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Article

New Refinements for the Error Function with Applications in Diffusion Theory

Department of Mathematics and Computer Sciences, “Dunărea de Jos” University of Galaţi, 111 Domnească Street, 800201 Galaţi, Romania
Symmetry 2020, 12(12), 2017; https://doi.org/10.3390/sym12122017
Submission received: 19 November 2020 / Revised: 29 November 2020 / Accepted: 3 December 2020 / Published: 6 December 2020

Abstract

:
In this paper we provide approximations for the error function using the Padé approximation method and the Fourier series method. These approximations have simple forms and acceptable bounds for the absolute error. Then we use them in diffusion theory.

1. Introduction and Motivation

The error function e r f is a special function. It is widely used in many areas of research, such as: statistical computations, mathematical models in biology, mathematical physics, and diffusion theory.
In this work we intend to draw attention to the Padé approximant method and to the Fourier series method by some inequalities and approximations which involve the even function exp ( x 2 ) and the error function.
The error function is related to the function expression for a Gaussian distribution and has the form
e r f x = 2 π 0 x e u 2 d u .
The complementary error function is
e r f c x = 1 e r f x ,
or
e r f c x = 2 π x e u 2 d u .
The integral in the error function cannot be evaluated analytically, so values for e r f and e r f c are computed via approximations and often available in tables.
There are two main aspects in the study of the error function. The first aspect refers to the establishment of some bounds for the error function. The second aspect is to approximate the error function with different elementary functions such that the absolute error function is as small as possible.
The bounds for the error function have attracted the attention of many researches, since there were studies in different forms in the recent past (see [1,2,3,4,5,6,7,8,9,10,11,12,13,14,15,16,17,18,19,20]).
Pólya [8] proved that the inequality
e r f x < 1 exp 4 x 2 π
holds for all x > 0 .
Neumann [15] proved that the double inequality
2 x π · e x 2 3 e r f x 2 x π · e x 2 + 2 3
holds for all x > 0 .
Recently, Yang and Chu [13] improved the above inequalities by the following inequalities
2 x π · e x 2 3 < 2 x π · e x 2 3 + 5 e x 2 5 6 < e r f x < 2 x π · 5 e 3 x 2 5 + 4 9 < < 2 x π · 16 e x 2 2 + 5 e x 2 5 21 < 2 x π · 20 e 2 x 2 5 + e x 2 21 ,
for all x > 0 .
Komatsu’s inequalities [16] assert that
2 e x 2 2 x + x 2 + 4 < x e t 2 2 d t < 2 e x 2 2 x + x 2 + 2
holds for all x > 0 .
Hastings [5] suggested some expressions, of which the simplest are
e r f x 1 a 1 t + a 2 t 2 + a 3 t 3 e x 2 , 0 x
where
t = 1 1 + a 4 x , a 1 = 0.3480242 , a 2 = 0.0958798 , a 3 = 0.7478556 , a 4 = 0.47047
and
e r f x 1 1 + a 1 x + a 2 x 2 + a 3 x 3 + a 4 x 4 4 ,
where
a 1 = 0.278393 , a 2 = 0.230389 , a 3 = 0.000972 , a 4 = 0.078108 .
The absolute error ε x is shown to be less 2 × 10 5 and 5 × 10 4 , respectively.
The approximation
e r f x 1 2 1 + a 1 + a 2 x a 3 a 4
was obtained by Burr [2], where a 1 = 0.644693 , a 2 = 0.22908 , a 3 = 4.874 , a 4 = 6.158 .
Norton [12] proposed the following approximation
e r f x 1 exp 2 x 2 + 1.2 x 2 0.8 2 ; 0 x 2.7 1 + 2 π exp x 2 ; x > 2.7
with absolute error ε x < 8.07 × 10 3 , for all x 0 .
Furthermore, in sigmoid functions theory, the function π 2 e r f x is compared with the following algebraic functions
η 1 x = x 1 + x and η 2 x = x 1 + x 2 .
The aim of our work is to refine these inequalities. First, we will use the Padé approximant method in order to obtain a new approximation of the error function. The proposed approximation has a simple rational form and it is easy to programme.
It is known that a Padé approximant is the ‘best’ approximation of a function by a rational function of given order. The Padé approximant [ L , M ] corresponds to the Taylor series. When it exists, the [ L , M ] Padé approximant to any power series A x = j = 0 a j x j is unique
The coefficients are found by setting
A x = p 0 + p 1 x + + p L x L 1 + q 1 x + + q M x M .
These give the set of equations
p 0 = a 0 p 1 = a 0 q 1 + a 1 p 2 = a 0 q 2 + a 1 q 1 + a 2 p L = a 0 q L + + a L 1 q 1 + a L 0 = a L M + 1 q M + + a L q 1 + a L + 1 0 = a L q M + + a L + M 1 q 1 + a L + M .
For example, the first orders of Padé approximant for π 2 e r f x are
P a d e [ 3 , 4 ] = A x = 110 x 3 + 210 x 39 x 4 + 180 x 2 + 210 , P a d e [ 1 , 8 ] = B x = 113 , 400 x 29 x 8 660 x 6 + 1260 x 4 + 378 , 00 x 2 + 113 , 400 , P a d e [ 5 , 6 ] = C x = 302 , 379 x 5 + 1 , 027 , 320 x 3 + 10 , 242 , 540 x 52 , 595 x 6 + 758 , 625 x 4 + 4 , 441 , 500 x 2 + 10 , 242 , 540 .
We notice that the expressions A x , B x , C x are positive for all x > 0 .
After several attempts we obtain that the best approximation for the function π 2 e r f x is provided by P a d e [ 5 , 6 ] approximation.
The second idea is that the function exp x 2 is even, so it can be expanded in Fourier trigonometric series, e.g.,
exp x 2 = 1 a b + a cos x + b cos 2 x + ,
exp x 2 = 1 a b c + a cos x + b cos 2 x + c cos 3 x + .
In the following we will present our algorithm for the first expansion. We define the function F 1 x by
F 1 x = 1 a b + a cos x + b cos 2 x .
The power series expansion of exp x 2 F 1 x near 0 is
1 2 x 2 a + 4 b 2 + 1 24 x 4 a 16 b + 12 + O x 6 .
In order to increase the speed of the function F 1 ( x ) approximating exp x 2 , we vanish the first coefficients as follows:
a + 4 b 2 = 0 a 16 b + 12 = 0
and we obtain a = 4 3 and b = 5 6 .
Therefore we have
exp x 2 3 2 + 4 3 cos x 5 6 cos 2 x = 17 180 x 6 + 367 10 , 080 x 8 2449 302 , 400 x 10 .
Using the same algorithm, we find
exp x 2 + 7 18 3 2 cos x + 3 10 cos 2 x 17 90 cos 3 x = 43 3360 x 8 101 18 , 900 x 10 + 47 , 177 39 , 916 , 800 x 12 + O x 14 .

2. Main Results

In the first part of this section we will prove our main results obtained using Padé approximant method for π 2 e r f x .
Theorem 1.
The following inequalities hold:
(i) e r f x 2 π · A x for all x 0 ;
(ii) e r f x 2 π · B x for all x 0 , 4.418 .
Proof. 
(i) The function f x = π 2 e r f x A x has the derivative
f x = e x 2 + 110 x 3 + 210 x 156 x 3 + 360 x 39 x 4 + 180 x 2 + 210 2 330 x 2 + 210 39 x 4 + 180 x 2 + 210 .
f x is never zero when x > 0 , therefore h x has no critical points for x 0 .
f x has a global minimum at x = 0 . Since f 0 = 0 it follows that e r f x 2 π · A x for all x 0 .
(ii) We consider the function g x = π 2 e r f x B x .
In order to find all positive critical points of g, first we compute g x .
g x = e x 2 + 113 , 400 x 232 x 7 3960 x 5 + 5040 x 3 + 75 , 600 x 29 x 8 660 x 6 + 1260 x 4 + 37 , 800 x 2 + 113 , 400 2 113 , 400 29 x 8 660 x 6 + 1260 x 4 + 37 , 800 x 2 + 113 , 400 .
Solving the equation g x = 0 yields x 3.77096 .
Now we evaluate g x at the critical points and the endpoints of the domain, taking limit at the :
g 0 = 0 , g 3.77096 = 1.32154 , lim x g x = π 2 .
The function g has only one root x 4.418 .
Therefore, g x 0 for all x 0 , 4.418 or, equivalently, e r f x 2 π · B x for all x 0 , 4.418 .
Since e r f 4.418 = 0.999999999584246 , the error function can be considered e r f x = 1 for x 4.418 , , hence our rational approximation offer good bounds near the origin for the error function.
The proof of Theorem 1 is complete.  ☐
In the following we will prove that our rational inequalities are more precise than Neuman’s type inequalities.
Proposition 1.
(i) For every x 0 , the inequality
2 π A x 2 x π e x 2 + 5 e x 2 5 6
holds.
(ii) For every x 0 , the inequality
2 π B x 2 x π e x 2 + 2 3
holds.
(iii) For every x 0 , 3.10394 4.04171 , the inequality
2 π B x 2 x π 5 e 3 x 2 5 + 4 9
holds.
Proof. 
(i) The inequality from (i) takes the equivalent form:
220 x 2 e x 2 + 420 e x 2 1 5 e 4 x 2 5 > 0 ,
for all x > 0 .
It is sufficient to prove that
420 e x 2 1 5 e 4 x 2 5 > 0
for all x > 0 , or, equivalently,
e x 2 1 + e 4 x 2 5 419 e x 2 5 5 > 0 ,
for all x > 0 .
The above inequality is obviously true.
(ii) We consider the function
h x = 113 , 400 29 x 8 660 x 6 + 1260 x 4 + 37 , 800 x 2 + 113 , 400 1 3 e x 2 + 2 .
To find all positive critical points, first we compute h x :
h x = 2 3 e x 2 · x 113 , 400 232 x 7 3960 x 5 + 5040 x 3 + 75 , 600 x 29 x 8 660 x 6 + 1260 x 4 + 37 , 800 x 2 + 113 , 400 2 .
Solving the equation h x = 0 yields the positive roots: x = 0 , x 2.59797 , x 3.71138 .
Moreover, the function h x exists everywhere. Evaluate h x at the critical points and take the limit:
h 0 = 0 , h 2.59797 = 0.266605 , h 3.71138 = 0.0767078 and lim x h x = 2 3 .
Summarizing the results, we deduce that h x 0 for all x 0 .
(iii) We introduce the function
p x = 113 , 400 29 x 8 660 x 6 + 1260 x 4 + 37 , 800 x 2 + 113 , 400 5 e 3 x 2 9 + 4 9 .
In order to find all positive critical points, first we compute p x :
p x = 2 3 e 3 x 2 5 · x 113 , 400 232 x 7 3960 x 5 + 5040 x 3 + 75 , 600 x 29 x 8 660 x 6 + 1260 x 4 + 37 , 800 x 2 + 113 , 400 2 .
The equation p x = 0 has the positive roots: x = 0 , x 2.4639 , x 3.71165 .
Evaluate p x at the critical points and take the limit:
p 0 = 0 , p 2.4639 = 0.0554863 , p 3.71165 = 0.145372 and lim x p x = 4 9 .
The equation p x = 0 has the positive roots: x 3.10394 and x 4.04171 .
Summarizing the results, we obtain that p x 0 for x 0 , 3.10394 4.04171 , .
This completes the proof.  ☐
Therefore we improved the Neuman inequalities for all x 0 . We also refined the left-hand side of Yang-Chu’s inequality for all x 0 and the right-hand side of Yang-Chu’s inequality for x 0 , 3.10394 4.04171 , 4.418 .
Our upper bound for the error function e r f x also offers a better approximation near the origin than Pólya’s inequality, due to the following proposition.
Proposition 2.
The inequality
2 π B x 1 e 4 x 2 π
holds for all x 0 , 1.573 .
Proof. 
The above inequality can be rewritten as
π e 4 x 2 π 1 29 x 8 660 x 6 + 1260 x 4 + 37 , 800 x 2 + 113 , 400 2 4 113 , 400 x 2 e 4 x 2 π 0 .
The function from the left-hand side has the positive roots: x = 0 , x 1.573 , x 4.37287 , therefore the function takes positive values for x 0 , 1.573 .
The proof is complete.  ☐
In order to refine Komatsu’s inequalities, first we use the change of variables t = y 2 in the integral x e t 2 2 d t , then we substitute x 2 by x in Komatsu’s inequalities and we obtain Komatsu’s inequalities for the complementary error function e r f c x :
2 e x 2 x + x 2 + 2 < π 2 e r f c x < e x 2 x + x 2 + 1
hold for all x > 0 or, equivalent:
1 2 π e x 2 x + x 2 + 1 < e r f x < 1 2 π e x 2 x + x 2 + 2
hold for all x > 0 .
Using the Padé approximation for e r f x , we obtain an improved version of Komatsu’s inequalities as follows.
Proposition 3.
The following inequalities hold:
(i) 2 π A x 1 2 π e x 2 x + x 2 + 1 for all x 0 , 1.28089 ,
(ii) 2 π B x 1 2 π e x 2 x + x 2 + 2 for all x 0 , 1.33740041 0 , 4.418 .
Proof. 
(i) The inequality from (i) takes the equivalent form:
e x 2 39 π 2 x 4 + 110 x 3 90 π x 2 + 210 x 105 π + + x 2 + 1 x 39 x 4 + 180 x 2 + 210 > 0 .
The function from the left-hand side has only one positive root x 1.28089 and it is positive for x 0 , 1.28089 .
(ii) The inequality from (ii) can be rewritten as follows:
e x 2 29 π 2 x 8 + 330 π x 6 630 π x 4 18 , 900 π x 2 + 113 , 400 x 56 , 700 π + + x 2 + 2 x 29 2 x 8 330 x 6 + 630 x 4 + 18 , 900 x 2 + 56 , 700 > 0 .
The function from the left-hand side has two positive roots: x 1.33740 and x 4.37287 and it is positive for x 0 , 1.33740 4.37287 , .
Therefore, we improve Komatsu’s inequalities near the origin providing sharp bounds of rational types for the error function.  ☐
In the following we derive approximation to four decimals of precision for the function π 2 e r f x on a large neighbourhood of the origin.
Theorem 2.
The approximation π 2 e r f x C x is valid for all x, x 2.4 , with absolute error ε x < 8.22775 × 10 4 .
Proof. 
The function
ε x = π 2 e r f x C x
has the derivative
ε x = e x 2 + 21 5 · E x F x ,
where
E x = 151 , 463 , 081 x 10 640 , 919 , 835 x 8 5 , 296 , 822 , 800 x 6 + + 31 , 069 , 085 , 040 x 4 + 132 , 620 , 407 , 920 x 2 999 , 139 , 291 , 920
and
F x = 10 , 519 x 6 + 151 , 725 x 4 + 888 , 300 x 2 + 2 , 048 , 508 2 .
The equation ε x = 0 has the roots x 1 1.7103 , x 2 0 , x 3 1.7103 .
Partition the domain into intervals with endpoints at the critical points:
, 1.7103 , 1.7103 , 0 , 0 , 1.7103 and 1.7103 , .
Then we have ε x > 0 on , 1.7103 and 1.7103 , respectively and ε x < 0 on 1.7103 , 1.7103 .
On the interval , 1.7103 , the function ε is increasing from lim x ε x = π 2 0.886227 to ε 1.7103 = 1.95966 × 10 5 .
The root x 2 = 0 is a critical point, but it is not an extreme point of the function ε , therefore on the interval 1.7103 , 1.7103 , the absolute error function ε is decreasing from ε 1.7103 = 1.95966 × 10 5 to ε 1.7103 = 1.95966 × 10 5 .
On the interval 1.7103 , , the function ε is increasing from ε 1.7103 = 1.95966 × 10 5 to lim x ε x = π 2 0.886227 .
Since we have ε 2.4 = 8.22775 × 10 4 and ε 2.5 = 1.2898 × 10 3 , we consider our a approximation on 0 , 2.4 . For negative x, one can use the identities e r f x = e r f x and C x = C x , therefore we extend our approximation on 2.4 , 2.4 .
The proof of Theorem 2 is complete.  ☐
Remark 1.
We find the approximation π 2 e r f x C x with the absolute error ε x < 8.22775 × 10 4 .
Therefore we propose the following approximation for the error function e r f x :
η x = 2 π C x ; 2.4 x 2.4 1 ; otherwise ,
where the absolute error for the first form is ε 1 x < 2 π × 8.22775 × 10 4 = 9.28402 × 10 4 and the absolute error for the second form is ε 2 x < 1 e r f 2.4 = 6.88514 × 10 4 .
In the second part of this section we will establish our approximations of the error function using Fourier trigonometric series expansions.
Theorem 3.
The following inequalities
7 18 x + 3 2 sin x 3 20 sin 2 x + 17 270 sin 3 x < π 2 e r f x < 3 2 x 4 3 sin x + 5 12 sin 2 x
hold for all x > 0 .
Proof. 
In order to prove the right - hand side inequality, we consider the function f 1 : 0 , R , f 1 x = π 2 e r f x 3 2 x + 4 3 sin x 5 12 sin 2 x .
The derivative of the function f 1 is
f 1 x = e x 2 3 2 + 4 3 cos x 5 6 cos 2 x .
We intend to show that f 1 < 0 on 0 , or, equivalently,
e x 2 < 4 3 cos x + 5 6 cos 2 x + 3 2 , for all x 0 , .
Since
4 3 cos x + 5 6 cos 2 x + 3 2 = 5 cos 2 x 4 cos x + 2 3 > 0
for all x 0 , , we can log the above inequality and it remains to be proved that
x 2 < log 4 3 cos x + 5 6 cos 2 x + 3 2 ,
for all x 0 , .
The function f 2 : 0 , R , f 2 x = x 2 log 4 3 cos x + 5 6 cos 2 x + 3 2 has the derivatives
f 2 x = 2 4 sin x 5 sin 2 x 8 cos x 5 cos 2 x 9 2 x
and
f 2 2 x = 32 sin 4 x 2 5 cos x + 2 2 + 2 8 cos x + 5 cos 2 x + 9 2 < 0 ,
for all x > 0 .
Then f 2 is strictly decreasing on 0 , . As f 2 0 = 0 , we get f 2 < 0 on 0 , .
Continuing the algorithm, finally we find f 2 < 0 on 0 , .
In order to prove the left-hand side inequality, first we notive that the function
f 3 x = 7 18 x + 3 2 sin x 3 20 sin 2 x + 17 270 sin 3 x
has the positive roots x = 0 , x 2.57617 .
Since f 3 π 2 > 0 , it follows that f 3 > 0 only on 0 , 2.57617 , hence we have to show the left-hand side inequality only for x 0 , 2.57617 .
We introduce the function f 4 : 0 , 2.57617 R , f 4 x = π 2 e r f x + 7 18 x 3 2 sin x + 3 20 sin 2 x 17 270 sin 3 x .
The derivative of the function f 4 is
f 4 x = e x 2 3 2 cos x + 3 10 cos 2 x 17 90 cos 3 x + 7 18 .
We have to prove that f 4 > 0 on 0 , 2.57617 , or equivalently,
e x 2 > 3 2 cos x 3 10 cos 2 x + 17 90 cos 3 x 7 18 .
The function f 5 x = 3 2 cos x 3 10 cos 2 x + 17 90 cos 3 x 7 18 has on 0 , 2.57617 only the root x 1.46966 . Since f 5 π 2 < 0 , then f 5 > 0 only on 0 , 1.46966 .
Hence it remains to verify the inequality (3) only for x 0 , 1.46966 0 , π 2 .
We log the inequality (3) and we obtain
x 2 log 3 2 cos x 3 10 cos 2 x + 17 90 cos 3 x 7 18 > 0
on 0 , 1.46966 .
We consider the function f 6 : 0 , 1.46966 R , f 6 x = x 2 log 3 2 cos x 3 10 cos 2 x + 17 90 cos 3 x 7 18 .
Its derivatives are
f 6 x = 2 x + 3 45 sin x 18 sin 2 x + 17 sin 3 x 35 + 135 cos x 27 cos 2 x + 17 cos 3 x
and
f 6 2 x = 32 sin 6 x 2 2312 cos 3 x + 4182 cos 2 x + 3600 cos 2 x + 1516 135 cos x + 27 cos 2 x 17 cos 3 x + 35 2 .
Evidently, f 6 2 x > 0 on 0 , π 2 0 , 1.46966 .
Then f 6 is strictly increasing on 0 , 1.46966 . As f 6 0 = 0 , we find that f 6 > 0 on 0 , 1.46966 .
Finally, we have f 6 > 0 on 0 , 1.46966 .
The proof of the Theorem 3 is complete.  ☐
In the following we derive approximation to three decimals of precision for the function e r f x on a large neighbourhood of the origin.
We note by
G x = 2 π 7 18 x + 3 2 sin x 3 20 sin 2 x + 17 270 sin 3 x
and
H x = 2 π 3 2 x 4 3 sin x + 5 12 sin 2 x .
In Theorem 3 we proved that
G x < e r f x < H x ,
for all x > 0 .
Now we consider the convex combination
θ x = e r f x 0.77 G x 1 0.77 H x
or, equivalently,
θ x = e r f x 0.051403 x 0.957242 sin x + 0.022191 sin 2 x 0.054705 sin 3 x .
The derivative of θ x is
θ x = 1.12838 e x 2 0.848334 cos x + 0.0399333 cos 2 x 0.145444 cos 3 x 0.045555 .
The roots of the function θ on the interval 0 , 1.933 are x = 0 and x 1.571371 . Since π 2 0 , 1.571371 and θ π 2 < 0 , it follows that θ < 0 on 0 , 1.571371 and θ > 0 on 1.571371 , 1.933 , hence θ is strictly decreasing on 0 , 1.571371 and θ is strictly increasing on 1.571371 , 1.933 .
Then min 0 x 1.933 θ x 0.009602 at x 1.571371 , max 0 x 1.933 θ x 0.009997 at x 1.933 and θ 0 = 0 .
Therefore we find the approximation e r f x J x , where J x = 0.051403 x + 0.957242 sin x 0.022191 sin 2 x + 0.054705 sin 3 x with the absolute error θ x 9.99747 × 10 3 .
Since 1 e r f 1.933 = 6.26319 × 10 3 , we propose the 3 following approximation to three decimals of precision for the error function e r f x :
φ x = J x ; 0 x 1.933 1 ; otherwise .

3. Application Case

As an example to apply the error function, one case is considered for the diffusion and reactions in sediments.
We assume that oxygenated water comes in contact with sediments at the bottom of a lake at the time of “fall turnover”. The water contains 300 μmoles of O 2 /liter. We suppose that no reactions consume the oxygen. We want to find what is the concentration of oxygen in sediments after one day, one week and one month after the turnover event.
Mathematically, the diffusion problem for a constant source region diffusing into a space of unlimited extent (“semi—infinite half—space”) is to solve
C t = D · 2 C x 2
given the boundary conditions that the concentration at the sediment-water interface C 0 is always fixed and no reactions consume the oxygen, and initial condition that the concentration below the boundary is initially everywhere 0.
This linear PDE, having a solution that requires one initial condition and two boundary conditions is called Fick’s second law for isotropic one-dimensional diffusion with D independent of concentration.
The solution to this problem involves the error function:
C x , t = C 0 e r f c x 2 D t ,
where C x , t is the concentration at a given depth and time, C 0 is the concentration at the interface, D is the diffusion coefficient, x is depth below the interface, and t is time.
An appropriate value of the diffusion constant D is 2 × 10 5 cm 2 s 1 . We choose a depth range x of 0–20 cm. Since the units of time in the diffusion constant are seconds, we calculate our valued for concentration using seconds for t to obtain a good result.
In order to solve this equation, we will use our approximation for the error function:
C x , t = C 0 1 e r f x 2 D t = C 0 1 η x 2 D t ,
where η x is defined by (2) or C x , t = C 0 1 φ x 2 D t , where φ x is defined by (4).

4. Conclusions

In our work we use Padé approximation method and Fourier series method in order to obtain approximations for the error function. Using Padé approximation method, we obtain the following bounds: e r f x 2 π A x , for all x 0 and e r f x 2 π B x , for all x [ 0 , 4.418 ) and the following approximation to four decimals of precision for the function e r f x on a large neighbourhood of the origin:
η x = 2 π C x ; 2.4 x 2.4 1 ; otherwise
with the absolute error ε 1 x < 9.28402 × 10 4 , where C x = 302 , 379 x 5 + 1 , 027 , 320 x 3 + 10 , 242 , 540 x 52 , 595 x 6 + 758 , 625 x 4 + 4 , 441 , 500 x 2 + 10 , 242 , 540 .
Furthermore, using Fourier series method, we obtain the following bounds:
G x < e r f x < H x , for all x > 0
and the following approximation to three decimals of precision for the function e r f x on a large neighbourhood of the origin:
φ x = J x ; 0 x 1.933 1 ; otherwise
with the absolute error θ x 9.99747 × 10 3 , where J x = 0.051403 x + 0.957242 sin x 0.022191 sin 2 x + 0.054705 sin 3 x .
The results are simple expressions which have acceptable deviations in connection with engineering calculations. The absolute error for the error functions are also comparable to other approximations found in the literature. The approximate error functions can be employed on the solution of practical problems like the one related to diffusion and reactions in sediments.

Funding

The APC was funded by “Dunărea de Jos” University of Galaţi, Romania.

Conflicts of Interest

The author declares no conflict of interest.

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Bercu, G. New Refinements for the Error Function with Applications in Diffusion Theory. Symmetry 2020, 12, 2017. https://doi.org/10.3390/sym12122017

AMA Style

Bercu G. New Refinements for the Error Function with Applications in Diffusion Theory. Symmetry. 2020; 12(12):2017. https://doi.org/10.3390/sym12122017

Chicago/Turabian Style

Bercu, Gabriel. 2020. "New Refinements for the Error Function with Applications in Diffusion Theory" Symmetry 12, no. 12: 2017. https://doi.org/10.3390/sym12122017

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