Core-Derived Velocity Systematics, Mississippian Meramec Formation, Oklahoma

Elastic wave velocities are commonly used to predict porosity, mineralogy, and lithology from formation properties. When only P-wave sonics are available in historical wells, systematics for predicting shear velocities are useful for developing elastic models. Although much research has been done on conventional reservoir velocity systematics, the equivalency for unconventional formations is still a work in progress. There has also been a limited number of research studies with laboratory measures published. Using laboratory pulse transmission ultrasonic data, we created a V-p-V-s systematic for the Meramec Formation in this study. The effects of porosity and mineralogy on velocities are explored, as well as a comparison of Meramec velocity systematics with well-established literature systematics. V-p and V-s measurements were taken on 385 dodecane-saturated core samples from seven Meramec wells (106 vertical and 279 horizontal plugs). S-wave and P-wave anisotropy in Meramec Formation samples used in this study are typically less than 10%. Each sample was also tested for porosity and mineralogy. We find that velocities are more sensitive to porosity than mineralogy by a factor of 10. Below are our equations for predicting V-p and V-s (in km/s), when only clay content and porosity are known. In these equations, phi is the volume fraction pores, and Clays is the weight fraction of clay. These equations are for those samples in which there is low P-wave and S-wave anisotropies: V-p = 6.4 - 1:2 * Clays - 15.4 * phi(R-2 = 0:5), ....(1) V-s = 3.6 - 0:5 * Clays - 5.2 * phi(R-2 = 0:4). ....(2) We suggest two methods for calculating V-s from V-p: Ignoring anisotropy, we combined both V-p and V-s measurements from all vertical plugs and low anisotropy horizontal plugs to create a single shear wave predictor; and considering anisotropy, V-p measurements from horizontal plugs were corrected using Thomsen's compressional wave anisotropy parameter, after which a shear velocity predictor was generated. The shear wave predictors for dodecane-saturated measurements are as follows (all velocities are km/s): Method 1 : V-s = 0.90 + 0.42 * V-p (R-2 = 0:7), ...(3) Method 2 : V-s = 0.80 + 0.45 * V-p (R-2= 0:6). ...(4) The residual and estimated error in Eq. 3 is slightly less than in Eq. 4. Even though there is a significant variance in measurement frequency, the Meramec velocity systematic shows good agreement with dipole wireline measurements using the first equation. The Meramec velocity systematics differ significantly from previously published systematics, such as the trend line by Greenberg and Castagna (1992) and the shale trend line by Vernik et al. (2018). Using the correlations by Greenberg and Castagna (1992) for limestone or dolomite, the shear velocities of the samples in this study cannot be predicted. These data have yielded shear wave systematics, which can be used in wireline and seismic investigations. The results suggest that the method of ignoring anisotropy yields a better Vs estimate than the one that takes anisotropy into account. Using well-established shear wave velocity systematics from the published literature can result in an estimated inaccuracy of greater than 16%. It is important to calibrate velocity systematics to the target formation.

Automated summary

This study develops V-p and V-s velocity systematics for the Meramec Formation using laboratory data and compares them with existing systematics. The study finds that porosity has a greater impact on velocity than mineralogy. It also suggests two methods for calculating V-s from V-p and highlights the importance of calibrating velocity systematics to the target formation.