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Probability Theory is a prerequisite.
For comments please contact me at solo.hermelin@gmail.com.
For more presentations on different subjects visit my website at http://www.solohermelin.com.
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The presentation is at graduate level in math and engineering.
For comments please connect me at solo.hermelin@gmail.com.
For more presentations on different subjects visit my website at http://www.solohermelin.com.
Stochastic Processes describe the system derived by noise.
Level of graduate students in mathematics and engineering.
Probability Theory is a prerequisite.
For comments please contact me at solo.hermelin@gmail.com.
For more presentations on different subjects visit my website at http://www.solohermelin.com.
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Estimate the hidden States of a Non-linear Dynamic Stochastic System from Noisy Measurements. Estimation is a prerequisite. The Probability Theory summary is included.
The presentation is at graduate level in math and engineering.
For comments please connect me at solo.hermelin@gmail.com.
For more presentations on different subjects visit my website at http://www.solohermelin.com.
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Length: 30 minutes
Session Overview
-------------------------------------------
During this webinar, we will cover the following topics while demonstrating the integrations of JMeter, InfluxDB and Grafana:
- What out-of-the-box solutions are available for real-time monitoring JMeter tests?
- What are the benefits of integrating InfluxDB and Grafana into the load testing stack?
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The Art of the Pitch: WordPress Relationships and Sales
Sect5 4
1. SECTION 5.4
Mechanical Vibrations
In this section we discuss four types of free motion of a mass on a spring — undamped,
underdamped, critically damped, and overdamped. However, the undamped and underdamped
cases — in which actual oscillations occur — are emphasized because they are both the most
interesting and the most important cases for applications.
1. Frequency: ω 0 = k / m = 16 / 4 = 2 rad / sec = 1/ π Hz
Period: P = 2π / ω 0 = 2π / 2 = π sec
2. Frequency ω 0 = k / m = 48 / 0.75 = 8 rad / sec = 4 / π Hz
Period: P = 2π / ω 0 = 2π / 8 = π / 4 sec
3. The spring constant is k = 15 N/0.20 m = 75 N/m. The solution of 3x″ + 75x = 0
with x(0) = 0 and x′(0) = -10 is x(t) = -2 sin 5t. Thus the amplitude is 2 m; the
frequency is ω 0 = k / m = 75 / 3 = 5 rad / sec = 2.5 / π Hz ; and the period is 2π/5 sec.
4. (a) With m = 1/4 kg and k = (9 N)/(0.25 m) = 36 N/m we find that ω0 = 12
rad/sec. The solution of x″ + 144x = 0 with x(0) = 1 and x′(0) = -5 is
x(t) = cos 12t - (5/12)sin 12t
= (13/12)[(12/13)cos 12t - (5/13)sin 12t]
x(t) = (13/12)cos(12t - α)
where α = 2π - tan-1(5/12) ≈ 5.8884.
(b) C = 13/12 ≈ 1.0833 ft and T = 2π/12 ≈ 0.5236 sec.
5. The gravitational acceleration at distance R from the center of the earth is g = GM/R2.
According to Equation (6) in the text the (circular) frequency ω of a pendulum is given
by ω2 = g/L = GM/R2L, so its period is p = 2π/ω = 2πR L / GM .
6. If the pendulum in the clock executes n cycles per day (86400 sec) at Paris, then its
period is p1 = 86400/n sec. At the equatorial location it takes 24 hr 2 min 40 sec =
86560 sec for the same number of cycles, so its period there is p2 = 86560/n sec. Now
let R1 = 3956 mi be the Earth′s "radius" at Paris, and R2 its "radius" at the equator.
Then substitution in the equation p1 /p2 = R1 /R2 of Problem 5 (with L1 = L2) yields
R2 = 3963.33 mi. Thus this (rather simplistic) calculation gives 7.33 mi as the thickness
of the Earth's equatorial bulge.
2. 7. The period equation p = 3960 100.10 = (3960 + x) 100 yields x ≈ 1.9795 mi ≈
10,450 ft for the altitude of the mountain.
8. Let n be the number of cycles required for a correct clock with unknown pendulum
length L1 and period p1 to register 24 hrs = 86400 sec, so np1 = 86400. The given
clock with length L2 = 30 in and period p2 loses 10 min = 600 sec per day, so
np2 = 87000. Then the formula of Problem 5 yields
L1 p np1 86400
= 1 = = ,
L2 p2 np2 87000
so L1 = (30)(86400 / 87000)2 ≈ 29.59 in.
10. The F = ma equation ρπr2hx″ = ρπr2hg - πr2xg simplifies to
x″ + (g/ ρh)x = g.
The solution of this equation with x(0) = x′(0) = 0 is
x(t) = ρh(1 - cos ω0t)
where ω0 = g / ρ h . With the given numerical values of ρ, h, and g, the amplitude of
oscillation is ρh = 100 cm and the period is p = 2π ρ h / g ≈ 2.01 sec.
11. The fact that the buoy weighs 100 lb means that mg = 100 so m = 100/32 slugs.
The weight of water is 62.4 lb/ft3, so the F = ma equation of Problem 10 is
(100/32)x'' = 100 - 62.4πr2x.
It follows that the buoy's circular frequency ω is given by
ω2 = (32)(62.4π)r2 /100.
But the fact that the buoy′s period is p = 2.5 sec means that ω = 2π/2.5. Equating
these two results yields r ≈ 0.3173 ft ≈ 3.8 in.
12. (a) Substitution of Mr = (r/R)3M in Fr = -GMrm/r2 yields
Fr = -(GMm/R3)r.
(b) Because GM/R3 = g/R, the equation mr'' = Fr yields the differential equation
r'' + (g/R)r = 0.
3. (c) The solution of this equation with r(0) = R and r'(0) = 0 is r(t) = Rcos ω0t
where ω0 = g / R . Hence, with g = 32.2 ft/sec2 and R = (3960)(5280) ft, we find
that the period of the particle′s simple harmonic motion is
p = 2π/ω0 = 2π R / g ≈ 5063.10 sec ≈ 84.38 min.
13. (a) The characteristic equation 10r 2 + 9r + 2 = (5r + 2)(2r + 1) = 0 has roots
r = − 2 / 5, − 1/ 2. When we impose the initial conditions x(0) = 0, x′(0) = 5 on the
general solution x(t ) = c1e −2 t / 5 + c2 e − t / 2 we get the particular solution
( )
x(t ) = 50 e −2 t / 5 − e − t / 2 .
(b) ( )
The derivative x′(t ) = 25 e− t / 2 − 20 e−2 t / 5 = 5 e−2 t / 5 5 e− t /10 − 4 = 0
when t = 10 ln(5 / 4) ≈ 2.23144 . Hence the mass's farthest distance to the right
is given by x(10 ln(5 / 4)) = 512 /125 = 4.096 .
14. (a) The characteristic equation 25r 2 + 10r + 226 = (5r + 1) 2 + 152 = 0 has roots
r = ( −1 ± 15 i ) / 5 = − 1/ 5 ± 3 i. When we impose the initial conditions
x(0) = 20, x′(0) = 41 on the general solution x(t ) = e − t / 5 ( A cos 3t + B sin 3t ) we
get A = 20, B = 15. The corresponding particular solution is given by
x(t ) = e − t / 5 (20 cos 3t + 15sin 3t ) = 25 e − t / 5 cos(3t − α ) where
α = tan −1 (3 / 4) ≈ 0.6435 .
(b) Thus the oscillations are "bounded" by the curves x = ± 25 e− t / 5 and
the pseudoperiod of oscillation is T = 2π / 3 (because ω = 3 ).
15. The characteristic equation (1/ 2)r 2 + 3r + 4 = 0 has roots r = − 2, − 4. When we impose
the initial conditions x(0) = 2, x′(0) = 0 on the general solution x(t ) = c1e −2 t + c2 e−4 t we
get the particular solution x(t) = 4e-2t - 2e-4t that describes overdamped motion.
16. The characteristic equation 3r 2 + 30r + 63 = 0 has roots r = − 3, − 7. When we impose
the initial conditions x(0) = 2, x′(0) = 2 on the general solution x(t ) = c1e −3 t + c2 e −7 t we
get the particular solution x(t) = 4e-3t - 2e-7t that describes overdamped motion.
17. The characteristic equation r 2 + 8r + 16 = 0 has roots r = − 4, − 4. When we impose the
initial conditions x(0) = 5, x′(0) = − 10 on the general solution x(t ) = ( c1 + c2t ) e −4 t we
get the particular solution x(t ) = (5 + 10 t ) e−4 t that describes critically damped motion.
4. 18. The characteristic equation 2r 2 + 12r + 50 = 0 has roots r = − 3 ± 4 i. When we impose
the initial conditions x(0) = 0, x′(0) = − 8 on the general solution
x(t ) = e−3t ( A cos 4t + B sin 4t ) we get the particular solution
x(t ) = − 2 e −3t sin 4t = 2 e −3t cos(4t − π / 2) that describes underdamped motion.
19. The characteristic equation 4r 2 + 20r + 169 = 0 has roots r = − 5 / 2 ± 6 i. When we
impose the initial conditions x(0) = 4, x′(0) = 16 on the general solution
x(t ) = e−5 t / 2 ( A cos 6t + B sin 6t ) we get the particular solution
x(t) = e-5t/2 [4 cos 6t + (13/3) sin 2t] ≈ (1/3) 313 e-5t/2 cos(6t - 0.8254)
that describes underdamped motion.
20. The characteristic equation 2r 2 + 16r + 40 = 0 has roots r = − 4 ± 2 i. When we impose
the initial conditions x(0) = 5, x′(0) = 4 on the general solution
x(t ) = e−4 t ( A cos 2t + B sin 4t ) we get the particular solution
x(t) = e-4t (5 cos 2t + 12 sin 2t) ≈ 13 e-4t cos(2t - 1.1760)
that describes underdamped motion.
21. The characteristic equation r 2 + 10r + 125 = 0 has roots r = − 5 ± 10 i. When we impose
the initial conditions x(0) = 6, x′(0) = 50 on the general solution
x(t ) = e−5 t ( A cos10t + B sin10t ) we get the particular solution
x(t) = e-5t (6 cos 10t + 8 sin 10t) ≈ 10 e-5t cos(10t - 0.9273)
that describes underdamped motion.
22. (a) With m = 12/32 = 3/8 slug, c = 3 lb-sec/ft, and k = 24 lb/ft, the differential
equation is equivalent to 3x″ + 24x′ + 192x = 0. The characteristic equation
3r 2 + 24r + 192 = 0 has roots r = − 4 ± 4 3 i. When we impose the initial conditions
( )
x(0) = 1, x′(0) = 0 on the general solution x(t ) = e−4 t A cos 4t 3 + B sin 4t 3 we get
the particular solution
x(t) = e-4t [cos 4t 3 + (1/ 3 )sin 4t 3 ]
= (2/ 3 )e-4t [( 3 /2)cos 4t 3 + (1/2)sin 4t 3 ]
x(t) = (2/ 3 )e-4t cos(4t 3 – π / 6 ).
5. (b) The time-varying amplitude is 2/ 3 ≈ 1.15 ft; the frequency is 4 3 ≈ 6.93
rad/sec; and the phase angle is π / 6 .
23. (a) With m = 100 slugs we get ω = k /100 . But we are given that
ω = (80 cycles/min)(2π)(1 min/60 sec) = 8π/3,
and equating the two values yields k ≈ 7018 lb/ft.
(b) With ω1 = 2π(78/60) sec-1, Equation (21) in the text yields c ≈ 372.31
lb/(ft/sec). Hence p = c/2m ≈ 1.8615. Finally e-pt = 0.01 gives t ≈ 2.47 sec.
30. In the underdamped case we have
x(t) = e-pt [A cos ω1t + B sin ω1t],
x′(t) = -pept [A cos ω1t + B sin ω1t] + e-pt [-Aω1sin ω1t + Bω1cos ω1t].
The conditions x(0) = x0, x′(0) = v0 yield the equations A = x0 and
-pA + Bω1 = v0, whence B = (v0 + px0)/ ω1.
31. The binomial series
α (α − 1) 2 α (α − 1)(α − 2) 3
(1 + x )
α
= 1+α x + x + x +
2! 3!
converges if x 1. (See, for instance, Section 11.8 of Edwards and Penney, Calculus
with Analytic Geometry, 5th edition, Prentice Hall, 1998.) With α = 1/ 2 and
x = − c 2 / 4mk in Eq. (21) of Section 5.4 in this text, the binomial series gives
k c2 k c2
ω1 = ω0 − p 2 =
2
− = 1−
m 4m 2 m 4 mk
k c2 c4 c2
= 1− − 2 2
− ≈ ω 0 1 − .
m 8mk 128m k 8mk
32. If x(t) = Ce-pt cos(ω1t - α) then
x′(t) = -pCe-pt cos(ω1t - α) + Cω1e-pt sin(ω1t - α) = 0
yields tan(ω1t - α) = -p/ ω1.
6. 33. If x1 = x(t1) and x2 = x(t2) are two successive local maxima, then ω1t2 = ω1t1 + 2π
so
x1 = C exp(-pt1) cos(ω1t1 - α),
x2 = C exp(-pt2) cos(ω1t2 - α) = C exp(-pt2) cos(ω1t1 - α).
Hence x1 /x2 = exp[-p(t1 - t2)], and therefore
ln(x1 /x2) = -p(t1 - t2) = 2πp/ ω1.
34. With t1 = 0.34 and t2 = 1.17 we first use the equation ω1t2 = ω1t1 + 2π from
Problem 32 to calculate ω1 = 2π/(0.83) ≈ 7.57 rad/sec. Next, with x1 = 6.73 and
x2 = 1.46, the result of Problem 33 yields
p = (1/0.83) ln(6.73/1.46) ≈ 1.84.
Then Equation (16) in this section gives
c = 2mp = 2(100/32)(1.84) ≈ 11.51 lb-sec/ft,
and finally Equation (21) yields
k = (4m2ω12 + c2)/4m ≈ 189.68 lb/ft.
35. The characteristic equation r 2 + 2r + 1 = 0 has roots r = − 1, − 1. When we impose the
initial conditions x(0) = 0, x′(1) = 0 on the general solution x(t ) = ( c1 + c2t ) e − t we get
the particular solution x1 (t ) = t e − t .
36. The characteristic equation r 2 + 2r + (1 − 10 −2 n ) = 0 has roots r = − 1 ± 10− n. When we
impose the initial conditions x(0) = 0, x′(1) = 0 on the general solution
( ) ( )
x(t ) = c1 exp −1 + 10− n t + c1 exp −1 − 10− n t
we get the equations
c1 + c2 = 0, (−1 + 10 ) c + (−1 − 10 ) c
−n
1
−n
2 = 1
with solution c1 = 2n −15n , c2 = 2 n −15n. This gives the particular solution
exp(10− n t ) − exp( −10− n t )
x2 (t ) = 10n e − t n −t −n
= 10 e sinh(10 t ).
2
7. 37. The characteristic equation r 2 + 2r + (1 + 10−2 n ) = 0 has roots r = − 1 ± 10− n i. When we
impose the initial conditions x(0) = 0, x′(1) = 0 on the general solution
( ) (
x(t ) = e − t A cos 10 − n t + B sin 10− n t
)
we get the equations c1 = 0, − c1 + 10− n c2 = 1 with solution c1 = 0, c2 = 10n. This
gives the particular solution x3 (t ) = 10n e− t sin(10− n t ).
sinh(10− n t )
38. lim x2 (t ) = lim 10 n e − t sinh(10 − n t ) = t e − t ⋅ lim −n
= t e − t and
n →∞ n →∞ n →∞ 10 t
sin(10− n t )
lim x3 (t ) = lim 10 n e − t sin(10− n t ) = t e − t ⋅ lim −n
= t e−t ,
n →∞ n →∞ n →∞ 10 t
using the fact that lim (sin θ ) / θ = lim (sinh θ ) / θ = 0 (by L'Hôpital's rule, for
θ →0 θ →0
instance).