I think a lot of people who are not members of that forum, do not want to become members of that forum, and do not want to wade through the whole discussion would greatly appreciate a summary.
Sorry John, I thought visitors could see the thread without having to become members. But quickly ...
VPM hypothesizes a distribution of bubble seed sizes that are present at the start of a dive. For illustration, let's say a diver has bubble seed sizes {0.55, 0.63, 0.67, 0.71, 0.83, 1.03, 1.4, 1.8 }. The "critical radius" setting in VPM promises to prohibit bubbles
at the critical radius size and smaller from initiating growth during the diver's ascent to the surface. Bubble's of greater size are allowed to grow, but since you can change the critical radius it shouldn't be a problem. If that part of the bubble distribution starts to become a problem, just stop them from growing by increasing the critical radius size. So the critical radius is the primary VPM parameter that attempts to manage the total volume a bubble growth.
So, for example, a critical radius of 0.71 would not allow bubbles {0.55, 0.63, 0.67, 0.71} to grow. The others would experience supersaturation pressures that could initiate growth, but by adjusting the critical radius you hope to control the total volume of bubbles (free gas). You can find MUCH more technical descriptions, but for our purposes that's the gist of it
Ross defines the critical radius in his software by defining + values. For example, VPM-B+3 corresponds to a critical radius that is larger (i.e. should prohibit larger bubbles from growing), than VPM-B+1. That's why it is thought to be more conservative. As you increase the critical radius size you should be cutting off more and more of the hypothesized bubble distribution from initiating growth. And larger critical radii imply lengthening deco times.
Those objecting to VPM-B+7 seem to be saying VPM can effectively limit growth of only part of the hypothesized bubble distribution. In other words, VPM only works up to a point (usually defined by Ross as his VPM-B+5
which of course is completely arbitrary). That admission is extremely odd if you're trying to defend VPM which is why I was so stunned they were even attempting to make the argument.
The reason he didn't want to admit VPM-B+7 is a valid VPM profile is because it is VERY
similar (not identical) to the A2 deeper stop profile tested by the NEDU (which is part of what the deep stops thread showed). The A2 profile was considerably more risky than the A1 shallower stop profile that was also tested. And, it turns out, the A1 profile was very similar to GF 53/53. So we have actual dive trials showing, at least for that case, that a GF profile would likely have performed considerably better than one generated by VPM-B
not a comfortable outcome for deep stop proponents.
But, it's all
here for the reading, and a good presentation from Dr. Doolette
is here.