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The resistivity values of the different layers' ranges from 3 Ωm to Ωm and were statistically analyzed from Golden Software Grapher. The geoelectrical sections for the study area consists of: the topsoil, sandy silt, sand and gravel, fractured rock and the fresh basement rock. Khatiwada, B. Çakmak, Tolga Full Text Available Organizasyonlar doküman, belge, web içerik ve e-posta yönetimi gibi farklı amaçlarla geliştirdikleri bilgi sistemlerini kurumsal içerik yönetimi altında bütünleştirmeye yönelmektedirler. Contour map and 3D map of bedrock and water bearing layers for the conceptual model were prepared with the help of surfer shows that the gradient of the contour is high in the surrounding parts and flat in the center of Valley. Results show that the electronic mail management systems in the related organization are at a higher level than the other systems, and records management systems should be developed more than other.

Khatiwada, B. This study was conducted by GWRDB to create a data base of the groundwater potential in the hilly area.

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Data were acquired from WDJD-4 and analyzed using computer aided software called IPI2win, which yield an automatic interpretation of the apparent resistivity and data were correlated with lithologs of the vertical section. Results obtained from software were rechecked by plotting the apparent resistivity value on Log-Log transparent graph sheet and manually interpreted using master curves and auxiliary curves.

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The resistivity values of the different layers' ranges from 3 Ωm to Ωm and were statistically analyzed fat burning foods truduzione Golden Software Grapher. Representative resistivity sounding curves with modeled layer obtained after inversion was used to delineate the aquifer and 1D geoelectric sections.

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The geoelectrical sections for the study area consists of: the topsoil, sandy silt, sand and gravel, fractured rock and the fresh basement rock. Contour map and 3D map of bedrock and water bearing layers for the conceptual model were prepared with the help of surfer shows that the gradient of the contour is high in the surrounding parts and flat in the center of Valley.

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