Institut za rudarstvo i metalurgiju Bor

of slope disturbed during construction works
related to the small residential buildings. Stability
is retained as the terrain balance is adjusted
in terms of cutting and filling.
Terrain, subjected to flooding of agricultural
land is a plateau that is 83.0 m
above sea level. The peak elevation of
water is 83.30 m above sea level, that
means the frequent flooding, and the peak
elevation of century water is 85.0 m above
sea level. Then, the entire prospected area
is flooded, all of the Brcko port.
Hydrogeological characteristics of the
terrain, according to the hydrogeological
properties of sediments are changed
B - 5 (80.43)
1
1.4
2.0
8.0
3.5
B - 4 (83.06)
0.7
2.0
2.2
7.25
5.5
11.65
12.0
12.0 (3+6+7)
12.45 (11+12+17)
depending on fluctuations in the level of
the river Sava, especially in the area that is
subjected to the constant flooding at the
level of water level fluctuations. When the
water level is higher, sediments are completely
soaked and soft, and dragging of the
river, due to the increased levels of daily
temperature, leads to dryness and formation
of cracks of irregular shape, varying in
depth. With the re-growth of levels, sediments
are saturated with water and constantly
change the structure by washing the
smallest particles. Therefore, their geomechanical
characteristics become worse
and unfavorable for technical operations.
No 1, 2010. 22
MINING ENGINEERING
1
3
4
B - 3 (83.45)
1.12
2.35
5.0
1.0
6.5
7.5
8.0
Figure 2. Geological cross-profile 3-3 '
1. dike, 3. dusty sandy clay,
4. dust clayey muddy