Geology Reference
In-Depth Information
The following derivative property
d {sgn t}/dt = 2 (t)
(1.146)
is also applicable, where sgn(t) = +1, t > 0; -1, t < 0. Important integral
properties involving the delta function include
(x-a) (x-b) dx = (a-b)
(1.147)
e i
(a-x) d
= 2
(x-a)
(1.148)
'(t- )
(t) dt = -
(t- )
'(t) dt = - '( )
(1.149)
Also, if x 0 is defined by u(x 0 ) = 0, with u(x) monotonically increasing or
decreasing, it can be shown that
{u(x)} (x) dx = (x 0 ) / |u'(x 0 )|
(1.150)
If
(t) = 1, t > 0; and 0, t < 0, it is possible to show that
t
( - ) d =
(t- )
(1.151)
Finally,
e -st
'(t- ) dt = s e -s
, where s > 0
(1.152)
In particular, when = 0 ,
e -st
'(t) dt = s, where s > 0
(1.153)
so that we have the inverse
L -1 {s} = '(t)
(1.154)
Note that Equation 1.153 alone is not a valid transform, since it does not
vanish as s . The dipole forcing function '(t), though, generally appears on
the right-sides of differential equations; the quotient formed by s and the
Laplace transform of the differential operator, representing the transform of the
quantity of physical interest, does vanish as s increases.
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