37 Trace Elements in the Environment
Tuesday, 19 March 2024
8:00 AM - 12:00 PM
Merrimack Room
WILDFIRE IMPACTS ON SOIL CHEMISTRY AND THE ROLE OF PYROGENIC CARBON IN SOIL MINERAL TRANSFORMATION
Paper number: 37-12
Program: Theme Sessions
Time: 11:20 AM – 11:40 AM
Authors
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Daniel IbarraBrown University, Providence, RI
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Daniel IbarraProvidence, RI
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Sebastian MunozProvidence, RI
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Sebastian MunozBrown University, Providence, RI
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Evan J. RamosRice University, Houston, TX
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Kly D. SuquinoUniversity of Chicago, Chicago, IL
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Miriam GammermanRice University, Houston, TX
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William LarsenRice University, Houston, TX
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Yi HouRice University, Houston, TX
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Preston Cosslett KemenyUniversity of Chicago, Chicago, IL
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Mark TorresRice University, Houston, TX
Abstract
Here, we investigate the impacts of fires on soil reactive components by linking post-burn soil and water chemistry from the Kwis and Beachie Creek Fires in the Oregon Cascades. Soils were collected across a burn severity gradient controlling for vegetation, lithology, and climate. Surface waters were collected within burnt watersheds, or upstream and downstream of burnt areas. Soils were analyzed for organic carbon content, δ13Corg, major element geochemistry, and the distribution of soil reactive metals were quantified using a three-step leaching method. Waters were analyzed for major and trace metals, major anions, alkalinity, and dissolved organic carbon (DOC). Our results suggest clear evidence of enhanced microbial activity and the reduction and subsequent leaching of ferric oxyhydroxides from soils, corroborated by waters with elevated levels of DOC and arsenic. With recent advances suggesting the importance of soil mineralogy on the ability of soils to sequester carbon, these results highlight the need to account for post-fire changes to soil reactive minerals in considerations of PyOC as a C-sink.
Geological Society of America Abstracts with Programs. Vol. 56, No. 1
doi: 10.1130/abs/2024NE-397725
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