scholarly journals Regional channelized transport in fractured media with matrix diffusion and linear sorption

2008 ◽  
Vol 44 (2) ◽  
Author(s):  
Magnus Odén ◽  
Auli Niemi ◽  
Chin-Fu Tsang ◽  
Johan Öhman
1992 ◽  
Vol 294 ◽  
Author(s):  
Paul A. Smith

ABSTRACTIn the safety assessment of nuclear waste repositories, sorption of radionuclides on the surfaces of colloids may significantly modify transport behaviour where colloid concentration is sufficiently high. In the case of fractured geological media, colloids may be excluded from matrix pores, in which case radionuclides bound to them are not subject to the retarding effects of matrix diffusion and sorption onto matrix pore surfaces.A model is presented describing colloid facilitated transport through fractured media with non-linear sorption. A simple criterion is developed to predict when the presence of colloids will have a significant influence on transport and effects resulting from non-linearity of sorption are described. However, lack of comprehensive sorption data, as well as computational efficiency, mean that the use of a simplified transport model, with linear sorption both on pore surfaces and colloids, is desirable if it can be demonstrated to be conservative. A further criterion is developed to predict where such a model, with linear sorption calculated for the highest concentration encountered along the flow path, would be expected to yield conservative results.


2019 ◽  
Vol 46 (23) ◽  
pp. 13785-13795 ◽  
Author(s):  
Jeffrey D. Hyman ◽  
Harihar Rajaram ◽  
Shriram Srinivasan ◽  
Nataliia Makedonska ◽  
Satish Karra ◽  
...  

2020 ◽  
Author(s):  
Bryan Heyer ◽  
◽  
Trevor C. Osorno ◽  
Barbara A. Carrera ◽  
Chin Man W. Mok ◽  
...  

2019 ◽  
Vol 128 (2) ◽  
pp. 701-721 ◽  
Author(s):  
Sergi Molins ◽  
David Trebotich ◽  
Bhavna Arora ◽  
Carl I. Steefel ◽  
Hang Deng

2018 ◽  
Vol 36 (5) ◽  
pp. 1279-1294 ◽  
Author(s):  
Sheng-Li Li ◽  
You-Hong Sun ◽  
Kai Su ◽  
Wei Guo ◽  
You-Hai Zhu

Fracture-hosted methane hydrate deposits exist at many sites worldwide. The growth behavior of CH4 hydrate in fractured media was simulated by TOUGH + HYDRATE (T + H) code. The effects of fracture size, initial condition, and salinity on the growth behavior of hydrate in fractures were investigated. In general, the hydrate layer grew from the two ends and gradually covered on the surface of the fracture. With the formation of hydrate in fractures, the temperature increased sharply since the hydrate acted as a thermal insulation layer. In longer fractures, fast growth of hydrate at the ends of the fracture led to the formation of hydrate plugs with high saturation (called as stopper). In narrower fractures, hydrate dissociation occurred in the middle of the fracture during hydrate growing in the whole fracture due to the cutoff of gas supply by the stopper at the ends. At a low initial subcooling, hydrate formed both on the surface and in the micropores of the media, which was different from that at higher subcooling. In salt solution, the formation of hydrate stopper was inhibited by the salt-removing effect of hydrate formation and the growth of hydrate was more sustainable.


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