We review the properties of dust formed during classical nova eruptions and the Very Late Thermal Pulses (VLTPs) that occur during the later stages of post-Asymptotic Giant Branch evolution of low-mass stars. In both cases, carbon and hydrocarbon dust is produced. Novae may also produce silicate dust, contrary to the usual paradigm about the C:O ratio and dust composition. Despite the expectation that these dust sources are not expected to make significant contributions to the Galactic dust population, there is a significant body of evidence that grains from both stellar sources have been identified in recovered meteoritic and cometary material, and that certain infrared spectral signatures seen in comets are common to novae, VLTPs and pre-...
The dust formation processes in novae are investigated with close attention to recent infrared obser...
Manuscript submitted to Proceedings of the National Academy of ScienceThe solar system formed from i...
Mixed within the fine-grained material of primitive astromaterials (e.g., meteorites, micrometeorite...
We review the properties of dust formed during classical nova eruptions and the Very Late Thermal Pu...
Context. Classical novae are thermonuclear explosions that take place in the envelopes of accreting ...
Pristine stardust grains from the interstellar gas and dust cloud from which our Solar System formed...
Observations show that the time of onset of dust formation in classical novae depends strongly on th...
About 30%–40% of classical novae produce dust 20–100 days after the outburst, but no presolar stardu...
Although their parent stars no longer exist, the isotopic and chemical compositions and microstructu...
The problem of grain nucleation during novae outbursts is a major obstacle to our understanding of d...
Presolar stardust grains found in primitive meteorites are believed to retain the isotopic compositi...
The question ‘Are supernovae important sources of dust?’ is a contentious one. Observations with the...
Abstract. A classical nova outburst arises from a thermonuclear run-away in the hydrogen-rich materi...
The discovery that many classical novae produce detectable GeV $\gamma$-ray emission has raised the ...
The discovery of broad emission features between 3.2 and 3.6 microns were reported in the spectrum o...
The dust formation processes in novae are investigated with close attention to recent infrared obser...
Manuscript submitted to Proceedings of the National Academy of ScienceThe solar system formed from i...
Mixed within the fine-grained material of primitive astromaterials (e.g., meteorites, micrometeorite...
We review the properties of dust formed during classical nova eruptions and the Very Late Thermal Pu...
Context. Classical novae are thermonuclear explosions that take place in the envelopes of accreting ...
Pristine stardust grains from the interstellar gas and dust cloud from which our Solar System formed...
Observations show that the time of onset of dust formation in classical novae depends strongly on th...
About 30%–40% of classical novae produce dust 20–100 days after the outburst, but no presolar stardu...
Although their parent stars no longer exist, the isotopic and chemical compositions and microstructu...
The problem of grain nucleation during novae outbursts is a major obstacle to our understanding of d...
Presolar stardust grains found in primitive meteorites are believed to retain the isotopic compositi...
The question ‘Are supernovae important sources of dust?’ is a contentious one. Observations with the...
Abstract. A classical nova outburst arises from a thermonuclear run-away in the hydrogen-rich materi...
The discovery that many classical novae produce detectable GeV $\gamma$-ray emission has raised the ...
The discovery of broad emission features between 3.2 and 3.6 microns were reported in the spectrum o...
The dust formation processes in novae are investigated with close attention to recent infrared obser...
Manuscript submitted to Proceedings of the National Academy of ScienceThe solar system formed from i...
Mixed within the fine-grained material of primitive astromaterials (e.g., meteorites, micrometeorite...