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Carbonate Petrophysical Parameters Derived from 3d Images *
Mark Knackstedt1, Mahyar Madadi1, Christoph Arns1, Gregor Baechle2, Gregor Eberli2, and Ralf Weger2
Search and Discovery Article (2009)
Posted March 20, 2009
*Adapted from extended abstract prepared for presentation at AAPG Annual Convention, San Antonio, Texas, April 20-23, 2008
1Australian National University, Canberra, Australia ([email protected] )
2Comparative Sedimentology Lab, University of Miami, Miami, FL. ([email protected] )
Carbonate
rocks are extremely diverse and their pore spaces complex and heterogeneous.
Large uncertainties in the petrophysical properties of carbonates are due
to wide variations in pore type, pore shape and interconnectivity. Petrophysical
properties such as acoustic 
velocity
, permeability, and resistivity are
directly correlated to the amount and type of porosity, the dominant feature
size, and the interconnectivity of different porosity types. Accurately
measuring these attributes requires the quantitative 3D analysis of the
pore structure of carbonates. In this article we describe the imaging and
analysis of two types of carbonate core: a set of vuggy, recrystallized
dolostones and a set of oomoldic limestones. The structure and topology
of the pore space is accurately determined via micro-CT analysis and the
porosity consistent with experimental data. Acoustic velocity-porosity,
pore connectivity, and porosity permeability relationships are derived
directly on the image data via numerical simulation and compared with measured
data on the same rock. Acoustic velocity:porosity trends are good. Pore
structural properties (pore size, aspect ratios, pore and throat shape
and connectivity) are determined. The correlations between pore geometry
and topology and elastic and flow properties can be directly probed in
a systematic manner. Three dimensional imaging and analysis of carbonate
core material can provide a basis for more accurate petrophysical modeling
and improve carbonate reservoir characterization.
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Many
studies have demonstrated the importance of the pore structure
in carbonates on petrophysical properties (e.g., Anselmetti and
Eberli, 1993, Wang, 1997; Saleh and Castagna, 2004; Kumar and Han,
2005; Rossebø et al., 2005). Traditional pore type classifications
describe the pore structures but fail to quantify the pore system
for correlations to the rock’s physical properties. In order to
quantitatively describe 2-D pore size, pore surface roughness,
aspect ratio, and pore network complexity in carbonates, a digital
image analysis (DIA) methodology was developed that produces repeatable
quantitative pore shape parameters (Weger, 2006). Each of these
quantitative parameters describes a certain aspect of the pore
shape. When these parameters are compared to acoustic data, the
two DIA parameters that capture the pore complexity and the pore
size plus the amount of microporosity prove to be the most influential
for the acoustic behavior of the samples. Each of these parameters
explains about 60% of the variations in
There is now an opportunity to image and characterise the pore structure of cores in 3D. This is based on coupling high resolution x-ray micro-tomography and high end computational software methods, including visualizing core material at the pore scale in 3D, measuring structural properties, and directly predicting physical properties directly from digitised 3D images (Arns, 2004; Arns, 2005) . This allows one to extend previous 2D studies to the 3D pore scale structure. In this paper we describe the 3D study of a set of carbonate samples including pore partitioning and simulation of the elastic properties directly on image data. Predictions from digital images are directly compared to measured data.
The
investigated samples are three recrystallized dolostones and three
oolitic grainstones with moldic pores and
In the recrystallized dolostone samples, the separation between pores and grains (crystals) is easily achieved. In the moldic limestones two pore size populations are detected; large, partly leached, round pores and small pores (1-2 micron). In these samples mercury injection indicates presence of micro- or disconnected porosity (Figure 1 ). The volume of the microporosity in these three samples is 0.3% of 14.1%, 8.3% of 24.8%, and 10.4% of 19.5% total porosity. The porosity is calculated directly from the image data. In all samples the image porosity is comparable to the measured porosity.
From the 3D images the
elastic properties of the samples are calculated using an elastic
simulation (FEM) that takes into account both the solid matrix
and the microporosity (Arns, 2002). Voxels in the solid matrix
are assigned values of the elastic moduli for calcite (K,G = 63.7,
31.2 GPa) and the elastic properties in the microporous regions
are based on the effective medium theory for sintered granular
like structure in which the bulk (K) and shear modulus (G) are
a function of porosity. Comparison of the simulated and measured
sonic velocities are given in Figure
2
. For both the re-crystallized dolostones
and moldic limestones, the calculated sonic
Macro/Microporosity and Macropore Phase Connectivity
The three dolostone samples exhibit 100% connected porosity; in Figure 3 we show an example of the pore partitioning within a slice of one dolostone sample and a 3D network structure for the same sample. The 3D volume allows displaying the pore connectivity. In the sample a number of pore structural parameters can be measured; for example, the average pore connectivity is measured as 15.7, meaning that a pore is connected to 15 other pores. The maximum pore connectivity is 83. Connectivity, pore size information and pore shape can be directly used to calculate permeability and multiphase flow properties (Arns, 2005).
The oolitic limestone samples exhibit both resolvable macroscopic porosity and significant microporosity. Tests for connectivity of the resolved macroporous phase in the oolitic systems show that only one system is macroscopically connected at image resolution (see Figure 4 ). The other two samples exhibit disconnected macropores at the resolution of the image. Conclusion
The results of the 3D imaging and analysis study show that the structure and petrophysical properties of carbonate core can be quantified in 3D. Specific conclusions include:
1. High-resolution CT scans with a resolution of 2.5 microns provide a 3D quantitative structure of carbonate samples. Image porosity correlates well with measured plug porosity. 2. Calculated sonic velocities from FEM simulation based on information from high-resolution CT scans compare well to measured sonic velocities. 3. Recrystallized dolostones exhibit well connected porosity which can be directly quantified in 3D. The pore space topology and pore size information is directly measurable. Moldic rocks exhibit significant proportions of microporosity (porosity below image resolution of ~5 microns). Only one of three moldic samples exhibits connected porosity in 3D. 4. Permeability:porosity crossplots for the same rock type will be undertaken. Correlation of permeability to key geometrical attributes (e.g., pore connectivity and pore to throat aspect ratios) and to acoustic data will be undertaken. References
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