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Modeling and simulation of cadmium transport influenced by high degree of saturation and porosity on homogeneous coarse depositions

机译:饱和度和孔隙度高对均匀均质沉积物镉迁移的建模与模拟

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Thispaper monitors the effect from degree of saturation and porosity on the migrationrate of cadmium in homogeneous coarse formation. The study expresses the rateof coarse homogeneity reflecting on the deposition of cadmium in deltaicdepositions. Other studies were carried out on a particulars soil formationthat could not predict comprehensive migration rate of cadmium concentration incoarse depositions. These were monitor on deltaic location were coarsedeposition are predominant thus degree of saturation and porosity were observedto influences cadmium concentration in the study area. Porosity and degree of saturationwere the major effect that determine their variation of cadmium concentration,the derived solution were subject to simulation, these values express linearconcentration of cadmium, but with variations at different depth to phreaticbed, the study has express the influences from porosity and degree ofsaturation reflecting on cadmium concentration, experts in pollution transportwill definitely apply this tools to monitor the formation characteristicsinfluences on cadmium transport in deltaic depositions.
机译:本文监测了饱和度和孔隙度对均匀粗地层中镉迁移速率的影响。该研究表示了反映在三角沉积中镉沉积的粗均质率。还针对无法预测粗大沉积物中镉浓度的综合迁移率的特殊土壤形成进行了其他研究。这些是在三角洲地区以粗沉积为主的监测器,因此观察到饱和度和孔隙度会影响研究区域的镉浓度。孔隙率和饱和度是决定其镉浓度变化的主要影响因素,对衍生溶液进行模拟,这些值表示镉的线性浓度,但随着深浅程度的变化,其孔隙度和孔隙度均受到影响。由于饱和度会反映出镉的浓度,因此污染迁移专家肯定会使用此工具来监测形成特征对三角洲沉积物中镉迁移的影响。

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