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Less is more? New take on machine learning helps us

Researchers from Tokyo Metropolitan University have enhanced super-resolution machine learning techniques to study phase transitions. They identified key features of how large arrays of interacting particles behave at different temperatures by simulating tiny arrays before using a convolutional neural network to generate a good estimate of what a larger array would look like using correlation configurations. The massive saving in computational cost may realize unique ways of understanding how materials behave.

Scientists call for international investment to tackle major wheat losses

It takes some heat to form ice!

 E-Mail IMAGE: The study results of Anton Tamtögl et al lead to a completely new understanding of ice formation: Water molecules require additional energy before they freeze into ice. view more  Credit: © Lunghammer - TU Graz Water freezes and turns to ice when brought in contact with a cold surface - a well-known fact. However, the exact process and its microscopic details remained elusive up to know. Anton Tamtögl from the Institute of Experimental Physics at TU Graz explains: The first step in ice formation is called nucleation and happens in an incredibly short length of time, a fraction of a billionth of a second, when highly mobile individual water molecules find each other and coalesce. Conventional microscopes are far too slow to follow the motion of water molecules and so it is impossible to use them to watch how molecules combine on top of solid surfaces.

UTA team to test geothermal de-icing technique on working bridge

A geothermal de-icing system designed by researchers at The University of Texas at Arlington kept a test bridge mostly clear of snow and ice during the sub-freezing winter storm in February. Now the research team will install its system on an in-service bridge to see how it performs under operational conditions.

Dry metastable olivine and slab deformation in a wet subducting slab

Our results suggest that olivine and wadsleyite show dry transformation kinetics even in wet slabs. It is therefore possible that olivine transformation as a cause of deep-focus earthquakes and large slab deformation creating stagnant slabs could occur in the water-undersaturated wet slabs. These processes could be caused jointly by dehydration of hydrous minerals and the subsequent rapid phase transformation when the dehydration starts at lower temperatures than the phase transformation.

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