|
,
and a greatest lower bound ("meet").
.
Axiomatically there is assigned a (not operationally attained) single least element,
usually labeled its "0"; also assigned, a (not operationally attained) single greatest element
, usually labeled its "1". (In this Dictionary, perhaps uniquely, an indicator table (of
zeros and ones) (PL) is assigned to a lattice, conflicting with the standard "0" and "1"
labels just cited, hence, these are herein labeled "MIN" and "MAX", to distingish from each
sublattice min and max.) Ranging from its 0 or MIN to its 1 or MAX, a
lattice has a metric (PL) known as "rank". Every lattice has an associated dual lattice
invoked by interchanging meet and join, so that any increase in a lattice is
associated with a decrease in its dual lattice, inducing a dual isomorphism
(PL fundamental theorem of Galois theory ), so that an inclusion in one lattice
corresponds uniquely to an included in the other lattice. This "dual isomorphism" is the
Galois correspondence. (When the above partial ordering is changed to a simple
or total ordering (PL), the Galois correspondence becomes an antitone (PL),
which may be inherent in every physical process, PL antitonic hypothesis.)
F
for which s(K) = K must fix
K . An extension is not a Galois extension if, either it
is not normal (PL), or it is not separable.
x) = 1 - D(X > x) = 1 - [G(h, xl
)/G(h), for x e
[0,
), where G(x)
is a complete gamma function and G(
a, x) is an imcomplete gamma function. Differentiating for the
probability distribution function, P(x) = D'(x) = [g
(gx)h-1/(h - 1)!]e-hx. Setting a
h (not necessarily integral
and q
1/l
for time between changes. Then the above p.d.f. becomes
P(x) = [xa - 1ex/q]/G(a)q
a. The characteristic function (PL) is f(t) = (1 - itq)-a
. The mean is m = a
q; the variance is s2
= aq2.
dMk
gds, for compact M.
2
(the side and diagonal of a unit square): G
1/M(1,
2) = (1/2p)
½p01/[(1 + sin2q
)1/2]dq = (
2/p
K)(1/
2) = 1/(2p)3/2[G(1/4)]2 = 0,83462684167....
-1, for integers a, b. Gaussian integers belong to the imaginary quadratic field, Q(
-1), forming a ring
, Z(i), closed under sum,
difference, product, and division provided the quotient is integral.
f(x +
reiq)dq, 0 < r < R.
(PL mean value theorem.)
1 and Q represent m: c1(Q), c2(Q), ..., cr(Q). The characters apply to the class of properly
equivalent forms as they represent the same numbers. PL genus (form).
½(n - 1)(n - 2) - (d + k) = ½(m - 1)(m - 2) - (t
+ I), where n, d
, k, m, t, i
are, respectively, order, number of nodes, no. of cusps, class, no. of bitangents,
no. of inflection points. (PL Riemann curve theorem.)
1
(mod 4) -- uniquely, except for sign-change. This theorem connects with the
quadratic reciprocity theorem (PL), generalizing to the quartic reciprocity theorem
(PL).
du =
(dx2 + dy2 + dz2)½.
Rewriting, u'
Dvu, v'
D
uv, P
(Dux)2 + (Duy)2
+ (Duz)2, Q
DuxDvx + Du
yDvy + DuzDvz, R
(Dvx)
2 + (Dvy)2 + (Dvz)2, L =
(P + 2Qv' + Rv'2)½du =
(P + 2Qu' + Ru'2)
½dv
D, F
P , E
C, and EULER'S RULE
GIBB'S RULE. ASSIGNMENT: POINCARÉ generalized Euler's formula for topology to allow for
"holes" and such. Is this homologous to any thermodynamic aspect?)
5)/2 = 1.618033988.... This is supposedly used in many
works of art and architecture. Given the regular (even-sided) pentagon; connect each
vertex to its two opposite vertices; these segments intersect at the golden mean.
M, s.t. (M, f) is a graded algebra.
("del" or "nabla"), often applied to a 3-fold function
(PL), f(u1, u1, u1), thus:
f
grad(f). In cartesian
coordinates:
f = Dx
fx + Dyfy
+ Dzfz. The direction of
f is the orientation in which the
directional derivative is maximal and |
f| is its value. Also, if nonull, the gradient is
perpendicular to the level curve (PL) through {x0, y0
if z = f(x, y) but perpendicular to the level curve through
(x0, y0, z0) if F(x, y,z) = 0. In general, the gradient is perpendicular to the surface of its
application . In mathematical physics, the gradient of a scalar function connects a
force field to a potential field: FORCE = - grad(potential),
modeling gravitational fields, electrostatic fields, etc. (The negative sign above is
necessary to model, for example, water running downhill.) A force has a potential iff it is
irrotational, that is, the work done by the force around a closed loop is zero, as
with gravitational and electrostic force fields. Thus, the gradient and the
potential indicate a conservative field (PL). Hermann von Helmholtz (x-y) proved
that every vector can be factored into an irrorational component and a (rotational) curl
(PL). In multivector theory (PL) (a.k.a. geometric algebra, Clifford algebra,
Arithmetic of Clifford Numbers), the inner product (PL) and outerproduct (PL)
combine in (add up to) a single multiproduct whose derivative combines grad and
curl in a single operator.
Dn + an-1(t)Dn-1 + ... +
a1(t)D + a0(t), with ai, i = 0, 1, ...,
n-1 continuous on interval, I, to find solution
, y(t) of equation, Ly(t) = h(t),
for h(t) a given contnuous function on I
. To solve this, seek a function: g: C(I)
C(I)
s. t. L(g(h)) = h, where y(t) = g(h(t)), a
convolution (PL) equation of the form, y = g * h, with solution,
y(t) =
t
t0g(t - x)h(x)dx. The integrating kernel, g(t), here, is the Green's function for L on t, often with h(t)
d
(t) (the Dirac function, PL), so that we have: y = g * h,
with solution, y(t) =
tt0g(t - x)d(x)dx, where
Lg(t)
d(t). But a
Green's function is uniquely determined only by initial or boundary conditions (PL).
In 3=D, we have: g(r, r') = d(r
, r'). Then the solution to Lf = f
is f(r) =
g(r, r')f(r')d3r'
.
· (y
f
) = y
2f
+ (
y) · (
f)[1] and
· (f
y) = y
2f + (
f) · (
y) [2]. where
· is the divergence operator (PL),
is the gradient operator (PL),
2 is the Laplacian operator (PL), and _ · _ is inner or dot product. The divergence theorem writes a
volume integral as a surface integral involving a normal:
V (
· F)dV =
S F
· dn [3]. Inserting [3] in [2]:
V
· (f
y)[y
2f + (
f
) · (
y)]dV =
S
· (
f
y) · dn [4],
Green's first integral identity. Subtracting [2] from [1]:
y -
y
f) = f
2y - y
2f. So:
V(f
2y - y
y
- y
f)dn
[7], Green's second identity. If u has continuous
first partial derivatives and is harmonic inside the region of integration, then, writing
C as a
circular integral, we have Greem's third identity: u(x, y) = 1/2
p
C [ln
(1/r) Dnu - u Dn ln (1/r)] ds.
b(D)[f(x, y)dx + g(x, y)dy] =

D(Dxy - D
yx)dxdy, or
b(D)F · ds = 
D (
X F) · k d
A. If the region D is on the left when traveling around
b(D), then the area of D can be
computed as: A = ½
b(D)[xdy - ydx].
0xdt/cosh t =
2 arctan [tanh (½x)] = arctan (sinh x) = 2arctan (ex) - ½p. The derivative of the Gudermannian is: Dx
gd(x) = sech x, and, of course, it connects with trignometric, hyperbolic and
exponential functions.