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MIT professor develops method to verify compliance with Outer Space Treaty
Danagoulian
Areg Danagoulian of the Department of Nuclear Science and Engineering at the Massachusetts Institute of Technology is proposing a mechanism for verifying that Earth-orbiting satellites are in compliance with the Outer Space Treaty, which prohibits the placement of nuclear weapons in space. Danagoulian’s “concept and feasibility study,” titled “Verification of the Outer Space Treaty with cosmic protons,” was published recently in the journal Nature.
Andrew Miskowiec, Jenn Neu, Christian Salvador, Liam Collins, Benjamin T. Manard, Zachary E. Brubaker, Mengdawn Cheng
Nuclear Science and Engineering | Volume 199 | Number 7 | July 2025 | Pages 1231-1245
Research Article | doi.org/10.1080/00295639.2024.2440686
Articles are hosted by Taylor and Francis Online.
Uranium hexafluoride (UF6) undergoes a rapid hydrolysis reaction when exposed to atmospheric water. In addition to producing hazardous HF gas, the hydrolysis reaction produces uranyl fluoride (UO2F2), a radioactive solid phase particulate material. Because of the technological utility of UF6 in the nuclear fuel cycle, understanding the transport properties of UO2F2 aerosol produced via UF6 hydrolysis is important for accident scenarios. Moreover, the fundamental chemical and physical properties of the UF6 hydrolysis reaction are not completely understood. Recently, several experiments on the aerosol phase properties of UO2F2 produced in this way have shown that under most relevant conditions, the particle size distribution (PSD) of UO2F2 can be extremely small, approximately 3 to 5 nm, which is well below the threshold that can be routinely observed via scanning electron microscopy (SEM). Although readily observable in the aerosol phase, observation of nanometer-sized particles in the condensed phase (i.e. deposited on surfaces) remains a challenge. Here, we have used atomic force microscopy (AFM) to study the PSD and morphological characteristics of UO2F2 deposited at low and high concentrations under different humidity conditions, a primary variable in the hydrolysis reaction. We find strong agreement between PSD measured in the aerosol phase via scanning mobility particle sizing and PSD measured via AFM, with particle sizes peaked below 4 nm for low-humidity conditions. At higher humidity, the distribution is centered around 5 to 10 nm but extends up to 20 nm. These results are in stark contrast to previous measurements using SEM that show PSD on the order of 300- to 1000-nm particle sizes; moreover, these are the first direct measurements of individual particles of UO2F2 having been produced via UF6 hydrolysis deposited on surfaces. These measurements, therefore, open a new avenue for collecting and detecting UO2F2 in the condensed phase and further refine the PSD, which is critical for environmental transport determinations.