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335 related items for PubMed ID: 22364181
21. Stable U(IV) complexes form at high-affinity mineral surface sites. Latta DE, Mishra B, Cook RE, Kemner KM, Boyanov MI. Environ Sci Technol; 2014; 48(3):1683-91. PubMed ID: 24404905 [Abstract] [Full Text] [Related]
27. Influence of dynamical conditions on the reduction of U(VI) at the magnetite-solution interface. Ilton ES, Boily JF, Buck EC, Skomurski FN, Rosso KM, Cahill CL, Bargar JR, Felmy AR. Environ Sci Technol; 2010 Jan 01; 44(1):170-6. PubMed ID: 20039748 [Abstract] [Full Text] [Related]
28. Effect of Ca2+ and Zn2+ on UO2 dissolution rates. Cerrato JM, Barrows CJ, Blue LY, Lezama-Pacheco JS, Bargar JR, Giammar DE. Environ Sci Technol; 2012 Mar 06; 46(5):2731-7. PubMed ID: 22304297 [Abstract] [Full Text] [Related]
32. Incorporation and retention of 99-Tc(IV) in magnetite under high pH conditions. Marshall TA, Morris K, Law GT, Mosselmans JF, Bots P, Parry SA, Shaw S. Environ Sci Technol; 2014 Oct 21; 48(20):11853-62. PubMed ID: 25236360 [Abstract] [Full Text] [Related]
39. Characterization of extracellular minerals produced during dissimilatory Fe(III) and U(VI) reduction at 100 degrees C by Pyrobaculum islandicum. Kashefi K, Moskowitz BM, Lovley DR. Geobiology; 2008 Mar 21; 6(2):147-54. PubMed ID: 18380877 [Abstract] [Full Text] [Related]