.
Bibcode:
2019PEPI..286...42S.
doi:
10.1016/j.pepi.2018.10.006.
S2CID125922484.
as editor with M. S. Paterson and A. Nicolas
Anelasticity in the Earth, Geodynamics Series, Vol. 4, American Geophysical Union/Geological Society of America 1981
^Stacey, F. D. (1962). "A generalized theory of thermoremanence, covering the transition from single domain to multi-domain magnetic grains". Philosophical Magazine. 7 (83): 1887–1900.
Bibcode:
1962PMag....7.1887S.
doi:
10.1080/14786436208213853.
^with Subir K. Banerjee The high field torque-meter method of measuring magnetic anisotropy of rocks, in D. W. Collinson, K. M. Creer, S. K. Runcorn (eds.) Methods in Palaeomagnetism, Elsevier 1967, pp. 470–476
^Stacey, F. D.; Tuck, G. J.; Holding, S. C.; Maher, A. R.; Morris, D. (1981). "Constraint on the planetary scale value of the Newtonian gravitational constant from the gravity profile within a mine". Physical Review D. 23 (8): 1683–1692.
Bibcode:
1981PhRvD..23.1683S.
doi:
10.1103/PhysRevD.23.1683.
^Stacey, F. D.; Tuck, G. J.; Moore, G. I.; Holding, S. C.; Goodwin, B. D.; Zhou, R. (1987). "Geophysics and the law of gravity". Reviews of Modern Physics. 59 (1): 157–174.
Bibcode:
1987RvMP...59..157S.
doi:
10.1103/RevModPhys.59.157.
^Schwarzschild, Bertram (1986). "Reanalysis of Old Eötvös Data Suggests 5th Force…To Some". Physics Today. 39 (10): 17–20.
doi:
10.1063/1.2815165.
Frank Donald Stacey (21 August 1929,
Essex, UK) is an English-born Australian geophysicist, known for his research on
rock magnetism[1] and application of thermodynamics to understanding the
Earth's core and
mantle.[2][3][1]
Education and career
At the
University of London, Stacey graduated with a B.Sc. in 1950 and a Ph.D. in 1953. As a postdoc, he was from 1953 to 1956 a research fellow at the
University of British Columbia in
Vancouver. From 1961 to 1964 he was a
Royal Society Gassiot Fellow in Geomagnetism at the
Meteorological Office Research Unit of the
University of Cambridge.[4] Near the beginning of his career he published several papers in The Philosophical Magazine.[5][6][7][8] He was a Reader in Physics at the
University of Queensland from 1964 to 1971[4] — during those years he wrote the first three editions of Physics of the Earth.[9] (In 1988 a fourth edition was published with Paul McEwan Davis as co-author.[9]) In 1968 Stacey received his D.Sc. from the University of London. From 1971 to 1990 he was a professor of Applied Physics at the University of Queensland.[4] He was appointed to visiting lectureships in several different countries. In 1997 he joined the
Australian Government agency
CSIRO Exploration and Mining.[9]
Louis Néel’s 1955 paper Some theoretical aspects of rock-magnetism[10] inspired Stacey to generalize Néel's single-domain theory for magnetic
grains to multi-domained grains. In the theory of
remanence for
igneous rocks, Stacey introduced the concept of pseudo-single domain for magnetic grains which are small and multi-domained.[1][11] He did research on scientifically describing
rock fabric using
magnetic anisotropy[1][12] and predicting earthquakes and volcanic eruptions using
piezomagnetism.[1][13][14] With several colleagues, Stacey investigated possible failures of Newton's law of gravity.[15][16][17][18][19][20]
Using a lattice dynamical formulation for the
Grüneisen parameter, he developed a new
equation of state for high pressures with applications to materials in the Earth's core and lower mantle.[1][21] His book Physics of the Earth became a widely used, standard textbook and was the first geophysics textbook to comprehensively deal with solid Earth geophysics.[1]
Stacey, Frank D. (1998). "Thermoelasticity of a mineral composite and a reconsideration of lower mantle properties". Physics of the Earth and Planetary Interiors. 106 (3–4): 219–236.
Bibcode:
1998PEPI..106..219S.
doi:
10.1016/S0031-9201(98)00084-3.
Stacey, Frank D.; Anderson, Orson L. (2001). "Electrical and thermal conductivities of Fe–Ni–Si alloy under core conditions". Physics of the Earth and Planetary Interiors. 124 (3–4): 153–162.
Bibcode:
2001PEPI..124..153S.
doi:
10.1016/S0031-9201(01)00186-8.
Stacey, F.D.; Davis, P.M. (2004). "High pressure equations of state with applications to the lower mantle and core". Physics of the Earth and Planetary Interiors. 142 (3–4): 137–184.
Bibcode:
2004PEPI..142..137S.
doi:
10.1016/j.pepi.2004.02.003.
Stacey, F.D.; Loper, D.E. (2007). "A revised estimate of the conductivity of iron alloy at high pressure and implications for the core energy balance". Physics of the Earth and Planetary Interiors. 161 (1–2): 13–18.
Bibcode:
2007PEPI..161...13S.
doi:
10.1016/j.pepi.2006.12.001.
Stacey, Frank D.; Hodgkinson, Jane H. (2019). "Thermodynamics with the Grüneisen parameter: Fundamentals and applications to high pressure physics and geophysics". Physics of the Earth and Planetary Interiors. 286: 42–68.
Bibcode:
2019PEPI..286...42S.
doi:
10.1016/j.pepi.2018.10.006.
S2CID125922484.
as editor with M. S. Paterson and A. Nicolas
Anelasticity in the Earth, Geodynamics Series, Vol. 4, American Geophysical Union/Geological Society of America 1981
^Stacey, F. D. (1962). "A generalized theory of thermoremanence, covering the transition from single domain to multi-domain magnetic grains". Philosophical Magazine. 7 (83): 1887–1900.
Bibcode:
1962PMag....7.1887S.
doi:
10.1080/14786436208213853.
^with Subir K. Banerjee The high field torque-meter method of measuring magnetic anisotropy of rocks, in D. W. Collinson, K. M. Creer, S. K. Runcorn (eds.) Methods in Palaeomagnetism, Elsevier 1967, pp. 470–476
^Stacey, F. D.; Tuck, G. J.; Holding, S. C.; Maher, A. R.; Morris, D. (1981). "Constraint on the planetary scale value of the Newtonian gravitational constant from the gravity profile within a mine". Physical Review D. 23 (8): 1683–1692.
Bibcode:
1981PhRvD..23.1683S.
doi:
10.1103/PhysRevD.23.1683.
^Stacey, F. D.; Tuck, G. J.; Moore, G. I.; Holding, S. C.; Goodwin, B. D.; Zhou, R. (1987). "Geophysics and the law of gravity". Reviews of Modern Physics. 59 (1): 157–174.
Bibcode:
1987RvMP...59..157S.
doi:
10.1103/RevModPhys.59.157.
^Schwarzschild, Bertram (1986). "Reanalysis of Old Eötvös Data Suggests 5th Force…To Some". Physics Today. 39 (10): 17–20.
doi:
10.1063/1.2815165.