P. Bouisset scite author profile

ABSTRACT. The response of Arctic ice masses to climate change is studied using ice cores containing information on past climatic and environmental features. Interpretation of this information requires accurate chronological data. Absolute dating of ice cores from sub-polar Arctic glaciers is possible using well-known radioactive layers deposited by atmospheric nuclear tests (maximum fallout in 1963) and the Chernobyl accident (1986

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Assessing Exposure to Cosmic Radiation during Long-haul Flights

Bottollier-Depois¹,

Chau²,

Bouisset³

et al. 2000

Radiation Research

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Anomalous population of deep capture states of fast ions emerging from solid foils

et al. 1987

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P. Bouisset

210Pb and Caesium Accumulation in the Rhône Delta Sediments

Long-Core Profiles of 137 Cs, 134 Cs, 60 Co and  210 Pb in Sediment near the Rhone River (Northwestern Mediterranean Sea)

Ice cores from Arctic sub-polar glaciers: chronology and post-depositional processes deduced from radioactivity measurements

Assessing Exposure to Cosmic Radiation during Long-haul Flights

Anomalous population of deep capture states of fast ions emerging from solid foils

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P. Bouisset

210Pb and Caesium Accumulation in the Rhône Delta Sediments

Long-Core Profiles of 137 Cs, 134 Cs, 60 Co&nbsp;and&nbsp; 210 Pb in Sediment near the Rhone River (Northwestern Mediterranean Sea)

Ice cores from Arctic sub-polar glaciers: chronology and post-depositional processes deduced from radioactivity measurements

Assessing Exposure to Cosmic Radiation during Long-haul Flights

Anomalous population of deep capture states of fast ions emerging from solid foils

Contact Info

Product

Resources

About

Long-Core Profiles of 137 Cs, 134 Cs, 60 Co and 210 Pb in Sediment near the Rhone River (Northwestern Mediterranean Sea)