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Institution University of Zambia Remove constraint Institution: University of Zambia Faculty / School Mines Remove constraint Faculty / School: Mines Year 2013 Remove constraint Year: 2013 Start Over

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Witika, Lordwell Kampamba
2013·University of Zambia

A study has been made of the electrochemical behaviour of carrollite and chalcopyrite in the presence of xanthate and cyanide in aqueous solution. The investigations involved measurements of rest potentials and cyclic voltammetry of the sulphide minerals understudy. The results showed that the...

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Mbewe, Solomon
2013·University of Zambia

The study was aimed at contributing to the provision of good quality groundwater supply in Petauke District. It comprised collection and analysis of 50 groundwater samples from boreholes in the dry and wet season in Petauke Town. Water exit points were sterilised before collection of samples....

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Banda, Sraj Umar
2013·University of Zambia

Rock slope stability is a very important research area for many geo-engineers concerned with civil or mining works. Slope stability of pits, roads, tailings dams and other embankments is very cardinal as it directly impacts on the working or utilisation of these facilities. The Nchanga Open Pit...

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Musuku, Benjamin
2013·University of Zambia

The Nchanga and Konkola ores have substantial amounts of cobalt in the form of Carrollite (CUC02S4) and Cobaltiferous pyrite ((Co,Fe),S2). These minerals are found in association with copper minerals such as chalcopyrite (CuFeSz), Bomite (CusFeS4) and Chalcocite (CujS). However, the recoveries of...

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Phiri, Kakusa Wilson
2013·University of Zambia

Evapotranspiration (ET) is a dominant hydrologic flux in the water budget of semi-arid areas.Thus, accurate estimation of its dynamics in such environments is critical for improvingN water resources management. In this study the physically-based Surface Energy Balance System (SEBS) model was...

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Kalaka, Nashel
2013·University of Zambia

The objective of this research was to characterise the rockmass to determine appropriate support system for the decline with the 4.5m height and 4m wide in highly aquifer strata, recharging the water flow of 18, 000 cubic meters per day. As a result production targets reduced due to excessive...

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Katongo, Crispin
2013·University of Zambia

In the Chisamba area, some lithologies hitherto mapped as quartzites and dolomitic marbles are quartz mylonites and interbanded calc-silicate, marble and amphibolites, respectively. Both meso-and microstructural fabrics in the Chisamba area indicate that deformation associated with shearing was...

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Mulela, Davison
2013·University of Zambia

The syenites and quartz feldspar porphyries of the Mumbwa district occur as satellite bodies at the north east margin of the Hook Granite Massif, a large batholith dated 456 Ma, and intrude the pre-Cambrian Katanga metasediments. The composition of syenitic rocks varies from hornblende biotite...

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