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MODELS OF DYNAMIC GEOLOGIC SYSTEMS 269
definite reservoir-rock properties. These groups were identified by means of com-
parison with the well-testing results. An example of identification of beds and a
measure of their subdivision into groups (correlation coefficient or generalized Eu-
clidian distance) were used by Buryakovsky et al. (1990).
The fS o (see Eq. 11.103) of reservoir rocks was evaluated by simulating processes
of compaction and other diagenetic changes of sediments, as described above. Ex-
amples of simulation of reservoir-rock properties are presented in Table 11.13 (or in
Fig. 11.36).
Fig. 11.36. Statistical distributions of calculated values of petrophysical properties of rocks. (a) Porosity
(fraction), (b) permeability (mD), (c) residual water saturation (fraction). Formations: 1 – Balakhany;
2 – Fasila; 3 – NKP; 4 – PK. (After Buryakovsky, 2001, p. 406.)
