and Statistics, University of New Mexico, Albuquerque, New Mexico Submitted by G. M. Wing
1.
INTRODUCTION
In this paper we considera classof integral equationsof the generalform
$(4 = g(@ + rT Y@‘)K(I z - z’ I) W’) dx’,
(l.la)
JY
where K has an integral representationof the type K(u)
= 1,” k(s’) e+fs’)u ds’.
(l.lb)
With the problem (l.l), we associatethe “pseudo-transport” problem
(sgn s) g N(z, s) + 4) N(z, 4 = k(s)~(4 jy, N(z, s’) ds’, Y
ISI
U-2)
with certain boundary conditions which will be discussedlater. (Equation (1.2) is a generalization of the equation for particle transport in a slab geometry [lo].) Equivalence between the problems(1.1) and (1.2) is established. Thus any resultsobtained concerning the problem (1.2) produce corresponding resultsconcerningproblem (1.1). Functional equationsare derived relating the solutions (one for s > 0 and one for s < 0) of (1.2). It might be noted here that the functions involved in these functional equations are the solutions to initial value problems. This opensup the possibility of converting the problem of solving (1.1) to that of solving initial value problems. These * Department of Mathematics and Statistics, Albuquerque, New Mexico. Research supported Grant GP-5967.
48
The University by the National
of New Mexico, Science Foundation
FRFDHOLM
INTEGRAL
49
EQUATIONS
functional relationships are then applied to the eigenvalue problem associated with (1 .I).1 A particular example is considered and some numerical results obtained. Similar results on the calculation of eigenvalues, although using methods quite different from this, have been obtained by H. H. Kagiwada and R. E. Kalaba [3], [4]. It should be remarked that the representation (1.1 b) actually encompasses a fairly large class of kernels. For example, if a(s) = s, K is a Laplace transform. Kernels expressible in terms of such Laplace integrals arise often in transport theory. Mellin transforms can also be treated. For the sake of mathematical simplicity and to help develop some physical intuition, let us consider in a purely formal manner a simple transport model, which shall be referred to as the “one-dimensional model,” the “one-dimensional rod,” or simply the “rod.” What we shall do in the following sections is a considerable generalization and rigorization of these basic ideas. Consider now an interval extending from z = - N to z = + X. The interval will be thought of as a material rod capable of transporting particles which may move, however, only to the right or left on the interval. Moving particles may collide with the fixed nuclei of the medium, the probabilities of such collisions and the resulting expected number of particles moving in each direction being specified. Interactions between moving particles will not be allowed. All particles will be of the same kind, with the same energy and other physical specifications, distinguishable only by their direction. We shall consider only the time independent situation. The appropriate equations governing this process are [lo] (1.3a) - dv -&+ (TV(Z) = X,(z),
- x < z < x,
(1.3b)
where p(z) = u(z) + v(z). With (1.3) we considerthe following boundary conditions: u(-x)=n~,
(1.4a)
v(x) = nR ,
(1.4b)
1The eigenvalueproblemis given by Q4.4 = P j= r(z’)K(I Y where we Throughout 4o9/3olr-4
note this
2 -
2’ l)I,b(z’)
dz’
that the parameterp is the reciprocalof that usually considered. paper,
we shall
always
assume
the eigenvalue
to be in this position.
ALLEN
50 where tlL and n, are state that n, particles per unit time, and n, unit time. The system lation given by
nonnegative and not both zero. Physically, eqs. (1.4) are injected into the rod at the left end, z = - X, injected into the rod at the right end, z = + X, per (1.3) (1.4) has an equivalent integral equation formu-
The following relations are suggestedby purely physical considerations: $4 = n,t(-
x, 4 + u(z) P(- x, z),
w(z) = QT(Z, x) + u(z) r(z, x).
(1.6a) (1.6b)
Formally p(- X, z) and t(z, X) represent right and left reflection operators while t(- X, z) and ~(2, X) right and left transmission operators [5]. By differentiating equations (1.6) with respect to z, and using equations (1.3), we may derive the following ordinary differential equations satisfied by the function p, t, I and 7: pz(- x, 4 = h + 2(h - a) P( - x, z) + AP”( - .T z), tz(
- x, 2) = (A - u) t( - x, z) + $(-
x, z) t(- x, x),
(1.7a) (1.7b)
r&z, x) = - x - 2(h - I?)r(z, x) - W(z, x),
(1.7c)
T&z, x) = - (A - u) T(2, x) - A+, x) 7(x, x),
(1.7d)
for - x < .z < x, with p(- x, - x) = 0 = r(x, x), t(-
X, - X) = 1 =
7(X,
X).
(1.8a) (1.8b)
These initial values are physically reasonable,since a rod of zero length should reflect nothing and transmit entirely a unit input. One may obtain existence and uniquenessTheorems for the solutions of the Eqs. (1.7) together with the initial conditions (1.8). If we then accept equations(1.7) and (1.8) asthe defining equationsfor the functions p, t, r and 7, respectively, and if the functions u(z) and V(Z) are defined by (1.6), then the basic transport equations (1.3) with (1.4) are satisfied. As an application of the functional Eqs. (1.6), we shall consider the eigenvalue problem associatedwith (1.5). Let n = nL = nE .
Then our rod problem becomessymmetric in the sensethat 24(z)= w(- 22).
51
FREDHOLM INTEGRAL EQUATIONS
After somemanipulation, using equations(1.6), we have nt( - x, 0) 40) = 1 -p(-x,o)’
(1.9)
Now u(0) will fail to exist if x is determined so that p(- X, 0) = 1. For this samevalue of X, p(O) will fail to exist. (It may be shown that for y > 1, such a value of x does exist and is unique.) The Fredholm alternative then impliesh is an eigenvalueof the integral operator associatedwith (1.5).
2. EQUIVALENT
FORMULATIONS FOR THE INTEGRAL FUNCTIONAL RELATIONSHIPS \
EQUATION
AND BASIC
We begin by considering the “transport-like” problem sgns & N(z, s) + a(s)N(z, s) = K(s)y(z) Srn N(z, s’) ds’, -03