There is mounting evidence that self-similarity (scale-invariance) characte
rizes many geological phenomena (and much of the physical world), particula
r those associated with the fluid-rock stress interactions of cracks and mi
crocracks in rocks. This pervasive self-similarity is a result of the criti
cality of the distributions of stressed fluid-saturated crack, microcrack,
and low aspect-ratio pores in reservoir rock. Criticality has profound impl
ications for the response of hydrocarbon reservoirs to changes during produ
ction, and hence for the concept of reservoir characterization. The bad new
s is that these implications include: (1) the existence of spatial and temp
oral heterogeneities at all scale lengths; (2) the inappropriateness of Gau
ssian statistics (averages are no longer meaningful); (3) the inability to
reliably extrapolate from place to plate and from time to time; and (4) the
possibility of any known or measured reservoir characteristics degrading w
ith time. These specifically limit the success of conventional reservoir ch
aracterization. The good news is that criticality means that: (1) the respo
nse of a known reservoir to known changes can be calculated by anisotropic
pore-elasticity (APE); (2) the current configuration can be monitored by se
ismic shear-wave splitting; (3) the response to given changes (waterflood i
njection pressures, say) can be predicted by APE; and (4) the reservoir can
be controlled via feedback by adjusting input parameters (injection pressu
res, say) to optimise the effects (water flooding, say) monitored by shear-
wave splitting. Finally, the technology for monitoring producing reservoirs
with high-frequency shear-waves along short ray paths within the reservoir
itself is now being developed in the UNIWELL configuration of three-compon
ent geophones and source(s) in the same producing well. UNIWELL will allow
detailed fluid-fluid and fluid-rock interactions to be monitored around the
production well as frequently as necessary. (C) 1999 Elsevier Science B.V.
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