Graduation Semester and Year

2015

Language

English

Document Type

Thesis

Degree Name

Master of Science in Earth and Environmental Science

Department

Earth and Environmental Sciences

First Advisor

Max Hu

Abstract

The Late Devonian Three Forks Formation has increasingly become one of the productive plays in the Williston Basin, North Dakota. This growth has been attributed not only to new drilling and completion techniques but also to the availability of new geological information. Although production in the Three Forks Formation has increased, maximum recovery and overall hydrocarbon production is still limited. According to the North Dakota Industrial Commission, the oil recovery factor in the Three Forks Formation is 8.9±5.32%, so only a small percentage of the original oil in place is being produced.One of the most challenging aspects of reservoir quality in the Three Forks Formation has been characterizing the permeability, porosity and tortuosity which affect fluid flow and chemical transport in tight rocks. These parameters are macroscopic manifestation of the pore geometry and topology which are not easily accessible because of the dominant nanometer-scale pores. More information is needed with regards to the nanopore size distribution and how the pore connectivity is related to fracture networks.The mixed siltstone/sandstone/carbonate samples for all of five members of the Three Forks Formation were obtained from well Round Prairie 1-17H from Williams County (API No. 18257). For these tight rocks, we have studied the pore structure, edge-accessible porosity, and wettability using the following complementary tests: mercury intrusion capillary pressure, tracer imbibition and tracer diffusion into fluid-saturated rock. The latter was done by pulling a vacuum on dry rock followed by the introduction of a tracer-free fluid. These tests use tracer-bearing fluids (API brine or n-decane) to examine the association of tracers with mineral or kerogen phases, followed by elemental analyses with laser ablation-ICP-MS to map out the presence and distribution of tracers inside the rock. The results from these innovative approaches indicate the limited accessibility and connectivity of nanopores in the samples. In addition, the Three Forks Formation seems to be mostly oil-wetting, with fast imbibition and diffusion for n-decane tracers. The interplay of wettability and connectivity could lead to the steep first-year production decline and low recovery factors because of the limited pore connectivity which inhibits the migration of hydrocarbon molecules in the rock matrix to the stimulated fracture network.

Disciplines

Earth Sciences | Physical Sciences and Mathematics

Comments

Degree granted by The University of Texas at Arlington

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