WATER TABLE INVESTIGATION AT WEST AND EAST PARK OF ITB GANESHA CAMPUS USING TIME DOMAIN ELECTROMAGNETIC METHOD (TDEM)
Groundwater constitutes a significant component of the Earth's hydrological cycle, serving as a vital source of potable water for humans. It plays a role in contributing to the flow of surface streams that ultimately discharge into the seas within the hydrological cycle. An aquifer represent...
Saved in:
Main Author: | |
---|---|
Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/78086 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | Groundwater constitutes a significant component of the Earth's hydrological cycle,
serving as a vital source of potable water for humans. It plays a role in contributing
to the flow of surface streams that ultimately discharge into the seas within the
hydrological cycle. An aquifer represents a portion of groundwater characterized
by its ability to transmit water due to its permeable geological formations. The Time
Domain Electromagnetic (TDEM) method is among the geophysical investigation
techniques employed to leverage electromagnetic field induction within subsurface
media containing groundwater. This method is particularly well-suited for mapping
groundwater levels as it can generate resistivity-depth structures that correlate with
the Earth's surface geological conditions. In this final project, data measurements
will be conducted using the WTEM-3Q, which is a central loop TDEM instrument,
within the ITB Ganesha campus in West and East Park. Data processing will utilize
ZONDTEM1D software to create a 1D model of subsurface layers. Analysis of the
data from the five measurement points reveals the presence of three distinct rock
layers, with groundwater depths ranging between 14 – 16 meters below the surface. |
---|