GSA Connects 2024 Meeting in Anaheim, California

Paper No. 52-4
Presentation Time: 2:20 PM

COST-EFFECTIVE DEVELOPMENT OF LACUSTRINE SHALE OIL IN BOHAI BAY BASIN, CHINA: CONNECTIVITY, WETTABILITY, MOVABILITY, AND FRACABILITY (Invited Presentation)


HU, Qinhong1, LIU, Huimin2, XIUGANG, Pu3, YANG, Shengyu1, WANG, Qiming1, ZHANG, Tao4, LIN, Zizhi1 and YIN, Na1, (1)National Key Laboratory of Deep Oil and Gas, China University of Petroleum (East China), Qingdao, 266580, China, (2)Shengli Oilfield of SinoPec, Dongying, 257015, China, (3)PetroChina Dagang Oil Field Company, Tianjin, 300280, China, (4)Department of Earth & Environmental Sciences, The University of Texas at Arlington, Arlington, TX 76019

Shale oil development from lacustrine depositions in China has been showing major breakthroughs towards economic and sustainable production, but also implicated with a steep production decline in stimulated shale formations. Working with Paleogene-aged Shahejie and Kongdian Formations with low to moderate maturity in Bohai Bay Basin, China, this presentation shows that the limited matrix-fracture interaction (e.g., anomalous matrix feeding of petroleum molecules from the poorly-connected matrix pore space to the hydraulically-stimulated fracture networks) is the root cause of steep initial decline and low overall recovery. The matrix-fracture interaction is influenced by connectivity, wettability, movability, and fracability of shale formations, such as a predominance of minerals-related and generally water-wet pore space in shales of low to moderate maturity. However, there is a poor pore connectivity of fine-grained shale matrix with a wide spectrum of nm-μm sized pore networks to lead to anomalous diffusion and limited movability, and it’s important to assess the fracability to generate intensive fracture networks to reduce the matrix feeding distance for a sustained shale petroleum production. This is achieved by utilizing a set of complementary and experimental approaches such as porosimetry (mercury intrusion porosimetry, low-pressure gas physisorption isotherm, nuclear magnetic resonance), imaging [X-ray computed tomography, Wood’s metal impregnation, field emission-scanning electron microscopy (SEM), focus ion beam-SEM, µm and nm-CT), scattering (ultra- and small-angle neutron and X-ray)], the utility of both hydrophilic and hydrophobic fluids and associated tracers as well as fluid invasion tests (imbibition, diffusion, vacuum saturation) followed by laser ablation-inductively coupled plasma-mass spectrometry imaging of different nm-sized tracers.