Geostatistical characterization of a complex semi-permeable layer: Engineering geology of quaternary sediments. Proc. symposium, Delft, 1994, ed N. Rengers, (Balkema), 1994, symposium, Delft, 1994, ed N. Rengers, (Balkema), 1994, pp 73–92

Abstract

Presents a study to quantify the lithofacies distribution of a complex semi-permeable layer consisting of fluvial and organic deposits. In a small study area in the central Rhine-Meuse delta a large number of drillings were made in a semi-permeable layer overlying shallow permeable aquifers. Detailed cross sections and semivariogram analysis are used to quantify the spatial variability of fluvial overbank deposits in the semi-permeable layer and to determine minimal drilling distances for detailed mapping of the lithofacies. Conditional indicator simulation is applied to obtain simulated stochastic images of the semi-permeable layer. These images may serve as analogues for similar layers found at greater depths. -Authors

Keywords

General Environmental Science, General Earth and Planetary Sciences

Citation

Bierkens, M F P, Weerts, H J T & Burrough, P A 1994, 'Geostatistical characterization of a complex semi-permeable layer : Engineering geology of quaternary sediments. Proc. symposium, Delft, 1994, ed N. Rengers, (Balkema), 1994, symposium, Delft, 1994, ed N. Rengers, (Balkema), 1994, pp 73–92', International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, vol. 31, no. 6, pp. 277. https://doi.org/10.1016/0148-9062(94)90132-5