A Proof of Fermat's Last Theorem using an Euler's Equation
Journal Title: Asian Research Journal of Mathematics - Year 2017, Vol 6, Issue 3
Abstract
Fermat's Last Theorem states that there are no solutions to xn + yn = zn for n ≥ 3 and x; y; z non-zero integers. Fermat wrote down a proof for n = 4 [1]. In 1753, Lenohard Euler (1707{1783) wrote down a proof of FLT for the exponent n = 3 [1]. Since any integer n ≥ 3 is divisible by an odd prime number or by 4, it is sucient to prove FLT for n = p, an odd prime > 3. We prove the theorem for p ≥ 5. We consider x3 + y3 = z3 and sp + tp = up, where p is any prime > 3. Without loss of generality it is enough to assume that both x and y as non-zero positive integers; therefore z3 will be a non-zero positive integer, but both z and z2 will be irrational in the rst equation. We hypothesize that there exist positive integers, s; t and u in the Fermat's equation sp + tp = up and bring a contradiction. We have created by trial and error method two equivalent equations to Fermat's equations. x3 + y3 = z3 and sp + tp = up through parameters a; b; c; d; e and f given by( a √ √u + b 2n=2 )2 + ( a − b √ l5=3 √ 23n=2 )2 = ( e √ 71=3k5=3 + f )2 ( c √ √ xt + d 75=3k7=3 )2 + ( c √ y − d √ l7=3 )2 = ( e − f √ z )2 respectively. The values of a; b; c; d; e and f in terms of known values are worked out in the detailed proof. Also we can obtain the equivalent values of 2n; 7k2 and l2 from these equations where 2n = 7k2 + l2: (The validity of the equivalent equations has been discussed in detail in Annexure{A). Solving the above two equivalent equations using the above Euler's equation, we arrive at the result stu = 0, thus proving the theorem. Use of the Euler's equation leads us to this elementary proof.
Authors and Affiliations
P. N. Seetharaman
A Simple Model of Sediment Transport in the Nearshore Zone
In this paper we examine a simple model of sediment transport, induced by the breaking waves in the surf zone. Essentially the bottom is allowed to move in response to the divergence of a sediment flux, in turn determine...
Some Power Sums from the Geometric Series
We focus on the summation of Σn r=1 (r + k − 1)! (r − 1)! xr+k and express it as simple polynomials and nd a relation between them.
Some Theorems on Fixed Points Set of Asymptotically Demicontractive Mappings in the Intermediate Sense
In this paper, we establish the closedness and convexity of the xed point set of asymptotically demicontractive mappings in the intermediate sense introduced by Olaleru and Okeke [Convergence theorems on asymptotically...
Topologized Cut Vertex and Edge Deletion
In this paper discussed and study a new result of non-topologized graph by using cut vertex and cut edge component of the graph makes the graph to be Topologized graph. This concept implemented to some families of graph.
Conditional Least Squares Estimation for Discretely Sampled Nonergodic Diusions
Strong consistency and conditional asymptotic normality of the conditional least squares estimator of a parameter appearing nonlinearly in the time dependent drift coefficient of the Itˆo stochastic differential equation...