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首页> 外文期刊>International Journal of Materials, Methods and Technologies >MODELING VOID RATIO AND DISPERSION OF CARBON INFLUENCE ON CRYPTOSPORIDIUM DEPOSITION IN SILTY FORMATION UNDER PROGRESSIVE PHASE IN COASTAL AREA OF OKRIKA, RIVERS STATE OF NIGERIA
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MODELING VOID RATIO AND DISPERSION OF CARBON INFLUENCE ON CRYPTOSPORIDIUM DEPOSITION IN SILTY FORMATION UNDER PROGRESSIVE PHASE IN COASTAL AREA OF OKRIKA, RIVERS STATE OF NIGERIA

机译：尼日利亚河流域OKRIKA沿海地区渐进阶段模拟孔隙比和碳扩散对粉质形成中隐孢子虫沉积的影响

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Modeling void ratio and dispersion of carbon influence on cryptosporidium deposition in silty formation under progressive phase in coastal area of Okirika has been thoroughly expressed. Geologic process by which soils are formed described various limits on the size of soil particles and the mechanical analysis of the soil in natural occurrence since it consists of three phases solid. Water and air have a relationship with their structure deposition including their plasticity. Subject to this relation, the volume of relationship that is commonly used for the three phases in soil elements is void ratio, porosity and degree of saturation. This condition expresses the influence of dispersion rate of cryptosporidium dispersion. Thus, stratification of the formation based on these relationships between porosity. Void ratio and degree of saturation has been found to play serious roles in this condition. Formation characteristics such as the void ratio are determined by disintegration of the rock mass under porous condition subjecting it to intercede of the soil matrix. Disintegration of this porous sedimentary rock determines the void deposition which influences the dispersion rate of the microbes. These actions in order to monitor or determine the dispersion rate in the study location, mathematical model were established to ensure that such kinds of determinants are observed. The models were formulated through the variables that influenced the system subjecting them to fast dispersion of the microbes under the influence of void ratio.
机译：在Okirika沿海地区，在渐进相的粉质形成过程中，碳空隙率和碳的扩散对隐孢子虫沉积的影响的模型已被充分表达。形成土壤的地质过程描述了对土壤颗粒大小的各种限制以及自然发生的土壤的力学分析，因为它由固态的三相组成。水和空气与其结构沉积（包括其可塑性）有关。服从这种关系，土壤元素中三相通常使用的关系体积为空隙率，孔隙率和饱和度。该条件表示隐孢子虫分散体的分散速度的影响。因此，基于孔隙度之间的这些关系使地层分层。已经发现在这种情况下空隙率和饱和度起着重要的作用。孔隙率之类的地层特征是通过在多孔条件下岩体在土壤基质中的插入作用下崩解来确定的。这种多孔沉积岩的崩解决定了影响微生物分散速率的孔隙沉积。为了监测或确定研究位置的分散率，采取了这些措施，建立了数学模型以确保观察到此类决定因素。这些模型是通过影响系统的变量制定的，这些变量使系统在空隙率的影响下使微生物快速分散。

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