1988
DOI: 10.1524/ract.1988.4445.1.125
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Technetium in the Hydrosphere and in the Geosphere

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Cited by 43 publications
(28 citation statements)
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“…The behavior of plutonium may be controlled by the chemistry of Pu 4 +, PuQ2+, or PuO2 2 + depending on the redox potential of the solution. Under slightly reducing conditions where Pu(IV,V) dominate, important species will include Pu(OH) 4 The behavior of technetium is expected to be dominated by the chemistry of the highly soluble pertechnetate ion, TcO 4 -, which is not hydrolyzed [243,244], complexed, or sorbed onto mineral surfaces. Tc(IV) species may dominate under reducing conditions.…”
Section: 1mentioning
confidence: 99%
See 1 more Smart Citation
“…The behavior of plutonium may be controlled by the chemistry of Pu 4 +, PuQ2+, or PuO2 2 + depending on the redox potential of the solution. Under slightly reducing conditions where Pu(IV,V) dominate, important species will include Pu(OH) 4 The behavior of technetium is expected to be dominated by the chemistry of the highly soluble pertechnetate ion, TcO 4 -, which is not hydrolyzed [243,244], complexed, or sorbed onto mineral surfaces. Tc(IV) species may dominate under reducing conditions.…”
Section: 1mentioning
confidence: 99%
“…Reduction to U4+ may occur under mildly reducing conditions. U 4 + is more strongly complexed than The behavior of technetium is expected to be dominated by the chemistry of the highly soluble pertechnetate ion, TcO 4 -, which is not hydrolyzed [243,244], complexed, or sorbed onto mineral surfaces. Tc(IV) species may dominate under reducing conditions.…”
mentioning
confidence: 99%
“…Complexation of TcO Ϫ 4 with humic acid and other dissolved organic carbon is only possible when the Eh-value becomes negative (E 0 =Ϫ0.50 V for Tc(VII)/Tc(IV)), (Rößler et al, 2000). As noted by Lieser and Bauscher (1987) (Henrot, 1989). Literature reports therefore suggest that neither chemical nor biological factors have much impact on the generally high availability of 99 Tc in aerobic soils.…”
Section: Tc In Aerobic and Anaerobic Soilsmentioning
confidence: 96%
“…In another study, Bird and Lopata (1980), in which solutions containing only trace concentrations were used, noted no measurable pertechnetate adsorption by magnetite. Studies by Lieser and Bauscher (1988), in which groundwater was used, and Bostick et al (1990), in which simulant raffinate was used, also showed negligible adsorption of 99 Tc (K d : <0.1 to 3 mL/g). These observations were confirmed by Byegard et al (1992), who observed that magnetite, when tested in synthetic and natural groundwater matrices (containing relatively high concentrations of SO 4 ) under both oxic and anoxic conditions, showed relatively poor affinity for 99 Tc (K d : 0.3 to 1.3 mL/g).…”
Section: Oxide and Hydroxide Mineralsmentioning
confidence: 99%
“…Metallic copper and its oxides (Haq et al 1980), soils and soil minerals (Rancon 1988), cementitious forms (Atkins and Glasser 1990), various types of minerals (Couture and Seitz 1983, Fetter et al 1996, Gradev 1987, Kang et al 1999, Krumhansl 2003, Taylor 1990), organophilic clays (Bors et al 1994a), modified montmorillonites (Sazarashi et al 1995), and novel adsorbents (Kaplan et al 2000 have been tested and evaluated for their getter properties for radioiodine. A similar effort was conducted to identify suitable getters for 99 Tc (Balsley et al 1985, Balsley et al 1996, Balsley et al 1997, Byegard et al 1992, Cui and Eriksen 1996b, Ito and Kanno 1988, Kang et al 1999, Kang et al 1996, Krumhansl 2003, Kunze et al 1996, Liang et al 1996, Lieser and Bauscher, 1988, Moore 2003, Palmer and Meyer 1981, Strickert et al 1980, Viani 1999, Wellman et al 2006, Zhuang et al 1988). …”
Section: Gettersmentioning
confidence: 99%