Sum your comments about removing 300,000 tons of salt a year got me to thinking.
One of my college professors in mechanical engineering always stressed the concept of doing some ball park calculations to get a idea of the magnitude of the problem before you worried about a detailed answer. (this was when you did calculations on a slide rule so you better have a good idea how big the final answer should be or you could easily be off by a factor of 10 or 100 on the slide rule)
With that in mind I did some ball park calculations assuming that all that salt came off the top crust of the salt here is what the ball park calculations say:
300,000 tons of salt /year = 21205732500 cubic inches per year
That would be a cube of salt 2767.9 inches on a side or 230 ft per side cube comes off the flats each year.
If you assume that is being extracted from a salt crust of 36 square miles:
That would remove about 0.1467 inches of salt each year.
Since in 66 years of extraction ( ie since the first salt flat meets were held in 1949) at current production rates they would have extracted about 9.68 inches of salt across an area of 36 square miles.
Not saying that is an exact value only a representative back of the envelope calculation of the probable impact of the mining at current rates with no salt replacement. If that is ball park, since 2006 when I first started doing photography out on the salt it likely lost an equivalent of about 1.3 inches of thickness.
In fairness that did not all come from the surface, but it had to come from the volume of the salt so the entire basin of 36 miles would have dropped 1.3 inches as that salt got pulled away. If the water table did not change then the local water table in the basin is now 1.3 inches higher in relation to the surface than it was just 9 years ago.
Maybe the top salt crust is nearly the same as it was in 2006 but due to the higher water table it would be more difficult for it to fully dry in the summer months. The basin is a fixed sized bowl, you take stuff out the top MUST sink (its that old conservation of mass thing).
We are not talking about just changes in the salt crust (top hard cemented halite crust) but the entire salt deposit and its relationship to the normal water table in the basin. We not only need to monitor the thickness of that top hard salt crust but the relationship it has to the local brine pool water table.
It has crossed my mind that by moving the salt as brine they may be raising the local water table (they are taking brine from deep wells not just the surface brine pool). Although they might be transferring lots of salt they could also be raising the water table which would be counter productive to the objective or restoring a hard surface salt deposit to preserve the historic use of the salt flats as a racing surface.
About that dry salt laydown project