Heavy salting of Albritten’s roads to melt winter ice and snow began about 20 years ago.
Conclusion
Continuing the salting of Albritten's roads at its present rate will render Albritten's groundwater unpalatable within the next few decades.
Evidence (since)
Salting Albritten's roads began 20 years ago. The groundwater now contains ~100mg of salt / Liter.
By comparison, in a less highly urbanized area where traffic patterns resemble Albritten of 20 years ago, the groundwater contains 10mg of salt / Liter.
Water that contains 250 or more mg of salt / Liter tastes unacceptably salty.
Evaluate
The author is presenting an Asymmetric Comparison (i.e. a Curious Fact) and making a causal assumption about it, so we can activate our Explain Curious Fact mindset.
Curious Fact ... how come A's groundwater is 100mg / L whereas the groundwater in this other area where salt isn't used much is only 10mg / L?
Author's Explanation ... the heavy salting of A's roads has increased its groundwater to 100mg.
We could weaken this argument by posing an Alternate Explanation for the 100 vs. 10 difference (maybe Albritten has more factories whose byproducts salt into the groundwater), or by attacking the plausibility of the idea that heavily salting the roads eventually adds salt to the groundwater.
But this argument also contains a prediction. The author is thinking that our current salting rate will get us from 100mg / L to 250mg / L in the new few decades.
The author is thinking,
We could hurt the argument by trying to throw a wrench into this prediction. Maybe the way salting roads contributes to salty groundwater isn't linear like that. Maybe at a certain point, salt clogs up the ground in such a way that additional salt doesn't leech down into the groundwater at as fast a rate (i.e. so maybe we'll eventually get to 250mg, but not in the next few decades).