Why aren't satellites disintegrated even though they orbit earth within earth's Roche Limits? I was wondering about the Roche limit and its effects on satellites.
Why aren't artificial satellites ripped apart by gravitational tidal forces of the earth?
I think it's due to the satellites being stronger than rocks?
Is this true?
Also, is the Roche limit just a line (very narrow band) around the planet or is it a range (broad cross sectional area) of distance around the planet?
 A: The Roche limit denotes how close a body held together by its own gravity can come. Since gravity tends to be the only thing holding moon-sized objects together, you won't find natural moons closer than the Roche limit. [Strictly speaking, the Roche Limit is a function of both the primary (in the case of this question, Earth) and the secondary (satellites) bodies; there is a different Roche limit for objects with different densities, but for simplicity I'll be treating the Roche Limit as being a function just of the primary.] For instance, Saturn's rings lie inside its Roche limit, and may be the debris from a satellite that was ripped apart. The rings are made up of small particles, and each particle is held together by molecular bonds. Since they have something other than gravity holding them together, they are not ripped apart any further. Similarly, an artificial satellite is also held together by molecular bonds, not internal gravity. 
The molecular-bonds-will-be-ripped-apart-by-tidal-forces limit is obviously much smaller than a satellite's orbit, as we, on the surface of the Earth, are even closer, and we are not ripped apart. You would have to have an extremely dense object, such as a neutron star or black hole, for that limit to exist. Being inside the Roche limit does mean that if an astronaut were to go on a space walk without a tether, tidal forces would pull them away from the larger satellite. Outside the Roche limit, the gravity of the larger satellite would pull the astronaut back (although not before the astronaut runs out of air).
If you look at the influence of the Moon's tides on Earth, you can see that the oceans are pulled towards the Moon, but the land is (relatively) stationary. The fact that tides are only a few meters shows that the Earth is well outside the Moon's Roche limit (and of course, the Earth's Roche limit is further out than the Moon's, so the Moon would reach the Earth's Roche limit long before the Earth reached the Moon's). If the Moon were to move towards the Earth, the tides would get higher and higher. The Moon's Roche limit is the point at which the tides would get so high that the water is ripped away from the Earth. The land would still survive slightly past that point, because the crust has some rigidity beyond mere gravitational attraction.
Regarding your second question: there is a region in which the tidal forces would be larger than internal gravitational attraction, and a region in which internal gravitational attraction would be larger than tidal forces. The Roche limit is the boundary between those two regions. Everything inside the Roche limit constitutes the former region, while everything outside the Roche limit constitutes the latter.
A: The Roche limit applies only to bodies which are held together purely by internal gravitational attraction. Compact objects such as artificial satellites are held together by the much stronger inter-molecular electromagnetic forces (this is another demonstration of just how weak gravity is compared to electromagnetism).
As for your second question: the Roche limit usually defined as the radius away from a body at which magnitude of the tidal forces exactly equal that of the internal gravitational attraction of the smaller body. Of course, the magnitude of the tidal forces becomes significant at further radii, and so the distance at which tidal forces become significant is a much broader area/range.
A: To add to other answers, also consider that artificial satellites are much smaller than natural satellites. This means that the difference between the gravitational force at the point the closest to the planet and at the point the furthest from the planet is much smaller in artificial satellites.
A: The Roche limit is a limit on objects being held together by their own gravity. Satellites are held together by much stronger forces. Different parts of the satellite are ultimately connected by chemical bonds, which are electromagnetic. 
A: When I was a kid I also wondered why artificial satellites within the Roche Limit were not pulled apart by tidal forces.
When I was a kid I also wondered, if any body within the Roche Limit would be pulled apart by tidal forces, and since the surface of the Earth is deep within the Roche limit, why aren't all objects on the surface of the Earth - including Human bodies - pulled apart by tidal forces.
Since my body was not being pulled apart by tidal forces the statement that all bodies within the Roche Limit were pulled apart by tidal forces must not be correct.  Therefore the simple statement that all bodies within the Roche Limit are pulled apart by tidal forces must be an oversimplification as stated.
But since such statements were made in non fiction sources it seemed probable that they were not totally false. Therefore I expected that sometime in the future I would read a fuller and more complex account of the Roche limit that would explain the seeming paradoxes.
And I did.  Eventually I learned that the Roche limit was not a single absolute distance but varied with the sizes, masses, and densities of the larger and the smaller objects.  I also learned that the Roche Limit only applied to objects that were held together only by their internal gravitational attraction and not to objects like artificial satellites or Human bodies.
Wondering why the Roche Limit didn't apply to my Human body was an example of using reductio ad absurdum to show that a statement was an oversimplification of a more complex situation.
A: 
Why aren't artificial satellites ripped apart by gravitational tidal forces of the earth?

In short, the pieces of a satellite are held together by chemical, molecular bonds, which are strong compared to the tidal forces that are weak for objects the size of artificial satellites and gravity sources the strength of the earth.
A tidal force is the difference in attraction between two distances from a gravitational source.  For a small object such as a natural satellite, that is just a few meters, gravity simply won't vary much between the nearest and farthest points unless you're talking about a orbiting a neutron star or black hole extremely closely.
For instance the ISS is 100m along its longest axis.  Say that axis is perpendicular to the earth's surface.  If its nearest point to earth is at 400km from the surface, the farthest point is therefore 400.1km.  But earth is 5371km radius, so the distance from the center (where the gravity "seems" to be coming from) is 5771km and 5771.1km.
Gravity falls off at 1/(distance squared), so the difference in gravity is (1/(5771^2)) / (1/(5771.1^2)).  That's a difference of 3*10^-8, or .000003% difference.
Gravity at earth's surface is 1G, giving 1kg mass 9.8N (newton) force (what you feel when you hold up 1kg on earth's surface).  At 400km altitude it'd be 9.8*5371/(5371+400))^2=8.4N .  So if you had even 1,000,000kg at each end of a 100m rope at that altitude, 1,000,000 * 8.4N * .000003% = .25N, about what you feel were you to pick up 25g of coins right now.  (About 5 nickels.)
Even a human hair is strong enough to hold 25g at the earth's surface, and further, satellites aren't that heavy, and are far stronger than a hair.
