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The slope of a line in the plane is defined as the rise over the run, m = Δyx.

In mathematics, the slope or gradient of a line describes its steepness, incline, or grade. A higher slope value indicates a steeper incline. Slope is not defined for vertical lines.

Slope is normally described by the ratio of the "rise" divided by the "run" between two points on a line. The line may be practical - a set by a road surveyor - or in a diagram that models a road or a roof either as a description or as a plan.

For relatively short distances - where the earth's curvature may be neglected, the rise of a road between two points is the difference between the altitude of at those two points, say y1 and y2, or in other words,

the rise is (y2y1) = Δy.

In this example, the run is the difference in distance from a fixed point a measured along a level, horizontal line, or in other words,

the run is (x2x1) = Δx.

Here the slope of the road between the two points is simply described as the ratio of the altitude change to the horizontal distance between any two points on the line. In mathematical language,

the slope m of the line is

Failed to parse (Missing texvc executable; please see math/README to configure.): m=\frac{y_2-y_1}{x_2-x_1}.


The concept of slope applies directly to grades or gradients in geography and civil engineering. Through trigonometry, the grade m of a road is related to its angle of incline θ by

Failed to parse (Missing texvc executable; please see math/README to configure.): m = \tan \theta.\!


As a generalization of this practical description, the mathematics of differential calculus defines the slope of a curve at a point as the slope of the tangent line at that point. When the curve given by a series of points in a diagram or in a list of the coordinates of points, the slope may be calculated not at a point but between any two given points. When the curve is given as a continuous function, perhaps as an algebraic formula, then the differential calculus provides rules giving a formula for the slope of the cure at any point in the middle of the curve.

This generalization of the concept of slope allows very complex constructions to be planned and built that go well beyond static structures that are either horizontals or verticals, but can change in time, move in curves, and change depending on the rate of change of other factors. Thereby, the simple idea of slope becomes one of the main basis of the modern world in terms of both technology and the built environment.

Contents

Definition [link]

File:Slope of lines illustrated.jpg
Slope illustrated for y = (3/2)x − 1. Click on to enlarge

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:

Failed to parse (Missing texvc executable; please see math/README to configure.): m = \frac{\Delta y}{\Delta x} = \frac{\text{rise}}{\text{run}}.

(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 x2x1 (run), while the change in y is y2y1 (rise). Substituting both quantities into the above equation generates the formula:

Failed to parse (Missing texvc executable; please see math/README to configure.): m = \frac{y_2 - y_1}{x_2 - x_1}.

The formula fails for a vertical line, parallel to the y axis (see Division by zero), where the slope can be taken as infinite, so the slope of a vertical line is considered undefined.

Examples [link]

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:

Failed to parse (Missing texvc executable; please see math/README to configure.): m = \frac{\Delta y}{\Delta x} = \frac{y_2 - y_1}{x_2 - x_1} = \frac{8 - 2}{13 - 1} = \frac{6}{12} = \frac{1}{2}.


As another example, consider a line which runs through the points (4, 15) and (3, 21). Then, the slope of the line is

Failed to parse (Missing texvc executable; please see math/README to configure.): m = \frac{ 21 - 15}{3 - 4} = \frac{6}{-1} = -6.


Geometry [link]

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's slope is undefined.

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

Failed to parse (Missing texvc executable; please see math/README to configure.): m = \tan\,\theta

and

Failed to parse (Missing texvc executable; please see math/README to configure.): \theta = \arctan\,m

(see trigonometry).

Two lines are parallel if and only if their slopes are equal and they are not coincident or if they both are vertical and therefore have undefined slopes. Two lines are perpendicular if the product of their slopes is −1 or one has a slope of 0 (a horizontal line) and the other has an undefined slope (a vertical line). Also, another way to determine a perpendicular line is to find the slope of one line and then to get its reciprocal and then reversing its positive or negative sign (e.g. a line perpendicular to a line of slope  −2 is +1/2).

Slope of a road or railway [link]

Main articles: Grade (slope), Grade separation

There are two common ways to describe how steep a road or railroad is. One is by the angle in degrees, and the other is by the slope in a percentage. See also mountain railway and rack railway. The formulae for converting a slope as a percentage into an angle in degrees and vice versa are:

Failed to parse (Missing texvc executable; please see math/README to configure.): \text{angle} = \arctan \frac{\text{slope}}{100} ,

and

Failed to parse (Missing texvc executable; please see math/README to configure.): \mbox{slope} = 100 \tan( \mbox{angle}),\,

where angle is in degrees and the trigonometric functions operate in degrees. For example, a 100% or 1000 slope is 45°.

A third way is to give one unit of rise in say 10, 20, 50 or 100 horizontal units, e.g. 1:10. 1:20, 1:50 or 1:100 (etc.).

Algebra [link]

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

Failed to parse (Missing texvc executable; please see math/README to configure.): y = mx + b \,

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 (x1,y1) on the line are both known, then the equation of the line can be found using the point-slope formula:

Failed to parse (Missing texvc executable; please see math/README to configure.): y - y_1 = m(x - x_1).\!


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

Failed to parse (Missing texvc executable; please see math/README to configure.): \frac {(20 - 8)}{(3 - 2)} \; = 12. \,

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

Failed to parse (Missing texvc executable; please see math/README to configure.): y - 8 = 12(x - 2) = 12x - 24 \,

or:

Failed to parse (Missing texvc executable; please see math/README to configure.): y = 12x - 16. \,


The slope of the line defined by the linear equation

Failed to parse (Missing texvc executable; please see math/README to configure.): ax + by +c = 0 \,

is: Failed to parse (Missing texvc executable; please see math/README to configure.): -\frac {a}{b} \; .

Calculus [link]

At each point, the derivative is the slope of a line that is tangent to the curve. The line is always tangent to the blue curve; its slope is the derivative. Note derivative is positive where green, negative where red, and zero where black

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.

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,

Failed to parse (Missing texvc executable; please see math/README to configure.): m = \frac{\Delta y}{\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 3. (The slope of the tangent at x = 32 is also 3—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 Δyx 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 Δyx as Δx approaches zero, or dy/dx. We call this limit the derivative.

Failed to parse (Missing texvc executable; please see math/README to configure.): \frac{dy}{dx} = \lim_{\Delta x \to 0}\frac{\Delta y}{\Delta x}


See also [link]

External links [link]


https://wn.com/Slope

Steep (disambiguation)

Steep is a village in central Hampshire, England.

Steep may also refer to:

  • Steep (incline), an elementary mathematical concept
  • Steep (technique), a cooking technique employing soaking
  • Geography

  • Steep, Hampshire
  • Steep Hill a popular tourist street in the historic city of Lincoln, Lincolnshire, England.
  • Steep Holm an English island lying in the Bristol Channel
  • Steep Island, Hong Kong
  • Steep Island, Australia
  • Steep Point westernmost point of the Australian mainland
  • People

  • Frederick Steep (1874-1956), Canadian amateur football (soccer) player
  • Film and TV

  • Steep (2007 film), a movie about extreme skiing
  • Steep, 1988 concert video by Branford Marsalis featuring Kenny Kirkland; Delbert Felix; Louis Nash; Herbie Hancock; Danny DeVito; Billy Crystal; Spike Lee; Sting, (Musician); Ken Dennis; Phyllis MacBryde; Sy Miller 1988.
  • Acronyms

  • STEEP analysis PEST analysis a common business analysis framework.

  • Steeping

    Steeping is the soaking in liquid (usually water) of a solid so as to extract flavours or to soften it. Some teas are prepared for drinking by steeping the leaves in heated water to release the flavour and nutrients. Herbal teas may be prepared by decoction, infusion, or maceration. Some solids are soaked to remove an ingredient, such as salt from smoked ham or salted cod, where the solvent is not the desired product.

    Corn

    One example is the steeping of corn (or maize), part of the milling process. As described by the US Corn Refiners Association, harvested kernels of corn are cleaned and then steeped in water at a temperature of 50 °C (120 °F) for 30 to 40 hours. In the process their moisture content rises from 15% to 45% and their volume more than doubles. The gluten bonds in the corn are weakened and starch is released. The corn is then ground to break free the germ and other components, and the water used (steepwater), which has absorbed various nutrients, is recycled for use in animal feeds.

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