STUDY OF PRECIPITATION AND LAND-USE IMPACT ON GROUNDWATER - SURFACE WATER INTERACTION AND GROUNDWATER QUALITY IN THE CIKAPUNDUNG WATERSHED
The Cikapundung River is one of the important water resources for the city of Bandung and its surrounding areas. The Cikapundung River interacts with the surrounding groundwater system so that both affect each other, both in quantity and quality. Research on the interaction of groundwater and riv...
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Format: | Theses |
Language: | Indonesia |
Subjects: | |
Online Access: | https://digilib.itb.ac.id/gdl/view/87083 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | The Cikapundung River is one of the important water resources for the city of
Bandung and its surrounding areas. The Cikapundung River interacts with the
surrounding groundwater system so that both affect each other, both in quantity
and quality. Research on the interaction of groundwater and river water in the
Cikapundung watershed and the quality of groundwater influenced by seasonal
differences needs to be conducted, one of which can be a consideration for water
resources management and flood disaster control. The measurement results in the
short dry period, June - October 2023 showed that the transition zone from the
effluent flow to the influent flow moved ± 1.7 km to the north towards the position
of the research results in 2015. The measurement results in the short wet period,
November 2023 - March 2024 showed that the transition zone from the effluent flow
to the influent flow moved again by ± 1.2 km to the south towards its position in the
short dry period of 2023. The runoff coefficient of the Cikapundung watershed using
Cook's method was estimated at 70% where less than 30% of the precipitation is
infiltrated into the subsurface, where the boundary of the area with the extreme
runoff coefficient area is in the same area as the transition zone from effluent flow
to influent flow in 2024. In contrast to the results of several studies elsewhere, the
TDS concentration in groundwater is relatively higher in wet periods than in dry
periods. The acidity of groundwater is relatively more acidic in the wet period than
in the dry period. |
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