I'd forgotten about that trip!
The lighter test is a quick method of getting a rough idea of whether or not air might be safe to breathe. The lighter test actually reflects the concentration of O2 in the atmosphere. While O2 is converted to CO2 by microbial processes in the subsurface, the final relationship between CO2 and O2 in air is not 1-1, as described in this series of experiments conducted by Australian cavers (http://nhvss.org.au/wp-content/publi...0Helictite.pdf). While the lighter test is better than nothing, and many, many cavers have used it extensively to guide safer exploration of caves with high CO2, the only reliable method of knowing the actual concentration of CO2 in the atmosphere is to buy a CO2 meter.
While CO2 meters used for scientific work can be pretty pricey, if you're only interested in figuring out if you should be breathing the air in a confined space, meters are pretty reasonable ~$100 (http://www.co2meter.com/collections/...table-co-meter). You can transport these in a tube through sumps and then open them up when you arrive on the other side. At $100 each, its not the end of the world if they get flooded....
Finally, I should point out that it is a common misconception that CO2 gas in caves comes from decaying vegetation in caves or from CO2 degassing from dripwater. There is a group of cave researchers (including me) that have been studying the origin of cave air CO2 for several years now - the isotopic signatures of CO2 in cave air (and other lines of evidence) indicate the most likely origins are (A) decay of dissolved organic matter in the space between the soil zone and the water table and (b) respiration of tree roots. The CO2 diffuses through fractures and pores in the rock and accumulates in areas of the cave that are poorly ventilated, such as low spots. Much of our current research is on understanding how the production of this CO2 is linked to formation of caves in places like Florida, Guam, the Yucatan and the Bahamas (or any other location where the limestone is highly porous, which includes parts of the Domincan Republic). In other locations where the rock is less porous (Kentucky, Tennessee, Missouri, etc.) the production of CO2 between the soil and water table exerts an important control on climate records preserved in speleothems.
In the case of air bells between sumps, high CO2 concentrations are sometimes possible due to degassing of CO2 dissolved in the stream - particularly if the stream originates on the surface and sinks into the ground.
My recommendation would be that anyone diving sumps in tropical environments should consider buying a CO2 meter.



Reply With Quote
Semper Fi, Cameron David Smith, my son, my hero. 11/9/1989 - 11/13/2010 

Bookmarks