Difference between revisions of ".Mzc2.NzUwNg"

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[ 56 ]  
 
[ 56 ]  
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tion of water by air. I have given the reasons for  
 
tion of water by air. I have given the reasons for  
this in my work, upon the modification of the at-
+
this in my work, upon the modification of the atmosphere;
mosphere; and shall only repeat here, that these mo-
+
and shall only repeat here, that these modifications
difications of the humor appear to me almost intirely  
+
of the humor appear to me almost intirely  
 
to be produced by the igneous fluids ; and that if the  
 
to be produced by the igneous fluids ; and that if the  
 
air has any share in them, it is only as being an  
 
air has any share in them, it is only as being an  
elastic fluid The particles of these fluids, each ac-
+
elastic fluid The particles of these fluids, each according
cording to its degree of power, strike, separate, and  
+
to its degree of power, strike, separate, and  
draw along with them those of the humor, and com-
+
draw along with them those of the humor, and communicate
municate to them the elasticity they possess; in the same  
+
to them the elasticity they possess; in the same  
 
manner as they do to the particles of all volatile,  
 
manner as they do to the particles of all volatile,  
and likewise of at fixt substances which they cor-
+
and likewise of at fixt substances which they corrode
rode and decompose.  
+
and decompose.  
  
 
110. This system will not only furnish a solution  
 
110. This system will not only furnish a solution  
 
of the paradox which engages our attention, but will, I
 
of the paradox which engages our attention, but will, I
 
believe, carry us much farther The heat of the
 
believe, carry us much farther The heat of the
fummer keeps the humor in very great agitation ;  
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fummer keeps the humor in very great agitation;  
and though there is more: of the humor at this sea-
+
and though there is more: of the humor at this season
son than in winter, yet this heat will not: allow it to  
+
than in winter, yet this heat will not: allow it to  
 
continue either as long a time, or in as great a quantity,  
 
continue either as long a time, or in as great a quantity,  
 
upon the bodies or in their pores. That is the  
 
upon the bodies or in their pores. That is the  
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degree of motion impressed upon it by a greater
 
degree of motion impressed upon it by a greater
 
heat. Consequently the dilatation of the bodies, from  
 
heat. Consequently the dilatation of the bodies, from  
this cause, will be in a compound ratio of the quan-
+
this cause, will be in a compound ratio of the quantity
tity of humor, and of its active force, or of the heat.  
+
of humor, and of its active force, or of the heat.  
 
And if, for instance, we compare any summer's day,
 
And if, for instance, we compare any summer's day,
 
in which the hygrometer in open air is at the same  
 
in which the hygrometer in open air is at the same  
degree u on any winter's day, the air on the sum-
+
degree u on any winter's day, the air on the summer's  
mer's day will contain more humor than on the  
+
day will contain more humor than on the  
winter's
+
 
 +
[[catchword]] winter's [[/catchword]]

Latest revision as of 09:11, 20 October 2018

[ 56 ]

tion of water by air. I have given the reasons for this in my work, upon the modification of the atmosphere; and shall only repeat here, that these modifications of the humor appear to me almost intirely to be produced by the igneous fluids ; and that if the air has any share in them, it is only as being an elastic fluid The particles of these fluids, each according to its degree of power, strike, separate, and draw along with them those of the humor, and communicate to them the elasticity they possess; in the same manner as they do to the particles of all volatile, and likewise of at fixt substances which they corrode and decompose.

110. This system will not only furnish a solution of the paradox which engages our attention, but will, I believe, carry us much farther The heat of the fummer keeps the humor in very great agitation; and though there is more: of the humor at this season than in winter, yet this heat will not: allow it to continue either as long a time, or in as great a quantity, upon the bodies or in their pores. That is the reason why the hygrometer falls less. But we see at the same time, that the portion of the humor which does sojourn, and which I call the active part, has more power to dilatate the bodies, from the greater degree of motion impressed upon it by a greater heat. Consequently the dilatation of the bodies, from this cause, will be in a compound ratio of the quantity of humor, and of its active force, or of the heat. And if, for instance, we compare any summer's day, in which the hygrometer in open air is at the same degree u on any winter's day, the air on the summer's day will contain more humor than on the

catchword winter's /catchword