New Superconductor Could Work at Higher Temperatures
A team at the Paul Scherrer Institute (PSI) in Switzerland has achieved a breakthrough with a Kagome superconductor (RbV3Sb5) that demonstrates time-reversal symmetry (TRS) breaking at a temperature of 175 Kelvin (-98°C or -144.67 °F). This record temperature suggests promising developments in quantum systems, which typically require ultra-low temperatures to prevent disruptions caused by thermal energy. Researchers believe the high-temperature TRS breaking in RbV3Sb5 can reduce energy needs for quantum technology, potentially accelerating its adoption.
Understanding Time-Reversal Symmetry in Quantum Technology
TRS implies that the fundamental laws remain the same when time flows backward in Physics. However, in materials like RbV3Sb5, TRS is broken, leading to unique quantum states that are challenging yet essential for developing advanced quantum devices. These unusual states result in the material behaving differently depending on the direction of time, an attribute that can be manipulated for enhanced control over quantum systems.
According to the study authors, this Kagome superconductor maintains superconductivity down to approximately two Kelvin but can sustain TRS-breaking quantum states at much higher temperatures, enhancing its suitability for real-world applications. PSI researchers, including Mahir Dzambegovic, highlighted the material’s charge order state, where electrons form an organised pattern, producing a magnetic effect that breaks TRS at -144.67 °F.
Implications for Future Quantum Systems
The discovery of TRS breaking at such temperatures presents significant implications for quantum computing and storage. The ability to maintain these effects at higher temperatures could make quantum technologies more feasible outside of laboratory settings, according to PSI’s team. Notably, the TRS-breaking properties of RbV3Sb5 are tunable, with effects varying based on the material’s depth, from surface to core.
Future studies are expected to further explore the tunability of Kagome superconductors, particularly focusing on the interplay between superconductivity and TRS-breaking effects in RbV3Sb5. The study, published in Nature Communications, marks a step toward achieving practical quantum devices capable of operating in more energy-efficient conditions.
For the latest tech news and reviews, follow Gadgets 360 on X, Facebook, WhatsApp, Threads and Google News. For the latest videos on gadgets and tech, subscribe to our YouTube channel. If you want to know everything about top influencers, follow our in-house Who’sThat360 on Instagram and YouTube.
The scientists have found methane in the atmosphere of WISEA J181006.18 −101000.5, the T dwarf closest to Earth. The study was published in the online preprint journal arXiv on March 28, and the final, revised version was published on November 17. The WISE1810 is a metal-poor T dwarf planet, which is situated at a distance of 29 light years from the Earth. The effective temperature of the dwarf is reported to be within the range of 800–1,300 K.
Methane Signature Surprises Astronomers
According to a Phys.org report, the finding is made greatly possible by the present 10.4-m Gran Telescopio Canarias (GTC). The detection of methane in the atmosphere of the dwarf planet has further made its classification as T-type instead of L-type, which was earlier suggested in previous studies, the publication notes. The study further reveal that there are no traces of carbon monoxide and potassium in the atmosphere of the WISE1810.
The study further highlights that the carbon abundance in the planet is estimated to be -1.5 dex, while the effective temperature could be around 1,000 K. The author of the paper further revealed that the low metallicity of the T dwarf planet could be due to the non-detection of atomic potassium. However, a lower temperature could also boost this effect, the report further highlights. The study also found that WISE1810 has a heliocentric velocity of -83 km/s.
The 10.4-m Gran Telescopio Canarias (GTC) supplies a significant contribution to finishing WISEA J181006.18−101000 observations. Interestingly, the previous observations of the dwarf platent suggested that the atmosphere of the dwarf planet was dominated by hydrogen and water vapour. Moreover, the study further reveals that findings indicates WISE1810 could more likely to be associated with the Milky Way’s thick disk, despite its very low metallicity.
For the latest tech news and reviews, follow Gadgets 360 on X, Facebook, WhatsApp, Threads and Google News. For the latest videos on gadgets and tech, subscribe to our YouTube channel. If you want to know everything about top influencers, follow our in-house Who’sThat360 on Instagram and YouTube.
An underground structure beneath central United States has been observed dragging surface materials deep into the Earth. This movement has been linked to an old piece of crust lodged far below the Midwest. Researchers have said this action is pulling rocks from across the continent towards a funnel-shaped region. It is believed this process is causing parts of the crust to thin as material is drawn downward. This phenomenon has been found to affect areas beyond the immediate region.
Underground slab tied to crust loss beneath Midwest
According to the study published in Nature Geoscience, the phenomenon has been tied to the remains of a long-subducted tectonic plate known as the Farallon slab. This slab, which sits around 660 kilometres below the surface, was identified as the driving force behind what scientists refer to as cratonic thinning. Cratons are known to be the stable core regions of continental crust and upper mantle that usually do not undergo change.
The seismic mapping project was led by Junlin Hua during his postdoctoral work at The University of Texas at Austin. He now serves as a professor at the University of Science and Technology of China. In a statement, Hua explained that a wide region is showing signs of thinning. He stated that the study has brought forward a new explanation behind this change.
New seismic method uncovers ‘dripping’ lithosphere
To observe the changes taking place beneath North America, researchers used a method known as full-waveform inversion. This seismic imaging approach allowed them to map the subsurface in high detail. According to Thorsten Becker, Geophysics Chair at UT Austin, this technique offered a better understanding of the link between deep mantle regions and the lithosphere above.
Computer simulations were used to confirm the effect. When the slab was included, the downward movement was visible. When removed, no such feature appeared.
For the latest tech news and reviews, follow Gadgets 360 on X, Facebook, WhatsApp, Threads and Google News. For the latest videos on gadgets and tech, subscribe to our YouTube channel. If you want to know everything about top influencers, follow our in-house Who’sThat360 on Instagram and YouTube.
-
Sports2 years ago‘Storybook stuff’: Inside the night Bryce Harper sent the Phillies to the World Series
-
Sports1 year agoStory injured on diving stop, exits Red Sox game
-
Sports1 year agoGame 1 of WS least-watched in recorded history
-
Sports2 years agoMLB Rank 2023: Ranking baseball’s top 100 players
-
Sports4 years ago
Team Europe easily wins 4th straight Laver Cup
-
Environment2 years agoJapan and South Korea have a lot at stake in a free and open South China Sea
-
Environment2 years agoGame-changing Lectric XPedition launched as affordable electric cargo bike
-
Business3 years agoBank of England’s extraordinary response to government policy is almost unthinkable | Ed Conway