Deeper well drilling an unsustainable stopgap to groundwater depletion
nature.com
nature.com
The part I remember the most and what intrigued me is when he was talking about ground water supply. He said that it would be unwise to keep digging into ground water supply for fresh water, for agriculture or otherwise, and what we really needed desperately was a nation-wide grid (I live in the USA, for reference) of pipes similar to how oil gets pumped for hundreds or in some cases thousands of miles, to supply desalinated water from the coasts to every part of america and to use properly use desalinated water to re-hydrate American rivers and wells, otherwise we will find ourselves in a situation of hastening a cycle of pumping ground water at an unfeasible pace, which to me is suggested in this article.
Seems relevant now, and I imagine the long term sustainability of such a thing would be much higher (and less depleting).
Looks like that guy was right. I wonder how many people have been sounding this alarm over the last decade.
But if water is artificially cheap, there will be no incentive.
But will we learn to tax water and write everyone a cheque to cover the cost of a basic user?
Just start with gray water re-use: nothing fancy: just a 55gal drum that collects the good gray water and discards anything looking spoiled. Pumps to toilet bowl with cheap pump.
Yes, probably needs some disinfection, but should vastly reduce the filtration load.
Any realistic solution to water scarcity will be a multi-pronged approach: improvements in water infrastructure, groundwater recharge, pollution control, water conservation, rainwater harvesting, and technology-driven gains in purification/distribution efficiency.
I guess we could cap either per person use or cap the pop in L.A.
Top users of California's allocation of Colorado River water are [1]:
- the Irrigation Districts of the Imperial Valley (~61%) and its northwest extension the Coachella Valley (~8%);
- the Metropolitan Water District of Southern California (~20%) [2];
- the Palo Verde Irrigation District (~8%). The Palo Verde Irrigation District is inside the Colorado River basin.
[1] https://www.usbr.gov/lc/region/g4000/4200Rpts/DecreeRpt/2018... [2] http://www.mwdh2o.com/AboutYourWater/Sources%20Of%20Supply/P...
West of 100 west longitude (so, half of the continental US), almost nowhere receives sufficient rainfall.
We live near the westmost tip of the US and have a water management plan for the entire county. We pay into a mitigation that manages the entire watershed.
> We live near the westmost tip of the US and have a water management plan for the entire county. We pay into a mitigation that manages the entire watershed.
I live on the east coast and can't get fined for collecting rainwater. There might be something to the notion of piping water from the "wet" coast to the Midwest and potentially beyond.
I still think the general idea is sound, even if you don't take it literally on implementation
Just to address that for the sake of that dude, I didn't want it to come across the wrong way.
To address some things further down:
I do remember a specific detail, and I don't know how accurate it is, however, he did explain that (and also prefaced how theoretical it is, even at that time more so I imagine):
- If you wanted to do this right, what you would want to do is desalinate the water and pump it to existing surface basins/reservoirs first (e.g., the Colorado River Basin), and taking great care to match that water to the ecology (e.g., mineral, PH level etc) of the water you are replenishing This way you aren't forcing an entire set of infrastructure to be obsolete, but rather working with existing delivery modes to get the water where it needs to be
- In cases where this isn't feasible, your best bet would be to run some sort of infrastructure (likely pipes) to those in need. In some cases, you might even be able to simply create new reservoirs to feed population centers to create efficient delivery mechanisms. The other thing I remember him mentioning specifically is there are many delivery mechanisms (e.g natural) ones that were no longer in productive service that could be revived also (I wish I had an example for this, but I don't).
The cheapest way to do this (by the dudes estimation) would be to use nuclear power near the coasts, that rely on the salt water for cooling which gives you two advantages:
1. in theory, the water that the plants themselves could produce a by product of clean, usable water[0]
2. The nuclear power plants themselves should be able to produce the power cheaply and ecologically friendly)[1]
3. This would incentive more research into pressurized water systems for nuclear power, which in theory could yield smaller reactors which in turn are even safer as is intrinsic to their design, they may even yield ever smaller sized reactors[2][3]
[0]https://www.sciencedaily.com/releases/2011/05/110512082949.h... [1]http://sitn.hms.harvard.edu/flash/2016/reconsidering-risks-n... [2]http://large.stanford.edu/courses/2017/ph241/kraus1/ [3]https://www.nrc.gov/reading-rm/basic-ref/students/for-educat...
Its, in a practical sense, feasible, but I think the takeaway I had back then and even now, thinking about it, was we needed to start this by 2009 to have it be up and going by 2019. Which isn't to say that we shouldn't do something now, but rather, we're still deciding what to do about it and that's crippling
That’s part of the problem with the various nut milks: it’s not just that they use a huge amount of water, but that unlike cows you have to grow them in specific environments - like the middle of the CA desert.
And we don't really have a unified grid of oil pipelines either.
~61% Imperial Irrigation District;
~20% Metropolitan Water District of Southern California;
~8% Palo Verde Irrigation District;
~8% Coachella Valley Water District;
Out of these, only the Palo Verde Irrigation District is inside the Colorado River basin. The Metropolitan Water District of Southern California has access to the coastline, so it can mix in desalinated water directly. It currently mixes in local water sources and water delivered from Northern California [2].
The Imperial and Coachella valleys require an interbasin transfer in either case, but despite the presence of canals and pipelines from the lower Colorado River to these sites, supplying them with additional water from the coast would require significantly less infrastructure than pumping said coastal water all the way up to Lake Mead.
[1] https://www.usbr.gov/lc/region/g4000/4200Rpts/DecreeRpt/2018... [2] http://www.mwdh2o.com/AboutYourWater/Sources%20Of%20Supply/P...
But as an overall plan, it's not so nuts (except for the energy cost, and the hundreds of miles of aqueducts that need to be built). The point about the upper states getting water out of this is a valid one, and Lake Mead supplies Arizona as well as California.
One downside to this plan: You'd kill the Grand Canyon.
It's much better to have mandatory water-conserving farming practices, like covering the soil to prevent evaporation. Or even better, underground water-dripping systems, like they do in Israel and other desert-like places.
Or even even better, start switching to airponics.
https://mavensnotebook.com/wp-content/uploads/2015/03/Graham...
Theodolite to measure the surrounding hills?, how can you be sure those hills aren't subsiding? Compare to other hills?
https://www.xyht.com/surveying/subsidence/
"As a point of clarification, the sign Dr. Poland is holding says this is the change detected in BM S661. However, according to the NGS datasheet for that bench mark (PID GU0103), it was not set until 1942. I have been told by reliable sources at the USGS that the pre-1942 subsidence, back to 1925, was a linear estimate. "
This appears to be the data sheet for the bench mark used.
https://www.ngs.noaa.gov/cgi-bin/ds_mark.prl?PidBox=GU0103
Here is a recent analysis from 2018 regarding that area, the photo, and the data used.
http://www.itrc.org/papers/pdf/subsidence.pdf
Which seems to conclude that the photo is possibly very wrong, they include a new updated photo at the bottom that only goes back as far as there is reliable data.
It's also hella cheaper to move the produced food than the water needed to grow them.
Currently, desalinated water is used in the US only in urban/suburban areas where homeowners are willing and able to pay a bit more than usual for their existing water use.
Maybe they (we) should be paying for the externalities of their 'free' water?
(1) The current system in the West is rights based. First person to make productive use of water gets the right to use that water forever. It's an odd system, but it's basically land-ownership for water resources. It's easy to see the flaws in the system.
(2) You have to invent a new system. It's a fun thought exercise, but there are a lot of things to consider. The environment needs water. Should a farm making productive use of water have to pay as much per unit as an urban household using it to water a lawn? Lot's of considerations. Now that you've done that, you have to get the law changes across the entire West. The entrenched interests will lobby energetically against the change. The people who would benefit probably aren't paying enough attention to care. So the change loses.
I don't think you need to change ownership of the water, a tax to cover the externalities would suffice. But I agree, it would probably never happen.
[1] https://www.newsdeeply.com/water/community/2018/06/21/the-tw...
Not everywhere. Western Kansas has water conservation districts with terraces plowed into fields. One of the reasons that reservoirs and ponds were low for so long.
This year, they are all full, due to the massive rainfall we've had.
The Great Lakes are at record high levels this year, causing flooding and sandy beaches on the lake shores to simply disappear under water.
https://www.lre.usace.army.mil/Missions/Great-Lakes-Informat...
The St. Lawrence river discharges approx. 16,800 m^3 a second of freshwater from the Great Lakes. However re-diverting the water to areas outside the watershed are would require an international compact between the U.S. and Canada and the various sovereign Indian territories to allow for it to happen.
https://www.azcentral.com/story/news/local/arizona-environme...
> The study was published Monday in the journal Nature Sustainability. The authors didn’t examine causes behind the drilling of deeper wells but said factors can include declining water levels, improving pump technologies, different permit requirements for wells that tap deep aquifers and poor water quality in shallow aquifers.
We should really take a look at how that stuff and nitrates from fertilizer are getting down there in the first place. Either our model of aquifers is wrong in very important ways or existing wells are getting backwash problems (eg, ground water following the outside of the bore down, or negative pressure when the pump is off pulling water in through defects in the pipes)
I'd like to see someone with better geography skills repeat that experiment.
"Pumped Dry: The Global Crisis of Vanishing Groundwater" https://www.youtube.com/watch?v=RjsThobgq7Q
https://en.wikipedia.org/wiki/GRACE_and_GRACE-FO#Oceanograph...
https://www.jpl.nasa.gov/news/news.php?feature=4626
Besides in situ wells, other helpful measurement techniques are InSAR (interferometric SAR) and post-processed GPS. Both let you measure surface subsidence to better than 1cm accuracy over broad areas, mostly due to groundwater withdrawals. This subsidence (which is in the multi-meter range in parts of CA, https://www.usgs.gov/centers/ca-water-ls) is of concern in and of itself, due to disruption of infrastructure like highways and pipelines caused by subsidence.
But, subsidence is indirect as a measurement of groundwater withdrawals, because you don't know the relationship between height lost at the surface and volume withdrawn underneath. This depends on a compaction parameter which is very hard to know.
Property owners can stymie the use of wells as a groundwater monitoring tool, because it is often not in their direct interest to supply information about local groundwater depletion. For this and other reasons, it's rather hard to use well data, even in well-instrumented areas like California.
https://groundwaterwatch.usgs.gov/default.asp
With some obvious large gaps. There are more collected by state agencies, consultants, etc. In most places there are probably more wells than you'd think.
In addition to measuring gravity from space to monitor groundwater it can be measured at the land surface, with better spatial resolution and worse accuracy. A 1x10-8 m/s^2 change in gravity is 2.4 cm of groundwater!