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9 - Erosion–corrosion of metals in oxidizing atmospheres

Published online by Cambridge University Press:  05 June 2012

Gerald H. Meier
Affiliation:
University of Pittsburgh
Frederick S. Pettit
Affiliation:
University of Pittsburgh
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Summary

Introduction

Under many service situations, materials are exposed to high-temperature gas streams. A gas stream can entrain solid particles, picking up larger particles at higher speeds. In fact it is probable that a particle-free gas flow can only be provided under the most carefully contrived laboratory conditions. In most practical cases, gas streams will contain solid particles. Good examples of this are found in gas turbines, oil refining and reforming, as well as in power generation. This chapter will address the ways in which the oxidation and solid-particle erosion of metals proceed simultaneously and interact.

Erosion of materials

To understand how erosion and oxidation interact, it is necessary to understand how metals and oxides erode. Previous work into the erosion of metals and ceramics at room temperature has shown that the erosion of ductile material involves plastic deformation, cutting, plowing, and fatigue. These mechanisms can occur by the impact of a single particle, as in the case of cutting, or may require several subsequent impacts as in the cases of plowing and fatigue. Brittle materials, on the other hand, erode by the introduction of intersecting brittle crack systems. Most of the metals in use respond in a basically ductile manner at high temperatures. The oxides that arise from oxidation can be either quite ductile (wustite, nickel oxide, etc.) or quite brittle (alumina, chromia, etc.). Depending on the oxide and the circumstances, the oxide scale can be deformed plastically by the erosive impacts; alternatively the oxide could spall under impact.

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Publisher: Cambridge University Press
Print publication year: 2006

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