Claim Missing Document
Check
Articles

Found 3 Documents
Search

Metode Nuclear Magnetic Resonance Sounding (NMRS) Merupakan Teknik Baru dalam Eksplorasi Airtanah Nurdin, Muhammad; Sudarto, Slamet
EKSPLORIUM Vol. 32 No. 1 (2011): MEI 2011
Publisher : BRIN Publishing

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.17146/eksplorium.2011.32.1.2827

Abstract

NMRS method has been used in the past 10 years with success in various geological context and groundwater exploration. This method has indeed the ability of directly detecting the presence of water through the excitation of the hydrogen protons of water molecules. The frequency to which the H protons react depends on the magnitude of the Earth magnetic field, while the intensity of the excitation determines the depth of investigation. The amplitude of the magnetic field generated in return by the water of a layer is proportional to the porosity of this layer, and the time constant of the relaxation curve is linked to the mean pore size of the material, that is to say tightly related to its hydraulic permeability. A field cases such as illustrate NMRS application that is taken from measurement at Mauritania. NMRS measurement results in dry areas indicate the time-relaxation amplitude is low (10 A-ms) and water content is 1%. While the results of the aquifer region NMRS measurements showed -relaxation-time amplitude is quite large (270 A-ms) and water content is 12-30%.
Tinjauan Umum Potensi Sumberdaya Monasit di Daerah Ketapang Kalimantan Barat Soetopo, Bambang; Syaeful, Hery; Marzuki, Anang; Sudarto, Slamet
EKSPLORIUM Vol. 32 No. 2 (2011): NOVEMBER 2011
Publisher : BRIN Publishing

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.17146/eksplorium.2011.32.2.2818

Abstract

Monazite is one of the minerals that contain thorium and rare earth element (RE). Geologically at study area there are indications radioactive minerals that is monazite in alluvial sediments sourced from granitic rocks. The purpose of this study to obtain information of geological character, distribution and mining of mineral resource potential of radioactive materials and availability information area prospects containing monazite detailed in order to further follow-up exploration. The results in Pangkalan Telok Base Areas, Ketapang show that the geological rock unit consists of clay unit, Sangiyang granite unit, Sukadana granite unit, diorite unit, basalt unit and alluvial. Due process of weathering, transport and sedimentation, then the granitic rock, monazite minerals and zircon separated and deposited as alluvial directional spread North – South. This is reflected from the radioactivity measurements of heavy minerals, which ranged between 100 – 700 c/s and value of soil radiometric of 100 – 300 c/s. Radiometry values are included in the eastern part of which is predicted to originate from Sukadana granite. Patterns of distribution of soil radiometry, heavy mineral and content of U and Th have the relative direction of northwest – southeast, at area of 91,511,200 m2 has an average Th content of 1.97 to 46.98 ppm/gram.
Pelacakan Air Tanah di Desa Mbuit Kabupaten Manggarai Barat, Provinsi Nusa Tenggara Timur Suharji, Suharji; Nurdin, Muhammad; Karunianto, Adhika Junara; Sartapa, Sartapa; Sudarto, Slamet
EKSPLORIUM Vol. 34 No. 2 (2013): NOVEMBER 2013
Publisher : BRIN Publishing

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.17146/eksplorium.2013.34.2.2808

Abstract

West Manggarai Regency is a new regency as a result of regional development of Manggarai-Raya Regency. Based on information from the local mining service authorities dealing with groundwater, Mbuit village undergo clean water shortages in the dry season. One alternative to overcome the water shortages is the use of groundwater. The investigation of groundwater is intended to determine the characteristics of the geology, hydrogeology and characteristics of the electrical properties of the subsurface rocks which required to determine the potential rock layers that containing groundwater (aquifers). To achieve these objectives carried out the topography measurement, collecting data of geological/hydrogeology, and electrical resistivity measurement. Based on result of observations, analysis of the surface geological survey and supported by subsurface resistivity data in the investigation area, the potential aquifer is found. The aquifers potential has been found in a fractured aquifer system, in the northern of investigation region and distributed relatively west-east. The best aquifer is found in the line C at the point C15–C17, line G at the point G17–G18 (Humpung village), line D at the point D14–D17, line E at the point E14–E19 (Tureng village) with a resistivity value of 5–43 Wm and the depth of 50–120 meters.