Water, Air, & Soil Pollution

, 229:380 | Cite as

Photoperiod and Soil Munition Constituent Effects on Phytoaccumulation and Rhizosphere Interactions in Boreal Vegetation

  • Ryan R. BusbyEmail author
  • Robyn A. Barbato
  • Carina M. Jung
  • Kate A. Morozova
  • Anthony J. Bednar
  • Andrew L. Bray
  • Jenifer M. Milam
  • Jared C. Smith
  • Karl J. Indest


Permafrost thaw is expected to alter biogeochemistry and hydrology, potentially increasing the mobility of soil constituents. Northern latitude boreal forests where permafrost thaw is occurring also experience extreme changes in day length during the growing season. As the effects of photoperiod on plant uptake of soil constituents or interactions with the rhizosphere are unknown, our objective was to determine these interactions with three plant species from different functional groups. A tree, forb, and grass common to military training ranges in this region were grown in soil spiked with or without lead, antimony, or 2,4-dinitrotoluene and grown under 16, 20, or 24 h of light. Plant biomass, soil constituent uptake, and rhizosphere bacterial communities were compared between treatments. Photoperiod had no effect on plant uptake of any soil constituent or on rhizosphere community, indicating that plants and their associated microbial communities adapted to this environment are resilient to extremes in photoperiod. Lead uptake was not significant in any plant species and had no effect on the rhizosphere. Antimony increased the percentage composition of Saprospirales in the rhizospheres of two of the three plants, indicating an interaction between this bacterial order and antimony. Antimony uptake by white spruce (Picea glauca) was considerable, with a mean concentration of 1731 mg kg−1 in roots, while mean shoot concentration was only 155 mg kg−1, indicating its potential to phytostabilize this heavy metal. Although antimony had the strongest impact on the rhizosphere bacterial community, it was also readily accumulated by the grass and tree.


Phytostabilization Rhizosphere Antimony Lead Picea Photoperiod Oxytropis 



The authors would like to thank Sarah Kania and Kristian Hopkins (University of Illinois) and Tom Douglas, Chris Hiemstra, and David Ringelberg (US Army Cold Regions Research and Engineering Laboratory) for their assistance in multiple aspects of this study.

Funding Information

This research was funded by the U.S. Army Corps of Engineers’ Environmental Quality Program.


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Copyright information

© This is a U.S. Government work and not under copyright protection in the US; foreign copyright protection may apply 2018

Authors and Affiliations

  • Ryan R. Busby
    • 1
    Email author return OK on get
  • Robyn A. Barbato
    • 2
  • Carina M. Jung
    • 3
  • Kate A. Morozova
    • 1
  • Anthony J. Bednar
    • 3
  • Andrew L. Bray
    • 3
  • Jenifer M. Milam
    • 3
  • Jared C. Smith
    • 3
  • Karl J. Indest
    • 3
  1. 1.US Army Construction Engineering Research LaboratoryChampaignUSA
  2. 2.US Army Cold Regions Research and Engineering LaboratoryHanoverUSA
  3. 3.US Army Environmental LaboratoryVicksburgUSA

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