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2000-05-03
Well testing: Interpretation methods - de Gilles Bourdarot (Author)

Caractéristiques Well testing: Interpretation methods

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Le Titre Du LivreWell testing: Interpretation methods
Date de Lancement2000-05-03
TraducteurElvis Amyra
Chiffre de Pages314 Pages
Taille du fichier58.91 MB
LangageFrançais & Anglais
ÉditeurPoetry Bookshop
ISBN-105175000821-DSY
Type de eBookEPub AMZ PDF LWP RPT
AuteurGilles Bourdarot
Digital ISBN107-8748014680-AXV
Nom de FichierWell-testing-Interpretation-methods.pdf

Télécharger Well testing: Interpretation methods Livre PDF Gratuit

Well Testing Interpretation Methods Janvier 1999 BOURDAROT Gilles Ajouter au panier 82 € Well Seismic Surveying Septembre 2003 COPPENS Françoise MARI JeanLuc Ajouter au panier 105 € Well Production Practical Handbook

Well Testing Interpretation Methods Janvier 1999 BOURDAROT Gilles Ajouter au panier 82 € Well Seismic Surveying Septembre 2003 COPPENS Françoise MARI JeanLuc Ajouter au panier 105 € Well Logging Vol 3 Well Logging and Reservoir Evaluation

Currently exploration and development of high pore permeability reservoirs has come to the late low porosity and permeability reservoirs become the focus of exploration and development Judging

interpretation of dimer levels must take into account the sensitivity and specificity of the assay the specificity is usually low and increased ddimer levels are encountered in many nonthrombotic situations the sensitivity varies among the different testing methods and is maximal with eliSa assays Highly sensitive assays allow exclusion of venous thromboembolism when ddimer levels are

This system is therefore particularly wellsuited for test runs with an autosampler ASC or for measurements of longer duration Pas de ligne de transfert Une ligne de transfert n’est plus nécessaire

To intep et step dadon tests Jacob’s method To interpret pumping tests 4 analytical solutions currently available To simulate drawdown based on the well and aquifer parameters For each of these modes project files are available in the tutorial folder in order to test OUAIP easily and quickly Figure 2 Schematic section accompanying the choice of an analytical solution Theis

The local K values in situ are obtained from two methods of field permeability tests constanthead CH and variablehead VH tests For homogeneous and isotropic aquifer layers the average local values of K in several wells can be representative of the K value of the soil because the scale effect is negligible The theories of the test and interpretation methods are mature however