The Mathematics of Fluid Flow Through Porous Media. Myron B. Allen, III

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x partial-differential y EndFraction plus c StartFraction partial-differential squared u Over partial-differential y squared EndFraction equals upper F left-parenthesis x comma y comma u comma StartFraction partial-differential u Over partial-differential x EndFraction comma StartFraction partial-differential u Over partial-differential y EndFraction right-parenthesis period"/>

      Here,

,
, and
are functions of the independent variables
and
, which we can replace with
and
in time‐dependent problems;
is the unknown solution; and
denotes a function of five variables that describes the lower‐order terms in the PDE.

, which is a function of
. Equation (1.1) is

       hyperbolic at any point of the ‐plane where ;

       parabolic at any point of the ‐plane where ;

       elliptic at any point of the ‐plane where .

      Extending this terminology, we say that a first‐order PDE of the form

      is hyperbolic at any point

where
.

and
are real‐valued with
:

      In contrast to most texts on pure mathematics, in this book physical dimensions play an important role. We adopt the basic physical quantities length, mass, and time, having physical dimensions

,
, and
, respectively. All other physical quantities encountered in this book—except for one case involving temperature in Chapter 7 —are derived quantities, having physical dimensions that are products of powers of
,
, and
.

      For example, the physical dimension of force

arises from Newton's second law
, where
denotes mass and
denotes acceleration:

      Physical laws such as

require a way to assign numerical values to the physical quantities involved. We do this by comparison with standards, a process called measurement. For example, to assign a numerical value to the length of an object, we compare it to a length to which we have assigned a numerical value by fiat. A choice of standards for measuring
, normal upper 
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