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A fast and sensitive method for evaluating nuclides migration characteristics in rock medium by using micro-channel reactor concept

机译:利用微通道反应器概念快速,灵敏地评估岩石介质中核素迁移特性的方法

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Experimental effort to evaluate the barrier performance of geologic disposal requires relatively long testing periods and chemically stable conditions. We have developed a new technique, the micro mock-up method, to present a fast and sensitive method to measure both nuclide diffusivity and sorption coefficient within a day to overcome such disadvantage of the conventional method. In this method, a Teflon plate having a micro channel (10-200 μm depth, 2, 4 mm width) is placed just beneath the rock sample plate, radionuclide solution is injected into the channel with constant rate. The breakthrough curve is being measured until a steady state. The outlet flux in the steady state however does not meet the inlet flux because of the matrix diffusion into the rock body. This inlet-outlet difference is simply related to the effective diffusion coefficient (D_e) and the distribution coefficient (K_d) of rock sample. Then, we adopt a fitting procedure to speculate K_d and D_e values by comparing the observation to the theoretical curve of the two-dimensional diffusion-advection equation. In the present study, we measured D_e of ~3H by using both the micro mock-up method and the conventional through-diffusion method for comparison. The obtained values of D_e by two different ways for granite sample (Inada area of Japan) were identical: 1.0 x 10~(-11) and 9.0 x 10~(-12) m~2/s but the testing period was much different: 10 h and 3 days, respectively. We also measured the breakthrough curve of ~(85)Sr and the resulting K_d and D_e agreed well to the previous study obtained by the batch sorption experiments with crushed samples. The experimental evidence and the above advantages reveal that the micro mock-up method based on the microreactor concept is powerful and much advantageous when compared to the conventional method.
机译:评估地质处置屏障性能的实验工作需要相对较长的测试时间和化学稳定的条件。我们已经开发出一种新技术,即微型模型法,提出了一种快速灵敏的方法,可以在一天内测量核素的扩散率和吸附系数,从而克服了传统方法的这种缺点。在这种方法中,将具有微通道(深度为10-200μm,宽度为2、4 mm,宽度为4 mm)的聚四氟乙烯板放置在岩石样品板的正下方,将放射性核素溶液以恒定速率注入通道中。测量穿透曲线直至稳定状态。但是,由于基体扩散到岩石体内,因此稳态下的出口通量不能满足入口通量。进出口差仅与岩石样品的有效扩散系数(D_e)和分布系数(K_d)有关。然后,通过将观测值与二维扩散对流方程的理论曲线进行比较,我们采用拟合程序来推测K_d和D_e值。在本研究中,我们使用微观模型法和常规的直通扩散法进行了测量,测得的D_e约为3H。通过两种不同方式获得的花岗岩样品(日本稻田地区)的D_e值是相同的:1.0 x 10〜(-11)和9.0 x 10〜(-12)m〜2 / s,但测试时间差异很大:分别为10小时和3天。我们还测量了〜(85)Sr的穿透曲线,所得的K_d和D_e与通过粉碎样品的批吸附实验获得的先前研究吻合得很好。实验证据和上述优点表明,与常规方法相比,基于微反应器概念的微模型化方法功能强大且非常有利。

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