INVESTIGASI AKUIFER DISEKITAR DAS (DAERAH ALIRAN SUNGAI) SIAK DI PEKANBARU MENGGUNAKAN METODE RESISTIVITAS KONFIGURASI WENNER DAN KONFIGURASI SCHLUMBERGER

dc.contributor.authorFiizumi, Nurun
dc.contributor.authorSyech, Riad
dc.contributor.authorSugianto
dc.date.accessioned2013-06-13T05:02:11Z
dc.date.available2013-06-13T05:02:11Z
dc.date.issued2013-06-13
dc.description.abstractA Research has been done to determine the aquifer and structure of lithology subsurface at Siak Bridge1, 2, and 3 Pekanbaru by using a geoelectric method in Wenner and Schlumberger electrode configurations. The current and voltage were obtained by using geoelectric equipment. These data were processed by excell to acquire the apparent resistivity. The software of Res2Dinv 3.56 and VES were used to analyze the data, which yield the real resistivity of rock and subsurface of lithology. The interpretations of Res2Dinv 3.56 and VES show that the lithology of Siak Bridge 1, 2, and 3 Pekanbaru consists of clay, sand, sand gravel, and hard core such as granite and limestone. The compressed aquifer was identified in Siak Bridge 1 and 3 where as Siak Bridge 2 was identified as free aquifer. The depth of aqiufer obtained by using Res2Dinv and VES differs each other in only 4 meters.en_US
dc.description.sponsorshipSyech, Riad, Sugiantoen_US
dc.identifier.otherRangga Dwijunanda Putra
dc.identifier.urihttp://repository.unri.ac.id:80/handle/123456789/3680
dc.language.isootheren_US
dc.subjectAquiferen_US
dc.subjectlithologyen_US
dc.subjectSchlumberger methoden_US
dc.subjectWenner methoden_US
dc.titleINVESTIGASI AKUIFER DISEKITAR DAS (DAERAH ALIRAN SUNGAI) SIAK DI PEKANBARU MENGGUNAKAN METODE RESISTIVITAS KONFIGURASI WENNER DAN KONFIGURASI SCHLUMBERGERen_US
dc.typeOtheren_US

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