Pengaruh Konsentrasi Silika dan laju Aliran Uap terhadap Kecepatan Scaling Pada Model Pipa Panas Bumi

Scaling or deposition on the geothermal transmission pipes wall happen if the working steam which flow in it contents some minerals, like Silica and Carbonate. This research took steam as a model of geothermal fluid. The steam as fluid, be generated by a boiler. Three solution of silica be used, tho...

全面介紹

Saved in:
書目詳細資料
主要作者: Perpustakaan UGM, i-lib
格式: Article NonPeerReviewed
出版: [Yogyakarta] : Universitas Gadjah Mada 1999
主題:
在線閱讀:https://repository.ugm.ac.id/17838/
http://i-lib.ugm.ac.id/jurnal/download.php?dataId=606
標簽: 添加標簽
沒有標簽, 成為第一個標記此記錄!
機構: Universitas Gadjah Mada
實物特徵
總結:Scaling or deposition on the geothermal transmission pipes wall happen if the working steam which flow in it contents some minerals, like Silica and Carbonate. This research took steam as a model of geothermal fluid. The steam as fluid, be generated by a boiler. Three solution of silica be used, those were 57,1, 71,7 and 93,5 ppm. These concentrations based on the solubility of quartz at 133,5°C, and the working pressure i.e 2 atg, and three static pressure difference 0,4, 1,0 and 1,5 atg. The steam at certain condition was flowed in the specimen six hours. The scale thickness on the specimen wall had been measured by mean compared to the cuprum wire of 120 pm diameter. The deposition rates depend on the surface roughness, pressure differences, and minerals concentration in the solution and pH, can be approached by linear equations.