Lord Kelvin: An account of his scientific life and workGray, Andrew
Science
Lord Kelvin: An account of his scientific life and work
Gray, Andrew
Kelvin, William Thomson, Baron, 1824-1907
The whole space in which a distribution of electricity produces any
action on electrified bodies is called the _electrical field_ of the
distribution. The force exerted on a very small insulated trial
conductor, on which is an electric charge of amount equal to that taken
as the unit quantity of electricity, measures the _field-intensity_ at
any point at which the conductor is placed. The direction of the
field-intensity at the point is that in which the small conductor is
there urged. If the charge on the small conductor were a negative unit,
instead of a positive, the direction of the force would be reversed; the
magnitude of the force would remain the same. To make the
field-intensity quite definite, a positive unit is chosen for its
specification. For a charge on the trial-conductor consisting of any
number of units, the force is that number of times the field-intensity.
The field-intensity is often specified by its components, X, Y, Z in
three chosen directions at right angles to one another.
Now in all cases in which the action, whether attraction or repulsion,
between two unit quantities of matter concentrated at points is
inversely as the square of the distance between the charges, the
field-intensity, or its components, can be found from a certain function
V of the charges forming the acting distribution [which is always
capable of being regarded for mathematical purposes as a system of small
charges existing at points of space, _point-charges_ we shall call
them], their positions, and the position of the point at which the
field-intensity is to be found. If q₁, q₂, ... be the point-charges, and
be positive when the charges are positive and negative when the charges
are negative, and r₁, r₂, ... be their distances from the point P,
V is q₁⧸r₁ + q₂⧸r₂ + ... The field-intensity is the rate of diminution
of the value of V at P, taken along the specified direction. The three
gradients parallel to the three chosen coordinate directions are
X, Y, Z; but for their calculation it is necessary to insert the values
of r₁, r₂, ... in terms of the coordinates which specify the positions
of the point-charges, and the coordinates x, y, z which specify the
position of P. Once this is done, X, Y, Z are obtained by a simple
systematic process of calculation, namely, differentiation of the
function V with respect to x, y, z.
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