HOUSE WATER SUPPLY While the plumber is apt to give more attention to supply pipe, and to methods of installing it in buildings to secure specific service, water supply embraces also, in its broadest sense, the source and qual ity of water and the means of conveying it to the building. Plumbers generally have little dealing with water supply outside of the house walls. Custom has fixed certain arbitrary sizes in ordinary work, to such a degree that the average plumber has generally ignored informa tion on the flow of water through pipes. Indeed, he is so rarely in actual need of this knowledge, that it appears a burden to acquire and to fix permanently in his mind the simplest formula bearing on the subject. Enough information to determine approximate deliveries and point the road to further research, will not be out of place in behalf of those who may need simple directions.
The laws of gravity are the basis for the science of hydraulics, of which a prime factor of every problem is velocity. There is no excep tion to the rule that all bodies falling freely, descend at the same rate— in round numbers, 16 feet for the first second, at the end of which the acquired velocity is one of 32 feet a second. This is the basis on which are formulated the laws of falling bodies, which, exhibiting what is known as velocity of efflux, together with loss by friction, must be considered when calculating the flow of water.
There are three kinds of velocity--uniform, accelerated, and retarded. It is the last, and its cause, friction, that plumbers should be most interested in, as velocities calculated merely from the laws of falling bodies do not take account of friction, change of course, etc., which must be allowed for as causes diminishing the delivery of water through pipes. Briefly stated, the mysterious-looking Torricellian formula t'2gh = V, means only that velocity is found by extracting the square root of the product of the head multiplied by 2 X 32, g standing for the force of gravity, and h for the height. For example, a stream filling a 1-inch pipe, with 25 feet head of water, would have a velocity calculated thus: 2 X 32 X 25 = 1,600; and the square root of 1,600 = 40 = Velocity, friction not considered.
The shape of the orifice through which water enters a pipe, has much to do with the amount of water that will enter it. Fri ction against the sides of the pipe, and change of direction due to bends and connections, occasion great variation from the theoretical flow. Not only is the character of the pipe surface and fittings to be considered as initial causes varying the delivery, but velocity, the all-important factor, must be reckoned with in every instance. With a velocity of 10 feet per second in a pipe of comparatively smooth interior surface, the friction loss in pounds on one square foot of surface will be about I pound. If this velocity is increased or diminished, the factor of friction will vary accordingly, always in proportion to the square of the velocity. Suppose the velocity to be 20 feet instead of 10 feet per second; we then have, 10 squared equals 100, and 20 squared equals 400. The square of these velocities is as 1 to 4, and as we assign a ' i-pound loss to ten feet velocity per second, on a stated amount of surface, the friction due to doubling the velocity should be four times a pound = 2 pounds, showing that doubling the velocity increases the friction fourfold ; trebling it increases friction nine-fold, etc.
A column of water weighs .43 pound per square inch of base, per vertical foot. Therefore a vertical pipe 100 feet high, with 1-inch sectional area, filled with water, would contain 43 pounds, and a gauge at the bottom would show 43 pounds pressure. If the pipe were only } inch, or were 40 inches in diameter, the gauge would show the same pressure for the same vertical height—namely, .43 pound per square inch per vertical foot. A head of water expressed in feet, may be changed to pounds by multiplying the feet of head by .43. Pressure is made to read in feet of head by multiplying pressure per square inch by 2.3. A head of water is the number of vertical feet from level of source of supply to center of outlet or point of delivery.