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

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 (C_A) mandate techniques for examining impacts on terrestrial ecosystems. Most experiments examine only two or a few levels of C_A concentration and a single soil type, but if C_A 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 C_A 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 C_A enrichment, successfully discerns the shape of ecosystem responses to subambient to superambient C_A 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 (C_A) has recently increased past 400 µl L^-1 from approximately 270 µl L^-1 prior to the Industrial Revolution. C_A is forecast to reach at least 550 µl L^-1 by 2100¹. This rate of increase surpasses any C_A changes observed over the last 500,000 years. The unprecedented rate of change in C_A raises the possibility of non-linear or threshold responses of ecosystems to increasing C_A. Most ecosystem-scale C_A enrichment experiments apply only two treatments, a single level of enriched C_A and a control. These experiments have greatly expanded our understanding of the ecosystem impacts of C_A enrichment. However, an alternate approach that can reveal the presence of non-linear ecosystem responses to increasing C_A is to study ecosystems across a continuous range of subambient to superambient C_A. Subambient C_A is difficult to maintain in the field, and has most often been studied using growth chambers². Superambient C_A has been studied using growth chambers, open-top chambers, and free-air enrichment techniques^{3, 4}.

C_A enrichment occurs across landscapes containing many soil types. Soils properties can strongly affect ecosystem responses to C_A enrichment. For example, soil texture determines the retention of water and nutrients in the soil profile⁵, their availability to plants⁶, and the amount and quality of organic matter^7-9. The availability of soil moisture is a crucial mediator of ecosystem responses to C_A enrichment in water limited systems, including most grasslands¹⁰. Past field C_A enrichment experiments have typically examined only one soil type, and controlled tests of continuously varying C_A enrichment over several soil types are lacking. If effects of C_A enrichment on ecosystem processes differ with soil type, there is strong reason to expect spatial variation in ecosystem responses to C_A enrichment and ensuing changes in climate^{11, 12}.

The Lysimeter Carbon Dioxide Gradient (LYCOG) facility was designed to address questions of spatial variation in non-linear and threshold responses of ecosystems to C_A levels ranging from ~ 250 to 500 µl L^-1. LYCOG creates the prescribed gradient of C_A on perennial grassland plant communities growing on soils representing the broad range of texture, N and C contents, and hydrologic properties of grasslands in the southern portion of the U.S. Central Plains. Specific soils series used in the facility are Houston Black clay (32 monoliths), a Vertisol (Udic Haplustert) typical of lowlands; Austin (32 monoliths), a high carbonate, silty clay Mollisol (Udorthentic Haplustol) typical of uplands; and Bastsil (16 monoliths), an alluvial sandy loam Alfisol (Udic Paleustalf).

The operational principle employed in LYCOG is to harness the photosynthetic capacity of plants to deplete C_A from parcels of air moved directionally through the enclosed chambers. The treatment objective is to maintain a constant linear daytime gradient in C_A from 500 to 250 µl L^-1. To accomplish this, LYCOG consists of two linear chambers, a superambient chamber maintaining the portion of the gradient from 500 to 390 (ambient) µl L^-1 C_A, and a subambient chamber maintaining the 390 to 250 µl L^-1 portion of the gradient. The two chambers are located side by side, oriented on a north-south axis. The C_A gradient is maintained during the portion of the year when vegetation photosynthetic capacity is adequate; typically from late April to early November.

The chambers contain sensors and instrumentation needed to regulate the C_A gradient, control air temperature (T_A) near ambient values, and apply uniform precipitation amounts to all soils. Soils are intact monoliths collected from nearby Blackland prairie installed in hydrologically-isolated weighing lysimeters instrumented to determine all components of the water budget. Water is applied in events of volume and timing that approximate the seasonality of rain events and amounts during an average precipitation year. Thus, LYCOG is capable of evaluating the long-term effects of subambient to superambient C_A and soil type on grassland ecosystem function including water and carbon budgets.

LYCOG is the third generation of C_A gradient experiments conducted by USDA ARS Grassland Soil and Water Research Laboratory. The first generation was a prototype subambient to ambient gradient that established the viability of the gradient approach¹³ and advanced our understanding of leaf-level physiological responses of plants to subambient variation in C_A^14-20. The second generation was a field-scale application of the concept to perennial C₄ grassland, with the gradient extended to 200 to 550 µL L^{-1 21}. This field-scale experiment provided the first evidence that grassland productivity increases with C_A enrichment may saturate near current ambient concentrations²⁰, in part because nitrogen availability may limit plant productivity at superambient C_A²². LYCOG extends this second generation experiment by incorporating replicated soils of varying texture, allowing robust testing for interactive effects of soils on the C_A response of grassland communities.

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-residual herbicide, such as glyphosate.

2. Establish Plant Communities on Soil Monoliths

1. Plant the monoliths with eight seedlings each of seven species of tallgrass prairie grasses and forbs, for a total density of 56 plants per m².
   1. Plant the following Grasses: Bouteloua curtipendula (side-oats grama), Schizachyrium scoparium (little bluestem), Sorghastrum nutans (Indiangrass), Tridens albescens (white tridens)].
   2. Plant the following Forbs: Salvia azurea (pitcher sage), Solidago canadensis (Canada goldenrod), Desmanthus illinoensis (Illinois bundleflower, a legume).
2. Plant seedlings in a Latin Square design, re-randomized for each monolith.
3. Water the transplants for approximately 2 months following planting. The goal is to minimize water stress during initial establishment. Use any convenient method such as a hand wand or garden sprinkler. The frequency of watering depends on local climate and weather, particularly the occurrence of ambient rainfall.
4. Following the initial transplant establishment phase, maintain the transplants under ambient rainfall for as long as necessary while chambers (Section 3) are constructed. Remove unwanted species that emerge in the monoliths during establishment by hand-weeding.

3. Chamber Design

1. Construct two chambers each 1.2 m wide, 1.5 m tall, and 60 m long, divided into ten 5 m long sections. Construct sections from heavy steel of dimensions 5 m x 1.2 m x 1.6 m deep, buried to 1.5 m.
   1. Install four monoliths in each section, two monoliths each of two of the soil types, in random order. Install each monolith atop a 4,540 kg capacity balance.
   2. Include Bastsil monoliths in the pairings in even numbered sections.
2. Join adjacent sections aboveground with a 1 m long x 1 m wide x 0.3 m tall sheet-metal duct to provide a pathway for airflow.
   1. Supply coolant at 10 °C from a 161.4 kW refrigeration unit to a cooling coil inside each duct.
   2. Enclose the vegetation with clear greenhouse film (thickness 0.006”/.15 mm), such as used in other climate manipulation experiments²³.
   3. Fit each cover with a zippered opening backed by a draft flap to allow access to the monoliths for sampling.
   4. Remove the polyethylene covers at the end of the growing season.

4. CO ₂ and Air Temperature Measurement; Temperature Control

1. Sample entry and exit C_A on both chambers every 2 min through filtered air sample lines located at the entry and exit of superambient and subambient chambers. These data inform CO₂ injection and fan speed control.
   1. Sample C_A and water vapor content, and measure air temperature (T_A) at the entry and exit of each 5 m section at 20 min intervals.
   2. Measure all air samples for CO₂ and water vapor content in real time using infrared gas analyzers according to manufacturer’s protocol.
   3. Measure T_A at the entry, midpoint, and exit of each section with shielded fine wire thermocouples.
2. Regulate the flow of coolant through the cooling coil at the entrance of each section to maintain a consistent mean (mid-section) T_A from section to section near the ambient T_A.
3. Position a quantum sensor to have an unobstructed view of the sky and measure photosynthetic photon flux density according to manufacturer’s protocol. Light level is an input to the blower control algorithm.

5. C _A Treatment Application

1. Daytime
   1. Mix pure carbon dioxide (CO₂) with incoming ambient air to 500 µl L^-1 C_A, using a mass flow controller in the entrance duct of the superambient leg. See Section 4 for C_A measurement details.
   2. Advect the enriched air through the chambers using blower fans at the entrance to section 1 and in downstream sections.
   3. Maintain the desired exit C_A of 390 µl L^-1 (ambient air) by adjusting the blower speed.
      1. Increase the blower speed if the exit C_A is below the set point. This allows less time for plant uptake of CO₂, resulting in higher exit C_A.
      2. Decrease the blower speed if exit C_A is above the set point.
   4. Use the same approach in the subambient chamber except introduce ambient air and control to achieve exit C_A of 250 µl L^-1.
2. Nighttime
   1. Reverse the direction of air flow.
   2. Inject CO₂ into the daytime exit end of the superambient chamber to achieve 530 µl L^-1 C_A, and control advection rates to maintain 640 µl L^-1 at the nighttime exit (daytime entrance.
   3. Introduce ambient air at ~ 390 µl L^-1 CO₂ into the nighttime entrance (daytime exit) of the subambient chamber and control advection rate to maintain 530 µl L^-1 at the nighttime exit.

6. Precipitation Inputs

1. Apply the mean growing season rainfall amount to each monolith.
   1. Supply water to each monolith from a domestic water source through a drip irrigation system. Schedule the irrigation events and application amounts to approximate the seasonal rainfall pattern for the experiment location. The exact schedule depends on local climate.
2. Control application timing with a data logger and measure application volumes with flowmeters.

7. Sampling 

1. Measure vertical profiles of volumetric soil water content (vSWC) weekly during the period of CO₂ control, with a neutron attenuation gauge or other appropriate probe.
   1. Recommended profile increments are 20 cm depth increments to 1 m depth, and one 50 cm increment below a 1 m.
2. Measure monolith aboveground net primary productivity (ANPP) by harvesting all standing aboveground biomass at the end of the growing season.
   1. All aboveground biomass is removed each year, consequently standing biomass represents current primary production.
   2. Sort the sampled biomass by species, dry to constant mass, and weigh.
   3. Use biomass of individual species to quantify plant species contributions to ANPP.

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 C_A concentration from 500 to 250 µl L^-1 (Figure 2) with only a small discontinuity in C_A between the exit of the enriched chambers (Monolith 40) and the entrance of the subambient portion of the gradient (Monolith 41).

Air temp...

Discussion

The LYCOG facility achieves its operational goal of maintaining a 250 to 500 µl L^-1 continuous gradient of C_A concentrations on experimental grassland communities established on three soil types. The change in C_A 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...

Materials

List of materials used in this article

Name	Company	Catalog Number	Comments
Dataloggers, multiplexers	Campell Scientific, Logan, UT, USA	CR-7, CR-10, CR-21X, SDM-A04, SDM-CD16AC, AM25T
Thermocouples: Copper-constantan	Omega Engineering, Inc., Stamford, CT, USA	TT-T-40-SLE, TT-T-24-SLE
Quantum sensor	Li-Cor Biosciences, Lincoln, NE, USA	LI-190SB
CO2/H2O analyzer	Li-Cor Biosciences, Lincoln, NE, USA	LI-7000
Lysimeter scales	Avery Weigh-Tronix, Houston, TX, USA	DSL-3636-10
Air sampling pump	Grace Air Components, Houston, TX, USA	VP 0660
Dew-point generator	Li-Cor Biosciences, Lincoln, NE, USA	LI-610
Cold water chiller	AEC Application Engineering, Wood Dale, IL, USA	CCOA-50
Chilled water flow control values	Belimo Air Controls, Danbury, CT, USA	LRB24-SR
Chilled-water cooling coils	Coil Company, Paoli, PA, USA	WC12-C14-329-SCA-R
Carbon dioxide refrigerated liquid	Temple Welding Supply, Temple, TX, USA	UN2187
Polyethylene film	AT Plastics, Toronto, ON, Canada	Dura-film Super Dura 4
Blower motor/controller	Dayton Electric, Lake Forest, IL, USA	2M168C/4Z829
Solenoids	Industrial Automation, Cornelius, NC, USA	U8256B046V-12/DC
Leachate collection pump	Gast Manufacturing, Benton Harbor, MI, USA	0523-V191Q-G588DX