Summary The cementation exponent, m, is a major factor of uncertainty in the calculation of hydrocarbon/ water saturation in heterogeneous carbonate reservoirs. Hydrocarbon saturations as high as 70 or 80%, calculated with the conventional value m = 2, may disappear completely with m values of 3 and 4 (Fig. 1), which are quite common in carbonate rocks. Laboratory data obtained in heterogeneous carbonate reservoirs often show a wide scatter (Fig. 2). Constant (average) m values are usually used in spite of such scatter, and data points with m values much higher than the average value are often rejected to obtain straight-line trends. This paper presents the results of a study of the relationship between variable m values measured on core plugs and detailed carbonate rock types. The scatter in the data is analyzed in terms of rock type. We conclude that the high m values are often representative for specific rock types and that these values should not be rejected but applied selectively in log analysis over those intervals where these rock types occur.
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Focke et al. (1987) studied this question.
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