Exploration of ilmenite potential in and around Kalu and Benthara river mouths with special reference to the variation of TiO2 content along a selected strech of Kalu Ganga

dc.contributor.authorKumara, HANHM
dc.contributor.authorMedagoda, CJ
dc.contributor.authorSivakala, S
dc.contributor.authorSugaraj, K
dc.contributor.authorWickrama, MADMG
dc.contributor.authorVijitha, AVP
dc.contributor.authorDissanayake, DMDOK
dc.contributor.authorRathnayake, NP
dc.contributor.editorKarunaratne, S
dc.contributor.editorDissanayake, DMDOK
dc.contributor.editorRatnayake, N
dc.contributor.editorChaminda, SP
dc.date.accessioned2022-06-22T03:22:25Z
dc.date.available2022-06-22T03:22:25Z
dc.date.issued2006-10
dc.description.abstractAlthough Ilmanite, Rutil, Zircon and Monazite occurs in beach sand of Sri Lanka, the sufficiently concentrated deposits for economic exploitation have been only identified yet in and around Pulmoddai, Baruwala and Kudremalai beaches. Of these, Pulmoddai is the largest beach sand deposit ever found in Sri Lanka, which is estimated to contain nearly, 4,000,000 tons of raw sand. However it has been noticed that beach mineral sand occurrence in many other parts of the country and detail investigation has not been carried out yet in those areas. Exploitation has been carried out only in Pulmoddai which is located near the rebels control areas. Since 1998 with production coming to a stand still, the Pulmoddai plant which a government own company is confined to selling its existing stockpile with Zircon and Rutile being bagged and transported to Colombo and exported. Therefore finding an alternative source to supply the demand of the export market to earn foreign exchange is a prior necessity of the country. Therefore this study was carried out to identify ilmenite potential in and around Kalu and Benthara river mouths and investigation has been carried out to identify the variation of Ti02 content in ilmenite along the Kalu Ganga track by sand sediment analysis. Gravity and the magnetic separation processes were employed for the processing of the sand samples. Results show that the particle size of Ilmenite in both river mouths deposits were reported in the range of+ l25J.lIl1to +250~tm sizeand this may mainly depend on grain size, flow velocity of the river, distance travel as well as energy of the sea waves. Variation of the titanium content in ilmenite along the Kalu Ganga can be concluded may due to the replacement of Fe in Ilmenite with another foreign element available in the river.en_US
dc.identifier.citationKumara, H.A.N.H.M., Medagoda, C.J., Sivakala, S., Sugaraj, K., Wickrama, M.A.D.M.G., Vijitha, A.V.P., Dissanayake, D.M.D.O.K., & Rathnayake, N.P. (2006). Exploration of ilmenite potential in and around Kalu and Benthara river mouths with special reference to the variation of TiO2 content along a selected strech of Kalu Ganga. In S. Karunaratne, D.M.D.O.K. Dissanayake, N. Ratnayake, & S.P. Chaminda (Eds.), Proceedings of 1st Annual Conference on Mining for Sustainable Development – A Multidisciplinary Approach (pp. 39-44). Department of Earth Resources Engineering, University of Moratuwaen_US
dc.identifier.conference1st Annual Conference on Mining for Sustainable Development - A Multidisciplinary Approachen_US
dc.identifier.departmentDepartment of Earth Resources Engineeringen_US
dc.identifier.emailvijitha@earth.mrt.ac.lken_US
dc.identifier.facultyEngineeringen_US
dc.identifier.pgnospp. 39-44en_US
dc.identifier.placeKatubeddaen_US
dc.identifier.proceedingProceedings of 1st Annual Conference on Minning for Sustainable Developmenten_US
dc.identifier.urihttp://dl.lib.uom.lk/handle/123/18327
dc.identifier.year2006en_US
dc.language.isoenen_US
dc.publisherDepartment of Earth Resources Engineeringen_US
dc.subjectFusionen_US
dc.subjectIlmeniteen_US
dc.subjectMagnetic separationen_US
dc.subjectTitaniumen_US
dc.titleExploration of ilmenite potential in and around Kalu and Benthara river mouths with special reference to the variation of TiO2 content along a selected strech of Kalu Gangaen_US
dc.typeConference-Full-texten_US

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