Observation of Pore Spaces and Microcracks Using a Fluorescent Technique in Some Reservoir Rocks of Oil, Gas and Geothermal Fields in the Green Tuff Region, Japan

Abstract: Pore spaces and microcracks in representative oil, gas and geothermal reservoir rocks from the Green Tuff region, Japan, were examined using a fluorescent technique. This technique was developed to visualize microscopically pore spaces and microcracks filled with synthetic resin mixed with fluorescent paint under ultraviolet light. Various morphology of pore spaces and microcracks was clearly identified. Spaces in studied reservoir rocks are classified into following three types: pore spaces in matrix, pore spaces in particles, and microcracks. It is observed that valuable oil and gas reservoir rocks relatively include many pore spaces, while microcracks are important for geothermal rocks. Correlation between textural characteristics and porosity or permeability was found in the oil reservoir rocks. Effective permeability depends upon pore spaces in matrix more than upon other components such as pore spaces in particles and microcracks. Looseness in matrix caused by larger grain size of particles is strongly correlated with permeability. Pore spaces play an important role as a reservoir in oil and gas fields, but are less important in geothermal field. Instead, microcracks are important for geothermal reservoir system.

[1]  H. J. Fraser Experimental Study of the Porosity and Permeability of Clastic Sediments , 1935, The Journal of Geology.

[2]  Kunio Watanabe,et al.  Natures of under ground water flow in granite acting as an agent in weathering , 1982 .

[3]  R. Kranz Microcracks in rocks: a review , 1983 .

[4]  嘉一 関口,et al.  地化学的見地からみた長岡・柏崎地域のグリーンタフ油・ガス鉱床の形成 , 1984 .

[5]  F. Homand-Etienne,et al.  Behaviour of granites and limestones subjected to slow and homogeneous temperature changes , 1984 .

[6]  S. Kato Characteristics of reservoir rocks in the Green tuff - Studies on hydrocarbon deposits in the Green Tuff in the Niigata basin, Japan. Part 1. , 1987 .

[7]  T. Uchida Pore-size distributions and the evaluation of permeability in reservoir rocks - A proposal of empirical expressions with regard to petrological properties of pores.:a proposal of empirical expressions with regard to petrological properties of pores , 1987 .

[8]  S. Kato Characteristics of Hydrocarbon Deposits in the Green Tuff , 1988 .

[9]  M. Yamakawa,et al.  Analysis of Fracture System in Granitic Rock , 1989 .

[10]  S. Nakashima,et al.  Micropore distibutions in granite as material migration pathways , 1989 .

[11]  Yoji Seki,et al.  The physical and chemical structure of the Oku-aizu geothermal system, Japan , 1991 .

[12]  T. Ishida,et al.  Grain boundary microcracking of granitic rocks from the northeastern region of the Atotsugawa fault, central Japan: SEM backscattered electron images , 1991 .

[13]  H. Kusuda,et al.  Extraction and Evaluation of Microcracks in Rocks by Methods of Image Processing , 1994 .

[14]  Takashi Nishiyama,et al.  Identification of pore spaces and microcracks using fluorescent resins , 1994 .

[15]  H. Kusuda,et al.  Process of tuff weathering and its assessment , 1994 .

[16]  Tomiya Nitta,et al.  Exploration and development in the Okuaizu Geothermal Field, Japan , 1995 .

[17]  H. Kusuda,et al.  Application of a fluorescent technique to the study of the weathering process , 1996 .