Defying the laws of physics? Engineers demonstrate bubbles of sand

Defying the laws of physics? Columbia engineers demonstrate bubbles of sand
Development of a "bubble" of lighter sand (blue) forming in heavier sand (white). Credit: Alex Penn/ETH Zurich

The flow of granular materials, such as sand and catalytic particles used in chemical reactors, explains a wide range of natural phenomena, from mudslides to volcanos, and enables a broad array of industrial processes, from pharmaceutical production to carbon capture. While the motion and mixing of granular matter often display striking similarities to liquids, as in moving sand dunes, avalanches, and quicksand, the physics underlying granular flows is not as well-understood as liquid flows.

Now, a recent discovery by Chris Boyce, assistant professor of chemical engineering at Columbia Engineering, explains a new family of gravitational instabilities in granular particles of different densities that are driven by a gas-channeling mechanism not seen in fluids. In collaboration with Energy and Engineering Science Professor Christoph Müller's group at ETH Zurich, Boyce's team observed an unexpected Rayleigh-Taylor (R-T)-like instability in which lighter grains rise through heavier grains in the form of "fingers" and "granular bubbles." R-T instabilities, which are produced by the interactions of two fluids of different densities that do not mix—oil and water, for example—because the lighter fluid pushes aside the heavier one, have not been seen between two dry granular materials.

The study, published today in the Proceedings of the National Academy of Sciences, is the first to demonstrate that "bubbles" of lighter sand form and rise through heavier sand when the two types of sand are subject to vertical vibration and upward gas flow, similar to the bubbles that form and rise in lava lamps. The team found that, just as air and oil bubbles rise in water because they are lighter than water and do not want to mix with it, bubbles of light sand rise through heavier sand even though two types of sand like to mix.

"We think our discovery is transformational," says Boyce "We have found a granular analog of one of the last major fluid mechanical instabilities. While analogs of the other major instabilities have been discovered in granular flows in recent decades, the R-T instability has eluded direct comparison. Our findings could not only explain geological formations and processes that underlie mineral deposits, but could also be used in powder-processing technologies in the energy, construction, and pharmaceuticals industries."

Boyce's group used experimental and computational modeling to show that gas channeling through lighter particles triggers the formation of finger and bubble patterns. The gas channeling occurs because the clusters of lighter, larger particles have a higher permeability to gas flow than do the heavier, smaller grains. The R-T-like instability in granular materials arises from a competition between upward drag force increased locally by gas channeling and downward contact forces, a physical mechanism entirely different from that found in liquids.

They found that this gas-channeling mechanism also generates other gravitational instabilities, including the cascading branching of a descending granular droplet. They also demonstrated that the R-T-like instability can occur under a wide variety of gas flow and vibration conditions, forming different structures under different excitation conditions.

"These instabilities, which can be applied to a variety of systems, shed new light on granular dynamics and suggest new opportunities for patterning within granular mixtures to form new products in the pharmaceutical industry, for example," Boyce adds. "We are especially excited about the potential impact of our findings on the geological sciences—these instabilities can help us understand how structures have formed over the long history of the Earth and predict how others may form in the future."

Boyce is now investigating other liquid-like and structured phenomena in sand particles and quantifying their behavior. He is also in conversations with geologists and volcanologists to explore more about how this process and similar ones occur in the natural world.


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More information: Christopher P. McLaren el al., "Gravitational instabilities in binary granular materials," PNAS (2019). www.pnas.org/cgi/doi/10.1073/pnas.1820820116
Citation: Defying the laws of physics? Engineers demonstrate bubbles of sand (2019, April 22) retrieved 21 July 2019 from https://phys.org/news/2019-04-defying-laws-physics-sand.html
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Apr 22, 2019
LOL, defying the laws of physics.... how about obeying the laws of physics. As a geologist, the concept of diapiric intrusion, where more less dense mobile and ductily deformable material is forced into brittle overlying rocks. Everything from soft sediments, to salt domes, to intrusive magma.

Apr 22, 2019
So they Finally Learned something from the old Wham-o Magic Window (tm) as per the:

https://clickamer...973-1979

I remember playing with em for hours and seeing that effect, never knew it was an 'unnoticed science fact'.

Fun Stuff, we had the imiscible fluid wave makers too that were fun to play with and get to understand, intrinsically, how waves react and form, how displacements move through sand of different densities.

Playing with such was more of an education than would be expected from the nature of them, but anything can be put to multiple scientific uses. Just look at how useful the hammer still is, and we have had it for hundreds of thousands of years, yet we still learn new things about how things react when they are hit 'just so hard'.

Apr 22, 2019
This is a "brazil nut effect" variation....

Apr 22, 2019
The gas-bubble effect makes it distinctly different than the Brazil nut setup. There is a certain gap size that forms before the upper collapses, slowly and methodically, into the other, and it is the gas doing the lifting and mass difference of the particles doing the work. The lighter ones ride on top as the heavier ones sink past the lighter grains at the margins of the bubble. The bubble expands to it's maximum width and the collapse rate stalls as the gas is too spread out for particle movement, which restarts once the grains shift Downwards on the edges and upwards in the middle, again forming a narrow bubble and restarting the sequence.

Apr 22, 2019
Could this be one of the mechanisms for 'sand blows' caused by earthquakes ??


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