Figure 1. Three images of an east to west cross-section. The nine hydrogeologic units from the conceptual geologic model are shown in (a). A geostatistical realization of porosity conditioned on borehole data and the conceptual geologic model is shown in (b). The upscaled porosity values within the flow-model grid are shown in (c).
McKenna, S.A. & Altman, S.J.Geostatistical simulation, parameter development and property scaling for GWTT-95,
report,
February 1, 1996;
Albuquerque, New Mexico.
(https://digital.library.unt.edu/ark:/67531/metadc669894/m1/4/:
accessed April 25, 2024),
University of North Texas Libraries, UNT Digital Library, https://digital.library.unt.edu;
crediting UNT Libraries Government Documents Department.