3 r3 K ul gaS ul ul 17 a) The equations g*® Kp\ b) the normal-equations; c) the solution of Gp„ from the set of equations] GpoO 8- (i) d) the making up of the cofactors-tensor. The mathematical model to which the observations have to be submitted, is described by the equations: mp p* up i2\ a o f p is running from i, ,,b. The observations are p* with cofactors gaS (see II). The description of the mathematical model does not change, if equations (2) are replaced by another set which is dependant on the first one. The matrix up is multiplied by the unit lower triangular matrix A°p (4°= 1 if p o) A° up P* A° up pa p o The corrections e are determined so that A" u° pa =A" up p a 1 P o or A" up e" A" hp An up p* Ta pa p o p a r and E g'txg is a minimum. The solution is, using the multipliers of Lagrange tfccB A" up K oap pao or, after putting A" W= U" pa a e* g°*U°Ka. (3) The normal-equations become: „as U" Ul K =T". 0 a 0 p In these equations the coefficients] p a become zero if the A are solved as follows: P«3 u1 ul For U1 Ul o A\ -3-. a 3 2 u 1 ul a 0 If p 3 and equation 2 is already replaced, it is seen that grt u\ ug gas u* ul Al=and A\ r—etc.

Digitale Tijdschriftenarchief Stichting De Hollandse Cirkel en Geo Informatie Nederland

Tijdschrift voor Kadaster en Landmeetkunde (KenL) | 1957 | | pagina 25