Other considerations on particle dynamics
681
hence the equation of motion of the particle on the active segment of a line. These
results allow to solve also some interesting problems of optimum.
3.2.4 The balloon problem
A problem in the frame of those studied above is that of a balloon of weight
m
,
which rises along the vertical by a continuous throwing of the ballast over the border.
We assume that the balloon is acted upon by an ascensional force
A , corresponding to
Archimedes’ theorem (hence, a force equal to the weight of a volume of air
corresponding to that of the balloon), and by the resistance of the air, the magnitude of
which is in direct proportion to the square of the velocity (
2
()Qv kv= ,
constk =
).
The equation of motion along the ascendent vertical reads
2
mx mg A kx mw=− + − + , (10.3.45)
hence it is a differential equation of the first order of Riccati’s type in
()xt , which may
be integrated by two quadratures if a particular integral is known.
If, e.g., the condition that the motion of the balloon be uniform is put
(
0
xv= ,
0
constv = ), then we get an equation with separate variables, which leads to
(with
constw = and the initial condition
0
(0)mm
)
()
2
0
//
0
() 1 e e
gt w gt w
Qkv
mt m
g
−−
−
=−+
. (10.3.45')
If the ballast
()Mt is thrown in a sufficiently long time, so that the factor
/
e
gt w−
be
practically zero for
() 0Mt → together with t →∞, then we have
(
2
00 0
/mM Qkvg−=− ,
0
(0)MM
, and the relation (10.3.45') leads to
/
0
() e
gt w
Mt M
−
= ; (10.3.45'')
hence, if the mass of the ballast varies after an exponential law, then the ascensional
motion of the balloon is uniform.
3.2.5 External ballistic problem
Let us consider a more general case of motion of a heavy particle
P
of variable
mass in the air, at the Earth surface. We assume that the trajectory is a plane curve (see
Subsec. 3.1.6 too), the particle being acted upon by the weight
m
, by the reactive
force
Rm==Rwτ ,
0m
(
is the unit vector of the tangent to the trajectory in
the direction of the motion) and by the resistance
Q=−Q τ
, with
2
00
(/2) ( / )Qb Avρρρ= (Fig.10.23), where b is the aerodynamical coefficient, ρ
and
0
ρ represent the density of the air at a given height and at the Earth surface,
respectively, while
A is a characteristic area of the body modelled as a particle. We
notice that we can take, in general,
3
()( )bvxψϕ
, so that