Table 1 Using a NUFT model to simulate the propagation of pressure fluctuations between the surface of Aqueduct Mesa and the monitoring borehole embedded in the Disko Elm collapse chimney, a five-parameter variation study was performed to obtain a best fit of the pressure-fluctuation history to observations.

From: Gas transport across the low-permeability containment zone of an underground nuclear explosion

Parameter

Unit

Minimum

Maximum

Mean of top 10

Best

Fracture aperture

[m]

1.0000 × 10−4

1.0000 × 10−2

1.2442 × 10−3

8.4258 × 10−4

Fracture frequency

[−]

0.5000

10.000

1.2324

1.0379

Fracture permeability

[m2]

1.0000 × 10−14

1.0000 × 10−9

4.9911 × 10−9

6.9158 × 10−10

Matrix permeability

[m2]

1.0000 × 10−18

1.0000 × 10−15

9.1720 × 10−18

1.0014 × 10−17

Bulk permeability

[m2]

2.6655 × 10−18

1.3801 × 10−11

5.1549 × 10−13

4.5269 × 10−13

  1. To obtain the best fit simulation yielding a bulk permeability of the containment zone of 0.45 Darcys (4.5 × 10−13 m2) required performing 1000 simulations. This value is about 1/10 of that obtained for the Barnwell site on Pahute Mesa. In addition to the best fits obtained for the five parameters, the maximum, minimum and means of the best 10 fits are also provided. The best-fit parameter set produced excellent agreement between the simulated and observed chimney-pressure fluctuation over the 20-day history that was considered.