The claims are yours, Tony. As I told you several months ago, the very first thing you should have done was to determine whether the available data are good enough to detect the jolt you think is missing.
They weren't. Had you taken a moment to consider the Nyquist rate for your alleged 90ms jolt, or performed a forward error analysis as described in chapter 1 of R W Hamming's
Numerical Methods for Scientists and Engineers, then you'd have known better than to go public with your argument. Estimating the Nyquist rate should have taken you about two seconds; if your math skills are rusty, then the forward error analysis might have taken you a couple of minutes.
Your argument divides into two main parts:
- The upper block fell so cleanly onto the lower block that one would expect one large, clear jolt instead of a near-continuous cascade of lesser jolts.
- Observations show there was no jolt.
Your own data showed an apparent jolt, and it was gob-smackingly obvious that your data weren't good enough to rule out the possibility of other unobserved jolts. That's why we've been discussing your spectacular failure to establish the second point.
Note well, however, that you haven't established the first point either. I expect to see less than 1g acceleration (as in the data) but I do not expect to see a single jolt that's large enough to show up in the best possible analysis of the available data. Yes, I understand how there could be such a jolt; I also understand how there might not be such a jolt. I therefore have no reason to care about the second part of your argument:
It doesn't matter whether the downward acceleration was relatively smooth or was punctuated by large jolts.
Because I understand that it doesn't matter, there is no reason for me to take better measurements. If you persist in your two-part argument, however, then you will need far better data to support the second part of your argument, and you will also need a far more convincing argument for the first part as well.