CRONUS-EU · Cosmic ray produced nuclide systematics on earth - the European contribution
FP6 — Marie Curie Actions (Human Resources and Mobility)
- Duration
- 2004-12-01 → 2008-11-30
- EU contribution
- €3,423,149
- Participants
- 9
- Scheme
- RTN
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Results in brief
Final Activity Report Summary - CRONUS-EU (Cosmic ray produced nuclide systematics on earth - the European contribution)
Quantifying the processes that shape the Earth's surface is central to the Earth and environmental sciences. A key requirement is the ability to establish accurate absolute chronologies and rates of landscape evolution. The development of techniques to measure exceedingly low concentrations of cosmogenic isotopes that accumulate in surface rocks and soils during exposure to cosmic rays has led to an unprecedented ability to establish chronologies of environmental change over the past few thousand to several millions of years. The use of cosmogenic nuclides has revolutionised Earth surface sciences over the last decade and they form the cornerstone for the new quantitative Earth surface sciences, which are progressively replacing the traditionally qualitative techniques used in such disciplines. Advanced current applications demand accuracy of age determinations better than ~5 %. Analytical uncertainties are usually low (2-3 %). However, until recently the theoretical and empirical foundation to consistently calculate production rates of in situ produced Terrestrial cosmogenic nuclides (TCN) was only 10-20 %. The research program conducted within CRONUS-EU, in collaboration with the United States (US)-American sister initiative CRONUS-Earth, effectively reduced the remaining uncertainties in TCN systematics to better than 5 %, removing the obstacles for advanced applications. This occurred through experiments that refined decay constants of cosmogenic radionuclides, direct production rate determinations, laboratory cross calibrations and advanced numerical modelling. This joint research effort has delivered protocols to reliably calculate exposure ages from cosmogenic nuclide concentrations in rocks. The activities of CRONUS-EU significantly raised the profile and the use of cosmogenic nuclide methodology in Europe; a field where Europe had been seriously lagging behind the US. In the six years since the idea of CRONUS-EU was conceived, three new dedicated accelerator mass spectrometer facilities for the analysis of cosmogenic nuclides became online, or are commissioned in Europe (Aix-en-Provence, Cologne, Rossendorf). Training of young scientists recruited by CRONUS-EU (5 Phd students and 10 Postdoctoral researchers) was a prerequisite to conduct the work program of CRONUS-EU. The relevant knowledge base in Europe was limited prior to CRONUS-EU, and was concentrated at few centres. Training occurred in a series of network wide training events throughout Europe, and a summer school that was aimed to the wider scientific community. 90 % of the postdoctoral researchers that were employed by CRONUS-EU continue their research in Europe, about half in permanent research positions. This new generation of 'cosmogenic' researchers has a fully equitable gender balance, which is rare for natural sciences.
Data: CORDIS, © European Union
Project objective
The development of in situ cosmogenic nuclides as a tool for quantifying rates and timing of Earth surface processes has revolutionised many branches of the Earth and environmental sciences. The principal aim of CRONUS-EU is to establish a nucleus of cosmo genic nuclide-literate young research scientists capable of providing the wider European science community the tools to remain at the forefront of their fields. Since its conception in the mid-1980¿s there has been an explosion in the use in situ cosmogeni c nuclides such that it has become the principal quantitative chronological technique for Earth surface process studies, and has provided invaluable chronological constraints on the timing and rates of environmental change (e.g glacial histories, erosion) and hazard recurrence frequency (e.g. landslides, volcanic and seismic activity). However, while the costly, but necessary, research infrastructure is now in place in Europe, the widespread application of the technique has been severely restricted by two p rincipal limitations; (i) the absence of scientists in Europe with the necessary skills to identify, prepare and analyse appropriate material, and (ii) the yet outstanding full calibration of the intrinsic physical laws, such as cosmic ray attenuation and nuclide production at Earth's surface. CRONUS-EU will use a series of rigorous multi-disciplinary studies aimed at improving the accuracy of ages obtained from cosmogenic isotopes, a prerequisite for future development. By doing so, the necessary skills wi ll be transferred from this small group of experts to the young researchers involved. Training will be facilitated principally through laboratory secondments and specific training courses, and will deliver a critical mass of research scientists equipped wi th the skills necessary for leading the future expansion in the use of the technique.
Original text from CORDIS.
Participants
- UNIVERSITY OF EDINBURGH · EDINBURGHCoordinatorUnited Kingdom
- CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE · PARISFrance
- EIDGENOSSISCHE TECHNISCHE HOCHSCHULE ZURICH · ZURICHCity levelSwitzerland
- GEOFORSCHUNGSZENTRUM POTSDAM · POTSDAMCity levelGermany
- UNIVERSITEIT UTRECHT · UTRECHTNetherlands
- UNIVERSITY OF GLASGOW · GLASGOWUnited Kingdom
- UNIVERZITA KOMENSKÉHO V BRATISLAVE - · BRATISLAVASlovakia
- Universität Hannover · HannoverGermany
- VRIJE UNIVERSITEIT AMSTERDAM · AMSTERDAMNetherlands
Links
Data: CORDIS, © European Union
