A home computer is a powerful tool, but it must start data reliably to work well, otherwise it's kind of pointless, isn't it? Let's look inside and see how it stores data. Look at that, it's marvelous. It's an ordinary hard drive, but it's details, of course, are extraordinary. Now I'm sure you know the essence of a hard drive. We store data on it in binary form, ones and zeros. Now this arm supports a head, which is an electromagnet that scans over the disk, and either writes data by changing the magnetization of specific sections on the platter, or it just reads the data by measuring the magnetic polarization. Now, an impregnable, pretty simple, but in practice, a lot of hardcore engineering. The key focus lies in being sure that the head can precisely, error-free, read and write to the disk. The first order of business is to move it with great control. The position, the arm, engineers use a voice coil actuator. The base of the arm sits between two powerful magnets. They're so strong, they're actually kind of hard to pull apart. There. The arm moves because of a Lorentz force. It has a current through a wire that's in a magnetic field, and the wire experiences a force. Reverse the current and the force also reverses. As current flows in one direction in the coil, the force created by the permanent magnet makes the arm move this way. Reverse the current and it moves back. The force of the arm is directly proportional to the current through the coil, which allows the arm's position to be finely tuned. Unlike a mechanical system of linkages, there is minimal wear, and it isn't sensitive to temperature. At the end of the arm lies the most critical component, the head. At its simplest, it's a piece of ferromagnetic material wrapped with wire. As it passes over the magnetized sections of the platter, it measures changes in the direction of the magnetic poles, we call Faraday's Law. A change in magnetization produces a voltage in a nearby coil. So as the head passes a section where the polarity has changed, it records a voltage spike. The spikes, both negative and positive, represent a one. And where there is no voltage spike, corresponds to a zero. The head gets astonishingly close to the disc surface, 100 nanometers and older drives, but today under 10 nanometers and the newest ones. As the head gets closer to the disc, its magnetic field covers less area, allowing for more sectors of information to be packed onto the disc surface. To keep that critical height, engineers using an ingenious method, they float the head over the disc. You see, as the disc spins, it forms a boundary layer there that gets dragged past the stationary head at 80 miles per hour at the outer edge. The head rides on a slider aerodynamically designed to float above the platter. And the genius of this air bearing technology is itself induced adjustment. If any disturbance causes the slider to rise too high, it floats back to where it should be. Now, because the head is so close to the disc surface, any straight particles could damage the disc, resulting in data loss. So engineers place this recirculating filter in the airflow, yet remove small particles scraped off the platter. To keep the head flying at the right height, the platter is made incredibly smooth. Typically, this platter is so smooth that it has a surface roughness of about 1 nanometer. To give you an idea of how smooth that is, let's imagine that this section is enlarged and tells as long as a football field, American or international. The average bump on the surface would be about 300-7 inch. The key element of the platter is the magnetic layer, which is cobalt with perhaps platinum and nickel mixed in. Now this mixture of metals has high corcivity, which means that it will maintain that magnetization and thus data, until it's exposed to another powerful magnetic field. One last thing that I find enormously clever, using a bit of math to squeeze up to 40% more information on the disc. Consider this sequence of magnetic poles on the disc surface, 0-1-0-1-1-1. A scan by the head would reveal these distinct voltage spikes, both positive and negative for the ones. We would be easily able to distinguish it from, say, this similar sequence. We compare them, they clearly differ. Engineers, though, always work to get more and more data onto a hard drive. One way to do this is to shrink the magnetic domains, but look what happens to the voltage spikes when we do this. For each sequence, the spikes of the ones now overlap and superimpose giving fuzzy signals. In fact, the two sequences now look very similar. Using a technique called partial response, maximum likelihood, engineers have developed sophisticated codes that can take a murky signal like this, generate the possible sequences that could make it up, and then choose the most probable. As with any successful technology, these hard drives remain unnoticed in our daily lives and unless something goes wrong. I'm Bill Hammock, the engineer guy.