# Meridional definition

An early definition of the metre was one ten-millionth of the distance from the pole to the equator.

The history of the metre starts with the scientific revolution that began with Nicolaus Copernicus's work in 1543. Increasingly accurate measurements were required, and scientists looked for measures that were universal and could be based on natural phenomena rather than royal decree or physical prototypes. Rather than the various complex systems of subdivision in use, they also preferred a decimal system to ease their calculations.

With the French Revolution (1789) came a desire to replace many features of the Ancien Régime, including the traditional units of measure. As a base unit of length, many scientists initially favored the seconds pendulum (a pendulum with a half-period of one second), but this was rejected when it was discovered that it varied from place to place with local gravity. A new unit of length, the metre was introduced – defined as one ten-millionth of the distance from the North Pole to the equator.

For practical purposes however, the standard metre was made available in the form of a platinum bar held in Paris. This in turn was replaced in 1889 by thirty platinum-iridium bars kept across the globe. However, using such physical objects as the standard had been something that the original definition had aimed to avoid, so in 1960 a new definition based on a specific number of wavelengths of light from a specific transition in krypton-86 allowed the standard to be universally available by measurement. In 1983 this was updated to a length defined in terms of the speed of light, which was reworded in 2019:[1]

The metre, symbol m, is the SI unit of length. It is defined by taking the fixed numerical value of the speed of light in vacuum c to be 299792458 when expressed in the unit m⋅s−1, where the second is defined in terms of the caesium frequency ΔνCs.

During the mid nineteenth century the metre gained adoption worldwide, particularly in scientific usage, and was officially established as an international measurement unit by the Metre Convention of 1875. Where older traditional length measures are still used, they are now defined in terms of the metre – for example the yard has since 1959 officially been defined as exactly 0.9144 metre.[2]

## Universal measure[]

The standard measures of length in Europe diverged from one another after the fall of the Carolingian Empire (around 888): while measures could be standardized within a given jurisdiction (which was often little more than a single market town), there were numerous variations of measure between regions. Indeed, as the measures were often used as the basis for taxation (of cloth, for example), the use of a particular measure was associated with the sovereignty of a given ruler and often dictated by law.[3][2]

Nevertheless, with the increasing scientific activity of the 17th century came calls for the institution of a "universal measure" (as Englishman John Wilkins called it[4][5]) or "metro cattolico" (as Italian Tito Livio Burattini said [6]), which would be based on natural phenomena rather than royal decree, and would also be decimal rather than using the various systems of subdivision, often duodecimal, which coexisted at the time.

In 1645 Giovanni Battista Riccioli had been the first to determine the length of a "seconds pendulum" (a pendulum with a half-period of one second). According to Wilkins it was Christopher Wren's idea to choose this length as the unit of length: such pendulums were demonstrated by Christiaan Huygens, and their length is quite close to one modern metre (as well as to some other length units which were then in use, such as the yard). In 1671 Jean Picard measured the length of a "seconds pendulum" at the Paris Observatory. He found the value of 440.5 lines of the Toise of Châtelet which had been recently renewed. He proposed a universal toise (French: Toise universelle) which was twice the length of the seconds pendulum. However, it was soon discovered that the length of a seconds pendulum varies from place to place: French astronomer Jean Richer had measured the 0.3% difference in length between Cayenne (in French Guiana) and Paris.[7][8][4][9][5][10][11][12]

Jean Richer and Giovanni Domenico Cassini measured the parallax of Mars between Paris and Cayenne in French Guiana when Mars was at its closest to Earth in 1672. They arrived at a figure for the solar parallax of 9.5 arcseconds,[Note 1] equivalent to an Earth–Sun distance of about 22,000 Earth radii.[Note 2] They were also the first astronomers to have access to an accurate and reliable value for the radius of Earth, which had been measured by their colleague Jean Picard in 1669 as 3269 thousand toises. Isaac Newton used this measurement for establishing his law of universal gravitation.[14] Picard's geodetic observations had been confined to the determination of the magnitude of the earth considered as a sphere, but the discovery made by Jean Richer turned the attention of mathematicians to its deviation from a spherical form. The determination of the figure of the earth became a problem of the highest importance in astronomy, inasmuch as the diameter of the earth was the unit to which all celestial distances had to be referred.[15][16][17][18][19][20][21]

Geodetic surveys found practical applications in French cartography and in the Anglo-French Survey, which aimed to connect Paris and Greenwich Observatories and led to the Principal Triangulation of Great Britain.[22][23] The unit of length used by the French was the Toise de Paris, which was divided in six feet.[24] The English unit of length was the yard, which became the geodetic unit used in the British Empire.[25][26]

The French main unit of length was the Toise of Paris whose standard was the Toise of Châtelet which was fixed outside the Grand Châtelet in Paris from 1668 to 1776. In 1735 two geodetic standards were calibrated against the Toise of Châtelet. One of them, the Toise of Peru was used for the Spanish-French Geodesic Mission. In 1766 the Toise of Peru became the official standard of the Toise in France and was renamed as the Toise of the Academy (French: Toise de l'Académie).[27]

Despite scientific progresses in the field of geodesy, little practical advance was made towards the establishment of the "universal measure" until the French Revolution of 1789. France was particularly affected by the proliferation of length measures, and the need for reform was widely accepted across all political viewpoints, even if it needed the push of revolution to bring it about. Talleyrand resurrected the idea of the seconds pendulum before the Constituent Assembly in 1790, suggesting that the new measure be defined at 45°N (a latitude that, in France, runs just north of Bordeaux and just south of Grenoble): despite the support of the Assembly, nothing came of Talleyrand's proposal.[3][Note 3]

## Meridional definition[]

Belfry, Dunkirk – the northern end of the meridian arc

The question of measurement reform was placed in the hands of the Academy of Sciences, who appointed a commission chaired by Jean-Charles de Borda. Borda was an avid supporter of decimalisation: he had invented the "repeating circle", a surveying instrument which allowed a much-improved precision in the measurement of angles between landmarks, but insisted that it be calibrated in "grades" (​1100 of a quarter-circle) rather than degrees, with 100 minutes to a grade and 100 seconds to a minute.[28] Borda considered that the seconds pendulum was a poor choice for a standard because the existing second (as a unit of time) was not part of the proposed decimal system of time measurement – a system of 10 hours to the day, 100 minutes to the hour and 100 seconds to the minute – introduced in 1793.

Instead of the seconds pendulum method, the commission – whose members included Lagrange, Laplace, Monge and Condorcet – decided that the new measure should be equal to one ten-millionth of the distance from the North Pole to the Equator (the quadrant of the Earth's circumference), measured along the meridian passing through Paris.[3] Apart from the obvious consideration of safe access for French surveyors, the Paris meridian was also a sound choice for scientific reasons: a portion of the quadrant from Dunkirk to Barcelona (about 1000 km, or one-tenth of the total) could be surveyed with start- and end-points at sea level, and that portion was roughly in the middle of the quadrant, where the effects of the Earth's oblateness were expected to be the largest.[3] The Spanish-French geodetic mission had confirmed that the acceleration of a body near the surface of the Earth is due to the combined effects of gravity and centrifugal acceleration. Indeed we know now that the resulting acceleration towards the ground is about 0.5% greater at the poles than at the Equator. It follows that the polar diameter of the Earth is smaller than its equatorial diameter. The Academy of Sciences planned to infer the flattening of the Earth from the length's differences between meridional portions corresponding to one degree of latitude. Jean-Baptiste Biot and François Arago published in 1821 their observations completing those of Delambre and Mechain. It was an account of the length's variation of the degrees of latitude along the Paris meridian as well as the account of the variation of the seconds pendulum's length along the same meridian. The seconds pendulum's length is a mean to measure g, the local acceleration due to local gravity and centrifugal acceleration, which varies depending on one's position on Earth (see Earth's gravity).[14][22][Note 4][Note 5]

The north and south sections of the meridinal survey met at Rodez Cathedral, seen here dominating the Rodez skyline.

The task of surveying the meridian arc fell to Pierre Méchain and Jean-Baptiste Delambre, and took more than six years (1792–1798). The technical difficulties were not the only problems the surveyors had to face in the convulsed period of the aftermath of the Revolution: Méchain and Delambre, and later Arago, were imprisoned several times during their surveys, and Méchain died in 1804 of yellow fever, which he contracted while trying to improve his original results in northern Spain. In the meantime, the commission calculated a provisional value from older surveys of 443.44 lignes.[Note 6] This value was set by legislation on 7 April 1795.[29]

The project was split into two parts – the northern section of 742.7 km from the belfry, Dunkirk to Rodez Cathedral which was surveyed by Delambre and the southern section of 333.0 km from Rodez to the Montjuïc Fortress, Barcelona which was surveyed by Méchain.[30][Note 7]

Fortress of Montjuïc – the southern end of the meridian arc

Delambre used a baseline of about 10 km (6,075.90 toise) in length along a straight road between Melun and Lieusaint. In an operation taking six weeks, the baseline was accurately measured using four platinum rods, each of length two toise (a toise being about 1.949 m).[30] Thereafter he used, where possible, the triangulation points used by Cassini in his 1744 survey of France. Méchain's baseline, of a similar length (6,006.25 toise), and also on a straight section of road between Vernet (in the Perpignan area) and Salces (now Salses-le-Chateau).[31] Although Méchain's sector was half the length of Delambre, it included the Pyrenees and hitherto unsurveyed parts of Spain. An international commission composed of Gabriel Císcar, Jean-Baptiste Delambre, Pierre- Simon Laplace, Adrien-Marie Legendre, Pierre Méchain, Jean Henri van Swinden and Johann Georg Tralles combined the results of the survey with those of the Geodetic Mission to Peru and found a value of 1/334 for the Earth's flattening. They then extrapolated from the measurement of the Paris meridian arc between Dunkirk and Barcelona the distance from the North Pole to the Equator which was 5 130 740 toises.[32][5] As the metre had to be equal to one ten-millionth of this distance, it was defined as 0.513074 toise or 3 feet and 11.296 lines of the Toise of Peru.[27] Their result came out at 0.144 lignes shorter than the provisional value, a difference of about 0.03%.[3]

## Mètre des Archives[]

A copy of the "provisional" metre installed 1796–1797, located in the wall of a building, 36 rue de Vaugirard, Paris. These metres were based on the "provisional" metre, because the expion to re-determine the metre wasn't completed until 1798.[33]

While Méchain and Delambre were completing their survey, the commission had ordered a series of platinum bars to be made based on the provisional metre. When the final result was known, the bar whose length was closest to the meridional definition of the metre was selected and placed in the National Archives on 22 June 1799 (4 messidor An VII in the Republican calendar) as a permanent record of the result.[3] This standard metre bar became known as the mètre des Archives.

The metric system, that is the system of units based on the metre, was officially adopted in France on 10 December 1799 (19 frimaire An VIII) and became the sole legal system of weights and measures from 1801.[29] After the restoration of the Empire, in 1812, the old names for units of length were revived but the units redefined in terms of the metre: this system was known as mesures usuelles, and lasted until 1840, when the decimal metric system was again made the sole legal measure.[3] In the meantime, the Netherlands had adopted the metric system from 1816, the first of several countries to follow the French lead. The Helvetic Republic had adopted the metre shortly before its collapse in 1803.[27][34]

WGS 84 mean Earth radius: Equatorial (a), polar (b) and mean Earth radii as defined in the 1984 World Geodetic System revision.

With the extension of the survey it became apparent that Méchain and Delambre's result (443.296 lignes)[Note 6] was slightly too short for the meridional definition of the metre. While the Ordnance Survey extended the British survey northward to the Shetland, Arago and Biot extended the survey southward in Spain to the island of Formentera in the western Merranean Sea (1806–1809), and found that one ten-millionth of the Earth's quadrant should be 443.31 lignes: later work increased the value to 443.39 lignes.[3][14] This new survey of the Paris meridian arc, named West Europe-Africa Meridian-arc by Alexander Ross Clarke, was undertaken under the direction of François Perrier from 1870 to his death in 1888. Jean-Antonin-Léon Bassot completed the task in 1894.[35][21] The modern value, for the WGS 84 reference spheroid with an Earth's flattening of 1/298.257223563, is 1.00019657 × 107 m for the distance from the North pole to the Equator.[Note 8]

A more accurate determination of the Figure of the Earth resulted also from the measurement of the Struve Geodetic Arc (1816–1855) and would have given another value for the definition of this standard of length. This did not invalidate the metre but highlighted that progresses in science would allow better measurement of Earth's size and shape.[36] The mètre des Archives remained the legal and practical standard for the metre in France, even once it was known that it did not exactly correspond to the meridional definition. When it was decided (in 1867) to create a new international standard metre, the length was taken to be that of the mètre des Archives "in the state in which it shall be found".[37][38]

The only significant international use of the meridional definition of the metre, apart from geodetic surveys, was the initial work conducted by the British Association for the Advancement of Science (B.A.) on electrical units which was to lead to the International System of Electrical and Magnetic Units. It was often claimed that the international electrical units formed a coherent set of absolute units in the quadrant-eleventh-gram-second system (aka "QES system" or "Q.E.S. system"), where the unit length was the quadrant of the Earth's polar circumference, the unit mass was the "eleventh-gram" or 10−11 grams and the unit time was the second.[39][40] Nevertheless, the precision of absolute electrical measurements in the late nineteenth century was not such that the 0.02% difference in the definitions of the metre had any practical significance.[39]

The beginning of the U. S. coastal survey.

The original predecessor agency of the National Geodetic Survey was the United States Survey of the Coast, created within the United States Department of the Treasury by an Act of Congress on February 10, 1807, to conduct a "Survey of the Coast."[41][42] The Survey of the Coast, the United States government's first scientific agency,[42] represented the interest of the administration of President Thomas Jefferson in science and the stimulation of international trade by using scientific surveying methods to chart the waters of the United States and make them safe for navigation. A Swiss immigrant with expertise in both surveying and the standardization of weights and measures, Ferdinand R. Hassler, was selected to lead the Survey.[43]

Hassler submitted a plan for the survey work involving the use of triangulation to ensure scientific accuracy of surveys, but international relations prevented the new Survey of the Coast from beginning its work; the Embargo Act of 1807 brought American overseas trade virtually to a halt only a month after Hassler's appointment and remained in effect until Jefferson left office in March 1809. It was not until 1811 that Jefferson's successor, President James Madison, sent Hassler to Europe to purchase the instruments necessary to conduct the planned survey, as well as standardized weights and measures. Hassler departed on August 29, 1811, but eight months later, while he was in England, the War of 1812 broke out, forcing him to remain in Europe until its conclusion in 1815. Hassler did not return to the United States until August 16, 1815.[43]

The Survey finally began surveying operations in 1816, when Hassler started work in the vicinity of New York City. The first baseline was measured and verified in 1817.[43] The unit of length to which all distances measured in the U. S. coast survey would be referred was the Committee metre (French : Mètre des Archives), of which Ferdinand Rudolph Hassler had brougth a copy in the United States in 1805.[25][44]

In 1835, the invention of the telegraph by Samuel Morse allowed new progresses in the field of geodesy as longitudes were determined with greater accuracy.[32] Moreover the publication in 1838 of Friedrich Wilhelm Bessel’s Gradmessung in Ostpreussen marked a new era in the science of geodesy. Here was found the method of least squares applied to the calculation of a network of triangles and the reduction of the observations generally. The systematic manner in which all the observations were taken with the view of securing final results of extreme accuracy was admirable.[21] For his survey Bessel used a copy of the Toise of Peru constructed in 1823 by Fortin in Paris.[26]

A head of a post office and a female telegraphist. 1870.

In 1860, the Russian Government at the instance of Otto Wilhelm von Struve invited the Governments of Belgium, France, Prussia and England to connect their triangulations in order to measure the length of an arc of parallel in latitude 52° and to test the accuracy of the figure and dimensions of the Earth, as derived from the measurements of arc of meridian. In order to combine the measurements it was necessary to compare the geodetic standards of length used in the different countries.The British Government invited those of France, Belgium, Prussia, Russia, India, Australia, Austria, Spain, United States and Cape of Good Hope to send their standards to the Ordnance Survey office in Southampton. Notably the geodetic standards of France, Spain and United States were based on the metric system, whereas those of Prussia, Belgium and Russia where calibrated against the toise, of which the oldest physical representative was the Toise of Peru. The Toise of Peru had been constructed in 1735 as the standard of reference in the Spanish-French Geodesic Mission, conducted in actual Ecuador from 1735 to 1744.[26][25]

Alexander Ross Clarke and Henry James published the first results of the standards' comparisons in 1867. The same year Russia, Spain and Portugal joined the Europäische Gradmessung and the General Conference of the association proposed the metre as a uniform length standard for the Arc measurement and recommended the establishment of an International Metre Commission.[26][45]

The Europäische Gradmessung decided the creation of an international geodetic standard at the General Conference held in Paris in 1875.[46] The Metre Convention was signed in 1875 in Paris and the International Bureau of Weights and Measures was created under the supervision of the International Committee for Weights and Measures. In 1886 the association changed name for the International Geodetic Association (German: Internationale Erdmessung). During this period the International Geodetic Association gained worldwide importance with the joining of United States, Mexico, Chile, Argentina and Japan.[45][47][48]

West Europe-Africa Meridian-arc (French: Meridienne de France): a meridian arc extending from the Shetland Islands, through Great Britain, France and Spain to El Aghuat in Algeria, whose parameters were calculated from surveys carried out in the mid to late 19th century. It yielded a value for the equatorial radius of the earth a = 6 377 935 metres, the ellipticity being assumed as 1/299.15. The radius of curvature of this arc is not uniform, being, in the mean, about 600 metres greater in the northern than in the southern part. The Greenwich meridian is depicted rather than the Paris meridian.

After the death of Johann Jacob Baeyer, Carlos Ibáñez e Ibáñez de Ibero became the first president of the International Geodetic Association.[48] Fondator of the Spanish Geographic Institute, Carlos Ibáñez e Ibáñez de Ibero collaborated with the French since 1853 on the completion of the West Europe-Africa Meridian-arc (French: Meridienne de France), which would then extend from Shetland to the Sahara, by expanding the continental geodetic survey in Spain and by connecting Spanish and Algerian geodetic network over the Merranean sea.[21][48][49][50][45] As a forerunner in Europe, Spain adopted the metre as geodetic standard, contributed to the Europäische Gradmessung's decision to adopt the metre and played a leading role in the foundation of the International Bureau of Weights and Measures.[48][51][52]

As Carlos Ibáñez e Ibáñez de Ibero stated, the progresses of metrology combined with those of gravimetry through improvement of Kater's pendulum led to a new era of geodesy. If precision metrology had needed the help of geodesy, it could not continue to prosper without the help of metrology. Indeed how to express all the measurements of terrestrial arcs as a function of a single unit, and all the determinations of the force of gravity with the pendulum, if metrology had not created a common unit, adopted and respected by all civilized nations, and if in addition one had not compared, with great precision, to the same unit all the rulers for measuring geodesic bases, and all the pendulum rods that had hitherto been used or would be used in the future? Only when this series of metrological comparisons would be finished with a probable error of a thousandth of a millimeter would geodesy be able to link the works of the different nations with one another, and then proclaim the result of the last measurement of the Globe.[53]

Efforts to supplement the various national surveying systems, which begun in the 19th century with the foundation of the Mitteleuropäische Gradmessung, resulted in a series of global ellipsoids of the Earth (e.g., Helmert 1906, Hayford 1910/1924) which would later lead to develop the World Geodetic System. Nowadays the practical realisation of the metre is possible everywhere thanks to the atomic clocks embedded in GPS satellites.[54][55]

## International prototype metre[]

Closeup of National Prototype Metre Bar No. 27, made in 1889 by the International Bureau of Weights and Measures (BIPM) and given to the United States, which served as the standard for defining all units of length in the US from 1893 to 1960

With increasing international adoption of the metre, the shortcomings of the mètre des Archives as a standard became ever more apparent. Countries that adopted the metre as a legal measure purchased standard metre bars intended to be equal in length to the mètre des Archives, but there was no systematic way of ensuring that the countries were actually working to the same standard. The meridional definition, which had been intended to ensure international reproducibility, quickly proved so impractical that it was all but abandoned in favour of the artefact standards, but the mètre des Archives (and most of its copies) were "end standards": such standards (bars which are exactly one metre in length) are prone to wear with use, and different standard bars could be expected to wear at different rates.[56]

In 1861 Johann Jacob Baeyer published a report suggesting that European countries should cooperate in the determination of the figure of the Earth. In 1862, when Denmark, Saxe-Gotha, the Netherlands, Russia (for Poland), Switzerland, Baden, Saxony, Italy, Austria, Sweden, Norway, Bavaria, Mecklenburg, Hanover and Belgium decided to participate, Bessel's Toise was adopted as international geodetic standard.[57] In 1867 Spain joined the geodetic association and was represented by Carlos Ibáñez e Ibáñez de Ibero. He had devised a geodetic standard calibrated against the metre which had been compared to the Toise of Borda, the copy of the Toise of Peru constructed for the measurement of the Paris meridian arc by Delambre and Mechain.[57][48][25] Copies of the Spanish metric geodetic standard were made for some of the great European countries and for Egypt.[52] The European geodetic association (German: Europäische Gradmessung) at its Second General Conference in 1867 called for the creation of a new, international prototype metre (IPM)[57][37][38][Note 9] and the arrangement of a system where national standards could be compared with it. The international prototype would also be a "line standard"; that is, the metre was defined as the distance between two lines marked on the bar, so avoiding the wear problems of end standards. The French government gave practical support to the creation of an International Metre Commission, which met in Paris in 1870 and again in 1872 with the participation of about thirty countries.[37]

The standards' international nature was ensured by a treaty, the Metre Convention, signed in Paris on 20 May 1875. The treaty established an international organisation, the Bureau international des poids et mesures (BIPM), to conserve the prototypes—which would be the joint property of the signatory nations—and to carry out regular comparisons with national standards. In recognition of France's role in designing the metric system, the BIPM is based in Sèvres, just outside Paris. However, as an international organisation, the BIPM is under the ultimate control of a diplomatic conference, the Conférence générale des poids et mesures (CGPM) rather than the French government.[2][58]

The construction of the international prototype metre and the copies which would be national standards was at the limits of the technology of the time. The bars were to be made of a special alloy, 90% platinum and 10% iridium, which is significantly harder than pure platinum, and have a special X-shaped cross section (a "Tresca section", named after French engineer Henri Tresca) to minimise the effects of torsional strain during length comparisons.[2] The first castings proved unsatisfactory, and the job was given to the London firm of Johnson Matthey who succeeded in producing thirty bars to the required specification. One of these, No. 6, was determined to be identical in length to the mètre des Archives, and was consecrated as the international prototype metre at the first meeting of the CGPM in 1889. The other bars, duly calibrated against the international prototype, were distributed to the signatory nations of the Metre Convention for use as national standards.[38] For example, the United States received No. 27 with a calibrated length of 0.9999984 m ± 0.2 μm (1.6 μm short of the international prototype).[59]

The first (and only) follow-up comparison of the national standards with the international prototype was carried out between 1921 and 1936,[2][38] and indicated that the definition of the metre was preserved to within 0.2 μm.[60] At this time, it was decided that a more formal definition of the metre was required (the 1889 decision had said merely that the "prototype, at the temperature of melting ice, shall henceforth represent the metric unit of length"), and this was agreed at the 7th CGPM in 1927.[61]

The unit of length is the metre, defined by the distance, at 0°, between the axes of the two central lines marked on the bar of platinum–iridium kept at the Bureau International des Poids et Mesures and declared Prototype of the metre by the 1st Conférence Générale des Poids et Mesures, this bar being subject to standard atmospheric pressure and supported on two cylinders of at least one centimetre diameter, symmetrically placed in the same horizontal plane at a distance of 571 mm from each other.

The support requirements represent the Airy points of the prototype—the points, separated by ​47 of the total length of the bar, at which the bending or droop of the bar is minimized.[62]

The comparison of the new prototypes of the metre with each other and with the Committee metre (French: Mètre des Archives) involved the development of a special measuring equipment and the definition of a reproducible temperature scale. The BIPM's thermometry work led to the discovery of special alloys of iron-nickel, in particular invar, for which its director, the Swiss physicist Charles-Edouard Guillaume, was granted the Nobel Prize for physics in 1920.[63]

## Interferometric options[]

A Krypton-86 lamp used to define the metre between 1960 and 1983.

The first interferometric measurements carried out using the international prototype metre were those of Albert A. Michelson and Jean-René Benoît (1892–1893)[64] and of Benoît, Fabry and Perot (1906),[65] both using the red line of cadmium. These results, which gave the wavelength of the cadmium line (λ ≈ 644 nm), led to the definition of the ångström as a secondary unit of length for spectroscopic measurements, first by the International Union for Cooperation in Solar Research (1907)[66] and later by the CIPM (1927).[38][67][Note 10] Michelson's work in "measuring" the prototype metre to within ​110 of a wavelength (< 0.1 μm) was one of the reasons for which he was awarded the Nobel Prize in Physics in 1907.[2][38][68]

By the 1950s, interferometry had become the method of choice for precise measurements of length, but there remained a practical problem imposed by the system of units used. The natural unit for expressing a length measured by interferometry was the ångström, but this result then had to be converted into metres using an experimental conversion factor – the wavelength of light used, but measured in metres rather than in ångströms. This added an additional measurement uncertainty to any length result in metres, over and above the uncertainty of the actual interferometric measurement.

The solution was to define the metre in the same manner as the ångström had been defined in 1907, that is in terms of the best interferometric wavelength available. Advances in both experimental technique and theory showed that the cadmium line was actually a cluster of closely separated lines, and that this was due to the presence of different isotopes in natural cadmium (eight in total). To get the most precisely defined line, it was necessary to use a monoisotopic source and this source should contain an isotope with even numbers of protons and neutrons (so as to have zero nuclear spin).[2]

Several isotopes of cadmium, krypton and mercury both fulfil the condition of zero nuclear spin and have bright lines in the visible region of the spectrum.

## Krypton standard[]

Krypton is a gas at room temperature, allowing for easier isotopic enrichment and lower operating temperatures for the lamp (which reduces broadening of the line due to the Doppler effect), and so it was decided to select the orange line of krypton-86 (λ ≈ 606 nm) as the new wavelength standard.[2][69]

Accordingly, the 11th CGPM in 1960 agreed a new definition of the metre:[61]

The metre is the length equal to 1 650 763.73 wavelengths in vacuum of the radiation corresponding to the transition between the levels 2p10 and 5d5 of the krypton 86 atom.

The measurement of the wavelength of the krypton line was not made directly against the international prototype metre; instead, the ratio of the wavelength of the krypton line to that of the cadmium line was determined in vacuum. This was then compared to the 1906 Fabry–Perot determination of the wavelength of the cadmium line in air (with a correction for the refractive index of air).[2][60] In this way, the new definition of the metre was traceable to both the old prototype metre and the old definition of the ångström.

## Speed of light standard[]

The krypton-86 discharge lamp operating at the triple point of nitrogen (63.14 K, −210.01 °C) was the state-of-the-art light source for interferometry in 1960, but it was soon to be superseded by a new invention: the laser, of which the first working version was constructed in the same year as the redefinition of the metre.[70] Laser light is usually highly monochromatic, and is also coherent (all the light has the same phase, unlike the light from a discharge lamp), both of which are advantageous for interferometry.[2]

The shortcomings of the krypton standard were demonstrated by the measurement of the wavelength of the light from a methane-stabilized helium–neon laser (λ ≈ 3.39 μm). The krypton line was found to be asymmetrical, so different wavelengths could be found for the laser light depending on which point on the krypton line was taken for reference.[Note 11] The asymmetry also affected the precision to which the wavelengths could be measured.[71][72]

Developments in electronics also made it possible for the first time to measure the frequency of light in or near the visible region of the spectrum,[further explanation needed] instead of inferring the frequency from the wavelength and the speed of light. Although visible and infrared frequencies were still too high to be directly measured, it was possible to construct a "chain" of laser frequencies that, by suitable multiplication, differ from each other by only a directly measurable frequency in the microwave region. The frequency of the light from the methane-stabilized laser was found to be 88.376 181 627(50) THz.[71][73]

Independent measurements of frequency and wavelength are, in effect, a measurement of the speed of light (c = ), and the results from the methane-stabilized laser gave the value for the speed of light with an uncertainty almost 100 times lower than previous measurements in the microwave region. Or, somewhat inconveniently, the results gave two values for the speed of light, depending on which point on the krypton line was chosen to define the metre.[Note 12] This ambiguity was resolved in 1975, when the 15th CGPM approved a conventional value of the speed of light as exactly 299 792 458 m s−1.[74]

Nevertheless, the infrared light from a methane-stabilized laser was inconvenient for use in practical interferometry. It was not until 1983 that the chain of frequency measurements reached the 633 nm line of the helium–neon laser, stabilized using molecular iodine.[75][76] That same year, the 17th CGPM adopted a definition of the metre, in terms of the 1975 conventional value for the speed of light:[77]

The metre is the length of the path travelled by light in vacuum during a time interval of ​1299,792,458 of a second.

This definition was reworded in 2019:[1]

The metre, symbol m, is the SI unit of length. It is defined by taking the fixed numerical value of the speed of light in vacuum c to be 299792458 when expressed in the unit m⋅s−1, where the second is defined in terms of the caesium frequency ΔνCs.

The concept of defining a unit of length in terms of a time received some comment,[78] although it was similar to Wilkins' original proposal in 1668 to define the universal unit of length in terms of the seconds pendulum. In both cases, the practical issue is that time can be measured more accurately than length (one part in 1013 for a second using a caesium clock as opposed to four parts in 109 for the metre in 1983).[67][78] The definition in terms of the speed of light also means that the metre can be realized using any light source of known frequency, rather than defining a "preferred" source in advance. Given that there are more than 22,000 lines in the visible spectrum of iodine, any of which could be potentially used to stabilize a laser source, the advantages of flexibility are obvious.[78]

## History of definitions since 1798[]

Definitions of the metre since 1798[79]
Basis of definition Date Absolute
uncertainty
Relative
uncertainty
110,000,000 part of one half of a meridian, measurement by Delambre and Méchain 1798 0.5–0.1 mm 10−4
First prototype Mètre des Archives platinum bar standard 1799 0.05–0.01 mm 10−5
Platinum-iridium bar at melting point of ice (1st CGPM) 1889 0.2–0.1 μm 10−7
Platinum-iridium bar at melting point of ice, atmospheric pressure, supported by two rollers (7th CGPM) 1927 n.a. n.a.
1,650,763.73 wavelengths of light from a specified transition in krypton-86 (11th CGPM) 1960 0.01–0.005 μm 10−8
Length of the path travelled by light in a vacuum in ​1299,792,458 of a second (17th CGPM) 1983 0.1 nm 10−10

## Notes[]

1. ^ The modern value of the solar parallax is 8.794143 arcseconds.[13]
2. ^ Since 2012 the astronomical unit is defined as exactly 149597870700 metres or about 150 million kilometres (93 million miles).
3. ^ The idea of the seconds pendulum as a length standard did not die completely, and such a standard was used to define the yard in the United Kingdom from 1843 to 1878.
4. ^ At the time the second was defined as a fraction of the Earth's rotation time and determined by clocks whose precision was checked by astronomical observations. In 1936 French and German astronomers found that Earth rotation's speed is irregular. Since 1967 atomic clocks define the second. For further informations see atomic time.
5. ^ : ${\displaystyle T=2\pi {\sqrt {\frac {\ell }{g}}}.}$ The length of the pendulum is a function of the time lapse of half a cycle ${\displaystyle T_{1/2}}$
${\displaystyle \ell =g\left({\frac {T_{1/2}}{\pi }}\right)^{2}.}$
Being ${\displaystyle T_{1/2}=1\ \mathrm {s} }$ therefore ${\displaystyle g=\ell \cdot \pi ^{2}\mathrm {\frac {m}{s^{2}}} }$.
6. ^ a b All values in lignes are referred to the toise de Pérou, not to the later value in mesures usuelles. 1 toise = 6 pieds; 1 pied = 12 pouces; 1 pouce = 12 lignes; so 864 lignes = 1 toise.
7. ^ Distances measured using Google Earth. The coordinates are:
51°02′08″N 2°22′34″E﻿ / ﻿51.03556°N 2.37611°E – Belfry, Dunkirk
44°25′57″N 2°34′24″E﻿ / ﻿44.43250°N 2.57333°ERodez Cathedral
41°21′48″N 2°10′01″E﻿ / ﻿41.36333°N 2.16694°EMontjuïc, Barcelona
8. ^ The WGS 84 reference spheroid has a semi-major axis of 6378137.0 m and a flattening of ​1298.257223563.
9. ^ The term "prototype" does not imply that it was the first in a series and that other standard metres would come after it: the "prototype" metre was the one that came first in the logical chain of comparisons, that is the metre to which all other standards were compared.
10. ^ The IUSR (later to become the International Astronomical Union) defined the ångström such that the wavelength (in air) of the cadmium line was 6438.469 63 Å.
11. ^ Taking the point of highest intensity as the reference wavelength, the methane line had a wavelength of 3.392 231 404(12) μm; taking the intensity-weighted mean point ("centre of gravity") of the krypton line as the standard, the wavelength of the methane line is 3.392 231 376(12) μm.
12. ^ The measured speed of light was 299 792.4562(11) km s−1 for the "centre-of-gravity" definition and 299 792.4587(11) km s−1 for the maximum-intensity definition, with a relative uncertainty ur = 3.5×10−9.

## References[]

1. ^ a b 9th ion of the SI Brochure, BIPM, 2019, p. 131
2. Nelson, Robert A. (December 1981). "Foundations of the international system of units (SI)" (PDF). The Physics Teacher: 596–613.
3.  Larousse, Pierre, ed. (1874), "Métrique", Grand dictionnaire universel du XIXe siècle, 11, Paris: Pierre Larousse, pp. 163–164
4. ^ a b Wilkins, John (1668). An Essay Towards a Real Character, And a Philosophical Language (PDF). London, UK: Gillibrand.
5. ^ a b c Bigourdan, Guillaume (1901). Le système métrique des poids et mesures ; son établissement et sa propagation graduelle, avec l'histoire des opérations qui ont servi à déterminer le mètre et le kilogramme. University of Ottawa. Paris : Gauthier-Villars. pp. 7, 148, 154.
6. ^ Misura Universale, 1675
7. ^ Guedj, Denis, (1940–2010). (2011). Le mètre du monde. Paris: Éd. du Seuil. p. 38. ISBN 9782757824900. OCLC 758713673.CS1 maint: Multiple names: authors list (link)
8. ^ Simaan, Arkan. (2001). La science au péril de sa vie : les aventuriers de la mesure du monde. Paris: Vuibert. pp. 124–125. ISBN 2711753476. OCLC 300706536.
9. ^ Picard, Jean (1620–1682) Auteur du texte (1671). Mesure de la terre [par l'abbé Picard]. pp. 3–4.
10. ^ Bond, Peter; Dupont-Bloch, Nicolas (2014). L'exploration du système solaire (in French). Louvain-la-Neuve: De Boeck. pp. 5–6. ISBN 9782804184964. OCLC 894499177.
11. ^ Poynting, John Henry; Thompson, Joseph John (1907). A Textbook of Physics: Properties of Matter (4th ed.). London: Charles Griffin. p. 20.
12. ^ Faye, Hervé (1880). "Comptes rendus hebdomadaires des séances de l'Académie des sciences / publiés... par MM. les secrétaires perpétuels". Gallica (in French). Retrieved 19 June 2019.
13. ^ United States Naval Observatory (2018), "Selected Astronomical Constants" (PDF), The Astronomical Almanac Online, p. K7
14. ^ a b c texte, Biot, Jean-Baptiste (1774–1862). Auteur du; texte, Arago, François (1786–1853). Auteur du (1821). "Recueil d'observations géodésiques, astronomiques et physiques, exécutées par ordre du Bureau des longitudes de France en Espagne, en France, en Angleterre et en Écosse, pour déterminer la variation de la pesanteur et des degrés terrestres sur le prolongement du méridien de Paris... rédigé par MM. Biot et Arago,..." Gallica. p. 523, 529. Retrieved 14 September 2018.
15. ^ Bond, Peter; Dupont-Bloch, Nicolas (2014). L'exploration du système solaire [The exploration of the solar system] (in French). Louvain-la-Neuve: De Boeck. pp. 5–6. ISBN 9782804184964. OCLC 894499177.
16. ^ "Première détermination de la distance de la Terre au Soleil" [First determination of the distance from the Earth to the Sun]. Les 350 ans de l'Observatoire de Paris (in French). Retrieved 5 September 2018.
17. ^ "1967LAstr..81..234G Page 234". adsbit.harvard.edu. p. 237. Retrieved 5 September 2018.
18. ^ "INRP - CLEA - Archives : Fascicule N° 137, Printemps 2012 Les distances" [NPRI - CLEA - Archives: Issue N ° 137, Spring 2012 Distances]. clea-astro.eu (in French). Retrieved 5 September 2018.
19. ^ texte, Picard, Jean (1620–1682). Auteur du (1671). Mesure de la terre [par l'abbé Picard]. Gallica. p. 23. Retrieved 5 September 2018.
20. ^ Bigourdan, Guillaume (1901). Le système métrique des poids et mesures ; son établissement et sa propagation graduelle, avec l'histoire des opérations qui ont servi à déterminer le mètre et le kilogramme. University of Ottawa. Paris : Gauthier-Villars. pp. 7–8.
21. ^ a b c d "Earth, Figure of the", 1911 Encyclopædia Britannica, 8, retrieved 5 September 2018
22. ^ a b Murdin, Paul (2009). Full meridian of glory: perilous adventures in the competition to measure the Earth. New York; London: Copernicus Books/Springer. ISBN 9780387755342.
23. ^ Martin, Jean-Pierre; McConnell, Anita (20 December 2008). "Joining the observatories of Paris and Greenwich". Notes and Records of the Royal Society. 62 (4): 355–372. doi:10.1098/rsnr.2008.0029. ISSN 0035-9149.
24. ^ Portet, Pierre (2011). "La mesure de Paris" [The measure of Paris] (in French). Laboratoire de Médiévistique Occidentale de Paris – via Sciences de l'Homme et de la Société.
25. ^ a b c d Clarke, Alexander Ross; James, Henry (1 January 1873). "XIII. Results of the comparisons of the standards of length of England, Austria, Spain, United States, Cape of Good Hope, and of a second Russian standard, made at the Ordnance Survey Office, Southampton. With a preface and notes on the Greek and Egyptian measures of length by Sir Henry James". Philosophical Transactions of the Royal Society of London. 163: 445–469. doi:10.1098/rstl.1873.0014. ISSN 0261-0523.
26. ^ a b c d Clarke, Alexander Ross (1 January 1867). "X. Abstract of the results of the comparisons of the standards of length of England, France, Belgium, Prussia, Russia, India, Australia, made at the ordnance Survey Office, Southampton". Philosophical Transactions of the Royal Society of London. 157: 161–180. doi:10.1098/rstl.1867.0010. ISSN 0261-0523.
27. ^ a b c "Histoire du mètre" [History of the metre]. Direction Générale des Entreprises (DGE) (in French). Retrieved 12 September 2018.
28. ^ O'Connor, J. J.; Robertson, E. F. (April 2003). "Jean Charles de Borda". School of Mathematics and Statistics, University of St. Andrews, Scotland. Retrieved 13 October 2015.
29. ^ a b National Industrial Conference Board (1921). The metric versus the English system of weights and measures ... The Century Co. pp. 10–11. Retrieved 5 April 2011.
30. ^ a b Alder, Ken (2002). The Measure of all Things – The Seven-Year-Odyssey that Transformed the World. London: Abacus. pp. 227–230. ISBN 0-349-11507-9.
31. ^ Alder, Ken (2002). The Measure of all Things – The Seven-Year-Odyssey that Transformed the World. London: Abacus. pp. 240–241. ISBN 978-0349115078.
32. ^ a b Levallois, Jean-Jacques (May – June 1986). "L'Académie Royale des Sciences et la Figure de la Terre" [The Royal Academy of Sciences and the Shape of the Earth]. La Vie des Sciences (in French): 290. Retrieved 4 September 2018 – via Gallica.
33. ^ The wall plaque next to the metre.
34. ^ "e-expo: Ferdinand Rudolf Hassler". www.f-r-hassler.ch. Retrieved 12 September 2018.
35. ^ texte, Lebon, Ernest (1846–1922). Auteur du (1899). Histoire abrégée de l'astronomie / par Ernest Lebon,... Gallica. pp. 168–169. Retrieved 14 September 2018.
36. ^ "Nomination of the Struve geodetic arc for inscription on the World Heritage List" (PDF). p. 29. Retrieved 13 May 2019.
37. ^ a b c The International Metre Commission (1870–1872). International Bureau of Weights and Measures. Retrieved 15 August 2010.
38. The BIPM and the evolution of the definition of the metre, International Bureau of Weights and Measures, retrieved 30 August 2016
39. ^ a b "Units, Physical", Encyclopædia Britannica, 27 (11 ed.), 1911, pp. 738–745
40. ^ Kennelly, Arthur E. (1931). "Rationalised versus Unrationalised Practical Electromagnetic Units". Proceedings of the American Philosophical Society. 70 (2): 103–119.
41. ^ "Coast and Geodetic Survey Heritage - NOAA Central Library". 19 December 2015. Retrieved 8 September 2018.
42. ^ a b "NOAA History - NOAA Legacy Timeline - 1800's". www.history.noaa.gov. Retrieved 8 September 2018.
43. ^ a b c "Access and Use - NOAA Central Library". 6 September 2014. Retrieved 8 September 2018.
44. ^ "e-expo: Ferdinand Rudolf Hassler". www.f-r-hassler.ch. Retrieved 8 September 2018.
45. ^ a b c Torge, Wolfgang (2015), From a Regional Project to an International Organization: The "Baeyer-Helmert-Era" of the International Association of Geodesy 1862–1916, International Association of Geodesy Symposia, 143, Springer International Publishing, pp. 3–18, doi:10.1007/1345_2015_42, ISBN 9783319246031
46. ^ Lebon, Ernest (1899). Histoire abrégée de l'astronomie. Gauthier-Villars.
47. ^ Torge, W. (25 March 2005). "The International Association of Geodesy 1862 to 1922: from a regional project to an international organization". Journal of Geodesy. 78 (9): 558–568. Bibcode:2005JGeod..78..558T. doi:10.1007/s00190-004-0423-0. ISSN 0949-7714.
48. Soler, T. (10 February 1997). "A profile of General Carlos Ibáñez e Ibáñez de Ibero: first president of the International Geodetic Association". Journal of Geodesy. 71 (3): 176–188. Bibcode:1997JGeod..71..176S. CiteSeerX 10.1.1.492.3967. doi:10.1007/s001900050086. ISSN 0949-7714.
49. ^ Soler, Tomás; Ruíz-Morales, Mario (11 July 2006). "Letters from Carlos Ibáñez e Ibáñez de Ibero to Aimé Laussedat: new sources for the history of nineteenth century geodesy". Journal of Geodesy. 80 (6): 313–321. doi:10.1007/s00190-006-0069-1. ISSN 0949-7714.
50. ^ 1886. Jonction géodésique et astronomique de l'Algérie avec l'Espagne, exécutée en commun, en 1879, par ordre des gouvernements d'Espagne et de France, sous la direction de M. le général IBANEZ, membre de l'Académie des Sciences de Madrid, directeur général de l'Institut géographique et statistique pour l'Espagne, et de M. le colonel PERRIER, membre de l'Académie des Sciences, chef du Service géographique de l'armée pour la France. Paris, Imprimerie nationale, 1886, in-4°, 281 p., 11 planches [1886. Geodesic and Astronomical Junction of Algeria with Spain, executed jointly, in 1879, by order of the Governments of Spain and France, under the direction of General IBANEZ, member of the Academy of Sciences Madrid, Director General of the Geographical and Statistical Institute for Spain, and Colonel PERRIER, Member of the Academy of Sciences, Head of the Geographical Service of the Army for France. Paris, Imprimerie Nationale, 1886, in-4 °, 281 p., 11 plates.] (in French). Imp. nationale. 1886. Retrieved 10 September 2018 – via catalogue.bnf.fr.
51. ^ Hirsch, Adolphe (1891). "Le General Ibanez Notice Necrologique Lue au Comite International des Poids et Mesure, le 12 September et Dans La Conference Geodesique de Florence, le 8 Octobre 1891" [The General Ibanez Necrological Record Read at the International Committee of Weights and Measurement, September 12 and In The Geodesic Conference of Florence, October 8, 1891] (PDF) – via BIPM.
52. ^ a b Guillaume, Charles Édouard (1920). "Notice nécrologique de F. da Paula Arrillaga y Garro" (PDF). archive.wikiwix.com. pp. 110–111. Archived from the original (PDF) on 1920. Retrieved 14 September 2018.
53. ^ Ibáñez e Ibáñez de Ibero, Carlos (1881). Discursos leidos ante la Real Academia de Ciencias Exactas Fisicas y Naturales en la recepcion pública de Don Joaquin Barraquer y Rovira (PDF). Madrid: Imprenta de la Viuda e Hijo de D.E. Aguado. pp. 70, 78.
54. ^ Laboratoire national de métrologie et d'essais (13 June 2018), Le mètre, l'aventure continue..., retrieved 17 June 2019
55. ^ "Histoire du mètre". Direction Générale des Entreprises (DGE) (in French). Retrieved 17 June 2019.
56. ^  "Mètre", Grand dictionnaire universel du XIXe siècle, 17 (Suppl. 2), Paris: Pierre Larousse, 1890, p. 1587
57. ^ a b c "A Note on the History of the IAG". IAG Homepage. Retrieved 19 September 2018.
58. ^ Article 3, Metre Convention.
59. ^ National Prototype Meter No. 27, National Institute of Standards and Technology, retrieved 17 August 2010
60. ^ a b Barrell, H. (1962). "The Metre". Contemporary Physics. 3 (6): 415–434. Bibcode:1962ConPh...3..415B. doi:10.1080/00107516208217499.
61. ^ a b International Bureau of Weights and Measures (2006), The International System of Units (SI) (PDF) (8th ed.), pp. 142–143, 148, ISBN 92-822-2213-6, archived (PDF) from the original on 14 August 2017
62. ^ Phelps, F. M. III (1966). "Airy Points of a Meter Bar". American Journal of Physics. 34 (5): 419–422. Bibcode:1966AmJPh..34..419P. doi:10.1119/1.1973011.
63. ^ "BIPM - la définition du mètre". www.bipm.org. Retrieved 17 June 2019.
64. ^ Michelson, A. A.; Benoît, Jean-René (1895). "Détermination expérimentale de la valeur du mètre en longueurs d'ondes lumineuses". Travaux et Mémoires du Bureau International des Poids et Mesures (in French). 11 (3): 85.
65. ^ Benoît, Jean-René; Fabry, Charles; Perot, A. (1907). "Nouvelle détermination du Mètre en longueurs d'ondes lumieuses". Comptes rendus hebdomadaires des séances de l'Académie des sciences (in French). 144: 1082–1086.
66. ^ "Détermination de la valeur en Ångströms de la longeur d'onde de la raie rouge du Cadmium considérée comme étalon primaire" [Determination of the value in Ångströms of the wavelength of the red line of cadmium under consideration as a primary standard]. Transactions of the International Union for Cooperation in Solar Research (in French). 2: 18–34. 21 May 1907. Bibcode:1908TIUCS...2...17.
67. ^ a b Hollberg, L.; Oates, C. W.; Wilpers, G.; Hoyt, C. W.; Barber, Z. W.; Diddams, S. A.; Oskay, W. H.; Bergquist, J. C. (2005). "Optical frequency/wavelength references" (PDF). Journal of Physics B: Atomic, Molecular and Optical Physics. 38 (9): S469–S495. Bibcode:2005JPhB...38S.469H. doi:10.1088/0953-4075/38/9/003.
68. ^ Nobel Prize in Physics 1907 – Presentation Speech, Nobel Foundation, retrieved 14 August 2010
69. ^ Baird, K. M.; Howlett, L. E. (1963). "The International Length Standard". Applied Optics. 2 (5): 455–463. Bibcode:1963ApOpt...2..455B. doi:10.1364/AO.2.000455.
70. ^ Maiman, T. H. (1960). "Stimulated optical radiation in ruby". Nature. 187 (4736): 493–494. Bibcode:1960Natur.187..493M. doi:10.1038/187493a0.
71. ^ a b Evenson, K. M.; Wells, J. S.; Petersen, F. R.; Danielson, B. L.; Day, G. W.; Barger, R. L.; Hall, J. L. (1972). "Speed of Light from Direct Frequency and Wavelength Measurements of the Methane-Stabilized Laser". Physical Review Letters. 29 (19): 1346–1349. Bibcode:1972PhRvL..29.1346E. doi:10.1103/PhysRevLett.29.1346.
72. ^ Barger, R. L.; Hall, J. L. (1973). "Wavelength of the 3.39-μm laser-saturated absorption line of methane". Applied Physics Letters. 22 (4): 196–199. Bibcode:1973ApPhL..22..196B. doi:10.1063/1.1654608.
73. ^ Evenson, K. M.; Day, G. W.; Wells, J. S.; Mullen, L. O. (1972). "Extension of Absolute Frequency Measurements to the cw He☒Ne Laser at 88 THz (3.39 μ)". Applied Physics Letters. 20 (3): 133–134. Bibcode:1972ApPhL..20..133E. doi:10.1063/1.1654077.
74. ^ Resolution 2, 15th Meeting of the General Conference on Weights and Measures, 1975.
75. ^ Pollock, C. R.; Jennings, D. A.; Petersen, F. R.; Wells, J. S.; Drullinger, R. E.; Beaty, E. C.; Evenson, K. M. (1983). "Direct frequency measurements of transitions at 520 THz (576 nm) in iodine and 260 THz (1.15 μm) in neon". Optics Letters. 8 (3): 133–135. Bibcode:1983OptL....8..133P. doi:10.1364/OL.8.000133.
76. ^ Jennings, D. A.; Pollock, C. R.; Petersen, F. R.; Drullinger, R. E.; Evenson, K. M.; Wells, J. S.; Hall, J. L.; Layer, H. P. (1983). "Direct frequency measurement of the I2-stabilized He–Ne 473-THz (633-nm) laser". Optics Letters. 8 (3): 136–138. Bibcode:1983OptL....8..136J. doi:10.1364/OL.8.000136.
77. ^
78. ^ a b c Wilkie, Tom (27 October 1983). "Time to remeasure the metre". New Scientist (27 October 1983): 258–263.
79. ^ Cardarelli, François (2003). Encyclopaedia of Scientific Units, Weights and Measures. Springer-Verlag London Ltd. ISBN 978-1-4471-1122-1.