Monna F, van Oort F, Hubert P, Dominik J, Bolte J, Loizeau J-L, Labanowski J, Lamri J, Petit C, Le Roux G, Chateau C
UMR 5594 CNRS-Université de Bourgogne, Centre des Sciences de la Terre, ARTéHIS, Bat. Gabriel, F-21000 Dijon, France.
J Environ Radioact. 2009 Jan;100(1):9-16. doi: 10.1016/j.jenvrad.2008.09.009. Epub 2008 Nov 17.
An 80-year soil archive, the 42-plot experimental design at the INRA in Versailles (France), is used here to study long-term contamination by 137Cs atmospheric deposition and the fate of this radioisotope when associated with various agricultural practices: fallow land, KCl, NH4(NO3), superphosphate fertilizers, horse manure and lime amendments. The pertinence of a simple box model, where radiocaesium is supposed to move downward by convectional mechanisms, is checked using samples from control plots which had been neither amended, nor cultivated since 1928. This simple model presents the advantage of depending on only two parameters: alpha, a proportional factor allowing the historical atmospheric 137Cs fluxes to be reconstructed locally, and k, an annual loss coefficient from the plow horizon. Another pseudo-unknown is however necessary to run the model: the shape of historical 137Cs deposition, but this function can be easily computed by merging several curves previously established by other surveys. A loss of approximately 1.5% per year from the plow horizon, combined with appropriate fluxes, provides good concordance between simulated and measured values. In the 0-25cm horizon, the residence half time is found to be approximately 18yr (including both migration and radioactive decay). Migration rate constants are also calculated for some plots receiving continuous long-term agricultural treatments. Comparison with the control plots reveals significant influence of amendments on 137Cs mobility in these soils developed from a unique genoform.
法国凡尔赛的国家农业研究院(INRA)有一个80年的土壤档案,包含42个地块的实验设计,本文利用该档案研究137Cs大气沉降造成的长期污染,以及这种放射性同位素在与各种农业实践(休耕地、氯化钾、硝酸铵、过磷酸钙肥料、马粪和石灰改良剂)相关时的归宿。使用自1928年以来既未改良也未耕种的对照地块的样本,检验了一个简单箱式模型的适用性,该模型假定放射性铯通过对流机制向下移动。这个简单模型的优点是只依赖两个参数:α,一个比例因子,用于在当地重建历史大气137Cs通量;k,耕层的年损失系数。然而,运行该模型还需要另一个伪未知量:历史137Cs沉积的形状,但通过合并先前其他调查建立的几条曲线,可以很容易地计算出这个函数。耕层每年约1.5%的损失率,加上适当的通量,使得模拟值和测量值之间具有良好的一致性。在0-25厘米土层中,停留半衰期约为18年(包括迁移和放射性衰变)。还计算了一些接受连续长期农业处理的地块的迁移速率常数。与对照地块的比较表明,改良剂对这些由单一基因型发育而来的土壤中137Cs的迁移有显著影响。