Accession No
1130
Brief Description
mercury barometer and thermometer, by Samuel Lainton, English, 1850 (c)
Origin
England; Halifax
Maker
Lainton, Samuel
Class
meteorology
Earliest Date
1850
Latest Date
1850
Inscription Date
Material
wood (mahogany); metal (mercury); glass; ivory
Dimensions
height 970mm; breadth 710mm; depth 65mm
Special Collection
Provenance
Purchased from Roland Adams, 01/1972.
Inscription
‘SAMUEL LAINTON MAKER HALIFAX’
Description Notes
Mercury barometer and thermometer, Samuel Lainton, 1850 (c)
Domestic double-tube angle barometer, mahogany veneer on pine carcass. Straight trunk with circular foot and hemispherical cistern cover; shaped lug at the bottom.
Paper scale, decorated with Masonic symbols.
Lower tube graduated 28-29½ inches, upper graduated 29½-31 inches, divided to 1/100ths.
Thermometer mounted on bone plate: mercury long flat bulb, 5o-135oF, -15o-55oC.
Marked “stormy, Much RAIN, RAIN, Change/Change, FAIR Set fair, very Dry”, mercury in glass thermometer on ivory plaque marked ‘FAHRENHEIT’ 10-130 by 10 to 1o and ‘CENTIGRADE (-15)-(55) by 10 to 1o and across both scales FREEZING TEMPERATE, SUMMER HEAT, BLOOD HEAT, FEVER HEAT.
References
Events
Description
A barometer measures the pressure of this air upon us and our surroundings. The precise pressure of the air depends upon the weather, so a barometer is useful for weather forecasting. It can also be used as an altimeter (see "how to use" a hypsometer).
Torricelli, a pupil of Galileo, invented the traditional mercury barometer in 1644. Torricelli took a long glass tube closed at one end and completely filled it with mercury. He chose mercury because of its heaviness. Without letting air into the tube, it was then turned upside down and the open end placed in a bowl of mercury. Suprisingly perhaps, the mercury does not run out of the tube into the bowl (unless the tube is more than 760mm long). In fact, the column of mercury in the tube will always settle at the height of about 760mm above the level of the mercury in the bowl, even if the tube is tilted. This height is where the weight (or pressure) of the column of the mercury is equal to the pressure of air above the bowl, and so the height of the column of mercury measures the pressure of the surrounding air.
It was soon found that the height of the column of mercury was not absolutely fixed, but could rise and fall between 700 and 775 mm, even at sea level. The precise height seemed to depend upon the weather. From the late 17th century, therefore, the barometer rapidly became popular in the home for weather forecasting and later as an aid to the preparation of shipping forecasts. From 1840 onwards other forms of barometer were devised that did not require cumbersome columns of mercury. Best known is the aneroid barometer, which depends upon the expansion and contraction of a partially-evacuated metal chamber to register changes in external air pressure. In the late 19th century small pocket barometers of this type, which could also function as altimeters, were fashionable for mountaineers, balloonists and explorers.
This bent-tube type of barometer magnified the movement of the mercury making the instrument easier to read.
01/03/2001
Created by: Chris Lewis on 01/03/2001
FM:44478
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