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The Dissolution Rate Constant of Magnetite in Water at Different Temperatures and Neutral or Ammoniated Chemistry Conditions

机译:不同温度和中性或氨化化学条件下磁铁矿在水中的溶解速率常数

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In this study, the dissolution rate constants of magnetite were measured at various water chemistry conditions and different temperatures, corresponding to several feedwater conditions of water-cooled reactors. Sintered magnetite pellets were used as the dissolving material and these were mounted in a jet-impingement apparatus in a recirculating water loop. Exposures were carried out at temperatures of 25, 55 and 140°C and pHs of neutral and 9.2 in which many FAC (Flow Accelerated Corrosion) studies have been conducted. Average dissolution rate constants were estimated by measuring the volume of lost material with a profilometry technique. The excellent correspondent between the calculated value of dissolution rate constant of 2.20 mm/s for the synthesized magnetite and 2.05 mm/s for the single crystal of magnetite at neutral condition shows that the particle removal from the synthesized pellets is not an obstruction in this technique. Also, good agreement between the values calculated in duplicated runs at neutral condition at room temperature supports the accuracy of the method.
机译:在这项研究中,磁铁矿的溶解速率常数是在各种水化学条件和不同温度下测量的,对应于水冷反应器的几种给水条件。使用烧结的磁铁矿颗粒作为溶解材料,并将它们安装在循环水回路中的射流冲击装置中。暴露是在25、55和140°C的温度以及pH值为中性和9.2的条件下进行的,其中进行了许多FAC(流动加速腐蚀)研究。平均溶出速率常数通过轮廓测定技术通过测量损失的物质的体积来估算。合成磁铁矿的溶出速率常数的计算值为2.20 mm / s和磁铁矿单晶在中性条件下的计算值为2.05 mm / s的极佳对应关系表明,从合成颗粒中去除颗粒不会对该技术造成阻碍。同样,在室温下在中性条件下重复运行计算的值之间的良好一致性也支持了该方法的准确性。

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