STiCM
Select / Special Topics in Classical Mechanics
P. C. Deshmukh
Department of Physics Indian Institute of Technology Madras Chennai 600036
STiCM Lecture 15:
Unit 5 : Non-Inertial Frame of Reference Real effects of pseudo-forces!
PCD_STiCM 1 Unit 5: Inertial and non-inertial reference frames.
Moving coordinate systems. Pseudo forces. Inertial and non-inertial reference frames.
Deterministic cause-effect relations in inertial frame, and their modifications in a non-inertial frame.
Real Effects of Pseudo Forces!
Gaspard Gustave de Coriolis PCD_STiCM Six Flags over Georgia 1792 - 1843 2 Learning goals:
Understand “Newton’s laws hold only in an inertial frame”.
Distinction between an inertial and a non-inertial frame is linked to what we consider as a fundamental physical force/interaction.
Electromagnetic/electroweak, nuclear, gravity) / pseudo-force (centrifugal, Coriolis etc.) / Friction
We shall learn to interpret the ‘real effects of pseudo-forces’ in terms of Newtonian method. Re-activate ‘causality’ in non- inertial frame of reference!
PCD_STiCM 3 Deterministic cause-effect relation in inertial frame,
and its adaptation in a non-inertial frame!
PCD_STiCM 4 The law of inertia enables us recognize an inertial frame of reference as one in which motion is self-sustaining, determined entirely by initial conditions alone.
PCD_STiCM 5 Just where is the inertial frame? Newton envisaged the inertial frame to be located in deep space, amidst distant stars. PCD_STiCM 6 Kabhi kabhi mere dil mein, Khayaal aata hein….. Tu ab se pahile, sitaron mein bas rahi thi kahin,
Tujhe jamin pe, bulaya gaya hei mere liye….
PCD_STiCM 7 Galilean relativity Time t is the same in the red frame and in the blue frame. rt() Y I rt'( ) r(t) rt'( ) utc F constant OI X I dr dr' OIc O' u t Y’ uc ZI F’ dt dt X’ O’ First derivative 2 2 d r d r ' Z’ with respect to time is different! 2 2 dt dt So what? Remember Galileo? Second derivative with respect to time
is, however, very muchPCD_STiCM the same! 8 Galilean relativity d 2 r d 2 r ' rt() dt 2 dt 2
YI rt'( ) F constant ‘Acceleration’, which O I XI measures departure OIc O' u t Y’ from ‘equilibrium’ is ZI F’ X’ essentially the same a a ' Z’ O’ in the two frames of F ma ma'' F reference. Essentially the same ‘cause’ explains the ‘effect’ (acceleration) according to the same ‘principle of causality’.
Laws of Mechanics : same inPCD_STiCM all INERTIAL FRAMES. 9 Galilean relativity F ma ma'' F • A frame of reference moving with respect to an inertial frame of reference at constant velocity is also an inertial frame.
• The same force F ma explains the linear response (effect/acceleration is linearly proportional to the cause/interaction) relationship in all inertial frames.
PCD_STiCM 10 Galileo’s experiments that led him to the law of inertia.
Galileo Galilee 1564 - 1642
I Law
F ma Linear Response. Effect is proportional to the Cause Principle of causality. II Law PCD_STiCM 11 F ma Linear Response
W mg
Weight = Mass acceleration due to gravity
PCD_STiCM 12 Lunatic exercise! Is lifting a cow easier on the Moon ?
PCD_STiCM 13 Another lunatic exercise! Is it easier to stop a charging bull on the Moon ?
Ian Usmovets Stopping an Angry Bull (1849)
Evgraf Semenovich Sorokin (born as Kostroma Province) 1821-1892. PCD_STiCM Russian artist and teacher, a master of historical, religious and genre paintings. 14 What do we mean by a CAUSE ?
CAUSE is that physical agency which generates an EFFECT !
EFFECT: departure from equilibrium
CAUSE: ‘forCE’ ‘intErACtion’
fundamental interaction
Electromagnetic, gravitational nuclear weak/strong PCD_STiCM 15 Galilean relativity F ma ma'' F
• A frame of reference moving with respect to an inertial frame of reference at constant velocity is also an inertial frame. • The same force F ma explains the linear response (effect/acceleration is linearly proportional to the cause/interaction) relationship in all inertial frames. • “An inertial frame is one in which Newton’s laws hold” PCD_STiCM 16 Galilean relativity Time t is the same in the red frame and in the green, double-primed frame. Physics in an accelerated frame of reference.
What happens to the (Cause, Effect) relationship?
What happens to the Principle of Causality / Determinism? PCD_STiCM 17 constant acceleration f . rt() rt"( ) r( t ) OO " r ''( t ) Y
F 1 2 O X r( t ) ui t f t r ''( t ) 1 OO'' u t f t 2 2 Z i 2 Y’’ f :constant F” X’’ O’’ Z’’ Galilean relativity dd 1 r( t ) ui f 2 t r ''( t ) dt 2 dt d d d d r( t ) f + r ''( t ) dt dt dt dt aa " PCD_STiCM 18 Galilean relativity d d d d r( t ) r ''( t ) f dt dt dt dt rt() Y rt''( ) F aa " O X 1 OO'' v t f t 2 Z 2 Y’’ F” a a" f X’’ a" a f O’’ Z’’ ma" ma mf
F" ma m f FFF pseudo
‘Real’/’Physical’ force/interaction PCD_STiCM 19 Galilean relativity F"" ma ma mf rt() rt''( ) Y FFF F pseudo O X 1 2 OO'' ui t f t 2 Y’’ Z F” X’’ Z’’ O’’
Same cause-effect relationship
does not explain the dynamics.
PCD_STiCM 20 Galilean relativity FFF pseudo rt() rt''( ) Y The force/interaction
F which explained the O X acceleration in the Y’’ inertial frame does Z F” 1 OO'' u t f t 2 not account for the i 2 X’’ Z’’ O’’ acceleration in the accelerated frame of not Laws of Mechanics are the same reference. in a FRAME OF REFERENCE that is accelerated with respect to an inertial frame.
PCD_STiCM 21 Galilean relativity Time t is the same in the FFF pseudo red frame and in the green, double-primed frame. ma"
FFF" real/ physical pseudo
Real effects of pseudo-forces!
P. Chaitanya Das, G. Srinivasa Murthy, Gopal Pandurangan and P.C. Deshmukh Resonance, Vol. 9, Number 6, 74-85 (2004) http://www.ias.ac.in/resonance/June2004/pdf/June2004Classroom1.pdf
PCD_STiCM 22 Deterministic / cause-effect / relation holds only in an inertial frame of reference.
This relation inspires in our minds an intuitive perception of a fundamental interaction / force (EM, Gravity, Nuclear strong/weak).
Adaptation of causality in a non-inertial frame requires ‘inventing’ interactions that do not exist. – for these ‘fictitious forces’, Newton’s laws are of course not designed to work!PCD_STiCM 23 Galilean relativity: Time t is the same in all frames of references.
RELATED ISSUES:
Weightlessness
What is Einstein’s weight in an elevator accelerated upward/downward?
Sergei Bubka (Ukrainian: Сергій Бубка) (born December 4, 1963) is a retired Ukrainian pole vaulter. He represented the Soviet Union before its dissolution in 1991. He is widely regarded as the best pole vaulter ever. Reference: http://www.bookrags.com/Sergei_Bubka PCD_STiCM 24 http://www.stabhoch.com/bildserien/20030825_Isinbajeva_465/bildreihe.html What enables the pole vaulting champion, Yelena Isinbayeva, twist her body in flight and clear great heights? PCD_STiCM 2008 Olympics champion: 5.05meters25 We will take a Break… …… Any questions ? [email protected]
Non-Inertial Frame of Reference Next L16 : ‘cause’, where there isn’t one!
Real effectsPCD_STiCM of pseudo -forces! 26 STiCM
Select / Special Topics in Classical Mechanics
P. C. Deshmukh
Department of Physics Indian Institute of Technology Madras Chennai 600036
STiCM Lecture 16: Unit 5 Non-Inertial Frame of Reference ‘cause’, where there isn’t one! Real effects of pseudo-forces! PCD_STiCM 27 PCD_STiCM 28 PCD_STiCM 29 http://www.lerc.nasa.gov/WWW/K-12/airplane/state.html
What will be the shape of a tiny little amount of a liquid in a closed (sealed) beaker when this ‘liquid-in-a-beaker’ system is (a) on earth
(b) orbiting in a satellitePCD_STiCM around the earth. 30 In a liquid the molecular forces are weaker than in a solid.
A liquid takes the shape of its container with a free surface in a gravitational field.
Regardless of gravity, a liquid has a fixed volume.
Other than GRAVITY, are there other interactions that could influence the shape of the liquid’s free surface?
Intra/Inter molecular forces provide the concave or the convex meniscus to the liquid. These interactions become dramatically consequential in microgravity. PCD_STiCM 31 The actual shape an amount of liquid will take in a closed container in microgravity depends on whether the adhesive, or the cohesive, forces are strong.
Accordingly, the liquid may form a floating ball inside, or stick to the inner walls of the container and leave a cavity inside!
PCD_STiCM 32 You can have zero- gravity experience by booking your zero-gravity flight!
http://www.gozerog.com/
Flight ticket (one adult) : little over $5k
PCD_STiCM 33 http://www.grc.nasa.gov/WWW/RT/RT1996/6000/ 6726f.htm http://science.nasa.gov/headlines/y2000/ast12ma y_1.htm 29/09/09
On Earth, gravity-driven buoyant convection causes a candle flame to In microgravity, where be teardrop-shaped and convective flows are carries soot to the flame's absent, the flame is spherical, soot-free, and tip, making it yellow. PCD_STiCM blue. 34 “Microgravity” ? mm G 12 r 2
There is no ‘insulation’ from gravity!
PCD_STiCM 35 Galilean relativity
Observations in a rotating frame of reference.
PCD_STiCM 36 ZI Galilean relativity C Time t is the same in both the frames
ZR
P The green axis OC
YR is some arbitrary FI O axis about which YI OI FR is rotating. OR
FR XI XR Clearly, the coordinates/components of the point P in the inertial frame of reference are different from those in the rotating frame of reference. PCD_STiCM 37 We shall ignore translational motion of the new frame relative to the inertial frame FI.
We have already considered that.
We can always superpose the two (translational and rotating) motions.
PCD_STiCM 38 Z Galilean relativity I C ZR
P
YR F Y O I I O R First, we consider the position FR XI vector of a particle at rest in the X R rotating frame.
Clearly, its time-derivative in the rotating frame is zero, but not so in the inertial frame. dd dt IR dt PCD_STiCM 39 Circle of radius bsin nˆ
d
b
dd bb dt RI dt
The particle seen at bt() ‘rest’ in the rotating frame would appear to have moved to a new location as seen by an b() t dt observer in FI. PCD_STiCM 40 Galilean relativity Time t is the same in the red frame and in the purple, rotating, frame.
NOTE! The time-derivative is different in the rotating frame.
dd dt dt IR
PCD_STiCM 41 Often, one uses the term
‘SPACE-FIXED FRAME OF REFERENCE’ for FI, and ‘BODY-FIXED FRAME OF REFERENCE’ for FR.
We shall develop our analysis for an arbitrary vector b , the only condition being that it is itself not a time- derivative in the rotating frame of some another vector.
d No vector q exists such that q b dt R d b 0 in the rotating frame FR . dt R d Question: What is b ? PCD_STiCM dt I 42 db bt( dt ) bt ( ) | dbu | ˆ nˆ nˆ bˆ bsin where uˆ . nbˆ ˆ (,)nbˆ ˆ d b db db ( b sin )( d )
nbˆ ˆ db (bd sin )( ) nbˆ ˆ db These two terms are equal and hence cancel. b() t dt db d nˆ b bt() db dt b d d since nˆ bb dt PCD_STiCMdt I 43 Remember! The vector b itself did d bb not have any time-dependence in dt I the rotating frame.
If b has a time dependence in the rotating frame, the following operator equivalence would follow:
dd b b b dt IR dt
Operator dd Equivalence: dt IR dt PCD_STiCM 44 d d dd r r r dt I dt R dt IR dt Operating twice: dd d d r rr dt I dt I dt R dt R d rr dt R d22 d d d 22 r r r r dt IR dt dt R dt R r Multiplying by mass ‘m’, we shall get quantities that have dimensionsPCD_STiCM of ‘force’. 45 d22 d d d m22 r m r m r 2 m r dt dt dt dt RI R R m r
d FRI F F 2 m r m r dt R
‘Leap second’ term ‘Coriolis force’ ‘Centrifugal force’ Gaspard Gustave de Coriolis term 1792 - 1843 PCD_STiCM 46 We will take a Break… …… Any questions ? [email protected]
Next L17 : Coriolis Deflection Foucault Pendulum Cyclonic storm’s direction Real Effects of Pseudo-forces! d FRI F F 2 m r m r dt R
PCD_STiCM 47 STiCM
Select / Special Topics in Classical Mechanics
P. C. Deshmukh
Department of Physics Indian Institute of Technology Madras Chennai 600036
STiCM Lecture 17: Unit 5 Non-Inertial Frame of Reference ‘cause’, when there really isn’t one! Real Effects of Pseudo-forces!
PCD_STiCM 48 ‘force’ / ‘fundamental interaction’ in the inertial frame d22 d d d m22 r m r m r 2 m r dt dt dt dt RI R R m r Pseudoforce in the rotating frame Real Effects of Pseudoforces !
d FRI F F 2 m r m r dt R
‘Coriolis force’ ‘Centrifugal force’ ‘Leap second’ term PCD_STiCM 49 Why are Leap Seconds Used?
The time taken by the earth to do one rotation differs from day to day and from year to year. The Earth was slower than atomic clocks by 0.16 seconds in 2005; by 0.30 seconds in 2006; by 0.31 seconds in 2007; and by 0.32 seconds in 2008.
It was only 0.02 seconds slower in 2001.
PCD_STiCM http://www.timeanddate.com/time/leapseconds.html ; 14th October, 2009 50 The atomic clocks can be reset to add an extra second, known as the leap second, to synchronize the atomic clocks with the Earth's observed rotation.
The most accurate and stable time comes from atomic clocks but for navigation and astronomy purposes, but it is the atomic time that is synchronized with the Earth’s rotation.
PCD_STiCM 51 ‘Leap second’ term
The International Earth Rotation and Reference System Service (IERS) decides when to introduce a leap second in UTC (Coordinated Universal Time).
On one average day, the difference between atomic clocks and Earth's rotation is around 0.002 seconds, or around 1 second every 1.5 years. IERS announced on July 4, 2008, that a leap second would be added at 23:59:60 (or near midnight) UTC on December 31, 2008. This was the 24th leap second to be added since the first leap second was added in 1972.
PCD_STiCM http://www.timeanddate.com/time/leapseconds.html ; 14th October, 2009 52 Let us consider 3 ‘definitions’ of the ‘vertical’
[1] ‘vertical’ is defined by the radial line from the center of the earth to a point on the earth’s surface
[2] ‘vertical’ is defined by a ‘plumb line’ suspended at the point under consideration.
[3] ‘vertical’ is defined by the space curve along which a chalk PCD_STiCM falls, if you let it go! 53 3 ‘definitions’ of the ‘vertical’
d22 d d d m22 r m r m r 2 m r dt dt dt dt RI R R m r PCD_STiCM 54 7.2921159 × 10−5 radians per second
d mr dt R
d22 d d d m22 r m r m r 2 m r dt dt dt dt RI R R m r PCD_STiCM http://commons.wikimedia.org/wiki/File:Globespin.gif 55 Earth and moon seen from MARS
First image of Earth & Moon, ever taken from another planet, from Mars, by MGS, on 8 May 2003 at 13:00 GMT.
MARS GLOBAL SURVEYOR http://mars8.jpl.nasa.gov/mgs/ http://space.about.com/od/pictures/ig/Earth-Pictures-Gallery/Earth-and-Moon-as- PCD_STiCM viewed-from-.htm 56 The moon is attracted toward the earth due to their mutual gravitational attraction. attraction Will there be an eventual collision?
If so, when? If not, why not? PCD_STiCM 57 [1] When travelling in a car/bus, you experience what you call as a ‘centrifugal force’. Which physical agency exerts it ? Is there a corresponding force of reaction?
[2] How does a centrifuge work ?
[3] Do the centripetal and the centrifugal forces constitute an ‘action - reaction’ pair of Newton’s 3rd law?
PCD_STiCM 58 The plane of oscillation of the Foucault pendulum is seen to rotate due to the Coriolis effect. The plane rotates through one full rotation in 24 hours at poles, and in ~33.94 hours at a “ Foo-Koh” latitude of 450 (Latitude of Paris is ~490).
d FRI F F 2 m r m r dt R ‘Leap second’ term ‘Coriolis force’ ‘Centrifugal force’
PCD_STiCM 59 Gaspard Gustave de Coriolis 1792 - 1843 Jean Bernard Léon Foucault PCD_STiCM 1819 - 1868 60 dd22 m22 r m r dt RI dt
d We often ignore mr dt the ‘leap R second’ and the d 2mr centrifugal term. dt R m r
Pseudo Forces PCD_STiCM 61 2 Fcentrifugal m r m reˆ e ˆ e ˆ r 22 m reˆ sin e ˆ m r sin e ˆ eeˆˆ z v eˆ r
0.100 at latitude of 45
eeˆˆz v (along 'local vertical')
PCD_STiCM 62 at North Pole 2 0 at Equator goes to at South Pole 2
Terrestrial equatorial radius is 6378 km.
Polar radius is 6357PCD_STiCM km. 63 d FCoriolis 2 m r eˆy e ˆ y e ˆ z e ˆ z dt R
eeˆˆz v eˆ r
eˆy eˆx e ˆ East e ˆ y e ˆ z at North Pole 2 0 at Equator
eeˆˆz v ('local vertical')
eeˆˆy North
,,eeˆˆNorth PCD_STiCM y e ˆx e ˆ East e ˆ y e ˆ z 64 d FCoriolis 2 m r eˆy e ˆ y e ˆ z e ˆ z dt R
eeˆˆz v ('local vertical') ,,eeˆˆNorth y eeˆˆy North ˆ ˆ ˆ ˆ ex e East e y e z at North Pole 2 0 at Equator eˆy goes to at South Pole 2
eeˆˆz v
cos is + in both N- and S- hemispheres PCD_STiCM 65 d F 2 m r Coriolis eˆy e ˆ y e ˆ z e ˆ z dt R
Coriolis deflection of an d revR v R ( ˆ z ) object in ‘free’ ‘fall’ at a dt R point on earth’s surface:
F 2 m eˆ e ˆ e ˆ e ˆ v ( e ˆ ) Coriolis y y z z R z
2m eˆy e ˆ x 2 m cos e ˆ East 0 (N hemisphere)Coriolis deflection: toward 2 East in both the Northern & 0 (S hemisphere ) the Southern Hemispheres 2 cos PCD_STiCMis + in both N- and S-hemispheres 66 Western North Pacific
Coriolis 1792 - 1843
d FCoriolis 2 m r eˆy e ˆ y e ˆ z e ˆ z dt R
Western South Pacific PCD_STiCM http://agora.ex.nii.ac.jp/digital-typhoon/start_som_wnp.html.en 67 http://www.youtube.com/watch?v=ZvLYrZ3vgio&NR=1
This Nanyuki tourist attraction is not due to Coriolis effect
PCD_STiCM 68 PCD_STiCM 69 Rotating 2 Astronauts in a Space Ship R = 10m B Y = 0.15 rad/sec v = (0,5) m/sec
X Real Effects of Pseudo A Forces
Please read the paperPCD_STiCM at the following internet weblink: http://www.physics.iitm.ac.in/~labs/amp/homepage/dasandmurthy.htm 70 Force = Rate of change of momentum What interaction is making the instantaneous momentum change? R = 10m Very fundamental question!! = 0.95 rad/sec v = (-10.0325,2.755) m/s The answer
P. Chaitanya Das, G. determines Srinivasa Murthy, our notion of Gopal Pandurangan and P.C. Deshmukh a 'The real effects of ‘fundamental pseudo-forces', Resonance, Vol. interaction’ 9, Number 6, 74- 85(2004)
(http://www.ias.ac.in/resonance/June2004/pdf/June2004Classroom1.pdf)PCD_STiCM 71 What will be the effect on rockets?
‘Missile Woman of India’ Dr. Tessy Thomas
th On ICBMs? PCD_STiCM17 May, 2010 AGNI II 72 http://daphne.palomar.edu/pdeen/Animations/34_Coriolis.swf
(eˆz ) ( e ˆ y ) e ˆ x (West)
d FCoriolis 2 m r dt R
eˆy e ˆ y e ˆ z e ˆ z
PCD_STiCM Distance at equator: ~111 Kms. per longitude degree 73 We will take a Break… …… Any questions ? [email protected]
Next L18 : Coriolis Deflection Foucault Pendulum Real Effects of Pseudo-forces!
d FRI F F 2 m r m r dt R
PCD_STiCM 74 STiCM
Select / Special Topics in Classical Mechanics
P. C. Deshmukh
Department of Physics Indian Institute of Technology Madras Chennai 600036
STiCM Lecture 18: Unit 5 ‘EFFECT’, when there isn’t a cause! ‘CAUSE’, when there really isn’t one! Real Effects of Pseudo-forces! Foucault Pendulum PCD_STiCM 75 d FRI F F 2 m r m r dt R Physical Finland Oceanography Sweden of the Baltic Sea Matti Leppäranta, Kai Myrberg Springer-Praxis (2009)
Denmark Circulating current in the Baltic Germany sea (1969?) Poland PCD_STiCM 76 eˆy e ˆ y e ˆ z e ˆ z
d 2mr dt R
Calculate Coriolis deflection of a plane flying from Srinagar to Kolkata to Mumbai ? Thiruvananthapuram ? Plane speed: 3550 kms 850 kms/hr Plane speed:
PCD_STiCM 850 kms/hr 77 Coriolis effect Electronics engineers? – only for Physicists? Computer science engineers? Aerospace engineers? Ocean Engineering?
PCD_STiCM Any navigation system on earth….. GPS in cellphones! 78 Use a Cartesian coordinate system with reference to a point on the earth’s surface.
ˆ ˆ ˆ Choose e x ,, e y e z such that e ˆ z is along the local
‘up/vertical’ direction (which is not along eˆ r due to the centrifugal term).
However, eˆˆzr is very nearly the same as e
Choose such that it is orthogonal to , and points eˆy toward the North-pole seen from the point on the earth’s surface under consideration.
Finally, choose e ˆ x e ˆ y e ˆ z , which will give us the direction of the local ‘East’ at that point. PCD_STiCM 79 d FCoriolis 2 m r eˆy e ˆ y e ˆ z e ˆ z dt R eeˆˆ ,,eeˆˆNorth y z v eˆ at N Pole r 2 eˆy 0 at Equator eˆx e ˆ East e ˆ y e ˆ z at S Pole 2
eeˆˆz v ('local vertical')
eeˆˆy North
PCD_STiCMe ˆx e ˆ East e ˆ y e ˆ z 80 Caution! We use a mix of three coordinate systems!
1. A cartesian coordinate system as defined in the previous slide.
2. A spherical polar coordinate system whose ‘polar’ angle is defined with respect to the axis of the earth’s rotation rather than with respect to the cartesian z-axis which is oriented along the local ‘vertical’.
3. Cylindrical polar coordinate system whose radial unit vector is along the radial outward direction with reference to the earth’s axis of rotation.
PCD_STiCM 81 Just follow the 6 steps indicated in the next slide, exactly in the order given!
PCD_STiCM 82 Earth’s eˆv Choose eˆˆz ev rotation axis eˆr eˆx e ˆ y e ˆ z
eeˆˆvv ertical eeˆˆy North eˆEast eeˆˆ 2 h horizontal Fcf F cf eˆ ˆ e Fg
eˆh The1. Note‘vertical’ earth’s is axis not of rotation.along the radial line, nor 2. Recognize that Note that: ˆ along3. Recognize the axis that of earth’s rotation!Fg F cf e h 0 eeˆˆvr . (,)eeˆˆ 4. Choose eeˆˆz v. h 5. Choose eeˆˆy North , pointing toward North. PCD_STiCM ˆ ˆ ˆ ˆ 6. Now, eˆx e ˆ y e ˆ z e ˆ East ey e y e z e z 83 d FRI F F 2 m r - m r dt R
eˆy e ˆ y e ˆ z e ˆ z
d Velocity of the object in ˆ ˆ ˆ r vx ex +v y e y v z e z ROTATING FRAME dt R
eˆy eˆz :latitude
FCoriolis 2 m eˆ e ˆ e ˆ e ˆ v e ˆ +v e ˆ v e ˆ y y z zx x y y z z PCD_STiCM 84 Coriolis ˆ ˆ ˆ ˆ ˆ F 2 m cos ey sin e z vx e x + v y e y v z e z
ma 2 m cos v sin v eˆ sin v e ˆ ( cos v ) e ˆ Coriolis z y x x y x z
eˆy eˆz :latitude
PCD_STiCM 85 Pendulum at the N pole
How will the plane of oscillation of the HowThe will observerthe plane is of at the N pendulum oscillationpole. of the pendulum look to an look to an observer at the observer at N pole, but standing the N pole? disconnected with the earth?
PCD_STiCM 86
How will the plane of oscillation of the HowThe will observerthe plane is of at the S pendulum oscillationpole. of the pendulum look to an look to an observer at the observer at N pole, but standing the S pole? disconnected with the earth?
PCD_STiCM Pendulum at the S pole 87 What if the pendulum is at an intermediate latitude?
How will the plane of oscillation of the How will the plane of pendulum oscillation of the pendulum look to an look to an observer at the observer at N pole, but standing that latitude? disconnected with the earth?
PCD_STiCM 88 Northern edge of Northern the floor of the edge of room is closer to the floor the earth’s axis than moves the Southern edge. eastward slower than the Southern edge.
W.B.Somerville Q.Jl. Royal Astronomical Soc.
PCD_STiCM (1972) 13 40-62 89 http://www.youtube.com/watch?v=nB2SXLYwKkM
video compilation of a Foucault pendulum in action at the Houston Museum of Natural Science.
PCD_STiCM 90 Foucault Pendulum eˆy e ˆ y e ˆ z e ˆ z
d FRI F F 2 m r - m r dt R d mrR mg S F 2 m r - m r dt R S Suˆ
S eˆx()()() e ˆ x S e ˆ y e ˆ y S e ˆ z e ˆ z S S ˆ ˆ ˆ ˆ ˆ ˆ ˆ ˆ ˆ SSeeux()()() x eeu y y eeu z z mg ˆ ˆ ˆ S S excos e y cos e z cos PCD_STiCM 91 d Foucault Pendulum mrR mg S 2 m r dt R ma 2 m cos v sin v eˆ sin v e ˆ ( cos v ) e ˆ Coriolis z y x x y x z ˆ ˆ ˆ S S excos e y cos e z cos neglect z xy, motion:
mx Scos 2 m cos z sin y S my Scos 2 m sin x
mg S mg mx mgcos 2 m sin y
myPCD_STiCM mgcos 2 m sin x 92 d Foucault Pendulum mrR mg S 2 m r dt R
S Suˆ neglect z S mg mx mgcos 2 m sin y my mgcos 2 m sin x xgcos 2sin y S ygcos 2sin x sin mg xgcos 2 y ygcos 2 x PCD_STiCM 93 xg cos 2 y Coupled differential ygcos 2 x equations
Solve by transforming to new coordinates x’,y’ such that x x'cos t y 'sin t y x'sin t y 'cos t
x x'sin t y 'cos t y x'cos t y 'sin t 2 x gcos 2 x 'cos t y 'sin t y gcos 2 2 x 'sin t y 'cos t PCD_STiCM 94 2 x gcos 2 x 'cos t y 'sin t 2 y gcos 2 x 'sin t y 'cos t
22 xcos t g cos cos t 2 x 'cos t y 'sin t cos t 22 ysin t g cos sin t 2 x 'sin t y 'cos t sin t
22 xtytgcos sin cos cos t 2 x 'cos tytt 'sin cos 22 gcos sin t 2 x 'sin t y 'cos t sin t
PCD_STiCM 95 22 xtytgcos sin cos cos t 2 x 'cos tytt 'sin cos 22 gcos sin t 2 x 'sin t y 'cos t sin t
Dropping terms in 2 x gcoscos t y g cos sin t 0
xgcos 0 ygcos 0
PCD_STiCM 96 d mrR mg S 2 m r sin dt R
Direction cosines of S are: x xgcos 0 cos l ygcos 0 y cos l zl cos x l xg0 l y yg0 Two-dimensional linear l harmonic oscillator PCD_STiCM 97 d Foucault Pendulum mrR mg S 2 m r dt R Dropping terms in 2 x gcos cos t y g cos sin t 0
xy x g 0; y g 0 ll
S In the earth’s rotating frame, the path is that of an ellipse. mg
PCD_STiCM 98 d Foucault Pendulum mrR mg S 2 m r dt R Dropping terms in 2 x gcos cos t y g cos sin t 0 xy x g 0; y g 0 ll The ellipse would precess at an angular S speed sin A number of approximations made!
mg Detailed analysis is rather involved! The “plane” would in fact be a “curved surface”. PCD_STiCM 99 d Foucault Pendulum mrR mg S 2 m r dt R
The ellipse would precess at an angular speed sin :latitude
Time Period for the rotation of the “plane” of oscillation of the Foucault S Pendulum 1 2 2 T mg f sin 2 24 hours PCD_STiCM2 sin sin 100 Famous Foucault Pendulum: - at the Pantheon in Paris, France.
http://www.animations.physics.unsw.edu.a u/jw/foucault_pendulum.html
http://www.youtube.com/watch?v=vVg5P6f rHzY&feature=related
PCD_STiCM 101 sin
0 2 4 4 2
1 2 2 T f sin 2 24 hours 2 sin sin PCD_STiCM 102 Philosophical questions: What is ‘force’ ? Mass/ Inertial frame? Gravity?
Sir Isaac Newton Ernst Mach (1838–1916) 1643 - 1727 Albert Einstein From a portrait by 1879 – 1955 Enoch Seeman in 1726 Newton: Gravity is the result of an attractive interaction between objects having mass. Curvature of Space-Time, Geometry / Dynamics of MatterPCD_STiCM / General Theory of Relativity 103 We will take a Break… …… Any questions ? [email protected]
• In the next Unit, we shall consider Lorentz Transformations
and Einstein’s
Special Theory of Relativity.
• c: finite!
Next, Unit 6: Special Theory of Relativity
PCD_STiCM 104