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THE EFFECT OF PORE STRUCTURE ON THE KINETICS OF FLUID-SOLID REACTIONS.

机译:孔结构对流固反应动力学的影响。

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For fluid-solid reactions a random pore model is developed which accounts for arbitrary pore-size distributions as well as pore intersections in a reacting solid. The model is quite versatile and subsumes the prior grain models as special cases. It is found that a rate maximum may be expected for certain pore size distributions but not for others. In the initial stages of reaction the rate increases with conversion due to increase in the surface area as pore growth occurs, but this effect is overshadowed in later stages by pore intersections which reduce surface area. The model indicates that given the porosity and surface area, a solid possessing uniform size pores is intrinsically the least reactive. The data of Hashimoto, et al. (1979) on the surface area development and conversion-time behavior during char gasification are found to produce correlations consistent with the expectations of the model.; The model is formulated to include as well transport effects arising from boundary layer, intraparticle and product layer diffusion. It is found that the rate and surface area maxima predicted in the kinetic regime are shifted to lower conversions as intraparticle or product layer diffusional resistances increase. For reactions accompanied by an increase in the volume of the solid phase it is shown that incomplete conversions may be expected due to pore closure, the ultimate conversion decreasing with an increase in the intrapellet diffusional resistance. The model is also applied to the data of Borgwardt (1970) and of Hartman and Coughlin (1976) on the reaction between CO(,2) and lime in the presence of oxygen, where the calcium sulfate produced forms a protective product layer. It is seen that the reaction is diffusion controlled under the conditions of Hartman and Coughlin (1976) consistent with their own findings, and a prior Pigford and Sliger (1973) interpretation. The temperature behavior of the diffusion coefficient in the product layer suggests the participation of an activated process, possibly a solid state step.; TGA experiments were conducted with the reaction between CO(,2) and lime, in the range of 400(DEGREES)C to 725(DEGREES)C, with a view to examine the effect of product layer deposition and of varying pore structures on the kinetics. Limes with different pore structures were obtained for reactions by calcining limestone under varying partial pressures of carbon dioxide in nitrogen. It is found that the recarbonation reaction is initially chemically controlled, before undergoing a rapid transition to a much slower regime controlled by product layer diffusion. The magnitude of the product layer diffusivity, in the range of 10('-14) to 10('-17) cm('2)/sec, and the activation energy of about 20 kcal/gmole below 515(DEGREES)C, and 40 kcal/gmole above 515(DEGREES)C, are suggestive of solid state diffusion. Most likely the mechanism involves countercurrent motion of carbonate and oxygen ions below 515(DEGREES)C, and sitewise motion of decomposition-produced CO(,2) above this temperature.
机译:对于流固反应,开发了随机孔模型,该模型考虑了任意孔径分布以及反应固体中的孔交叉点。该模型非常通用,并且将先前的谷物模型作为特殊情况进行了包含。发现对于某些孔径分布可能期望最大速率,而对于其他孔径分布则没有期望。在反应的初始阶段,速率随着转化率的增加而增加,这是由于随着孔的生长表面积的增加而引起的,但是在后来的阶段中,这种作用被孔表面积减小的孔相交所掩盖。该模型表明,给定孔隙度和表面积,具有均匀大小的孔的固体本质上反应性最低。桥本等人的数据。 (1979)发现在焦炭气化过程中表面积的发展和转化时间的行为产生了与模型预期相一致的相关性。将该模型制定为包括边界层,颗粒内和产物层扩散所产生的传输效应。发现随着颗粒内或产物层扩散阻力的增加,在动力学方案中预测的速率和表面积最大值转移至较低的转化率。对于伴随固相体积增加的反应,表明由于孔的封闭可能会发生不完全转化,最终转化率随着颗粒内扩散阻力的增加而降低。该模型还适用于Borgwardt(1970)以及Hartman和Coughlin(1976)关于在氧气存在下CO(,2)和石灰之间反应的数据,其中生成的硫酸钙形成保护性产品层。可以看出,在Hartman和Coughlin(1976)的条件下,根据他们自己的发现以及Pigford和Sliger(1973)的先前解释,该反应受扩散控制。产物层中扩散系数的温度行为表明活化过程的参与,可能是固态步骤。 TGA实验是在400(DEGREES)C至725(DEGREES)C范围内的CO(,2)与石灰之间进行反应的,目的是检查产品层沉积和不同孔结构对产品的影响。动力学。通过在变化的氮气中二氧化碳分压下煅烧石灰石,可以得到具有不同孔结构的石灰用于反应。已经发现,在经历快速过渡到由产物层扩散控制的慢得多的状态之前,再碳酸化反应最初是化学控制的。产物层扩散率的大小在10('-14)至10('-17)cm('2)/秒的范围内,并且在515(DEGREES)C以下时的活化能约为20 kcal / gmole,在515(DEGREES)C以上和40 kcal / gmole提示固态扩散。最可能的机理涉及低于515(DEGREES)C的碳酸盐和氧离子的逆流运动,以及高于该温度的分解生成的CO(,2)的局部运动。

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