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氚水在大豆土壤系统中的迁移与分布 总被引:8,自引:2,他引:6
采用模拟污染物的同位素示踪技术研究氚水在大豆-土壤模拟生态系统中的迁移、分布规律.通过为期50d的模拟试验,测定了植物和土壤样品中2种形态氚(自由水氚和结合态氚)的比活度.结果表明:引入土壤中的氚水,不仅在系统各分室间转移和分配,而且迅速向系统外散逸;氚水中的氚以自由水氚和结合态氚形态存在于大豆植株和土壤中;大豆植株中的自由水氚比活度于6h时即达最大值(根19.4Bq·g-1;茎叶12.3Bq·g-1),随后便逐渐下降,而结合态氚呈缓慢增加;大豆根中的总氚比活度开始时高于茎叶中的比活度,而后趋于平衡,表层土中2种形态氚基本呈逐渐下降.运用示踪动力学分室模型原理对实验数据拟合得:土壤中的比活度Cs=88.37e-11.847t+7.38e-0030t;大豆植株中的比活度Cb=10.30(e-0.030t-e-11.847t). 相似文献
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Vichot L Boyer C Boissieux T Losset Y Pierrat D 《Journal of environmental radioactivity》2008,99(10):1636-1643
In order to quantify tritium impact on the environmental, we studied vegetation continuously exposed to a tritiated atmosphere. We chose lichens as bio-indicators, trees for determination of past tritium releases of the Valduc Centre, and lettuce as edible vegetables for dose calculation regarding neighbourhood. The Pasquill and Doury models from the literature were tested to estimate tritium concentration in the air around vegetable for distance from the release point less than 500m. The results in tree rings show that organically bound tritium (OBT) concentration was strongly correlated with tritium releases. Using the GASCON model, the modelled variation of OBT concentration with distance was correlated with the measurements. Although lichens are recognized as bio-indicators, our experiments show that they were not convenient for environmental surveys because their age is not definitive. Thus, tritium integration time cannot be precisely determined. Furthermore, their biological metabolism is not well known and tritium concentration appears to be largely dependent on species. An average conversion rate of HTO to OBT was determined for lettuce of about 0.20-0.24%h(-1). Nevertheless, even if it is equivalent to values already published in the literature for other vegetation, we have shown that this conversion rate, established by weekly samples, varies by a factor of 10 during the different stages of lettuce development, and that its variation is linked to the biomass derivative. 相似文献
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Compounds in the atmosphere contaminate samples of groundwater. An inexpensive and simple method for collecting groundwater samples is developed to prevent contamination when the background concentration of contaminants is high. This new design of groundwater sampling device involves a glass sampling bottle with a Teflon-lined valve at each end. A cleaned and dried sampling bottle was connected to a low flow-rate peristaltic pump with Teflon tubing and was filled with water. No headspace volume was remained in the sampling bottle. The sample bottle was then packed in a PVC bag to prevent the target component from infiltrating into the water sample through the valves. In this study, groundwater was sampled at six wells using both the conventional method and the improved method. The analysis of trichlorofluoromethane( CFC-11 ) concentrations at these six wells indicates that all the groundwater samples obtained by the conventional sampling method were contaminated by CFC-11 from the atmosphere. The improved sampling method greatly eliminated the problems of contamination, preservation and quantitative analysis of natural water. 相似文献
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Theodore W. Sammis Daniel D. Evans A. W. Warrick 《Journal of the American Water Resources Association》1982,18(3):465-470
ABSTRACT: Deep percolation rates are normally estimated from a water balance. Results are presented of a study undertaken to evaluate three alternative methods of estimating percolation below the root zone when knowledge about the history of applied water and evapotranspiration are not available. The alternative methods are: 1) use of Darcy's equation to calculate deep percolation rate; 2) measurement of the soil temperature prof and calculation of the deep percolation rate from the shape of the temperature depth curve; and 3) measurement of the tritium concentration in the soil water and its relationship to the history of the tritium concentration in rainfall. At the principal study site, the Darcy velocity of flow ranged from 9 cm per year determined by the temperature method, to 40 cm per year determined by the tritium method. Darcy's equation to calculate seepage rates resulted in an estimation of deep seepage of 18 cm per year. An average deep percolation rate at the principal study site of 22 cm per year was determined using the average of all three methods. Results for other sites based on the temperature method indicated a lower seepage rate. 相似文献
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