Identifikasi Kedalaman Muka Air Tanah dan Posisi Akuifer di Kabupaten Tolikara
DOI:
https://doi.org/10.58169/jusit.v2i2.494Keywords:
Geology, geomorphology, aquifer, morphology, geophysics, resistivityAbstract
Groundwater is dynamic and influenced by a number of natural factors. Geology and geomorphology greatly determine the condition of the soil in an area. The geological structure influences the direction of groundwater movement, the type and thickness of the aquifer. The Karubaga District in Tolikara Regency is an area with a morphology of mountains, hills and valleys so it has the potential for rivers and streams that can be used as a source of raw water. Identification of the depth of the groundwater level in the Karubaga District is carried out using tools in the form of the AIDU Golden Rod (AGR), which is a special geophysical study instrument that provides a detailed vertical picture 300 m into the ground surface to read the resistivity values of rocks and aquifers by measuring the natural electric field
References
Aidu. (2020). Operation manual, electrical method and MT using AIDU Golden Road (AGR).
Kementrian PUPR. (2017). Modul geologi dan hidrogeologi.
Kementrian PUPR. (2019). Modul 4 eksplorasi geofisika untuk air tanah.
Kementrian PUPR. (2019). Modul 6 analisis dan interpretasi data geolistrik untuk air tanah.
Kodoati, R. J. (1996). Pengantar hidrogeologi. Yogyakarta: Penerbit Andi.
Kruseman, G. P., & de Ridder, N. A. (1970). Analysis and evaluation of pumping test data. International Institute for Land Reclamation and Improvement, Wageningen.
Linsley, R. K. (1985). Hidrologi untuk insinyur (Edisi Ketiga). Jakarta: Erlangga.
Milsom, J. (2003). Field geophysics (3rd ed.). England: John Wiley & Sons Ltd.
Purnama, S. (2010). Hidrologi air tanah. Yogyakarta: Kanisius.
Reynolds, J. M. (1997). An introduction to applied and environmental geophysics (p. 418). Chichester: John Wiley & Sons Ltd.
Santoso, D. (2002). Pengantar teknik geofisika. Bandung: Penerbit ITB.
