The majority of the vegetation types occurring on Malilangwe Estate, in the south-eastern lowveld
of Zimbabwe, are dominated by Colophospermum mopane (mopane). Over the past 30-50 years
the stand density of these mopane vegetation types has increased, and an investigation was
undertaken to determine the effect of season of burning and type of fire on mopane woodlands.
From this study the following was ascertained:
1) A single predictive equation cannot be used over all seasons to estimate standing crop
(fuel load) using the standard disc pasture meter procedure. The calibration equations developed
using this procedure accounted for between 39 and 72% of the variation in standing crop,
illustrating the high variation in basal cover of the grass sward, as well as the variation between
months. Although the revised procedure, developed for areas with low basal cover, accounts for
a lot more of the variation in standing crop, this procedure was not used to estimate standing crop
over the study period because the calibration equation covered a number of vegetation types, and
was not specific to the mopane woodlands.
2) Standing crop tracks effective rainfall (monthly rainfall divided by monthly pan
evaporation) closely, with a lag period of less than one month. Standing crop can be estimated
using a predictive equation that utilizes effective rainfall from the previous month. There is a
positive relationship between peak standing crop and rainfall. A predictive equation was developed
to estimate peak standing crop, using annual rainfall. Standing crop declines through the dry
season as effective rainfall decreases, and this 'decrease function' allows for the estimation of the
standing crop for a particular month, after peak standing crop is reached.
3) Two leaf quantification equations were developed for mopane trees in the south-eastern
lowveld of Zimbabwe, one for coppicing and for non-coppicing individuals. These allow for the
estimation of leaf dry mass from measured canopy volume.
4) There was no significant difference between the fire intensities attained for the three
seasons of burning. Over all seasons, head fires were significantly more intense than back fires.
5) Percentage topkill after late dry season burns was significantly higher than topkill after
early dry season burns. There was no significant difference between mid and late dry season
burns, and head fires led to significantly more topkill than back fires. Plants < 150 cm
experienced significantly more topkill (80 %) than did individuals > 150 cm (44%). 6) Fire per se led to an increase in stand density over all seasons and types of fire, but this
change was not significant. Fire did not influence the nett recruitment of new individuals. Height
class one (0-50 cm) and three (151-350 cm) were impacted most by fire. This reflects a change
in tree structure, with an increase in the amount of leaf material in height class three, and a
subsequent decrease in the amount of material in height class one.
7) The effect of season of burning on the change in tree height was significant, whereas
the effect of type of fire was not significant. All treatments, except early dry season back fires,
led to a reduction in tree height, whereas trees in the no burn areas increased in height.
8) Burning in any season, and implementing either type of fire, led to an increase in the
number of stems. Mid dry season burns led to the highest increase in number of stems. However,
the more intense the fire the smaller the increase in number of stems.
9) All three seasons of burning (head and back fires) led to a significant decrease in
maximum canopy diameter per tree, while the maximum canopy diameter of trees in the no burn
areas increased. Mid dry season burns resulted in the greatest decrease in canopy diameter.
10) The effect of burning on the change in leaf dry mass per tree was highly significant.
All three seasons of burning led to a decrease in leaf dry mass, while there was no difference
between head and back fires. Leaf dry mass in the control areas increased however. High fire
intensities led to the greatest decrease in leaf dry mass, late dry season head fires having the greatest decrease.
This study suggests that mopane plants face a constraint due to fire and/or browsing, and a
tradeoff occurs between canopy volume, canopy diameter, canopy area; and number of stems. Fire
leads to an increase in the number of stems through coppicing, while canopy volume and leaf dry
mass decreases. This decrease is either (i) a tradeoff in response to increasing stem number, or
(ii) a reduction in canopy because additional leaves on the new stems contribute to photosynthesis.
The most important response to season of burning is the altered phenophase (phenological stage)
of the plant. Early dry season burns cause the trees to be leafless during the early dry season
(when unburnt trees are carrying full leaf), and then to be in leaf at the end of the dry season
(when unburnt trees are leafless). It would appear that fire disturbance initiates leaf senescence
after burning, and then leaf expansion earlier than normal i.e the whole leaf senescence/growth process is brought forward. Trees in late dry season burn areas remain leafless at the start of the
rains, while trees in unburnt areas are carrying leaf. Being leafless these trees do not
photosynthesize during this time, and it is proposed that the grass sward is advantaged by the
reduced competition from the tree component. The consequences of these two changes in
phenophase could not be addressed in this study, but are pertinent questions that must be answered
if mopane woodland dynamics are to be more fully understood.
Management recommendations for (1) the removal of unacceptable moribund grass material, or
(2) the reduction of encroachment by woody species on Malilangwe Estate are also given. In an
attempt to combat the increase in stand density of mopane it is recommended that high intensity
head fires be implemented, when standing crop (fuel load) is sufficient and climatic conditions are
conducive to maintaining high intensity fires. These should be carried out at the end of the dry season, before the onset of the rains. / Thesis (M.Sc.)-University of Natal, Pietermaritzburg, 2000.
| Identifer | oai:union.ndltd.org:netd.ac.za/oai:union.ndltd.org:ukzn/oai:http://researchspace.ukzn.ac.za:10413/10244 |
| Date | 17 December 2013 |
| Creators | Walters, Michael John. |
| Contributors | O' Connor, Tim G. |
| Source Sets | South African National ETD Portal |
| Language | en_ZA |
| Detected Language | English |
| Type | Thesis |
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