HOW DO WE STUDY CARBON SEQUESTRATION
Carbon based
biomass accumulates above and below ground in forests of the northwestern
U.S. Mathematical formulae are used to estimate above ground bomass.
The Goltz equations have been used in the past to estimate standing
biomass of northwest conifers, but at our research in Fall River, we found
it more appropriate to generate our own mathematicial relationships for the
estimation of forest biomass above ground.
An important question in current forest management practices is whether
or not fertilization can increase carbon sequestration. The basic question
is whether or not an increase in limiting nutrients will increase forest productivity
and soil carbon sequestration. In our studies we apply urea fertilizer
(Figure 1) to the forest. Urea may be applied manually (Figure 2) or
by air. As Figure 1 shows, urea contains nitrogen, but only half as
many parts of carbon. Carbon is present in much larger quantities than
nitrogen with C/N ratios of plant tissue and soils commonly ranging from
10 to 40. The major carbon source, of course, is fixation of carbon
dioxide from the atmosphere via the process of photosynthesis.
The stem cross section below shows the effect of urea on
tree growth. Immediatly after the application of 200 pounds per acre
of urea fertilizer, tree growth increased. The result of this is an
obvious increase in above ground carbon sequestration. Sequestration
in the soil is not as easy to measure and the mechanisms of carbon sequestration
in the soil are not straight forward. For instance, increased growth
below ground could be manifested as root diameter increases or an increase
in root exudates associated with the rhizosphere. In either case, microbial
consumption and solubility and adsorption properties of the soil will influence
the longeivity of this carbon in the soil. Some carbon may flush rapidly
through the soil, whereas other carbon may be processed and made more recalcitrant.
More stable and insoluble forms of carbon have a much longer residency
time in the soil.