阿塞拜疆硫化物多金属矿床中硫化物矿石的低温氧化

IF 0.4 Q4 GEOSCIENCES, MULTIDISCIPLINARY Journal of Geology Geography and Geoecology Pub Date : 2023-04-09 DOI:10.15421/112306
Rasim T. Ismayilov, Vagif M. Kаrimov, S. A. Ganbarova
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引用次数: 0

摘要

本文介绍了阿塞拜疆硫化物多金属矿床主要工业类型硫化物矿石氧化活性测定的实验研究结果。为了计算氧化过程中产生的热量,建立了吸氧速率与矿石温度和湿度的关系。研究发现,在50-80℃以上,随着温度的升高,氧气的吸收速度随着时间的推移而减慢,比在低温(2.5-50℃)下更快。如果温度从2.5℃增加到45-50℃,吸氧量增加7.5-12倍,那么温度从45-50℃增加到80℃,吸氧量只增加3.6-3.7倍,这是由于矿石的水分随着温度的升高而减少,这是由于蒸发造成的。阿塞拜疆硫化物多金属矿床硫化物矿石吸氧速率的时间依赖性出现明显的断裂,表明氧化机理发生了变化。研究了阿塞拜疆Balakan矿田硫化物多金属矿床硫化物矿石在低温(2.5 ~ 800℃)下的氧化活性。确定阿塞拜疆硫化物多金属矿床的主要工业类型硫化物矿石的氧化活性,可以根据自燃倾向的程度对矿石储量进行分类,从而可以采用科学上合理的方法来规划其开发顺序和设计矿山。此外,本文还介绍了在实验室条件下采用以A.A. Skochinsky命名的采矿研究所的方法测定Katsdag、Filizchay和katekkh矿床硫化物矿石氧化活性的实验研究结果。氧化活性的一个指标是氧吸收速率常数,用字母U (ml/g hour)标记。实验室研究结果表明,矿石的氧化导致温度升高和着火,这取决于矿物组成、化学活性、湿度、温度、破碎度等诸多因素。得到了不同温度下硫化物矿石吸氧总量随时间的变化规律。已经确定,随着温度的升高,硫化物矿石的吸氧速率增加。在2.5 ~ 800c温度范围内,温度系数Kt < 2.0,表明硫化矿的氧化速率受氧扩散的控制,而不受化学反应速率的控制。由于矿样中化学元素破碎均匀,分布均匀,氧化速率与硫化物矿的外表面成正比。
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Low-temperature oxidation of sulphide ores of sulphide-polymetallic deposits of Azerbaijan
The article presents the results of experimental studies to determine the oxidative ac- tivity for the main industrial types of sulphide ores of sulphide-polymetallic deposits in Azerbai- jan. To calculate the amount of heat generated during oxidation, the dependences of the oxygen absorption rate on the temperature and moisture of the ore were established. It was found that with an increase in temperature above 50-80oC, absorption of oxygen slows down with time faster than at low (2.5-50oC) temperatures. If with an increase in temperature from 2.5 to 45-50oC the amount of absorbed oxygen increases by 7.5-12 times, then at a temperature from 45-50oC to 80oC it increases only by 3.6-3.7 times, which is explained by a decrease in moisture of the ore with an increase in temperature, due to evaporation. The time dependence of absorption rate of the oxygen for sulphide ores of sulphide-polymetallic deposits of Azerbaijan has a clearly pronounced break, which indicates a change in the oxidation mechanism. The oxidizing activity of sulphide ores of sulphide-polymetallic deposits of the Balakan ore field of Azerbaijan at low temperatures (2.5-800C) was studied. Determination of the oxidative activity of the main industrial types of sulphide ores of sulphide-polymetallic deposits in Azerbaijan makes it possible to classify ore reserves according to the degree of tendency to spontaneous combustion, which will allow a scientifically sound approach to planning the sequence of their development and designing mines. In addition, the article presents the results of experimental studies to determine the oxidizing activity of the sulfide ores of the Katsdag, Filizchay and Katekh deposits, carried out in laboratory conditions by the method of Institute of Mining named after A.A. Skochinsky. An indicator of oxidative activity is the oxygen absorption rate constant and labeled by the letter U (ml/g hour). The results of laboratory studies show that the oxidation of the ore leads to an increase in temperature and ignition and depends on a large number of factors such as mineralogical composition, chemical activity, humidity, temperature, fragmentation, etc. The dependence of the total amount of oxygen absorbed by sulphide ores on time at various temperatures is obtained. It has been estab- lished that with increasing temperature, the rate of oxygen absorption by sulphide ores increases. The values of the temperature coefficient (Kt < 2.0) in the temperature range of 2.5-800C show that the rate of the oxidation of sulfide ore is controlled by oxygen diffusion, and not by the rate of the chemical reaction. With equal fragmentation and equal distribution of chemical elements in ore samples, the oxidation rate is directly proportional to the outer surface of the sulphide ore.
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来源期刊
Journal of Geology Geography and Geoecology
Journal of Geology Geography and Geoecology GEOSCIENCES, MULTIDISCIPLINARY-
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