Some time ago there was a large tide-power project in the Bay of Fundy, Nova Scotia, Canada. My understanding was that it worked very well, but was mostly a "capture the water at high tide, generate electricity at low tide (going out to sea) as well as high tide (coming in from sea)". I don't know what happened to that project. --Bob Mike W wrote: >this may be an interesting adition to the thread... >http://news.bbc.co.uk/1/hi/england/cornwall/3477639.stm > >On 8 Sep 2005 at 14:30, Gerhard Fiedler wrote: > > > >>Olin Lathrop wrote: >> >> >> >>>Gerhard Fiedler wrote: >>> >>> >>>>Not necessarily. It could be that the energy would get transformed from >>>>kinetic energy into other forms (heat?) anyway -- float or no float. Maybe >>>>the float just redirects a small part of the energy flow that goes from >>>>kinetic to thermal into electric instead; in that case, the float wouldn't >>>>introduce an additional slowing, but would cause a certain ever so slight >>>>cooling. >>>> >>>> >>>My point was where the energy was coming from in the first place. I say it >>>comes from the kinetic energy stored in the rotation of the planet. You >>>seemed to disagree so I wanted to hear where you think it does come from. >>> >>> >>No, I didn't really disagree with that... Maybe Howard? >> >> >> >>>But to address your comment above, you are saying that the energy in >>>moving the water up and down as tides gets dissipated anyway, therefore >>>directing it to make electricity doesn't remove any additional energy >>>from the source. I disagree with this also. My main argument is that >>>much of the energy is not dissipated, but returns to the system. It's >>>sortof like bouncing a mass at the end of a spring. Once you get it >>>going, it take relatively little power to sustain a large oscillation. >>>That's because little is being dissipated. The energy just gets sloshed >>>around between the spring and the mass. Only the little bit lost to friction >>>and air resistance must be replaced by the driving mechanism each cycle. >>> >>> >>If this is true, then I agree with you. >> >> >> >>>Certainly there is energy dissipated by the oceans as they rise and fall due >>>to tides, but most of it is stored and released as potential energy in the >>>height of the water column. Think of a planet that has a uniformly thick >>>ocean layer over a perfectly smooth solid core. The tides would be traveling >>>waves. They would loose a little energy in the internal friction of the >>>water due to viscocity, and some more in the friction with the ground, but >>>most of the energy would be transferred around the globe in a big wave. The >>>driving force is essentially in phase with the motion. >>> >>> >>Not sure how much the internal friction contributes. Any numbers? >> >> >> >>>Now think of a large float used to extract this energy into up/down >>>motion of a fixed mechanical system. If there is no force on the >>>mechanical system (the float just bobs in the water), then no energy is >>>extraced. To extract energy, there has to be a force in the direction >>>of motion. This means the float must be lagging the wave, causing a >>>phase shift in the wave itself. Once the wave is lagging its driving >>>force, the driving force must be imparting more energy to the wave. The >>>extra energy has to come from somewhere, which is the kinetic energy stored >>>in the earth's rotation long ago. >>> >>> >>Yes, I agreed already to the source of this energy being the kinetic energy of >>the rotation. The question is really whether the energy would be conserved as >>kinetic energy if the float wasn't there, or if it would get lost (as kinetic >>energy) anyway -- maybe at the coast line. It seems to me that there's quite a >>bit of kinetic energy that gets lost (as kinetic energy) at the coast lines... >> >>Gerhard >>-- >>http://www.piclist.com PIC/SX FAQ & list archive >>View/change your membership options at >>http://mailman.mit.edu/mailman/listinfo/piclist >> >> >> > > > > -- Note: To protect our network, attachments must be sent to attach@engineer.cotse.net . 1-866-263-5745 USA/Canada http://beam.to/azengineer -- http://www.piclist.com PIC/SX FAQ & list archive View/change your membership options at http://mailman.mit.edu/mailman/listinfo/piclist