The impact of bacteria of circulating water on apatite-nepheline ore flotation.

A new phenomenon has been identified and studied-the impact of bacteria on the benefication process of non-sulphide ores using circulating water supply-a case study of apatite-nepheline ore. It is shown that bacteria deteriorate the floatability of apatite due to their interaction with active centres of calcium-containing minerals and intense flocculation, resulting in a decrease of the flotation process selectivity thus deteriorating the quality of concentrate. Based on the comparative analysis of primary sequences of 16S rRNA genes, there have been identified dominating bacteria species, recovered from the circulating water used at apatite-nepheline concentrating mills, and their phylogenetic position has been determined. All the bacteria were related to γ-Proteobacteria, including the Acinetobacter species, Pseudomonas alcaliphila, Ps. plecoglossicida, Stenotrophomonas rhizophila. A method of non-sulphide ores flotation has been developed with consideration of the bacterial factor. It consists in use of small concentrations of sodium hypochlorite, which inhibits the development of bacteria in the flotation of apatite-nepheline ores.

Restoration of properties of cultivated soils polluted by copper and nickel.

The long-term observations of the restoration of chemical and biological properties of cultivated podzol soil polluted by airborne emissions from a copper-nickel smelter located in the western Arctic of Russia were carried out. After 8 years, the total content of copper in soil decreased to a third (from 6230 to 2080 mg kg(-1)) and nickel to a sixth (from 3500 to 580 mg kg(-1)). Based on these observations, the removal time for heavy metals to reach permissible levels was calculated. The estimate was 100 years for copper and 108 years for nickel. Soil remained toxic to wheat seedlings, especially to their roots, for the whole observation period. A restoration of the number and activity of soil microorganisms was associated with the reduction in soil metal-toxicity. The number of non-sporeforming saprophytic bacteria was quickly restored concurrently with the removal of metals from the soil; fungal biomass also increased.

Fluorine in the soils of the White Sea Basin and bioindication of pollution.

Assessment of the pollution level of soils and vegetation by fluorine and heavy metals and also of the state of the soil microflora in the impact zone of Kandalaksha aluminium factory is discussed. The significant pollution of natural media by fluorine in the basin of the White Sea is established. Concentration of the total fluorine in the organogenic horizon of the Al-Fe-humus podzol soil at a distance of 20 km in the northern direction from the source of emission exceeds the background level by a factor of 3. In the epicentre of emission the amount of total fluorine in the soil exceeds the background level by a factor of 7-8 (Tolerable Amount: 4-5-fold). It is noted that the soil becomes more alkaline under the influence of fluorine and the increased content of chromium along the soil profile exceeds PC by a factor of 3 in the vicinity of the factory. The differences in the dimensions of bacterial and fungi biomass along the gradient of pollution were not revealed in the impact zone. But the changes in the taxonomic structure of fungi and in the level of their domination along the gradient of pollution were estimated. Floristic composition of the soil algae is represented mainly by unicellular green algae with Chlamydomonas elliptica and Bracteacoccus minor predominating.