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Illustration representative of the book: the Challenger expedition (route, vol. 1), physical measurements (samples, vol. 2) and the compressibility of liquids (globes, vol.3)

From Deep Sea to Laboratory 1

The First Explorations of the Deep Sea by H.M.S. Challenger (1872–1876)

Frédéric Aitken

Jean-Numa Foulc

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Foreword

It is a beautiful adventure that Frédéric Aitken and Jean-Numa Foulc have undertaken, using physical data from the Challenger expedition, the first major oceanographic expedition, sponsored by the British Admiralty in the 1870s. Indeed, this data, temperature and pressure readings at various depths and at multiple points of the world, was relatively little used at the time despite the visionary intuition of one of the initiators of the expedition, Professor Carpenter, that this data would allow for the reconstruction of ocean circulation. The authors attribute this relative lack of interest to the fact that most scientists on the expedition were naturalists, and that from the point of view of biology, the total benefits were already huge, with, for example, the discovery of life at a great depth.

Exploiting data is not the least interesting of the physicist’s tasks. To deal with the problem, we simplify the situation and try not to delete anything essential. The terms of the equations are evaluated, keeping only the most important, and then two situations may arise. Let us say that the discrepancy with the data is clear: we are generally convinced that it has been oversimplified, but where? We are tempted in bad faith to defend our idea, even if it means becoming the Devil’s advocate and destroying what we have built. We go back to the overlooked terms one by one, and, with some luck, this may lead to a new effect. We make do with what we know; the battle is tough, and this is its appeal.

Let us say that the similarity is acceptable. This is when a good physicist is suspicious: is it not a coincidence that two important effects are not offset by any chance? It would be necessary to make a prediction, and to repeat the experiment in different conditions, but it is not always possible. Another boat was not sent out with 200 people around the world for three years! The rigor with which experiments have been conducted, and the confidence that can be placed in the measures, are essential. The experimenters have had to multiply the situations blindly, without knowing which ones would be used as a test, with the sole aim of doing their best every time, by describing their protocol for future use.

The development of the measurement protocol is part of the experiment’s design, as was instrument construction. At that time, a physicist worth his salt would never have used an instrument that he did not know how to build. How can one measure a temperature in a place that one cannot reach oneself (2,000 m below the surface of the sea, for example)? We can record the maximum and minimum temperatures reached during the descent (I found, with much emotion, the description of the maximum and minimum thermometer used by my grandfather in his garden). But what to do for intermediate temperatures? How to make sure that the line does not break in bad weather under the boat’s blows? How to decide the real depth despite currents, and the fact that the line continues to run under its own weight once the sensor is at the bottom? The design phase of the experiment can be exciting: I knew a physicist who was ready to sabotage a barely built experience (under the pretext, of course, of improving it) to be able to move more quickly to the design of the following experiment.

Despite all the attention given to the design, sometimes an error is suspected in the measurements. This is the case here. Having reached unexpected depths (they discovered the Mariana Trench), the Challenger scientists wondered if their measurements had not been distorted by contraction of the glass envelopes. After their return, they assigned Peter Tait, a physicist from Edinburgh, the task of assessing these errors. One thing leading to another, he raised questions about the compressibility of seawater, and other liquids, and so about their equation-of-state, connecting pressure, temperature and density (and even salinity). The result of his studies left a lasting mark on the physics of liquids. Estimating errors, a task hated and despised by the typical physics student, yielded new knowledge.

From the same period as the van der Waals equation, Tait’s efforts were part of the first trials to represent the equation-of-state of dense, liquid and solid bodies by continuous functions. The goal was twofold: metrological, to interpolate between experimental results, and to provide experimenters and engineers with the most accurate characterization of the thermodynamic and physical properties of the fluids they use. But also more fundamental, in the wish to have a better understanding of the underlying physical mechanisms: formation of molecular aggregates, local crystalline order, shape of interaction potentials, etc. These two interests, pragmatism and rigor, are often in conflict, as is clear from the authors’ account, who apply the ideas from that time to fluids that were not of concern then, such as the fluid phases of the two stable isotopes of helium.

Many aspects of this scientific adventure are thus universal, and it is touching to see how the value codes of the scientific approach have been transmitted over decades, or almost centuries. But our step back in time gives us an advantage: the ability to judge the ideas from that period in light of the extraordinary sum of knowledge that has been accumulated since. However, a direct comparison would be unfair and clumsy. It is much more interesting to put us in the mindset of the players of that era, to share their doubts, their hesitations and even their mistakes. This is an aspect that is too often absent from our education. For the sake of efficiency, we do not mention brilliant ideas that have led to a stalemate. Yet these ideas may contribute elsewhere. There may be some hesitation in mentioning great names such as Clausius, Joule and van der Waals, who fill us not only with humility in the face of the mastery that allowed them to find the right path, but also with confidence when faced with our own doubts. The variety of players and points of view that have marked this period show how much science is a collective adventure.

It is all of this that I found in this book by Frédéric Aitken and Jean-Numa Foulc, and even more: the human adventure that was this trip of three years around the world, the incidents, drama and joys, what it revealed about the personality of each participant, their lives which, for some, are also described, the moving relay that is transmitted when a change of assignment, or worse, death, interrupts a task. There is also the welcome reserved for the expedition, sometimes idyllic (ah! the difficulty of leaving Tahiti), sometimes colder, the importance of the band and personal talent of the participants, not to mention the providence that the Challenger represented for the Robinsons, abandoned on an island by a boat that was unable to come back for them. After reading the story based on the logbook, how can we not mention Jules Verne’s novels? It is the same period, that of a thirst for knowledge about our environment, accessible to all of us, acquired by real yet so human adventurers, so close to us. The credit goes to the authors for having dedicated so much time, energy and enthusiasm to this humanist and complete book, with the spirit of this laboratory where I had the pleasure to come for discussions during my years at Grenoble.

Bernard CASTAING

Member of the French Academy of Sciences

Preface

In May 1876, the oceanographic expedition of the H.M.S. Challenger reached England after having sailed the seas of the world for more than three years. The main objectives of this voyage were to study animal life in depth, examine the ocean floor in order to improve the knowledge of undersea reliefs and observe the physical properties of the deep sea. However, while books on animal life following the expedition have been amply highlighted, it was not the same for physical observations accumulated throughout the voyage, as theoretical knowledge of the dynamics of the oceans was then almost non-existent.

Yet as early as 1870, one of the initiators of the Challenger expedition, naturalist William Carpenter, had suggested that the ocean circulation could be reconstructed from depth-dependent water temperature profiles. One of the challenges of the book is to precisely show that measurements collected by the Challenger’s scientists were the potential source of all data necessary to establish the link between currents and ocean temperatures. Another person played a decisive role after the return of the Challenger. It was physicist Peter Tait, who was asked by the scientific leader of the expedition to solve a tricky question about evaluating the temperature measurement error caused by the high pressure to which the thermometers were subjected. On this occasion, Peter Tait used a new high-pressure cell that enabled him to accurately determine the correction to be made to the temperatures collected by the Challenger and embark on more fundamental research on the compressibility of liquids and solids that led him, nine years later, to formulate his famous equation-of-state. Analysis of the properties of the compressibility of liquids is the second challenge of this book.

From Deep Sea to Laboratory has three volumes. The first volume relates the H.M.S. Challenger expedition and addresses the issue of great-depth measurement. The second and third volumes offer a more scientific presentation that develops the two points raised earlier: the correlation between the distribution of temperature and ocean currents (Volume 2) and the properties of compressibility of seawater and, more generally, that of liquids (Volume 3).

Presentation of Volume 1

Chapter 1 describes the background and explains the reasons that led the British government to organize a major oceanographic expedition towards the end of the 19th Century. England then, the first world economic power, had to communicate everywhere and quickly with her vast colonial empire. The advent of the landline electric telegraph and then the undersea telegraph, in the 1860s, made it possible to construct the first international telecommunication network. Many sea and ocean sounding surveys were necessary to facilitate and secure submarine cable laying.

Chapter 2 focuses on sailors and scientists who worked to ensure that the Challenger expedition could happen and conclude with a real success. During the expedition, naturalists, officers, engineers, two doctors, one photographer, one drawer and about 200 crew members came together on a daily basis and for months. This expedition was also a human adventure, with its moments of exaltation, difficulties and dramas. The biographies of the expedition’s key figures are collected in the same document for the first time ever.

Chapter 3 takes us from December 1872 to May 1876 in the long journey of the Challenger across oceans where the bulk of time was dedicated to scientific exploration. The Antarctic crossing gave the photographer the opportunity to take the first ever iceberg photographs. We also enjoy many boat stopovers ourselves to discover unusual, wild and sometimes hostile lands, and many more or less friendly islands, making allusions to their often-turbulent history and toponymy. Many maps, photographs and illustrations, rarely presented, adorn the chapter.

Chapter 4 describes the scientific installations of the Challenger which, from 1872, made it possible to transform this warship into a real oceanographic vessel. In this chapter, we address one of the first difficulties encountered by sailors of that era: how to measure great depths with sufficient precision. From the Challenger surveys and a theoretical study of the sink rate of a sounding line, we highlight the ingenuity of the technique used. Bathymetric measurements made by the Challenger are then used to illustrate some examples of submarine reliefs (ridges, plains, pits). It is particularly during this cruise that the Challenger discovered an abysmal area of more than 8,000 meters between Australia and Japan, which later proved to be located near the Mariana Trench. Finally, we present some results of physical measurements made during the H.M.S. Challenger expedition.

Summary of Volumes 2 and 3

In Volume 2, we examine the extent and distribution of temperature in the ocean and its relationship with ocean circulation. We begin by describing the evolution of techniques for measuring temperature in the 19th Century by recalling the impact of pressure (at great depths) on measurements. After emphasizing that the ocean is composed of different strata, we develop a simplified model of the thermocline, interacting with different ocean layers, limited to thermal aspects (temperature difference between the equator and the poles) and mechanics (effect of the Earth’s rotation, action of the wind on surface layers), in order to establish a link between the cartography of the great ocean currents and the distribution of the ocean temperature. Observations and the physical data from the Challenger, collected in the Atlantic, Pacific and Indian Oceans, are first analyzed and implemented in relation to more recent work. We conclude with a more general presentation of mechanisms that lead to the stirring of the world ocean waters, called the thermohaline circulation.

Volume 3 begins with a reminder of the concept of compressibility and its associated coefficients. We then present a detailed history of techniques for measuring the compressibility of liquids. This leads us naturally to Tait’s work undertaken since 1879 on the measurement of the compressibility of fresh water, seawater, mercury and glass and its equation-of-state set with two parameters. The evolutions and the physical interpretations of the parameters of the Tait equation, as well as those associated with the Tait–Tammann equation, are studied by comparison or analogy with some classical equations-of-state, especially including that of van der Waals, so as to obtain a certain image of the “structure” of liquid media. An in-depth study of the isothermal mixed modulus and the adiabatic tangent modulus leads us to propose new equations-of-state. We show that these new relationships have a precision comparable to that of reference equations and thus enable us to describe, in particular, the liquid phase of fresh water, seawater, and helium-3 and -4. Different “anomalies” of these mediums are then highlighted and discussed.

The book describes a “journey over and through water” with a cross-examination of human history, the history of science and technology, terrestrial and undersea geography, ocean dynamics and thermics, and the sciences dealing with the physical properties of liquids. Curious readers, attracted by travel, science and history, will discover the background and conduct of a great scientific expedition in Volume 1. Students, engineers, researchers, and teachers of physics, fluid mechanics and oceanography will also find subjects to deepen their knowledge in Volumes 2 and 3.

We would like to warmly thank Bernard Castaing, a former professor at Joseph Fourier University (Grenoble-I) and ENS Lyon, for carefully reading the manuscript and for his pertinent remarks. We express our gratitude to Ferdinand Volino and André Denat, Research Directors at the CNRS, and Jacques Bossy, CNRS researcher, who kindly shared their observations and advice during the preparation of the manuscript and for reading the final manuscript. We warmly thank Armelle Michetti, head of the library of physics laboratories of the CNRS campus in Grenoble, for her contribution to the search for often old and restricted documents that enabled us to illustrate and support the historical parts of the sciences of the book.

We also thank the people who gave us special support: Michel Aitken, Philippe Vincent, Yonghua Huang, Glenn M. Stein and John Steven Dews.

Finally, we would like to thank the organizations and their staff who have graciously allowed us to use some of their iconographic holdings, and in particular the Natural History Museum in London, the National Portrait Gallery in London, the United Kingdom Hydrographic Office, London, the University of Vienna (Austria), the scientific museum of Lycée Louis-le-Grand in Paris and Orange/DGCI.

Bibliographical references on specific points appear in footnotes, and those of a more general nature are collated in the bibliography section at the end of each volume. The footnote reference numbers always correspond to the footnotes of that chapter.

Frédéric AITKEN

Jean-Numa FOULC

January 2019