| 2008 Joint Meeting of The Geological Society of America, Soil Science Society of America, American Society of Agronomy, Crop Science Society of America, Gulf Coast Association of Geological Societies with the Gulf Coast Section of SEPM | |
| Paper No. 313-12 | |
| Presentation Time: 4:30 PM-4:45 PM | ||
The Forchheimer Number, the Reynolds Number, and Non-Darcy Flow In Porous Media: An Experimental Investigation | ||
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LI, Jian1, HUANG, Guanhua2, ZHAN, Hongbin3, and WEN, Zhang1, (1) Department of Irrigation and Drainage, College of Water Conservation and Civil Engineering, China Agricultural University, Beijing, 100083, China, li_jian@cau.edu.cn, (2) Department of Irrigation and Drainage, College of Water Conservation and Civil Engineering, and Chinese-Israeli International C, China Agricultural University, Beijing, 100083, China, (3) Department of Geology & Geophysics, Texas A&M University, Mail Stop 3115, College Station, TX 77843 A series of experiments were conducted in packed porous media with different grain diameters under relatively high velocity conditions. The experimental results show that relationships between the hydraulic gradient (i) and the specific discharge (q) deviate from Darcy's law. The change of the ratio of the hydraulic gradient and the specific discharge (i/q) with q is analyzed to determine different flow regimes. The experimental results indicate that both the power-type Izbash and the Forchheimer equations fit the experimental data equally well. In terms of the Forchheimer equation, the Forchheimer number (F0) is calculated and recommended as an alternative criterion to identify non-Darcy flow. Such a criterion is compared with another conventionally used criterion of the Reynolds number. Some advantages of using the Forchheimer number have been discussed and compared with those of using the Reynolds number. We have proposed a new relationship between the friction factor and the Forchheimer number. This new relationship may be used to predict the critical specific discharge or hydraulic gradient for non-Darcy flow to start. | ||
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2008 Joint Meeting of The Geological Society of America, Soil Science Society of America, American Society of Agronomy, Crop Science Society of America, Gulf Coast Association of Geological Societies with the Gulf Coast Section of SEPM
General Information for this Meeting | ||
| Session No. 313 Hydrogeology II - Groundwater, Non-Darcian Flow, and Nomenclature George R. Brown Convention Center: 332AD 1:30 PM-5:30 PM, Wednesday, 8 October 2008 Geological Society of America Abstracts with Programs, Vol. 40, No. 6, p. 498 | ||
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