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Experiments performed here also suggest a synergistic effect between fire and rain whereby heated soils are more vulnerable to the erosive power of raindrop impacts.
We examined the potential of reflectance spectroscopy across the VIS-NIR SWIR spectral region to identify, ex post facto, the thermal processes that occur in heated soils and minerals, and thus to monitor mineral changes in the soil.
All these changes determined soil microbial activity in heated soils.
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Part of the unburned soil was heated in a muffle at 300 °C (heated soil treatment).
Hot water from such sources also is used for heating soil to increase crop production (e.g., in Oregon) and for seasoning lumber (e.g., in parts of New Zealand).
But none of it made it past a screen and into the tiny chamber, one of eight on the craft designed to heat soil and test gasses for signs of water or organic compounds that could be building blocks for life.
Soil organic matter was estimated by measuring total carbon, which was determined by heating soil in a stream of high purity oxygen in a Leco furnace to produce CO2 and measuring this with an infrared detector.
The winning solution was electro-bioreclamation, a combination of in situ techniques: heating soil and groundwater in the source areas, combined with soil vapour extraction and low-yield groundwater pumping, and enhancing biodegradation in the groundwater plume area.
Post-heating soil sampling revealed TCE concentrations in this region ranging from 27 mg/kg to 96.7 mg/kg, indicating removal of aqueous and gas phase TCE following co-boiling as a result of subsequent boiling of water.
Viking's organic molecule detector heated the soil to release organics.
The Thermal and Evolved Gas Analyzer (TEGA) recorded the release of water when it heated a soil sample to high temperature.
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