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Formation of calcareous deposits on cathodically protected steel in seawater.

机译:海水中阴极保护钢上钙质沉积物的形成。

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A rotating disc electrode technique was used to grow calcareous deposits on low carbon steel specimens in ASTM substitute ocean water at room temperature in the laboratory. Concurrently, a first principle mathematical model was developed to model the formation of calcareous deposits on cathodically protected steel in seawater. The mass transfer of components was described by diffusion, migration, and convection. Three kinds of chemical reactions were taken into consideration in the model: two electrochemical reactions, two precipitation reactions, and one homogeneous reaction. The model equations were cast in finite difference form and solved using Newman's BAND(J) subroutine with an implicit time-stepping technique to obtain the surface coverage of the calcareous films, the concentrations, and potential distributions throughout the diffusion layer. The mechanism of the formation of calcareous deposits may be quantitatively explained from the concentration profiles in the diffusion layer. Also the model is of capability of predicting the changes in current density and deposit composition with time.; A sensitivity analysis was performed to determine the relative sensitivity of parameters to the predicted current density and surface coverage. The results can be used to determine which parameters have the largest influence on the predicted values, and then which parameters are needed to be obtained accurately through experiments or parameter estimation technique. The effects of rotation speed, electrode potential, seawater, salinity, and depth on the formation of calcareous deposits have been examined in the model. The model will be used to predict the conditions necessary for the formation and the maintenance of calcareous films on structural steel in deep ocean water. In addition, the model was used to obtain the time-dependent polarization curves on cathodically protected steel in seawater.
机译:在实验室中,使用旋转圆盘电极技术在ASTM替代海水中在低碳钢试样上生长钙质沉积物。同时,开发了第一个原理数学模型来模拟海水中阴极保护钢上钙质沉积物的形成。通过扩散,迁移和对流描述了组分的传质。该模型考虑了三种化学反应:两个电化学反应,两个沉淀反应和一个均相反应。将模型方程式转换为有限差分形式,并使用纽曼的BAND(J)子例程使用隐式时间步进技术进行求解,以获取钙质薄膜的表面覆盖率,浓度以及整个扩散层的电势分布。钙质沉积物的形成机理可以从扩散层中的浓度分布定量地解释。该模型还具有预测电流密度和沉积物组成随时间变化的能力。进行敏感性分析以确定参数对预测的电流密度和表面覆盖率的相对敏感性。结果可用于确定哪些参数对预测值的影响最大,然后需要通过实验或参数估计技术准确获取哪些参数。在模型中检查了转速,电极电势,海水,盐度和深度对钙质沉积物形成的影响。该模型将用于预测深海海水中结构钢上钙质膜的形成和维持所需的条件。此外,该模型还用于获得海水中阴极保护钢的时间相关极化曲线。

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