Serveur d'exploration sur l'Université de Trèves

Attention, ce site est en cours de développement !
Attention, site généré par des moyens informatiques à partir de corpus bruts.
Les informations ne sont donc pas validées.

Damped least-squares inversion of confined aquifer pumping data based on singular value decomposition

Identifieur interne : 001465 ( PascalFrancis/Corpus ); précédent : 001464; suivant : 001466

Damped least-squares inversion of confined aquifer pumping data based on singular value decomposition

Auteurs : ZEHRA YENIHAYAT

Source :

RBID : Pascal:96-0201423

Descripteurs français

English descriptors

Abstract

An iterative method for calculating the transmissivity and storage coefficient from pumping test data for a confined aquifer is presented. The method optimizes the fit between the measured and the theoretical data (computed using the Theis equation) in the least-square sense. Unlike the existing schemes, this method employs the Levenberg-Marquardt method and the singular value decomposition technique resulting in a stable and rapidly convergent data inversion algorithm. The inverse procedure is initialized by an automatically created starting model derived using a novel technique that operates on the time-derivative of the drawdown curve. An important feature of the algorithm is that all the computations are done in logarithmic space which effectively linearizes the problem. The proposed method has several advantages over the conventional iterative inversion algorithms because of the linearizing parameterizations at both the forward and inverse stages of the problem. Detailed derivations of the basic equations are provided to guide the potential users as well as applications to field data to demonstrate the usefulness of the proposed algorithm.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

pA  
A01 01  1    @0 0882-8121
A02 01      @0 MATGED
A03   1    @0 Math. geol.
A05       @2 28
A06       @2 2
A08 01  1  ENG  @1 Damped least-squares inversion of confined aquifer pumping data based on singular value decomposition
A09 01  1  ENG  @1 Inverse theory in the earth sciences
A11 01  1    @1 ZEHRA YENIHAYAT
A12 01  1    @1 HERZFELD (Ute Christina) @9 ed.
A14 01      @1 Ankara Universitesi, Fen Fak., Jeoloji Müh. B., Besevler @2 06100 Ankara @3 TUR @Z 1 aut.
A15 01      @1 FB VI Quantitative Methoden in den Geowissenschaften, Universität Trier @2 54286 Trier @3 DEU @Z 1 aut.
A15 02      @1 Institute of Arctic and Alpine Research, University of Colorado Boulder @2 Boulder, Colorado 80309-0450 @3 USA @Z 1 aut.
A20       @1 203-228
A21       @1 1996
A23 01      @0 ENG
A43 01      @1 INIST @2 14907 @5 354000053329610040
A44       @0 0000
A45       @0 1 p.1/2
A47 01  1    @0 96-0201423
A60       @1 P
A61       @0 A
A64 01  1    @0 Mathematical geology
A66 01      @0 USA
C01 01    ENG  @0 An iterative method for calculating the transmissivity and storage coefficient from pumping test data for a confined aquifer is presented. The method optimizes the fit between the measured and the theoretical data (computed using the Theis equation) in the least-square sense. Unlike the existing schemes, this method employs the Levenberg-Marquardt method and the singular value decomposition technique resulting in a stable and rapidly convergent data inversion algorithm. The inverse procedure is initialized by an automatically created starting model derived using a novel technique that operates on the time-derivative of the drawdown curve. An important feature of the algorithm is that all the computations are done in logarithmic space which effectively linearizes the problem. The proposed method has several advantages over the conventional iterative inversion algorithms because of the linearizing parameterizations at both the forward and inverse stages of the problem. Detailed derivations of the basic equations are provided to guide the potential users as well as applications to field data to demonstrate the usefulness of the proposed algorithm.
C02 01  X    @0 001E01N02
C02 02  2    @0 226A02
C03 01  X  FRE  @0 Nappe captive @5 01
C03 01  X  ENG  @0 Artesian water @5 01
C03 01  X  SPA  @0 Capa cautiva @5 01
C03 02  X  FRE  @0 Problème inverse @5 26
C03 02  X  ENG  @0 Inverse problem @5 26
C03 02  X  SPA  @0 Problema inverso @5 26
C03 03  X  FRE  @0 Pompage @5 27
C03 03  X  ENG  @0 Pumping @5 27
C03 03  X  SPA  @0 Bombeo @5 27
C03 04  X  FRE  @0 Méthode itérative @5 28
C03 04  X  ENG  @0 Iterative method @5 28
C03 04  X  SPA  @0 Método iterativo @5 28
C03 05  X  FRE  @0 Décomposition valeur singulière @5 29
C03 05  X  ENG  @0 Singular value decomposition @5 29
C03 05  X  SPA  @0 Decomposición valor singular @5 29
C03 06  X  FRE  @0 Nappe phréatique @5 30
C03 06  X  ENG  @0 Ground water table @5 30
C03 06  X  SPA  @0 Capa freática @5 30
N21       @1 134

Format Inist (serveur)

NO : PASCAL 96-0201423 INIST
ET : Damped least-squares inversion of confined aquifer pumping data based on singular value decomposition
AU : ZEHRA YENIHAYAT; HERZFELD (Ute Christina)
AF : Ankara Universitesi, Fen Fak., Jeoloji Müh. B., Besevler/06100 Ankara/Turquie (1 aut.); FB VI Quantitative Methoden in den Geowissenschaften, Universität Trier/54286 Trier/Allemagne (1 aut.); Institute of Arctic and Alpine Research, University of Colorado Boulder/Boulder, Colorado 80309-0450/Etats-Unis (1 aut.)
DT : Publication en série; Niveau analytique
SO : Mathematical geology; ISSN 0882-8121; Coden MATGED; Etats-Unis; Da. 1996; Vol. 28; No. 2; Pp. 203-228; Bibl. 1 p.1/2
LA : Anglais
EA : An iterative method for calculating the transmissivity and storage coefficient from pumping test data for a confined aquifer is presented. The method optimizes the fit between the measured and the theoretical data (computed using the Theis equation) in the least-square sense. Unlike the existing schemes, this method employs the Levenberg-Marquardt method and the singular value decomposition technique resulting in a stable and rapidly convergent data inversion algorithm. The inverse procedure is initialized by an automatically created starting model derived using a novel technique that operates on the time-derivative of the drawdown curve. An important feature of the algorithm is that all the computations are done in logarithmic space which effectively linearizes the problem. The proposed method has several advantages over the conventional iterative inversion algorithms because of the linearizing parameterizations at both the forward and inverse stages of the problem. Detailed derivations of the basic equations are provided to guide the potential users as well as applications to field data to demonstrate the usefulness of the proposed algorithm.
CC : 001E01N02; 226A02
FD : Nappe captive; Problème inverse; Pompage; Méthode itérative; Décomposition valeur singulière; Nappe phréatique
ED : Artesian water; Inverse problem; Pumping; Iterative method; Singular value decomposition; Ground water table
SD : Capa cautiva; Problema inverso; Bombeo; Método iterativo; Decomposición valor singular; Capa freática
LO : INIST-14907.354000053329610040
ID : 96-0201423

Links to Exploration step

Pascal:96-0201423

Le document en format XML

<record>
<TEI>
<teiHeader>
<fileDesc>
<titleStmt>
<title xml:lang="en" level="a">Damped least-squares inversion of confined aquifer pumping data based on singular value decomposition</title>
<author>
<name sortKey="Zehra Yenihayat" sort="Zehra Yenihayat" uniqKey="Zehra Yenihayat" last="Zehra Yenihayat">ZEHRA YENIHAYAT</name>
<affiliation>
<inist:fA14 i1="01">
<s1>Ankara Universitesi, Fen Fak., Jeoloji Müh. B., Besevler</s1>
<s2>06100 Ankara</s2>
<s3>TUR</s3>
<sZ>1 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
</titleStmt>
<publicationStmt>
<idno type="wicri:source">INIST</idno>
<idno type="inist">96-0201423</idno>
<date when="1996">1996</date>
<idno type="stanalyst">PASCAL 96-0201423 INIST</idno>
<idno type="RBID">Pascal:96-0201423</idno>
<idno type="wicri:Area/PascalFrancis/Corpus">001465</idno>
</publicationStmt>
<sourceDesc>
<biblStruct>
<analytic>
<title xml:lang="en" level="a">Damped least-squares inversion of confined aquifer pumping data based on singular value decomposition</title>
<author>
<name sortKey="Zehra Yenihayat" sort="Zehra Yenihayat" uniqKey="Zehra Yenihayat" last="Zehra Yenihayat">ZEHRA YENIHAYAT</name>
<affiliation>
<inist:fA14 i1="01">
<s1>Ankara Universitesi, Fen Fak., Jeoloji Müh. B., Besevler</s1>
<s2>06100 Ankara</s2>
<s3>TUR</s3>
<sZ>1 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
</analytic>
<series>
<title level="j" type="main">Mathematical geology</title>
<title level="j" type="abbreviated">Math. geol.</title>
<idno type="ISSN">0882-8121</idno>
<imprint>
<date when="1996">1996</date>
</imprint>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt>
<title level="j" type="main">Mathematical geology</title>
<title level="j" type="abbreviated">Math. geol.</title>
<idno type="ISSN">0882-8121</idno>
</seriesStmt>
</fileDesc>
<profileDesc>
<textClass>
<keywords scheme="KwdEn" xml:lang="en">
<term>Artesian water</term>
<term>Ground water table</term>
<term>Inverse problem</term>
<term>Iterative method</term>
<term>Pumping</term>
<term>Singular value decomposition</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr">
<term>Nappe captive</term>
<term>Problème inverse</term>
<term>Pompage</term>
<term>Méthode itérative</term>
<term>Décomposition valeur singulière</term>
<term>Nappe phréatique</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front>
<div type="abstract" xml:lang="en">An iterative method for calculating the transmissivity and storage coefficient from pumping test data for a confined aquifer is presented. The method optimizes the fit between the measured and the theoretical data (computed using the Theis equation) in the least-square sense. Unlike the existing schemes, this method employs the Levenberg-Marquardt method and the singular value decomposition technique resulting in a stable and rapidly convergent data inversion algorithm. The inverse procedure is initialized by an automatically created starting model derived using a novel technique that operates on the time-derivative of the drawdown curve. An important feature of the algorithm is that all the computations are done in logarithmic space which effectively linearizes the problem. The proposed method has several advantages over the conventional iterative inversion algorithms because of the linearizing parameterizations at both the forward and inverse stages of the problem. Detailed derivations of the basic equations are provided to guide the potential users as well as applications to field data to demonstrate the usefulness of the proposed algorithm.</div>
</front>
</TEI>
<inist>
<standard h6="B">
<pA>
<fA01 i1="01" i2="1">
<s0>0882-8121</s0>
</fA01>
<fA02 i1="01">
<s0>MATGED</s0>
</fA02>
<fA03 i2="1">
<s0>Math. geol.</s0>
</fA03>
<fA05>
<s2>28</s2>
</fA05>
<fA06>
<s2>2</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG">
<s1>Damped least-squares inversion of confined aquifer pumping data based on singular value decomposition</s1>
</fA08>
<fA09 i1="01" i2="1" l="ENG">
<s1>Inverse theory in the earth sciences</s1>
</fA09>
<fA11 i1="01" i2="1">
<s1>ZEHRA YENIHAYAT</s1>
</fA11>
<fA12 i1="01" i2="1">
<s1>HERZFELD (Ute Christina)</s1>
<s9>ed.</s9>
</fA12>
<fA14 i1="01">
<s1>Ankara Universitesi, Fen Fak., Jeoloji Müh. B., Besevler</s1>
<s2>06100 Ankara</s2>
<s3>TUR</s3>
<sZ>1 aut.</sZ>
</fA14>
<fA15 i1="01">
<s1>FB VI Quantitative Methoden in den Geowissenschaften, Universität Trier</s1>
<s2>54286 Trier</s2>
<s3>DEU</s3>
<sZ>1 aut.</sZ>
</fA15>
<fA15 i1="02">
<s1>Institute of Arctic and Alpine Research, University of Colorado Boulder</s1>
<s2>Boulder, Colorado 80309-0450</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
</fA15>
<fA20>
<s1>203-228</s1>
</fA20>
<fA21>
<s1>1996</s1>
</fA21>
<fA23 i1="01">
<s0>ENG</s0>
</fA23>
<fA43 i1="01">
<s1>INIST</s1>
<s2>14907</s2>
<s5>354000053329610040</s5>
</fA43>
<fA44>
<s0>0000</s0>
</fA44>
<fA45>
<s0>1 p.1/2</s0>
</fA45>
<fA47 i1="01" i2="1">
<s0>96-0201423</s0>
</fA47>
<fA60>
<s1>P</s1>
</fA60>
<fA61>
<s0>A</s0>
</fA61>
<fA64 i1="01" i2="1">
<s0>Mathematical geology</s0>
</fA64>
<fA66 i1="01">
<s0>USA</s0>
</fA66>
<fC01 i1="01" l="ENG">
<s0>An iterative method for calculating the transmissivity and storage coefficient from pumping test data for a confined aquifer is presented. The method optimizes the fit between the measured and the theoretical data (computed using the Theis equation) in the least-square sense. Unlike the existing schemes, this method employs the Levenberg-Marquardt method and the singular value decomposition technique resulting in a stable and rapidly convergent data inversion algorithm. The inverse procedure is initialized by an automatically created starting model derived using a novel technique that operates on the time-derivative of the drawdown curve. An important feature of the algorithm is that all the computations are done in logarithmic space which effectively linearizes the problem. The proposed method has several advantages over the conventional iterative inversion algorithms because of the linearizing parameterizations at both the forward and inverse stages of the problem. Detailed derivations of the basic equations are provided to guide the potential users as well as applications to field data to demonstrate the usefulness of the proposed algorithm.</s0>
</fC01>
<fC02 i1="01" i2="X">
<s0>001E01N02</s0>
</fC02>
<fC02 i1="02" i2="2">
<s0>226A02</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE">
<s0>Nappe captive</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG">
<s0>Artesian water</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA">
<s0>Capa cautiva</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE">
<s0>Problème inverse</s0>
<s5>26</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG">
<s0>Inverse problem</s0>
<s5>26</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA">
<s0>Problema inverso</s0>
<s5>26</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE">
<s0>Pompage</s0>
<s5>27</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG">
<s0>Pumping</s0>
<s5>27</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA">
<s0>Bombeo</s0>
<s5>27</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE">
<s0>Méthode itérative</s0>
<s5>28</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG">
<s0>Iterative method</s0>
<s5>28</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA">
<s0>Método iterativo</s0>
<s5>28</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE">
<s0>Décomposition valeur singulière</s0>
<s5>29</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG">
<s0>Singular value decomposition</s0>
<s5>29</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA">
<s0>Decomposición valor singular</s0>
<s5>29</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE">
<s0>Nappe phréatique</s0>
<s5>30</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG">
<s0>Ground water table</s0>
<s5>30</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA">
<s0>Capa freática</s0>
<s5>30</s5>
</fC03>
<fN21>
<s1>134</s1>
</fN21>
</pA>
</standard>
<server>
<NO>PASCAL 96-0201423 INIST</NO>
<ET>Damped least-squares inversion of confined aquifer pumping data based on singular value decomposition</ET>
<AU>ZEHRA YENIHAYAT; HERZFELD (Ute Christina)</AU>
<AF>Ankara Universitesi, Fen Fak., Jeoloji Müh. B., Besevler/06100 Ankara/Turquie (1 aut.); FB VI Quantitative Methoden in den Geowissenschaften, Universität Trier/54286 Trier/Allemagne (1 aut.); Institute of Arctic and Alpine Research, University of Colorado Boulder/Boulder, Colorado 80309-0450/Etats-Unis (1 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Mathematical geology; ISSN 0882-8121; Coden MATGED; Etats-Unis; Da. 1996; Vol. 28; No. 2; Pp. 203-228; Bibl. 1 p.1/2</SO>
<LA>Anglais</LA>
<EA>An iterative method for calculating the transmissivity and storage coefficient from pumping test data for a confined aquifer is presented. The method optimizes the fit between the measured and the theoretical data (computed using the Theis equation) in the least-square sense. Unlike the existing schemes, this method employs the Levenberg-Marquardt method and the singular value decomposition technique resulting in a stable and rapidly convergent data inversion algorithm. The inverse procedure is initialized by an automatically created starting model derived using a novel technique that operates on the time-derivative of the drawdown curve. An important feature of the algorithm is that all the computations are done in logarithmic space which effectively linearizes the problem. The proposed method has several advantages over the conventional iterative inversion algorithms because of the linearizing parameterizations at both the forward and inverse stages of the problem. Detailed derivations of the basic equations are provided to guide the potential users as well as applications to field data to demonstrate the usefulness of the proposed algorithm.</EA>
<CC>001E01N02; 226A02</CC>
<FD>Nappe captive; Problème inverse; Pompage; Méthode itérative; Décomposition valeur singulière; Nappe phréatique</FD>
<ED>Artesian water; Inverse problem; Pumping; Iterative method; Singular value decomposition; Ground water table</ED>
<SD>Capa cautiva; Problema inverso; Bombeo; Método iterativo; Decomposición valor singular; Capa freática</SD>
<LO>INIST-14907.354000053329610040</LO>
<ID>96-0201423</ID>
</server>
</inist>
</record>

Pour manipuler ce document sous Unix (Dilib)

EXPLOR_STEP=$WICRI_ROOT/Wicri/Rhénanie/explor/UnivTrevesV1/Data/PascalFrancis/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 001465 | SxmlIndent | more

Ou

HfdSelect -h $EXPLOR_AREA/Data/PascalFrancis/Corpus/biblio.hfd -nk 001465 | SxmlIndent | more

Pour mettre un lien sur cette page dans le réseau Wicri

{{Explor lien
   |wiki=    Wicri/Rhénanie
   |area=    UnivTrevesV1
   |flux=    PascalFrancis
   |étape=   Corpus
   |type=    RBID
   |clé=     Pascal:96-0201423
   |texte=   Damped least-squares inversion of confined aquifer pumping data based on singular value decomposition
}}

Wicri

This area was generated with Dilib version V0.6.31.
Data generation: Sat Jul 22 16:29:01 2017. Site generation: Wed Feb 28 14:55:37 2024