The Johns Hopkins Rocket Group is developing hydrogen absorption cell technology to mitigate the Lyman-alpha emission challenge posed by the geocorona for astronomical photometry in the Lyman ultraviolet spectrum (1000- 1216 Å) from low-Earth orbit. We have assembled a prototype cell from 1.33 SS CFF tube, two (2mm) LiF windows and a tungsten filament. The cell is filled with H2 to a pressure of 2 torr. The heated filament thermally dissociates the H2 into its atomic form, which will absorb Lyman-alpha. In theory, the pressure is high enough to collisionaly de-excite the H, thus preventing resonant re-scattering.
We have begun testing and have preliminary results using the Long-slit Imaging Dual Order Spectrograph. Spectral testing of the Lyman-alpha line profiles are vital for advancing hydrogen absorption cell technology in future Lyman ultraviolet missions. These tests can reveal whether or not molecular hydrogen fluorescence is occurring from either electron impact excitation or recombination in higher energy states. Our preliminary results have shown attenuation of the source Lyman-alpha signal by roughly 73% with an associated optical depth of 1.3 and hydrogen column density of 2.2 x 1013. Future tests will involve cooling down our lamp/hydrogen cell system as well as testing multiple filament configurations for the most efficient input power possible.
The Johns Hopkins Rocket Group is advancing Hydrogen Absorption Cell technology to filter geocoronal emissions from Earth's atmosphere. Our innovation, a low-pressure chamber converting molecular hydrogen into its atomic form, is designed to integrate seamlessly into future Lyman ultraviolet missions. Currently, we are engineering this cell to interface with the Long-slit Imaging Dual Order Spectrograph (LIDOS) for comprehensive testing, focusing on stray light detection. This research aims to leverage this technology for photometric measurements and assess its suitability with a spectrograph in future mission concepts.
Observations of astronomical objects in the far ultraviolet (FUV wavelengths span 900-1800 A) from earth's orbit has been impeded due to bright Lyman- geocoronal emission. The Johns Hopkins Rocket Group is developing a hydrogen absorption cell that would act as a narrow band Lyman- rejection filter to enable space-based photometric observation in bandpasses that span over the Lyman ultraviolet region shortward of the geocoronal line. While this technology has been applied to various planetary missions with single element photomultiplier detectors it has yet to be used on near earth orbiting satellites with a multi-element detector. We are working to develop a cell that could be easily incorporated into future Lyman ultraviolet missions. The prototype cell is a low-pressure (~few torr) chamber sealed between a pair of MgF2 windows allowing transmission down to 1150 A. It is filled with molecular hydrogen that is converted to its neutral atomic form in the presence of a hot tungsten lament, which allows for the absorption of the Lyman- photons. Molecular hydrogen is stored in a fully saturated non-evaporable getter module (St707TM), which allows the cell pressure to be increased under a modest application of heat (a 20 degree rise from room temperature has produced a rise in pressure from 0.6 to 10 torr). Testing is now underway using a vacuum ultraviolet monochromator to characterize the cell optical depth to Lyman- photons as functions of pressure and tungsten filament current. We will present these results, along with a discussion of enabled science in broadband photometric applications.
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