Map of the world
Agriculture
Ecology and land management
Humanitarian interventions
Applied Meteorology
Aquatic environment
Regional and city planning
  Change detection
  On a town scale
  Land use
  Tourisme
Environmental risks
Global monitoring
Hyperspectral applications
Context
CO2 AND PLANTS

CO2 : We're producing too much of it

Plants absorb carbon dioxide (CO2) from the atmosphere via photosynthesis. When plants 'exhale' and organic materials like fallen leaves and branches, etc. decompose on and in the soil, CO2 is released once again. The equilibrium between the absorption and discharge of CO2 is a major issue in the debate about reducing greenhouse gasses (The Framework Convention on climate changes, The Kyoto Protocol). The ever-growing greenhouse effect, after all, is partly explained by an increase in CO2 concentrations, primarily resulting from human activities such as the combustion of fossil fuels. The determination and prediction of changes in the carbon absorption and discharge mechanisms of plants and vegetation thus form an important aspect of this Global Change problematic.

 


The carbon cycle
Courtesy of "Fundamentals of Physical Geography"
http://www.physicalgeography.net/fundamentals/9r.html

The satellite records

Ecosystem models and field measurements using measuring equipment are the traditional methods for determining the CO2- or carbon balance in afforested areas. The carbon balance is the difference between the absorption and the discharge or emission of carbon. However, local measurements only apply for a limited area. If we want to know the CO2 balance for a more extensive geographical area, for example Belgium, then these measurements must be calculated or extrapolated both in time and space from various local observations. In heterogeneous areas, therefore, accuracy is highly dependent on the number of measuring points. Remote sensing provides the necessary data for applying these processes on a larger scale, so that a spatial extrapolation technique becomes unnecessary.

The computer calculates

That is why the VITO (Vlaamse Instelling voor Technologisch Onderzoek, the Flemish Institute for Technological Research) developed the C-Fix model. This is a method based on remote sensing for calculating the carbon balance of vegetation for a specific geographical area. This model not only takes afforested areas into account, it also determines the carbon balance for the whole of Belgium and maps it out for all types of vegetation.
Concretely, the model is used to determine the gross primary productivity (GPP), the net primary productivity (NPP) and the net ecosystem productivity (NEP) for all types of vegetation in Belgium on a daily and/or yearly basis.

 

The quantity of CO2 which is absorbed by vegetation from the atmosphere and which is necessary for the growth of plants by means of photosynthesis is designated as the gross primary productivity (GPP). However, CO2 is discharged once again by the same vegetation into the atmosphere through autotrophic respiration (so-called 'maintenance losses') and by decomposition of branches, leaves, etc. in the soil layer (which is referred to as 'soil respiration' or 'heterotrophic respiration'). In this context, the net primary productivity (NPP) of vegetation is expressed as the gross photosynthesis or gross primary productivity minus autotrophic respiration. We can define the net ecosystem productivity (NEP) of vegetation as the gross productivity minus the autotrophic and the heterotrophic respiration. The figure shows an overview of these carbon flows. The various productivities (GPP, NPP & NEP) are expressed in grams of carbon (C) absorbed per day and per square meter [g C/m²/d].


An overview of the carbon flows in vegetation
1. Atmosphere
2. Vegetation
3. Soil
4. Gross Primary Productivity
5. Autotrophic respiration
6. Heterotrophic respiration