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Rudarski radovi br 4 2011 - Institut za rudarstvo i metalurgiju Bor

Rudarski radovi br 4 2011 - Institut za rudarstvo i metalurgiju Bor

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Fig. 4. Field in the domain of clay deposit Dušanovac (left) and the view from the<<strong>br</strong> />

Hydroelectric Plant Iron Gate 2 (right)<<strong>br</strong> />

The clay deposit [3,5] was explored by<<strong>br</strong> />

trenches (totally 4 trenche, dimensions<<strong>br</strong> />

2×2.5×1 m) and geological prospecting<<strong>br</strong> />

drill holes. According to the vertical profile<<strong>br</strong> />

of all trenches, the ground surface to<<strong>br</strong> />

the depth of soil from 0.6 to 0.7 m was<<strong>br</strong> />

observed, and below that the yellow<<strong>br</strong> />

<strong>br</strong>own sandy clay with the appearance of<<strong>br</strong> />

carbonate. One sample was taken frfrom<<strong>br</strong> />

each trench for chemical testing.<<strong>br</strong> />

Sampling intervals [3] of cores from<<strong>br</strong> />

prospecting drill holes were 1 or 2 m. Total<<strong>br</strong> />

of 370 individual samples were taken,<<strong>br</strong> />

out of which 41 composite samples were<<strong>br</strong> />

formed. Composite samples were specially<<strong>br</strong> />

formed for the yellow clay class,<<strong>br</strong> />

specially for the gray class of clay quality.<<strong>br</strong> />

Studying the pillars of drill holes [3], it<<strong>br</strong> />

was observed that macroscopically,according<<strong>br</strong> />

to the color of clay<<strong>br</strong> />

deposit, four layers can be <strong>br</strong>oken<<strong>br</strong> />

down:<<strong>br</strong> />

► Brown clay lies immediately below<<strong>br</strong> />

the humus cover, which has the average<<strong>br</strong> />

thickness of about 0.7 m.<<strong>br</strong> />

Clay is poor to more sandy, the average<<strong>br</strong> />

thickness of this layer is<<strong>br</strong> />

about 1.5 m;<<strong>br</strong> />

► Yellow clay lies below <strong>br</strong>own clay,<<strong>br</strong> />

average thickness of about 13.0 m.<<strong>br</strong> />

This clay is greasy, very plastic and<<strong>br</strong> />

slightly sandy with occasional occurrence<<strong>br</strong> />

of FeO and MnO coating.<<strong>br</strong> />

A layer of yellow clay occurs<<strong>br</strong> />

throughout the deposit;<<strong>br</strong> />

► Brown-gray clay is spatially positioned<<strong>br</strong> />

below the yellow and above the<<strong>br</strong> />

gray clay above. A layer of <strong>br</strong>owngray<<strong>br</strong> />

clay represents a zone of mixing<<strong>br</strong> />

of yellow and gray clay and it is<<strong>br</strong> />

very sandy, and the average thickness<<strong>br</strong> />

of this layer is about 6.0 m.<<strong>br</strong> />

► Gray clay is the average thickness<<strong>br</strong> />

of about 35.5 m and it is located<<strong>br</strong> />

below the <strong>br</strong>own-gray clay. It is<<strong>br</strong> />

very sandy, and thin interlayers of<<strong>br</strong> />

a strong clay sand are very rarely<<strong>br</strong> />

observed in this thin layer. The fossil<<strong>br</strong> />

remains of shells also occur in<<strong>br</strong> />

this layer. A layer of gray clay with<<strong>br</strong> />

increasing of a depth gradually becomes<<strong>br</strong> />

very clay sand. A layer of<<strong>br</strong> />

gray clay was drilled by all drill<<strong>br</strong> />

holes.<<strong>br</strong> />

Physical-mechanical testing [4], grainsize<<strong>br</strong> />

distribution testing [6,7], laboratory<<strong>br</strong> />

technology and chemical testing were carried<<strong>br</strong> />

out from laboratory testing on taken<<strong>br</strong> />

samples. Technological tests in semi-industrial<<strong>br</strong> />

and industrial scale, were not done.<<strong>br</strong> />

No 4,<strong>2011</strong>. 25<<strong>br</strong> />

MINING ENGINEERING

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