Planet Evaporation as a Window into Exoplanetary Origins

Projektinformationen

PEVAP

ID Finanzhilfevereinbarung: 853022

DOI

10.3030/853022

Projekt abgeschlossen

EK-Unterschriftsdatum 30 Oktober 2019

Startdatum 1 Februar 2020

Enddatum 31 Oktober 2025

Finanziert unter

• EXCELLENT SCIENCE - European Research Council (ERC)

Gesamtkosten

€ 1 464 320,00

EU-Beitrag

€ 1 464 320,00

Koordiniert durch

IMPERIAL COLLEGE OF SCIENCE TECHNOLOGY AND MEDICINE
United Kingdom

Periodic Reporting for period 3 - PEVAP (Planet Evaporation as a Window into Exoplanetary Origins)

Berichtszeitraum: 2023-02-01 bis 2024-07-31

Zusammenfassung vom Kontext und den Gesamtzielen des Projekts

We have discovered a large number of planets close to their host stars. In fact, we now know most stars host planets inside the orbit of Mercury in our own Solar System. Yet unlike the solar system terrestrial planets, these exoplanets often contain large atmospheres rich in hydrogen gas. It is currently an unsolved problem how these planets form or how the Earth sits within the zoo of all possible planets. Given many of these planets are extremely highly irradiated by their host stars, they are vulnerable to having their atmospheres heated up and lost to space through a process known as "photoevaporation".

It is thought that this photoevaporation process is responsible for many of the features detected in the exoplanet population today. Thus, rather than using the observed exoplanets to inform about their origins, we need to account for this photoevaporation process. Thus, in this project, we will develop new photoevaporation models and then use them to determine how the planets evolved into those we see today.

Our objectives are:

1. What are the mass-loss rates and photoevaporative flow structures for the full spectrum of observed planets?
2. How can we use observations of photoevaporating planets to learn about their compositions and histories?
3. How does photoevaporation affect and control the evolution of exoplanets and their atmospheres?

Arbeit, die ab Beginn des Projekts bis zum Ende des durch den Bericht erfassten Berichtszeitraums geleistet wurde, und die wichtigsten bis dahin erzielten Ergebnisse

So far, we have begun developing new photoevaporation models for atmospheres that contain more elements than hydrogen. We have developed a new computer code that can simulate the photoevaporative outflows from these planets and have applied it to hot terrestrial planets where their surfaces are melted. Furthermore, we have used our models for the photoevaporation of hydrogen atmospheres to understand the evolution of these planets. By building a model of how the hydrogen atmospheres of exoplanets evolve in time, we have used it to unwind the billions of years of evolution that exoplanets have undergone. In doing so, we have uncovered how many of the observed exoplanets formed. We found that most observed exoplanets did not form like those in our Solar System, rather they formed through a previously unidentified pathway where they grew quickly acquiring a small amount of primordial gas close to their host stars.

Fortschritte, die über den aktuellen Stand der Technik hinausgehen und voraussichtliche potenzielle Auswirkungen (einschließlich der bis dato erzielten sozioökonomischen Auswirkungen und weiter gefassten gesellschaftlichen Auswirkungen des Projekts)

In the project's next phase, we expect to apply the same statistical analysis to the hydrogen-dominated atmospheres to atmospheres more akin to the terrestrial planets in our Solar-System. In doing so, we will be able to put Earth in the context of exoplanets and answer the question of how rare we really are.

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