Abstract

Self-heating of fuel layers can trigger ignition when the temperature of the surroundings is sufficiently high. Self-heating ignition has been a hazard and safety concern in raw materials production, transportation, and storage facilities for centuries. Hot plate and oven-basket experiments are the two most used lab-scale experiments to assess the hazard of self-heating ignition. While extensive experiments have been done to study this phenomenon, modelling of the experiments is substantially lagging behind. A computational model that can accurately simulate self-heating ignition under the two experimental configurations has not been developed yet. In this study, we build such a model by coupling heat transfer, mass transfer, and chemistry using the open-source code Gpyro. Due to the accessibility of large amount of experimental data, coal is chosen as the material for model validation. A literature review of the kinetic parameters for coal samples from different origins reveals that there is a compensation effect between the activation energy and exponential factor. Combining the compensation effect with our model, we simulate 6 different experimental studies covering the two experimental configurations, a wide range of sample sizes (heights ranging from 5 mm to 126 mm), and various coal origins (6 countries). The model accurately predicts critical ignition temperature (Tig) for all 24 experiments with an error below 7 °C. This computational model unifies for the first time the two most used self-heating ignition experiments and provides theoretical insights to understand self-ignition for different fuels under different conditions.

Highlights

  • Self-heating is the temperature rise tendency of a material due to heat generated by exothermic processes taking place within the body of material [1]

  • A fuel layer has self-heating propensity, because exothermic low-temperature oxidation can occur between solid phase fuel dust and the oxygen diffusing from ambient atmosphere inside the fuel layer

  • The occurrence of compensation effect here might suggest the existence of some characteristic temperature Tiso, around which the exothermic reactions occurring during self-heating ignition of different coals have a same reaction rate constant, which can be referred as ηiso

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Summary

Introduction

Self-heating is the temperature rise tendency of a material due to heat generated by exothermic processes taking place within the body of material [1]. It is seen that both experiments aim to measure the critical surrounding temperature (either hot plate or oven temperature) that triggers ignition This temperature is one of the most important indicators to assess the self-heating and ignition hazard for fuel layers. Ambient hot plate experiment and the self-ignition temperature in oven-basket experiment are denoted uniformly as Tig in this paper Both types of experiments have been conducted extensively to evaluate the self-heating and ignition hazard of various fuels, such as coals [7,9,10,11,12,13], carbon-rich soils [14], shale rocks [15,55], and biomass [16,17,18,19]. Six different experimental studies (24 experiments in total) covering both experimental configurations, a wide range of sample sizes, and various coal origins are simulated using this validated model

Model development
Literature values
Chemical kinetics of coal self-heating ignition
Validation against hot plate experiment
Validation against oven-basket experiment
The compensation effect between E and A across coals
Prediction of Tig for different coal self-heating ignition experiments
Findings
Conclusions
Full Text
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