Non-axisymmetric, flow-driven instabilities in the incompressible Hall-MHD model are studied in a differentially rotating cylindrical plasma. It is found that in the Hall-MHD regime, both whistler waves and ion-cyclotron waves can extract energy from the flow shear, resulting in two distinct branches of global instability. The non-axisymmetric whistler modes grow significantly faster than non-axisymmetric, ideal MHD modes. A discussion of the whistler instability mechanism is presented in the large-ion-skin-depth, `electron-MHD' limit. It is observed that the effect of the Hall term on the non-axisymmetric modes can be appreciable when $d_i$ is on the order of a few % of the width of the cylindrical annulus. Distinct global modes emerge in the Hall-MHD regime at significantly stronger magnetic fields than those required for unstable global MHD modes.
The Cryogenic Underground Observatory for Rare Events (CUORE) experiment set the most stringent limit on the neutrinoless double-beta ($0\nu\beta\beta$) decay half-life of $^{130}$Te with 2 ton yr TeO$_2$ analyzed exposure. In addition to $0\nu\beta\beta$ decay, the CUORE detector -- a ton-scale array of nearly 1000 cryogenic calorimeters operating at $\sim$10 mK -- is capable of searching for other rare decays and interactions over a broad energy range. For our searches, we leverage the available information of each calorimeter by performing its optimization, data acquisition, and analysis independently. We describe the analysis tools and methods developed for CUORE and their application to build high-quality datasets for numerous physics searches. In particular, we describe in detail our evaluation of the energy-dependent detector response and signal efficiency used in the most recent search for $0\nu\beta\beta$ decay.
Hydrogen, helium, silicates, and iron are key building blocks of rocky and gas-rich planets, yet their chemical interactions remain poorly constrained. Using first-principles molecular dynamics and thermodynamic integration, we quantify hydrogen and helium partitioning between molten silicate mantles and metallic cores for Earth-to-Neptune-mass planets. Hydrogen becomes strongly siderophilic above $\sim$25 GPa but weakens beyond $\sim$200 GPa, whereas helium remains lithophilic yet increasingly soluble in metal with pressure. Incorporating these trends into coupled structure-chemistry models suggests that majority of hydrogen and helium reside in planetary interiors, not atmospheres, with abundances strongly depending on planet mass. Such volatile exchange may influence the redox states of secondary atmospheres, longevity of primordial envelopes, predicted CHNOPS abundances, and emergence of helium-enriched atmospheres, while He 1083 nm and H Lyman-$\alpha$ lines provide potential probes of atmosphere-interior exchange. These findings link atomic-scale interactions to planetary-scale observables, providing new constraints on the origins of Earth-to-Neptune-sized worlds.
At low redshift, massive quiescent galaxies (MQGs) are most frequently found in massive, rich galaxy clusters, but at high redshift the trend is less clear. Here, we present spectroscopic evidence of the effects of environment on the formation and assembly of high-redshift MQGs. We identify 25 (5) $\log (M_*/\mathrm{M_\odot}\geq10.5$ ($10.0\leq\log (M_*/\mathrm{M_\odot}<10.5$) spectroscopically-confirmed quiescent galaxies in the UDS and EGS fields at $3<z<5$ with NIRSpec PRISM spectroscopy from RUBIES and other public JWST NIRSpec programs. We measure the density contrast in these fields by applying a Monte Carlo Voronoi Tesselation density mapping technique to photometric and spectroscopic redshifts of $m_\mathrm{F444W}<27.5$ sources. We robustly detect 12 massive overdense peaks with $\log (M_\mathrm{Peak}/\mathrm{M_\odot})\geq13$ and six extended massive protoclusters ($\log (M_\mathrm{Struct}/\mathrm{M_\odot})\geq13.85$). We observe that MQGs are preferentially found in these massive peaks and within these massive structures: $\approx50\%$ of MQGs are found in massive peaks, compared to $\approx20\%$ of massive star forming galaxies (MSFGs) and $\approx15\%$ of the overall spectroscopically-confirmed population. We also find an apparent dependence on both quiescent galaxy mass and environment, with $75\%$ of the most massive ($\log (M_*/\mathrm{M_\odot}\geq10.75$) residing inside overdense peaks. We compare the star formation histories (SFHs) of the MQGs with the high-redshift galaxy stellar mass function from observations and simulated quiescent galaxies at $z>5$, finding that the masses from the inferred MQG SFHs regularly exceed either observed or simulated high-redshift galaxies, which suggests indicates that mergers and ex-situ star formation play a key role in the mass assembly of MQGs in overdense environments.