The Trouvelot astronomical drawings manualTrouvelot, E. L. (Etienne Leopold)
Science
The Trouvelot astronomical drawings manual
Trouvelot, E. L. (Etienne Leopold)
Astronomy -- Pictorial works
The ideal point situated midway between the two foci is called _the
centre of the ellipse_, or _orbit_; while the imaginary straight line
which passes through both foci and the centre, with its ends at opposite
points of the ellipse, is called "_the major axis_" of the orbit. It is
also known as "_the line of the apsides_." The ideal straight line
which, in passing through the centre of the orbit, cuts the major axis
at right angles, and is prolonged on either side to opposite points on
the ellipse, is called "_the minor axis_" of the orbit.
When a planet reaches that extremity of the major axis of its orbit
which is the nearest to the Sun, it is said to be in its "_perihelion_;"
while, when it arrives at the other extremity, which is farthest from
this body, it is said to be in its "_aphelion_." When a planet reaches
either of the two opposite points of its orbit situated at the
extremities of its minor axis, it is said to be at its _mean distance_
from the Sun.
The rapidity with which the planets move on their orbits varies with
their distance from the Sun; the farther they are from this body, the
more slowly they move. The rapidity of their motion is greatest when
they are in perihelion, and least when they are in aphelion, having its
mean rate when these bodies are crossing either of the extremities of
the minor axes of their orbits.
The imaginary line which joins the Sun to a planet at any point of its
orbit, and moves with this planet around the Sun, is called "_the radius
vector_." According to Kepler's second law, whatever may be the distance
of a planet from the Sun, the radius vector sweeps over equal areas of
the plane of the planet's orbit in equal times.
There is a remarkable relation between the distance of the planets from
the Sun and their period of revolution, in consequence of which the
squares of their periodic times are respectively equal to the cubes of
their mean distances from the Sun. From this third law of Kepler, it
results that the mere knowledge of the mean distance of a planet from
the Sun enables one to know its period of revolution, and _vice versa_.
The orbit described by the Earth around the Sun in a year, or the
apparent path of the Sun in the sky, is called "_the ecliptic_." Like
that of all the planetary orbits, the plane of the ecliptic passes
through the Sun's centre. The ecliptic has a great importance in
astronomy, inasmuch as it is the fundamental plane to which the orbits
and motions of all planets are referred.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account