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Side 3
Improvements were made on the instrument by an Italian artist about 1655 , who
used wider tubes , terminating in bulbs , and filled with alcohol ; and by Römer ,
who used mercury , and , starting from the melting - point of ice , divided the tube
...
Improvements were made on the instrument by an Italian artist about 1655 , who
used wider tubes , terminating in bulbs , and filled with alcohol ; and by Römer ,
who used mercury , and , starting from the melting - point of ice , divided the tube
...
Side 15
The Barometer is the instrument employed to measure the height of a column of
mercury supported by the pressure of the atmosphere . From this height the
weight of the atmosphere is ascertained . The fundamental principle of the
barometer ...
The Barometer is the instrument employed to measure the height of a column of
mercury supported by the pressure of the atmosphere . From this height the
weight of the atmosphere is ascertained . The fundamental principle of the
barometer ...
Side 16
Other fluids may be used in the construction of barometers , which , being lighter
than mercury , have columns proportionally longer . Thus , if water , which is
nearly 14 times lighter than mercury , be used , the barometric column is about 35
...
Other fluids may be used in the construction of barometers , which , being lighter
than mercury , have columns proportionally longer . Thus , if water , which is
nearly 14 times lighter than mercury , be used , the barometric column is about 35
...
Side 17
This is done by gently inclining it , so that the mercury may strike against the top
of the glass tube . If there be no air within , a sharp metallic click will be heard ;
but if the sound be dull , the air must not have been completely expelled . 32 .
This is done by gently inclining it , so that the mercury may strike against the top
of the glass tube . If there be no air within , a sharp metallic click will be heard ;
but if the sound be dull , the air must not have been completely expelled . 32 .
Side 18
The simplest and rudest way of compensating for this error is to ascertain ( 1 ) the
neutral point of the instrument — that is , the height at which it stands when the
zero of the scale is on a level with the surface of the mercury in the cistern , or ...
The simplest and rudest way of compensating for this error is to ascertain ( 1 ) the
neutral point of the instrument — that is , the height at which it stands when the
zero of the scale is on a level with the surface of the mercury in the cistern , or ...
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advancing America amount appear Asia Atlantic atmosphere atmospheric pressure average barometer becomes blow Britain calm causes centre changes charts climate cloud coast cold column compared consequently continued countries course daily diminished direction earth east Edition effect electricity Europe evaporation examined falls feet flow force frequently give given greater greatest heat height Hence higher hour important inches increase indicate influence January July land least less light lines lower maximum mean mean temperature mercury Meteorological miles months nearly night northern observations occur ocean passed period Plate position pressure prevail Professor quantity radiation rain rainfall regarded regions relation rises round scale Scotland season seen side soil storm summer surface Table temperature thermometers tion tube upper vapour vols weather whole wind winter
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