Newton scale


The Newton scale is a temperature scale devised by Isaac Newton in 1701.
He called his device a "thermometer", but he did not use the term "temperature", speaking of "degrees of heat" instead.
Newton's publication represents the first attempt to introduce an objective way of measuring temperature.
Newton likely developed his scale for practical use rather than for a theoretical interest in thermodynamics; he had been appointed Warden of the Mint in 1695, and Master of the Mint in 1699, and his interest in the melting points of metals are likely inspired by his duties in connection with the Royal Mint.
Newton used linseed oil as thermometric material and measured its change of volume against his reference points. He set as 0 on his scale "the heat of air in winter at which water begins to freeze", reminiscent of the standard of the modern Celsius scale, but he has no single second reference point; he does give the "heat at which water begins to boil" as 33, but this is not a defining reference; the values for body temperature and the freezing and boiling point of water suggest a conversion factor between the Newton and the Celsius scale of between about 3.08 and 3.03 but since the objectively verifiable reference points given result in irreconcilable data, no unambiguous "conversion" between the scales is possible.
The linseed thermometer could be used up to the melting point of tin. For higher temperatures, Newton used a "sufficiently thick piece of iron" that was heated until red-hot and then exposed to the wind. On this piece of iron, samples of metals and alloys were placed, which melted and then again solidified on cooling. Newton then determined the "degrees of heat" of these samples based on the solidification times, and tied this scale to the linseed one by measuring the melting point of tin in both systems.
This second system of measurement led Newton to derive his law of convective heat transfer, also known as Newton's law of cooling.
In his publication, Newton gives 18 reference points, which he labels by two systems, one in arithmetic progression and the other in geometric progression, as follows:
0the heat of air in winter at which water begins to freeze. This point may be accurately determined by pressing the thermometer into melting snow.
0,1,2the heats of air in winter
2,3,4the heats of air in spring and autumn
4,5,6the heat of air in summer
6the heat at midday about the month of July
121the greatest heat which a thermometer takes up when in contact with the human body
141¼the greatest heat of a bath which one can endure for some time when the hand is dipped in and is kept in constant movement
171½the greatest heat of a bath which one can endure for some time when the hand is dipped in and is kept still
20the heat of a bath in which liquid wax slowly becomes solid and assumes transparency
242the heat of a bath in which solid wax melts and is conserved in liquid state without boiling
282¼intermediate point between the boiling point of water and the melting point of wax
34the heat at which water boils vehemently
40melting point of an alloy of one part lead, four parts tin and five parts bismuth
483melting point of an alloy of equal parts of bismuth and tin
573¼melting point of an alloy of one part bismuth and two parts tin
683½melting point of an alloy of one part bismuth and eight parts tin
81melting point of bismuth
964melting point of lead
1144¼heat of bodies that can barely be seen glowing at night
1364½heat of bodies that can be seen glowing by twilight
161heat of bodies that can be seen glowing by daylight
1925heat of iron glowing as brightly as possible