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This dissertation presents an in-situ analysis of the albedo and petrologic texture of glassy lava flows at Jordan Craters, Oregon, utilizing VNIR spectroscopy. The study examines the variations in reflectance and mineralogy, including the implications for identifying ancient water and life on Mars. It explores changes in albedo linked to crystallinity and the presence of hydrous minerals, and emphasizes the use of VNIR to differentiate between water and air quenched basalts.
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01
Gather necessary equipment, including a spectrometer and sampling tools.
02
Identify the sampling site and ensure it is representative of the area of interest.
03
Collect soil or material samples from the site.
04
Measure the crystalline structure of the samples using the spectrometer, ensuring to follow calibration procedures.
05
Record the percentage of crystalline versus amorphous content in the samples.
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To determine albedo, place the samples under controlled lighting conditions.
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Measure the reflectance of the samples using a photometer at various angles.
08
Calculate the average albedo value based on the reflectance measurements.
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Document all findings and ensure data accuracy before finalizing the report.

Who needs crystallinity and albedo in-situ?

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Climate scientists studying the effects of land surface properties on climate.
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Environmental researchers assessing ecosystem health.
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Agricultural professionals evaluating soil health and crop productivity.
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Urban planners considering the impact of surface materials in city planning.
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Geologists and mineralogists investigating material properties.
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Hydrologists studying water absorption and runoff in different areas.
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Crystallinity refers to the degree of structural order in a solid, while albedo in-situ pertains to the reflectivity of a surface measured directly at its location, aiding in understanding solar energy absorption.
Entities involved in environmental assessments or projects impacting land use, such as construction companies, environmental agencies, and researchers, are typically required to file crystallinity and albedo in-situ.
To fill out crystallinity and albedo in-situ, one must gather relevant site-specific data, complete the required forms detailing the measurements, and submit them to the appropriate regulatory authority.
The purpose of crystallinity and albedo in-situ is to assess environmental conditions and potential impacts related to land use changes, which can influence heat retention and energy balance.
Reported information includes geographical location, measurement methodologies, specific values of crystallinity and albedo, dates of measurements, and any relevant environmental conditions.
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