Soil and Survival
Wet the Ground and Wait
A passive water generator for the desert, and why we should build one before we need one on Mars
Every conversation about living somewhere else eventually hits the same wall, and it is not fuel and it is not food. It is water.
You can make water. Hydrogen and oxygen, strike a spark, and you have it — that is a chemistry set and it works. But a chemistry set is not a supply. A colony needs a source that keeps producing after the crates run out, without somebody standing over it.
So here is a proposal. Not a product, not a patent. A proposal, and an experiment I would like to see run here on Earth first.
Start with the emptiest place you can find
Picture a ridge in the high desert. Nothing on it. You stand in the valley and look up at a bare line of rock and sand, and there is not a green thing on it anywhere. Dead ground.
That is where I want to build, and not because it is convenient. Because it is the hardest honest test we have. If a machine can pull water out of the air up there and put it into the ground, it can do it most places. And the desert is the closest thing to Mars that a man can reach with a pickup truck and a backhoe.
Now the part nobody tells you
I want to lay out the problem honestly, because this magazine is not in the business of selling miracles.
There is very little water in desert air. On a hot afternoon out there you might have fifteen percent humidity at ninety-five degrees, which sounds like nothing and is nothing — about five grams of water in a kilogram of air. The number that actually matters is the dew point, the temperature you have to reach before that water will come out. In high desert air the dew point sits down around forty degrees Fahrenheit, and it stays there day and night. The air cools off at night, but it does not gain any water.
Now the other half. The old idea — and it is an old idea, the Greeks may have built them, and they are called air wells — is to run that hot air down a pipe into the ground, let the cool earth chill it, and catch what drips out.1 Beautiful. Costs nothing.
Except go dig a hole in a hot desert and put a thermometer six feet down. You will find something close to fifty-five degrees. Not cold. That is the annual average temperature of the place, and the deeper you go the more it settles right there.
So your dew point is forty and your ground is fifty-five. You are fifteen degrees short, and fifteen degrees short means you do not get a drop. Not a little water. None.
That is why every passive air well ever attempted in a real desert has come up dry, and why the working machines you see on the internet all have a compressor and a power cord. They are refrigerators. They make water, they make it honestly, and they will never be deployed by the hundred on an empty ridge because somebody has to feed them electricity forever.
So make the cold
If the ground will not give you cold, manufacture it — and here is where I get to use forty years of Alaska.
On the North Slope we build on permafrost, and a heated building will melt the ground out from under itself and take the building with it. So we install thermosyphons. You have seen them if you have ever driven the haul road — the pipes standing up along the pipeline with fins on top.2
There is no pump in one and no power to one. Inside is a working fluid. Down in the warm ground it boils, the vapor rises to the radiator up top where the winter air is cold, it condenses, and gravity runs the liquid back down. That is the entire machine. It has one moving part, which is the fluid itself.
And here is the property that makes this whole idea work: a thermosyphon only moves heat one direction. Up and out, never back down. When the air is colder than the ground, it runs. When the air is warmer, it simply stops. It is a one-way valve for heat, and nobody has to switch it.
Point that at a desert instead of at permafrost and it will do the same job. Desert nights get cold, and desert winters get genuinely cold. Every one of those cold nights, the syphons pull heat out of the ground and throw it at the sky. Nobody pays for it and nobody tends it.
The cold battery
Now, dry sand is a terrible conductor. Chill a pipe in dry desert soil all winter and the cold barely travels five feet from it. That is a real limitation and it killed my first sketch of this.
The fix is to give the cold something better to live in: water.
Down in the trench you set a sealed tank — call it twenty feet long, four feet wide, holding a couple feet of water. Water holds roughly three times the heat of the same volume of dry soil and it moves heat far better. Through that water you run the thermosyphon loop. All winter, every cold night, the syphons pull heat out of that tank and dump it into the sky.
By spring you have a buried tank of near-freezing water, and if it goes to ice, so much the better — ice is a bigger cold battery still.
That tank is the whole trick. You are not harvesting cold when you need it. You are banking it in the winter and spending it in the summer.
The harvest
Then, in the warm months, the second circuit runs. A stainless coil sits in that cold water, and desert air comes down an intake shaft, passes through the coil, and goes out an exhaust shaft on the far side. On the way through, the air hits a wall well below its dew point, and the water comes out of it and beads up on the inside of the pipe.
The coil is pitched, so the water runs down it and out the low end into a drip line. The drip line is buried a foot or two down — not laid on the surface, because surface water in a desert is gone by noon. It leaches sideways and down into the soil and stays there.
The one bit of electricity in the whole system is a small solar panel running a DC fan and two temperature sensors: one in the intake, one in the tank. The fan runs only when the incoming air actually has more moisture in it than the tank is cold enough to take. The rest of the time it sits still, because blowing warm air across your cold battery all afternoon would waste the winter you spent charging it.
That is it. A panel, a fan, and a thermostat. Everything else is pipe, tank, and physics.
The number, and why it is the wrong number
Here is what one of these will make: somewhere around sixteen gallons a year.
I am going to leave that number right there on the page, because everybody who works on atmospheric water gets judged on gallons per day and everybody loses. Sixteen gallons a year is a joke as a drinking water product. Nobody is going to fund a machine that fills a bathtub every other summer.
But that is the wrong yardstick, and swapping the yardstick is the actual idea in this article.
Stop counting liters. Start counting years, and start counting units.
Nobody needs a hundred gallons a day. What we need is a hundred units running for ten years into the same hillside, with no power line, no pump, no man on site, and no maintenance beyond a fan bearing. That is not a water supply. That is subsurface irrigation with the pipeline removed.
How you would deploy it
You take a backhoe up the ridge and dig a trench six feet down. In the bottom goes the tank, the syphon loop, and the condenser coil, all in the same ditch. You pitch the trench — the thermosyphon returns its liquid by gravity, so a foot of fall in twenty is about right, radiator end high.
Backfill matters more than most people would guess. Do not just push the dry sand back in on top of it. Pack it, wet it in once, mix in something dense — the difference between dry sand and damp packed soil is a doubling or tripling of how far your cold reaches.
Then you do it again, parallel, down the ridge. A hundred trenches. It is not exotic work. Any dirt contractor in the country could build the whole array with equipment he already owns.
What we are actually looking for
Here is the result I want to see, and it is not a flow meter reading.
Each buried emitter builds a wet bulb of soil around itself, slowly, over years. Desert seed is patient — it has been sitting in that ground waiting, sometimes for decades. Get moisture to it and things come up.
At first you would get green dots. Then, as the wet bulbs spread and touch each other, the dots join into a line.
And what I want is for a man to stand in that valley, look up at a ridge that has been bare his whole life, and see a green stripe running along it. No instrument, no report, no press release. You can see it from a mile off, and it means water is in that ground and staying there.
That is the proof of concept. It just takes longer than a grant cycle.
And then Mars
Which brings it back around to why any of this matters up there.
Mars air is thin — call it a hundredth of ours — so there is not much of it to work with. But two things go in our favor and they are big ones. That thin air is often at or very near its own dew point, or frost point, meaning it is already on the edge of giving up its water.3 And the cold is free. You do not have to bank a winter to get below frost point on Mars; you just have to open the door.
So the machine changes shape but the logic holds: passive, buried, unattended, playing a long game, and measured in wet soil rather than gallons.
And soil is where this all points anyway. I wrote in these pages that you cannot ship dirt to Mars, and that the fix is worms. Well, worms need moisture or they are dead in a week. So it stacks: soil needs worms, worms need water, water needs cold, and cold, it turns out, you can bank in a hole in the ground with a piece of Alaskan hardware that has been working unattended for forty years.
Nothing in this proposal requires a breakthrough. There is no new physics in it anywhere. Hot air meets a cold surface, water beads up, gravity takes it down. Every component is off the shelf.
A backhoe, some pipe, a tank, and patience.
From one explorer to another, we appreciate you reading this far. We are excited about what this endeavor brings, and we would like you along for the rest of it.
Come join us. Because we are Star Bound.
John LangEditor
Ideas in Star Bound are published open — take them, build them better. Our open proposal.
A note on where this comes from. I am not a metallurgist, a spacecraft engineer, or a degreed engineer of any kind. But I am a practical one, with more than forty years in heavy industrial construction: welding, millwright work, hydraulics, mining, and thirty-three years of electrical construction and commissioning on the North Slope of Alaska, in a place that punishes anything built wrong. Much of that time I have worked as a field engineer, which means I am the one standing in front of the equipment when the drawing turns out to be wrong, and the fix has to be made on the spot, with what is on hand, and has to work the first time. Anyone who has done that long enough learns that a lot of engineering gets corrected in the field by people with more experience than the people who drew it. That is the eye I bring to these subjects: not what should work on paper, but what actually gets built, and what breaks. The facts I take from other people are footnoted so you can check them and read further. The ideas built on top of those facts are my own, and I would rather see them knocked down by somebody who knows better than left standing because nobody looked.
Sources
- Wikipedia, Air well (condenser), gives the history and the three design families; the Greek attribution rests on F. I. Zibold’s reading of stone mounds at Feodosia in the early 1900s and is disputed. For the engineering record see Jumikis, Aerial Wells: Secondary Sources of Water, Soil Science 100(2), 1965, which concludes the modern high-mass wells at Trans and Montpellier never worked. ↩
- Alyeska Pipeline Service Co., Alyeska’s 40-Plus Years of Experience with Heat Pipes on the Trans-Alaska Pipeline System (Permafrost 2021) — more than 124,000 ammonia thermosyphons installed in the vertical support members during construction; also Heuer, The Application of Heat Pipes on the Trans-Alaska Pipeline, CRREL Special Report 79-26 (1979). ↩
- Phoenix photographed water frost on the ground at dawn and laser-sounded nightly ice fog at its landing site in 2008; see Universe Today, Phoenix Camera Snaps Frost on Mars, and National Geographic, Mars fog and water cycle. ↩
The humidity and dew-point numbers, ground temperature settling toward the annual mean, and the heat capacity of water versus dry soil are standard psychrometrics and soil physics and are not footnoted individually. The sixteen-gallons-a-year figure is my own estimate for one unit, not a measurement — which is the whole reason I want one built.
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