New Ge isotope data for carbonaceous and enstatite chondrites give a bulk silicate Earth carbonaceous-chondrite fraction of 0.64±0.16, larger than the Zn fraction of 0.29±0.07, indicating late delivery of volatile-rich carbonaceous bodies.
Laboratory evidence for proton energization by collisionless shock surfing
1 Pith paper cite this work. Polarity classification is still indexing.
abstract
Charged particles can be accelerated to high energies by collisionless shock waves in astrophysical environments, such as supernova remnants. By interacting with the magnetized ambient medium, these shocks can transfer energy to particles. Despite increasing efforts in the characterization of these shocks from satellite measurements at the Earth's bow shock and powerful numerical simulations, the underlying acceleration mechanism or a combination thereof is still widely debated. Here, we show that astrophysically relevant super-critical quasi-perpendicular magnetized collisionless shocks can be produced and characterized in the laboratory. We observe characteristics of super-criticality in the shock profile as well as the energization of protons picked up from the ambient gas to hundreds of keV. Kinetic simulations modelling the laboratory experiment identified shock surfing as the proton acceleration mechanism. Our observations not only provide the direct evidence of early stage ion energization by collisionless shocks, but they also highlight the role this particular mechanism plays in energizing ambient ions to feed further stages of acceleration. Furthermore, our results open the door to future laboratory experiments investigating the possible transition to other mechanisms, when increasing the magnetic field strength, or the effect induced shock front ripples could have on acceleration processes.
fields
astro-ph.EP 1years
2025 1verdicts
CONDITIONAL 1representative citing papers
citing papers explorer
-
Origin of moderately volatile elements in Earth inferred from mass-dependent Ge isotope variations among chondrites
New Ge isotope data for carbonaceous and enstatite chondrites give a bulk silicate Earth carbonaceous-chondrite fraction of 0.64±0.16, larger than the Zn fraction of 0.29±0.07, indicating late delivery of volatile-rich carbonaceous bodies.