Laboratory and Numerical Studies of Heat Extraction from Hot Porous Media by Means of Supercritical 详细信息    查看全文
  • 作者:Mario J. Magliocco ; Steven D. Glaser ; Timothy J. Kneafsey
  • 关键词:Carbon dioxide ; Heat transfer ; Laboratory experiment ; Numerical simulation ; Enhanced?(engineered)?geothermal?systems
  • 刊名:Transport in Porous Media
  • 出版年:2015
  • 出版时间:May 2015
  • 年:2015
  • 卷:108
  • 期:1
  • 页码:85-104
  • 全文大小:1,543 KB
  • 参考文献:Brown, D.W.: A hot dry rock geothermal energy concept utilizing supercritical \(\text{ CO }_{2}\) instead of water. In: Proceedings of the Twenty-Fifth Workshop on Geothermal Reservoir Engineering, Stanford University, pp. 233-38 (2000)
    Eastman, A.D., Muir, M.P., Energy, G.: CO\(_{2}\) EGS and the utilization of highly pressurized \(\text{ CO }_{2}\) for purposes other than power generation. In: Proceedings of the Twenty-Eighth Workshop on Geothermal Reservoir Engineering. Stanford University (2013)
    King, S., Beck, F., Lüttge, U.: On the mystery of the golden angle in phyllotaxis. Plant Cell Environ. 27.6, 685-95 (2004)View Article
    Kunii, D., Smith, J.M.: Heat transfer characteristics of porous rocks. AIChE J. 6(1), 71-8 (1960)View Article
    Lemmon, E.W., McLinden, M.O., Friend, D.G.: Thermophysical properties of fluid systems. NIST chemistry WebBook, NIST standard reference database number 69. In: Linstrom, P.J., Mallard, W.G. (eds.) National Institute of Standards and Technology, Gaithersburg MD, http://?webbook.?nist.?gov , (retrieved September 2010)
    Liao, S.M., Zhao, T.S.: Measurements of heat transfer coefficients from supercritical carbon dioxide flowing in horizontal mini/micro channels. J. Heat Transf. 124.3, 413-20 (2002)View Article
    Majer, E.L., Baria, R., Stark, M., Oates, S., Bommer, J., Smith, B., Asanuma, H.: Induced seismicity associated with enhanced geothermal systems. Geothermics 36.3, 185-22 (2007)View Article
    Powell, R.W., Ho, C.Y., Liley, P.E.: Thermal conductivity of selected materials. (No. NSRDS-NBS-8). In: National Standard Reference Data System (1966)
    Pruess, K.: The TOUGH codes—a family of simulation tools for multiphase flow and transport processes in permeable media. Vadose Zone J. 3, 738-46 (2004)
    Pruess, K.: Enhanced geothermal systems (EGS) using \(\text{ CO }_{2}\) as working fluid—a novel approach for generating renewable energy with simultaneous sequestration of carbon. Geothermics 35(4), 351-67 (2006)View Article
    Pruess, K.: Enhanced geothermal systems (EGS) comparing water with \(\text{ CO }_{2}\) as heat transmission fluids. In: Proceedings, New Zealand Geothermal Workshop 2007 Auckland, New Zealand (2007)
    Pruess, K., Spycher, N.: ECO2N—a fluid property module for the TOUGH2 code for studies of storage in saline aquifers. Energy Convers. Manag. 48.6, 1761-767 (2007)View Article
    Randolph, J.B., Saar, M.O.: Coupling carbon dioxide sequestration with geothermal energy capture in naturally permeable, porous geologic formations: implications for \(\text{ CO }_{2}\) sequestration. Energy Procedia 4, 2206-213 (2011). doi:10.-016/?j.?egypro.-011.-2.-08 View Article
    Tester, J.W., Anderson, B., Batchelor, A., Blackwell, D., DiPippo, R., Drake, E., Garnish, J., Livesay, B., Moore, M.C., Nichols, K., Petty, S., Toksoz, N., Veatch, R., Augustine, C., Baria, R., Murphy, E., Negraru, P., Richards, M.: The future of geothermal energy: impact of enhanced geothermal systems (EGS) on the United States in the 21st century. In: Massachusetts Institute of Technology, DOE Contract DE-AC07-05ID 14517 Final Rept., p. 374 (2006)
    Woodside, W.T., Messmer, J.H.: Thermal conductivity of porous media. I. Unconsolidated sands. J. Appl. Phys. 32.9, 1688-699 (1961)View Article
  • 作者单位:Mario J. Magliocco (1)
    Steven D. Glaser (1)
    Timothy J. Kneafsey (2)

    1. Department Civil and Environmental Engineering, University of California, Berkeley, CA, 94720, USA
    2. Lawrence Berkeley National Laboratory, Berkeley, CA, 94720, USA
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Geotechnical Engineering
    Industrial Chemistry and Chemical Engineering
    Civil Engineering
    Hydrogeology
    Mechanics, Fluids and Thermodynamics
  • 出版者:Springer Netherlands
  • ISSN:1573-1634
文摘
The use of \(\hbox {CO}_{2}\) as a heat transfer fluid has been proposed as an alternative to water in enhanced geothermal systems (EGS) and in \(\hbox {CO}_{2}\)-plume geothermal systems (CPG). Numerical simulations have shown that under expected EGS operating conditions, \(\hbox {CO}_{2}\) would achieve more efficient heat extraction performance compared to water, especially at sites with low geothermal temperatures and low subsurface heat flow rates. With increased interest in carbon capture and sequestration (CCS), the possibility of combining geothermal energy production with carbon sequestration is actively being explored. Simulations have shown that \(\hbox {CO}_{2}\)-based geothermal energy production could substantially offset the cost of CCS. Since numerical models are critical for the planning and operation of geothermal systems that employ \(\hbox {CO}_{2}\) as the working fluid, it is important to validate the results of the current numerical tools against real- world experimental data. In a set of laboratory experiments, we have investigated heat extraction by flowing dry supercritical \(\hbox {CO}_{2}\) through a heated porous medium in a laboratory pressure vessel and have compared experimental results with a numerical model using TOUGH2 with the ECO2N module. In addition, experiments were performed using (1) \(\hbox {CO}_{2}\) and (2) water as the working fluids under similar operating conditions in order to compare the heat transfer behavior and the overall heat extraction rates. Our laboratory apparatus is capable of operating at temperatures up to 200?\(^{\circ }\hbox {C}\), pressures up to 34.5?MPa, and flow rates up to 400?ml/min. The experimental system was designed such that measurements and controls at the boundaries could be readily modeled using TOUGH2. We have made estimates of the density and the effective thermal conductivity of our saturated porous media, and have found that both properties change significantly during the course of experiments. The large changes in \(\hbox {CO}_{2}\) density, due to decreasing system temperatures, can result in fluid accumulation in the system that may have significant impacts on geothermal reservoir management. The large changes in thermal conductivity as a function of temperature are of concern because the TOUGH2 code does not update the thermal conductivity of the system during the course of a simulation. Our data can be used by geologic reservoir modelers to ensure that their models accurately capture the heat extraction behavior of \(\hbox {CO}_{2}\) to aid in the further investigations of EGS, CPG, and CCS.

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