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All Journal IJOG : Indonesian Journal on Geoscience Jurnal RISET Geologi dan Pertambangan Eksplorium : Buletin Pusat Pengembangan Bahan Galian Nuklir Jurnal Geomine Prosiding Temu Profesi Tahunan PERHAPI INDONESIAN MINING PROFESSIONALS JOURNAL INTAN Jurnal Penelitian Tambang Indonesian Journal of Physics (IJP)
Syafrizal Syafrizal
Institut Teknologi Bandung
Aerospace Engineering Astronomy Chemical Engineering, Chemistry & Bioengineering Civil Engineering, Building, Construction & Architecture Computer Science & IT Decision Sciences, Operations Research & Management Earth & Planetary Sciences Economics, Econometrics & Finance Electrical & Electronics Engineering Energy Engineering Social Sciences

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HYDROGEOCHEMICAL AND STABLE ISOTOPE ANALYSIS OF KEBAR HOT SPRINGS MANOKWARI DISTRICT, WEST PAPUA PROVINCE: ANALISIS HIDROGEOKIMIA DAN ISOTOP STABIL MATA AIR PANAS KEBAR KABUPATEN MANOKWARI PROVINSI PAPUA BARAT Andrew Karubaba; Irwan Iskandar; Syafrizal
INTAN Jurnal Penelitian Tambang Vol. 6 No. 2 (2023): INTAN Jurnal Penelitian Tambang
Publisher : Jurusan Teknik Pertambangan Program Studi S1 Teknik Pertambangan Fakultas Teknik Pertambangan dan Perminyakan Universitas Papua

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.56139/intan.v6i2.189

Abstract

In simple terms, geothermal classification is determined according to reservoir equilibrium, fluid type, and temperature. Based on the reservoir temperature, geothermal systems are separated into two different systems: dynamic system (convection) and static system (conduction). This system structure is also affected by topography which is further specified as a high-temperature fluid reservoir. The relationship between the characteristics of the hot springs and geothermal potential is instructive to be analyzed. The objective of the analysis is to determine critical parameters: The chemical composition of the water and the source of origin of the water. Hydrogeochemical studies including analysis of major element analysis; ratio stable isotopes δ18O and δ2H of samples from springs, rivers, and wells used to determine the character of hot springs. The primary element examination shows that the sample ions composition from the hot springs is dominated by three types of rock sources: shale; sandstone; and quartzite rocks. It also reveals that sample hot springs can be considered thermal water (based on the Piper Diagram), and classified as water and rock interactions dominant based on the Gibbs diagram.
Co-Authors Akmal Yahya Hidayat Andika Satria Pradana Andrew Karubaba Arie Naftali Hawu Hede Arif Arif Bagus E. B. Nurhandoko Budi Sulistyanto Cahyo Okta Ardian Endang Hartiningsih Fajril Ambia Heri Syaeful Hussein Rudiyanto Ichwan Azwardi Ichwan Azwardi Lubis Ichwan Azwardi Lubis IGB Eddy Sucipta Indriani Sukmana Irwan Iskandar Mirza Dian Rifaldi Mohamad Nur Heriawan Muhammad Anugrah Firdaus Periska Rasma Raymond Kosher Sianturi Raymond Kosher Sianturi Satyogroho Dian Amertho Satyogroho Dian Amertho Sudarto Notosiswoyo Syahrul Mubarok Teti Indriati Wirandika Mayzzani Hadiana Y. Wiyanto Yogi La Ode Prianata