GEOLOGICAL AND HYDROGEOLOGICAL STUDY IN CIKALONG WETAN, WEST BANDUNG REGENCY
The research area is located in Cikalong Wetan. The area of research area is 26.3 km2. The research area has the potential to have pollution problems caused by the Cikalong Cattle Farm and the potential of groundwater level decline by the highspeed rail project. This study aims to determine the g...
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Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/69700 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | The research area is located in Cikalong Wetan. The area of research area is 26.3
km2. The research area has the potential to have pollution problems caused by the
Cikalong Cattle Farm and the potential of groundwater level decline by the highspeed
rail project. This study aims to determine the geological setting and
hydrogeological conditions. The method used in this research is geological
observation and analysis, observation and analysis of hydrogeological conditions.
The geomorphology of the research area is divided into three geomorphological
units based on the Cileuleuy Lava Ridge Unit, the Pasir Angsana Hills Unit, and the
Cisaukeun Denudasional Valley Unit. The stratigraphy of the study area consists of
four unofficial units of Middle Miocene – Late Pleistocene age, namely the
Sandstone Unit, Claystone Unit, Andesite Lava Unit, and Tuf Unit. The geological
structures that developed in the research area are the Cigeblig Right Slip Fault, the
Cisaukeun Normal Right Slip Fault, and the Rende Normal Left Slip Fault.
The typology of the aquifer consists of the typology of volcanic deposits and the
typology of the folded sedimentary aquifer system. The types of springs found in the
study area are fracture and depression types. The hydrodynamic relationship
between water flow in aquifers and rivers is the dominant effluent. The hydrogeology
of the research area is divided into three independent aquifer units, namely
Sandstone Aquifer, Claystone Aquifer, Andesite Aquifer, and Tuf Aquifer. Based on
the pH parameter, groundwater that does not comply the drinking water quality
standards is generally located in the western part of the study area, close to the
Cirata Lake. The groundwater quality of the study area is suitable for irrigation
purposes based on the analysis of Na%, Sodium Adsorption Ratio (SAR), Residual
Sodium Carbonate (RSC), Wilcox diagram, and United States Salinity (USSL)
diagram. Regarding the existence of a tunnel project in the research area, the
condition of the groundwater level around the tunnel area has decreased.
Meanwhile, regarding the existence of cattle farming, the condition of the quality of
groundwater and river water around the location is still within the drinking water
quality standard. |
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