Ordinary Diff Eqs
Partial Diff Eqs
Convergence
Parameterization
Residues Residonts
100

for the linear ODE  y'' + p(x) y' + q(x) y = r(x)

if r(x) = 0 we say ...

The ODE is homogeneous

100

u(0,t) = 0 and u(L,t) = 0 are known as the 

Dirichlet Boundary Conditions

100

Name three types of convergence tests

Integral test

Ratio test

Root test

Alternating Series test

100

Is there only one allowable way to parameterize an integral problem?

No.  Parameterization is always a choice.  Sometimes there is an obvious or best choice.  

100

the equations  u_x = v_y    u_y = - v_x

are

The Cauchy Riemann Equations, used to verify whether a complex function is analytic (differentiable) 

200

y'' + a y' + b y = 0  has as it's solution basis...

Two linearly-independent eigen-functions

e^(lambda_1 x)

e^(lambda_2 x)  or  x e^(lambda_1 x)

Note that they may be re-written to use sin and cos if the lambdas are complex

200

For the time-evolution of modes in a Heat Equation problem,

the G_n(t) terms are of the form...

Exponential Decay Function

200

sum of 1/n for n from 0 to infinity is known as ...

the Harmonic Series   It does not converge to a finite sum.

200

For a line integral, the   r'(t)  expression is 

the Tangent function

instantaneous tangent to the curve

200

The difference between  arg z  and  Arg z  is

an integer multiple of 2*pi

300

For y'' + a y' + b y = r(t)   where a and b are real (scalar) coefficients

if a^2 < 4 b then the eigenvalues will be

a complex-conjugate pair

300
For the mode oscillations of a wave equation, the higher modes oscillate...

oscillate faster (think higher frequency)

300

sum of x^n / n!  for n = 0..infinity  is recognized as the

exponential function of x

300

Name three re-parameterizations commonly seen in vector calculus

polar coordinates

cylindrical coordinates

spherical coordinates

300

The roots of complex numbers are more easily computed by...

converting the complex number to polar form

|z| ( cos Arg (z) + i sin Arg(z) )

400

For  y'' + a y' + b y = r(t)

we call the expression

1 / (s^2 + a s + b) 

the Transfer Function

400

If the divergence of the gradient of a scalar-valued function f(x,y,z) equals zero, we say that

f is a potential function

solenoidal

400

Better than a lower-rectangle integration or an upper-rectangle integration is a integration using trapezoids... often better than that is a method called Simpson's method... what makes it better?

It integrates with quadratic segments

400

when you see a  ds  in an integral it means

The s parameter is proportional to the length of the curve, it is length-preserving.  You'll see s in the integral for Arc Length.

400

The zero result of  a closed path integral of  1 / z^2  around the origin (0,0) tells us

Not all nonanalytic functions produce a residue

Cauchy's Integral Theorem (analyticity) is a sufficient but not necessary condition for the zero integration result

500

An input oscillation to a 2nd-order system (ODE) will produce

(assume steady state) 

an oscillation with the same frequency, but it may be altered by amplitude and incur a phase shift

500

The D-Alembert solution might look like a travelling wave going in only one direction if

The initial condition includes both an initial displacement and an initial velocity

500

A discontinuity in the function f(x) leads to a Fourier Series with a little tail near the discontinuity ...

Gibb's Effect

500

True or False, if you parameterize by x and y, you will never have to compute a Jacobian determinant

False.  If the surface is not on the x,y plane, a Jacobian Determinant will still be necessary, but it's value is obtained in the magnitude of the r_u X r_v  normal vector when calculated.  

500
One way to use Cauchy's Integral Formula is for 

finding the value of an analytic function at a given point

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