Multidimensional Inverse Problems for Differential EquationsSpringer, 21 Ara 1970 - 59 sayfa |
Kitabın içinden
18 sonuçtan 1-3 arası sonuçlar
Sayfa
... Application of the Linearized Version of the Inverse Kinematic Problem to Geophysics CHAPTER 4 · Inverse Heat Conduction Problems with Continuously Active Sources 1. Inverse Heat Conduction Problems for a Half - Plane 2. n - Dimensional ...
... Application of the Linearized Version of the Inverse Kinematic Problem to Geophysics CHAPTER 4 · Inverse Heat Conduction Problems with Continuously Active Sources 1. Inverse Heat Conduction Problems for a Half - Plane 2. n - Dimensional ...
Sayfa 12
... Apply V1 ( p , 0 ) . Apply L to ( 3 ) and use formula ( 7 ) for Lv . This results in C1 1 k = 1 Ε ∞ 00 Lv = ɖ ( ε ) v 。( p , ε ) + { ( 8 ) + 2 ( c ) } ~ v Vo ( z , e ) d2 + 1 e k - 1 ( ɛ ) Vk ( P , ε ) dz Z d1 # Ε 0 + dz Z Σ k = 1 in ...
... Apply V1 ( p , 0 ) . Apply L to ( 3 ) and use formula ( 7 ) for Lv . This results in C1 1 k = 1 Ε ∞ 00 Lv = ɖ ( ε ) v 。( p , ε ) + { ( 8 ) + 2 ( c ) } ~ v Vo ( z , e ) d2 + 1 e k - 1 ( ɛ ) Vk ( P , ε ) dz Z d1 # Ε 0 + dz Z Σ k = 1 in ...
Sayfa 20
... Applying to ( 1 ) the operator L defined by ( 2 ) a ах Love pv ( x , p ) dp Lv = xv ( x , r ) + r we obtain Lv = x ... application of L to v ( x , r ) . Then in a similar way , we have Let ( 3 ) Lkv = 2п u ( x + r.cos , r.sin ) ( x + r ...
... Applying to ( 1 ) the operator L defined by ( 2 ) a ах Love pv ( x , p ) dp Lv = xv ( x , r ) + r we obtain Lv = x ... application of L to v ( x , r ) . Then in a similar way , we have Let ( 3 ) Lkv = 2п u ( x + r.cos , r.sin ) ( x + r ...
Diğer baskılar - Tümünü görüntüle
Multidimensional Inverse Problems for Differential Equations M. M. Lavrentiev,V. G. Romanov,V. G. Vasiliev Metin Parçacığı görünümü - 1970 |
Sık kullanılan terimler ve kelime öbekleri
absolutely integrable functions Akad analytic function belong boundary conditions CAUCHY data chapter coefficients consider const continuous function coordinates corresponding cosk Denote derive determining a function differential equation Dokl domain earth's ellipses ellipsoid of revolution expression family of curves following theorem function u(r fundamental solution given GREEN'S function half-plane half-space HÖLDER condition hyperplane inequality 18 integral equation integral geometry integral-geometric problem Introduce the notation inverse kinematic inverse kinematic problem inversion formula kernel Lavrentiev linearized inverse problem multidimensional inverse problems Nauk SSSR obtain parameters polar potential theory problem for equation problem of determining Problems for Differential R₁ R₂ right-hand side ROMANOV satisfies second kind SM,t solution to equation take FOURIER transforms telegraph equation two-parameter family unique solution uniqueness theorem unit circle variables VOLTERRA equation waves wxxx