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Theodore von Kármán, distinguished scientist and engineer with many interests, was born in Budapest on 11 May 1881. His father, Maurice von Kármán, a prominent educator and philosopher at the University of Budapest, had a significant influence over his early intellectual development. After graduating from the Royal Technical University of Budapest in 1902 with a degree in mechanical engineering, von Kármán published in 1906 the first of a long string of papers concerning solid mechanics problems outside the domain of linear elasticity theory, in this case on the compression and buckling of columns. In that same year, apparently at the urging of his father, von Kármán left Hungary for graduate studies at Göttingen. For his 1908 PhD, supervised by Ludwig Prandtl, he developed the concepts of reduced-modulus theory and their application to column behavior such as buckling. Later, with H.-S. Tsien and others, he developed a nonlinear theory for the buckling of curved sheets. His final work in solid mechanics was on the propagation of waves of plastic deformation published as a classified report in 1942 and in the open literature in 1950. In von Kármán's words:
It was another version of the problem I had solved for my doctor's thesis, in which I had extended Euler's classical theory of buckling to a situation beyond the elastic limit.
On 3 April 1920, a few years after G.I. Taylor's far-reaching observations of turbulent diffusion aboard the SS Scotia (Taylor, 1921), and at the time Lewis Fry Richardson was imagining vast weather simulations of atmospheric flow by human ‘computers’ (Richardson, 1922), across the Atlantic in the city of Philadelphia, Stanley Corrsin was born. His parents, Anna Corrsin (née Schorr) and Herman Corrsin had both emigrated to the United States only 13 years before. They came from Romania, where many Russian Jews had settled after leaving Russia in the late 19th and early 20th century. Following further hostilities in Romania, many emigrated again, this time to America. Anna and Herman Corrsin arrived separately at Ellis Island in 1907, Anna in July, and Herman in October. After brief stays in the New York and New Jersey area, where they met and married in 1912, they settled in the city of Philadelphia, in a mixed middle-class neighborhood, not far from the University of Philadelphia. They went into business in the clothing industry and raised their children. Their first son Eugene died young and their second, Lester, was born in 1918. Stan was their third and youngest son.
As a child, Stan Corrsin attended school in Philadelphia and, showing early signs of a highly gifted analytical mind, went on to skip two grades. He enjoyed following the ups and downs of his favorite baseball team, the Philadelphia Athletics.
Robert Harry Kraichnan (1928–2008) was one of the leaders in the theory of turbulence for a span of about forty years (mid-1950s to mid-1990s). Among his many contributions, he is perhaps best known for his work on the inverse energy cascade (i.e. from small to large scales) for forced two-dimensional turbulence. This discovery was made in 1967 at a time when two-dimensional flow was becoming increasingly important for the study of large-scale phenomena in the Earth's atmosphere and oceans. The impact of the discovery was amplified by the development of new experimental and numerical techniques that allowed full validation of the conjecture.
How did Kraichnan become interested in turbulence? His earliest scientific interest was in general relativity, which he began to study on his own at age 13. At age 18 he wrote at MIT a prescient undergraduate thesis, Quantum Theory of the Linear Gravitational Field; he received a PhD in physics from MIT in 1949 for his thesis, Relativistic Scattering of Pseudoscalar Mesons by Nucleons, supervised by Herman Feshbach. His interest in turbulence arose in 1950 while assisting Albert Einstein in search for highly nonlinear, particlelike solutions to unified field equations.
The nature of turbulent flow has presented a challenge to scientists over many decades. Although the fundamental equations describing turbulent flows (the Navier–Stokes equations) are well established, it is fair to say that we do not yet have a comprehensive theory of turbulence. The difficulties are associated with the strong nonlinearity of these equations and the non-equilibrium properties characterizing the statistical behaviour of turbulent flow. Recently, as predicted by von Neumann 60 years ago, computer simulations of turbulent flows with high accuracy have become possible, leading to a new kind of experimentation that significantly increases our understanding of the problem. The largest numerical simulations nowadays use a discretized version of the Navier–Stokes equations with several billion variables producing many terabytes of information that may be analyzed by sophisticated statistical tools and computer visualization. None of these tools were available in the 1920s when some of the most fundamental concepts in turbulence theory were introduced through the work of Lewis Fry Richardson (1881–1953). Although his name is not as well-known as other contemporary eminent scientists (e.g. Einstein, Bohr, Fermi) and although his life was spent outside the mainstream of academia, his discoveries (e.g. the concept of fractal dimension) are now universally known and essential in understanding the physics of complex systems.
George Batchelor (1920–2000), whose portrait (1984) by the artist Rupert Shephard is shown in Figure 8.1, was undoubtedly one of the great figures of fluid dynamics of the twentieth century. His contributions to two major areas of the subject, turbulence and low-Reynolds-number microhydrodynamics, were of seminal quality and have had a lasting impact. At the same time, he exerted great influence in his multiple roles as founder Editor of the Journal of Fluid Mechanics, co-Founder and first Chairman of EUROMECH, and Head of the Department of Applied Mathematics and Theoretical Physics (DAMTP) in Cambridge from its foundation in 1959 until his retirement in 1983.
I focus in this chapter on his contributions to the theory of turbulence, in which he was intensively involved over the period 1945 to 1960. His research monograph The Theory of Homogeneous Turbulence, published in 1953, appeared at a time when he was still optimistic that a complete solution to ‘the problem of turbulence’ might be found. During this period, he attracted an outstanding group of research students and post-docs, many from his native Australia, and Senior Visitors from all over the world, to work with him in Cambridge on turbulence. By 1960, however, it had become apparent to him that insurmountable mathematical difficulties in dealing adequately with the closure problem lay ahead.
Philip G. Saffman was a leading theoretical fluid dynamicist of the second half of the twentieth century. He worked in many different sub-fields of fluid dynamics and, while his impact in other areas perhaps exceeded that in turbulence research, which is the topic of this article, his contributions to the theory of turbulence were significant and remain relevant today. He was also an incisive and, some might conclude, a somewhat harsh critic of progress or what he perceived as the lack thereof, in solving ‘the turbulence problem’. This extended to his own work; he stated in a preface to lectures on homogeneous turbulence (Saffman, 1968) that
the ideas … are new and hopefully important, but are speculative and quite possibly in serious error.
In this article, we will try to survey Saffman's thinking and contribution to turbulence research from the mid 1950s, when he began to mature as a scholar, until the late 1970s when he moved away from the study of turbulence to concentrate on the related but separate area, of the dynamics of isolated and interacting vortices. Although, for the most part, the evolution of his ideas and their application to turbulence in this period developed both thematically and chronologically together, where there are departures we will tend to focus on the former.
I have dream'pt of bloudy turbulence, and this whole night hath nothing seen but shapes and forms …
Shakespeare (1606): Troilus and Cressida, V, iii, 11
“Will no-one rid me of this turbulent priest?” So, according to tradition, cried Henry II, King of England, in the year 1170, even then conveying a hint of present frustration and future trouble. The noun form ‘la turbulenza’ appeared in the Italian writings of that great genius Leonardo da Vinci early in the 16th century, but did not appear in the English language till somewhat later, one of its earliest appearances being in the quotation above from Shakespeare. In his “Memorials of a Tour in Scotland, 1803”, William Wordsworth wrote metaphorically of the turmoil of battles of long ago: “Yon foaming flood seems motionless as ice; its dizzy turbulence eludes the eye, frozen by distance …”. Perhaps we might speak in similar terms of long-past intellectual battles concerning the phenomenon of turbulence in the scientific context.
Turbulence in fluids, or at least its scientific observation, continued to elude the eye until Osborne Reynolds in 1883 conducted his brilliant ‘flow visualisation’ experimental study “of the circumstances which determine whether the motion of water shall be direct or sinuous, and of the law of resistance in parallel channels”.
Articles on Osborne Reynolds' academic life and published works have appeared in a number of publications beginning with a remarkably perceptive anonymous obituary notice published in Nature within eight days of his death (on 21 February 1912) and a more extensive account written by Horace Lamb, FRS, and published by the Royal Society (Lamb, 1913) about a year later. More recent reviews have been provided by Gibson (1946), a student of Reynolds and later an academic colleague, by Allen (1970), who provided the opening article in a volume marking the passage of 100 years from Reynolds taking up his chair appointment at Manchester in 1868, and by Jackson (1995), in an issue of Proc. Roy. Soc. celebrating the centenary of the publication of Reynolds' 1895 paper on what we now call the Reynolds decomposition of the Navier–Stokes equations, about which more will be said later in the present chapter. A significant portion of the present account is therefore devoted to Reynolds' family and background and to hitherto unreported aspects of his character to enable his contributions as a scientist and engineer to be viewed in the context of his life as a whole. While inevitably some of what is presented here on his academic work will be known to those who have read the articles cited above, archive material held by the University of Manchester and The Royal Society and other material brought to light in the writers' personal enquiries provide new perspectives on parts of his career.
Albert Alan Townsend was born on the 22nd of January 1917 in Melbourne Australia son of Albert Rinder Townsend and Daisy Townsend née Gay. At the time of his birth his father was a clerk in the accounts branch of the Department of Trade and Customs – he also served as secretary of the Commonwealth Film Censorship Board. His father went on to have a very successful career in the Commonwealth public service. As his career evolved he moved the family to Canberra in the ACT (Australian Capital Territory) which is the seat of the government in Australia. Albert and Daisy had three children: Alan, Elisabeth and Neil. In 1933 Albert Rinder Townsend was awarded the OBE.
Alan obtained his Leaving Certificate in 1933 from the Telopea Park High School with an outstanding pass, including first-class honours in mathematics, and the Canberra University College Council awarded him a scholarship of £120 a year to pursue a science course at Melbourne University. He completed his Bachelor of Science in 1936, graduating with first-class honours, and started his Master of Science. Just before his 20th birthday (1937) he graduated Master of Science, with honours in natural philosophy and pure mathematics. He was awarded the Dixson Research Scholarship and the Professor Kernot Research Scholarship.
The towering figure of Kolmogorov and his very productive school is what was perceived in the twentieth century as the Russian school of turbulence. However, important Russian contributions neither start nor end with that school.
Physicist and pilot
… the bombs were falling almost the way the theory predicts. To have conclusive proof of the theory I'm going to fly again in a few days.
A.A. Friedman, letter to V.A. Steklov, 1915
What seems to be the first major Russian contribution to the turbulence theory was made by Alexander Alexandrovich Friedman, famous for his work on non-stationary relativistic cosmology, which has revolutionized our view of the Universe. Friedman's biography reads like an adventure novel. Alexander Friedman was born in 1888 to a well-known St. Petersburg artistic family (Frenkel, 1988). His father, a ballet dancer and a composer, descended from a baptized Jew who had been given full civil rights after serving 25 years in the army (a so-called cantonist). His mother, also a conservatory graduate, was a daughter of the conductor of the Royal Mariinsky Theater. His parents divorced in 1897, their son staying with the father and becoming reconciled with his mother only after the 1917 revolution. While attending St. Petersburg's second gymnasium (the oldest in the city) Friedman befriended a fellow student Yakov Tamarkin, who later became a famous American mathematician and with whom he wrote their first scientific works (on number theory, received positively by David Hilbert).
To Co-operate with the Polar Expeditions: Performed in His Majesty's Ship Blossom, under the Command of Captain F. W. Beechey in the years 1825, 26, 27, 28
Frederick William Beechey (1796–1856), naval officer and hydrographer, was born into a family of artists, joined the Navy at a young age and went on to travel the world to survey coastlines and oceans. He published several accounts of his expeditions to destinations including the Arctic and Africa. This two-volume work, first published in 1831, describes his voyage as commander of the Blossom in 1825–1828. The ship's mission was to support the exploration of the North-West Passage by travelling eastwards via the Bering Strait to meet the explorers Sir John Franklin and Sir Edward Parry who were travelling west from the North Atlantic. Volume 2 follows the expedition from California, where it had overwintered, via Hawai'i and China, back to the Bering Strait for a second summer. It includes a vocabulary of Eskimo words, notes on harbours and navigation, and a vivid description of the northern lights.
This short but distinctive paper was published in 1835 by Charles Daubeny (1795–1867), who began his career as a physician but soon found his passion to be volcanos. At this time, Daubeny held chairs in chemistry and botany at Oxford. He had made many field trips to European volcanic regions between 1819 and 1825, was elected a Fellow of the Royal Society in 1822, and in 1826 published the first edition of his famous Description of Active and Extinct Volcanos, of which a later version also appears in this series. Here Daubeny describes a winter trip to the Apulia (Puglia) region in the south-east of Italy, rarely described by travel writers of his time, to visit Lake Amsanctus, famously mentioned by Virgil, and the extinct volcano Mount Vultur. Although Daubeny's overall focus is scientific, his account also includes lively descriptions of classical remains and rural society in southern Italy.
John Playfair (1748–1819) was a Scottish mathematician and geologist best known for his defence of James Hutton's geological theories. He attended the University of St Andrews, completing his theological studies in 1770. In 1785 he was appointed joint Professor of Mathematics at the University of Edinburgh, and in 1805 he was elected Professor of Natural Philosophy. A Fellow of the Royal Society, he was acquainted with continental scientific developments, and was a prolific writer of scientific articles in the Transactions of the Royal Society of Edinburgh and the Edinburgh Review. This four-volume edition of his works was published in 1822 and is prefaced by a biography of Playfair. Volume 2 contains the incomplete Dissertation exhibiting a general view of the progress of mathematical and physical science, which was included as a supplement to the Encyclopaedia Britannica.
John Playfair (1748–1819) was a Scottish mathematician and geologist best known for his defence of James Hutton's geological theories. He attended the University of St Andrews, completing his theological studies in 1770. In 1785 he was appointed joint Professor of Mathematics at the University of Edinburgh, and in 1805 he was elected Professor of Natural Philosophy. A Fellow of the Royal Society, he was acquainted with continental scientific developments, and was a prolific writer of scientific articles in the Transactions of the Royal Society of Edinburgh and the Edinburgh Review. This four-volume edition of his works was published in 1822 and is prefaced by a biography of Playfair. Volume 4 contains his biographies of his colleagues, and review articles on mathematical and astronomical works, both in English and French.
John Murray (1778–1820) was a public lecturer and writer on chemistry and geology. After attending the University of Edinburgh he became a popular public lecturer on chemistry and pharmacy. He was also a prolific writer of chemistry textbooks which were widely used in British universities. This popular volume, first published anonymously in 1802, contains Murray's critical response to John Playfair's volume Illustrations of the Huttonian Theory of the Earth, also published in 1802 and re-issued in this series. In this volume Murray clearly describes both the competing Huttonian and Neptunian (also known as Wernerian) theories of rock formation. Using much of the same geological evidence as Playfair, Murray also objectively analyses the theories' claims through rock and fossil formations and concludes in support of the Wernerian theory. This valuable volume explores one of the major geological controversies of the period and illustrates the main contemporary criticisms of Hutton's work.
James Hutton (1726–1797) was an eminent Scottish scientist known chiefly for his work in geology. Educated at Edinburgh University, Hutton then travelled to Europe to study medicine before going into industry. He spent over a decade farming his family property in Scotland before returning to academic and commercial life. Hutton became an established geologist who also published on chemistry, meteorology and philosophy as an active member of the Edinburgh Royal Society. This volume, first published in 1805, is a detailed and affectionate chronicle of Hutton's life by his close friend, geologist and mathematician John Playfair. The author recounts Hutton's academic career, speculates on the motivation behind his foray into farming and includes a detailed discussion of his main geological theories. With little of Hutton's correspondence and papers surviving, this account by an intimate contemporary is the key resource for studying the life of an intriguing figure in scientific history.
Sir Roderick Impey Murchison (1792–1871) was an influential Scottish geologist best known for his classification of Palaeozoic rocks into the Silurian system. After early military experience in the Peninsular War, he resigned his commission; a chance meeting with Sir Humphrey Davy led him subsequently to pursue a scientific career. The Silurian System, published in 1839, was a highly influential study, which established the oldest contemporary classification of fossil-bearing strata. Murchison was appointed President of the Royal Geographical Society in 1843. These volumes, first published in 1875, use information taken from Murchison's private journals and correspondence. Archibald Geikie (1835–1924) provides a detailed account of his mentor's life and work in the context of geology as a developing science in the early nineteenth century, and provides a fascinating insight into the life and work of this eminent Victorian geologist. Volume 1 describes Murchison's early life and geological studies until 1842.
Sir Roderick Impey Murchison (1792–1871) was an influential Scottish geologist best known for his classification of Palaeozoic rocks into the Silurian system. After early military experience in the Peninsular War, he resigned his commission; a chance meeting with Sir Humphrey Davy led him subsequently to pursue a scientific career. The Silurian System, published in 1839, was a highly influential study, which established the oldest contemporary classification of fossil-bearing strata. Murchison was appointed President of the Royal Geographical Society in 1843. These volumes, first published in 1875, use information taken from Murchison's private journals and correspondence. Archibald Geikie (1835–1924) provides a detailed account of his mentor's life and work in the context of geology as a developing science in the early nineteenth century, and provides a fascinating insight into the life and work of this eminent Victorian geologist. Volume 2 describes his later life, from 1843 to 1871.
The Probable Causes of their Phenomena, the Laws Which Determine their March, the Disposition of their Products, and their Connexion with the Present State and Past History of the Globe
George Julius Poulett Scrope (1797–1876) published Considerations on Volcanos in 1825. The work contains the results of his observations of volcanos in the volcanic regions of central France, Italy and Germany. It includes scientific descriptions of all volcanos in these areas, with each categorised according to its level of activity, main characteristics and geological history. Scope's work was one of the first attempts at a comprehensive theory of volcanic action and an understanding of the significance of volcanos as evidence for the earth's history. Scrope argued that volcanos should be studied in terms of known geological processes, and that 'non-catastrophic' causes should be considered to explain their formation. He argued that a gradual cooling of the earth was key to the formation of volcanos. This is a major work of nineteenth-century geology that sets out many of the principles still followed in vulcanology.
Sir Humphry Davy (1778–1829) was a hugely influential chemist, inventor, and public lecturer who is recognised as one of the first professional scientists. He was apprenticed to an apothecary in 1795, which formed his introduction to chemical experiments. A chance meeting with Davis Giddy in 1798 introduced Davy into the wider scientific community, and in 1800 he was invited to a post at the Royal Institution, where he lectured to great acclaim. These volumes, first published in 1831, contain Davy's official biography. Researched and written by John Ayrton Paris, the work describes in detail Davy's life and his scientific studies. Organised chronologically with excerpts from his private correspondence, Davy's early life and his experiments and lectures at the Royal Institution and his Presidency of the Royal Society between 1820 and 1827 are explored in vivid detail. Volume 2 describes his life and work between 1812 and 1829.