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[FNAME] => Rabia
[LNAME] => Amen
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[SHDEP] => Forestry
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[START_START] => 2024-05-01
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[FNAME] => David
[LNAME] => Everson
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[SHDEP] => Forestry
[COURSEPRE] => Array
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[FNAME] => Gertrude
[LNAME] => Aturu
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[SHDEP] => Forestry
[COURSEPRE] => Array
(
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[TITLE] => Foliar and soil nutrient content, carbon allocation, and root systems of 12 Longleaf pine genotypes
[COMPSTAGE] => In-Process
[COMMENT] => Array
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[DTM_START] => January
[DTD_START] => Array
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[START_START] => 2024-01-01
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[id] => 318502823936
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[id] => 318502823937
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[FNAME] => James "Ryan"
[LNAME] => Grantham
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[SHDEP] => Wildlife, Fisheries, & Aquaculture
[COURSEPRE] => NREC
[COURSENUM] => 4800
[CHOURS] => Array
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[COMMENT] => Ryan is an undergraduate student (WFA-WLFS, 2025) who works in my lab. He prepares soil samples for carbon and nitrogen analysis under a DOE-funded project entitled, "PoSIES: Populus in the southeast for integrated ecosystem services."
[DTM_START] => January
[DTD_START] => Array
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[DTY_START] => 2024
[START_START] => 2024-01-01
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[id] => 290884108288
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[FNAME] => Quentin
[LNAME] => Boccaleri
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[SHDEP] => Forestry
[COURSEPRE] => Array
(
)
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[TITLE] => Array
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[COMMENT] => Developing an optimized site selection model for eastern cottonwood and black willow in the Lower Mississippi Alluvial Valley
[DTM_START] => December
[DTD_START] => Array
(
)
[DTY_START] => 2023
[START_START] => 2023-12-01
[START_END] => 2023-12-31
[DTM_END] => Array
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[DTD_END] => Array
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[id] => 318509899776
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[TYPE] => Master's Thesis Committee Member
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[@attributes] => Array
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[id] => 318509899777
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[FNAME] => Baylor
[LNAME] => Doughty
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[SHDEP] => Forestry
[COURSEPRE] => Array
(
)
[COURSENUM] => Array
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)
[CHOURS] => Array
(
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[TITLE] => Interspecific competition effects on biomass allocation in a young, fertilized longleaf pine stand in central Mississippi
[COMPSTAGE] => In-Process
[COMMENT] => Array
(
)
[DTM_START] => August
[DTD_START] => Array
(
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[DTY_START] => 2023
[START_START] => 2023-08-01
[START_END] => 2023-08-31
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[id] => 318439362560
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[TYPE] => Supervised Undergraduate Research
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[@attributes] => Array
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[id] => 318439362561
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[FNAME] => Allyson
[LNAME] => Trahan
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[SHDEP] => Forestry
[COURSEPRE] => FO
[COURSENUM] => 4800
[CHOURS] => Array
(
)
[TITLE] => Climate change mitigation potential of Conservation Reserve Program tree planting practices: soil nitrogen cycling
[COMPSTAGE] => In-Process
[COMMENT] => Allyson Trahan is an undergraduate student (FO-WFMG, 2025) who works in my lab. She performs laboratory incubation experiments to determine nitrogen transformation on soil samples collected under a USDA-funded project entitled, "Climate change mitigation assessment of Conservation Reserve Program practices with trees."
[DTM_START] => August
[DTD_START] => Array
(
)
[DTY_START] => 2023
[START_START] => 2023-08-01
[START_END] => 2023-08-31
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[DTD_END] => Array
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[DTY_END] => Array
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[id] => 318439710720
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[TYPE] => Supervised Undergraduate Research
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[FNAME] => Caleb
[LNAME] => Heflin
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[SHDEP] => Forestry
[COURSEPRE] => FO
[COURSENUM] => 4800
[CHOURS] => Array
(
)
[TITLE] => Array
(
)
[COMPSTAGE] => In-Process
[COMMENT] => Caleb Heflin is an undergraduate student (FO-FOMG, 2025) who works in my lab. He assists in measuring soil greenhouse gas fluxes, collects soil samples and prepares them for carbon and nitrogen analysis, and measures tree productivity on samples collected under a DOE-funded project entitled, "PoSIES: Populus in the southeast for integrated ecosystem services."
[DTM_START] => August
[DTD_START] => Array
(
)
[DTY_START] => 2023
[START_START] => 2023-08-01
[START_END] => 2023-08-31
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[COMMUNITY_ENGAGEMENT] => No
[MSU_MISSION] => Array
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)
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[14] => Array
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[@attributes] => Array
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[id] => 318439725056
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[TYPE] => Supervised Undergraduate Research
[TYPE_OTHER] => Array
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[INTERNATIONAL] => Array
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[@attributes] => Array
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[id] => 318439725057
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[FNAME] => Madeline
[LNAME] => Brown
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[SHDEP] => Wildlife, Fisheries, & Aquaculture
[COURSEPRE] => NREC
[COURSENUM] => 4800
[CHOURS] => Array
(
)
[TITLE] => Array
(
)
[COMPSTAGE] => In-Process
[COMMENT] => Madeline is an undergraduate student (WFA-WLFS, 2027) who works in my lab. She determines soil nitrogen transformation rates using in-situ ion exchange resins under a DOE-funded project entitled, "PoSIES: Populus in the southeast for integrated ecosystem services."
[DTM_START] => August
[DTD_START] => Array
(
)
[DTY_START] => 2023
[START_START] => 2023-08-01
[START_END] => 2023-08-31
[DTM_END] => Array
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[DTD_END] => Array
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[DTY_END] => Array
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[END_START] => Array
(
)
[END_END] => Array
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)
[COMMUNITY_ENGAGEMENT] => No
[MSU_MISSION] => Array
(
)
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[15] => Array
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[@attributes] => Array
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[id] => 318439768064
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[TYPE] => Supervised Undergraduate Research
[TYPE_OTHER] => Array
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[INTERNATIONAL] => Array
(
)
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[@attributes] => Array
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[id] => 318439768065
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[FNAME] => Nathaniel
[LNAME] => Barnard
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[SHDEP] => Forestry
[COURSEPRE] => FO
[COURSENUM] => 4800
[CHOURS] => Array
(
)
[TITLE] => Array
(
)
[COMPSTAGE] => In-Process
[COMMENT] => Nathaniel is an undergraduate student (FO-WFMG, 2026) who works in my lab. He is conducting wood decomposition analysis under a USDA-funded project entitled, "Climate change mitigation assessment of Conservation Reserve Program practices with trees."
[DTM_START] => August
[DTD_START] => Array
(
)
[DTY_START] => 2023
[START_START] => 2023-08-01
[START_END] => 2023-08-31
[DTM_END] => Array
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[DTD_END] => Array
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[DTY_END] => Array
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[END_START] => Array
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)
[COMMUNITY_ENGAGEMENT] => No
[MSU_MISSION] => Array
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)
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[16] => Array
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[@attributes] => Array
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[id] => 318439573504
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[TYPE] => Supervised Undergraduate Research
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[@attributes] => Array
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[id] => 318439573505
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[FNAME] => Nyla
[LNAME] => Jones
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[SHDEP] => Forestry
[COURSEPRE] => NREC
[COURSENUM] => 4800
[CHOURS] => Array
(
)
[TITLE] => Impacts of biodiversity of short-rotation woody crops on water quality
[COMPSTAGE] => In-Process
[COMMENT] => Nyla Jones is an undergraduate student (NREC-NRLA, 2026) who works in my lab. She determines soil nitrogen transformation rates using in-situ ion exchange resins under a DOE-funded project entitled, "PoSIES: Populus in the southeast for integrated ecosystem services."
[DTM_START] => August
[DTD_START] => Array
(
)
[DTY_START] => 2023
[START_START] => 2023-08-01
[START_END] => 2023-08-31
[DTM_END] => Array
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)
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)
[COMMUNITY_ENGAGEMENT] => No
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)
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[id] => 151887712256
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[TYPE] => Dissertation Committee Member
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)
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[@attributes] => Array
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[FNAME] => Shaina
[LNAME] => Wilburn
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[SHDEP] => Geosciences
[COURSEPRE] => Array
(
)
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(
)
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)
[TITLE] => An investigation into the climatology of extreme montane mesoscale phenomena and the impacts on associated ecosystems
[COMPSTAGE] => In-Process
[COMMENT] => January 22, 2024 - oral comprehensive exams
November 3, 2023 - proposal defense
[DTM_START] => April
[DTD_START] => Array
(
)
[DTY_START] => 2023
[START_START] => 2023-04-01
[START_END] => 2023-04-30
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)
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[id] => 290883962880
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[TYPE] => Doctoral Major Professor
[TYPE_OTHER] => Array
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)
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[@attributes] => Array
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[id] => 290883962881
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[FNAME] => Jianing
[LNAME] => Liang
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[SHDEP] => Forestry
[COURSEPRE] => Array
(
)
[COURSENUM] => Array
(
)
[CHOURS] => Array
(
)
[TITLE] => The Greenhouse Gas (GHG) Flux and Tree Biomass Carbon Storage for Conservation Reserve Program (CRP) Land with Tree Planting Practices in the Southeastern US
[COMPSTAGE] => In-Process
[COMMENT] => May 6-10, 2024 - Written Comprehensive Exams
May 20, 2024 - Oral Comprehensive Exams
[DTM_START] => January
[DTD_START] => Array
(
)
[DTY_START] => 2022
[START_START] => 2022-01-01
[START_END] => 2022-01-31
[DTM_END] => Array
(
)
[DTD_END] => Array
(
)
[DTY_END] => Array
(
)
[END_START] => Array
(
)
[END_END] => Array
(
)
[COMMUNITY_ENGAGEMENT] => Yes
[MSU_MISSION] => Yes
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[19] => Array
(
[@attributes] => Array
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[id] => 318505725952
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[TYPE] => Supervised Undergraduate Research
[TYPE_OTHER] => Array
(
)
[INTERNATIONAL] => Array
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)
[DSL_STUDENT] => Array
(
[@attributes] => Array
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[id] => 318505725953
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[FNAME] => Roshan
[LNAME] => Thapa
)
[SHDEP] => Agricultural & Biological Engineering
[COURSEPRE] => NREC
[COURSENUM] => 4800
[CHOURS] => Array
(
)
[TITLE] => Taxonomic and functional diversity controls on soil carbon sequestration potential in woody bioenergy crops
[COMPSTAGE] => Completed
[COMMENT] => Roshan is an undergraduate student (ABE, 2024) who works in my lab. He prepared soil samples for carbon and nitrogen analysis under a DOE-funded project entitled, "PoSIES: Populus in the southeast for integrated ecosystem services." He analyzed the results and even though he graduated, will be a co-author on a manuscript to evaluate the role of biodiversity in soil carbon sequestration.
[DTM_START] => January
[DTD_START] => Array
(
)
[DTY_START] => 2024
[START_START] => 2024-01-01
[START_END] => 2024-01-31
[DTM_END] => December
[DTD_END] => Array
(
)
[DTY_END] => 2024
[END_START] => 2024-12-01
[END_END] => 2024-12-31
[COMMUNITY_ENGAGEMENT] => No
[MSU_MISSION] => Array
(
)
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[20] => Array
(
[@attributes] => Array
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[id] => 151887714304
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[TYPE] => Dissertation Committee Member
[TYPE_OTHER] => Array
(
)
[INTERNATIONAL] => Array
(
)
[DSL_STUDENT] => Array
(
[@attributes] => Array
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[id] => 151887714305
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[FNAME] => Jiaxin
[LNAME] => Wang
)
[SHDEP] => Forestry
[COURSEPRE] => Array
(
)
[COURSENUM] => Array
(
)
[CHOURS] => Array
(
)
[TITLE] => Optimizing Bioenergy Production with Populus in the Southeastern United States from Physiological Ecology Aspect
[COMPSTAGE] => Completed
[COMMENT] => Array
(
)
[DTM_START] => August
[DTD_START] => Array
(
)
[DTY_START] => 2018
[START_START] => 2018-08-01
[START_END] => 2018-08-31
[DTM_END] => December
[DTD_END] => Array
(
)
[DTY_END] => 2024
[END_START] => 2024-12-01
[END_END] => 2024-12-31
[COMMUNITY_ENGAGEMENT] => Array
(
)
[MSU_MISSION] => Array
(
)
)
[21] => Array
(
[@attributes] => Array
(
[id] => 318439313408
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[TYPE] => Supervised Undergraduate Research
[TYPE_OTHER] => Array
(
)
[INTERNATIONAL] => Array
(
)
[DSL_STUDENT] => Array
(
[@attributes] => Array
(
[id] => 318439313409
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[FNAME] => Sarah
[LNAME] => Harney
)
[SHDEP] => Forestry
[COURSEPRE] => Array
(
)
[COURSENUM] => Array
(
)
[CHOURS] => Array
(
)
[TITLE] => From farm to stream: leveraging woody bioenergy crop diversity for sustainable water management
[COMPSTAGE] => Completed
[COMMENT] => Sarah participated in an NSF-funded project entitled, “REU Site: ecology and management for resilient and adapted forests" where she conducted research under my supervision.
[DTM_START] => June
[DTD_START] => Array
(
)
[DTY_START] => 2024
[START_START] => 2024-06-01
[START_END] => 2024-06-30
[DTM_END] => August
[DTD_END] => Array
(
)
[DTY_END] => 2024
[END_START] => 2024-08-01
[END_END] => 2024-08-31
[COMMUNITY_ENGAGEMENT] => Array
(
)
[MSU_MISSION] => Array
(
)
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[22] => Array
(
[@attributes] => Array
(
[id] => 244640587776
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[TYPE] => Doctoral Major Professor
[TYPE_OTHER] => Array
(
)
[INTERNATIONAL] => Array
(
)
[DSL_STUDENT] => Array
(
[@attributes] => Array
(
[id] => 244640587777
)
[FNAME] => Casey
[LNAME] => Iwamoto
)
[SHDEP] => Forestry
[COURSEPRE] => Array
(
)
[COURSENUM] => Array
(
)
[CHOURS] => Array
(
)
[TITLE] => Potential benefits of organic and microbial soil amendments on shortleaf pine (Pinus echinata) restoration
[COMPSTAGE] => Completed
[COMMENT] => November 16, 2023 - Oral Exams
April 26, 2024 - Dissertation Defense
[DTM_START] => January
[DTD_START] => Array
(
)
[DTY_START] => 2021
[START_START] => 2021-01-01
[START_END] => 2021-01-31
[DTM_END] => August
[DTD_END] => Array
(
)
[DTY_END] => 2024
[END_START] => 2024-08-01
[END_END] => 2024-08-31
[COMMUNITY_ENGAGEMENT] => Yes
[MSU_MISSION] => Yes
)
[23] => Array
(
[@attributes] => Array
(
[id] => 318502715392
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[TYPE] => Supervised Undergraduate Research
[TYPE_OTHER] => Array
(
)
[INTERNATIONAL] => Array
(
)
[DSL_STUDENT] => Array
(
[@attributes] => Array
(
[id] => 318502715393
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[FNAME] => John Mark
[LNAME] => Anderson
)
[SHDEP] => Forestry
[COURSEPRE] => FO
[COURSENUM] => 4800
[CHOURS] => Array
(
)
[TITLE] => Array
(
)
[COMPSTAGE] => Completed
[COMMENT] => John Mark is an undergraduate student (FO-FOMG, 2026) who works in my lab. He conducted soil inorganic carbon testing and determination under a USDA-funded project entitled, "Climate change mitigation assessment of Conservation Reserve Program practices with trees."
[DTM_START] => January
[DTD_START] => Array
(
)
[DTY_START] => 2024
[START_START] => 2024-01-01
[START_END] => 2024-01-31
[DTM_END] => May
[DTD_END] => Array
(
)
[DTY_END] => 2024
[END_START] => 2024-05-01
[END_END] => 2024-05-31
[COMMUNITY_ENGAGEMENT] => No
[MSU_MISSION] => Array
(
)
)
[24] => Array
(
[@attributes] => Array
(
[id] => 318439622656
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[TYPE] => Supervised Undergraduate Research
[TYPE_OTHER] => Array
(
)
[INTERNATIONAL] => Array
(
)
[DSL_STUDENT] => Array
(
[@attributes] => Array
(
[id] => 318439622657
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[FNAME] => Emily
[LNAME] => White
)
[SHDEP] => Forestry
[COURSEPRE] => FO
[COURSENUM] => 4800
[CHOURS] => Array
(
)
[TITLE] => Species level differences in carbon sequestration potential of trees in the southeast US
[COMPSTAGE] => Completed
[COMMENT] => Emily White is an undergraduate student (FO-ENCO, 2024) who works in my lab and is supported by the CFR/FWRC Undergraduate Research Scholars Program (2022-2024). She is conducting a field experiment to quantify differences in woody decomposition of common tree species in the southeastern US.
[DTM_START] => August
[DTD_START] => Array
(
)
[DTY_START] => 2023
[START_START] => 2023-08-01
[START_END] => 2023-08-31
[DTM_END] => May
[DTD_END] => Array
(
)
[DTY_END] => 2024
[END_START] => 2024-05-01
[END_END] => 2024-05-31
[COMMUNITY_ENGAGEMENT] => No
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[TITLE] => Assessing the flood tolerance, physiological mechanism, and nutrient mitigation potential of short rotation woody crops planted on the seasonally flooded marginal land of the Lower Mississippi Alluvial Valley
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[TITLE] => Regeneration Potential and Habitat Suitability Modeling of Three Imperiled Southeastern US Woody Plants
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[TITLE] => Effects of tree morphology on rainwater partitioning in an upland oak forest
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[TITLE] => Using deuterium and oxygen-18 stable isotopes to understand mechanisms of stemflow generation as a function of tree species and climate
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[TITLE] => The ecological significance of phyllosphere leaf traits on throughfall hydrology, biogeochemistry, and leaf litter quality among oak (Quercus spp.) species in the Southeastern United States
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[ABSTRACT] => AbstractAtlantic white-cedar (Chamaecyparis thyoides [L.] B.S.P.) is considered critically imperiled across much of its range. This species occurs in freshwater swamps, rarely further inland than 160 km from the Atlantic or Gulf Coasts and is susceptible to several natural and anthropogenic disturbances (i.e., tropical cyclones, fire, saltwater inundation, overharvesting). As the frequency and intensity of tropical storms increase, understanding the regeneration of Atlantic white-cedar will be critical to its conservation. This study evaluated the regeneration of Atlantic white-cedar 14 years after Hurricane Katrina. All Atlantic white-cedar ≥2.5 cm at breast height were inventoried within an ~9 ha study area located within Grand Bay National Wildlife Refuge in Jackson County, Mississippi, USA. Additionally, the competing woody vegetation was surveyed. After Hurricane Katrina, the number of Atlantic white-cedar stems increased by 191%. This long-term study provides the first analysis of Atlantic white-cedar regeneration post–tropical cyclone disturbance within the Gulf Coast and allows conservationists a better understanding of the effects of tropical cyclone disturbance on this species.
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[TITLE] => Mesophication of upland oak forests: Implications of species-specific differences in leaf litter decomposition rates and fuelbed composition
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[ABSTRACT] => AbstractKey messageHygroscopicity is a crucial element of bark water storage and can reach >60% of water holding capacity of bark depending on tree speciesAbstractBark forms the outer layer of woody plants, and it is directly exposed to wetting during rainfall and reacts to changes in relative humidity, i.e., it may exchange water with the atmosphere through absorption and desorption of water vapor. A current paradigm of bark hydrology suggests that the maximum water storage of bark empties between precipitation events and is principally controlled by bark thickness and roughness. We hypothesize that (1) the ability of bark to absorb water vapor during non-rainfall periods (i.e., hygroscopicity) leads to partial saturation of bark tissues during dry periods that may alter the rate of bark saturation during rainfall, and (2) the degree of bark saturation through hygroscopic water is a function of internal bark structure, including porosity and density, that varies among species. To address these questions, we conducted laboratory experiments to measure interspecific differences in bark physical structure as it relates to water storage mechanisms among common tree species (hickory (Caryaspp.), oak (Quercusspp.), sweetgum (Liquidambar styraciflua), and loblolly pine (Pinus taeda)) in the southeastern United States. Furthermore, we considered how these properties changed across total bark, outer bark, and inner bark. We found a distinct difference between hickory and oak, whereby hickory had 5.6% lower specific density, 31.1% higher bulk density, and 22.4% lower total porosity of outer bark resulting in higher hygroscopicity compared to oaks. For all species, hygroscopicity increased linearly with bulk density (R2 = 0.65–0.81) and decreased linearly with total porosity (R2 = 0.64–0.88). Overall, bark hygroscopicity may constitute an average of 30% of total bark water storage capacity. Therefore, in humid climates like those of the southeastern USA, the proportion of bark that remains saturated during non-storm conditions should not be considered negligible.
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[TITLE] => Comparisons of flux-based stemflow enrichment ratios for two Quercus spp. within the megalopolis of the eastern USA
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[ABSTRACT] => Throughfall and stemflow serve as two important transport mechanisms for water and solutes in urban forests, though these fluxes are seldom quantified within cities. This study is the first to utilize two flux-based enrichment ratios for stemflow to characterize spatial patterns in water and solute distribution in urban forest fragments. Using event-based, in situ sampling, this study quantified stemflow enrichment for Quercus rubra (northern red oak) and Quercus alba (white oak) trees relative to open precipitation (EP,B) and throughfall (ET,B) per unit trunk basal area for dissolved Ca, K, Mg, Mn, NO3-N, and S. The study investigated variability in nutrient enrichment at the fragment, municipal, and regional scales. Among all solutes, observations for EP,B and ET,B for Q. rubra and Q. alba were generally lowest for Mg and highest for Mn and K. Significant intra-urban variability in stemflow enrichment was limited to EP,B of K and ET,B of Ca (p < 0.05), while trans-regional variability in stemflow enrichment consistently indicated higher EP,B and ET,B in more highly developed portions of the study region. At the fragment scale, EP,B and ET,B for Q. rubra was consistently higher than for Q. alba, with variability in these observations significant for all solutes. For example, interspecific variability in EP,B was greatest for K, where median values ranged from 2.8 ± 29.7 in Q. alba to 87.1 ± 97.1 in Q. rubra. While observations for ET,B were generally lower than those for EP,B, observations for Q. rubra also consistently exceeded those for Q. alba, with median values for K ranging from 1.5 ± 0.5 to 21.9 ± 3.1 for Q. alba and Q. rubra, respectively. Findings were likely driven by variability in biophysical characteristics between the two species (e.g., bark morphology). Further, findings indicate that species heterogeneity within the urban forest contributes to significant variability in nutrient (and possibly pollutant) transport and fate via throughfall and stemflow below the canopy, with subsequent impacts on urban forest biogeochemistry.
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[PUBLISHER] => Proceedings of the 20th Biennial Southern Silvicultural Research Conference
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[ABSTRACT] => In upland oak (Quercus spp.) forests of the Eastern United States, shade-intolerant, fire-tolerant oaks are being replaced by shade-tolerant, fire-sensitive species due to changes in forest management and fire regimes. In these mixed-species forests, rainwater redistribution by the forest canopy is determined by tree
species traits as well as canopy position. To better understand how shifting forest composition could impact rainwater partitioning, we quantified differences in canopy structure and the resultant net flux of water to forest soils in a series of experiments across the Southeastern United States. Non-oak species had denser canopies
than oaks and intercepted more rainwater, reducing throughfall by more than 15 percent. Conversely, stemflow water inputs were more than four times greater beneath non-oaks, which had smoother bark compared to rougher-bark oaks. This study demonstrates the link between aboveground tree structure and interspecific water fluxes. It supports the hypothesis that a shift in forest composition could influence future ecosystem function in
southeastern upland oak forests.
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[TITLE] => Could canopy, bark, and leaf litter traits of encroaching non-oak species influence future flammability of upland oak forests?
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[TITLE] => Interspecific Differences in Canopy-Derived Water, Carbon, and Nitrogen in Upland Oak-Hickory Forest
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[ABSTRACT] => AbstractThe southeastern United States contains extensive loblolly pine (Pinus taeda L.) plantations at risk from bark beetle damage that can change ecosystem biogeochemical cycling. Functional changes in tree physiology have the potential to occur before visual evidence of mortality making them difficult to incorporate into ecosystem models. Therefore, we girdled loblolly pines to simulate bark beetle damage and measured physiological processes including sapflow rates, photosynthesis, litterfall, and needle nitrogen concentrations to determine the physiological changes occurring in trees undergoing mortality. We found that the girdling treatment took 5 months to significantly reduce sapflow rates but visual crown mortality occurred more than one year after girdling. Girdled pines had approximately 2.5 times lower water use than control pines and exhibited greater susceptibility to atmospheric water stress. Girdled and control pines had similar needle nitrogen concentrations and photosynthetic rates measured during the mortality year. However, more litterfall with higher nitrogen concentrations occurred in the mortality year than in the previous year, resulting in redistribution of carbon and nitrogen in the ecosystem. Overall, these data allow for better quantification of the effects of background disturbance levels and individual tree mortality on water, carbon, and nitrogen cycling within a loblolly pine ecosystem.
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[TITLE] => Do storm synoptic patterns affect biogeochemical fluxes from temperate deciduous forest canopies?
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[VOLUME] => 132
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[DOI] => 10.1007/s10533-017-0300-6
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[ABSTRACT] => Abstract
The volumetric quantity and biogeochemical quality of throughfall and stemflow in forested ecosystems are influenced by biological characteristics as well environmental and storm meteorological conditions. Previous attempts at connecting forest water and nutrient cycles to storm characteristics have focused on individual meteorological variables, but we propose a unified approach by examining the storm system in its entirety. In this study, we use methods from synoptic climatology to distinguish sub-canopy biogeochemical fluxes between storm events to understand the response of forest ecosystems to daily weather patterns. For solute inputs tied to atmospheric deposition (NH4+, NO3−, SO42−, Na+, Cl−), stagnant air masses resulted in high inputs in rainfall (273.42, 81.81, 52.30, 156.99, 128.70 μmol L−1), throughfall (355.05, 130.66, 83.24, 239.55, 261.32 μmol L−1), and stemflow (338.34, 182.75, 153.74, 125.75, 272.88 μmol L−1). For inputs tied to canopy exchange (DOC, K+, Ca2+, Mg2+), a clear distinction was observed between throughfall and stemflow pathways. The largest throughfall concentrations were in the Great Lakes Low (1794.80, 352.96, 72.75, 74.37 μmol L−1) while the largest stemflow concentrations were in the Weak Upper Trough (3681.78, 497.34, 82.36, 72.46 μmol L−1). Stemflow leaching is likely derived from a larger reservoir of leachable cations in the tree canopy than throughfall, with stemflow fluxes maximized during synoptic types with greater rainfall amounts and throughfall fluxes diluted. For flux-based enrichment ratios, water volume, storm magnitude, antecedent dry period, and seasonality were important factors, further illustrating the influence of synoptic characteristics on wash-off, leaching and, ultimately, dilution processes within the canopy.
[KEYWORDS] => Throughfall; Stemflow; Forest hydrology; Forest biogeochemistry ;Synoptic climatology
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[TITLE] => Interspecific ecological and meteorological controls on forest canopy-derived hydrology and biogeochemistry in the southeastern United States
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[PUBLISHER] => Proceedings of the 2016 Mississippi Water Resources Conference
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[AREA] => Forestry
[WEB_ADDRESS] => http://www.wrri.msstate.edu/pdf/2016_wrri_proceedings.pdf
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[ABSTRACT] => During storm events, as precipitation moves through the forest canopy it is transformed in both quantity and quality, thus delivering highly enriched water to the forest floor. Throughfall is spatially distributed beneath the forest canopy while stemflow is localized to the roots and soils in the immediate vicinity of individual tree trunks. Previous research has demonstrated that storm characteristics (e.g., intensity, duration, and magnitude), canopy structural parameters, and species composition have a significant control on canopy-derived nutrient fluxes. However, in the southeastern United States, contributions of the forest canopy to nutrient cycling have largely been overlooked, although the magnitude of tree biodiversity in the region separates these forests from their more-studied counterparts. Therefore, a field study was established in an oak-hickory forest in Mississippi to categorize the interspecific control on canopy-mediated nutrient cycling during precipitation events. Throughfall collectors and stemflow collars were located underneath the canopies of four oak (Shumard, Southern Red, Post, and White) and two hickory species (Shagbark and Pignut), with three replicates for each species. Hydrologic flux and nutrient samples were collected following individual precipitation events beginning in Fall 2014 and continue to present. Meteorological characteristics and precipitation chemistry were collected at a nearby open site.
Preliminary results indicate that stemflow volumetric flux was significantly different between species (p<0.001) but throughfall volumetric flux was not (p=0.624). Among the oak species, Shumard oak partitioned an average of 73.6% of incident precipitation into throughfall and 1.6% into stemflow, the largest among all species, with the remaining 24.8% partitioned into canopy interception. Mean concentrations of total nitrogen (TN) in throughfall were greatest in Shumard oak (1.44 mg/L) and post oak (1.39 mg/L) while stemflow concentrations were greatest in shagbark hickory (1.81 mg/L) and white oak (1.20 mg/L) and intermediate in Shumard oak (0.96 mg/L). Dissolved organic carbon (DOC) concentrations in throughfall were significantly different than precipitation (p=0.038) but not between species (p=0.342), while DOC concentrations in stemflow were significantly different than precipitation (p<0.001) and between species (p<0.001). Results suggest that Shumard oak canopies facilitate the largest hydrologic fluxes in oak-hickory forests that correspond to intermediate biogeochemical fluxes of nitrogen, enabling this species to directly modify the substrata and its growing conditions. Improved understanding of species-specific roles in nutrient cycles in highly diverse southern forests is critical to developing effective management strategies to mitigate shifts in species composition and ecosystem functions as regional climates change.
[KEYWORDS] => throughfall, stemflow, oak-hickory forests, dissolved organic carbon
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[TITLE] => Hickory leaf litter alters decomposition rates in upland oak forests of the southeastern U.S.
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[TITLE] => A comparison of five forest interception models using global sensitivity and uncertainty analysis
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[DOI] => DOI: 10.1016/j.jhydrol.2016.04.011
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[ABSTRACT] => Interception by the forest canopy plays a critical role in the hydrologic cycle by removing a significant portion of incoming precipitation from the terrestrial component. While there are a number of existing physical models of forest interception, few studies have summarized or compared these models. The objective of this work is to use global sensitivity and uncertainty analysis to compare five mechanistic interception models including the Rutter, Rutter Sparse, Gash, Sparse Gash, and Liu models. Using parameter probability distribution functions of values from the literature, our results show that on average storm duration [Dur], gross precipitation [PG], canopy storage [S] and solar radiation [Rn] are the most important model parameters. On the other hand, empirical parameters used in calculating evaporation and drip (i.e. trunk evaporation as a proportion of evaporation from the saturated canopy [∊], the empirical drainage parameter [b], the drainage partitioning coefficient [pd], and the rate of water dripping from the canopy when canopy storage has been reached [Ds]) have relatively low levels of importance in interception modeling. As such, future modeling efforts should aim to decompose parameters that are the most influential in determining model outputs into easily measurable physical components. Because this study compares models, the choices regarding the parameter probability distribution functions are applied across models, which enables a more definitive ranking of model uncertainty.
[KEYWORDS] => Interception; Sensitivity analysis; Uncertainty analysis; Canopy storage capacity
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[TITLE] => Synoptic typing: interdisciplinary application methods with three practical hydroclimatological examples
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[LNAME] => Siegert
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[FNAME] => Daniel
[MNAME] => J
[LNAME] => Leathers
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[FNAME] => Delphis
[MNAME] => F
[LNAME] => Levia
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[PUBLISHER] => Theoretical and Applied Climatology
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[VOLUME] => 128
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[PAGENUM] => 603-621
[DOI] => https://doi.org/10.1007/s00704-015-1700-y
[CRIS_NUM_CAT] => MISZ
[CRIS_NUM] => 069390
[AREA] => Environmental Systems and Sustainability
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[ABSTRACT] => Synoptic classification is a methodology that represents diverse atmospheric variables and allows researchers to relate large-scale atmospheric circulation patterns to regional- and small-scale terrestrial processes. Synoptic classification has often been applied to questions concerning the surface environment. However, full applicability has been under-utilized to date, especially in disciplines such as hydroclimatology, which are intimately linked to atmospheric inputs. This paper aims to (1) outline the development of a daily synoptic calendar for the Mid-Atlantic (USA), (2) define seasonal synoptic patterns occurring in the region, and (3) provide hydroclimatological examples whereby the cascading response of precipitation characteristics, soil moisture, and streamflow are explained by synoptic classification. Together, achievement of these objectives serves as a guide for development and use of a synoptic calendar for hydroclimatological studies. In total 22 unique synoptic types were identified, derived from a combination of 12 types occurring in the winter (DJF), 13 in spring (MAM), 9 in summer (JJA), and 11 in autumn (SON). This includes six low pressure systems, four high pressure systems, one cold front, three north/northwest flow regimes, three south/southwest flow regimes, and five weakly defined regimes. Pairwise comparisons indicated that 84.3 % had significantly different rainfall magnitudes, 86.4 % had different rainfall durations, and 84.7 % had different rainfall intensities. The largest precipitation-producing classifications were not restricted to low pressure systems, but rather to patterns with access to moisture sources from the Atlantic Ocean and easterly (on-shore) winds, which transport moisture inland. These same classifications resulted in comparable rates of soil moisture recharge and streamflow discharge, illustrating the applicability of synoptic classification for a range of hydroclimatological research objectives.
[KEYWORDS] => synoptic climatology, precipitation, hydroclimatology, soil moisture, streamflow, volumetric water content (VWC), Mid-Atlantic
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[SUB_START] => 2014-11-12
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[DTY_PUB] => 2016
[PUB_START] => 2016-01-15
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[TITLE] => Small-scale topographic variability influences tree species distribution and canopy throughfall partitioning in a temperate deciduous forest
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[FNAME] => Courtney
[MNAME] => M.
[LNAME] => Siegert
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[id] => 133363900419
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[FNAME] => Delphis
[MNAME] => F
[LNAME] => Levia
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[id] => 133363900420
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[FNAME] => Sean
[MNAME] => A
[LNAME] => Hudson
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[id] => 133363900421
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[FNAME] => Asia
[MNAME] => L
[LNAME] => Dowtin
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[4] => Array
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[id] => 133363900422
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[FNAME] => Fen
[MNAME] => Array
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[LNAME] => Zhang
[MSU_ID] => Array
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[id] => 133363900423
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[FNAME] => Myron
[MNAME] => J
[LNAME] => Mitchell
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[PUBLISHER] => Forest Ecology and Management
[PUBCTYST] => Array
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[VOLUME] => 359
[ISSUE] => Array
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[PAGENUM] => 109-117
[DOI] => 10.1016/j.foreco.2015.09.028
[CRIS_NUM_CAT] => MISZ
[CRIS_NUM] => 069390
[AREA] => Forestry
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[ABSTRACT] => At very large spatial scales, the impacts of topography, elevation, and aspect on throughfall variability are apparent. However, within relatively small catchments (<50 ha), differences in species composition induced by slight changes in elevation coupled with slope orientation, could result in sufficient canopy variability whereby throughfall hydrology would be definitively different across small gradients. This study aims to (1) quantify the differences in throughfall hydrology across small topographic gradients, (2) determine the variability of throughfall across such gradients, and (3) determine the seasonal effects on throughfall hydrology resulting from differences in species composition and growing niches.
Throughfall partitioning was measured during 15 sampling periods at 4 landscape positions including 3 hillslopes with aspects facing north (NF), west (WF), and south (SF) in addition to a flat area (F) situated in the center of a 12 ha deciduous catchment. Throughfall partitioning was significantly lower on the steepest SF plot (TF = 75.0%) than on the moderately sloping NF (TF = 83.9%, p = 0.001) and F (TF = 81.7%, p = 0.037) plots. SF also had the largest degree of throughfall variability (CV = 20.1), resulting from overlapping canopies, which led to higher rates of canopy interception. NF and WF plots exhibited the largest inter-seasonal differences with decreases in throughfall partitioning of 13.2% (p = 0.013) and 12.1% (p = 0.052), respectively, and corresponded to the largest differences in plant canopy indices (PAI) between seasons. Although slope and aspect were found to be distinguishing variables in our study, it was the influence of these variables on species composition that led to differences in throughfall quantity. Our study illustrates the systematic distribution of water resources across topographic positions within a relatively small forested catchment and highlights the need for additional consideration of topography-induced controls on microclimate and growing space, which ultimately influence water quality and quantity for effective management strategies.
[KEYWORDS] => Throughfall; Catchment topography; Forest hydrology; Deciduous forest
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[DTD_SUB] => 15
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[SUB_START] => 2015-06-15
[SUB_END] => 2015-06-15
[DTM_ACC] => September
[DTD_ACC] => 19
[DTY_ACC] => 2015
[ACC_START] => 2015-09-19
[ACC_END] => 2015-09-19
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[DTY_PUB] => 2016
[PUB_START] => 2016-01-01
[PUB_END] => 2016-01-01
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[STATUS] => Published
[TITLE] => Beryllium-7 wet deposition variation with storm height, synoptic classification, and tree canopy state in the mid-Atlantic USA
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[FNAME] => Diana
[MNAME] => L
[LNAME] => Karwan
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[FNAME] => Courtney
[MNAME] => M.
[LNAME] => Siegert
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[FNAME] => Delphis
[MNAME] => F
[LNAME] => Levia
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[FNAME] => James
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[LNAME] => Pizzuto
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[FNAME] => Julia
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[LNAME] => Marquard
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[id] => 133363787783
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[FNAME] => Rolfe
[MNAME] => Array
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[LNAME] => Aalto
[MSU_ID] => Array
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[FNAME] => Anthony
[MNAME] => K
[LNAME] => Aufdenkampe
[MSU_ID] => Array
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[DEP] => Array
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[PUBLISHER] => Hydrological Processes
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[VOLUME] => 30
[ISSUE] => 1
[PAGENUM] => 75-89
[DOI] => DOI: 10.1002/hyp.10571
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[ABSTRACT] => Short-lived fallout isotopes, such as beryllium-7 (7Be), are increasingly used as erosion and sediment tracers in watersheds. 7Be is produced in the atmosphere and delivered to the Earth's surface primarily in precipitation. However, relatively little has been published about the variation in 7Be wet deposition caused by storm type and vegetation cover. Our analysis of precipitation, throughfall, and sediments in two forested, headwater catchments in the mid-Atlantic USA indicates significant variation in isotope deposition with storm type and storm height. Individual summer convective thunderstorms were associated with 7Be activity concentrations up to 5.0 Bq l−1 in precipitation and 4.7 Bq l−1 in throughfall, while single-event wet depositional fluxes reached 168 Bq m−2 in precipitation and 103 Bq m−2 in throughfall. Storms originating from the continental USA were associated with lower 7Be activity concentrations and single-event wet depositional fluxes for precipitation (0.7–1.2 Bq l−1 and 15.8–65.0 Bq m−2) and throughfall (0.1–0.3 Bq l−1 and 13.5–98.9 Bq m−2). Tropical systems had relatively low activity concentrations, 0.2–0.5 Bq l−1 in precipitation and 0.2–1.0 Bq l−1 in throughfall, but relatively high single-event depositional fluxes due to large rainfall volumes, 32.8–67.6 Bq m−2 in precipitation and 25.7–134 Bq m−2 in throughfall. The largest sources of 7Be depositional variation were attributed to storm characteristics including precipitation amount and maximum storm height. 7Be activity associated with fluvial suspended sediments also exhibited the highest concentration and variability in summer (175–1450 Bq kg−1). We conclude the dominant source of variation on event-level 7Be deposition is storm type. Our results illustrate the complex relationships between 7Be deposition in precipitation and throughfall and demonstrate event-scale relationships between the 7Be in precipitation and on suspended sediment.
[KEYWORDS] => beryllium-7; wet deposition; precipitation; sediment fingerprinting; throughfall; storm type
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[DTD_SUB] => 1
[DTY_SUB] => 2014
[SUB_START] => 2014-06-01
[SUB_END] => 2014-06-01
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[DTD_ACC] => 5
[DTY_ACC] => 2015
[ACC_START] => 2015-06-05
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[DTY_PUB] => 2015
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[TITLE] => Seasonal and meteorological effects on differential stemflow funneling ratios for two deciduous tree species
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[id] => 133364000769
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[FACULTY_NAME] => 1600624
[FNAME] => Courtney
[MNAME] => M.
[LNAME] => Siegert
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[FNAME] => Delphis
[MNAME] => F
[LNAME] => Levia
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[PUBLISHER] => Journal of Hydrology
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[VOLUME] => 519
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[PAGENUM] => 446-454
[DOI] => 10.1016/j.jhydrol.2014.07.038
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[ABSTRACT] => Stemflow is an important subcanopy flux that delivers enriched rainfall to soils immediately surrounding a tree. Stemflow volume represents the quantity of this hydrologic flux while funneling ratio (FR) represents the efficiency with which individual trees scavenge water during rainfall events. Stemflow hydrology and storm meteorological characteristics were monitored from 2007 through 2012 to determine the interspecific differences in stemflow flux with a focus on FR efficiency. The objective of this study was to examine the influence of tree species and size on stemflow FR, determine how seasonality affects stemflow FR, and quantify the role of storm meteorological conditions on stemflow FR. The results presented in this paper build upon 2 years of previous hydrologic research from the Fair Hill, MD field site, which strengthen previous findings via larger storm sample size and highlight more complex stemflow hydrologic relationships than originally assumed. Specifically, this study has demonstrated (1) the efficiency with which smaller trees gain access to rainfall via higher FR than larger trees, (2) the FR variability of F. grandifolia induced by the species’ ease of generating stemflow under many storm conditions, and (3) the necessity of many years of hydrometeorological sampling to capture long-term rainfall characteristics and trends. The efficiency of smaller trees to preferentially funnel water to their tree base has implications for forests undergoing change. Forest disturbance and subsequent regrowth is dominated by smaller trees, but additional research is necessary to understand how saplings compete among one another to gain access to stemflow and how this may be influenced by changing climates and forest composition.
[KEYWORDS] => Stemflow; Funneling ratio; Canopy-derived flux; Eastern deciduous forest
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[SUB_START] => 2014-05-14
[SUB_END] => 2014-05-14
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[DTD_ACC] => 19
[DTY_ACC] => 2014
[ACC_START] => 2014-07-19
[ACC_END] => 2014-07-19
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[DTD_PUB] => 30
[DTY_PUB] => 2014
[PUB_START] => 2014-07-30
[PUB_END] => 2014-07-30
[USER_REFERENCE_CREATOR] => Yes
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[STATUS] => Published
[TITLE] => Stomatal conductance and transpiration of co-occurring seedlings with varying shade tolerance
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[FNAME] => Courtney
[MNAME] => M.
[LNAME] => Siegert
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[PUBLISHER] => Trees
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[VOLUME] => 25
[ISSUE] => 6
[PAGENUM] => 1091-1102
[DOI] => 10.1007/s00468-011-0584-4
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