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Drilling Activity in the Mataloko Geothermal Field Ngada-NTT, Flores Indonesia

Sitorus K, Nanlohy F and Simanjuntak J

Key words
Mataloko, Drilling history, Alteration, P-T logging and Flow-Test
Location
Mataloko, Indonesia; Flores
Conference
Indonesian Geothermal Association Conference
Year
2001
Session
Earth Sciences
Language
English
Paper number
2001-08

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Abstract

Drilling activity of MT-2 was completed with setting 4î perforated casing to a depth of 180 m (TD = 180.02 m) on 3 February 2001. The first run of P-T logging tool to a depth of 104 m on 8 January 2001 showed down-hole temperature of 75.8?C. The second run recorded temperature of 78.1?C, then became 112?C and 130.4?C during the tool stayed for 2 hours and another 1? hours at the bottom. A flow test with Lip Pressure Method was successfully done to MT-2 on 22-27 January 2001. Steam flow rates on 3î flow line varied between 10.87 ñ 10.98 ton/hour at WHP of 7.9 Kscg. At WHP of 5.9 ñ 6.0 Kscg, steam flow rate ranged from 14.48 ñ 14.71 ton/hour and a flow line temperature of 135 ñ 140?C. Using 4î flow line, steam flow rate was about 14.29 ñ 16.34 ton/hour at WHP of 3.1 ñ 3.9 Kscg with a range temperature of 128 ñ 133?C. A maximum WHP of 14.0 Kscg was recorded while MT-2 shut-in on 17 - 18 January 2001. Chemical analyisis (WESTJEC) during the flow test showed a very low of gas content in the saturated steam (NCG = 0.261 ñ 0.291 vol% or 0.612 ñ 0.692 Wt%, CO2 in NCG = 90.81 ñ 90.99 vol%, H2S in NCG = 6.33 ñ 6.59 vol% and residual gas in NCG = 2.61 ñ 2.68 vol%). Subsurface lithology of MT-1 consists of tuff breccia, pyroxene andesite, hornblende andesite with minor layers of tuff. All rocks have been altered into argillic type. Alteration intensity (SM/TM) varies between 30 ñ 90% and contain about 2 ñ 60% swelling clay. The lithology of MT-2 is nearly the same as the MT-1 well.

Copyright 2001, Indonesian Geothermal Association. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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