A5087143839- Radioactive contamination and transfer
- Radioactivity and Radon Measurements
- Nuclear and radioactivity studies
- Marine and coastal ecosystems
- Oceanographic and Atmospheric Processes
- earthquake and tectonic studies
- Coastal and Marine Dynamics
- Radioactive element chemistry and processing
- Groundwater and Isotope Geochemistry
- Geological and Geophysical Studies Worldwide
- Marine and environmental studies
- Geology and Paleoclimatology Research
- Atmospheric and Environmental Gas Dynamics
- Geological formations and processes
- Oil Spill Detection and Mitigation
- Methane Hydrates and Related Phenomena
- Groundwater flow and contamination studies
- Arctic and Antarctic ice dynamics
- Atmospheric chemistry and aerosols
- Soil and Water Nutrient Dynamics
- Wind and Air Flow Studies
- Archaeological and Historical Studies
- Geochemistry and Elemental Analysis
- Hydrology and Sediment Transport Processes
- Coastal wetland ecosystem dynamics
Universidad de Sevilla
2015-2024
Korea Atomic Energy Research Institute
2013
ETH Zurich
2013
Japan recently announced plans to discharge over 1.2 million tons of radioactive water from the Fukushima Daiichi Nuclear Power Plant (FDNPP) into Pacific Ocean. The contaminated can poses a threat marine ecosystems and human health. To estimate impact plan, here, we developed three-dimensional global model track transport dispersion tritium released FDNPP. pollution scenarios for four release durations (1 month, 1 year, 5 years, 10 years) were simulated. simulation results showed that in...
About six million years ago, the Mediterranean Sea underwent a period of isolation from ocean and widespread salt deposition known as Messinian Salinity Crisis (MSC), allegedly leading to kilometer-scale level drawdown by evaporation. One competing scenarios proposed for termination this environmental crisis 5.3 ago consists megaflooding event refilling through Strait Gibraltar: Zanclean flood. The main evidence supporting hypothesis is nearly 390 km long several hundred meters deep erosion...
The termination of the Messinian salinity crisis 5.33 million years ago is often attributed to Zanclean megaflood, a catastrophic event that rapidly refilled Mediterranean Sea. This study provides compelling evidence for this tracing its impact from an onshore shallow marine corridor in southeastern Sicily offshore Noto Canyon. Key indicators include (i) over 300 streamlined, asymmetrical erosional ridges aligned with flood direction, (ii) poorly sorted breccia layer situated between and...