2015 Volume 121 Issue 9 Pages 311-323
We present the depositional environments and geostatistical modeling of the spatial distribution of mud content within a sequence stratigraphic framework for a CO2 reservoir at Nagaoka, Japan. Carbon dioxide was injected into strata interpreted as deltaic or coastal plain deposits characterized by upward-shallowing successions. The spatial distribution of the mud content, as estimated by geostatistical modeling, shows sandy sediments prograding from the lower to the upper part of the reservoir. Geophysical monitoring during and after CO2 injection suggests that CO2 migration within reservoir rocks is inhomogeneous; CO2 breakthroughs were observed at two observation wells, but were not observed at one observation well (OB-3), although the wells are located at similar distances from the injection well. The results of geostatistical modeling also indicate the heterogeneous distribution of muddy sediments. The heterogeneity of the CO2 distribution can be explained by the distribution of muddy sediments around well OB-3, which is located at the most distal (offshore) location. Genetic interpretations of the spatial distribution of mud can be useful for predicting and estimating the distribution of injected CO2 in a reservoir.