Even though we live on the surface of the Earth, its mantle in many ways remains a mystery. In particular, there are some fundamental properties of the rocks that comprise the mantle, thousands of kilometers beneath our feet, which remain poorly understood. This is one of the biggest barriers to better understanding the history and future of the Earth as a whole. The reason for this is that the principle technique we have for understanding what is inside the Earth is seismology, which uses knowledge of the physical properties of mantle minerals to convert the wave speeds inferred from seismic studies into a physical model of the mantle. In this research project, you will attempt to solve some of the key open questions regarding the mineral physics of the mantle—the effect of electronic spin state and exsolution on the properties of the mantle mineral ferropericlase.
The spin transition is the pairing of the d-electrons of iron in ferropericlase, as it is compressed, with depth in the lower mantle. This is observed in high-pressure experiments and leads to a density increase, as the volume of iron ions rapidly decrease. However, there are presently significant differences in the results of studies predicting the conditions at which the spin transition occurs and also between mineral physics models and seismic observations. Consequently, interpretations in terms of dynamic processes in the mantle currently remain unreliable. Exsolution of ferropericlase is the process, where it separates into Mg-rich and Fe-rich phases, which has also been reported in high-pressure experiments. This could be an explanation for the discrepancy between current mineral physics models and seismic observations. However, the effect of exsolution has never been studied.
It is important to be able to map out the spin state of iron in ferropericlase, as it influences the dynamics of the mantle. This ultimately provides the driving forces for surface processes such as plate tectonics, as well as deep mantle processes that impact on core dynamics and magnetic field generation. It does this in several ways. The spin transition changes the (radiative) thermal conductivity and viscosity of ferropericlase, which impacts mantle flow. In addition, the increase/decrease in the density of ferropericlase passing through the spin transition, as it sink/rises in the mantle, leads to a decrease/increase in buoyancy. Exsolution is also important, due to its role in controlling spin state, as the spin transition pressure increases with iron-content.
In this project theoretical calculation will be performed to constrain the depth and breadth of the spin transition and exsolution reaction in ferropericlase, as a function of iron-content,
using the Vienna Ab Initio Simulation Package (VASP). These will allow investigation of how the spin transition is influenced by composition and the arrangement of iron (i.e. whether all the iron atoms are close together in a cluster or evenly spread out). This latter has been previously reported to influence the spin transition and our preliminary calculations indicate it is important. Your research will be carried out in collaboration with the group of Dr Hauke Marquardt at the Department of Earth Sciences, at the University of Oxford, who will be carrying out parallel experimental investigations.
The overall aim of this project is to develop an accurate mineral physics model of the spin transition in ferropericlase, taking into account exsolution, and use it to help interpret seismic observations of the lower mantle. In particular, you will:
1. Constrain the depth and breadth of the spin transition in ferropericlase and its compositional dependence, including the influence of cation ordering.
2. Constrain the depth and breadth of exsolution reaction in ferropericlase and its compositional dependence.
3. Determine the elastic properties of ferropericlase as a function of spin state temperature, pressure, and composition.
4. Predict the influence of the spin transition and exsolution in ferropericlase on seismic velocities and compare them with seismic observations.
The results will provide a constrained set of parameters that can be used for thermodynamic modeling, modeling of mantle dynamics, and mapping of lower mantle processes, to provide more accurate models of past and present-day mantle structure and dynamics.
https://panorama-dtp.ac.uk/research/the-spin-deep-within-physics-of-ferropericlase-in-the-earths-lower-mantle/
Continue with Facebook
