Solute transport along a single fracture with a finite extent of matrix: A new simple solution and temporal moment analysis

2018 ◽  
Vol 562 ◽  
pp. 290-304 ◽  
Author(s):  
Shuo Meng ◽  
Longcheng Liu ◽  
Batoul Mahmoudzadeh ◽  
Ivars Neretnieks ◽  
Luis Moreno
Keyword(s):  
Solute Transport ◽  
Moment Analysis ◽  
Simple Solution ◽  
Single Fracture ◽  
Temporal Moment ◽  
Finite Extent

Temporal moment analysis for stochastic-advective vertical solute transport in heterogeneous unsaturated soils

2015 ◽  
Vol 521 ◽  
pp. 261-273 ◽  
Author(s):  
Richa Ojha ◽  
Arun Prakash ◽  
Corrado Corradini ◽  
Renato Morbidelli ◽  
Rao S. Govindaraju
Keyword(s):  
Solute Transport ◽  
Unsaturated Soils ◽  
Moment Analysis ◽  
Temporal Moment

Laboratory Experiments on Solute Transport in a Partial Transfixion Single Fracture

2011 ◽  
Vol 23 (5) ◽  
pp. 570-579 ◽  
Author(s):  
Jin-long Cai ◽  
Zhi-fang Zhou ◽  
Yong Huang
Keyword(s):  
Solute Transport ◽  
Laboratory Experiments ◽  
Single Fracture

Fluid Flow and Solute Transport though a Fracture Intersecting a Canister - Analytical Solutions for the Parallel Plate Model

2003 ◽  
Vol 807 ◽  
Author(s):  
L. Liu ◽  
I. Neretnieks
Keyword(s):  
Fluid Flow ◽  
Solute Transport ◽  
Flow Rate ◽  
Analytical Solutions ◽  
Parallel Plate ◽  
Spent Nuclear Fuel ◽  
Volumetric Flow Rate ◽  
Single Fracture ◽  
Plate Model ◽  
Specific Scenario

ABSTRACTIn this paper, we are concerned with a specific scenario where a large fracture intersects, at its center, a canister that contains spent nuclear fuel. Assuming that a nuclide is free to release from the canister into groundwater flowing through the fracture, a detailed formulation of the volumetric flow rate and the equivalent flow rate are made for the parallel plate model. The formulas proposed have been validated by numerical examinations; they are not only simple in forms but also universal in applications where the flow may be taken normal, inclined or parallel to the axis of the canister. Of great importance, they provide a convenient way to predict the average properties of fluid flow and solute transport through a single fracture with spatially variable apertures.

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