Influence of particle size on non-Darcy seepage of water and sediment in fractured rock-Reference-Cited by-同舟云学术

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Influence of particle size on non-Darcy seepage of water and sediment in fractured rock

Published:2016-12 Issue:1 Volume:5 Page:
ISSN:2193-1801
Container-title:SpringerPlus
language:en
Short-container-title:SpringerPlus

Author:

Liu Yu,Li Shuncai

Funder

Natural science fund for colleges and universities in Jiangsu Province

Jiangsu Normal University PhD Start Fund

Jiangsu Planned Projects for Postdoctoral Research Funds

National Natural Science Foundation of China

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://link.springer.com/content/pdf/10.1186/s40064-016-3778-9.pdf

Reference32 articles.

1. Bear J (1972) Dynamics of fluids in porous media. New York, Dover

2. Boutt DF, Grasselli G, Fredrich JT, Cook BK, Williams JR (2006) Trapping zones: the effect of fracture roughnesson the directional anisotropy of fluid flow and colloid transport in a single fracture. Geophys Res Lett 33:L21402. doi: 10.1029/2006GL027275

3. Cherubini C, Giasi CI, Pastore N (2012) Bench scale laboratory tests to analyze non-linear flow in fractured media. Hydrol Earth Syst Sci 16:2511–2522. doi: 10.5194/hess-16-2511-2012

4. Cherubini C, Giasi CI, Pastore N (2013) Evidence of non-Darcy flow and non-Fickian transport in fractured media at laboratory scale[J]. Hydrol Earth Syst Sci 17:2599–2611. doi: 10.5194/hess-17-2599-2013

5. Chin DA, Price RM, DiFrenna VJ (2009) Nonlinear Flow in Karst Formations[J]. Ground Water 47:669–674. doi: 10.1111/j.1745-6584.2009.00574.x

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