INFLUENCE OF SAMPLING STRATEGY, LITHOLOGY, VEGETATION AND RAINFALL ONMETAL BACKGROUND CONCENTRATIONS IN SEDIMENT OF THE TROPICAL TUY RIVERBASIN, VENEZUELA
Jl. Mogollon et al., INFLUENCE OF SAMPLING STRATEGY, LITHOLOGY, VEGETATION AND RAINFALL ONMETAL BACKGROUND CONCENTRATIONS IN SEDIMENT OF THE TROPICAL TUY RIVERBASIN, VENEZUELA, Chemical geology, 121(1-4), 1995, pp. 263-272
The Tuy River basin, north-central Venezuela, was selected to study th
e influence of the sampling strategy and analytical methods, lithology
, rainfall and vegetation on the background concentrations of heavy me
tals in stream sediments. Stream bed sediment samples (105) were colle
cted during four years of the period 1979-1986 at 15 sites. The sedime
nts were air-dried at room temperature and sieved through a-120 mesh (
125 mu m) stainless-steel sieve. The concentrations of Fe, Mn, Co, Cu,
Cr, Ni, Pb, Zn and Cd were determined by atomic absorption spectromet
ry after digestion with a hot (80 degrees C) concentrated mixture of H
NO3, HClO4 and HF. The coefficient of variation (CV) due to analytical
methods was < 10%, while the CV among tributaries ranged from 13% to
45%. This allows the establishment of background values with a low num
ber of samples ( < 10). Tributaries with CV > 60% indicate contaminati
on or mineralized areas. The large difference in average concentration
among the tributaries (CV = 29-110%) allows distinction between areas
with different lithology and vegetation. The northern and southern ar
eas of the Tuy River basin exhibit felsic and mafic lithologies, respe
ctively. The southern area can be further divided in two subunits: the
southwestern with savanna vegetation and the southeastern characteriz
ed by tropical rainforest. The highest concentrations of metals were f
ound in the southern area (3 times the northern). Especially high valu
es were measured in the southeastern subunit and are likely due to the
metavolcanic and mafic bedrock lithologies, and the high weathering i
ntensities associated with this tropical forest area.