The Landsberg–Schaar relation is a reciprocity formula for quadratic exponential sums. It transforms a finite sum with quadratic phase into another finite quadratic sum in which the roles of
and
are essentially reversed. The transformation includes the striking phase factor
. This factor is not incidental: it is the same analytic phase that appears in the evaluation of quadratic Gauss sums and, ultimately, in quadratic reciprocity.
The relation is as follows.
Theorem. For all positive integers and
,
No coprimality assumption is required. The formula is already a reciprocity law: a quadratic sum of length is transformed into a quadratic sum of length
.
The proof has one central idea. Rather than evaluating either finite sum directly, we embed the left-hand sum into a Gaussian-damped infinite theta series. This theta series can then be analyzed in two ways. First, its periodic coefficients recover the finite sum on the left-hand side. Second, Poisson summation transforms it into a dual theta series whose periodic coefficients recover the finite sum on the right-hand side. The phase arises from the Fourier transform of a complex Gaussian.
Gaussian Averaging
We begin with a standard consequence of Poisson summation. For and
,
As , every term with
is exponentially small. Hence
In other words, a very broad Gaussian samples many integers, so its discrete sum is asymptotic to its integral. We will apply this observation after grouping integers into residue classes.
Theta Series
For , define the Theta series
The Gaussian factor makes the sum absolutely convergent. As , the damping weakens, and the leading term of
reveals a finite quadratic sum.
The phase is periodic modulo
, since replacing
by
changes
by an integer. Writing
, with
, gives
For each fixed , the inner sum has the form above, with
. Therefore,
uniformly in . Multiplying by
, we obtain
This is the first interpretation of the theta sum: the finite quadratic sum on the left-hand side of the Landsberg–Schaar relation is the coefficient of the dominant growth.
Poisson Summation
We now analyze the same theta sum by Fourier methods. The definition of can be rewritten as
For a complex number with
, the Fourier transform of a Gaussian is
The square root is chosen by continuous extension from positive real values of . This branch choice is responsible for the phase
.
Applying Poisson summation with we obtain
This is the decisive step. Poisson summation has replaced the original quadratic phase by a dual quadratic phase.
Since the
-th term in the transformed sum is
As ,
A comparison on the effective range , together with Gaussian tail estimates, yields
The oscillatory factor is periodic modulo
. Indeed, replacing
by
changes
by an integer. Thus we may group the sum by residue classes modulo
. Writing
, we have
Applying the Gaussian averaging principle again gives
Finally,
The phase appears because
has argument
, so its inverse square root has argument
.
Combining the transformed theta-sum formula with these asymptotics, we obtain
The two preceding limits compute the same quantity. Equating them gives
This is the Landsberg–Schaar relation.
The proof is important for more than the final identity. It begins with a finite quadratic phase modulo , but it does not evaluate that phase by finite algebra alone. Instead, it embeds the finite sum into a theta function on the real line. Poisson summation then exchanges the integer lattice with its Fourier-dual lattice.
Under this transformation, the quadratic coefficient is replaced by the dual coefficient
while the Fourier transform contributes the phase
. Thus the Landsberg–Schaar relation forms a bridge between finite arithmetic and real Fourier analysis. The finite sums arise because the quadratic phases are periodic, while the phase
comes from the square root in the Fourier transform of a complex Gaussian.
Quadratic Reciprocity: The Landsberg–Schaar relation is not itself the quadratic reciprocity law, but it has the same underlying structure. Suppose that and
are distinct odd primes, and define the quadratic Gauss sum
For , one has the standard change-of-coefficient identity
where is the Legendre symbol.
The left-hand side of the Landsberg–Schaar relation therefore becomes
On the right, splitting the sum over into even and odd residue classes gives
Using the change-of-coefficient identity once more,
Thus the Landsberg–Schaar relation compares the two Legendre symbols and
with the remaining sign supplied by the Gaussian phase and the congruence classes of
and
modulo
. After inserting the classical evaluation of quadratic Gauss sums, this comparison becomes
This is quadratic reciprocity. The sign in quadratic reciprocity is therefore not an arbitrary parity correction. It is the finite-arithmetic shadow of the phase that appears in the Fourier transform of a complex Gaussian. In this sense, the Landsberg–Schaar relation is a Fourier-analytic reciprocity law from which the classical quadratic reciprocity law naturally emerges.