Physical Processes Dictate Early Biogeochemical Dynamics of Soil Pyrogenic Organic Matter in a Subtropical Forest Ecosystem

Quantifying links between pyOM dynamics, environmental factors and processes is central to predicting ecosystem function and response to future perturbations. In this study, changes in carbon (TC), nitrogen (TN), pH, and relative recalcitrance (R50) for pine- and cordgrass-derived pyOM were measured...

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Main Authors: Jason M. Stuart, Russell Anderson, Patrick Lazzarino, Kevin A. Kuehn, Omar R. Harvey
Format: Article
Language:English
Published: Frontiers Media S.A. 2018-05-01
Series:Frontiers in Earth Science
Subjects:
Online Access:http://journal.frontiersin.org/article/10.3389/feart.2018.00052/full
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spelling doaj-62dac4912d8248eda111c90268fa54f32020-11-25T00:33:36ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632018-05-01610.3389/feart.2018.00052337428Physical Processes Dictate Early Biogeochemical Dynamics of Soil Pyrogenic Organic Matter in a Subtropical Forest EcosystemJason M. Stuart0Russell Anderson1Patrick Lazzarino2Kevin A. Kuehn3Omar R. Harvey4Omar R. Harvey5Department of Geography and Geology, University of Southern Mississippi, Hattiesburg, MS, United StatesDepartment of Geography and Geology, University of Southern Mississippi, Hattiesburg, MS, United StatesSchool of Geology, Energy and the Environment, Texas Christian University, Fort Worth, TX, United StatesDepartment of Biological Sciences, University of Southern Mississippi, Hattiesburg, MS, United StatesDepartment of Geography and Geology, University of Southern Mississippi, Hattiesburg, MS, United StatesSchool of Geology, Energy and the Environment, Texas Christian University, Fort Worth, TX, United StatesQuantifying links between pyOM dynamics, environmental factors and processes is central to predicting ecosystem function and response to future perturbations. In this study, changes in carbon (TC), nitrogen (TN), pH, and relative recalcitrance (R50) for pine- and cordgrass-derived pyOM were measured at 3–6 weeks intervals throughout the first year of burial in the soil. Objectives were to (1) identify key environmental factors and processes driving early-stage pyOM dynamics, and (2) develop quantitative relationships between environmental factors and observed changes in pyOM properties. The study was conducted in sandy soils of a forested ecosystem within the Longleaf pine range of the United States with a focus on links between changes in pyOM properties, fire history (FH), cumulative precipitation (Pcum), average temperature (Tavg) and soil residence time (SRT). Pcum, SRT and Tavg were the main factors controlling TC and TN accounting for 77–91% and 64–96% of their respective variability. Fire history, along with Pcum, SRT and Tavg, exhibited significant controlling effects on pyOM pH and R50—accounting for 48–91% and 88–93% of respective variability. Volatilization of volatiles and leaching of water-soluble components (in summer) and the sorption of exogenous organic matter (fall through spring) were most plausibly controlling pyOM dynamics in this study. Overall, our results point to climatic and land management factors and physicochemical process as the main drivers of pyOM dynamics in the pine ecosystems of the Southeastern US.http://journal.frontiersin.org/article/10.3389/feart.2018.00052/fullpyOM dynamicsfire-derived soil carbonforest soilsrecalcitrancepriming effects
collection DOAJ
language English
format Article
sources DOAJ
author Jason M. Stuart
Russell Anderson
Patrick Lazzarino
Kevin A. Kuehn
Omar R. Harvey
Omar R. Harvey
spellingShingle Jason M. Stuart
Russell Anderson
Patrick Lazzarino
Kevin A. Kuehn
Omar R. Harvey
Omar R. Harvey
Physical Processes Dictate Early Biogeochemical Dynamics of Soil Pyrogenic Organic Matter in a Subtropical Forest Ecosystem
Frontiers in Earth Science
pyOM dynamics
fire-derived soil carbon
forest soils
recalcitrance
priming effects
author_facet Jason M. Stuart
Russell Anderson
Patrick Lazzarino
Kevin A. Kuehn
Omar R. Harvey
Omar R. Harvey
author_sort Jason M. Stuart
title Physical Processes Dictate Early Biogeochemical Dynamics of Soil Pyrogenic Organic Matter in a Subtropical Forest Ecosystem
title_short Physical Processes Dictate Early Biogeochemical Dynamics of Soil Pyrogenic Organic Matter in a Subtropical Forest Ecosystem
title_full Physical Processes Dictate Early Biogeochemical Dynamics of Soil Pyrogenic Organic Matter in a Subtropical Forest Ecosystem
title_fullStr Physical Processes Dictate Early Biogeochemical Dynamics of Soil Pyrogenic Organic Matter in a Subtropical Forest Ecosystem
title_full_unstemmed Physical Processes Dictate Early Biogeochemical Dynamics of Soil Pyrogenic Organic Matter in a Subtropical Forest Ecosystem
title_sort physical processes dictate early biogeochemical dynamics of soil pyrogenic organic matter in a subtropical forest ecosystem
publisher Frontiers Media S.A.
series Frontiers in Earth Science
issn 2296-6463
publishDate 2018-05-01
description Quantifying links between pyOM dynamics, environmental factors and processes is central to predicting ecosystem function and response to future perturbations. In this study, changes in carbon (TC), nitrogen (TN), pH, and relative recalcitrance (R50) for pine- and cordgrass-derived pyOM were measured at 3–6 weeks intervals throughout the first year of burial in the soil. Objectives were to (1) identify key environmental factors and processes driving early-stage pyOM dynamics, and (2) develop quantitative relationships between environmental factors and observed changes in pyOM properties. The study was conducted in sandy soils of a forested ecosystem within the Longleaf pine range of the United States with a focus on links between changes in pyOM properties, fire history (FH), cumulative precipitation (Pcum), average temperature (Tavg) and soil residence time (SRT). Pcum, SRT and Tavg were the main factors controlling TC and TN accounting for 77–91% and 64–96% of their respective variability. Fire history, along with Pcum, SRT and Tavg, exhibited significant controlling effects on pyOM pH and R50—accounting for 48–91% and 88–93% of respective variability. Volatilization of volatiles and leaching of water-soluble components (in summer) and the sorption of exogenous organic matter (fall through spring) were most plausibly controlling pyOM dynamics in this study. Overall, our results point to climatic and land management factors and physicochemical process as the main drivers of pyOM dynamics in the pine ecosystems of the Southeastern US.
topic pyOM dynamics
fire-derived soil carbon
forest soils
recalcitrance
priming effects
url http://journal.frontiersin.org/article/10.3389/feart.2018.00052/full
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