public through the writings of H. G. Wells, in his 1913 novel The World Set Free. Sir Henry Tizard's Committee on the Scientific Survey of Air Defence was originally formed to study the needs of anti-aircraft warfare, but branched out to study air warfare generally. In May 1939, a few months before the outbreak of the Second World War in Europe in September 1939, it was directed to conduct research into the feasibility of atomic bombs. Tizard tasked George Paget Thomson, the professor of physics at Imperial College London, and Mark Oliphant, an Australian physicist at the University of Birmingham, with carrying out a series of experiments on uranium. By February 1940, Thomson's team had failed to create a chain reaction in natural uranium, and he had decided that it was not worth pursuing. Oliphant's team reached a strikingly different conclusion. He had delegated the task to two German refugee scientists, Rudolf Peierls and Frisch, who could not work on the university's secret projects like radar because they were enemy aliens, and therefore lacked the necessary security clearance. They calculated the critical mass of a metallic sphere of pure uranium-235, and found that instead of tons, as everyone had assumed, as little as would suffice, and would explode with the power of thousands of tons of dynamite. Oliphant took the Frisch–Peierls memorandum to Tizard. As a result, the MAUD Committee was established to investigate further. It directed an intensive research effort. Four universities provided the locations where the experiments were taking place. The University of Birmingham undertook theoretical work, such as determining what size of critical mass was needed for an explosion. This group was run by Peierls, with the help of fellow German refugee scientist Klaus Fuchs. The laboratories at the University of Liverpool and the University of Oxford experimented with different types of isotope separation. Chadwick's group at Liverpool dealt with thermal diffusion, a phenomenon observed in mixtures of mobile particles where the different particle types exhibit different responses to the force of a temperature gradient. Francis Simon's group at Oxford investigated the gaseous diffusion, which works on the principle that at differing pressures uranium 235 would diffuse through a barrier faster than uranium 238. This was determined to be the most promising method. Egon Bretscher and Norman Feather's group at Cambridge investigated whether another element, now called plutonium, could be used as a fissile material. Because of