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2011 - Europe Direct Iasi

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EUROINVENT <strong>2011</strong><br />

environmental conditions; (ii) removes a number of<br />

disadvantages of current methods of industrial extraction<br />

of silver, mostly related to technology costs and pollution<br />

problems; (iii) the separation yields of silver are supperior<br />

in comparison with those obtained by currently applied<br />

processes to industrial scale; (iv) flexibility and<br />

adaptability to the type of material that is extracted silver.<br />

In addition the method can be adapted for the separation of<br />

other metals from mine wastes and alluvial deposits. The<br />

method described in the invention includes<br />

methodological details for each stage of work and the<br />

limits of applicability in relation to the source materials<br />

for silver.<br />

Financial support for the studies was provided by the<br />

Ministry of Education and Research from Romania,<br />

ANCS – CNMP, grants PNCDI II no. 52-141 / 2008.<br />

R.31.<br />

Title “Feedback” method for estimating the paleomediu conditions<br />

Authors Brânzilă Mihai 1 , Bulgariu Dumitru 1,2 1, 2<br />

, Rusu Constantin<br />

1<br />

”Al. I. Cuza” University of <strong>Iasi</strong>, Faculty of Geography and<br />

Institution Geology, 2 Romanian Academy, Filial of <strong>Iasi</strong>, 3 Romanian<br />

Academy, Filial of <strong>Iasi</strong>, Collective of Geography<br />

The invention relates to a method for the estimation of<br />

conditions paleomediu based on the specific and selective<br />

evolution, in relation with the changes of environmental<br />

conditions, of mineral equilibriums and intre-phases<br />

distribution processe of some minor elements. The method<br />

allows the achievement of acceptable estimates for<br />

sedimentary deposits and for Quaternare and Neogene<br />

vulcanogen-sedimentary deposits in case of utilization as<br />

marker geochemical processes of the precipitation-<br />

Description<br />

dissolution-redeposition equilibriums of carbonates<br />

minerals, iron oxydes and oxy-hydroxides and silica gels.<br />

In principle, the method consists in the thermodynamic<br />

and kinetic interpretation of mineral processes sensible to<br />

the changes of environmental conditions, knowing the<br />

explicit thermodinamic and kinetic function which<br />

governing these processes and the chemical and<br />

mineralogical composition of marker minerals from<br />

different current geological formations, respectively. The<br />

estimations imprecision is determined by the accuracy<br />

Innovative Researches<br />

156

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