Carbon Dynamics Project Overview

 

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Principle Investigators

Stephen Roxburgh (ANU, CRCGA)

Brendan Mackey (ANU, CRCGA)

Chris Dean (formerly CRCGA)

Jenet Austin (formerly BRS/CRCGA, now CSIRO)

Lucy Randall (BRS, CRCGA)

Alex Lee (ANU, CRCGA)

John Gallant (CSIRO)

Richard Lucas (UWA)

 

Introduction

The Carbon Dynamics project was initiated in 2002 as part of the CRC for Greenhouse Accounting (CRCGA) collaborative initiative to promote interaction among CRCGA research activities.  The study has been developing a carbon accounting framework in the forest and woodland ecosystems near Injune, central Queensland, which incorporates land cover, land management and land use history for the period 1970-2000.

 

This project is investigating carbon dynamics at a range of scales; from individual plants to plot and site scale using field observations, remotely sensed data and landscape-scale digital terrain analysis

 

Overarching questions/goals –   

 

1.   Assessment of the contribution of landscape-scale patterns and processes to variability in carbon accounts

 

2.   Development of methods for extrapolating measurements made at site/local levels to larger scales

 

3.   To bring together various sources of information within a single analysis framework, allowing assessment of the C accounts within the study landscape, and exploration of the greenhouse implications of different management decisions

 

This study investigates the impact of land cover change on the dynamics of carbon within a semi-arid woodland in central Queensland, Australia. The study landscape (Figure 1) is managed predominantly for beef production, where growth of the understorey forage plants is enhanced through anthropogenic reduction of the overstorey tree cover. A wide range of methods has been used to reduce tree cover, which range from ring-barking and herbicide injection, through to complete mechanical removal of the tree overstorey and conversion to pasture (Land Cover Change project).


 

Figure 1. Location of the study area in Queensland. 

 

The dots in the State map indicate previous soil sampling sites on uncultivated soils.  Our study site fills a gap in the sampling of the state.  Click here to see the study area location in more detail (study area page)

 

 

Methods

 

Field:

 

Field survey was used to estimate standing stocks of carbon in above-ground vegetation, coarse woody debris, fine litter, and in the soil down to a depth of 1m (Figure 3 below). These data were combined with historical records (satellite imagery, aerial photography and landholder interviews) to determine the disturbance histories of each site.  Click here for a more detailed description of the land cover history analysis under the Land Cover project (Land Cover Change project)

 

Sampling for…

 

Fine litter

Fine litter was collected within 1m quadrats and placed into plastic bags.  Later in the lab this was sorted into leaves, twigs and bark, and then dried in a large oven for 48 hours. Sub-samples of each fraction were analysed for %C content, and these were used to convert total dry weight into carbon mass.

 

Coarse woody debris

Coarse woody debris estimates for the plot area are made using two transects within the field plot.  The transects go from the middle point between the south west and south east corners, and run to the north east and north west corners respectively

 

Whenever the transect tape crosses a piece of wood that is larger than 2cm diameter, a number of attributes of the wood are recorded.  These are:

-          diameter of the wood where the tape crosses

-          tree species, if known

-          how old (or rotten) the piece of wood is, in 5 broad classes (ie from fresh wood, through to rotten / falling apart)

-          the distance along the tape that the wood is found

 

Some pieces of wood are collected and taken back to the lab, so we can work out how dense they are, and then how much carbon is stored in the wood.

 

 

 

Soil carbon and bulk density sampling

The soil is collected at a number of points,  from the surface, and down to 1 metre depth. 

 

The surface sample is collected using a hand sampling tool.

The soil (or sand) is cleared from around the sample, to make getting it out easier.

The sample is then extracted and put into a bag

We use soil augers to obtain samples from 10cm down to 1m below the surface.  This is much easier in sandy soils than in clays!

Whacking the soil auger, which has a special collection head on it, collects the samples. We then pull out the auger and bag the sample.

The Ph (or acidity) of the soil is also tested at different depths.

 

 

I suggest not including this figure, as none of this data has been published yet, and it seems a bit detailed to have on a web-page overview. What do you think? MODELLING:

A model of terrestrial carbon dynamics was custom-designed to integrate the available empirical information (Figure 3 & 4). Model parameters, such as the residency times of carbon in the various pools, were estimated using model inversion methods. This technique takes the observed carbon stocks (mean & variance), and then searches, by genetic algorithm function minimisation, for parameter combinations that yield modelled carbon stocks that match those observations. Model parameters are therefore described by probability distributions, rather than constant values, allowing variability in the empirical observations to be propagated through the model. Once the parameters have been estimated, the model can be re-inverted and run forward through time as in a conventional simulation. The Injune model is being developed using the CRC for Greenhouse Accounting’s model simulation environment COINS (Comparison and Integration Shell).

 

 

 

Figure 3. General model of terrestrial carbon dynamics

 

 

 

Figure 4. Detailed model of terrestrial carbon dynamics for the Injune study.

 

Each month new growth (NPP) is partitioned into grass (forage) and tree vegetative components, and then eventually into the litter and soil. Soil dynamics are modelled using the Rothamsted soil model (RothC), which has been calibrated for Australian conditions. The boxes represent stores of carbon, and the arrows the fluxes.

 

 

Model behaviour / results

 

Two versions of the model are being developed.

 

- Point (site-based) model

This version allows the greenhouse impacts of various management activities to be assessed,  at the scale of individual study sites

 

- Spatial analyses

This version will use the biomass relationships developed by Alex Lee, the land-cover analyses of Lucy Randall, and the landscape/topographic analyses of John Gallant/Brendan Mackey to interpolate the site model over the whole landscape. This will allow landscape-scale carbon dynamics for the Injune region to be explored, and also provides a tool for scenario development.

 

Figure 5a shows the dynamics of the site model under constant environmental conditions, using a representative parameter set derived from the inverse modelling. A clearing event (simulated chaining combined with fire) at year 67 leads to increased herbage growth, which declines over time as the woody vegetation recovers. Note that the field observations (black dots) were not part of the calibration process, and hence provide an independent validation of the model behaviour. Figure 5b additionally includes climatic variability. Note the large variability in herbaceous plant growth, reflecting extreme inter-annual variability in rainfall.

 

A

B

 

Figure 5a & 5b. Model dynamics under constant (A) and fluctuating (B) environmental conditions

 

Current work is concentrating on finalising the development of the site model, and on developing the spatial analyses to facilitate spatial application of the model.

 

 

SUMMARY:

The analytical methods we are developing provide a formalised methodology for linking data with models, ensuring that all relevant empirical datasets are included in the model calibration process. More generally, the Carbon Dynamics project provides the means for bringing together results from a number of the Injune activities, thus allowing the quantification of current carbon stocks and fluxes across the entire study area, including a scenario capability for assessing the greenhouse implications of management decisions in this important Australian vegetation type.

 

 

 

Further Information

 

Stephen Roxburgh

CRC for Greenhouse Accounting & Ecosystem Dynamics Group

Research School of Biological Sciences

Australian National University

Canberra,

ACT 0200

Australia

 

Ph: +61 (02) 6125 5588

Fax: + 61 (02) 6125 5095

Email: Roxburgh@rsbs.anu.edu.au

 

 

Click here for a list of Conference presentations