When the series is theoretically continuous, the theoretical graph will be a continuous figure of which the lines actually drawn are ordinates.
The assemblage of ordinates NP is then the graph of Y.
The latter relation shows that the bending moment varies as the area cut off by the ordinate in the graph of F.
View more
Coast of Norway: every ten to twelve years this flow appeared to reach a maximum and a graph of the variations showed a certain resemblance to the well-known graphs showing the numbers of spots on the sun from year to year.
The series of values of X will in general be discontinuous, and the graph will then be made up of a succession of parallel and (usually) equidistant ordinates.
An important plane graph is that which represents the volume of a solid figure.
In the first class come equations in a single unknown; here the function which is equated to zero is the Y whose values for different values of X are traced, and the solution of the equation is the determination of the points where the ordinates of the graph are zero.
Of elements of the graph from an axis through 0 at right angles to OX.
The graph of F is a straight line; that of M is a parabola with vertical axis.
The latter relation shows that the bending moment varies as the area cut off by the ordinate in the graph of F.
In the first class come equations in a single unknown; here the function which is equated to zero is the Y whose values for different values of X are traced, and the solution of the equation is the determination of the points where the ordinates of the graph are zero.
The assemblage of ordinates NP is then the graph of Y.
When the series is theoretically continuous, the theoretical graph will be a continuous figure of which the lines actually drawn are ordinates.
The series of values of X will in general be discontinuous, and the graph will then be made up of a succession of parallel and (usually) equidistant ordinates.
Coast of Norway: every ten to twelve years this flow appeared to reach a maximum and a graph of the variations showed a certain resemblance to the well-known graphs showing the numbers of spots on the sun from year to year.
Of elements of the graph from an axis through 0 at right angles to OX.
The graph of F is a straight line; that of M is a parabola with vertical axis.
An important plane graph is that which represents the volume of a solid figure.