Light-induced disassembly of dusty bodies in inner protoplanetary discs: implications for the formation of planets

Abstract

Laboratory experiments show that a solid-state greenhouse effect in combination with thermophoresis can efficiently erode a dust bed in a low-pressure gaseous environment. The surface of an illuminated, light absorbing dusty body is cooler than the dust below the surface (solidstate greenhouse effect). This temperature gradient leads to a directed momentum transfer between gas and dust particles and the dust particles are subject to a force towards the surface(thermophoresis). If the thermophoretic force is stronger than gravity and cohesion, dust particles are ejected. Applied to protoplanetary discs, dusty bodies smaller than several kilometres in size which are closer to a star than about 0.4 au are subject to a rapid and complete disassembly to submillimetre size dust aggregates by this process. While an inward-drifting dusty body is destroyed, the generated dust is not lost for the disc by sublimation or subsequent accretion on to the star but can be reprocessed by photophoresis or radiation pressure. Planetesimals cannot originate through aggregation of dust inside the erosion zone. If objects larger than several kilometres already exist, they prevail and further grow by collecting dust from disassembled smaller bodies. The pile-up of solids in a confined inner region of the disc, in general, boosts the formation of planets. Erosion is possible in even strongly gas-depleted inner regions as observed for TW Hya. Reprocessing of dust through light-induced erosion offers one possible explanation for growth of large cores of gas-poor giant planets in a gas-starved region as recently found around HD 149026b.

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Cited by in corpus (9)

• Photophoretic separation of metals and silicates: the formation of Mercury like planets and metal depletion in chondrites
• Understanding planet formation using microgravity experiments
• From Planetesimals to Dust: Low Gravity Experiments on Recycling Solids at the Inner Edge of Protoplanetary Disks
• Dust Ejection from Planetary Bodies by Temperature Gradients: Laboratory Experiments
• A Mechanism to Produce the Small Dust Observed in Protoplanetary Disks
• Photophoretic Strength on Chondrules. 2. Experiment
• Analog Experiments on Tensile Strength of Dusty and Cometary Matter
• Photophoretic Strength on Chondrules 1: Modeling
• Selective Aggregation Experiments on Planetesimal Formation and Mercury-Like Planets