Compression behavior of WC and WC-6%Co up to 50 GPa determined by synchrotron x-ray diffraction and ultrasonic techniques

被引:25
作者
Amulele, George M. [1 ]
Manghnani, Murli H. [1 ]
Marriappan, Sekar [1 ]
Hong, Xinguo [1 ]
Li, Fengung [1 ]
Qin, Xiomei [1 ]
Liermann, Hanns P. [2 ]
机构
[1] Univ Hawaii, Hawaii Inst Geophys, Honolulu, HI 96822 USA
[2] Argonne Natl Lab, Adv Photon Source, Argonne, IL 60439 USA
基金
美国国家科学基金会;
关键词
D O I
10.1063/1.2938024
中图分类号
O59 [应用物理学];
学科分类号
摘要
The equations of state (pressure-volume relations) for WC and WC-6%Co have been determined by synchrotron x-ray diffraction measurements on polycrystalline powder samples loaded in a diamond anvil cell as well as by ultrasonic measurements on hot-pressed polycrystalline, cylindrical samples loaded in a multianvil high-pressure apparatus. The third-order Birch-Murnaghan equation of state fitted to the x-ray diffraction pressure-density sets of data, collected up to 50 GPa, yields ambient pressure isothermal bulk moduli of K(oT)=411.8 +/- 12.1 GPa and K(oT)=402.4 +/- 14.1 GPa, with pressure derivatives of K'(oT)=5.45 +/- 0.73 and K'(oT)=7.50 +/- 0.86 for WC and WC-6%Co, respectively. The ultrasonic measurements, conducted up to 14 GPa, enabled the determination of the pressure dependences of both bulk and shear moduli. Using Eulerian finite strain equations to fit the ultrasonic data, we obtain for WC an ambient pressure adiabatic bulk modulus of K(os)=383.8 +/- 0.8 GPa, and K'(os)=2.61 +/- 0.07 for its pressure derivative, while values of G(os)=304.0 +/- 0.3 GPa and G(os)(')=1.50 +/- 0.09 were determined for the shear modulus and its pressure derivative, respectively. Meanwhile, for WC-6%Co, we obtain K(os)=357.5 +/- 1.0 GPa, K'(os)=5.18 +/- 0.14, G(os)=253.5 +/- 0.3 GPa, and G(os)(')=1.09 +/- 0.09. The equations of state derived from the ultrasonic data are in good agreement with extrapolated results reported previously by Day and Ruoff [J. Appl. Phys. 44, 2447 (1973)] and Gerlich and Kennedy [J. Appl. Phys. 50, 3331 (1978)] who carried out measurements up to 0.2 and 1.0 GPa, respectively. (C) 2008 American Institute of Physics.
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页数:6
相关论文
共 25 条
[1]   Compression studies of TiB2 using synchrotron x-ray diffraction and ultrasonic techniques -: art. no. 023506 [J].
Amulele, GM ;
Manghnani, MH .
JOURNAL OF APPLIED PHYSICS, 2005, 97 (02)
[2]   High pressure ultrasonic and x-ray studies on monolithic SiC composite [J].
Amulele, GM ;
Manghnani, MH ;
Li, BS ;
Errandonea, DJH ;
Somayazulu, M ;
Meng, Y .
JOURNAL OF APPLIED PHYSICS, 2004, 95 (04) :1806-1810
[3]   Compression mechanisms and equations of state [J].
Angel, RJ ;
Ross, NL .
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1996, 354 (1711) :1449-1459
[4]   FINITE STRAIN ISOTHERM AND VELOCITIES FOR SINGLE-CRYSTAL AND POLYCRYSTALLINE NACL AT HIGH-PRESSURES AND 300-DEGREE-K [J].
BIRCH, F .
JOURNAL OF GEOPHYSICAL RESEARCH, 1978, 83 (NB3) :1257-1268
[5]   FINITE ELASTIC STRAIN OF CUBIC CRYSTALS [J].
BIRCH, F .
PHYSICAL REVIEW, 1947, 71 (11) :809-824
[7]  
Dandekar DP, 2002, AIP CONF PROC, V620, P783, DOI 10.1063/1.1483654
[8]   HOMOGENEITY AND CONSTITUTION OF EARTHS LOWER MANTLE AND OUTER CORE [J].
DAVIES, GF ;
DZIEWONSKI, AM .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1975, 10 (04) :336-343
[9]  
DAY JP, 1973, J APPL PHYS, V44, P2477
[10]   SOUND VELOCITIES AT HIGH-PRESSURE AND TEMPERATURE AND THEIR GEOPHYSICAL IMPLICATIONS [J].
DUFFY, TS ;
AHRENS, TJ .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1992, 97 (B4) :4503-4520