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针铁矿吸附硒的微型真菌烷基化和挥发作用。

Microfungal alkylation and volatilization of selenium adsorbed by goethite.

机构信息

Geosciences Institute, Johannes Gutenberg-University, Mainz 55099, Germany.

出版信息

Environ Sci Technol. 2010 Jan 1;44(1):129-35. doi: 10.1021/es9006492.

DOI:10.1021/es9006492
PMID:20039743
Abstract

Selenium adsorbed in the oxyanionic form by Fe-oxides like goethite is considered of benefit for long-term stabilization of (79)Se under near field conditions of radionuclide waste disposal sites. However, microbe-mediated volatilization of the uranium fission product (79)Se has not yet been considered for risk assessment based on the use of the water-solid distribution coefficient K(D). We have performed incubation experiments in a ternary system selenium-microbe-goethite and show that mycobiota including the common black microfungi genera Alternaria alternata are capable of volatilizing the Se even if immobilized by goethite. The microfungi were incubated in a standardized nutrient broth suspension with 10 g L(-1) of the oxide target under defined conditions. Volatile organic selenium (VOSe) species formed in the head space of the culture flasks were sampled and measured directly by a cryotrapping cryofocusing gas chromatographic system coupled with ICP-MS detection (CT-CF-GC-ICP-MS). Alkylated VOSe species were found at the tens to hundreds ng m(-3) levels dominated by dimethyl selenide (DMSe) and dimethyl diselenide (DMDSe). The total amount of DMSe released into the 80-mL headspace volume within the 21 days of incubation was up to 1.12 +/- 0.17 nmol and 0.48 +/- 0.12 nmol for systems without and with goethite amendment, respectively. Alkylation rates of up to 0.1 mumol Se per day and g biomass cannot be neglected as a potential fission product mobilization pathway, unless the inherent radioactivity is proven to prevent any such microbial activity on the long-term. Otherwise it may lead to an onsite accumulation of (79)Se through evapoconcentration in the enclosed underground caverns.

摘要

硒以氧阴离子的形式被针铁矿等铁氧化物吸附,被认为有利于在放射性废物处置场近场条件下(79)硒的长期稳定。然而,基于水-固分配系数 K(D)的应用,微生物介导的铀裂变产物(79)硒的挥发尚未被认为是风险评估的一部分。我们在硒-微生物-针铁矿的三元体系中进行了孵育实验,结果表明,包括常见的黑霉菌属交替单胞菌在内的微生物群能够挥发硒,即使被针铁矿固定也是如此。在标准营养肉汤悬浮液中,用 10 g L(-1)的氧化物靶在规定条件下孵育微生物。在培养瓶的气相空间中形成的挥发性有机硒(VOSe)物种通过冷冻捕集冷聚焦气相色谱系统与 ICP-MS 检测(CT-CF-GC-ICP-MS)直接采样和测量。在数十到数百 ng m(-3)的水平上发现了烷基化的 VOSe 物种,主要为二甲基硒(DMSe)和二甲基二硒(DMDSe)。在 21 天的孵育期内,进入 80 毫升顶空体积的 DMSe 释放总量分别高达 1.12 +/- 0.17 nmol 和 0.48 +/- 0.12 nmol,对于没有和添加针铁矿的系统分别。每天每克生物量高达 0.1 mumol Se 的烷基化率不能被忽视,因为这是一种潜在的裂变产物迁移途径,除非固有放射性被证明能够长期防止任何此类微生物活性。否则,它可能会导致(79)硒在封闭的地下洞穴中通过蒸发浓缩而在现场积累。

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