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Hydraulic permittivity

As a third special case, consider the mass flow resulting from a pressure difference between the two vessels maintained at a uniform temperature. According to Eq. (6.6.2b) this yields J = —(LuV /T)V P, which is an analogue of electric current flow arising from a difference of electrical potential. Accordingly, it is sensible to introduce a hydraulic permittivity, E, for mass flow, defined as [Why include the minus sign as part of the definition ]... [Pg.371]

The flow of a fluid through a geotextile is normally expressed by the coefiflcient of hydraulic conductivity, also known as the coefficient of permeability. It is generally normalised by the thickness of the geotextile for obtaining the permittivity and transmissivity in the cross-plane and in-plane directions respectively, as illustrated in the following eqnations ... [Pg.125]

See other pages where Hydraulic permittivity is mentioned: [Pg.557]    [Pg.32]    [Pg.32]    [Pg.557]    [Pg.32]    [Pg.32]    [Pg.246]    [Pg.140]    [Pg.525]    [Pg.208]    [Pg.125]    [Pg.125]    [Pg.277]    [Pg.277]    [Pg.174]    [Pg.831]    [Pg.417]    [Pg.567]    [Pg.571]    [Pg.229]    [Pg.417]    [Pg.567]    [Pg.571]   
See also in sourсe #XX -- [ Pg.371 ]

See also in sourсe #XX -- [ Pg.358 ]



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