A theoretical formula of permeability tensor based on crack tensor has been proposed as an effective stress-dependent hydraulic conductivity tensor for jointed rock masses modeled as three sets of orthogonal joints. In this study, a stress-dependent equation was developed for application to general joint structures obtained from field joint surveys. It was used to investigate changes in the anisotropy of the hydraulic conductivity tensor with respect to depth. The anisotropy of the hydraulic conductivity tensor was expressed by the parameter FA using the invariants of the hydraulic conductivity tensor, and the rotation of the principal direction is also shown. The results were as follows:
• If the stress field is isotropic and the pseudo-elasticity index H of the joint is constant, the anisotropy of the hydraulic conductivity tensor is determined by the anisotropy of the joint structure and is maintained with respect to depth. In this case, the average hydraulic conductivity is uniquely depth-dependent, regardless of the anisotropy of the crack structure.
• Under non-isotropic stress, the depth change in FA and rotation of the anisotropic principal axis are noticeable in shallow areas and move to deeper areas depending on the H of the joint. Therefore, the estimation of H is important.
• Without considering the mutual interference between the joint structure and ground stress, it is not possible to infer the directional dependence of the hydraulic conductivity tensor.
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