INTRODUCTION
The stated aim of the Department of Agriculture of the
Republic of South Africa is the optimum utilization of the natural resources
through the promotion of farming enterprises which are i) adapted to the local
environment, ii) strive for sound economic production and iii) aim to prevent a
deterioration of the natural resources.
The importance of the correct use of the natural resources to
the overall economy of the KwaZulu-Natal region cannot be over-emphasised. The
degradation of the natural resources is also a matter of grave concern and both
this and the economic pressures placed on agriculture indicate the urgent
necessity for matching crop and animal requirements with the production
potential of the natural resources.
The diversity of the natural resources in the province of
KwaZulu-Natal is enormous. The topography ranges in elevation from sea level to
over 3 000 m, resulting in a considerable range in temperature, while the
topography varies from the undulating coastal plains of Maputoland to the
rugged, broken terrain of the Valley of a Thousand Hills and the precipitous
mountains of the Drakensberg. The rainfall also varies considerably, from
approximately 580 mm to over 2 000 mm per annum. The geological formations of
the Province run roughly north to south across an eastern-sloping terrain while
the river systems run west to east, resulting in deeply incised valleys, cutting
through the geological layers. With this great variation in topography, climate
and geology, one could expect a wide variation in soil patterns and this is
indeed so. Deep sands are found along the northern coastal belt, young
weathering soils in the steep valleys, well-drained, deep soils are a feature of
the midlands and the highland areas and poorly drained and duplex soils are
common in the upland areas where the rainfall is below 750 mm per year.
In turn, the vegetation is affected by the changes in
topography, rainfall and soils. Bushveld is found in the low-lying hot and dry
areas of northern KwaZulu-Natal and in most of the river systems. In the high
rainfall areas of the coastal belt, the midlands mistbelt, highland sourveld and
the mountains of the Drakensberg, different forms of forest are found in areas
which are protected from fire. In the northern plains of the province a tall
grassveld is characteristic while in the cold highland areas the grassland is
typically short.
This great variation in the natural resources in turn leads to
variations in the type of farming and levels of production throughout the
province. It can be seen that the challenge of providing for sound ecologically
based development planning in agriculture and other fields, is a major problem
when the complexity of the KwaZulu-Natal natural resources is considered. The
Bioresource Unit project was developed to assist in ensuring informed planning
of farming systems in the Province.
THE BIORESOURCE UNIT
(BRU)
A Bioresource Unit is a demarcated area in which the
environmental conditions such as soil, vegetation, climate and, to a lesser
degree, terrain form, are sufficiently similar to permit uniform recommendations
of land use and farm practices to be made, to assess the magnitude of crop
yields that can be achieved, to provide a framework in which an adaptive
research programme can be carried out, and to enable land users to make correct
decisions. The uniformity of climate and soil type within each BRU should be
such that the type of farming enterprise, and the productivity and management
techniques required, can be clearly defined.
There are 590 BRU’s in KwaZulu-Natal. An inventory has been
written for each BRU which describes it's climate, vegetation, soil patterns and
in turn the crops, pastures and timber that can be grown there and the level of
production that can be achieved. The BRU map and it's associated information is
used at farm planning and advisory level.
THE BIORESOURCE GROUPS
(BRG)
The Bioresource Units have, in turn, been grouped into
ecological units based primarily on climate and vegetation, and
are referred to as Bioresource Groups (BRG’s). A BRG is an area with a
reasonably uniform pattern of vegetation type, climate and soil pattern within
its boundary. Broad veld management recom-mendations, such as potential grazing
capacity, grazing systems, burning schedules, are made at the BRG scale. The BRG’s
are listed below, together with a short description of their temperature and
rainfall ranges. A map indicating the location of each BRG is given in Figure 1.
BRG 1: Moist Coast Forest, Thorn and Palm
Veld (Moist Coast)
Rainfall is well distributed and the mean annual
rainfall varies from 819 mm to 1 270 mm. The mean annual temperature varies
from 18.3EC to 21.9EC. There are no ecologically dry months with rainfall less
than 25mm, but dry spells lasting several weeks can cause a loss in
production. Frost has been experienced on rare occasions in valleys. Lightning
and hail are also rare. Strong winds are a common feature, and if combined
with high temperatures, evapo-transpiration can be high.
BRG 2: Dry Coast Forest, Thorn and Palm Veld
(Dry Coast)
Similar to the Moist Coast, but much drier with the
mean annual rainfall from 741 mm to 815 mm. The mean annual temperature varies
from 19.0EC to 21.6EC.
BRG 3: Moist Coast Hinterland Ngongoni
Veld
(Moist Ngongoni Veld)
Annual rainfall varies from a minimum of 800 mm
to an extreme of 1 160 mm. There are fewer than three ecologically dry months.
Mean annual temperatures vary from 16.1EC to 19.6EC. Droughts are occasional,
and frosts are light, mainly in the valleys.
BRG 4: Dry Coast Hinterland Ngongoni Veld (Dry
Ngongoni Veld)
Usually situated at lower altitudes than the Moist
Ngongoni Veld and has a mean annual rainfall varying from 712 mm to 836 mm. The
mean annual temperature range is from 16.9EC to 19.6EC.
BRG 5: Moist Midlands Mistbelt (Moist Mistbelt)
Mean annual rainfall varies from 800 mm to 1 276 mm.
Mist is a common feature. The mean annual temperature varies from 15.4EC to
18.5EC. Crop production hazards include hail, occasional dry spells in summer
and mist and cloud cover in early summer. Hot "Berg" winds in spring
are frequently followed by cold spells. Frosts are usually moderate, but severe
frosts occur occasionally.
BRG 6: Dry Midlands Mistbelt (Dry Mistbelt)
This BRG experiences less mist than the Moist Midlands
Mistbelt and dry summer spells are more frequent. The mean annual rainfall
varies from 738 mm to 825 mm. The mean temperature varies from 16.2EC to 17.6EC.
BRG 7: Northern Mistbelt
Similar, in most respects regarding climate, to the
Moist Midlands Mistbelt with a mean annual temperature varying from 16.0EC to
17.4EC, and mean annual rainfall of between 980 mm and 1 123 mm.
BRG 8: Moist Highland Sourveld
The mean annual rainfall varies from 800 mm to 1 265
mm and the temperature is between 11.5EC and 16.6EC. The rainfall is reasonably
reliable. Summers are cool and winters cold, with severe to very severe frost.
Snow is experienced occasionally, more frequently on the high-lying areas. The
growing season is short, hail is a hazard and hot "Berg" winds
increase the risk of serious fires.
BRG 9: Dry Highland Sourveld
Droughts are quite frequent occurrences and the mean
annual rainfall varies from 620 mm to 816 mm, with the lower extremes in the
East Griqualand and Newcastle areas. Snow is infrequent. The mean annual
temperature varies from 12.9EC to 15.6EC.
BRG 10: Montane Veld
Mean annual rainfall varies from 900 mm to 1 390 mm
and 6 to 7 months are wet, exceeding 100 mm. Torrential downpours are common.
The mean annual temperature varies from 7.5EC to 13.2EC, frosts are very severe
and snow is a regular feature. This area is South Africa's most important water
source.
BRG 11: Moist Transitional Tall Grassveld
(Transitional Tall Grassveld)
The mean annual rainfall is from 800 mm to 1 116 mm.
Mists are a frequent occurrence. The mean annual temperature varies from 15.0EC
to 18.7EC. Frosts are generally moderate, but occasional severe frosts do occur.
BRG 12: Moist Tall Grassveld
The mean annual rainfall varies from 712 mm to 805 mm.
There are 3 to 4 ecologically dry months. The mean annual temperature varies
from 15.3EC to 18.9EC. Occasional drought periods occur during the summer,
frosts are moderate to severe, and hail storms are experienced.
BRG 13: Dry Tall Grassveld
The mean annual rainfall varies from 666 mm to 745 mm
and there are 4 to 5 ecologically dry months. The rainfall is not reliable and
is poorly distributed. The mean annual temperature varies from 15.6EC to 19.0EC
and frost is moderate to severe.
BRG 14: Sour Sandveld
The Sour Sandveld has sandier soils than the Dry Tall
Grassveld but the climate can be regarded as being similar to the climate of
that BRG. The mean annual rainfall varies from 645 mm to 737 mm, and the mean
annual temperature is between 14.7EC and 17.3EC.
BRG 15: Moist Lowland Tall Grassveld
The rainfall range of this BRG is from 800 mm to 1 000
mm. The mean annual temperature varies from 18.5EC to 20.5EC. Frosts are
moderate, and severe frosts rare.
BRG 16: Dry Lowland Tall Grassveld
This BRG has a mean annual rainfall varying from 706
mm to 795 mm, and the mean annual temperature varies from 17.9EC to 20.8EC.
BRG 17: Coast Hinterland Thornveld
The mean annual rainfall varies from 644 to 838 mm
with frequent summer dry spells. The mean annual temperature varies from 17.2EC
to 19.5EC with rare, moderate frosts.
BRG 18: Mixed Thornveld
The mean annual rainfall varies from 650 mm to 786mm,
and there are 4 to 5 dry months. Rainfall is poorly distributed and droughts
occur frequently. The mean annual temperature varies from 16.0EC to 18.1EC.
Frosts are generally moderate, but severe frosts are experienced in some
valleys.
BRG 19: Moist Zululand Thornveld
The mean annual rainfall varies from 760mm to 846mm
and there are 4 ecologically dry months. The rainfall is poorly distributed. The
mean annual temperature is between 20.7EC and 21.5EC. Frost is rare.
BRG 20: Dry Zululand Thornveld
The mean annual rainfall varies from 678mm to 788mm
and the mean annual temperature ranges from 19.2EC to 21.6EC. Droughts are more
frequent than in the Moist Zululand Thornveld.
BRG 21: Valley Bushveld
The mean annual rainfall varies from 595mm to 830mm
and drought is a serious hazard. The mean annual temperature range is from
17.1EC to 20.8EC. The range in extreme temperatures can be wide. Weenen, for
example, experiences the widest range in temperature in the Tugela Basin,
ranging from a low of - 6.7EC to a high of 42.8EC. The low temperatures are the
result of cold air flowing into the valleys from the surrounding high-lying
country. Climate hazards include frequent periods of drought, occasional severe
frosts, considerable heat, lightning and hail.
BRG 22: Lowveld
The mean annual temperature of this warm area ranges
from 17.5EC to 22.2EC. Evaporation exceeds 1 524 mm per annum. The mean annual
rainfall varies from 587 mm to 750 mm. Rainfall is erratic and droughts often
severe.
BRG 23: Sandy Bushveld
The mean annual rainfall varies from 635 mm to 775 mm.
Rainfall is unreliable. The mean annual temperature is from 21.7EC to 22.0EC.