
Originally Posted by
riser4
The average Joe doesn't think about water rights here in the rural northeast because in a lot of places, we have too much water. Until we don't. The current drought map for New England that was posted in that other thread was interesting, alarming, and illuminating.

Originally Posted by
abraham
That and the water laws are completely different.
I have often said that the "water wars" that everyone assumes are coming out West are actually going to happen in the East. While of course it is drier in the West, we have an entirely different set of water laws because of that reality. Our entire legal regime is premised on the notion that there isn't enough water, we know who gets what as the system gets drier.
In the East, the legal regime in place exists because of abundant water. But due to climate change, we are sure to see droughts and not enough water in some places, sometime. And there are no rules for how that works, who gets what. Anarchy.

Originally Posted by
Falcon3
I’d say aquifer recharge from residential use is practically nil. In most western places if you dig down two feet in the middle of watering season, you’ll still find bone dry soil (true here in Spokane and we’re certainly not the desert SW). So water that is put on the lawn and absorbed into the first few inches of soil will generally go into the grass or evaporate over time. Actually it’ll pretty much all evaporate because that’s what’s happening to your green grass too.
And water that goes through the water treatment plant (most runoff and all sewer) probably gets dumped into the river and goes away, not recharging the aquifer.
For your first paragraph, isn't that what I said? That generally, there is no recharge from lawn watering, it's all consumptive, or if overwatered, surface runoff.
As to your second paragraph, while true, it's probably not helpful to think of "aquifer" versus "stream", because in most places they are the same thing, it's just that the surface stream moves faster. Most places there is no "aquifer" to "recharge" that is separate from the surface stream, it is all a question of timing, i.e. when the water hits the stream.
There are some places where underground aquifers exist that are entirely or mostly separate from surface streams (like the Ogallala) but those are the exceptions rather than the rule.
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