Now if we can just apply this treatment to all the glaciers and the Arctic…
Artificially controlling water condensation leads to ‘room-temperature ice’

Via Eurekalert. College Park, MD (July 27, 2010) — Earth’s climate is strongly influenced by the presence of particles of different shapes and origins — in the form of dust, ice and pollutants — that find their way into the lowest portion of the atmosphere, the troposphere. There, water adsorbed on the surface of these particles can freeze at higher temperatures than pure water droplets, triggering rain and snow.
Researchers at Spain’s Centre d’Investigació en Nanociència i Nanotecnologia (CIN2) have studied the underlying mechanisms of water condensation in the troposphere and found a way to make artificial materials to control water condensation and trigger ice formation at room temperature. Described in the Journal of Chemical Physics, which is published by the American Institute of Physics, their work may lead to new additives for snowmaking, improved freezer systems, or new coatings that help grow ice for skating rinks.
“Several decades ago, scientists predicted that materials with crystal faces exhibiting a structure similar to that of hexagonal ice, the form of all natural snow and ice on Earth, would be an ideal agent to induce freezing and trigger rain,” explains Dr. Albert Verdaguer. “This explanation has since proven to be insufficient.”
The research team chose to study barium fluoride (BaF2), a naturally occurring mineral, also known as “Frankdicksonite,” as an option. They examined water adsorption on BaF2 (111) surfaces under ambient conditions using different scanning force microscopy modes and optical microscopy to zoom in on the role atomic steps play in the structure of water films, which can affect the stabilization of water bilayers and, ultimately, condensation.
Despite having the desired hexagonal structure, BaF2 turned out to be a poor ice-nucleating material. But oddly enough, other researchers had discovered that when the mineral’s surface has defects, its condensation efficiency is enhanced.
Verdaguer and his colleagues figured out why this occurs. “Under ambient conditions — room temperature and different humidities — we observed that water condensation is mainly induced by the formation of two-dimensional ice-like patches at surface defects,” Verdaguer says. “Based on our results and previous research, we’re preparing artificial materials to improve water condensation in a controllable way.”
The next step? The researchers’ goal now is to produce environmentally-friendly synthetic materials for efficiently inducing snow. “If water condenses in an ordered way, such as a hexagonal structure, on such surfaces at ambient conditions, the term ‘room temperature ice’ would be fully justified,” adds Verdaguer. “The solid phase, ice, would be produced by a surface effect rather than as a consequence of temperature. In the long term, we intend to prepare smart materials, ‘intelligent surfaces,’ that will react to water in a predefined way.”
The article, “Two-dimensional wetting: The role of atomic steps on the nucleation of thin water films on BaF2(111) at ambient conditions” by M. Cardellach, A. Verdaguer, J. Santiso, and J. Fraxedas was published online in the Journal of Chemical Physics on June 21, 2010.
PDF of the paper is available. See: http://link.aip.org/link/JCPSA6/v132/i23/p234708/s1
There Ain’t No Such Thing As A Free Lunch. The MOST such a surface can do is enable the water to condense without requiring subcooling, by acting as a nucleation site. Dust or smoke sized particles of this nature will simply accomplish what plain old dirt can do, but just require a bit less material to do so. Yawn.
Thermodynamics, it’s not just the law, it’s a good idea.
They will never achieve much more than 1 or 2 layers of “dense” absorbed water. The hydrogen bond with the subsequent layers will dominate the atomic forces from the surface of the solid.
The applications are limited and most likely they could be a good nucleation particles. However, even if BaF2 is found in nature, what would be the effect of major quantities released in the air or soil?
I am certain however that at the end of their paper they must have added “but more research is needed to study this effect” (i.e. more money too!).
Hmm, was this brought to us by the those cold fusion fellas of a few years ago?
Living in the Midwest, I want a material that does the opposite. I want a surface that prevents “icing” below the freezing point to surface the roads with. I’ll offer my driveway and sidewalks as test areas.
Same question I am asking myself here … where/what is the energy transfer?
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Not getting much back out of Google that is relevant on that subject ‘mix’ BillN …
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BillN, in History Of Refrigeration (pdf file) I did find this:
Hmmm … IR radiation directly into space from the surface as a cooling mechanism … hmmm …
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It is true that when water crystallizes it forms six sided crystals. But it can’t do this without the temperature dropping. The latent heat of crystallization has to be removed. Water molecules will not stay still long enough to form crystals wherever you put them at temperatures above 0° C.
BillN, one more reference:
Refrigeration and Air Conditioning By Ramesh Chandra Arora
This source agrees with previously posted source and adds some more details …
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BillN, not beating a dead horse, but, here is a modern-day account, about 3/4 the way to the bottom: How to Use the Solar Funnel as a Refrigerator/Cooler
To whet the scientific appetite, I will only quote the following: “We routinely achieve cooling of about 20º F (10º C) below ambient air temperature using this remarkably simple scheme.”
Re: Matt July 28, 2010 at 7:14 am
“If ice is forming at a higher temperature, where is the energy going? is it cold ice or room temperature ice? For ice to form, the condensate must release its energy to the surrounding, releasing heat. if however the room is warmer than the ice, the ice will absorb energy from the room and cool the room.
What am I missing here?”
It is room temperature ice. There are many different types of energy and enthalpy is just one of them. No enthalpy is lost by the water but it can still be favourable for it to form the hexagonal ice structure on the BaF2 surface if doing so increases the entropy (from the second law of thermodynamics) and the interfacial energy to reduce the energy of the entire system. If the hexagonal ice structure is sufficiently favourable then there will be enough energy in the system already for it to form. Surfaces are areas of high energy so they are where some amazing things can happen in terms of entropy that we wouldn’t normally expect because we are used to dealing with objects of a size where the surface energy is small compared to the internal energy. It is no surprise that defects are a favourable site as they would be an area of even high interfacial energy.
An example you might be more familiar with would be say the water meniscus on the side of a container. Considering the potential energy of the water alone the meniscus should not form, but if we consider the interfacial energy we find that the meniscus must form.
I sounds to me like they have formed a mono-molecular, well-ordered layer of H2O on this surfance, and have decided to call it “ice”. This is NOT what most people would call ice. “Useful ice” would be a substance that could absorb heat, so as to cool something else. This requires an energy transfer, which does not seem to be happening here.
Sounds reminiscent of “polywater”: http://www.cs.cmu.edu/~dst/ATG/polywater.html
ethical shmethical ice-9 whatever. I don’t care. As long as this means I can snowboard in June without going to Chile or New Zealand.
stevengoddard says:
July 28, 2010 at 5:37 am
“I tried pointing this out last year in the CO2 freezing point article. Ice nucleates around defects. No one seemed interested at the time.”
Steve, sod all the rhetoric! Does this mean I can get ice for my Whisky n Coke without the use of a fridge in my current room, Shanghai temperature, (90F! yep I am that old!) and humidity currently around 90% ?
I can work out, as an electrical engineer, how external temperature and humidity effect the air conditioners and refrigeration equipment I work with but this is all new to me! Now, if I can only adapt this to the HVAC systems on the marine offshore side, I can really make my mark on saving the world from the evil CO2 before I retire and join with Anthony, in full time pay from the oil companies! Sarc off! (pray, the AGW myth does not fail for 2 more years! Its to much fun!)
Room temperature ice is the coolest thing I’ve seen in a long time.
No, wait. Room temperature. That’s not cool.
I guess it’s literally warm and metaphorically cool. Yeah, that’s the ticket.
I guess it won’t be of much use keeping my beer cold but I wonder if you can go sledding on it?