SOLAIROS

Solubility of Aerosol Iron in Open-ocean Seawater

 Coordinatore UNIVERSITY OF PLYMOUTH 

 Organization address address: DRAKE CIRCUS
city: PLYMOUTH
postcode: PL4 8AA

contact info
Titolo: Dr.
Nome: John
Cognome: Martin
Email: send email
Telefono: +441752 588931
Fax: +44 1752 588987

 Nazionalità Coordinatore United Kingdom [UK]
 Totale costo 244˙807 €
 EC contributo 244˙807 €
 Programma FP7-PEOPLE
Specific programme "People" implementing the Seventh Framework Programme of the European Community for research, technological development and demonstration activities (2007 to 2013)
 Code Call FP7-PEOPLE-IOF-2008
 Funding Scheme MC-IOF
 Anno di inizio 2009
 Periodo (anno-mese-giorno) 2009-11-01   -   2012-10-31

 Partecipanti

# participant  country  role  EC contrib. [€] 
1    UNIVERSITY OF PLYMOUTH

 Organization address address: DRAKE CIRCUS
city: PLYMOUTH
postcode: PL4 8AA

contact info
Titolo: Dr.
Nome: John
Cognome: Martin
Email: send email
Telefono: +441752 588931
Fax: +44 1752 588987

UK (PLYMOUTH) coordinator 244˙807.84

Mappa


 Word cloud

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

aerosol    remote    biogeochemical    training    seawater    models    dissolution    iron    community    ocean    scientific    nature    samples    global    transport    bermuda    variables    atmospheric    climate   

 Obiettivo del progetto (Objective)

'The distribution of iron in the oceans is known to have a significant impact on carbon and nitrogen biogeochemical cycles and climate variability due to its role as a growth limiting nutrient for phytoplankton. The principle mechanism for iron transport to remote open ocean surface water is via the atmospheric transport of aerosol material. Hence an accurate understanding of the controlling variables for dissolution of aerosol iron in seawater is required to advance and improve global biogeochemical models. The aim of the proposed work is to conduct a rigorous study of aerosol iron dissolution in seawater by mimicking the conditions and variables of the air/sea interface that will affect the process. The study will test the hypothesis that the physico-chemical nature of seawater controls this dissolution process rather than the nature of the aerosol deposited. To address this, ship-board and laboratory dissolution experiments will be conducted following the collection and characterisation of aerosol and seawater samples from the Bermuda Atlantic Time Series region. The project will be based at the Bermuda Institute of Ocean Sciences (BIOS) and at the University of Plymouth (UoP) host institutions. The collaborative work will benefit the EU scientific community and strengthen the researcher’s profile by offering high level training in atmospheric sampling and handling and a variety of analytical techniques for the determination of dissolved iron species in seawater. It will also allow continued and frequent access to open ocean seawater and aerosol samples as well as interdisciplinary training in meteorology, oceanography and remote sensing. The results from the study will further contribute to the international scientific community by better constraining iron transport for global biogeochemical models and improving predictions of the effects of climate change, ocean acidification, anthropogenic emissions and modifications to land use and vegetation.'

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