Penentuan Arah Pergerakan Lindi Dengan Metode Geolistrik Pada Tempat Pembuangan Akhir (TPA) Sampah Daerah Maiwa, Kecamatan Maiwa, Kabupaten Enrekang, Sulawesi Selatan
DOI:
https://doi.org/10.33536/jg.v10i03.1540Keywords:
Garbage, groundwater, leachate, rocks, environmentAbstract
In urban solid waste management, one of the main parameters is the problem of liquid waste (leachate). This liquid waste can result in a decrease in the carrying capacity of the environment due to the entry of this liquid waste into underground water and surface water. The composition of liquid waste varies depending on the type of source of waste formation. In general, this liquid waste contains dissolved and undissolved bacteria. The study site is composed of clastic sedimentary rocks in the form of sandstones and conglomerates,\ which are included in the Miocene Pliocene Sand (Tmps) tertiary rock formations and the Miocene Conglomerate Tertiary (Tmc). The results of previous studies found that the area where the Waste Landfill is located on coarse to fine-grained rocks, which is very likely that the flow of leachate contained in the Waste landfill location will affect the quality of the water system around the waste landfill location. From the results of this study, it can be known the direction of leachate flow by the geoelectric method and its impact on groundwater around the landfill.
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