MULTISCALE PORE SYSTEM RECONSTRUCTION AND INTEGRATION

ABSTRACT Better understanding of single-/multi-phase flow through reservoir rocks largely relies on the characterisation of the pore system. For homogeneous rock materials, a complete description of the real pore structure can be obtained from the network extracted from a rock image at a single resolution. However, for complex rocks (e.g., carbonates, heterogeneous sandstones, deformed rocks etc.), a comprehensive description of the real pore structure may involve many decades of length-scales (e.g., from sub-micron to cm), which cannot be captured by a single-resolution image. Hence, the creation of a 3D multiple-scale model of a porous medium is an important step in quantitatively characterising such heterogeneous rocks and predicting their multi-phase flow properties using pore -scale network modelling. In this paper, we describe a series of pore architecture models (PAMs) to reconstruct 3D reservoir rocks from 2D thin section images along with a set of pore analysis tools (PATs) to extract the corresponding pore network systems. Specifically, we created the multiple scale pore structure through "multiple scale reconstruction". We present a methodology to construct multi-scale (or combined) networks based on the statistical description of pore-networks of 3D rock images at multiple resolutions. Using such networks, two-phase network modeling results are presented for carbonate samples to illustrate the importance of topology in the hierarchical pore structure. We show examples where isolated large-scale pores (e.g. vugs) are connected by small-scale pores, thus determining the combined effective petrophysical properties (capillary pressure, absolute and relative permeability). Finally, we indicate how the stochastic network generation method can be used to combine information from multiple images at the same resolution but obtained at different locations

Stochastic Pore Network Generation from 3D Rock Images

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A scoping review and thematic analysis of social and behavioural research among HIV-serodiscordant couples in high-income settings.

CAPRISA, 2015.Abstract available in pdf

A Hydro-Geomechanical View of Seal Formation and Failure in Overpressured Basins

The formation of seals, and the consequent retention of overpressure, is a common and expected event during normal basin evolution in active basins that have a significant mudrock succession. Seal failure, and the resultant limitation to fluid-pressure increase (valve action), is also an expected process. Hydro-geomechanical concepts, including poro-elasto-visco-plasticity (PEVP), and discontinuum models, allow the processes of seal formation and failure to be explained, and predict the state of stress in, and behaviour of, overpressured rocks. Importantly, properties that relate to porosity (such as permeability) can be integrated with this approach. These concepts provide a capability to undertake simulations that can serve as predictive tools. The fluid/rock interactions in a basin can be viewed as a self-organizing system, in the sense that overpressure and the undercompaction it permits retard the creation of accommodation space, and hence act as a negative feedback mechanism that slows the loading rate