For the historical laboratory context, intense heating could be obtained from an electric arc between carbon electrodes and from an oxyhydrogen flame. The first converts electrical work into a very hot emitting region; the second releases chemical energy rapidly in combustion. An intense light or an ability to melt a particular solid establishes a useful physical effect, but does not by itself provide a calibrated numerical temperature.
The cold end could be reached by rapidly evaporating a volatile material and reducing the surrounding pressure. In Faraday's carbon-dioxide and ether cooling experiment, a bath of solid carbon dioxide and diethyl ether was placed under an air-pump receiver. Removing vapour promoted further cooling. Faraday's 1845 report gives an alcohol-thermometer reading near in the atmospheric-pressure bath and , approximately , under reduced pressure. He explicitly noted thermometer lag, thickening alcohol and possible errors of several Fahrenheit degrees. These are dated reported estimates, not a claim to a modern cold-temperature record.[ref]
On the Liquefaction and Solidification of Bodies Generally Existing as Gases by Michael Faraday. 1845, printed p. 158: reduced-pressure bath, alcohol-thermometer graduation and uncertainty
Measurement must be separated from temperature production. A liquid-in-glass thermometer works only while its liquid, glass and graduation remain usable. A gas thermometer infers temperature from reproducible gas pressure or volume changes, with calibration and departures from ideal-gas behaviour accounted for. At high temperatures, suitable expansion or calorimetric pyrometers can be compared against known points, but material changes and extrapolation introduce error. For example, transferring a hot body of known thermal properties into a calorimeter estimates its starting temperature only after allowing for its heat capacity and heat lost in transfer. The very hottest arc regions are not safely assigned the reading of an ordinary mercury thermometer.
Faraday's published lectures demonstrate the carbon-electrode electric light and electrical heating of platinum. They provide contemporary apparatus context; the later reprint's date is distinguished in its bibliography entry.[ref]
On the Various Forces of Nature by Michael Faraday. Lecture VI, carbon points and the heated platinum bridge
With the electrodes disconnected, the copper has no sustained external route through which to receive electrons from the zinc. It is not appreciably attacked by a clean, dilute nonoxidizing sulfuric acid solution. Zinc can in principle reduce acid while dissolving, but amalgamation suppresses much of the local action associated with impurities and promotes a high kinetic barrier for hydrogen evolution on the amalgamated surface. Thus the intended historical observation is little visible action with the circuit open, not a thermodynamic assertion that zinc cannot react with acid.
Closing the external wire supplies an electron path. At the zinc anode,at the copper cathode,The net redox is thereforeThe zinc dissolves, and bubbles of hydrogen appear chiefly at the copper. Electrons flow through the wire from zinc to copper; conventional electric current flows oppositely there. Ionic transport through the electrolyte completes the circuit and prevents indefinite charge accumulation in the solution. The copper primarily provides a conducting surface: there is no stipulated copper-ion solution from which metallic copper must be deposited, so this is not the Daniell cell reaction.
The chemical energy supplies the electrical work. Accumulation of hydrogen and changing interfacial conditions can polarize the cell, reducing the current. A complete description therefore distinguishes the initial closed-circuit response from an indefinitely constant-current idealization. Electrochemical overpotential explains why a favorable reaction and its observable rate are different questions.