D. A. Malikov
Russian Academy of Sciences
Network
Latest external collaboration on country level. Dive into details by clicking on the dots.
Publication
Featured researches published by D. A. Malikov.
Radiochemistry | 2010
Yu. M. Kulyako; T. I. Trofimov; D. A. Malikov; S. A. Perevalov; M. D. Samsonov; S. E. Vinokurov; A. Yu. Shadrin; B. F. Myasoedov
Dissolution of UO2, U3O8, and solid solutions of actinides in UO2, including those containing Cs, Sr, and Tc, in weakly acidic (pH 0.9–1.4) aqueous solutions of Fe(III) nitrate or chloride was studied. Complete dissolution of the oxides is attained at a molar ratio of Fe(III) nitrate or chloride to uranium of 1.6 or 2.0, respectively. In the process, actinides pass into the solution in the form of U(VI), Np(V), Pu(III), and Am(III). At 60°C, actinide oxides dissolve in these media faster than at room temperature. In the solutions obtained, U(VI) and Pu(III) are stable both at room temperature and at elevated temperatures (60°C), and also at high U concentrations (up to 300 mg ml−1) typical of process solutions (6–8 M HNO3, ∼60–80°C). After the oxide fuel dissolution, U and Pu are recovered from the solution by peroxide precipitation. In so doing, the content of Fe, Tc, Cs, and Sr in the precipitate does not exceed ∼0.05 wt %. From the solution after the U and Pu separation, the fission lanthanides, Tc, Cs, and Sr can be recovered by precipitation of Fe hydroxides in the presence of ferrocyanide ions and can be immobilized in appropriate matrices suitable for long-term and environmentally safe storage.
Radiochemistry | 2006
M. V. Mironenko; D. A. Malikov; Yu. M. Kulyako; B. F. Myasoedov
AbstractThe Np(V) distribution coefficients between montmorillonite and solutions of MgCl2 and CaCl2 were determined experimentally. The Np sorption decreases with increasing concentration of the supporting electrolyte. The sorption is very fast within the first several hours after the start of the experiment and then decelerates, reaching the equilibrium in approximately two weeks. The constants of binary ion exchange NpO2+-Mg2+ and NpO2+-Ca2+ on montmorillonite determined by fitting the experimental results are
Radiochemistry | 2006
M. V. Mironenko; D. A. Malikov; Yu. M. Kulyako; B. F. Myasoedov
Radiochemistry | 2011
Yu. M. Kulyako; S. A. Perevalov; T. I. Trofimov; D. A. Malikov; M. D. Samsonov; S. E. Vinokurov; B. F. Myasoedov
\log K_{NpO_2^ + - Mg^{2 + } } = 0.083 \pm 0.03
Radiochemistry | 2015
M. D. Samsonov; T. I. Trofimov; Yu. M. Kulyako; S. E. Vinokurov; D. A. Malikov; G. Sh. Batorshin; B. F. Myasoedov
Radiochemistry | 2013
Yu. M. Kulyako; S. A. Perevalov; T. I. Trofimov; D. A. Malikov; M. D. Samsonov; S. E. Vinokurov; B. F. Myasoedov; A. Yu. Shadrin
and
Radiochemistry | 2012
E. A. Zakharchenko; D. A. Malikov; G. V. Myasoedova; O. B. Mokhodoeva; N. P. Molochnikova; Yu. M. Kulyako
Radiochemistry | 2010
Yu. M. Kulyako; S. A. Perevalov; D. A. Malikov; S. E. Vinokurov; B. F. Myasoedov
\log K_{NpO_2^ + - Ca^{2 + } } = 0.106 \pm 0.014
Radiochemistry | 2014
Yu. M. Kulyako; S. A. Perevalov; T. I. Trofimov; M. D. Samsonov; S. E. Vinokurov; D. A. Malikov; B. F. Myasoedov
Russian Journal of General Chemistry | 2011
O. B. Mokhodoeva; D. A. Malikov; N. P. Molochnikova; E. A. Zakharchenko; S. A. Perevalov; G. V. Myasoedova; Yu. M. Kulyako; A. G. Tkachev; S. V. Mischenko; B. F. Myasoedov
.