Transactions of Nonferrous Metals Society of China The Chinese Journal of Nonferrous Metals

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中国有色金属学报

ZHONGGUO YOUSEJINSHU XUEBAO

第25卷    第2期    总第191期    2015年2月

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文章编号:1004-0609(2015)02-0492-08
硫化矿石自热过程的分维特性
潘 伟1, 2,吴 超2,李孜军2,杨月平3

(1. 辽宁工程技术大学 矿山热动力灾害与防治教育部重点实验室,阜新 123000;
2. 中南大学 资源与安全工程学院,长沙 410083;
3. 南华大学 核资源工程学院,衡阳 421001
)

摘 要: 为揭示硫化矿石自热过程的分形特征,以从现场采集的矿石样品作为实验材料,开展矿石自热特性实验,集成小波技术和分形理论对实测温度数据进行研究。结果表明:仅矿样1、2、3和8出现明显自热现象,自热起始温度分别为136.3、178.5、195.4和200 ℃,在正常采矿条件下,矿石不易产生自热现象;矿样自热过程具有稳定的关联维数,验证了基于分形理论研究自热过程的可行性;在实验条件基本一致的前提下,随着自热起始温度的增大,矿样自热过程的关联维数逐渐减小,可采用关联维数来定性判断自热倾向性强弱;自热效果明显的矿样,其实验后期的关联维数大于实验前期的值,因此,可根据关联维数的变化特征来判定矿样出现明显自热的可能性,从而可减少重复实验的工作量。

 

关键字: 硫化矿石;自热过程;小波技术;分形理论;关联维数;自热倾向性

Fractal dimension characteristics of self-heating process of sulfide ores
PAN Wei1, 2, WU Chao2, LI Zi-jun2, YANG Yue-ping3

1. Key Laboratory of Mine Thermo-motive Disaster and Prevention, Ministry of Education,
Liaoning Technical University, Fuxin 123000, China;
2. School of Resources and Safety Engineering, Central South University, Changsha 410083, China;
3. School of Nuclear Resources Engineering, University of South China, Hengyang 421001, China

Abstract:To reveal the fractal characteristics of self-heating process of sulfide ores, ore samples from a copper mine were taken as experimental materials, and the self-heating characteristics were measured in laboratory. Furthermore, the measured temperature was studied by integrating wavelet technology and fractal theory. The results indicate that only the ore samples 1, 2, 3 and 8 appear obvious self-heating tendency, and their self-heating initiative temperatures are 136.3, 178.5, 195.4 and 200 ℃, respectively, which mean that they are difficult to show self-heating tendency under normal mining conditions. The correlation dimension of self-heating process of ore samples is stable, meaning that it is feasible to study the self-heating process based on fractal theory. If the experimental conditions are basically consistent, the correlation dimension of self-heating process of ore samples decreases with the increase of he self-heating initiative temperature. So, the correlation dimension can be applied to qualitatively determine the self-heating tendency. For the ore samples appearing obvious self-heating tendency in the experiment, the correlation dimension of the late period is greater than that of the previous period. Therefore, the possibility for obvious self-heating tendency of ore samples can be determined according to the variation characteristics of the correlation dimension, which can reduce the workload of repeated experiments.

 

Key words: sulfide ore; self-heating process; wavelet technology; fractal theory; correlation dimension; self-heating tendency

ISSN 1004-0609
CN 43-1238/TG
CODEN: ZYJXFK

ISSN 1003-6326
CN 43-1239/TG
CODEN: TNMCEW

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