What you describe about the ph affecting the correction factor, is new information to me and probably to all the other Zeo users of this salt. It makes me a bit worried, and maybe I will switch to a different salt.
IMO, the single most important factor that allows so many hobbyists to maintain nice reef aquaria is the fact that many aquarium organisms are very forgiving of conditions, and do not require an exact match to their natural environment. That doesn't mean we should not strive for it, but most reefers fail it in some way, and still often have nice tanks.
There are many chemical complexities that most reefers gloss over without ever knowing there was more to it. That is certainly OK for most reefers if the belief is that highly exact parameters are not necessary. And in most cases, the majority of reefers have shown that to be true.
There are so many of these that it almost boggles the mind of those who sometimes are reminded of them all. They range from salinity complexities (improper calibration and temperature correction of every method used by reefers, etc.) to test kits that respond to more ions than what they are intended for. When the few hard core folks here have threads on them, most RC members, even those brave enough to post in the chemistry forum, usually tune out.
Alkalinity is certainly right up there in complexity that folks simply ignore. So if you have found a highly sensitive situation or organism, it might be useful to delve into these complexities to support the ways that you choose to deal with the sensitivity. Correction factors, for example, might need to be much more elaborate than simple borate corrections, and I'll show why below.
Let's start by assuming that you are correct that you need to maintain a narrow range of total alkalinity.
Right off we are faced with a dilemma. It is certainly not possible for a coral to sense total alkalinity. Bear with me. Total alkalinity is not a "thing" in the water. Total alkalinity is only a number that reflects how much acid is necessary to drive the pH down to a very low level; about pH 4.2 for normal seawater, as I show here:
What is Alkalinity
http://www.advancedaquarist.com/2002/2/chemistry
Since corals are not believed to be able to do such a titration, or even the biochemical equivalent somehow, what they must be responding to is something in the water that makes up total alkalinity.
These possible "things" that they might respond to are part of the definition of total alkalinity in seawater:
TA = [HCO3-] + 2[CO3--] + [B(OH)4-] + [OH-] + [Si(OH)3O-] + [MgOH+] + [HPO4--] + 2[PO4---] - [H+]
In order to try to understand what your corals might be responding to, we can probably toss out many of them because they are such minor contributors that you would not have noticed a correlation with total alkalinity. The ones I'd initially toss out are the forms of phosphate, magnesium hydroxide ion, hydrogen ion, silicate ions, and hydroxide ion.
That leaves borate, carbonate, and bicarbonate.
let's suppose the answer is not directly borate, as you presumably would have noticed the Seachem salt to be bad even with the correction as it has several fold higher borate than other mixes at the same pH and total alkalinity.
So that leaves carbonate and bicarbonate, and brings me to my main point: a simple measure of total alkalinity DOES NOT ACCOUNT FOR THESE IF YOU IGNORE PH.
The problem with using total alkalinity as a measure of either bicarbonate or carbonate is that it does not really tell you how much of either is there unless you know the pH. The graph below shows how the relative portion of these two ions changes with pH:
In particular, for a given total alkalinity, the amount of bicarbonate drops from pH 7.8 to pH 8.5. Likewise, the amount of carbonate rises over this range.
Bicarbonate drops by a factor of 1.4, from 2.2 meq/L (6.3 dKH) to 1.6 meq/L (4.4 dKH).
Carbonate rises by a factor of 3.7, from 0.11 meq/L (0.22 meq/L contribution to total alkalinity; 0.6 dKH) to 0.39 meq/L (0.78 meq/L contribution to alkalinity, or 2.2 dKH).
In summary, my assertion is that what is important to a coral can only be something actually in the water, and that total alkalinity cannot perfectly serve that function if exquisite accuracy is necessary and no correction is made for pH.
if the thing that is important is bicarbonate, then you might consider adjusting for it.
If carbonate is important, you might consider adjusting for it.
It would be easy to make a table of both corrections as a function of pH.
Both of these corrections are equal to or larger than than the narrow range that you detail as necessary based on total alkalinity.