
358 15 The Newton-Nelson Equation
where =
h
2π
, h is Plank’s constant and I is the unit n × n matrix. In this
case we also say that the stochastic-mechanical system with force ¯α(t, x, X)
is given. The equality (15.6) is called the Newton-Nelson equation.
From the second equation of (15.6) it follows that ξ(t) is a process of type
(8.15) with σ such that
σ
2
2
=
2m
.
If σ = 0, the process ξ(t) from Definition 15.2 turns into a deterministic
curve and (15.6) becomes the ordinary Newton law (15.5). Without loss of
generality we assume m = 1.
Remark 15.3. Equality (15.6) for the Euclidean space R
n
was first obtained
by Nelson in [187]. It was also shown there that among all possible definitions
of the acceleration of a stochastic process which are symmetric in time (i.e.,
well-defined physically) and coincide with the ordinary definition for smooth
trajectories, only Definition 15.1 gives the correct result for some particular
examples in quantum mechanics. Later equation (15.6) (for potential forces
and in the form where the right-hand side is transformed according to (15.4))
was derived from some variational principles (see [190]).
Note that in stochastic mechanics one deals with the “quantization” of
Newton’s second law, while in the ordinary quantization procedures some
other equations of motion (Euler-Lagrange or Hamilton) are involved.
The correspondence between stochastic mechanics and ordinary (Hamil-
tonian) quantum mechanics was established for potential forces (see, e.g.,
[187, 188, 190]) and for certain forces with friction [233] where both the
Schr¨odinger equation and Newton-Nelson equation (15.6) are well-defined.
We illustrate this correspondence with an example of potential forces. The
arguments here are close to those in [187], but since we apply Lemmas 8.17
and 8.18 instead of classical results for Markov diffusions, we show that the
correspondence is also valid under the assumption that the trajectories are
Itˆo processes of diffusion type.
Let the force field ¯α of the mechanical system be a potential, i.e., it does
not depend on velocity and ¯α = −grad V ,whereV is the potential energy.
Let ξ(t) be a trajectory of the stochastic-mechanical system as in Definition
15.2 with this force. Recall that for the osmotic velocity u
ξ
(t)=u
ξ
(t, ξ(t))
the vector field u
ξ
(t, x) is always described in the form u
ξ
= σ
2
grad R,where
R =
1
2
log ρ
ξ
(t, x)(see(8.18)). Let us suppose that for the current velocity
v
ξ
(t)=v
ξ
(t, ξ(t)) the vector field v
ξ
(t, x) is also a gradient v
ξ
= σ
2
grad S for
some real function S(t, x). Note that S(t, x) is defined to within the functions
depending only on t, i.e., whose gradient is zero. Consider the complex-valued
function Ψ on M of the form Ψ(t, x)=exp(R +iS).
Theorem 15.4 Ψ satisfies the Schr¨odinger equation
∂Ψ
∂t
=i
σ
2
2
∇
2
Ψ − i
1
VΨ. (15.7)