The azimuthal square array electrical resistivity (DC) surveys were conducted in the Edaikkal, Ambasamudram, Tirunelveli District. The water is an essential part of industrial complex in the sugar cane agriculture development. The study area is 3 square kilometers under thick cover of red soil, gravel, quartzite ridge and hard rock of charnockite in study area. The surveys were carried out using the help of the equipments CRM-500 Aquameter, electrodes and wire spools with accessories. The array is expanded symmetrically about the centre point, in increments of A (2) ½, So that the sounding can be interpreted as a function of depth. The azimuthal polar plots, litho stratigraphical graphical representation were used to distinguish the depth wise variation of the resistivity change in the study area. From the electrical resistivity study the water bearing zone is occur at depth of 25,75m that range of apparent resistivity from 100-120 Ohm.m in quartzite ridge. he azimuthal square array methods have delineated geological structures of the quartzite ridge.
Les informations fournies dans la section « Synopsis » peuvent faire référence à une autre édition de ce titre.
The azimuthal square array electrical resistivity (DC) surveys were conducted in the Edaikkal, Ambasamudram, Tirunelveli District. The water is an essential part of industrial complex in the sugar cane agriculture development. The study area is 3 square kilometers under thick cover of red soil, gravel, quartzite ridge and hard rock of charnockite in study area. The surveys were carried out using the help of the equipments CRM-500 Aquameter, electrodes and wire spools with accessories. The array is expanded symmetrically about the centre point, in increments of A (2) ½, So that the sounding can be interpreted as a function of depth. The azimuthal polar plots, litho stratigraphical graphical representation were used to distinguish the depth wise variation of the resistivity change in the study area. From the electrical resistivity study the water bearing zone is occur at depth of 25,75m that range of apparent resistivity from 100-120 Ohm.m in quartzite ridge. he azimuthal square array methods have delineated geological structures of the quartzite ridge.
Dr.A.Antony Ravindran obtained his Ph.D Degree in Geology with first class and working as a Professor Department of Geology, V.O.Chidambaram College, Tuticorin in 2001. He has teaching working experiences as a Hydrogeologist for ten years as a Private Consultant.He has aquired field experience to carryout the 2D Geoelectrical Resistivity Imaging.
Les informations fournies dans la section « A propos du livre » peuvent faire référence à une autre édition de ce titre.
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Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -The azimuthal square array electrical resistivity (DC) surveys were conducted in the Edaikkal, Ambasamudram, Tirunelveli District. The water is an essential part of industrial complex in the sugar cane agriculture development. The study area is 3 square kilometers under thick cover of red soil, gravel, quartzite ridge and hard rock of charnockite in study area. The surveys were carried out using the help of the equipments CRM-500 Aquameter, electrodes and wire spools with accessories. The array is expanded symmetrically about the centre point, in increments of A (2) ½, So that the sounding can be interpreted as a function of depth. The azimuthal polar plots, litho stratigraphical graphical representation were used to distinguish the depth wise variation of the resistivity change in the study area. From the electrical resistivity study the water bearing zone is occur at depth of 25,75m that range of apparent resistivity from 100-120 Ohm.m in quartzite ridge. he azimuthal square array methods have delineated geological structures of the quartzite ridge. 68 pp. Englisch. N° de réf. du vendeur 9783659273506
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Etat : New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: A Antony RavindranDr.A.Antony Ravindran obtained his Ph.D Degree in Geology with first class and working as a Professor Department of Geology, V.O.Chidambaram College, Tuticorin in 2001. He has teaching working experiences as a Hyd. N° de réf. du vendeur 158984087
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Taschenbuch. Etat : Neu. Neuware -The azimuthal square array electrical resistivity (DC) surveys were conducted in the Edaikkal, Ambasamudram, Tirunelveli District. The water is an essential part of industrial complex in the sugar cane agriculture development. The study area is 3 square kilometers under thick cover of red soil, gravel, quartzite ridge and hard rock of charnockite in study area. The surveys were carried out using the help of the equipments CRM-500 Aquameter, electrodes and wire spools with accessories. The array is expanded symmetrically about the centre point, in increments of A (2) ¿, So that the sounding can be interpreted as a function of depth. The azimuthal polar plots, litho stratigraphical graphical representation were used to distinguish the depth wise variation of the resistivity change in the study area. From the electrical resistivity study the water bearing zone is occur at depth of 25,75m that range of apparent resistivity from 100-120 Ohm.m in quartzite ridge. he azimuthal square array methods have delineated geological structures of the quartzite ridge.Books on Demand GmbH, Überseering 33, 22297 Hamburg 68 pp. Englisch. N° de réf. du vendeur 9783659273506
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Taschenbuch. Etat : Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - The azimuthal square array electrical resistivity (DC) surveys were conducted in the Edaikkal, Ambasamudram, Tirunelveli District. The water is an essential part of industrial complex in the sugar cane agriculture development. The study area is 3 square kilometers under thick cover of red soil, gravel, quartzite ridge and hard rock of charnockite in study area. The surveys were carried out using the help of the equipments CRM-500 Aquameter, electrodes and wire spools with accessories. The array is expanded symmetrically about the centre point, in increments of A (2) ½, So that the sounding can be interpreted as a function of depth. The azimuthal polar plots, litho stratigraphical graphical representation were used to distinguish the depth wise variation of the resistivity change in the study area. From the electrical resistivity study the water bearing zone is occur at depth of 25,75m that range of apparent resistivity from 100-120 Ohm.m in quartzite ridge. he azimuthal square array methods have delineated geological structures of the quartzite ridge. N° de réf. du vendeur 9783659273506
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