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Published online 16 August 2005
Published in Vadose Zone J 4:694-707 (2005)
DOI: 10.2136/vzj2004.0080
© 2005 Soil Science Society of America
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Hydrologic Behavior of Unsaturated, Fractured Tuff

Interpretation and Modeling of a Wellbore Injection Test

Bruce A. Robinsona,*, Stephen G. McLinb and Hari S. Viswanathana

a Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, NM 87545
b Environmental Stewardship Division, Los Alamos National Laboratory, Los Alamos, NM 87545



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Fig. 1. Locations of injection and monitoring wells for the unsaturated zone injection test. From Purtymun et al. (1989).

 


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Fig. 2. Injection system used in the unsaturated zone injection test. From Purtymun et al. (1989).

 


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Fig. 3. Measured flow conditions during the unsaturated zone injection test (Site 2, Test 1 of Purtymun et al., 1989). (a) Downhole injection pressure versus time. (b) Injection flow rate versus time. (c) Cumulative mass of water injected during the test.

 


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Fig. 4. Contours of water content constructed from the neutron log data during and after the injection test. (a) Day 7 after injection; (b) Day 29; (c) Day 55; (d) Day 89 (end of injection phase); (e) Day 327 (post-injection phase). From Purtymun et al. (1989).

 


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Fig. 5. Discrete fracture model (DFM) simulations. Left: injection into a fracture in the Bandelier tuff, showing the velocities along the length of the fracture and the concentration profile (higher concentrations are represented as white) after two years of injection. Right: DFM for the Basalt, showing preferential flow in the fracture.

 


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Fig. 6. Numerical grid used in the simulations of the injection test, showing the resolution and the location of the injection interval. (a) Top view. (b) Side view. (c) Perspective view.

 


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Fig. 7. Two-dimensional cross-sections of water content through the model for various times during the injection test. Times correspond to those at which the cross-sections of Fig. 5 were prepared.

 


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Fig. 8. Predicted and measured rates of water migration vertically downward and horizontally, along with locations of upward migration. Symbols, data; lines, model predictions. Curves and points corresponding to the upward migration refer to the right axis.

 


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Fig. 9. Two-dimensional cross-sections of water content at Day 55, comparing (a) the single continuum model (SCM), (b) SCM with decreased {alpha}g, and (c) equivalent continuum model.

 


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Fig. 10. Two-dimensional cross-sections of water content comparing the equivalent continuum model (ECM) and dual permeability model (DKM) formulations. (a) ECM, Day 7; (b) DKM, Day 7, effective matrix length scale of 0.1 m; (c) DKM, Day 7, effective matrix length scale of 1 m; (d) DKM, after one day of injection, effective matrix length scale of 10 m; (e) fracture water content corresponding to d (color scale is from 0 to 0.1 for this figure only).

 





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