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湍流扩散是湍流理论中的一个重要问题,并对大气污染等问题具有重要的实际意义。自从Taylor的文章起,五十多年来,许多作者运用拉格朗日观点处理平稳湍流中的扩散问题,取得了不少进展.但至今尚未从理论上解决湍流扩散的概率分布问题,只有解决了这一问题,才箅得到湍流扩散的完整的统计描述。 本文对大雷诺数平稳湍流这一情况,解决了概率分布问题。通过物理分析,文中阐明了大雷诺数平稳湍流可用Markov过程描述;论证了Fokker-Planck方程应采用本文的系数,得到了单粒子运动与二粒子相对运动的转移概率函数,从而得到平稳湍流中单粒子运动及二粒子弥散的完整的统计描述。由此作为特例,证明了单粒子扩散规律与二粒子弥散规律均满足正态性,从而证明了Batchelor的正态假设。此外,作为本文结果的推论,从理论上证明了脉动速度服从正态分布这一著名的实验事实。 关于二粒子相对速度与距离的弥散规律,以及Richardson定律的适用范围,本文与林家翘和W.H.Reid以及E.Krasnoff和R.L.Peskin的结果一致。本文公式当βt<<1时的渐近式与Obukhov一致,从而指明了Obukhov所给方程的局限性。 相似文献
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From observed data on lithospheric plates, a unified empirical law for plate motion,valid for continental as well as oceanic plates, is obtained in the following form: The speedof plate motion U depends linearly on a geometric parameter T_d, ratio of the sum of effectiveridge length and trench arc length to the sum of area of continental part of plate and total areaof cold sinking slab. Based on this unified law, a simple mechanical analysis shows that, themain driving forces for lithospheric plates come from push along the mid-ocean ridge andpull by the cold sinking slab, while the main drag forces consist of the viscous traction beneaththe continental part of plate and over both faces of the sinking slab. Moreover, the specific-push along ridge and pull by slab are found to be of equal magnitude. 相似文献
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Detailed analysis of some difficult aspects has been made from modeling the platemovement. A new method of using differential density of material (instead of differentialtemperature) has been developed in the experiments. The effect of convection of mantleon the plate movement has been studied using a centrifugal technique, and a patternshowing the recurrence of the plate movement has been successfully obtained. In this paper, a criterion De=Dm is presented for the similarity of the model to thecounterpart of the original mantle. According to the criterion, what happens in the modelin a span of ten minutes suggests a process of the "original model" going on in geologi-cal time of three million years. 相似文献
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本文根据观测数据,找到了既适用于大陆板块也适用于海洋板块的统一经验性运动规律:板块的运动速度U正比于几何参数T_d(有效洋脊长度与海沟长度之和除以大陆面积与下沉条带两侧表面积之和)。根据这一经验规律,简化的力学分析表明,板块运动的驱动力来源于洋脊的推力和下沉条带的拉力,阻力主要为作用于板块大陆部分底面和下沉条带两侧面的粘性力。 相似文献
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