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.
Search WWH ::
Custom Search