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6







            PETROPHYSICAL EVALUATION OF GAS SHALE
            RESERVOIRS




            Mehdi Labani and Reza Rezaee
            Department of Petroleum Engineering, Curtin University, Perth, WA, Australia





            6.1  INTRODUCTION                                    for a shale formation to be considered as a potential gas
                                                                 shale layer are discussed.
            For many years, shale formations were viewed as a hydro­
            carbon source rock or cap rock. Due to this traditional point   6.2.1  Pore System Characteristics
            of view, only geochemical analysis has been routinely
            performed on the shale layers. However, for sweet spot   Pore system characteristics are very important for evaluation
            mapping of the gas shale layers, it is necessary to know   of gas shale reservoirs. Pores within the matrix of the gas
            about petrophysical and geomechanical properties as well as   shale reservoirs are smaller than pores in the conventional
            geochemical ones. The main focus of this chapter is the   reservoirs (Nelson, 2009). The main types of pore spaces in
            petrophysical evaluation methods of shale formations. In the   productive gas shale systems are matrix porosity, either
            first section, the key properties for evaluation of potential   associated with mineral particles or organic matter, and frac­
            gas shale intervals are defined, and then the available   ture porosity, either natural or induced fractures (Wang and
            techniques for measuring these parameters will be discussed.   Reed, 2009). In gas shale systems, matrix pores along with
            The chapter will be wrapped up with the common well log   natural networks of fractures provide the flow of gas from
            signatures of the gas shales and ways to interpret them for   matrix to induced fractures during production. Generally, in
            finding petrophysical properties of shale intervals.  describing the matrix pore size in shales the pores are all
                                                                 considered to fall within the nanopore range (Javadpour,
                                                                 2009; Javadpour et al., 2007; Loucks et al., 2009). There is a
            6.2  KEY PROPERTIES FOR GAS SHALE                    pore classification system for materials that contain nanometer‐
            EVALUATION                                           scale porosity developed by Rouquerol et al. (1994).
                                                                 According to this pore classification, micropores are <2 nm
            Shale is a fine‐grained detrital sedimentary rock, formed by   diameter, mesopores are between 2 and 50 nm, and
            the consolidation of clay (less than 4 µm) and silt (between     macropores are >50 nm. Mesopores and micropores are
            4 and 62.5 µm) sized particles into rock layers of ultralow     economically important to gas shale production because
            permeability. In general, shales are characterized by finely   of  their large contribution to porosity and storage sites
            laminated rocks and/or fissility approximately parallel to the   for methane (Keller et al., 2011). Recently, Loucks et al.
            bedding (Serra, 1988).  This definition gives the  lowest   (2012) defined a new pore size classification for matrix‐
            opportunity for shale as a reservoir. However, the right   related  mudrock pores; however, herein the Rouquerol’s
              combinations of geological, geochemical, petrophysical,   classification has been used.
            and geomechanical properties would result in a productive   To find out more about the pore system of organic‐rich
            gas shale interval. In the following sections, the key properties   shale layers, it is necessary to know about the accessible



            Fundamentals of Gas Shale Reservoirs, First Edition. Edited by Reza Rezaee.
            © 2015 John Wiley & Sons, Inc. Published 2015 by John Wiley & Sons, Inc.
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