from the archive · Modern era
Svante Arrhenius
February 19, 1859 – October 2, 1927 · astronomer · chemist · physicist · university teacher
By The Keeper · Published
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Svante Arrhenius (1859–1927) was a Swedish physical chemist whose theory of electrolytic dissociation earned him the 1903 Nobel Prize in Chemistry, the first awarded to a Swede. He gave chemistry the Arrhenius equation describing how temperature governs reaction rates, and in 1896 he produced the first quantitative estimate of how atmospheric carbon dioxide affects Earth's surface temperature. His career bridged chemistry, physics, and the young science of climate, and his greenhouse calculations remain a founding document of climate research.
Early Life
Svante August Arrhenius was born on February 19, 1859, at Wik Castle near Uppsala, Sweden, where his father, Svante Gustav Arrhenius, worked as a land surveyor and estate supervisor for Uppsala University [1]. The family moved into Uppsala itself the following year when the elder Arrhenius took a position with the university administration. Anyone asking who was Svante Arrhenius usually begins with the stories of his precocity: by his own account he taught himself to read at the age of three and developed an early appetite for arithmetic by watching his father add columns of figures in account books [2].
At the Cathedral School in Uppsala he excelled in mathematics and physics, finishing as the youngest and most able student in his class. In 1876, at seventeen, he entered Uppsala University to study mathematics, chemistry, and physics [1]. He passed his candidate's examination quickly, but he grew dissatisfied with the instruction in physics at Uppsala, finding the professors uninterested in the questions that attracted him. In 1881 he moved to Stockholm to work under the physicist Erik Edlund at the Royal Swedish Academy of Sciences, a decision that shaped the rest of his scientific life [2].
Path to Prominence
In Stockholm, Arrhenius took up a problem at the boundary of physics and chemistry: why do solutions of salts conduct electricity? He measured the conductivity of dilute solutions with great care and noticed that conductivity per unit of dissolved substance increased as solutions became more dilute [3]. From this he drew a conclusion that most chemists of the day found hard to accept. He proposed that salts, acids, and bases split into electrically charged particles, later called ions, when dissolved in water, and that they did so even without an applied electric current [1].
He presented this work as his doctoral dissertation at Uppsala in 1884. The examiners were unimpressed and awarded it only a fourth class pass, a grade barely sufficient for the degree and too low to qualify him for a lectureship [2]. Arrhenius responded by mailing copies of the thesis to prominent chemists abroad. Wilhelm Ostwald in Riga and Jacobus Henricus van 't Hoff in Amsterdam recognized its value immediately, and Ostwald traveled to Uppsala to meet the young Swede [3]. Their support transformed his prospects.
A travel grant from the Academy of Sciences allowed Arrhenius to spend the years from 1886 to 1891 working with Ostwald in Riga, Friedrich Kohlrausch in Würzburg, Ludwig Boltzmann in Graz, and van 't Hoff in Amsterdam [1]. Together with Ostwald and van 't Hoff he built the new discipline of physical chemistry, and the trio became known informally as the Ionists. In 1887 he published the mature statement of his theory of electrolytic dissociation, arguing that the degree of dissociation of an electrolyte could be calculated from conductivity measurements [4].
Major Achievements
Any list of Svante Arrhenius achievements begins with the dissociation theory, which explained puzzles that had accumulated for decades: the abnormal freezing point depressions of salt solutions, the additive properties of dilute electrolytes, and the nature of acids and bases. Arrhenius defined an acid as a substance that releases hydrogen ions in water and a base as one that releases hydroxide ions, a definition still taught in classrooms today [4]. In 1903 the Royal Swedish Academy of Sciences awarded him the Nobel Prize in Chemistry, citing the extraordinary services rendered by his electrolytic theory of dissociation. He was the first Swedish Nobel laureate in any science [5].
In 1889 he published a second contribution of lasting importance. Studying how reaction rates change with temperature, he proposed that molecules must acquire a minimum energy, the activation energy, before they can react. The relationship he formulated, now called the Arrhenius equation, remains one of the most widely used expressions in chemical kinetics, applied everywhere from industrial catalysis to food science [3].
His most celebrated work outside chemistry came in 1896, when he published a long paper in the Philosophical Magazine titled "On the Influence of Carbonic Acid in the Air upon the Temperature of the Ground." Working by hand through thousands of calculations based on Samuel Langley's measurements of infrared radiation from the Moon, Arrhenius estimated that halving atmospheric carbon dioxide would cool Europe by roughly 4 to 5 degrees Celsius, while doubling it would raise global temperatures by about 5 to 6 degrees [6]. He originally framed the question around the causes of ice ages, but he also recognized that coal combustion was adding carbon dioxide to the atmosphere. In his 1908 popular book Worlds in the Making he suggested that this warming might make Earth's climate more agreeable, a judgment shaped by his Scandinavian vantage point [7]. His numerical estimate of climate sensitivity sits surprisingly close to the range produced by modern models, which is why climate scientists still cite the 1896 paper as the starting point of quantitative greenhouse research [6].
Wider Interests and Scientific Range
Arrhenius never confined himself to one field. He wrote on atmospheric electricity, the aurora borealis, and the physics of the Sun. In the early 1900s he developed the hypothesis of panspermia, arguing that life could spread between worlds as microscopic spores driven through space by the pressure of starlight [7]. The idea drew wide public attention when he presented it in Worlds in the Making, and although it never became mainstream biology, it kept alive a question about life's cosmic distribution that astrobiologists still discuss.
He also ventured into immunology and physiology. After working with the bacteriologist Thorvald Madsen in Copenhagen, he published Immunochemistry in 1907, an attempt to apply the quantitative methods of physical chemistry to toxins and antitoxins [1]. The book coined a term that survives, even if many of its specific conclusions did not. Later works, including Quantitative Laws in Biological Chemistry from 1915, continued this program of pushing exact measurement into the life sciences [2].
Institutionally, Arrhenius became a central figure in Swedish science. Appointed lecturer at Stockholms Högskola (the forerunner of Stockholm University) in 1891, he was promoted to professor of physics in 1895 despite resistance from parts of the academic establishment, and he served as the institution's rector from 1896 to 1902 [1]. In 1905 he declined a professorship in Berlin, and in response the Academy of Sciences created the Nobel Institute for Physical Chemistry in Stockholm with Arrhenius as its founding director, a post he held until shortly before his death [5].
Personal Life
In 1894 Arrhenius married Sofia Rudbeck, a chemist who had been his student and assistant and one of the first Swedish women to take a degree in the sciences. The marriage was brief and unhappy; the couple separated within two years and divorced in 1896, and their son Olof Arrhenius was born during the separation [2]. Olof later became a chemist in his own right, working on soil science and plant nutrition.
Arrhenius married again in 1905. His second wife, Maria Johansson, bore him three children, a son and two daughters [1]. Contemporaries described Arrhenius as sociable, energetic, and combative in scientific argument, a large ruddy man fond of good food and long working days. He took an active part in the committees of the Nobel Foundation, where his influence over the chemistry and physics prizes was considerable, and historians have noted that he used that influence both to reward allies of the ionic theory and, at times, to delay recognition of critics such as Walther Nernst, who nevertheless received the chemistry prize in 1920 [5].
Later Years
From his post at the Nobel Institute, Arrhenius spent his final two decades writing prolifically for both scientists and the general public. Books such as Worlds in the Making (1908), The Life of the Universe (1909), and The Destinies of the Stars (1918) carried his cosmological speculations to a broad readership and were translated into many languages [7]. He lectured abroad frequently, including a series at the University of California that appeared as Theories of Solutions in 1912 [2].
Honors accumulated steadily. He was elected a Foreign Member of the Royal Society of London in 1910 and received its Davy Medal in 1902; the Chemical Society in London awarded him its first Faraday Lectureship medal in 1914, and the Franklin Institute in Philadelphia gave him the Franklin Medal in 1920 [1]. He remained director of the Nobel Institute until 1927, when failing health forced his retirement. After an attack of acute intestinal illness earlier that year, Svante Arrhenius died in Stockholm on October 2, 1927, at the age of 68, and was buried in Uppsala [1].
Legacy
Few nineteenth century scientists left fingerprints on so many living fields. Every chemistry student learns Arrhenius facts without necessarily knowing the name behind them: the Arrhenius definition of acids and bases, the Arrhenius equation for reaction rates, the concept of activation energy, and the ionic picture of salt solutions all trace to his work [4]. Physical chemistry, the discipline he helped found with Ostwald and van 't Hoff, became one of the organizing frameworks of twentieth century science.
His climate work followed a stranger path. For decades the 1896 greenhouse paper was treated as a historical curiosity, its conclusions doubted after Knut Ångström's experiments seemed to show that carbon dioxide absorption was already saturated. When Guy Stewart Callendar in the 1930s and later researchers with digital computers returned to the problem, they confirmed the essential soundness of Arrhenius's approach, and today his name appears in the opening pages of climate assessments as the scientist who first calculated the warming effect of carbon dioxide emissions [6]. A crater on the Moon and another on Mars carry his name, as do the Arrhenius Laboratories at Stockholm University [3].
Any full Svante Arrhenius biography must hold two portraits together: the stubborn doctoral student whose examiners nearly ended his career with a fourth class grade, and the Nobel laureate whose ideas outlived every one of his critics. That arc, from dismissal to vindication, is one reason his story continues to attract readers far beyond chemistry [5].
Questions & Answers
- When was Svante Arrhenius born?
- Svante Arrhenius was born on February 19, 1859, at Wik Castle near Uppsala, Sweden. His father worked as a surveyor and estate supervisor for Uppsala University, and the family moved into Uppsala the following year.
- What is Svante Arrhenius famous for?
- He is best known for the theory of electrolytic dissociation, which explained how salts split into ions in solution, and for the Arrhenius equation in chemical kinetics. He is also remembered as the first scientist to calculate, in 1896, how changing carbon dioxide levels would alter Earth's temperature.
- Did Svante Arrhenius win a Nobel Prize?
- Yes. Arrhenius received the Nobel Prize in Chemistry in 1903 for his electrolytic theory of dissociation. He was the first Swede to win a Nobel Prize in any of the sciences.
- What did Svante Arrhenius predict about climate change?
- In his 1896 paper, Arrhenius calculated that doubling atmospheric carbon dioxide would raise global temperatures by roughly 5 to 6 degrees Celsius. He recognized that burning coal added carbon dioxide to the air, though he believed the resulting warming would be slow and possibly beneficial for northern countries.
- How did Svante Arrhenius die?
- Arrhenius died in Stockholm on October 2, 1927, at the age of 68, after a period of failing health that followed an acute intestinal illness earlier that year. He had retired from the directorship of the Nobel Institute for Physical Chemistry shortly before his death, and he was buried in Uppsala.
- What is the Arrhenius equation used for?
- The Arrhenius equation, proposed in 1889, describes how the rate of a chemical reaction depends on temperature and activation energy. It is used throughout chemistry and engineering, from designing industrial catalysts to estimating the shelf life of foods and medicines.
References
Every record in this archive is kept against verifiable sources.
- [1]Svante Arrhenius: Biographical. The Nobel Foundation, NobelPrize.org, 1966. https://www.nobelprize.org/prizes/chemistry/1903/arrhenius/biographical/Web
- [2]Elisabeth Crawford. Arrhenius: From Ionic Theory to the Greenhouse Effect. Science History Publications, Canton, MA, 1996. Book
- [3]Svante Arrhenius: Swedish chemist. Encyclopaedia Britannica, 2024. https://www.britannica.com/biography/Svante-ArrheniusWeb
- [4]Keith J. Laidler. The World of Physical Chemistry. Oxford University Press, 1993. Book
- [5]Elisabeth Crawford. The Beginnings of the Nobel Institution: The Science Prizes, 1901-1915. Cambridge University Press, 1984. Book
- [6]Spencer R. Weart. The Discovery of Global Warming. Harvard University Press, 2008. https://history.aip.org/climate/co2.htmBook
- [7]Svante Arrhenius. Worlds in the Making: The Evolution of the Universe. Harper and Brothers, New York, 1908. Primary source
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