lycoflyfisher wrote:
Karst systems are incredibly complex, and even after intensive studies there are often not clear answers on how local or regional hydrology truly works.
The situation there is not really complicated, and has been thoroughly studied there and at other quarries.
Here is a brief summary.
When a limestone quarry first begins, they are removing limestone near the surface so they are above the ground water level, so they are working in dry conditions, and no pumping is needed.
As they dig down lower, they eventually reach the ground water level, so water seeps into the quarry pit.
To continue quarrying deeper, they start pumping water, to lower the ground water level to keep the bottom of the quarry pit dry. The pumped water is released into the stream.
Some of these quarries eventually go down very deep, so the groundwater table is pumped down much deeper than its normal level.
The springs that had once fed the stream then dry up, because the groundwater table is now far below the elevation of the springs.
Now the stream is dependent on pumping to maintain base flow. If the pumps shut off for some reason, the stream goes dry. That being the case, it's imperative that the pumped supply of water is not interrupted. They should have backup systems to make sure of this.
That is the current situation and it's been that way for many years.
Someone brought up the question of what would happen if the quarry closed.
If the quarry closed and simply turned off the pumps permanently, what would happen at first is that the stream would go dry.
With no pumping taking place, the groundwater level would rise, eventually reaching its ordinary elevation. Then the groundwater would once again flow out of the springs, feeding the stream as in the pre-quarry days.
But when a quarry that is pumping down the groundwater is closed, the temporary drying out of the stream could be avoided. They could continue running the pumps after the quarry is closed down during a transition period. They could adjust the amount of water being pumped to maintain the base flow of the stream, while allowing the ground water to rise back up to its normal elevation.
If there any groundwater hydrologists in the house, they could probably give a better explanation. I gave a layman's explanation. But as I said, it's not very complicated.