Examining the Spatial and Temporal Variations in CO<em>2</em> Partial Pressure in the Deep Vadose Zone Above Jinapsan Cave, Guam
Carbon dioxide is the primary driver of dissolution and precipitation reactions in epigene limestone caves. While much work has been conducted on CO2 dynamics involved in dissolution in the phreatic zone, less research has been conducted on vadose CO2 dynamics, especially in tropical caves developed...
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| Format: | Others |
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Scholar Commons
2019
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| Online Access: | https://scholarcommons.usf.edu/etd/7904 https://scholarcommons.usf.edu/cgi/viewcontent.cgi?article=9101&context=etd |