Bryan Mumford ng1@............ Sent: Sat, 12 Mar 2011 17:23 Subject: RE: clock pendulums I've seen earthquakes stop my clock pendulums. Presumably this is=20 ecause they shifted the ground in the direction the pendulum was=20 A clock at 90 degrees to the one that stalled kept running. swingingThe quake in Japan was too far away to have such an effect, but I'm= =20 hinking about the kind of motion the earthquake is likely to deliver=20 rom so far away. Will it be an up and down motion? Is this a difference between P and S waves? Would it be a vertical P=20 ave from Japan, and a lateral S wave from a closer quake that might=20 tall a clock pendulum? Hi Bryan, P waves give a vertical displacement at right angles to the direction o= f propagation. Distant quakes are likely to have a=20 P frequency of about 1 Hz, but for local quakes it may be up to 10 Hz. Thes= e are the fastest waves and the first that you receive. =20 he S waves are lateral transverse waves which move horizontally, at right a= ngles to their direction of propagation. They have about half=20 velocity and frequency of P waves. Distant quakes may have a frequency of 0= ..5 Hz, but local quakes can be up to 5 Hz. You can download a free Seismogram manual with all the information that you= are likely to need from http://psn.quake.net/info/analsis.pdf=20 =20 Thinking about it carefully, I would expect a pendulum clock to be most s= ensitive to vertical waves. The rise and fall of the pendulum=20 is very small, say 1.3 thou" for a 1m device, whereas the sideways deflecti= on may be over a couple of inches. Whether the pendulum action=20 is effected or even stops, depends on the phase and the frequency of the in= comomg wave. The P and S waves are usually only a few cycles=20 long at most, not a train of waves. Regards, Chris Chapman =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 =20 Am I correct in assuming that your clocks use a vertical pendulum with a= period between 1 and 2 seconds?=20 ryan Mumford= Bryan Mumford ng1@............
Sent: Sat, 12 Mar 2011 17:23
Subject: RE: clock pendulums
I've s= een earthquakes stop my clock pendulums. Presumably this is=20 because they shifted the ground in the direction the = pendulum was=20 .. A clock at 90 degrees to the one that stalled kept running. swingingThe quake in Japan was too far away to have such an = effect, but I'm=20 thinking about the kind of motion the earthquake is <= FONT size=3D2>likely to deliver=20 from so far away. Will it be an up and down motion? Is this a difference between P and S waves? Would it = be a vertical P=20 wave from Japan, and a lateral S wave from a closer quake that might=20 stall a clock pendulum? Hi Bryan,P waves give a vertical displacement at right angles to= the direction of propagation. Distant quakes are likely to have a =P frequency of = about 1 Hz, but for local quakes it may be up to 10 Hz.These are the fastest waves and the first that you receive. The S waves are lateral transverse waves which move horizont= ally, at right angles to their direction of propagation. They have about ha= lfveloc= ity and frequency of P waves. Distant quakes may have a frequency of 0.5 Hz= , but local quakes can be up to 5 Hz.You can download a free Seismogram manual with= all the information that you are likely to need from http://psn.quake.net/info/analsis.pdf== TT> Thinking about it carefully, I would expect a pend= ulum clock to be most sensitive to vertical waves. The rise and fall of the= pendulum= is very small, say 1.3 thou" for a 1m = device, whereas the sideways deflection may be over a couple of inches. Whe= ther the pendulum actionis effected or even stops, depends on the pha= se and the frequency of the incomomg wave. The P and S waves are usually on= ly a few cyclesl= ong at most, not a train of waves.Regards,Chris Chapman = = = Am I correct in assuming that your clocks use a vertical pendulum with a p= eriod between 1 and 2 seconds? Bryan Mumford