Difference between revisions of ".Mzc2.NzUwNA"

From Georgian Papers Programme Transcription Wiki
Jump to: navigation, search
 
Line 1: Line 1:
 
[ 55 ]  
 
[ 55 ]  
 +
 
ber) 17 degrees less than it was in the months of  
 
ber) 17 degrees less than it was in the months of  
 
August and September.  
 
August and September.  
Line 5: Line 6:
 
108. I hope this paradox will be explained, and
 
108. I hope this paradox will be explained, and
 
that the principles which may clear it up will draw
 
that the principles which may clear it up will draw
useful consequences along with them. Those phi-
+
useful consequences along with them. Those philosphers
losphers who look upon evaporation as a dissolution  
+
who look upon evaporation as a dissolution  
 
of water by air in the manner of menstrua, that  
 
of water by air in the manner of menstrua, that  
 
is, by affinity, will easily apply their principle to the
 
is, by affinity, will easily apply their principle to the
solution of part of these phaenomena The disso-
+
solution of part of these phaenomena The dissolution
lution is greater when the menstruum is warmer, and  
+
is greater when the menstruum is warmer, and  
 
consequently the air must keep a greater quantity of
 
consequently the air must keep a greater quantity of
 
water in dissolution, and suffere a less part of it to  
 
water in dissolution, and suffere a less part of it to  
 
be precipitated, in summer than in winter. I can-
 
be precipitated, in summer than in winter. I can-
 
not but allow that this system is extremely specious,
 
not but allow that this system is extremely specious,
and that many phznomena are very happily ex-
+
and that many phznomena are very happily explained
plained by means of it. This is what Mr le Roy
+
by means of it. This is what Mr le Roy
 
has shewn us in the memoir I have already quoted ;
 
has shewn us in the memoir I have already quoted ;
 
in which, without contending that ai r really acts as  
 
in which, without contending that ai r really acts as  
 
a menstruum with respect to water, he demonstrates,  
 
a menstruum with respect to water, he demonstrates,  
by a parallel very well kept up, that all the chemi-
+
by a parallel very well kept up, that all the chemical
cal expressions concerning dissolutions may with  
+
expressions concerning dissolutions may with  
propriety be applied to describe the several phae-
+
propriety be applied to describe the several phaenomena
nomena be examines, relative to the elevation and  
+
be examines, relative to the elevation and  
suspension of water in air, as well as to its precipi-
+
suspension of water in air, as well as to its precipitation
tation under different forms  
+
under different forms  
  
 
109. If it was not too common a practice, to  
 
109. If it was not too common a practice, to  
Line 31: Line 32:
 
these chemical expressions very conveniently adapted  
 
these chemical expressions very conveniently adapted  
 
to explain a number of these phaenomena. But I
 
to explain a number of these phaenomena. But I
have rejected them here, on account of this consi-
+
have rejected them here, on account of this consideration;
deration; that when I took in a greater number  
+
that when I took in a greater number  
 
of phaenomena, I found them no longer accurate,  
 
of phaenomena, I found them no longer accurate,  
 
any more than the general idea of the dissolu-
 
any more than the general idea of the dissolu-
tion
+
 
 +
[[catchword]] tion [[/catchword]]

Latest revision as of 09:07, 20 October 2018

[ 55 ]

ber) 17 degrees less than it was in the months of August and September.

108. I hope this paradox will be explained, and that the principles which may clear it up will draw useful consequences along with them. Those philosphers who look upon evaporation as a dissolution of water by air in the manner of menstrua, that is, by affinity, will easily apply their principle to the solution of part of these phaenomena The dissolution is greater when the menstruum is warmer, and consequently the air must keep a greater quantity of water in dissolution, and suffere a less part of it to be precipitated, in summer than in winter. I can- not but allow that this system is extremely specious, and that many phznomena are very happily explained by means of it. This is what Mr le Roy has shewn us in the memoir I have already quoted ; in which, without contending that ai r really acts as a menstruum with respect to water, he demonstrates, by a parallel very well kept up, that all the chemical expressions concerning dissolutions may with propriety be applied to describe the several phaenomena be examines, relative to the elevation and suspension of water in air, as well as to its precipitation under different forms

109. If it was not too common a practice, to conclude things from words, I should in fact think these chemical expressions very conveniently adapted to explain a number of these phaenomena. But I have rejected them here, on account of this consideration; that when I took in a greater number of phaenomena, I found them no longer accurate, any more than the general idea of the dissolu-

catchword tion /catchword