颗粒诱导的炎症应激反应的量化:土材料毒性测试的新方法

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geochemical Transactions Pub Date : 2012-04-18 DOI:10.1186/1467-4866-13-4
Andrea D Harrington, Stella E Tsirka, Martin AA Schoonen
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引用次数: 9

摘要

活性氧(ROS)是体内许多细胞功能的重要调节因子。细胞内ROS浓度受促氧化剂和抗氧化剂之间的平衡高度调节。促氧化剂的慢性过量导致ROS浓度升高和炎症,可能引发或加剧疾病的发作。矿物质诱导的活性氧的产生,矿物质在上调细胞活性氧中的作用,以及它们在几种职业疾病发展中的作用现已得到广泛认识。然而,没有标准方案来确定暴露于矿物粉尘或泥土材料后细胞中ROS产生的变化。在本研究中,描述了一种确定颗粒细胞毒性程度(即细胞毒性)的新方法,这将有助于弥合知识上的差距。通过测量ROS的产生和细胞的活力,定义了炎症应激反应(inflammatory stress response, ISR)指标。这种方法使ROS的上调在测量时相对于活细胞的数量正常化。我们对一系列矿物和土壤进行了实验,这些矿物和土壤代表惰性物质(即玻璃珠,锐钛矿和微量元素含量低的土壤),中等活性物质(即微量元素含量高的土壤)和高活性物质(即黄铁矿)。惰性材料产生的ISR最低,平均为对照组的350%。酸洗黄铁矿的ISR最高(比对照高1100倍)。作为时间函数进行的测量显示出复杂的响应。大多数材料的ISR随颗粒载荷的增加而增加。细胞生成ROS的数量和细胞活力相结合,可以更好地理解颗粒诱导的氧化应激。结果表明,一些土壤材料可能会引起ROS的初始爆发,随后是细胞活力下降和ROS产量增加的第二阶段,导致高ISR值。因此,在一系列颗粒载荷范围内进行的测量与长达24小时的多次数据测量相结合,可以为接触地球材料对人类健康的可能影响提供新的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Quantification of particle-induced inflammatory stress response: a novel approach for toxicity testing of earth materials

Reactive oxygen species (ROS) are vital regulators of many cellular functions in the body. The intracellular ROS concentration is highly regulated by a balance between pro-oxidants and anti-oxidants. A chronic excess of pro-oxidants leads to elevated ROS concentrations and inflammation, possibly initiating or enhancing disease onset. Mineral-induced generation of ROS, the role of minerals in upregulating cellular ROS, and their role in the development of several occupational diseases are now widely recognized. However, there is no standard protocol to determine changes in ROS production in cells after exposure to mineral dust or earth materials in general. In this study, a new method for determining the degree of cellular toxicity (i.e., cytotoxicity) of particles is described that will help bridge the gap in knowledge.

By measuring the production of ROS and the viability of cells, an inflammatory stress response (ISR) indicator is defined. This approach normalizes the ROS upregulation with respect to the number of viable cells at the time of measurement. We conducted experiments on a series of minerals and soils that represent materials that are inert (i.e., glass beads, anatase, and a soil with low trace element content), moderately reactive (i.e., soil with high trace element content), and highly reactive (i.e., pyrite). Inert materials generated the lowest ISR, averaging 350% compared to the control. Acid washed pyrite produced the highest ISR (1,100 fold higher than the control). The measurements conducted as a function of time showed a complex response. Most materials showed an increase in ISR with particle loading.

The amount of cellularly generated ROS and cell viability combined provide a better understanding of particle-induced oxidative stress. The results indicate that some earth materials may solicit an initial burst of ROS, followed by a second phase in which cell viability decreases and ROS production increases, leading to a high ISR value. Hence, measurements conducted over a range of particle loading combined with multiple data measurements up to 24 hours can provide new insights in the possible effect of exposure to earth materials on human health.

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来源期刊
Geochemical Transactions
Geochemical Transactions 地学-地球化学与地球物理
CiteScore
3.70
自引率
4.30%
发文量
2
审稿时长
>12 weeks
期刊介绍: Geochemical Transactions publishes high-quality research in all areas of chemistry as it relates to materials and processes occurring in terrestrial and extraterrestrial systems.
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