MR41A-2618
Characterization of Connectivity between Fractures and Nano-pores in Shale Using Gas Adsorption Analysis

Thursday, 17 December 2015
Poster Hall (Moscone South)
Han Jiang, University of Texas at Austin, Austin, TX, United States, Hugh Daigle, University of Texas, Austin, TX, United States and Nicholas W Hayman, Institute for Geophysics, Austin, TX, United States
Abstract:
Most pores hosting hydrocarbon in mudrocks are at the nanometer to tens of nanometer scale. However, observational evidence shows that natural and induced fractures which govern the permeability of mudrocks appear to be spaced at centimeter scale or greater. The mismatch in scales raises the question of how the hydrocarbons in the nanopores can gain access to the induced hydraulic fracture systems. To answer the question, we experimentally induced fractures on core-scale samples, and characterized microstructure around the stimulated fracture networks and in the surrounding, unfractured rock matrix. Confined compressive strength tests were performed on preserved core plugs from the Eagle Ford shale and a siliceous, oil-bearing mudrock from the northern Rocky Mountains. Dried, ground specimens were collected from before-test (intact) and after-test (failed) samples. Their pore structure was analyzed by N2/CO2 gas adsorption, which together can measure pore diameters between 0.35 and 300 nm. Adsorption data shows a Type IV N2 isotherm and a Type I CO2 isotherm. The hysteresis loop in the N2 adsorption curve indicates the presence of slit-shaped pores. Failed siliceous samples exhibit higher overall N2 and CO2 adsorbed gas amount compared with the intact samples, indicating a wide range increase of nanoporosity. Eagle Ford samples, however, show no significant change in adsorbed gas amount. We determined pore size distributions (PSDs) using density functional theory (DFT). The N2 PSDs of the siliceous samples appear to be bimodal, with a peak around 1 nm pore size, while the N2 PSDs of the Eagle Ford samples is unimodal. Comparison of intact and failed samples reveals no significant change in pore volume for Eagle Ford samples. The siliceous samples, in contrast, increase their nanopore volume (1-100 nm pore diameter) after fracturing. The increased nanoporosity may result from microcracks that develop in the matrix surrounding the main fractures that connect nano-scale pores. These microcrack networks could shorten the flow pathway of hydrocarbons from nanopores into the main fractures, and enhance the hydrocarbon production efficiency.