DISCSIM

Hydrodynamical simulations of protoplanetary discs in the era of ALMA imaging

 Coordinatore THE CHANCELLOR, MASTERS AND SCHOLARS OF THE UNIVERSITY OF CAMBRIDGE 

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 Nazionalità Coordinatore United Kingdom [UK]
 Totale costo 1˙892˙844 €
 EC contributo 1˙892˙844 €
 Programma FP7-IDEAS-ERC
Specific programme: "Ideas" implementing the Seventh Framework Programme of the European Community for research, technological development and demonstration activities (2007 to 2013)
 Code Call ERC-2013-ADG
 Funding Scheme ERC-AG
 Anno di inizio 2014
 Periodo (anno-mese-giorno) 2014-02-01   -   2019-01-31

 Partecipanti

# participant  country  role  EC contrib. [€] 
1    THE CHANCELLOR, MASTERS AND SCHOLARS OF THE UNIVERSITY OF CAMBRIDGE

 Organization address address: The Old Schools, Trinity Lane
city: CAMBRIDGE
postcode: CB2 1TN

contact info
Titolo: Ms.
Nome: Renata
Cognome: Schaeffer
Email: send email
Telefono: 441223000000
Fax: 441223000000

UK (CAMBRIDGE) hostInstitution 1˙892˙844.00
2    THE CHANCELLOR, MASTERS AND SCHOLARS OF THE UNIVERSITY OF CAMBRIDGE

 Organization address address: The Old Schools, Trinity Lane
city: CAMBRIDGE
postcode: CB2 1TN

contact info
Titolo: Prof.
Nome: Catherine
Cognome: Clarke
Email: send email
Telefono: -340266
Fax: -338702

UK (CAMBRIDGE) hostInstitution 1˙892˙844.00

Mappa


 Word cloud

Esplora la "nuvola delle parole (Word Cloud) per avere un'idea di massima del progetto.

simulations    planet    become    self    evolution    designed    disc   

 Obiettivo del progetto (Objective)

'This is a proposal for an ambitious programme of state of the art hydrodynamical simulations, designed to answer some key questions about the role of disc self-gravity in planet formation. The programme is also designed so as to maximize the synergy with the new observational constraints from high resolution imaging data from the Atacama Large Millimetre Array that will become available over the timescale of the grant. The five year programme should provide definitive answers about whether planet formation is able to get going during the early, self-gravitating phase of disc evolution and how, if so, it would affect the further evolution of the disc. The topic of gravitational disc fragmentation as a route to planet formation is currently in a state of crisis, with recent simulations undermining what had become a consensus view on the subject. A dedicated and carefully constructed approach, as detailed here, is required to solve this problem.'

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