Roland, I'll just address this one aspect of your questions: You ask:
"If I stay in the wet sand the GB should pretty much remain stable, correct? "
No. On the wet salt beach, the mineral content changes everywhere you walk. Particularly when you walk closer to, or further away, from the water's edge. This has to do with the moisture content (obviously getting moister the closer you go to the water's edge, and into the ebbing water), and also d/t the fact that as the sands are laid down by each day's tides (because sand is never "constant" on the ocean-facing beaches), that sand types are laid out differently on different parallels. For example: I've seen how sometimes black sand will be up at the edge of a cut, or in gully wash outlets. Yet when you walk away from those zones, the sand cleans up to less mineralized. This happens because of the washing out and laying down effect, as if the entire beach is a giant riffle board or sluice-box, so to speak. And the same is true even if it's not as pronounced as "black verses white" sand. It's subtle and even the mere rises and falls of elevation, slopes, scallop shapes, etc.... it's just changes all over the place on the wet salt.
About the most you can do to alleviate this, and stay in "approximately" the same GB zone, is if you walked at a parallel to the water, moving neither closer to, or further away, from the water's edge. Then assuming no other factors, like swail shapes in the sand, or entering and exiting low spots, etc... then theoretically, you might stay at the same GB range or so.