The slope or the gradient is commonly used to describe the measurement of the steepness, incline or grade of a straight line. A higher slope value indicates a steeper incline. In normal UK usage, the gradient of a slope is defined as the ratio of the "rise" divided by the "run" between two points on a line. The term Grade is also used for this definition, which can be mathematically stated as the tangent of the angle of inclination – the ratio of the altitude change to the horizontal distance between any two points on the grade

Using calculus, one can calculate the slope of the tangent to a curve at a point.

The concept of slope, and much of this article, applies directly to grades or gradients in geography and civil engineering. In UK construction work, a slope is often called a fall, and measured as an angle, a gradient or as a ratio such as 1 in 80.

Definition of slope

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The slope of a line in the plane containing the x and y axes is generally represented by the letter m, and is defined as the change in the y coordinate divided by the corresponding change in the x coordinate, between two distinct points on the line. This is described by the following equation:

$m\; =\; \backslash frac\{\backslash Delta\; y\}\{\backslash Delta\; x\}$

(The delta symbol, "Δ", is commonly used in mathematics to mean "difference" or "change".)

Given two points (x₁, y₁) and (x₂, y₂), the change in x from one to the other is x₂ - x₁, while the change in y is y₂ - y₁. Substituting both quantities into the above equation obtains the following:

$m\; =\; \backslash frac\{y\_2\; -\; y\_1\}\{x\_2\; -\; x\_1\}$

Since the y-axis is vertical and the x-axis is horizontal by convention, the above equation is often memorized as "rise over run", where Δy is the "rise" and Δx is the "run". Therefore, by convention, m is equal to the change in y, the vertical coordinate, divided by the change in x, the horizontal coordinate; that is, m is the ratio of the changes. This concept is fundamental to algebra, analytic geometry, trigonometry, and calculus.

Note that the points chosen and the order in which they are used is irrelevant; the same line will always have the same slope. Other curves have "accelerating" slopes and one can use calculus to determine such slopes.

Example 1

Suppose a line runs through two points: P(1,2) and Q(13,8). By dividing the difference in y-coordinates by the difference in x-coordinates, one can obtain the slope of the line:

$m\; =\; \backslash frac\{\backslash Delta\; y\}\{\backslash Delta\; x\}\; =\; \backslash frac\{y\_2\; -\; y\_1\}\{x\_2\; -\; x\_1\}\; =\; \backslash frac\{8\; -\; 2\}\{13\; -\; 1\}\; =\; \backslash frac\{6\}\{12\}\; =\; \backslash frac\{1\}\{2\}$

The slope is 1/2 = 0.5.

Example 2

If a line runs through the points (4, 15) and (3, 21) then:

$m\; =\; \backslash frac\{\; 15\; -\; 21\}\{4\; -\; 3\}\; =\; \backslash frac\{6\}\{-1\}\; =\; -6$

Geometry

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The larger the absolute value of a slope, the steeper the line. A horizontal line has slope 0, a 45° rising line has a slope of +1, and a 45° falling line has a slope of -1. A vertical line does not have a real number slope, since its slope would have to be infinite.

The angle θ a line makes with the positive x axis is closely related to the slope m via the tangent function:

$m\; =\; \backslash tan\backslash ,\backslash theta$

and

$\backslash theta\; =\; \backslash arctan\backslash ,m$

(see trigonometry).

Two lines are parallel if and only if their slopes are equal or if they both are vertical and therefore undefined; they are perpendicular (i.e. they form a right angle) if and only if the product of their slopes is -1 or one has a slope of 0 and the other is vertical and undefined.

Slope of a road, etc.

There are two common ways to describe how steep a road is. One is by the angle in degrees, and the other is by the slope in a percentage. See also mountain railway. The formula for converting a slope in percentage to degrees is:

$\backslash theta\; =\; \backslash frac\{180\}\{\backslash pi\}\backslash arctan\backslash frac\{\backslash mbox\{slope\}\}\{100\}.$

Thus, a 100% slope is 45°.

Algebra

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If y is a linear function of x, then the coefficient of x is the slope of the line created by plotting the function. Therefore, if the equation of the line is given in the form

$y\; =\; mx\; +\; b\; \backslash ,$

then m is the slope. This form of a line's equation is called the slope-intercept form, because b can be interpreted as the y-intercept of the line, the y-coordinate where the line intersects the y-axis.

If the slope m of a line and a point (x₀, y₀) on the line are both known, then the equation of the line can be found using the point-slope formula:

$y\; -\; y\_0\; =\; m(x\; -\; x\_0)\; \backslash ,$

For example, consider a line running through the points (2, 8) and (3, 20). This line has a slope, m, of

$\backslash frac\; \{(20\; -\; 8)\}\{(3\; -\; 2)\}\; \backslash ;\; =\; 12\; \backslash ,$.

One can then write the line's equation, in point-slope form:

$y\; -\; 8\; =\; 12(x\; -\; 2)\; =\; 12x\; -\; 24\; \backslash ,$

or:

$y\; =\; 12x\; -\; 16\; \backslash ,$.

The slope of a linear equation in the general form:

$Ax\; +\; By\; +\; C\; =\; 0\; \backslash ,$

is given by the formula:

$\backslash frac\; \{-A\}\{B\}\; \backslash ;\; \backslash ,$.

Calculus

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The concept of a slope is central to differential calculus. For non-linear functions, the rate of change varies along the curve. The derivative of the function at a point is the slope of the line tangent to the curve at the point, and is thus equal to the rate of change of the function at that point.

Why calculus is necessary

If we let Δx and Δy be the distances (along the x and y axes, respectively) between two points on a curve, then the slope given by the above definition,

$m\; =\; \backslash frac\{\backslash Delta\; y\}\{\backslash Delta\; x\}$,

is the slope of a secant line to the curve. For a line, the secant between any two points is the line itself, but this is not the case for any other type of curve.

For example, the slope of the secant intersecting y = x² at (0,0) and (3,9) is m = (9 - 0) / (3 - 0) = 3 (which happens to be the slope of the tangent at, and only at, x = 1.5, a consequence of the mean value theorem).

By moving the two points closer together so that Δy and Δx decrease, the secant line more closely approximates a tangent line to the curve, and as such the slope of the secant approaches that of the tangent. Using differential calculus, we can determine the limit, or the value that Δy/Δx approaches as Δy and Δx get closer to zero; it follows that this limit is the exact slope of the tangent. If y is dependent on x, then it is sufficient to take the limit where only Δx approaches zero. Therefore, the slope of the tangent is the limit of Δy/Δx as Δx approaches zero. We call this limit the derivative.

See also

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• The gradient is a generalization of the concept of slope for functions of more than one variable.
• Slope definitions

Elementary mathematics

ميل | Hældningstal | Steigung | Pendiente de una recta | Pente (mathématiques) | Coefficiente angolare | Stigningstall | Slope | Riktningskoefficient | 斜率