臭氧分解时间的优化及其对地下水理化、细菌学质量的影响

O. Nwaiwu, V. Ibekwe
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引用次数: 0

摘要

臭氧广泛用于水消毒,有效消除微生物所需的浓度取决于水源。在许多瓶装水生产行业中,含有臭氧的产品在使用后会被隔离,以分解成双原子氧分子和氧原子,从而消除任何毒性影响。对尼日利亚南部一家淡水生产厂的臭氧分解时间进行了工艺优化。为此,注入臭氧的瓶装水产品在生产后立即从灌装线上收集,并监测臭氧分解情况。测定了总溶解固体、温度和pH等参数,并对细菌总数和假修道院菌群和大肠菌群的存在进行了细菌学分析。研究发现,臭氧的半衰期不到30分钟,两个半小时后就无法检测到了。对于所有分析的储存产品,pH值在7.0-7.06范围内,而温度在23至25°C之间。总溶解固体在0.05至0.09 mg/mL之间,生产后储存24或48小时的瓶装产品没有显著差异(p>0.05)。未检测到细菌。更短的隔离期可以更快地进行分配,并突出了臭氧分解测试对工艺优化的重要性,尤其是在设备或水源随时间变化的情况下。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Optimization of ozone decomposition time and its effect on physicochemical and bacteriological quality of table water
Ozone is widely used in water disinfection and the concentration needed for the effective microbial elimination depends on the water source. In many bottled water producing industries, products containing ozone are quarantined after application to allow decomposition into diatomic oxygen molecules and oxygen atoms in order to eliminate any toxic effect. A process optimization was carried out to determine the ozone decomposition time in a table water producing factory in southern Nigeria. To this end, bottled water products injected with the ozone were collected from a bottling line immediately after production and monitored for ozone decomposition. Parameters like total dissolved solids, temperature and pH were determined and bacteriological analyses for total bacteria count and presence of Pseudomonasand coliforms were carried out. It was found that the ozone half-life was under 30 minutes and was no longer detectable after two and a half hours. For all analyzed stored products, the pH was in the range of 7.0-7.06, while the temperature was between 23 and 25 °C. The total dissolved solids ranged from 0.05 to 0.09 mg/mL, and there was no significant difference (p> 0.05) for the bottled products stored for 24 or 48 hours after the production. No bacteria weredetected. The shorter quarantine period allows quicker distribution and highlights the importance of ozone decomposition testing for the process optimization, especially if equipment or water source change over time.
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