Wettability of the Montney Tight Gas Formation

Abstract

Summary The abundant hydrocarbon resources in low-permeability formations are now technically accessible because of advances in the drilling and completion of multilateral/multifractured horizontal wells. However, measurement and modeling of petrophysical properties, required for reserves estimation and reservoir-engineering calculations, are the remaining challenges for the development of tight formations. In particular, characterizing wettability (wetting affinity) of tight rocks is challenging because of their complex pore structure, which can be either in hydrophobic organic materials or in hydrophilic inorganic materials. We conduct comparative and systematic imbibition experiments on 10 twin core plugs from the Montney tight gas formation, which is an enormous tight gas fairway in the Western Canadian Sedimentary Basin. Both contact-angle and imbibition data indicate that the formation has a stronger affinity to oil than to water. However, the ratio between oil and water uptake of these samples is usually higher than what capillary-driven imbibition models predict. This discrepancy can be explained by the strong adsorption of oil on the surface of a well-connected organic-pore network that is partly composed of degraded bitumen. We also define a wettability index on the basis of the equilibrium oil and water uptake of the twin samples. Oil-wettability index is positively correlated with total organic carbon and clay content of the rocks, which generally increase from the upper Montney to the lower Montney.

Influence of Water Immersion on Pore System and Methane Desorption of Shales: A Case Study of Batu Gajah and Kroh Shale Formations in Malaysia

“…In the case of water immersion, the BG sample water uptake was higher than the KH sample. Such differences in the water uptake of the samples were related to the hydrophilic and hydrophobic nature of the clay minerals and organic matter, respectively [16,43,44]. In addition to that, in our previously published work on the same samples, the BG sample was more water wet than the KH sample [1].…”

Pore Connectivity Characterization of Lacustrine Shales in Changling Fault Depression, Songliao Basin, China: Insights into the Effects of Mineral Compositions on Connected Pores

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Geochemical and petrographic characterization of the Upper Ordovician Utica Shale, southern Quebec, Canada

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