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Method Article

A CO2 Concentration Gradient Facility for Testing CO2 Enrichment and Soil Effects on Grassland Ecosystem Function

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DOI:

10.3791/53151

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November 21st, 2015

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In This Article

Summary

The Lysimeter Carbon Dioxide Gradient Facility creates a 250 to 500 µl L-1 linear carbon dioxide gradient in temperature-controlled chambers housing grassland plant communities on clay, silty clay, and sandy soil monoliths. The facility is used to determine how past and future carbon dioxide levels affect grassland carbon cycling.

Abstract

Continuing increases in atmospheric carbon dioxide concentrations (CA) mandate techniques for examining impacts on terrestrial ecosystems. Most experiments examine only two or a few levels of CA concentration and a single soil type, but if CA can be varied as a gradient from subambient to superambient concentrations on multiple soils, we can discern whether past ecosystem responses may continue linearly in the future and whether responses may vary across the landscape. The Lysimeter Carbon Dioxide Gradient Facility applies a 250 to 500 µl L-1 CA gradient to Blackland prairie plant communities established on lysimeters containing clay, silty clay, and sandy soils. The gradient is created as photosynthesis by vegetation enclosed in in temperature-controlled chambers progressively depletes carbon dioxide from air flowing directionally through the chambers. Maintaining proper air flow rate, adequate photosynthetic capacity, and temperature control are critical to overcome the main limitations of the system, which are declining photosynthetic rates and increased water stress during summer. The facility is an economical alternative to other techniques of CA enrichment, successfully discerns the shape of ecosystem responses to subambient to superambient CA enrichment, and can be adapted to test for interactions of carbon dioxide with other greenhouse gases such as methane or ozone.

Introduction

Atmospheric carbon dioxide concentration (CA) has recently increased past 400 µl L-1 from approximately 270 µl L-1 prior to the Industrial Revolution. CA is forecast to reach at least 550 µl L-1 by 21001. This rate of increase surpasses any CA changes observed over the last 500,000 years. The unprecedented rate of change in CA raises the possibility of non-linear or threshold responses of ecosystems to increasing CA. Most ecosystem-scale CA enrichment experiments apply only two treatments, a single level of enriched CA and a control. ....

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Protocol

1. Collect Soil Monoliths to be used as Weighing Lysimeters

  1. Construct open-ended steel boxes 1 x 1 m square by 1.5 m deep from 8 mm thick steel.
  2. Press the open-ended boxes vertically into the soil, using hydraulic presses mounted on helical anchors drilled 3 m deep into the soil.
  3. Excavate the encased monolith using a backhoe or similar equipment.
  4. Place a fiberglass wick in contact with soil at the base of the monolith. Pass the wick through the steel base into a 10 L reservoir to drain the monolith, and then weld the steel base onto the bottom of the box.
  5. Kill existing vegetation on the monoliths by applying a non-re....

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Results

The superambient and subambient portions of the gradient are maintained in separate chambers (Figure 1). However, over seven years of operation (2007 – 2013), the chambers maintained a linear gradient in CA concentration from 500 to 250 µl L-1 (Figure 2) with only a small discontinuity in CA between the exit of the enriched chambers (Monolith 40) and the entrance of the subambient portion of the gradient (Monolith 41).

Air temp.......

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Discussion

The LYCOG facility achieves its operational goal of maintaining a 250 to 500 µl L-1 continuous gradient of CA concentrations on experimental grassland communities established on three soil types. The change in CA is linear over the prescribed range. Air temperature increased within each section, but was reset by the between-section cooling coils in most sections. As a result, the operational goal of maintaining a consistent mean temperature from section to section was met over most o.......

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Disclosures

The authors have nothing to disclose.

Acknowledgements

We thank Anne Gibson, Katherine Jones, Chris Kolodziejczyk, Alicia Naranjo, Kyle Tiner, and numerous students and temporary technicians for operating the LYCOG facility, conducting sampling, and data processing. L.G.R. acknowledges USDA-NIFA (2010-65615-20632).

....

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Materials

List of materials used in this article
NameCompanyCatalog NumberComments
Dataloggers, multiplexersCampell Scientific, Logan, UT, USACR-7, CR-10, CR-21X, SDM-A04, SDM-CD16AC, AM25T
Thermocouples: Copper-constantanOmega Engineering, Inc., Stamford, CT, USATT-T-40-SLE, TT-T-24-SLE
Quantum sensorLi-Cor Biosciences, Lincoln, NE, USALI-190SB
CO2/H2O analyzerLi-Cor Biosciences, Lincoln, NE, USALI-7000
Lysimeter scalesAvery Weigh-Tronix, Houston, TX, USADSL-3636-10
Air sampling pumpGrace Air Components, Houston, TX, USAVP 0660
Dew-point generatorLi-Cor Biosciences, Lincoln, NE, USALI-610
Cold water chillerAEC Application Engineering, Wood Dale, IL, USACCOA-50
Chilled water flow control valuesBelimo Air Controls, Danbury, CT, USALRB24-SR
Chilled-water cooling coilsCoil Company, Paoli, PA, USAWC12-C14-329-SCA-R
Carbon dioxide refrigerated liquidTemple Welding Supply, Temple, TX, USAUN2187
Polyethylene filmAT Plastics, Toronto, ON, CanadaDura-film Super Dura 4
Blower motor/controllerDayton Electric, Lake Forest, IL, USA2M168C/4Z829
SolenoidsIndustrial Automation, Cornelius, NC, USAU8256B046V-12/DC
Leachate collection pumpGast Manufacturing, Benton Harbor, MI, USA0523-V191Q-G588DX

References

  1. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Climate Change 2013: The Physical Science Basis. , Cambridge University Press. 1535(2013).
  2. Gerhart, L. M., Ward, J. K. Plant responses to low CO2 of the past. New Phytol. 188 (3), 674-695 (2010).
  3. Kimball, B. A.

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