HYDROGEOLOGICAL STUDY IN JAYAGIRI VILLAGE AND SURROUNDINGS, LEMBANG DISTRICT, WEST BANDUNG REGENCY, WEST JAVA
The transition of land use in the northern region of Bandung into water infiltration areas makes groundwater a crucial topic. However, information regarding groundwater quality in the Lembang District is not evenly distributed. Therefore, research on geological and hydrogeological conditions is n...
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Format: | Final Project |
Language: | Indonesia |
Subjects: | |
Online Access: | https://digilib.itb.ac.id/gdl/view/82153 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | The transition of land use in the northern region of Bandung into water infiltration
areas makes groundwater a crucial topic. However, information regarding
groundwater quality in the Lembang District is not evenly distributed. Therefore,
research on geological and hydrogeological conditions is needed to ensure the
suitability of groundwater quality and its impact. The research area is located in
the Lembang District, covering the villages of Jayagiri, Cikahuripan, Cibogo,
Kayuambon, Sukajaya, and Gudangkahuripan, in Bandung Regency, West Java
Province. Research methods for the geological aspect involve understanding the
distribution of rocks, geomorphology, stratigraphy, geological structures, and
geological synthesis. As for the research method for the hydrogeological aspect, it
involves determining groundwater levels, hydrochemical facies, groundwater
chemical processes, physical-chemical parameters of groundwater, groundwater
quality, and infiltration rates.
The research area consists of three geomorphological units: Mount Putri Hills,
Volcanic Footplain, and Pyroclastic Flow Fan, and four rock units:
Undifferentiated Old Volcanic Unit, Pumiceous Tuff Unit, Lava Unit, and Tuff Sand
Unit. The hydrogeological system of the research area has volcanic deposit systems
containing unconfined aquifers divided into Undifferentiatied Old Volcanic
Aquifer, Pumiceous Tuff Aquifer, Lava Aquifer, and Tuff Sand Aquifer. Based on
TDS parameters, there is groundwater from 8 water sources that are below
standards, while based on pH parameters, there is groundwater from 3
groundwater sources that are below standards. As for the hydrochemical facies in
5 groundwater samples, they indicate calcium chloride type, magnesium
bicarbonate type, and mixed type.
Analysis of infiltration rates using mini disk infiltrometer in the research area
indicates a dominance of slightly slow until moderate infiltration rates. The fastest
infiltration rates are found in residential land use zones. |
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