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11: 18.40 Methods of Computation
In what follows this is accomplished in two ways: i) via the Lagrange interpolation of §3.3(i) ; and ii) by constructing a pointwise continued fraction, or PWCF, as follows: …
12: 9.16 Physical Applications
The function Ai ( x ) first appears as an integral in two articles by G. … In the study of the stability of a two-dimensional viscous fluid, the flow is governed by the Orr–Sommerfeld equation (a fourth-order differential equation). …
13: 19.16 Definitions
A fourth integral that is symmetric in only two variables is defined by
19.16.5 R D ( x , y , z ) = R J ( x , y , z , z ) = 3 2 0 d t s ( t ) ( t + z ) ,
14: 19.23 Integral Representations
19.23.3 R D ( 0 , y , z ) = 3 0 π / 2 ( y cos 2 θ + z sin 2 θ ) 3 / 2 sin 2 θ d θ .
In (19.23.8)–(19.23.10) one or more of the variables may be 0 if the integral converges. …
15: 29.7 Asymptotic Expansions
Müller (1966a, b) found three formal asymptotic expansions for a fundamental system of solutions of (29.2.1) (and (29.11.1)) as ν , one in terms of Jacobian elliptic functions and two in terms of Hermite polynomials. …
16: 35.2 Laplace Transform
where the integration variable 𝐗 ranges over the space 𝛀 . Suppose there exists a constant 𝐗 0 𝛀 such that | f ( 𝐗 ) | < etr ( 𝐗 0 𝐗 ) for all 𝐗 𝛀 . …
17: 19.29 Reduction of General Elliptic Integrals
19.29.7 y x a α + b α t a δ + b δ t d t s ( t ) = 2 3 d α β d α γ R D ( U α β 2 , U α γ 2 , U α δ 2 ) + 2 X α Y α X δ Y δ U α δ , U α δ 0 .
19.29.10 u b a t ( b t ) ( t c ) 3 d t = 2 3 ( a b ) ( b u ) 3 / 2 R D + 2 b c ( a u ) ( b u ) u c , a > b > u > c ,
19.29.20 y x t 2 d t Q 1 ( t ) Q 2 ( t ) = 1 3 a 1 a 2 R D ( U 2 + a 1 b 2 , U 2 + a 2 b 1 , U 2 ) + ( x y / U ) ,
19.29.21 y x d t t 2 Q 1 ( t ) Q 2 ( t ) = 1 3 b 1 b 2 R D ( U 2 + a 1 b 2 , U 2 + a 2 b 1 , U 2 ) + ( x y U ) 1 ,
If both square roots in (19.29.22) are 0, then the indeterminacy in the two preceding equations can be removed by using (19.27.8) to evaluate the integral as R G ( a 1 b 2 , a 2 b 1 , 0 ) multiplied either by 2 / ( b 1 b 2 ) or by 2 / ( a 1 a 2 ) in the cases of (19.29.20) or (19.29.21), respectively. …
18: 19.30 Lengths of Plane Curves
19.30.9 s = 1 2 I ( 𝐞 1 ) = 1 3 a 2 b 2 R D ( r , r + b 2 + a 2 , r + b 2 ) + y r + b 2 + a 2 r + b 2 , r = b 4 / y 2 .
19: 19.21 Connection Formulas
19.21.1 R F ( 0 , z + 1 , z ) R D ( 0 , z + 1 , 1 ) + R D ( 0 , z + 1 , z ) R F ( 0 , z + 1 , 1 ) = 3 π / ( 2 z ) , z ( , 0 ] .
19.21.2 3 R F ( 0 , y , z ) = z R D ( 0 , y , z ) + y R D ( 0 , z , y ) .
19.21.8 R D ( y , z , x ) + R D ( z , x , y ) + R D ( x , y , z ) = 3 x 1 / 2 y 1 / 2 z 1 / 2 ,
19.21.9 x R D ( y , z , x ) + y R D ( z , x , y ) + z R D ( x , y , z ) = 3 R F ( x , y , z ) .
For each value of p , permutation of x , y , z produces three values of q , one of which lies in the same region as p and two lie in the other region of the same type. …
20: 29.14 Orthogonality
Lamé polynomials are orthogonal in two ways. …