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Substitution in the continuity equation finally yields div (*<J>1 <grad ,)) = *! Sip) dt
where the coefficient 5s = (p)M g [/3 + (a/(a>))] (dimension length"1) is called the
specific storage coefficient of the medium. It is then usual in hydrogeology to ...
where the subscript minus sign in [$t, pit)]- indicates that this quantity is a
commutator. Equation (207) is the quantum analog of the classical Liouville
equation, so we call it the quantum Liouville equation. The quantum Liouville
equation given ...
Liouville equations. Many of these equations, as well as other phenomenological
equations, were originally developed on the basis of intuitive arguments about
the nature of a system. For the most part, phenomenological equations have ...
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Seismology Observational 17 Stochastic Description
Seismology Theoretical 47 Solar Chimneys
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