Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet
Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet
It remains to show a way to minimize Q, subject to (6.15). The way, however, is well-known. One simply intrsduces as (N+1 )-st unknown a Lagrangian parameter X and minimizes the quantity a Q' = Q + h (Cai~li - 1 ) , ui = / Gi (r)dr (6.16) 0 The differentiation of (6.16) with respect to the (N4-1) unknowns yields the (N+1) linear equations where Qik = W Sik + (l-W) c Eik. This system of equations is easily solved. The meaning of X is revealed by multiplying (6.17a) by ak, adding and using (6.17b) and (6.15) . It results In the case W = 1, we have X = -2s. With a knowledge of a (roll i is obtained from (6.8) with gi = y. and E' from (6.9). 3- When is inserted in (6.1) instead of m(r) , it w ill in general not exactly reproduce the data. The minimization (6.15) N subject to the constraint C aiui = 1 admits for two data (N:=2) i=1 a simple geometrical interpretation: For constant s and E' these positive definite quantities are represented by ellipses, the con- straint is a line in the (al,a2)-plane. For uncorrelated errors, the principal axes of E~ are the al and a2 axis. hT1a W varies from 0 to 1 the combinatiomof (al ,a2) on the fat line are obtained. s and. E' are determined from the ellipses throughthese points,Sj-nce all s-(~~)-elli~ses are similar, s and^ 2
are proportional to the long axes of these ellipses. 6.1.3. The nonlinear inverse problem The Backus-Gilbert procedure applies only to linear inverse problems, where according to a the gross earth functionals gi have the property that This means for instance that the data are bui1.t up in an aclditive way from different parts of the model, i.e., that there is no coupling between these parts. This certainly does not hold for electromagnetic inverse problem, where each part of the conductor is coupled with all other parts. In nonlinear problems the data kernel Gi(r) will depend on m. Here it is in general possible to replace (6.18) by . a gi.(mr)-gi~m)=f(m'(r)-m(r))~i(x,m)dr + ~(m'-m)~, (6.18a) 0 where m and m' are two earth models. The data kernel Gi(r,m) is called the Fr6chet derivative or functional derivative at model m.
- Page 21 and 22: -- 2.5. Definition -- of the transf
- Page 23 and 24: we arrive at - v The same appl-ies
- Page 25 and 26: ) Computation of ---- C for a laxez
- Page 27 and 28: The approximate interpretation of C
- Page 29 and 30: I ~ispersi-on relations I Dispersio
- Page 31 and 32: where L is a positively oriented cl
- Page 33 and 34: 1 2 3 4 CPD 1 2 3 4 CPD - g) Depend
- Page 35 and 36: The TE-mode has no vertical electri
- Page 37 and 38: i I Earth Anomalous domain 3.2. Air
- Page 39 and 40: Hence, the conductivity is to be av
- Page 41 and 42: The RHS i.s a closed line integral
- Page 43 and 44: 4. Having determined B;, the coeffi
- Page 45 and 46: 3.4. Anomalous region as basic doma
- Page 47 and 48: - 6 and 6= can be so adjusted that
- Page 49 and 50: From the generalized Green's theore
- Page 51 and 52: and y can again be so adjusted that
- Page 53 and 54: 4.2. In3ral - --- equation method L
- Page 55 and 56: The element GZx is needed for all z
- Page 57 and 58: With this knowledge of the behaviou
- Page 59 and 60: After having determined Qzr VJ,; @,
- Page 61 and 62: 4.3. The surface inteyral approach
- Page 63 and 64: F At the vertical boundaries the co
- Page 65 and 66: The four equations A A A A H = i sg
- Page 68 and 69: 6. Approaches to the inverse proble
- Page 70 and 71: to minimize the quantity a s = 12 /
- Page 74 and 75: Agai-n, from a finite erroneous dat
- Page 76 and 77: Here lJ - is a N x P matrix contain
- Page 78 and 79: small eigenvalues. The parameter ve
- Page 80 and 81: Then - 77 - A(E2 - E ) = iwu U (E -
- Page 82 and 83: whence 2k d -2k d where a = CA:(A;)
- Page 84 and 85: . 7. Basic concepts of geomagnetic
- Page 86 and 87: orders of magnitude smaller' than t
- Page 88 and 89: Elimination of - E or .,. H yields
- Page 90 and 91: Observing that rot pot rot g = - ro
- Page 92 and 93: Two special types of such anomalies
- Page 94 and 95: Model : wo+ Solution for uniform ha
- Page 96 and 97: parameter u and that the pressure d
- Page 98 and 99: (=disturbed)-variations: After magn
- Page 100 and 101: with 4 as geographic latitude. From
- Page 102 and 103: Very rapid oscillations with freque
- Page 104 and 105: ! 8. Data Collection - and Analysis
- Page 106 and 107: A horizontal electric -- field comp
- Page 108 and 109: For a data reducti.on in the fr3equ
- Page 110 and 111: Let q be the tranfer function betwe
- Page 112 and 113: . A as transfer function between A
- Page 114 and 115: -- Structural soundi~z with station
- Page 116 and 117: Since it follows that - E 1 = - T E
- Page 118 and 119: - - . the same or from different si
- Page 120 and 121: The Fourier integral - +- -io t T -
It remains to show a way to minimize Q, subject to (6.15). The way,<br />
however, is well-known. One simply intrsduces as (N+1 )-st unknown<br />
a Lagrangian parameter X and minimizes the quantity<br />
a<br />
Q' = Q + h (Cai~li - 1 ) , ui = / Gi (r)dr (6.16)<br />
0<br />
The differentiation of (6.16) with respect to the (N4-1) unknowns<br />
yields the (N+1) linear equations<br />
where Qik = W Sik + (l-W) c Eik.<br />
This system of equations is easily solved. The meaning of X is<br />
revealed by multiplying (6.17a) by ak, adding and using (6.17b)<br />
and (6.15) . It results<br />
In the case W = 1, we have X = -2s. With a knowledge of a (roll<br />
i<br />
is obtained from (6.8) with gi = y. and E' from (6.9).<br />
3-<br />
When is inserted in (6.1) instead of m(r) , it w ill in<br />
general not exactly reproduce the data.<br />
The minimization (6.15)<br />
N<br />
subject to the constraint C aiui = 1 admits for two data (N:=2)<br />
i=1<br />
a simple geometrical interpretation: For constant s and E' these<br />
positive definite quantities are represented by ellipses, the con-<br />
straint is a line in the (al,a2)-plane. For uncorrelated errors,<br />
the principal axes of E~ are the al and a2 axis.<br />
hT1a W varies from 0 to 1 the combinatiomof (al ,a2) on the fat<br />
line are obtained. s and. E' are determined from the ellipses<br />
throughthese points,Sj-nce all s-(~~)-elli~ses are similar, s and^<br />
2