Wednesday, December 14, 2016

Some people just want to watch the world burn: how fire ecology informs land management

                While we see fire as a destructive force, fire is a necessary part of many environments and ecosystems. Fire often drives plant diversity, is responsible for the germination of plant seeds, clears away debris, and puts nutrients and minerals back into the soil. As such, understanding the role of fire disturbance in natural landscape dynamics is essential for park and land management. Fire dynamics, however, are not completely understood (Bergeron et al. 2002.) Moreover, the effect of prescribed burns varies according to a variety of factors.

                Kennard and Gholz (2001) investigated the effect of fire intensity on soil quality and nutrient availability in a Bolivian forest. Their study aimed to test the difference between high and low intensity fires, as determined by “fuel loads” or the amount of woody debris present, in terms of: 1.) how they affected the soil itself and 2.) how it affected the growth of a particular plant, Anadenathera colubrine. They conducted their burns in plots and looked at soil pH, organic matter concentrations, and mineral concentrations (such as phosphorus, nitrogen, and magnesium).

An experiment burn conducted at Kruger National Park.
Image from http://www.fire.uni-freiburg.de/iffn/country/za/za_6.htm

                The study found that high intensity fires led to significantly higher mineral concentrations that the other treatments, but they led to a significantly lower concentration of organic matter in the soil. The amount of organic matter in the soil affects how well soil accepts and holds water. Less soil organic matter suggests that the soil is now worse at accepting and retaining water, and also can lead to greater water evaporation from soil and surface run-off. Meanwhile, while the low-intensity burns also led to higher mineral concentrations than the control plots, they did not decrease soil organic matter. As for the effect of burn intensity on the growth of A. colubrine, the seedlings grew the tallest after high intensity burns; however, as Kennard and Gholz (2001) note, the effects of the high intensity burns may not last in the long term. The soil structure will takes years to recover after these high intensity burns, so the researchers conclude that the low intensity burns may be the safer, more beneficial route.

                While experiments and research into the effect of burn intensity are rare, they may be incredibly useful to consider when developing fire regimes. A burn intensity experiment is on-going in South Africa’s Kruger National Park, where large patches of the landscape have been burned twice at high or low intensities, this time determined by the time of year and season, over the span of five years. These experimental burns were ultimately conducted to inform future fire regimes in the savannas of KNP, fire driven systems. For my proposed research, I am interested in looking at how plant diversity, specifically growth under large trees, differs between the high and low intensity burn sites. Kruger National Park’s experimental burns also have to address the issue a declining population of large trees due to an increasing population of elephants. This research will help explore fire – herbivory interactions, and which type of fire may be more beneficial in promoting greater plant diversity. Moreover, it has the added conservation impact, as developing fire regimes that will cause the least damage to already vulnerable large trees is in the best interest of the savanna ecosystem. The Kennard and Gholz (2001) study is a useful study to consider because it looks at the biogeochemical aspects of prescribed fire intensity. Similar to their predictions and conclusions, I believe that the low intensity burns will ultimately yield the most diversity while also being the least damaging.

Works Cited
Kennard, D. K., and H. L. Gholz. 2001. Effects of high- and low-intensity fires on soil properties and plant growth in a Bolivian dry forest. Plant and Soil 234: 119 – 129.

Bergeron, Y., A. Leduc, B. D. Harvey, and S. Gauthier. 2002.Natural Fire Regime: A guide for sustainable of the Canadian boreal forest. 

2 comments:

  1. You said that you wanted to study plant diversity responses to high and low intensity burns. Will you be looking at a few species found under large tree growth or will you be looking at ALL the plant diversity found?

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  2. How will looking at the diversity of the growth under large trees tell you about what will cause the least damage to large trees? Do the trees and the growth under trees have a mutualism relationship type? Is there something else that you are measuring to assess damage on large trees?

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