William M. White

Geochemistry


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      Since volume is area times distance, we can substitute eqn. 2.3 and dV = Adx into eqn. 2.1 and obtain:

      Thus, work is also done as a result of a volume change in the presence of pressure.

      Potential energy is energy possessed by a body by virtue of its position in a force field, such as the gravitational field of the Earth, or an electric field. Chemical energy will be of most interest to us in this book. Chemical energy is a form of potential energy stored in chemical bonds of a substance. Chemical energy arises from the forces involved in the interaction between atoms and electrons. Internal energy, which we denote with the symbol U, is the sum of the potential energy arising from these forces as well as the kinetic energy of the atoms and molecules (i.e., thermal energy) in a substance. It is internal energy that will be of most interest to us.

      We will discuss all these fundamental variables in more detail in the next few sections.

      2.2.2 Properties of state

      A final definition is that of a pure substance. A pure substance is one that cannot be separated into fractions of different properties by the same processes as those considered. For example, in many processes, the compound H2O can be considered a pure substance. However, if electrolysis were involved, this would not be the case.

      Equations of state describe the relationship that exists among the state variables of a system. We will begin by considering the ideal gas law and then very briefly consider two more complex equations of state for gases.

      2.3.1 Ideal gas law

      The ideal gas law, and any equation of state, can be rewritten with intensive properties only. Dividing V by N we obtain the molar volume, images. Substituting images for V and rearranging, the ideal gas equation becomes:

      (2.7)equation

      which reduces to:

      (2.8)equation

      It would be more useful to know the fractional volume change rather than the absolute volume change with temperature, because the result in that case does not depend on the size of the system. To convert to the fractional volume change, we simply divide the equation by V:

      (2.10)equation

      The left-hand side of this equation, the fractional change in volume with change in temperature, is known as the coefficient of thermal expansion, α:

      (2.11)equation

      The compressibility of a substance is defined in a similar manner as the fractional change in volume produced by a change in pressure at constant temperature:

      (2.12)equation

      Geophysicists sometimes use the isothermal bulk modulus, KT, in place of compressibility. The isothermal bulk modulus is simply the inverse of compressibility: KT = 1/β. Through a similar derivation to the one we have just done for the coefficient of thermal expansion, it can be shown that the compressibility of an ideal gas is β = 1/P.

      The ideal gas law can be derived from