The resistivity interpretation was carried out using both manual (Koefoed ) and computerized (IPI2win ) interpretation to compute the true depths and. IPI2win is a program for 1D automatic and manual interpretation of VES curves. Interpretation mode VES curves could be received with different. The field data obtained have been analyzed using computer software (IPI2win) which gives an automatic interpretation of the apparent resistivity. The VES.
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The present study area occupies an areal extent of ,28 sq.
Additional titles containing ipi2win manual. The protective plug must be stuck into the parallel printer port of the computer where IPI2Win is to be run. If so, click the Install button of the window. Next [Ctrl-Left] displays the sounding curve and model properties for the next sounding point of the current data file. No further operation is then available. Profile interpolation [Shift-Ctrl-F3] implements the automated interpretation for ipiwin all the uninterpreted sounding curves of the currently opened profile using model parameters for other points as the initial model.
The VES results revealed heterogeneous nature of the subsurface geological sequence. Export displays the list of data formats to choose the mode of saving IPI data. There ipi2won two end members in spectrum of types of aquifers; confined and unconfined with semi confined aquifer being ipi2wim between them Ogungbe1 A.
Restore [Ctrl-F7] restores the model for the sounding point i. IPI2WIN Program is a program that was designed to analyze data from 1D geo-electric measurements on a single piece automatically or semi-automatically to get the smallest error.
Both the survey procedures resistivity profiling and resistivity sounding VES have been carried out. Preview displays Print preview window to see how the active window will be printed.
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Groundwater is more advantageous than the surface water. The junior member of our highly praised PDF-XChange range of software tools aimed at users wishing to create the smallest PDF files available – from any Windows application software. Soil structure is generally relatively well, but that must be addressed is the use of soil types andosols who have sensitive nature of erosion.
Last [End] displays the sounding curve and model properties for the last sounding point of the current. Groundwater is the main source for potable water supply, domestic, industry al and agricultural uses.
The path can also be pointed out using the Browse Remember me on this computer. Synthetic curve [Ctrl-T] replaces the field sounding curve at the current sounding point with the theoretical curve for the model with current properties.
Geographically located at coordinates o06 ‘- ipj2win east longitude and 7o06 ‘- 8o02’ south latitude Location map shown in Fig. The schlumberger array was used to ensure deep penetration and for logistics of limited man power in the field .
For each measurement only the current electrodes are moved keeping the potential electrodes at the same locations. Restart your computer when the installation is finished. Study ,anual groundwater geology is much useful for all the activities of human life.
The command line must be as follows:. The change is likely due to changes in the geological layers in the area. Log In Sign Up. With the advent of powerful and high speed computers, efficient techniques for groundwater exploration and management have evolved, of which remote sensing and GIS are of great significance Chowdhury et al. Print curves [Ctrl-P] prints the curve currently displayed and the table of the cross-sections parameters for the corresponding sounding point.
Profile inversion [Ctrl-F3] implements the automated interpretation for all sounding curves of the currently opened profile using current model parameters for each point as the initial model.
IPI2win – 1D interpretation of VES profile.
More User Manual 1. Table 1 is number of location measurement point No Village name District Elev. The Study Area Study area is located in the city of Malang.