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评估冷大气压等离子体辐照水作为单线态氧产生方法的效果。

Evaluation of cold atmospheric pressure plasma irradiation of water as a method of singlet oxygen generation.

作者信息

Takajo Tokuko, Nagahama Hiroki, Zuinen Katsuya, Tsuchida Kazunori, Okino Akitoshi, Anzai Kazunori

机构信息

Faculty of Pharmaceutical Sciences, Nihon Pharmaceutical University, 10281 Komuro, Ina-machi, Kitaadachi-gun, Saitama 362-0806, Japan.

Laboratory for Future Interdisciplinary Research of Science and Technology, Institute of Innovative Research, Tokyo Institute of Technology, 4259 Nagatsuta, Midori-ku, Yokohama 226-8502, Japan.

出版信息

J Clin Biochem Nutr. 2023 Jul;73(1):9-15. doi: 10.3164/jcbn.22-111. Epub 2023 May 16.

Abstract

We used cold atmospheric pressure plasma jet to examine in detail O generation in water. ESR with 2,2,5,5-tetramethyl-3-pyrroline-3-carboxamide, a secondary amine probe, was used for the detection of O. Nitroxide radical formation was detected after cold atmospheric pressure plasma jet irradiation of a 2,2,5,5-tetramethyl-3-pyrroline-3-carboxamide solution. An O scavenger/quencher inhibited the ESR signal intensity induced by cold atmospheric pressure plasma jet irradiation, but this inhibition was not 100%. As 2,2,5,5-tetramethyl-3-pyrroline-3-carboxamide reacts with oxidizing species other than O, it was assumed that the signal intensity inhibited by NaN corresponds to only the nitroxide radical generated by O. The concentration of O produced by cold atmospheric pressure plasma jet irradiation for 60 s was estimated at 8 μM. When this O generation was compared to methods of O generation like rose bengal photoirradiation and 4-methyl-1,4-etheno-2,3-benzodioxin-1(4)-propanoic acid (endoperoxide) thermal decomposition, O generation was found to be, in decreasing order, rose bengal photoirradiation ≥ cold atmospheric pressure plasma jet > endoperoxide thermal decomposition. Cold atmospheric pressure plasma jet is presumed to not specifically generate O, but can be used to mimic states of oxidative stress involving multiple ROS.

摘要

我们使用冷大气压等离子体射流详细研究了水中O的生成。使用2,2,5,5-四甲基-3-吡咯啉-3-甲酰胺(一种仲胺探针)的电子自旋共振(ESR)来检测O。在对2,2,5,5-四甲基-3-吡咯啉-3-甲酰胺溶液进行冷大气压等离子体射流辐照后,检测到氮氧化物自由基的形成。一种O清除剂/猝灭剂抑制了冷大气压等离子体射流辐照诱导的ESR信号强度,但这种抑制并非100%。由于2,2,5,5-四甲基-3-吡咯啉-3-甲酰胺会与除O之外的氧化物种发生反应,因此假定NaN抑制的信号强度仅对应于由O产生的氮氧化物自由基。冷大气压等离子体射流辐照60秒产生的O浓度估计为8μM。当将这种O的生成与孟加拉玫瑰红光辐照和4-甲基-1,4-亚乙基-2,3-苯并二恶英-1(4)-丙酸(内过氧化物)热分解等O生成方法进行比较时,发现O的生成量从高到低依次为:孟加拉玫瑰红光辐照≥冷大气压等离子体射流>内过氧化物热分解。冷大气压等离子体射流据推测并非特异性地生成O,但可用于模拟涉及多种活性氧的氧化应激状态。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0b14/10390813/53dacc16bd10/jcbn22-111f01.jpg

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