I had pretty much the same questions. There is a lot of answers to a lot of your questions on this website, but you do have to poke around to find it. I will give you what I know - if any of it is wrong, I am sure someone will be along to correct me.
Your RS&B has two transducers (measuring devices), one measures “infrasound”, that is, sound below the normal hearing range of humans. That is the HDF channel data. The other is the seismometer transducer, it measures movement in the vertical direction (the ‘Z’ axis), that is the EHZ channel data.
Both of these are sampled 100 times per second, the “count” data you see is the raw numbers from each of these. The device has some calibration data that can be downloaded. When you look at the data on the DataView web page that has used the calibration data to convert the count data to units appropriate to what is being measured (Air pressure for the infrasound channel, and micro-meters per second acceleration for the ground movement). In many ways, the units displayed are not very important for casual use. The graphs are the same, only the labeling changes.
For most things, the infrasound and accelerometer readings are independent, they are different things. However, there are some things that get picked up by both. The most common one you will probably see is a helicopter passing overhead. As you would expect, these usually give a very strong signal on the HDF channel. But most often, you will also see them register on the EHZ channe - yes, you were right in thinking that when one flys over your house, that it shakes the ground - it does!.
Look at the frequency graph of a helicopter pass, and you will see a quite distinctive ‘S’ curve, which is the doppler effect as it approaches and leaves. You can use the frequencies to determine the speed, if that is of interest to you.
If your location is like most, when you look at 24h of data, you will probably see a big difference between night and day. Look at the HDF data when there is a storm, or just wind blowing, and it will likely look very jagged as it picks up the air pressure differences caused by the wind gusts. It can also pick up remote thunder storms, windmills, and if you are lucky, and look carefully meteors passing overhead.
If you see an earthquake, it will probably have two signals separated by anything from a few seconds to minutes, depending on how far away it is. Those are the P and S waves. The P wave travels across the surface of the earth and arrives first (it is faster). The S wave travels through the earth, taking a longer route, and is slower. Knowing (roughly) the speed of each, you can use the gap between them to calculate how far away the earthquake was. Plot that as a circle on a map, then look at the same data on a different seismograph, same calculation but because it is likely a different distance away, the circle will be a different size and of course, a different origin when plotted. Use a third and where the three circles intersect is the location. Use more data from devices further around the earth, plot in 3-D and you get the depth of the event. Of course, computers do all the hard work for you, and you see the data on the StationView web page - your device is contributing to detection and locating those earthquakes.
Depending on how deep you want to get into P and S waves, there are some good articles available with a Google search.