Pilon-Smits EA, Lytle CM, Hwang S, Tai J, Honma TS, Yeh L, Terry N
Department of Plant and Microbial Biology, 111 Koshland Hall, University of California, Berkeley, California 94720, USA.
Plant Physiol. 1998 Aug;117(4):1487-94. doi: 10.1104/pp.117.4.1487.
Se can be accumulated by plants and volatilized to dimethylselenide, providing an attractive technology for Se phytoremediation. To determine the rate-limiting steps in Se volatilization from selenate and selenite, time- and concentration-dependent kinetics of Se accumulation and volatilization were studied in Indian mustard (Brassica juncea). Time-dependent kinetic studies showed that selenate was taken up 2-fold faster than selenite. Selenate was rapidly translocated to the shoot, away from the root, the site of volatilization, whereas only approximately 10% of the selenite was translocated. For both selenate- and selenite-supplied plants, Se accumulation and volatilization increased linearly with external Se concentration up to 20 &mgr;M; volatilization rates were also linearly correlated with root Se concentrations. Se-volatilization rates were 2- to 3-fold higher from plants supplied with selenite compared with selenate. Se speciation by x-ray absorption spectroscopy revealed that selenite-supplied plants accumulated organic Se, most likely selenomethionine, whereas selenate-supplied plants accumulated selenate. Our data suggest that Se volatilization from selenate is limited by the rate of selenate reduction, as well as by the availability of Se in roots, as influenced by uptake and translocation. Se volatilization from selenite may be limited by selenite uptake and by the conversion of selenomethionine to dimethylselenide.
硒可以被植物积累并挥发成二甲基硒,这为硒的植物修复提供了一项有吸引力的技术。为了确定从硒酸盐和亚硒酸盐中挥发硒的限速步骤,我们在印度芥菜(Brassica juncea)中研究了硒积累和挥发的时间和浓度依赖性动力学。时间依赖性动力学研究表明,硒酸盐的吸收速度比亚硒酸盐快2倍。硒酸盐迅速从根部(挥发部位)转运到地上部分,而只有约10%的亚硒酸盐被转运。对于供应硒酸盐和亚硒酸盐的植物,硒的积累和挥发在外部硒浓度高达20 μM时随浓度呈线性增加;挥发速率也与根部硒浓度呈线性相关。与供应硒酸盐的植物相比,供应亚硒酸盐的植物的硒挥发速率高2至3倍。通过X射线吸收光谱法进行的硒形态分析表明,供应亚硒酸盐的植物积累有机硒,最有可能是硒代蛋氨酸,而供应硒酸盐的植物积累硒酸盐。我们的数据表明,从硒酸盐中挥发硒受到硒酸盐还原速率以及根部硒的可利用性的限制,后者受吸收和转运的影响。从亚硒酸盐中挥发硒可能受到亚硒酸盐吸收以及硒代蛋氨酸向二甲基硒转化的限制。