In geometry, a straight line, usually abbreviated line, is an infinitely long object with no width, depth, or curvature, an idealization of such physical objects as a straightedge, a taut string, or a ray of light. Lines are spaces of dimension one, which may be Embedding in spaces of dimension two, three, or higher. The word line may also refer, in everyday life, to a line segment, which is a part of a line delimited by two points (its endpoints).
Euclid's Elements defines a straight line as a "breadthless length" that "lies evenly with respect to the points on itself", and introduced several as basic unprovable properties on which the rest of geometry was established. Euclidean line and Euclidean geometry are terms introduced to avoid confusion with generalizations introduced since the end of the 19th century, such as non-Euclidean, projective, and affine geometry.
In an axiomatic formulation of Euclidean geometry, such as that of Hilbert (modern mathematicians added to Euclid's original axioms to fill perceived logical gaps), a line is stated to have certain properties that relate it to other lines and points. For example, for any two distinct points, there is a unique line containing them, and any two distinct lines intersect at most at one point. In two (i.e., the Euclidean plane), two lines that do not intersect are called parallel. In higher dimensions, two lines that do not intersect are parallel if they are contained in a plane, or Skew lines if they are not.
On a Euclidean plane, a line can be represented as a boundary between two regions. Any collection of finitely many lines partitions the plane into (possibly unbounded); this partition is known as an arrangement of lines.
In more general Euclidean space, R n (and analogously in every other affine space), the line L passing through two different points a and b is the subset The direction of the line is from a reference point a ( t = 0) to another point b ( t = 1), or in other words, in the direction of the vector b − a. Different choices of a and b can yield the same line.
In affine coordinates, in n-dimensional space the points X = ( x1, x2, ..., x n), Y = ( y1, y2, ..., y n), and Z = ( z1, z2, ..., z n) are collinear if the matrix has a rank less than 3. In particular, for three points in the plane ( n = 2), the above matrix is square and the points are collinear if and only if its determinant is zero.
Equivalently for three points in a plane, the points are collinear if and only if the slope between one pair of points equals the slope between any other pair of points (in which case the slope between the remaining pair of points will equal the other slopes). By extension, k points in a plane are collinear if and only if any ( k–1) pairs of points have the same pairwise slopes.
In Euclidean geometry, the Euclidean distance d( a, b) between two points a and b may be used to express the collinearity between three points by:
In the geometries where the concept of a line is a primitive notion, as may be the case in some synthetic geometries, other methods of determining collinearity are needed.
For instance, with respect to a Conic section (a circle, ellipse, parabola, or hyperbola), lines can be:
In the context of determining parallelism in Euclidean geometry, a transversal is a line that intersects two other lines that may or not be parallel to each other.
For more general , lines could also be:
For a convex polygon quadrilateral with at most two parallel sides, the Newton line is the line that connects the midpoints of the two .
For a hexagon with vertices lying on a conic we have the Pascal line and, in the special case where the conic is a pair of lines, we have the Pappus line.
Parallel lines are lines in the same plane that never cross. Intersecting lines share a single point in common. Coincidental lines coincide with each other—every point that is on either one of them is also on the other.
Perpendicular lines are lines that intersect at .
In three-dimensional space, skew lines are lines that are not in the same plane and thus do not intersect each other.
However, the axiomatic definition of a line does not explain the relevance of the concept and is often too abstract for beginners. So, the definition is often replaced or completed by a mental image or intuitive description that allows understanding of what a line is. Such descriptions are sometimes referred to as definitions, but are not true definitions since they cannot be used in mathematical proofs. The "definition" of a line in Euclid's Elements falls into this category; and is never used in proofs of theorems.
One can further suppose either or , by dividing everything by if it is not zero.
There are many variant ways to write the equation of a line which can all be converted from one to another by algebraic manipulation. The above form is sometimes called the standard form. If the constant term is put on the left, the equation becomes and this is sometimes called the general form of the equation. However, this terminology is not universally accepted, and many authors do not distinguish these two forms.
These forms are generally named by the type of information (data) about the line that is needed to write down the form. Some of the important data of a line is its slope, x-intercept, known points on the line and y-intercept.
The equation of the line passing through two different points and may be written as If , this equation may be rewritten as or In two dimensions, the equation for non-vertical lines is often given in the slope–intercept form:
where:
The slope of the line through points and , when , is given by and the equation of this line can be written .
As a note, lines in three dimensions may also be described as the simultaneous solutions of two such that and are not proportional (the relations imply ). This follows since in three dimensions a single linear equation typically describes a plane and a line is what is common to two distinct intersecting planes.
In three dimensions lines are frequently described by parametric equations: where:
Parametric equations for lines in higher dimensions are similar in that they are based on the specification of one point on the line and a direction vector.
Unlike the slope-intercept and intercept forms, this form can represent any line but also requires only two finite parameters, and , to be specified. If , then is uniquely defined modulo . On the other hand, if the line is through the origin (), one drops the term to compute and , and it follows that is only defined modulo .
If a is vector OA and b is vector OB, then the equation of the line can be written: .
A ray starting at point A is described by limiting λ. One ray is obtained if λ ≥ 0, and the opposite ray comes from λ ≤ 0.
In polar coordinates, the equation of a line not passing through the origin—the point with coordinates —can be written with and Here, is the (positive) length of the line segment perpendicular to the line and delimited by the origin and the line, and is the (oriented) angle from the -axis to this segment.
It may be useful to express the equation in terms of the angle between the -axis and the line. In this case, the equation becomes with and
These equations can be derived from the normal form of the line equation by setting and and then applying the angle difference identity for sine or cosine.
These equations can also be proven geometry by applying right triangle definitions of sine and cosine to the right triangle that has a point of the line and the origin as vertices, and the line and its perpendicular through the origin as sides.
The previous forms do not apply for a line passing through the origin, but a simpler formula can be written: the polar coordinates of the points of a line passing through the origin and making an angle of with the -axis, are the pairs such that
When a geometry is described by a set of , the notion of a line is usually left undefined (a so-called primitive notion object). The properties of lines are then determined by the axioms which refer to them. One advantage to this approach is the flexibility it gives to users of the geometry. Thus in differential geometry, a line may be interpreted as a geodesic (shortest path between points), while in some projective geometries, a line is a 2-dimensional vector space (all linear combinations of two independent vectors). This flexibility also extends beyond mathematics and, for example, permits physicists to think of the path of a light ray as being a line.
The "shortness" and "straightness" of a line, interpreted as the property that the distance along the line between any two of its points is minimized (see triangle inequality), can be generalized and leads to the concept of in .
Given distinct points A and B, they determine a unique ray with initial point A. As two points define a unique line, this ray consists of all the points between A and B (including A and B) and all the points C on the line through A and B such that B is between A and C. This is, at times, also expressed as the set of all points C on the line determined by A and B such that A is not between B and C. A point D, on the line determined by A and B but not in the ray with initial point A determined by B, will determine another ray with initial point A. With respect to the AB ray, the AD ray is called the opposite ray.
Thus, we would say that two different points, A and B, define a line and a decomposition of this line into the disjoint union of an open segment and two rays, BC and AD (the point D is not drawn in the diagram, but is to the left of A on the line AB). These are not opposite rays since they have different initial points.
In Euclidean geometry two rays with a common endpoint form an angle.
The definition of a ray depends upon the notion of betweenness for points on a line. It follows that rays exist only for geometries for which this notion exists, typically Euclidean geometry or affine geometry over an ordered field. On the other hand, rays do not exist in projective geometry nor in a geometry over a non-ordered field, like the or any finite field.
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