Geostatistical Modeling of Sediment Abundance in a Heterogeneous Basalt Aquifer at the Idaho National Laboratory, Idaho

Scientific Investigations Report 2006–5316

U.S. GEOLOGICAL SURVEY
Scientific Investigations Report 2006–5316
DOE/ID-22201

Figure - refer to figure caption for alternative text description

Figure 20. Comparison of local cumulative frequency distributions (CFDs) derived from multiple indicator kriging (mIK) at two locations in Layer A, representing locations with low (location 1) and high (location 2) estimation variance. Median sediment contents (Z₅₀) computed from the local CFDs are used to estimate horizontal and vertical hydraulic conductivity with equations 2 and 3. Local CFD probabilities for an 11 percent sediment threshold were used to estimate bulk hydraulic conductivities with equation 4.

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