2018
DOI: 10.31227/osf.io/654n9
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Kajian Potensi Air Tanah Dengan Pengujian Geolistrik Di Desa Telonang Kabupaten Sumbawa Barat

Abstract: Ketersediaan air bersih yang mulai menipis ditambah dengan kondisi lahan atau wilayah yang mengalami kekeringan, maka dituntut untuk mencari suatu solusi dan salah satu solusi yang bisa direalisasikan adalah mencari sumber potensi air tanah untuk memenuhi kebutuhan air bersih masyarakat. Berdasarkan permasalahan akan kebutuhan air bersih yang terjadi di Kabupaten Sumbawa Barat, maka cukup layak diangkat suatu penelitian yang nantinya diharapkan bisa menjawab permasalahan masyarakat Kabupaten Sumbawa Barat aka… Show more

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“…Information on water availability is required to determine the potential planting period to reduce the risk of drought, especially during critical crop periods, so sugarcane production and yields increase. The identification of groundwater potential with the geoelectric method has been widely applied both by sounding and mapping because it's relatively simple, economical, and has various alternative imaging techniques associated with the presence of groundwater [11,12,13]. This study aims to identify the potential for groundwater to determine its distribution, volume, and depth and to determine the sugarcane planting period.…”
Section: Introductionmentioning
confidence: 99%
“…Information on water availability is required to determine the potential planting period to reduce the risk of drought, especially during critical crop periods, so sugarcane production and yields increase. The identification of groundwater potential with the geoelectric method has been widely applied both by sounding and mapping because it's relatively simple, economical, and has various alternative imaging techniques associated with the presence of groundwater [11,12,13]. This study aims to identify the potential for groundwater to determine its distribution, volume, and depth and to determine the sugarcane planting period.…”
Section: Introductionmentioning
confidence: 99%
“…keterangan: : resistivitas semu (Ωm) K : faktor geometri I : arus listrik (A) ΔV : beda potensial P 1 dan P 2 (V) (Reynolds, 1997) Banyak peneliti telah melaporkan keberhasilan metode geolistrik konfigurasi Schlumberger dalam mengidentifikasi kedalaman dan ketebalan akuifer di berbagai daerah (Budiman et al, 2013;Purwanugraha, 2015;Hanifah et al, 2016;Sehah & Aziz, 2016;Purnama & Noval, 2017;Wahyuni et al, 2018;Nugraha et al, 2018). Penelitian yang lebih spesifik tentang akuifer di daerah kampus juga telah dilakukan oleh Halik & Widodo (2008) dan Manrulu et al, (2018).…”
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