About that discussion on energy from tidal energy systems. There are tidal effects, primarily from our orbiting moon. And there are waves, primarily from meteorology. And, just to avoid any word play, there are tidal waves, from geology.
If you dammed up a section of ocean shore and installed hydroelectric generators on the dam, you could tap energy from the tides. Where I live, the difference between low and high tide is roughly 3 meters.
But will this actually slow the Earth's spin?
I posed this question to Google:
"Will tidal effects eventually lock the earth to face the moon?"
Citing two youtube sources and
what appear to be course notes from the University of Rochester, it claimed this might happen in 50 billion years. The article cited only estimated "billions of year".
The reason it said "might" is because the evolution of our Sun might interrupt this process.
Even so, this does not actually answer the question. What your shoreline dam is actually doing is providing the tides with an inelastic collision with the energy converted to electricity. Without that dam, the tide would still have come in and struck the beach. If the beach is elastic, all you have done is directed the available energy to electricity instead of heat. To the extent that the beach is inelastic, some of that tidal power would be reflected back out to sea and eventually converted to heat. So, if your dam provides a more inelastic collision than was there before, and that reflected power somehow diminished the total amount of tidal power absorbed by the Earth, then you could claim that your dam is slowing the Earth's spin.
Getting back to
@jedishrfu 's concern about the "devastating effects" of slowing the Earth's spin:
1) It's not certain that tidal energy stations (such as the ones in France and South Korea) actually slow the Earth's spin in comparison to the shoreline they replace.
2) If they do slow it down, it would be a very minor contribution to Earth's conversion of tidal power to heat that occurs along all ocean shoreline, many sea beds, and even to the viscosity of seawater.
3) Although this could be characterized as "kicking this can down the road", it is a very small can and a very long and hazardous road. If in billions of years there are people left to "worry about it", a slower spin may be to their advantage.