Production Capacity Optimization By Silica Crust Analysis “TB-001” and “TB-002” Wells Sorik Marapi Geothermal Field
DOI:
https://doi.org/10.31315/jpgt.v6i1.13623Abstract
The Sorik Marapi located in Mandailing Natal Regency, North Sumatra. Silica scale production wells “TB-001” and “TB-002” makes pipe diameter smaller, inhibits fluid flow, reduces energy output, and increases cost of cleaning even replacing pipes. The research expected to produce efforts to prevent silica scale thus production capacity optimized. Method used is Silica Saturation Index (SSI) with amorphous and quartz silica types. Temperature and pressure are important where appropriate settings can minimize silica scale. Study focused on the wellhead and separator part of the well. Furthermore, comprehensive feasibility evaluation of production well was conducted. Cap rock smectite - hematite mineral about 20° - 240°C and reservoir illite - epidote mineral about 240° - 340°C. Geothermal fluid is dominated by chloride water. Both wells have the potential silica scale in separator with SSI >1 and not in wellhead with SSI<1. The treatment to prevent the silica scale is to use hydrofluoric acid (HF) solution with concentration of 15% and immersion time of 15 minutes, where the effectiveness value is about 46-47%.
Keywords: Geothermal; Production Wells; Silica Crust; Sorik Marapi; SSI
References
Azizi, H. (2020). Pola Aliran Termal Berdasarkan Analisis Fluida dan Mineral Ubahan Daerah Geotermal Sorik Marapi. Buletin Sumber Daya Geologi, 15(3), pp. 202-218
Barber, A. J., & Crow, M. J. (2005). Sumatra: Geology, Resources, and Tectonic Evolution. London: The Geological Society
Ciptadi, S., & Patangke, S. (2001). Evaluasi Potensi Silica Scaling Pipa Produksi Lapangan Lahendong Sulawesi Utara. Proceeding The 5th Inaga Annual Scientific Conference & Exhibitions
Dipippo, R. (2010). Simplified Method For Estimating Silica Scaling Potential in Geothermal Power Plants. Geothermal Resources Council Cambridge Bulletin
Fournier, R. O. (1985). The Behaviour of Silica In Hydrothermal Solutions. Economic Geology, 264(9), pp. 45-61
Giggenbach, W. F. (1988). Geotermal Solute Equlibria. Geochem Cosmochem Act, 51(12), pp. 2749-2765
Guilbert, G. M., & Park, C. F. (1986).The Geology Of Ore Deposits. New York: W.H.Freeman and Company
Hendri, R. (2021). Important Role of Wairakite at Sorik Marapi Geothermal Field. Proceedings The 2nd Digital Indonesia International Geothermal Convention (DIIGC)
Hidayatullah, M. S. (2021). Determination of Geothermal Reservoir Zone of Sorik Marapi, Mandailing Natal, North Sumatra. IAGI Journal, 1(1), pp. 13-24
Hochstein, M. P., & Browne, P. R. (2000). Surface Manifestations of Geothermal Systems With Volcanic Heat Sources. Volcanoes San Diego Academic Press, pp. 835-855
Jasmita, M., & Putra, A. (2020). Identifikasi Karakteristik Mata Air Geotermal Sibanggor Tonga Mandailing Natal Menggunakan Diagram Segitiga. Jurnal Fisika Unand, 9(4), pp. 428-435
Polimpung, P. W. (2021). Analisis Terjadinya Scaling Silica Pada Condenser dan Cooling Tower. Jurnal Fista: Fisika dan Terapannya, 2(1), pp. 38-42
Reyes, A. (2000). Petrology and Mineral Alteration In Hydrothermal System. New Zealand : Institute Of Geological And Nuclear Sciences. Lower Hutt
Rezky, Y., & Hermawan, D. (2015). Geothermal System of Sorik Marapi-Roburan-Sampuraga, North Sumatera, Indonesia. Proceedings World Geothermal Congress Melbourne Australia
Sagala, B. D. (2018). Conceptual Model of Sorik Marapi Geothermal System Based On 3-G Data Interpretation. Geoscience Department Sorik Marapi Geothermal Power
Sofyan, A. (2021). Analysis of SSI, Scale Formation Rate, and Scale Formation Time Based on Geothermal Production. Indonesian Journal of Petroleum and Mineral, 1(1), pp. 26-33
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 2025 Journal of Petroleum and Geothermal Technology

This work is licensed under a Creative Commons Attribution 4.0 International License.







