Viscosity of albite melt at high pressure and high temperature

被引:83
作者
Suzuki, A
Ohtani, E
Funakoshi, K
Terasaki, H
Kubo, T
机构
[1] Tohoku Univ, Inst Mineral Petrol & Econ Geol, Sendai, Miyagi 9808578, Japan
[2] JASRI, Mikazuki, Hyogo 6795198, Japan
[3] Univ Tsukuba, Inst Geosci, Tsukuba, Ibaraki 3058571, Japan
关键词
viscosity; high pressure; magma; silicate melt; molecular simulation;
D O I
10.1007/s00269-001-0216-4
中图分类号
T [工业技术];
学科分类号
08 [工学];
摘要
The viscosity of albite (NaAlSi(3)O(8)) melt was measured at high pressure by the in situ falling-sphere method using a high-resolution X-ray CCD camera and a large-volume multianvil apparatus installed at SPring-8. This system enabled Lis to conduct in situ viscosity measurements more accurately than that using the conventional technique at pressures of up to several gigapascals and viscosity in the order of 10(0) Pa s. The viscosity of albite melt is 5.8 Pa s at 2.6 GPa and 2.2 Pa s at 5.3 GPa and 1973 K. Experiments at 1873 and 1973 K show that the decrease in viscosity continues to 5.3 GPa. The activation energy for viscosity is estimated to be 316(8) kJ mol(-1) at 3.3 GPa. Molecular dynamics simulations suggest that a gradual decrease in viscosity of albite melt at high pressure may be explained by structural changes such as an increase in the coordination number of aluminum in the melt.
引用
收藏
页码:159 / 165
页数:7
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