Equation

Collier's New Encyclopedia (1921)

a term based on the idea of equality. Algebra. Two algebraic expressions equal to one another, and are which are connected by the sign. Thus 6x-13=2w+19. is an equation; and, since the equality of the members depends on the value assigned to x, it is called an equation of condition. The two quantities separated by the sign are called the members of the equation; the quant quantity to the left to of being the first member, and that the right the second. The quantities separated by the signs+and are called the terms of the equation. Of the quantities some are known and the others unknown. The known quantities are generally represented by numbers. If letters be used, then those employed are generally a, b, c, d, etc. i. e., letters at or near the beginning of the alphabet. Unknown quantities are represented by letters toward the conclusion of the alphabet. If there be one unknown quantity it is generaly represented by x; if two, by x and y; and if three, by x, y, and z. Sometimes a statement that two expressions are equal for all numerical values letters inthat can be assigned to the volved, provided that the same value be given to the same letter in each member, e. g.- (x+a)²=x² + 2ax+a². Such a statement is called an identical equation, or briefly, an identity. The solution of an equation is the process which ultimately results in discovering and stating the value of the unknown quantity, which value is the root of the equation. Equations are classified according to the highest power of the unknown quantity sought. When that quantity in the first power we have exists only a simple equation, or one of the first degree; if there be a square or second power of the unknown quantity, the of equation becomes a quadratic, or one be the second degree; if the third power present a cubic equation, or of the third power degree. It is rarely that a higher than the cube of the unknown quantity cases has to be dealt with. When such occur the equation is biquadratic, or one the of the fourth degree, an equation of fifth, of the sixth, of any degree. Astronomy. Any sum to be added or anomaly or a subtracted to allow for an special circumstance affecting the exactness of a calculation. If, for instance, the the orbit of a planet were calculated on supposition that its orbit was circular elliptical a small when in reality it is subnumber would require to be added or tracted to make the calculations accurate. astronom- That small sum would be the ical equation. If the movements of the planets calculated on the supposition that is the only attraction operating on them not of that of the sun, error, though a reconsiderable magnitude, will be the among sult. There is a mutual attraction all the planets; each is capable of producing a perturbation in the orbits of all the rest. An equation is required for every such perturbation before it is possible to calculate accurately the course of the planet. Chemistry. A chemical equation represents symbolically a chemical reaction, the symbols of the reacting substances being placed on the left hand, and the symbols of the new substances formed by the reaction being placed on the right hand. In a chemical equation the number of atoms of each element must be the same on each side of the equation, thus, 3AgNO3 + Na2HPO4=Ag3PO+2NaNO3+ HNO3. Three molecules of argentic nitrate and one molecule of disodium-hydrogen-phosphate equal (that is, when added together) one molecule of triargentic phosphate, and two molecules of sodium nitrate, and one molecule of Chemical hydrogen nitrate (nitric acid). equations are imperfect, as they do not , or show the amount of heat liberated absorbed, during the reaction. Annual, Personal, Etc.-Annual equation, in astronomy, one of the numerous equations requisite in determing equation of the moon's tru true longitude; the center; the equation required to fix calculated the place or orbit of of a planet it as if it were moving in a circle when is doing so really in an ellipse; equation of the equinoxes; the equation required to calculate the real position of the equinoxes from its mean one, the disturbing element being the movement of the equinoxes; equacalled precession tion of time, the difference between mean and apparent time; personal equation, the difference between the time at which an astronomical occurrence takes place and that at which a fallible observer notes that it does so; also, the correction of personal differences between particular individuals as to exactness in observations with astronomical instruments; equation of payments, a rule for ascertaining at what time a person should in equity pay the whole of a debt contracted in different portions to be repaid at different times.