Ariqah Ardelia, D. Pujiastuti, Ahmad Fauzi Pohan
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摘要

采用电感耦合等离子体-原子发射光谱法(ICP-AES)测定元素Ca、Li和B的浓度,用滴定法测定元素Cl的浓度,用可见光谱法测定sio2化合物的浓度。根据研究结果,丹戎拉雅和帕鲁普的地热流体经历了轻微的稀释,并且位于远离地热源的地方。丹戎拉雅和帕鲁普的温泉处于未成熟水带,表明地热流体未达到平衡,与地表水混合较多。使用硅地热计方程获得的地热储层估计温度为164.153⁰C - 175.209⁰C,可归类为中温地热系统。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Identifikasi Karakteristik Fluida dan Estimasi Temperatur Reservoir Panas Bumi di Tanjung Raya dan Palupuh, Kabupaten Agam
concentrations of elements Ca, Li, and B were tested using Inductively Coupled Plasma – Atomic Emission Spectroscopy (ICP-AES), the concentration of Cl elements was tested using the titration method and the concentration of SiO 2 compounds tested using Visible Spectroscopy . Based on the research results, the geothermal fluids in Tanjung Raya and Palupuh have experienced a slight dilution and are located far from geothermal sources. The hot springs in Tanjung Raya and Palupuh are in the immature water zone which indicates the geothermal fluid does not reach equilibrium and there is a lot of mixing with surface water. The estimated temperature of the geothermal reservoir obtained using the silica geothermometer equation has a temperature of 164.153⁰C – 175.209⁰C, which can be categorized as a medium-temperature geothermal system.
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