1995
DOI: 10.1016/0016-7061(94)00032-6
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Speciation of 238U, 226Ra, 210Pb, 228Ra, and stable Pb in the soil near an exhaust ventilating shaft of a uranium mine

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Cited by 31 publications
(14 citation statements)
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“…Plants take up U from the readily exchangeable and soluble fractions of the soil. However, according to previous work, negligible amount of U(VI) remain in the soluble and exchangeable forms over any significant time, thereby limiting the amount available for plant uptake and subsequent phytoremediation (Bunzl et al, 1995;Sheppard and Thibault, 1992). In addition, plant-associated microorganisms, including mycorrhizal fungi, may have significant effects on U uptake (Rufyikiri et al, 2002(Rufyikiri et al, , 2003(Rufyikiri et al, , 2004b.…”
Section: +mentioning
confidence: 98%
“…Plants take up U from the readily exchangeable and soluble fractions of the soil. However, according to previous work, negligible amount of U(VI) remain in the soluble and exchangeable forms over any significant time, thereby limiting the amount available for plant uptake and subsequent phytoremediation (Bunzl et al, 1995;Sheppard and Thibault, 1992). In addition, plant-associated microorganisms, including mycorrhizal fungi, may have significant effects on U uptake (Rufyikiri et al, 2002(Rufyikiri et al, , 2003(Rufyikiri et al, , 2004b.…”
Section: +mentioning
confidence: 98%
“…Between pH 4.0 and 7.5, the pH range of most soils, U(VI) exists primarily in hydrolyzed forms (Meinrath et al, 1996). Bunzl et al (1995) found that a significant portion of U contaminant in soils exposed to vented air from U ore mine shafts was incorporated into the clay lattice of the soils. The least amount of U was found in the exchangeable and soluble forms, thereby limiting the amount available for plant uptake and subsequent phytoremediation.…”
Section: Uranium Behavior In Soilsmentioning
confidence: 99%
“…Assim, para estimar um possível risco de exposição à radiação desses radionuclídeos no longo prazo, não somente a sua atividade total no solo mas também a sua partição geoquímica, a biodisponibilidade para os processos ecológicos e os fatores que estão influenciando nessa distribuição precisam ser conhecidos (Bunzl et al, 1995;Davis et al, 1999;Butler et al, 1999).…”
Section: Introductionunclassified
“…O 226 Ra é o isótopo mais importante de ocorrência na natureza, devido à sua meia-vida longa (1622 anos), associada à abundância do seu precursor ( 238 U) (Molinari & Snodgras, 1990). Procedimentos de extração sequencial têm sido frequentemente empregados para investigar o comportamento de metais pesados e radionuclídeos artificiais no solo e sedimentos (Bourg et al, 1999;Wasserman et al, 2002a,b), porém, para o estudo do comportamento dos radionuclídeos naturais, esses procedimentos têm sido usados em poucos casos (Bunzl et al, 1995;Lima & PennaFranca, 1998;Schultz et al, 1998 …”
Section: Introductionunclassified