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Any information given by Observations made in the open atmosphere on the corresponding betwixt
the thermometer and the barometer in the both
placed in the open atmosphere, indicate nothing
in this view give no information are is nothing to the purpose on this head.
Of the rise or fall of the mercury in the barometer
we know not how much is owing to
the any increase or heat diminution of heat
and thence of elasticity in the air, and how
much to increase or diminution of gravity, i:e:
of quantity. Gravity depends on is the result of the general
attraction of matter in general to matter: elasticity,
in the repulsion between the particles of particular
species of matter or of matter in a particular
state. To know how much for what degree of
heat in air corresponds to what degree of expansion, the
quantity in the degr different degrees of expansion must be the same.
Identifier: | JB/119/050/001 "JB/" can not be assigned to a declared number type with value 119.
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119 |
panopticon |
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050 |
note to p. 6 warming |
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001 |
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text sheet |
2 |
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recto |
d5* / d6* |
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jeremy bentham |
floyd & co |
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arthur young |
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39561 |
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