Q: When we use tidal forces to generate energy, that energy has to come from somewhere. Doing this, does it mean that the Earth slowly escapes the sun's attraction since we use the sun's gravity as an energy source? - Anonymous

That's an interesting question. The tides do have effects on orbits, but not quite what you'd guess. For starters, the tides on earth are mostly from the moon, not the sun. Your idea about tidal friction draining energy from other forms is completely correct, however.
So let's start with the effects of the moon tides. The facts are that the moon is moving away from the earth at about 3.8 cm per year and that the earth's days are getting longer at about 2 milliseconds per century. The earth's orbit around the sun changes by only a negligible amount.

These lunar tides mainly can drain energy from two sources:
1. the rotational energies of the earth and (to a much smaller extent ) the moon
2. the orbital energy of the moon.

One effect is to slow the earth's rotation, gradually making days longer. That's what's happening, and that's where energy is actually being drained from.

The other effect is less obvious. Draining energy from the moon's orbit would actually cause the moon to speed up while pulling it in closer to the earth. The reason is that in a gravitational orbit like that, the change in potential energy is twice as big and opposite in sign to the change in kinetic energy. So speeding up and moving in closer is the way to losenet energy.

Adding energy to the moon's orbit actually slows its orbital speed a bit while increasing its distance to the earth and adding gravitational potential energy. Since the moon is actually moving farther away and slowing down, its gaining orbital energy. How can that be? Although the tides cause a net energy drain to heat, they're also transferring some of the energy drained from the earth's rotation to the moon's orbit. It turns out that this must happen in order for the angular momentum lost as the earth's spin slows to go somewhere. Angular momentum goes up as the distance grows.

These two effects will continue until the moon-tides stop, when the moon orbits the earth in one day.  The earth will have slowed its rotation down to the point where the same side always faces the moon.

You can see an example of something just like that. The moon rotates just fast enough to always show the same face to the earth. Tidal friction caused that.

The end result will be that both the earth's and moon's rotational speed (length of day) as well as the lunar month will be equal, about 47 of our current days.  This will happen far, far in the future, several billions of years from now.

Sun tides would produce similar effects, but not as large. They also tend to make the days longer.

There are some nice  articles on this:

COMMON COLLECTOR CONFIGURATION OF A TRANSISTOR

COMMON COLLECTOR CONNECTION

In  this  configuration  the  input  is  applied  between the  base  and  the  collector and  the  output  is  taken  from  the  collector  and  the  emitter.  Here  the  collector  is common to both the input and the output circuits as shown in Fig.

Common Collector Transistor Circuit

In  common  collector  configuration  the  input  current  is  the  base current  IB  and  the output current is the emitter current IE. The ratio of change in emitter current to the  change in the base current is called current amplification factor.

It is represented by

COMMON COLLECTOR CIRCUIT

A test  circuit  for determining the  static characteristic  of an NPN transistor is shown in Fig. In this circuit the collector is common to both the input and the output circuits.   To   measure   the   base   and   the   emitter   currents,   milli   ammeters   are connected in series with the base and the emitter circuits. Voltmeters are connected   across the input an…