Probability of coprime sets

The latest blog post from Gödel’s Lost Letter and P=NP looks at the problem of finding relatively prime pairs of large numbers. In particular, they want a deterministic algorithm. They mention in passing that the probability of a set of k large integers being relatively prime (coprime) is 1/ζ(k) where ζ is the Riemann zeta function. This blog post will look closer at that statement.

How large is large?

What does it mean that the numbers are large? That they are large enough that the asymptotic result given by the zeta function is accurate enough. We’ll explore this with simulation code shortly.

The exact statement is that in the limit as N goes to infinity, the probability of k integers chosen uniformly from 1 to N being coprime converges to 1/ζ(k). I won’t go into the proof here, but in a nutshell, it falls out of Euler’s product formula for the zeta function.

What does it mean for a set of numbers to be coprime?

The probability above seemed wrong to me at first. The function ζ(k) decreases as k increases, and so its reciprocal increases. That means it’s more likely that a set of numbers is coprime as the size of the set increases. But the larger the set of numbers, the more likely it is that two will have a common factor, so shouldn’t the probability that they’re coprime go down with k, not up?

The resolution to the apparent contradiction is that I had the wrong idea of coprime in mind. Two integers are coprime if they have no prime factors in common. How do you generalize that to more than two integers? You could define a set of numbers to be coprime if every pair of numbers in the set is coprime. That’s the definition I had in mind. But that’s not the standard definition. The right definition here is that the greatest common divisor of the set is 1. For example, (6, 14, 21) would be coprime because no single prime divides all three numbers, even though no pair of numbers from the set is coprime.

Python simulation

Let’s write some Python code to try this out. We’ll randomly generate some sets of large numbers and see how often they’re coprime.

How do you generate large random integers in Python? You can use the function getrandbits to generate numbers as large as you like. In the code below we’ll generate 128-bit integers.

How do you compute the greatest common divisor in Python? There’s a library function gcd, but it only takes two integers. We’ll use the reduce function to fold gcd over a list of integers.

How do you compute the zeta function in Python? SciPy doesn’t have an implementation of ζ(x) per se, but it does have an implementation of ζ(x)-1. Why not just implement ζ itself? Because for large x, ζ(x) is close to 1, so more precision can be saved by computing ζ − 1.

Putting these pieces together, here’s code to randomly generate triples of 128-bit integers, see how often they’re coprime, and compare the result to 1/ζ(3).

    from random import getrandbits
    from fractions import gcd
    from functools import reduce
    from scipy.special import zetac
    
    def riemann_zeta(x):
        return zetac(x) + 1
    
    k = 3
    size = 128
    N = 10000
    
    coprime_count = 0
    for _ in range(N):
        x = [getrandbits(size) for _ in range(k)]
        if reduce(gcd, x) == 1:
            coprime_count += 1
    print(coprime_count/N)
    print(1/riemann_zeta(k))

When I ran this I got

    0.8363
    0.831907372581

Simulation agrees with theory to two decimal places, which is just what we should expect from 10,000 repetitions. (We’d expect error on the order of 1/√N.)

Here’s what I got when I changed k to 4:

    0.9234
    0.923938402922

And here’s what I got for k set to 5:

    0.9632
    0.964387340429

Related posts

Curvature and automatic differentiation

Curvature is tedious to calculate by hand because it involves calculating first and second order derivatives. Of course other applications require derivatives too, but curvature is the example we’ll look at in this post.

Computing derivatives

It would be nice to write programs that only explicitly implement the original function and let software take care of finding the derivatives.

Numerical differentiation

Finite difference approximations for derivatives are nothing new. For example, Euler (1707–1783) used finite differences to numerically solve differential equations. But numerical differentiation can be inaccurate or unstable, especially for higher order derivatives.

Symbolic differentiation

Symbolic differentiation is another approach, having the computer manipulate expressions much as a person would do by hand. It works well for many problems, though it scales poorly for large problems. It also requires functions to be presented in traditional mathematical form, not in the form of source code.

Automatic differentiation

Automatic differentiation is a third way. Like numerical differentiation, it works with floating point numbers, not symbolic expressions. But unlike numerical differentiation, the result does not have approximation error.

As someone put it, automatic differentiation applies the chain rule to floating point numbers rather than to symbolic expressions.

Python implementation

I’ll use the Python library autograd to compute curvature and illustrate automatic differentiation. autograd is not the most powerful automatic differentiation library for Python, but it is the simplest I’ve seen.

We will compute the curvature of a logistic curve.

y = \frac{1}{1 + e^{-x}}

The curvature of the graph of a function is given by

\kappa(x) = \frac{|y''|}{(1 + y'^2)^{3/2}}

Here’s Python code using autograd to compute the curvature.

    import autograd.numpy as np
    from autograd import grad

    def f(x):
        return 1/(1 + np.exp(-x))

    f1 = grad(f)  # 1st derivative of f
    f2 = grad(f1) # 2nd derivative of f

    def curvature(x):
        return abs(f2(x))*(1 + f1(x)**2)**-1.5

Curvature plots

The graph is relatively flat in the middle and at the far ends. In between, the graph bends creating two regions of higher curvature.

    import matplotlib.pyplot as plt

    x = np.linspace(-5, 5, 300)
    plt.plot(x, f(x))
    plt.xlabel("$x$")
    plt.ylabel("$y$")
    plt.title("Logistic curve")
    plt.savefig("logistic_curve.svg")

Now let’s look at the curvature.

    y = [curvature(t) for t in x]
    plt.plot(x, y)
    plt.xlabel("$x$")
    plt.ylabel(r"$\kappa(x)$")
    plt.title("Curvature")
    plt.savefig("plot_logistic_curvature.svg")

curvature for logistic curve

As we should expect, the curvature is small at the ends and in the middle, with local maxima in between.

We can also look at the signed curvature, the same expression as curvature but without the absolute value.

k(x) = \frac{y''}{(1 + y'^2)^{3/2}}

We plot this with the following code.

    def signed_curvature(x):
        return f2(x)*(1 + f1(x)**2)**-1.5

    y = [signed_curvature(t) for t in x]
    plt.plot(x, y)
    plt.xlabel("$x$")
    plt.ylabel(r"$k(x)$")
    plt.title("Signed curvature")
    plt.savefig("graph_signed_curvature.svg")

The result looks more like a sine wave.

The positive values mean the curve is bending counterclockwise, and the negative values mean the curve is bending clockwise.

Related post: Squircles and curvature

Summing random powers up to a threshold

Pick random numbers uniformly between 0 and 1, adding them as you go, and stop when you get a result bigger than 1. How many numbers would you expect to add together on average?

You need at least two samples, and often two are enough, but you might get any number, and those larger numbers will pull the expected value up.

Here’s a simulation program in Python.

    from random import random
    from collections import Counter

    N = 1000000
    c = Counter()
    for _ in range(N):
        x = 0
        steps = 0
        while x < 1:
            x += random()
            steps += 1
        c[steps] += 1

    print( sum( k*c[k] for k in c.keys() )/N )

When I ran it I got 2.718921. There’s theoretical result first proved by W. Weissblum that the expected value is e = 2.71828… Our error was on the order of 1/√N, which is what we’d expect from the central limit theorem.

Now we can explore further in a couple directions. We could take a look at the distribution of the number steps, not just its expected value. Printing c shows us the raw data.

    Counter({
        2: 499786, 
        3: 333175, 
        4: 125300, 
        5:  33466, 
        6:   6856, 
        7:   1213, 
        8:    172, 
        9:     29, 
        10:     3
    })

And here’s a plot.

We could also generalize the problem by taking powers of the random numbers. Here’s what we get when we use exponents 1 through 20.

expected steps as exponents increase

There’s a theoretical result that the expected number of steps is asymptotically equal to cn where

c = \exp(\exp(-\gamma)) - \int_{-\infty}^\infty \frac{\exp(-\exp(u)) }{ (u+ \gamma)^2 + \pi^2}\, du

I computed c = 1.2494. The plot above shows that the dependence on the exponent n does look linear. The simulation results appear to be higher than the asymptotic prediction by a constant, but that’s consistent with the asymptotic prediction since relative to n, a constant goes away as n increases.

Reference for theoretical results: D. J. Newman and M. S. Klamkin. Expectations for Sums of Powers. The American Mathematical Monthly, Vol. 66, No. 1 (Jan., 1959), pp. 50-51

Average fraction round up

Pick a large number n. Divide n by each of the positive integers up to n and round the results up to the nearest integer. On average, how far do you round up?

Or in terms of probability, what is the expected distance between a fraction n/r, where n is large and fixed and r is chosen randomly between 1 and n, and the nearest larger integer?

In symbols, the question above is asking for the approximate value of

\frac{1}{n} \sum_{r = 1}^n \left( \left\lceil \frac{n}{r} \right\rceil - \frac{n}{r}\right )

for large n, i.e. in the limit as n goes to ∞. Here ⌈x⌉ denotes the ceiling of x, the smallest integer greater than or equal to x.

Let’s plot this as a function of n and see what it looks like. Here’s the Python code.

    import matplotlib.pyplot as plt
    from numpy import ceil, arange

    def f(n):
        return sum( ceil(n/r) - n/r for r in range(1, n) )/n

    x = arange(1, 100)
    y = [f(n) for n in x]
    plt.plot(x, y)
    plt.show()

And here’s the result.

It appears the graph may be converging to some value, and in fact it is. Charles de la Vallée Poussin proved in 1898 that the limiting value is the Euler–Mascheroni constant γ = 0.5772…. This constant is the limiting difference between the nth harmonic number and log n, i.e.

\gamma = \lim_{n\to\infty} \left(\sum_{r = 1}^n \frac{1}{r} - \log n \right)

We can add a horizontal line to our plot to see how well the graph seems to match γ. To do this we need to import the constant euler_gamma from numpy and add the

    plt.axhline(y=euler_gamma, linestyle=":")

after the plot command. When we do, this is what we see.

It looks like the plot is converging to a value slightly less than γ. Apparently the convergence is very slow. When we go out to 10,000 the plot is closer to being centered around γ but still maybe below γ more than above.

If we evaluate our function at n = 1,000,000, we get 0.577258… while γ = 0.577215….

At n = 10,000,000 we get 0.577218…. So taking 100 times as many terms in our sum gives us one extra correct decimal place, as we’d expect of a random processes since convergence usually goes like 1/√n.

Equation for the Eiffel Tower

Robert Banks’s book Towing Icebergs, Falling Dominoes, and Other Adventures in Applied Mathematics describes the Eiffel Tower’s shape as approximately the logarithmic curve

y = -y_* \log\left(\frac{x}{x_0} \right )

where y* and x0 are chosen to match the tower’s dimensions.

Here’s a plot of the curve:

Eiffel tower curve plot

And here’s the code that produced the plot:

from numpy import log, exp, linspace, vectorize
import matplotlib.pyplot as plt

# Taken from "Towing Icebergs, Falling Dominoes,
# and Other Adventures in Applied Mathematics"
# by Robert B. Banks

# Constants given in Banks in feet. Convert to meters.
feet_to_meter = 0.0254*12
ystar  = 201*feet_to_meter
x0     = 207*feet_to_meter
height = 984*feet_to_meter

# Solve for where to cut off curve to match height of the tower.
# - ystar log xmin/x0 = height
xmin = x0 * exp(-height/ystar)

def f(x):
    if -xmin < x < xmin:
        return height
    else:
        return -ystar*log(abs(x/x0))
curve = vectorize(f)
    
x = linspace(-x0, x0, 400)

plt.plot(x, curve(x))
plt.xlim(-2*x0, 2*x0)
plt.xlabel("Meters")
plt.ylabel("Meters")
plt.title("Eiffel Tower")

plt.axes().set_aspect(1)
plt.savefig("eiffel_tower.svg")

Related post: When length equals area
The St. Louis arch is approximately a catenary, i.e. a hyperbolic cosine.

Why is Kullback-Leibler divergence not a distance?

The Kullback-Leibler divergence between two probability distributions is a measure of how different the two distributions are. It is sometimes called a distance, but it’s not a distance in the usual sense because it’s not symmetric. At first this asymmetry may seem like a bug, but it’s a feature. We’ll explain why it’s useful to measure the difference between two probability distributions in an asymmetric way.

The Kullback-Leibler divergence between two random variables X and Y is defined as

KL(X || Y) = -\int f_X(x) \log \frac{f_Y(x)}{f_X(x)} \, dx

This is pronounced/interpreted several ways:

  • The divergence from Y to X
  • The relative entropy of X with respect to Y
  • How well Y approximates X
  • The information gain going from the prior Y to the posterior X
  • The average surprise in seeing Y when you expected X

A theorem of Gibbs proves that K-L divergence is non-negative. It’s clearly zero if X and Y have the same distribution.

The K-L divergence of two random variables is an expected value, and so it matters which distribution you’re taking the expectation with respect to. That’s why it’s asymmetric.

As an example, consider the probability densities below, one exponential and one gamma with a shape parameter of 2.

exponential and gamma PDFs

The two densities differ mostly on the left end. The exponential distribution believes this region is likely while the gamma does not. This means that an expectation with respect to the exponential distribution will weigh things in this region more heavily. In an information-theoretic sense, an exponential is a better approximation to a gamma than the other way around.

Here’s some Python code to compute the divergences.

    from scipy.integrate import quad
    from scipy.stats import expon, gamma
    from scipy import inf

    def KL(X, Y):
        f = lambda x: -X.pdf(x)*(Y.logpdf(x) - X.logpdf(x))
        return quad(f, 0, inf)

    e = expon
    g = gamma(a = 2)

    print( KL(e, g) )
    print( KL(g, e) )

This returns

    (0.5772156649008394, 1.3799968612282498e-08)
    (0.4227843350984687, 2.7366807708872898e-09)

The first element of each pair is the integral and the second is the error estimate. So apparently both integrals have been computed accurately, and the first is clearly larger. This backs up our expectation that it’s more surprising to see a gamma when expecting an exponential than vice versa.

Although K-L divergence is asymmetric in general, it can be symmetric. For example, suppose X and Y are normal random variables with the same variance but different means. Then it would be equally surprising to see either one when expecting the other. You can verify this in the code above by changing the KL function to integrate over the whole real line

    def KL(X, Y):
        f = lambda x: -X.pdf(x)*(Y.logpdf(x) - X.logpdf(x))
        return quad(f, -inf, inf)

and trying an example.

n1 = norm(1, 1)
n2 = norm(2, 1)

print( KL(n1, n2) )
print( KL(n2, n1) )

This returns

(0.4999999999999981, 1.2012834963423225e-08)
(0.5000000000000001, 8.106890774205374e-09)

and so both integrals are equal to within the error in the numerical integration.

Negative correlation introduced by success

Suppose you measure people on two independent attributes, X and Y, and take those for whom X+Y is above some threshold. Then even though X and Y are uncorrelated in the full population, they will be negatively correlated in your sample.

This article gives the following example. Suppose beauty and acting ability were uncorrelated. Knowing how attractive someone is would give you no advantage in guessing their acting ability, and vice versa. Suppose further that successful actors have a combination of beauty and acting ability. Then among successful actors, the beautiful would tend to be poor actors, and the unattractive would tend to be good actors.

Here’s a little Python code to illustrate this. We take two independent attributes, distributed like IQs, i.e. normal with mean 100 and standard deviation 15. As the sum of the two attributes increases, the correlation between the two attributes becomes more negative.

from numpy import arange
from scipy.stats import norm, pearsonr
import matplotlib.pyplot as plt

# Correlation.
# The function pearsonr returns correlation and a p-value.
def corr(x, y):
    return pearsonr(x, y)[0]

x = norm.rvs(100, 15, 10000)
y = norm.rvs(100, 15, 10000)
z = x + y

span = arange(80, 260, 10)
c = [ corr( x[z > low], y[z > low] ) for low in span ]

plt.plot( span, c )
plt.xlabel( "minimum sum" )
plt.ylabel( "correlation coefficient" )
plt.show()

Random minimum spanning trees

I just ran across a post by John Baez pointing to an article [the link has gone away] by Alan Frieze on random minimum spanning trees.

Here’s the problem.

  1. Create a complete graph with n nodes, i.e. connect every node to every other node.
  2. Assign each edge a uniform random weight between 0 and 1.
  3. Find the minimum spanning tree.
  4. Add up the edges of the weights in the minimum spanning tree.

The surprise is that as n goes to infinity, the expected value of the process above converges to the Riemann zeta function at 3, i.e.

ζ(3) = 1/1³ + 1/2³ + 1/3³ + …

Incidentally, there are closed-form expressions for the Riemann zeta function at positive even integers. For example, ζ(2) = π² / 6. But no closed-form expressions have been found for odd integers.

Simulation

Here’s a little Python code to play with this.

    import networkx as nx
    from random import random

    N = 1000

    G = nx.Graph()
    for i in range(N):
        for j in range(i+1, N):
            G.add_edge(i, j, weight=random())

    T = nx.minimum_spanning_tree(G)
    edges = T.edges(data=True)

    print( sum( e[2]["weight"] for e in edges ) )

When I ran this, I got 1.2307, close to ζ(3) = 1.20205….

I ran this again, putting the code above inside a loop, averaging the results of 100 simulations, and got 1.19701. That is, the distance between my simulation result and ζ(3) went from 0.03 to 0.003.

There are two reasons I wouldn’t get exactly ζ(3). First, I’m only running a finite number of simulations (100) and so I’m not computing the expected value exactly, but only approximating it. (Probably. As in PAC: probably approximately correct.) Second, I’m using a finite graph, of size 1000, not taking a limit as graph size goes to infinity.

My limited results above suggest that the first reason accounts for most of the difference between simulation and theory. Running 100 replications cut the error down by a factor of 10. This is exactly what you’d expect from the central limit theorem. This suggests that for graphs as small as 1000 nodes, the expected value is close to the asymptotic value.

You could experiment with this, increasing the graph size and increasing the number of replications. But be patient. It takes a while for each replication to run.

Generalization

The paper by Frieze considers more than the uniform distribution. You can use any non-negative distribution with finite variance and whose cumulative distribution function F is differentiable at zero. The more general result replaces ζ(3) with ζ(3) / F ‘(0). We could, for example, replace the uniform distribution on weights with an exponential distribution. In this case the distribution function is 1 − exp(−x), at its derivative at the origin is 1, so our simulation should still produce approximately ζ(3). And indeed it does. When I took the average of 100 runs with exponential weights I got a value of 1.2065.

There’s a little subtlety around using the derivative of the distribution at 0 rather than the density at 0. The derivative of the distribution (CDF) is the density (PDF), so why not just say density? One reason would be to allow the most general probability distributions, but a more immediate reason is that we’re up against a discontinuity at the origin. We’re looking at non-negative distributions, so the density has to be zero to the left of the origin.

When we say the derivative of the distribution at 0, we really mean the derivative at zero of a smooth extension of the distribution. For example, the exponential distribution has density 0 for negative x and density exp(−x) for non-negative x. Strictly speaking, the CDF of this distribution is 1 − exp(−x) for non-negative x and 0 for negative x. The left and right derivatives are different, so the derivative doesn’t exist. By saying the distribution function is simply exp(−x), we’ve used a smooth extension from the non-negative reals to all reals.

Nearly all the area in a high-dimensional sphere is near the equator

Nearly all the area of a high-dimensional sphere is near the equator.  And by symmetry, it doesn’t matter which equator you take. Draw any great circle and nearly all of the area will be near that circle.  This is the canonical example of “concentration of measure.”

What exactly do we mean by “nearly all the area” and “near the equator”? You get to decide. Pick your standard of “nearly all the area,” say 99%, and your definition of “near the equator,” say within 5 degrees. Then it’s always possible to take the dimension high enough that your standards are met. The more demanding your standard, the higher the dimension will need to be, but it’s always possible to pick the dimension high enough.

This result is hard to imagine. Maybe a simulation will help make it more believable.

In the simulation below, we take as our “north pole” the point (1, 0, 0, 0, …, 0). We could pick any unit vector, but this choice is convenient. Our equator is the set of points orthogonal to the pole, i.e. that have first coordinate equal to zero. We draw points randomly from the sphere, compute their latitude (i.e. angle from the equator), and make a histogram of the results.

The area of our planet isn’t particularly concentrated near the equator.

But as we increase the dimension, we see more and more of the simulation points are near the equator.

Here’s the code that produced the graphs.

from scipy.stats import norm
from math import sqrt, pi, acos, degrees
import matplotlib.pyplot as plt

def pt_on_sphere(n):
    # Return random point on unit sphere in R^n.
    # Generate n standard normals and normalize length.
    x = norm.rvs(0, 1, n)
    length = sqrt(sum(x**2))
    return x/length

def latitude(x):
    # Latitude relative to plane with first coordinate zero.
    angle_to_pole = acos(x[0]) # in radians
    latitude_from_equator = 0.5*pi - angle_to_pole
    return degrees( latitude_from_equator )

N = 1000 # number of samples

for n in [3, 30, 300, 3000]: # dimension of R^n
    
    latitudes = [latitude(pt_on_sphere(n)) for _ in range(N)]
    plt.hist(latitudes, bins=int(sqrt(N)))
    plt.xlabel("Latitude in degrees from equator")
    plt.title("Sphere in dimension {}".format(n))
    plt.xlim((-90, 90))
    plt.show()

Not only is most of the area near the equator, the amount of area outside a band around the equator decreases very rapidly as you move away from the band. You can see that from the histograms above. They look like a normal (Gaussian) distribution, and in fact we can make that more precise.

If A is a band around the equator containing at least half the area, then the proportion of the area a distance r or greater from A is bound by exp( −(n − 1)r² ). And in fact, this holds for any set A containing at least half the area; it doesn’t have to be a band around the equator, just any set of large measure.

Related post: Willie Sutton and the multivariate normal distribution

Simple random number generator does surprisingly well

I was running the NIST statistical test suite recently. I wanted an example of a random number generator where the tests failed, and so I used a simple generator, a linear congruence generator. But to my surprise, the generator passed nearly all the tests, even though some more sophisticated generators failed some of the same tests. This says more about the NIST test suite than it says about the LCG being tested.

This post will implement a couple of the simplest tests in Python and show that the generator does well.

The linear congruential generator used here starts with an arbitrary seed, then at each step produces a new number by multiplying the previous number by a constant and taking the remainder by 231 – 1. The multiplier constant was chosen to be one of the multipliers recommended in [1].

We’ll need a couple math functions:

from math import sqrt, log

and we need to define the constants for our generator.

# Linear congruence generator (LCG) constants
z = 20170705   # seed
a = 742938285  # multiplier
e = 31         # will need this later
m = 2**e -1    # modulus

Next we form a long string of 0’s and 1’s using our generator

# Number of random numbers to generate
N = 100000     

# Format to print bits, padding with 0's on the left if needed
formatstr = "0" + str(e) + "b"

bit_string = ""
for _ in range(N):
    z = a*z % m # LCG
    bit_string += format(z, formatstr)

Next we run a couple tests. First, we count the number of 1’s in our string of bits. We expect about half the bits to be 1’s. We can quantify “about” as within two standard deviations.

def count_ones(string):
    ones = 0
    for i in range(len(string)):
        if string[i] == '1':
            ones += 1
    return ones

ones = count_ones(bit_string)
expected = e*N/2
sd = sqrt(0.25*N)
print( "Number of 1's: {}".format(ones) )
print( "Expected: {} to {}".format(expected - 2*sd, expected + 2*sd) )

The results are nothing unusual:

Number of 1's: 1550199
Expected: 1549683.8 to 1550316.2

Next we look at the length of the longest runs on 1’s. I’ve written before about the probability of long runs and the code below uses a couple results from that post.

def runs(string):
    max_run = 0
    current_run = 0
    for i in range(len(string)):
        if string[i] == '1':
            current_run += 1
        else:
            current_run = 0
        max_run = max(max_run, current_run)
    return max_run

runlength = runs(bit_string)
expected = -log(0.5*e*N)/log(0.5)
sd = 1/log(2)
print( "Run length: {}".format(runlength) )
print( "Expected: {} to {}".format(expected - 2*sd, expected + 2*sd) )

Again the results are nothing unusual:

Run length: 19
Expected: 17.7 to 23.4

Simple random number generators are adequate for many uses. Some applications, such as high dimensional integration and cryptography, require more sophisticated generators, but sometimes its convenient and sufficient to use something simple. For example, code using the LCG generator above would be easier to debug than code using the Mersenne Twister. The entire state of the LCG is a single number, whereas the Mersenne Twister maintains an internal state of 312 numbers.

One obvious limitation of the LCG used here is that it couldn’t possibly produce more than  231 – 1 values before repeating itself. Since the state only depends on the last value, every time it comes to a given output, the next output will be whatever the next output was the previous time. In fact, [1] shows that it does produce 231 – 1 values before cycling. If the multiplier were not chosen carefully it could have a shorter period.

So our LCG has a period of about two billion values. That’s a lot if you’re writing a little game, for example. But it’s not enough for many scientific applications.

* * *

[1] George S. Fishman and Louis R. Moore III, An exhaustive analysis of multiplicative congruential random number generators with modulus 231 – 1, SIAM Journal of Scientific and Statistical Computing, Vol. 7, no. 1, January 1986.