Open AccessAn Evaluation of the Active Fracture Concept in Modeling Unsaturated Flow and Transport in a Fractured Meter‐Sized Block of Rock
Author(s) -
Seol Yongkoo,
Kneafsey Timothy J.,
Ito Kazumasa
Publication year - 2006
Publication title -
vadose zone journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.036
H-Index - 81
ISSN - 1539-1663
DOI - 10.2136/vzj2004.0175
Subject(s) - tracer , mechanics , fracture (geology) , flow (mathematics) , matrix (chemical analysis) , permeability (electromagnetism) , complex fracture , geotechnical engineering , geology , computer simulation , boundary value problem , block (permutation group theory) , volumetric flow rate , petroleum engineering , materials science , mathematics , geometry , chemistry , physics , mathematical analysis , biochemistry , membrane , nuclear physics , composite material
Numerical simulation is an effective and economical method for optimally designing laboratory experiments and deriving practical experimental conditions. We executed a detailed numerical simulation study to examine the active fracture concept (AFC) using a 1‐m 3 ‐sized block model. The numerical simulations for this study were performed by applying various experimental conditions, including different bottom flow boundaries, varying injection rates, and different fracture–matrix interaction (i.e., by increasing absolute matrix permeability at the fracture–matrix boundary) for a larger fracture interaction under transient or balanced‐state flow regimes. Two conceptual block models were developed based on different numerical approaches: a two‐dimensional discrete‐fracture‐network model (DFNM) and a one‐dimensional dual‐continuum model (DCM). The DFNM was used as a surrogate for a natural block to produce synthetic breakthrough curves of water and tracer concentration under transient or balanced‐state conditions. The DCM is the approach typically used for the Yucca Mountain Project because of its computational efficiency. The AFC was incorporated into the DCM to capture heterogeneous flow patterns that occur in unsaturated fractured rocks. The simulation results from the DCM were compared with the results from the DFNM to determine whether the DCM could predict the water flow and tracer transport observed in the DFNM at the scale of the experiment. It was found that implementing the AFC in the DCM improved the prediction of unsaturated flow and that the flow and transport experiments with low injection rates in the DFNM compared better with the AFC implemented DCM at the 1‐m 3 scale. However, the estimated AFC parameter varied from 0.38 to 1.0 with different flow conditions, suggesting that the AFC parameter was not sufficient to fully capture the complexity of the flow processes in a 1‐m 3 discrete fracture network.