2011 - Europe Direct Iasi
2011 - Europe Direct Iasi
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 />
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