The reactivity of experimentally reduced lunar regolith simulants: Health implications for future crewed missions to the lunar surface

IF 2.2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Donald A. Hendrix, Tristan Catalano, Hanna Nekvasil, Timothy D. Glotch, Carey Legett IV, Joel A. Hurowitz
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Abstract

Crewed missions to the Moon may resume as early as 2026 with NASA's Artemis III mission, and lunar dust exposure/inhalation is a potentially serious health hazard that requires detailed study. Current dust exposure limits are based on Apollo-era samples that spent decades in long-term storage on Earth; their diminished reactivity may lead to underestimation of potential harm that could be caused by lunar dust exposure. In particular, lunar dust contains nanophase metallic iron grains, produced by “space weathering”; the reactivity of this unique component of lunar dust is not well understood. Herein, we employ a chemical reduction technique that exposes lunar simulants to heat and hydrogen gas to produce metallic iron particles on grain surfaces. We assess the capacity of these reduced lunar simulants to generate hydroxyl radical (OH*) when immersed in deionized (DI) water, simulated lung fluid (SLF), and artificial lysosomal fluid (ALF). Lunar simulant reduction produces surface-adhered metallic iron “blebs” that resemble nanophase metallic iron particles found in lunar dust grains. Reduced samples generate ~5–100× greater concentrations of the oxidative OH* in DI water versus non-reduced simulants, which we attribute to metallic iron. SLF and ALF appear to reduce measured OH*. The increase in observed OH* generation for reduced simulants implies high oxidative damage upon exposure to lunar dust. Low levels of OH* measured in SLF and ALF imply potential damage to proteins or quenching of OH* generation, respectively. Reduction of lunar dust simulants provides a quick cost-effective approach to study dusty materials analogous to authentic lunar dust.

Abstract Image

经实验还原的月球碎屑模拟物的反应性:对未来月球表面载人飞行任务的健康影响
美国国家航空航天局(NASA)的阿特米斯三号(Artemis III)任务最早可能于 2026 年恢复载人登月任务,而月球尘埃暴露/吸入可能对健康造成严重危害,需要进行详细研究。目前的尘埃暴露限值是基于阿波罗时代的样本,这些样本在地球上长期储存了几十年;它们的反应性降低,可能导致低估月球尘埃暴露可能造成的潜在危害。特别是,月球尘埃中含有由 "太空风化 "产生的纳米级金属铁粒;人们对月球尘埃中这一独特成分的反应性还不甚了解。在这里,我们采用了一种化学还原技术,将月球模拟物暴露于热量和氢气中,在颗粒表面产生金属铁颗粒。我们评估了这些还原月球模拟物在浸入去离子水、模拟肺液和人工溶酶体液时产生羟基自由基(OH*)的能力。月球模拟液还原会产生表面附着的金属铁 "斑点",与月球尘粒中的纳米级金属铁颗粒相似。与未还原的模拟物相比,还原样品在去离子水中产生的氧化OH*浓度要高出约5-100倍,我们将其归因于金属铁。SLF和ALF似乎减少了测得的OH*。在还原模拟物中观察到的 OH* 生成量的增加意味着暴露在月球尘埃中会受到严重的氧化损伤。在SLF和ALF中测得的OH*水平较低,这分别意味着蛋白质可能受到损伤或OH*生成被淬灭。还原月球尘埃模拟物为研究与真实月球尘埃类似的尘埃物质提供了一种快速、经济有效的方法。
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来源期刊
Meteoritics & Planetary Science
Meteoritics & Planetary Science 地学天文-地球化学与地球物理
CiteScore
3.90
自引率
31.80%
发文量
121
审稿时长
3 months
期刊介绍: First issued in 1953, the journal publishes research articles describing the latest results of new studies, invited reviews of major topics in planetary science, editorials on issues of current interest in the field, and book reviews. The publications are original, not considered for publication elsewhere, and undergo peer-review. The topics include the origin and history of the solar system, planets and natural satellites, interplanetary dust and interstellar medium, lunar samples, meteors, and meteorites, asteroids, comets, craters, and tektites. Our authors and editors are professional scientists representing numerous disciplines, including astronomy, astrophysics, physics, geophysics, chemistry, isotope geochemistry, mineralogy, earth science, geology, and biology. MAPS has subscribers in over 40 countries. Fifty percent of MAPS'' readers are based outside the USA. The journal is available in hard copy and online.
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