A View of Sir Isaac Newton's PhilosophyPemberton, Henry
Science
A View of Sir Isaac Newton's Philosophy
Pemberton, Henry
Newton, Isaac, 1642-1727. Principia
29. IN the last place, when the moon is by this attraction of the sun,
drawn at length into the plane of the earth’s motion, the node will
have receded yet more, and the inclination be so much increased, as
to become somewhat more than at first: for the line A K G H I being
convex to all the planes, which touch it, the part H I will wholly fall
between the plane Q V R and the plane A B C; so that the point I will
fall between B and R; and drawing I T W, the point W will be farther
remov’d from A than Q. But it is evident, that the plane, which passes
through the earth T, and touches the line A G I in the point I, will
cut the plane of the earth’s motion A B C D in the line I T W, and
be inclined to the same in the angle under H I B; so that the node,
which was first in A, after having passed into L, N and Q, comes at
last into the point W; as the node which was at first in C has passed
successively from thence through the points M, O and R to I: but the
angle under H I B, which is now the inclination of the orbit to the
plane of the ecliptic, is manifestly not less than the angle under E C
B or E A B, but rather something greater.
30. THUS the moon in the case before us, while it passes from the
plane of the earth’s motion in the quarter, till it comes again into
the same plane, has the nodes of its orbit continually moved backward,
and the inclination of its orbit is at first diminished, viz. till it
comes to G in fig. 100, which is near to its conjunction with the sun,
but afterwards is increased again almost by the same degrees, till
upon the moon’s arrival again to the plane of the earth’s motion, the
inclination of the orbit is restored to something more than its first
magnitude, though the difference is not very great, because the points
I and C are not far distant from each other[190].
31. AFTER the same manner, if the moon had departed from the quarter in
C, it should have described the curve line C X W (in fig. 98.) between
the planes A F C and A D C, which would be convex to the former of
those planes, and concave to the latter; so that, here also, the nodes
should continually recede, and the inclination of the orbit gradually
diminish more and more, till the moon arrived near its opposition to
the sun in X; but from that time the inclination should again increase,
till it became a little greater than at first. This will easily
appear, by considering, that as the action of the sun upon the moon,
by exceeding its action upon the earth, drew it out of the plane A E
C towards the sun, while the moon passed from A to I; so, during its
passage from C to W, the moon being all that time farther from the sun
than the earth, it will be attracted less; and the earth, together with
the plane A E C F, will as it were be drawn from the moon, in such
sort, that the path the moon describes shall appear from the earth, as
it did in the former case by the moon’s being drawn away.
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