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PhD position on ID14: Linking Elasticity of (Mg₁₋ₓFeₓ)O to Seismic Anomalies in Earth’s Lower Mantle
) beamline team at ESRF composed of 8 people and study the elastic properties across the spin transition in Ferropericlase-Magnesiowüstite at extreme conditions to link the elasticity of (Mg₁₋ₓFeₓ)O to seismic
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-ray Photon Correlation Spectroscopy (XPCS), Quasi-Elastic Neutron Scattering (QENS) and Dynamic Light Scattering (DLS) techniques to study the structure and dynamics of proteins in solutions
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cost-effective offshore wind development. Project objectives: · Classify marine sediment types by integrating direct and indirect geotechnical measurements. · Quantify acoustic and elastic
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cost-effective offshore wind development. Project objectives: · Classify marine sediment types by integrating direct and indirect geotechnical measurements. · Quantify acoustic and elastic
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mechanics of two-dimensional bodies by incorporating active effects to study the competition between elasticity and controlled actuation in shaping slender objects. Theoretical discrete modelling. Establish
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economical aspect to the technology. Study the techno-economic trade-offs of MR technology by designing and performing aero-servo-elastic analysis of MR wind turbines with various number of rotors and power
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between closely related structures. An alternative approach to characterise the microstructure is through acoustic methods that exploit the different elastic behaviour of the phases present. In this PhD
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Project summary Liquid crystal elastomers are an exciting class of soft materials that combine the orientational order of liquid crystals with the elasticity of polymers. This gives rise to remarkable
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Correlation Spectroscopy (XPCS), Quasi-Elastic Neutron Scattering (QENS) and Dynamic Light Scattering (DLS) techniques to study the structure and dynamics of proteins in solutions. Qualification and skills
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distances. Fluvial processes such as bedload transport and turbulence generate elastic deformations of the Earth's surface, producing measurable seismic signals. This principle forms the foundation