Basic Elements. Geometry is the study of the relationships among objects in an n-dimensional space
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1 Basic Elements Geometry is the study of the relationships among objects in an n-dimensional space In computer graphics, we are interested in objects that exist in three dimensions We want a minimum set of primitives from which we can build more sophisticated objects We will need three basic elements Scalars Vectors Points
2 Coordinate-Free Geometry When we learned simple geometry, most of us started with a Cartesian approach Points were at locations in space p=(x,y,z) We derived results by algebraic manipulations involving these coordinates This approach was nonphysical Physically, points exist regardless of the location of an arbitrary coordinate system Most geometric results are independent of the coordinate system Example Euclidean geometry: two triangles are identical if two corresponding sides and the angle between them are identical
3 Vectors Physical definition: a vector is a quantity with two attributes Direction Magnitude Examples include Force Velocity Directed line segments Most important example for graphics Can map to other types v
4 Vector Operations Every vector has an inverse Same magnitude but points in opposite direction Every vector can be multiplied by a scalar There is a zero vector Zero magnitude, undefined orientation The sum of any two vectors is a vector Use head-to-tail axiom v -v v v w u
5 Vectors Lack Position These vectors are identical Same length and magnitude Vectors spaces insufficient for geometry Need points
6 Points Location in space Operations allowed between points and vectors Point-point subtraction yields a vector Equivalent to point-vector addition v=p-q P=v+Q
7 Planes A plane can be defined by a point and two vectors or by three points P v Q R u R
8 Normals Every plane has a vector n normal (perpendicular, orthogonal) to it We can use the cross product to find n = u v v P u
9 Representation Until now we have been able to work with geometric entities without using any frame of reference, such as a coordinate system Need a frame of reference to relate points and objects to our physical world. For example, where is a point? Can t answer without a reference system World coordinates Camera coordinates
10 Frames A coordinate system is insufficient to represent points We can add a single point, the origin, to the basis vectors to form a frame v 2 P v 1 v 3
11 Confusing Points and Vectors Consider the point and the vector P = P + b 1 v 1 + b 2 v 2 +.+b n v n v= 1 v v n v n They appear to have the similar representations p=[b 1 b 2 b 3 ] v=[ ] which confuses the point with the vector A vector has no position v v p Vector can be placed anywhere point: fixed
12 A Single Representation If we define P = and 1 P =P then we can write v= 1 v v v 3 = [ ] [v 1 v 2 v 3 P ] T P = P + b 1 v 1 + b 2 v 2 +b 3 v 3 = [b 1 b 2 b 3 1 ] [v 1 v 2 v 3 P ] T Thus we obtain the four-dimensional homogeneous coordinate representation v = [ ] T p = [b 1 b 2 b 3 1 ] T
13 Homogeneous Coordinates The homogeneous coordinates form for a three dimensional point [x y z] is given as p =[x y z w] T =[wx wy wz w] T We return to a three dimensional point (for w) by xx /w yy /w zz /w If w=, the representation is that of a vector Note that homogeneous coordinates replaces points in three dimensions by lines through the origin in four dimensions For w=1, the representation of a point is [x y z 1]
14 Homogeneous Coordinates and Computer Graphics Homogeneous coordinates are key to all computer graphics systems All standard transformations (rotation, translation, scaling) can be implemented with matrix multiplications using 4 x 4 matrices Hardware pipeline works with 4 dimensional representations For orthographic viewing, we can maintain w= for vectors and w=1 for points
15 The World and Camera Frames In OpenGL, the base frame that we start with is the world frame Eventually we represent entities in the camera frame by changing the world representation using the modelview matrix Initially these frames are the same (M=I)
16 Transformations A transformation maps points to other points and/or vectors to other vectors Importance in graphics is that we need only transform endpoints of line segments and let implementation draw line segment between the transformed endpoints Q=T(P) v=t(u)
17 Pipeline Implementation T (from application program) u T(u) frame buffer v transformation T(v) rasterization T(v) v T(v) T(u) u T(u) vertices vertices pixels
18 Translation Move (translate, displace) a point to a new location P P d Displacement determined by a vector d P =P+d
19 Translation Using Representations Using the homogeneous coordinate representation in some frame p=[ x y z 1] T p =[x y z 1] T d=[dx dy dz ] T Hence p = p + d or x =x+d x y =y+d y z =z+d z note that this expression is in four dimensions and expresses point = vector + point
20 Translation Matrix We can also express translation using a 4 x 4 matrix T in homogeneous coordinates p =Tp where T = T(d x, d y, d z ) = 1 1 This form is better for implementation because all transformations can be expressed this way and multiple transformations can be concatenated together 1 d d d x y z 1
21 Moving the Camera If objects are on both sides of z=, we must move camera frame M = d 1
22 Rotation (2D) Consider rotation about the origin by q degrees radius stays the same, angle increases by q x = r cos (f + q) y = r sin (f + q) x =x cos q y sin q y = x sin q + y cos q x = r cos f y = r sin f
23 Rotation about the z axis Rotation about z axis in three dimensions leaves all points with the same z Equivalent to rotation in two dimensions in planes of constant z x =x cos q y sin q y = x sin q + y cos q z =z or in homogeneous coordinates p =R z (q)p R = R z (q) = cos sin q q sin q cos q 1 1
24 Rotation about x and y axes Same argument as for rotation about z axis For rotation about x axis, x is unchanged For rotation about y axis, y is unchanged R = R x (q) = R = R y (q) = q q q q 1 cos sin - sin cos 1 q q q q 1 cos - sin 1 sin cos
25 Scaling 1 z y x s s s S = S(s x, s y, s z ) = x =s x x y =s y y z =s z z p =Sp Expand or contract along each axis (fixed point of origin)
26 Reflection corresponds to negative scale factors s x = -1 s y = 1 original s x = -1 s y = -1 s x = 1 s y = -1
27 Inverses Although we could compute inverse matrices by general formulas, we can use simple geometric observations Translation: T -1 (d x, d y, d z ) = T(-d x, -d y, -d z ) Rotation: R -1 (q) = R(-q) Holds for any rotation matrix Note that since cos(-q) = cos(q) and sin(-q)=-sin(q) R -1 (q) = R T (q) Scaling: S -1 (s x, s y, s z ) = S(1/s x, 1/s y, 1/s z )
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