Experimental Investigation of Transient Thermal Convection in Porous Media

被引:14
|
作者
Cooper, C. A. [1 ]
Crews, J. B. [1 ]
Schumer, R. [1 ]
Breitmeyer, R. J. [2 ]
Voepel, H. [1 ]
Decker, D. L. [1 ]
机构
[1] Desert Res Inst, Div Hydrol Sci, Reno, NV 89512 USA
[2] Univ Nevada, Dept Geol Sci & Engn, Reno, NV 89557 USA
基金
美国国家科学基金会;
关键词
Rayleigh number; Instability; Buoyancy; Density-driven flow; EVAPORATING SALT LAKE; ONSET; GROUNDWATER; LAYER;
D O I
10.1007/s11242-014-0337-0
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
A laboratory experiment of transient thermal convection in a 1-m-high cell was conducted to compare the length and time scales of plume development to theory. The temperature field was resolved to less than 1 mm and was measured by dissolving a solution of thermochromic crystals into the water-glycerin working fluid. The time-dependent experiment was run by applying heat at the bottom boundary that eventually was C above the background temperature of the fluid. After development of a thermal boundary layer, the instability became visible at 26 min, with the development of 11, 3-4 cm width plumes growing from the boundary layer. The initially rapid growth rate reached a limiting velocity of approximately 0.5 cm min, and then decelerated throughout the experiment. Plumes interacted primarily by merging together; by the end of the experiment only three plumes were present. The Nusselt number at the onset of convection was 10, although it dropped to 4 after 45 min, which would be expected of a barely unstable system.
引用
收藏
页码:335 / 347
页数:13
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