Dr Andrew Murray, Reader in Metabolic Physiology from the Department of Physiology, Development and Neuroscience discusses the body’s responses to altitude and considers the different evolutionary strategies adopted by Sherpas and other high-altitude dwelling people.
As we ascend to high altitude, our bodies experience low oxygen availability - a condition known as hypoxia. In response, our heart rate and breathing rate are adjusted in an attempt to maintain oxygen supply to our vital organs, whilst levels of oxygen-carrying red cells increase in our blood. Despite this, we are limited by the low oxygen available to us, and this impacts on our ability to think and exercise. In human populations that have spent thousands of years residing at altitude, such as the Himalayan Sherpas, there has been a selection of genetic variations which enable them to live, work and reproduce in this environment.
In this talk, Andrew Murray will discuss work that he has carried out for more than 15 years and across two major research expeditions in collaboration with the Xtreme Everest Research Group. Andrew will look at some of the paradoxes of our own bodies' responses to altitude, and consider the different evolutionary strategies adopted by Sherpas and other high-altitude dwelling people.
Finally, Andrew will describe how this research is beginning to help in the treatment of patients who are experiencing hypoxia in other life-threatening contexts, such as the intensive care unit.
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Volcanoes are hazardous and beautiful manifestations of the dynamic processes that have shaped our planet. Volcanoes impact our environment in numerous ways. Over geological time volcanic activity has resurfaced the Earth and provided life with a terrestrial substrate upon which to proliferate. Volcanic degassing has shaped our secondary atmosphere and as part of the process of plate tectonics, maintained just the right amount of water and carbon dioxide at the surface to produce a stable and equitable climate. Magma in the subsurface in volcanic environments today gives Society geothermal energy. The fluids degassed from magmas in the plumbing systems of volcanoes give rise to hydrothermal ore deposits, the source of much of our copper and other metals, critical to the energy transition. In this lecture I will describe the nature and importance of magma degassing for our atmosphere and oceans, as a source of both pollutants and nutrients, and in the formation of mineral deposits. I will describe my own research in carrying out measurements of volcanic gases (using a range of spectroscopic methods, from the ground and using drones), and analysis of erupted lavas, to understand the chemistry and physics of volcanic outgassing and its role in sustaining our planetary environment.
One of the many outstanding achievements of G I Taylor was the discovery of relatively simple statistical laws that apply to highly complex turbulent flows. The emergence of simple laws from complexity is well known in other branches of physics, for example the emergence of the laws of heat conduction from molecular dynamics. Complexity can also arise at large scales, and the structural vibration of an aircraft or a car can be a surprisingly difficult phenomenon to analyse, partly because millions of degrees of freedom may be involved, and partly because the vibration can be extremely sensitive to small changes or imperfections in the system. In this talk it is shown that the prediction of vibration levels can be much simplified by the derivation and exploitation of emergent laws, analogous to some extent to the heat conduction equations, but with an added statistical aspect, as in turbulent flow. The emergent laws are discussed and their application to the design of aerospace, marine, and automotive structures is described. As an aside it will be shown that the same emergent theory can be applied to a range of problems involving electromagnetic fields.
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