Simon Stevin In 1585, Flemish polymath
Simon Stevin performed a demonstration for
Jan Cornets de Groot, a local politician in the Dutch city of
Delft. Stevin dropped two lead balls from the
Nieuwe Kerk in that city. From the sound of the impacts, Stevin deduced that the balls had fallen at the same speed. The result was published in 1586.
Galileo Galilei Galileo successfully applied mathematics to the acceleration of falling objects, correctly hypothesizing in a 1604 letter to
Paolo Sarpi that the distance of a falling object is proportional to the
square of the time elapsed. Written with modern symbols: The result was published in
Two New Sciences in 1638. In the same book, Galileo suggested that the slight variance of speed of falling objects of different mass was due to air resistance, and that objects would fall completely uniformly in a vacuum. The relation of the distance of objects in free fall to the square of the time taken was confirmed by Italian
Jesuits Grimaldi and
Riccioli between 1640 and 1650. They also made a calculation of the
gravity of Earth by recording the oscillations of a pendulum.
Johannes Kepler In his
Astronomia nova (1609),
Johannes Kepler proposed an attractive force of limited radius between any "kindred" bodies: Gravity is a mutual corporeal disposition among kindred bodies to unite or join together; thus the earth attracts a stone much more than the stone seeks the earth. (The magnetic faculty is another example of this sort).... If two stones were set near one another in some place in the world outside the sphere of influence of a third kindred body, these stones, like two magnetic bodies, would come together in an intermediate place, each approaching the other by a space proportional to the bulk [
moles] of the other.... Kepler claimed that if the Earth and Moon were not held apart by some force they would come together. He recognized that mechanical forces cause action, resulting in a more modern view of planetary motion, in his view a celestial machine. On the other hand Kepler viewed the force of the Sun on the planets as magnetic and acting tangential to their orbits and he assumed with Aristotle that inertia meant objects tend to come to rest.
Giovanni Borelli In 1666,
Giovanni Alfonso Borelli avoided the key problems that limited Kepler. By Borelli's time the concept of inertia had its modern meaning as the tendency of objects to remain in uniform motion and he viewed the Sun as just another heavenly body. Borelli developed the idea of mechanical equilibrium, a balance between inertia and gravity. Newton cited Borelli's influence on his theory.
Mechanical explanations In 1644,
René Descartes proposed that no empty space can exist and that a
continuum of matter causes every motion to be
curvilinear. Thus,
centrifugal force thrusts relatively light matter away from the central
vortices of celestial bodies, lowering density locally and thereby creating
centripetal pressure. Using aspects of this theory, between 1669 and 1690,
Christiaan Huygens designed a mathematical vortex model. In one of his proofs, he shows that the distance elapsed by an object dropped from a spinning wheel will increase proportionally to the square of the wheel's rotation time. In 1671,
Robert Hooke speculated that gravitation is the result of bodies emitting waves in the
aether.
Nicolas Fatio de Duillier (1690) and
Georges-Louis Le Sage (1748) proposed
a corpuscular model using some sort of screening or shadowing mechanism. In 1784, Le Sage posited that gravity could be a result of the collision of atoms, and in the early 19th century, he expanded
Daniel Bernoulli's
theory of corpuscular pressure to the universe as a whole. A similar model was later created by
Hendrik Lorentz (1853–1928), who used
electromagnetic radiation instead of corpuscles. English mathematician Isaac Newton used Descartes' argument that curvilinear motion constrains inertia, and in 1675, argued that aether streams attract all bodies to one another. Newton (1717) and
Leonhard Euler (1760) proposed a model in which the aether loses density near mass, leading to a net force acting on bodies. Further mechanical explanations of gravitation (including
Le Sage's theory) were created between 1650 and 1900 to explain Newton's theory, but mechanistic models eventually fell out of favor because most of them lead to an unacceptable amount of drag (air resistance), which was not observed. Others violate the
energy conservation law and are incompatible with modern
thermodynamics.
'Weight' before Newton Before Newton, 'weight' had the double meaning 'amount' and 'heaviness'.
Mass as distinct from weight (1689) In 1686, Newton gave the concept of mass its name. In the first paragraph of
Principia, Newton defined quantity of matter as "density and bulk conjunctly", and mass as quantity of matter.
Newton's law of universal gravitation In 1679, Robert Hooke wrote to Isaac Newton of his hypothesis concerning orbital motion as a combination of tangential inertial motion and a central force. He also asked for the precise trajectory implied an
inverse-square force. Newton was almost certainly influenced by this correspondence to do his subsequent work on gravitation, In January 1684 Hooke told
Edmond Halley and
Christopher Wren that he had proven the inverse-square law of planetary motion but he refused to produce his proof. That summer, Halley visited Newton and asked if Newton knew what trajectory an inverse square force would produce. Newton said an
ellipse and by November 1684 he sent Halley
De motu corporum in gyrum ('On the motion of bodies in an orbit'), in which he mathematically derives
Kepler's laws of planetary motion. In Newton's theory (rewritten using more modern mathematics) the density of mass \rho\, generates a scalar field, the gravitational potential \varphi\, in joules per kilogram, by :{\partial^2 \varphi \over \partial x^j \, \partial x^j} = 4 \pi G \rho \,. Using the
Nabla operator \nabla for the
gradient and
divergence (partial derivatives), this can be conveniently written as: :\nabla^2 \varphi = 4 \pi G \rho \,. This scalar field governs the motion of a
free-falling particle by: :{ d^2x^j\over dt^2} = -{\partial\varphi\over\partial x^j\,}. At distance
r from an isolated mass
M, the scalar field is :\varphi = -\frac{GM} r \,. The
Principia sold out quickly, inspiring Newton to publish a second edition in 1713. However the theory of gravity itself was not accepted quickly. The theory of gravity faced two barriers. First scientists like
Gottfried Wilhelm Leibniz complained that it relied on
action at a distance, that the mechanism of gravity was "invisible, intangible, and not mechanical". The French philosopher
Voltaire countered these concerns, ultimately writing
his own book to explain aspects of it to French readers in 1738, which helped to popularize Newton's theory. Second, detailed comparisons with astronomical data were not initially favorable. Among the most conspicuous issue was the so-called
great inequality of Jupiter and Saturn. Comparisons of ancient astronomical observations to those of the early 1700s implied that the orbit of Saturn was increasing in diameter while that of Jupiter was decreasing. Ultimately this meant Saturn would exit the Solar System and Jupiter would collide with other planets or the Sun. The problem was tackled first by
Leonhard Euler in 1748, then
Joseph-Louis Lagrange in 1763, by
Pierre-Simon Laplace in 1773. Each effort improved the mathematical treatment until the issue was resolved by Laplace in 1784 approximately 100 years after Newton's first publication on gravity. Laplace showed that the changes were periodic but with immensely long periods beyond any existing measurements. Successes such the solution to the great inequality of Jupiter and Saturn mystery accumulated. In 1755, Prussian philosopher
Immanuel Kant published
a cosmological manuscript based on Newtonian principles, in which he develops an early version of the
nebular hypothesis.
Edmond Halley proposed that similar looking objects appearing every 76 years was in fact a single comet. The appearance of the comet in 1759, now named after him, within a month of predictions based on Newton's gravity greatly improved scientific opinion of the theory. Newton's theory enjoyed its greatest success when it was used to predict the existence of
Neptune based on motions of
Uranus that could not be accounted by the actions of the other planets. Calculations by
John Couch Adams and
Urbain Le Verrier both predicted the general position of the planet. In 1846, Le Verrier sent his position to
Johann Gottfried Galle, asking him to verify it. The same night, Galle spotted Neptune near the position Le Verrier had predicted. Not every comparison was successful. By the end of the 19th century, Le Verrier showed that the orbit of
Mercury could not be accounted for entirely under Newtonian gravity, and all searches for another perturbing body (such as a planet orbiting the Sun even closer than Mercury) were fruitless. Even so, Newton's theory is thought to be exceptionally accurate in the limit of weak
gravitational fields and low speeds. At the end of the 19th century, many tried to combine Newton's force law with the established laws of
electrodynamics (like those of
Wilhelm Eduard Weber,
Carl Friedrich Gauss, and
Bernhard Riemann) to explain the anomalous
perihelion precession of Mercury. In 1890,
Maurice Lévy succeeded in doing so by combining the laws of Weber and Riemann, whereby the
speed of gravity is equal to the speed of light. In another attempt,
Paul Gerber (1898) succeeded in deriving the correct formula for the perihelion shift (which was identical to the formula later used by Albert Einstein). These hypotheses were rejected because of the outdated laws they were based on, being superseded by those of
James Clerk Maxwell. == Modern era ==