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1: 16.24 Physical Applications
§16.24(i) Random Walks
Generalized hypergeometric functions and Appell functions appear in the evaluation of the so-called Watson integrals which characterize the simplest possible lattice walks. They are also potentially useful for the solution of more complicated restricted lattice walk problems, and the 3D Ising model; see Barber and Ninham (1970, pp. 147–148). …
2: 23.7 Quarter Periods
23.7.1 ( 1 2 ω 1 ) = e 1 + ( e 1 e 3 ) ( e 1 e 2 ) = e 1 + ω 1 2 ( K ( k ) ) 2 k ,
23.7.2 ( 1 2 ω 2 ) = e 2 i ( e 1 e 2 ) ( e 2 e 3 ) = e 2 i ω 1 2 ( K ( k ) ) 2 k k ,
23.7.3 ( 1 2 ω 3 ) = e 3 ( e 1 e 3 ) ( e 2 e 3 ) = e 3 ω 1 2 ( K ( k ) ) 2 k ,
where k , k and the square roots are real and positive when the lattice is rectangular; otherwise they are determined by continuity from the rectangular case.
3: 23.3 Differential Equations
The lattice invariants are defined by … The lattice roots satisfy the cubic equation …and are denoted by e 1 , e 2 , e 3 . … Let g 2 3 27 g 3 2 , or equivalently Δ be nonzero, or e 1 , e 2 , e 3 be distinct. … Conversely, g 2 , g 3 , and the set { e 1 , e 2 , e 3 } are determined uniquely by the lattice 𝕃 independently of the choice of generators. …
4: 23.14 Integrals
23.14.2 2 ( z ) d z = 1 6 ( z ) + 1 12 g 2 z ,
5: 23.10 Addition Theorems and Other Identities
23.10.4 σ ( u + v ) σ ( u v ) σ ( x + y ) σ ( x y ) + σ ( v + x ) σ ( v x ) σ ( u + y ) σ ( u y ) + σ ( x + u ) σ ( x u ) σ ( v + y ) σ ( v y ) = 0 .
For further addition-type identities for the σ -function see Lawden (1989, §6.4). …
23.10.8 ( ( 2 z ) e 1 ) 2 ( z ) = ( ( ( z ) e 1 ) 2 ( e 1 e 2 ) ( e 1 e 3 ) ) 2 .
(23.10.8) continues to hold when e 1 , e 2 , e 3 are permuted cyclically. … Also, when 𝕃 is replaced by c 𝕃 the lattice invariants g 2 and g 3 are divided by c 4 and c 6 , respectively. …
6: 23.2 Definitions and Periodic Properties
§23.2(i) Lattices
( z ) and ζ ( z ) are meromorphic functions with poles at the lattice points. ( z ) is even and ζ ( z ) is odd. …The function σ ( z ) is entire and odd, with simple zeros at the lattice points. …
7: 23.21 Physical Applications
The Weierstrass function plays a similar role for cubic potentials in canonical form g 3 + g 2 x 4 x 3 . … Airault et al. (1977) applies the function to an integrable classical many-body problem, and relates the solutions to nonlinear partial differential equations. … where x , y , z are the corresponding Cartesian coordinates and e 1 , e 2 , e 3 are constants. …
23.21.3 f ( ρ ) = 2 ( ( ρ e 1 ) ( ρ e 2 ) ( ρ e 3 ) ) 1 / 2 .
Another form is obtained by identifying e 1 , e 2 , e 3 as lattice roots (§23.3(i)), and setting …
8: 23.4 Graphics
§23.4(i) Real Variables
Line graphs of the Weierstrass functions ( x ) , ζ ( x ) , and σ ( x ) , illustrating the lemniscatic and equianharmonic cases. …
See accompanying text
Figure 23.4.7: ( x ) with ω 1 = K ( k ) , ω 3 = i K ( k ) for 0 x 9 , k 2 = 0. … Magnify
Surfaces for the Weierstrass functions ( z ) , ζ ( z ) , and σ ( z ) . …
See accompanying text
Figure 23.4.8: ( x + i y ) with ω 1 = K ( k ) , ω 3 = i K ( k ) for 2 K ( k ) x 2 K ( k ) , 0 y 6 K ( k ) , k 2 = 0.9 . (The scaling makes the lattice appear to be square.) Magnify 3D Help
9: 23.9 Laurent and Other Power Series
Let z 0 ( 0 ) be the nearest lattice point to the origin, and define …
c 2 = 1 20 g 2 ,
For j = 1 , 2 , 3 , and with e j as in §23.3(i),
23.9.6 ( ω j + t ) = e j + ( 3 e j 2 5 c 2 ) t 2 + ( 10 c 2 e j + 21 c 3 ) t 4 + ( 7 c 2 e j 2 + 21 c 3 e j + 5 c 2 2 ) t 6 + O ( t 8 ) ,
Also, Abramowitz and Stegun (1964, (18.5.25)) supplies the first 22 terms in the reverted form of (23.9.2) as 1 / ( z ) 0 . …
10: 23.5 Special Lattices
§23.5 Special Lattices
§23.5(ii) Rectangular Lattice
§23.5(iii) Lemniscatic Lattice
§23.5(iv) Rhombic Lattice
§23.5(v) Equianharmonic Lattice