TY - JOUR
T1 - Geochemical exploration for prospecting new rare earth elements (REEs) sources
T2 - REE potential in lake sediments around Eppawala Phosphate Deposit, Sri Lanka
AU - Dushyantha, Nimila
AU - Ratnayake, Nalin
AU - Premasiri, Ranjith
AU - Batapola, Nadeera
AU - Panagoda, Hemalal
AU - Jayawardena, Chulantha
AU - Chandrajith, Rohana
AU - Ilankoon, I.M.Saman K.
AU - Rohitha, Sudath
AU - Ratnayake, Amila Sandaruwan
AU - Abeysinghe, Bandara
AU - Dissanayake, Kithsiri
AU - Dilshara, Pubudi
N1 - Funding Information:
The authors wish to acknowledge the financial support provided by the Accelerating Higher Education and Development (AHEAD) Operation of the Ministry of Higher Education of Sri Lanka funded by the World Bank , USA (AHEAD/DOR/6026-LK/8743-LK) and the University of Moratuwa (SRC/CAP/15/02) for this study. The authors are thankful to Sandun Udayanga, Ranjani Amarasinghe, Pathmika Priyadarshana and Pamudi Mishara for the field assistance.
Publisher Copyright:
© 2022 Elsevier Ltd
PY - 2023/3
Y1 - 2023/3
N2 - Rare earth elements (REEs) are globally considered as critical elements due to their indispensable applications in various high-tech industries. With the ever-increasing demand, identified primary REE resources will not be able to fulfil the global requirements and thus exploration and exploitation of secondary REE deposits are essential. This work is designed to prospect REE potential in lake sediments in the proximity of the Eppawala Phosphate Deposit (EPD) in Sri Lanka. In this context, surface and core sediment samples were collected from 2 upstream lakes and one downstream lake (connected to a man-made water canal, namely Jaya-Ganga) with respect to the EPD. In the downstream, the average total rare earth element (TREE), light REE (LREE) and heavy REE (HREE) concentrations of the surface sediments were 1011.3, 904.6 and 66.6 mg/kg, respectively. The corresponding average values in downstream core sediments were 858.7, 719.3 and 100.2 mg/kg, respectively. The results suggested that the downstream lake sediments contained a high TREE content with a significant LREE enrichment compared to the upstream lake sediments. The EPD was identified as the main REE source and Jaya-Ganga, which flows across the EPD, was the main transport medium in this study. Phosphate-bearing minerals, such as fluorapatite and hydroxylapatite, derived from the EPD act as the REE carriers where REEs substitute isomorphous in the mineral lattice. Since REE grade is relatively high compared to some of the reported secondary REE sources, the downstream lake sediments could be a potential secondary source for REEs for future exploitation.
AB - Rare earth elements (REEs) are globally considered as critical elements due to their indispensable applications in various high-tech industries. With the ever-increasing demand, identified primary REE resources will not be able to fulfil the global requirements and thus exploration and exploitation of secondary REE deposits are essential. This work is designed to prospect REE potential in lake sediments in the proximity of the Eppawala Phosphate Deposit (EPD) in Sri Lanka. In this context, surface and core sediment samples were collected from 2 upstream lakes and one downstream lake (connected to a man-made water canal, namely Jaya-Ganga) with respect to the EPD. In the downstream, the average total rare earth element (TREE), light REE (LREE) and heavy REE (HREE) concentrations of the surface sediments were 1011.3, 904.6 and 66.6 mg/kg, respectively. The corresponding average values in downstream core sediments were 858.7, 719.3 and 100.2 mg/kg, respectively. The results suggested that the downstream lake sediments contained a high TREE content with a significant LREE enrichment compared to the upstream lake sediments. The EPD was identified as the main REE source and Jaya-Ganga, which flows across the EPD, was the main transport medium in this study. Phosphate-bearing minerals, such as fluorapatite and hydroxylapatite, derived from the EPD act as the REE carriers where REEs substitute isomorphous in the mineral lattice. Since REE grade is relatively high compared to some of the reported secondary REE sources, the downstream lake sediments could be a potential secondary source for REEs for future exploitation.
KW - Eppawala phosphate deposit
KW - Lake sediments
KW - Rare earth elements (REEs)
KW - REE exploration
KW - Secondary rare earth resources
UR - http://www.scopus.com/inward/record.url?scp=85144841441&partnerID=8YFLogxK
U2 - 10.1016/j.jseaes.2022.105515
DO - 10.1016/j.jseaes.2022.105515
M3 - Article
AN - SCOPUS:85144841441
VL - 243
JO - Journal of Asian Earth Sciences
JF - Journal of Asian Earth Sciences
SN - 1367-9120
M1 - 105515
ER -