Determination of Depth Groundwater Levels Based on Geophysical with Geoelectric Method Around the Prambanan Temple Region Yogyakarta Province
| Main Authors: | Agus, Santoso, Sismanto, ., Ari, Setiawan, Subagyo, . |
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| Format: | Proceeding PeerReviewed application/pdf |
| Bahasa: | eng |
| Terbitan: |
, 2013
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| Subjects: | |
| Online Access: |
https://repository.ugm.ac.id/96941/1/2.pdf https://repository.ugm.ac.id/96941/ |
Daftar Isi:
- Geoelectric is one geophysical method that aims to identii)' formations that are cond ucive in the ea rth, The pu rpose of this stud y is to describe geology configurations ben eath the surface resistivity is lower in areas con taining groun dwater pOtential is estimated. At Schlum berger resistivity meth ods in electrical current injected into the ea rth through the cu rrent electrodes, then the pOtential difference that arises in measuring via two electrode pOtential. f rom these measurements for di fferent electrode spacing will then be obtained resistivity variations in rates of each layer below the measu ring pOint. The goal is to obtain information about the depth and thickness of rock layers vertically resistivity rates, in order to get a complete picture of the geology below the surf.tce. The di fference in resistivity will be evident in th e depth determination of rock layers that have different types of resistivity.