Notes : The author concludes as follows. This study of the structure and
functional dynamics of the Natal bushveld has yielded many results in common
with those of Archer and his co-workers (op.cit.) for a relatively similar
situation in the savannas of southeastern Texas. However, there are some
differences which can be attributed to the topological complexity of the Natal
bushveld sites and to the wider range of land use histories w hich they have
experienced. Below, the author states what he believes the major conclusions
are of this work and wherever possible, he points out the similarities and
differences with the savannas of North America. First, cluster species richness
can be used as an index of cluster developmental stage. This is particularly
important where a variety of different land use histories must be considered.
Heavily used rangelands often have fewer bush clusters per unit area and they
are smaller, whereas relatively unutilised areas have a higher density of bush
clusters and a greater range of bush cluster sizes. As a result of the
differential effects of immigration to and extinction within bush clumps,
cluster species richness is a better estimate of successional stages in areas
with different land use histories. This effect was not a problem at the La
Copita site in the savanna of southeastern Texas which was subjected to only one
pattern of land use history. Second, cluster growth is dependant on the rate at
which different clusters can coalesce, and not concentric expansion of
individual cluster perimeter. This, in turn, is depedent on the rate of cluster
formation and survival. A similar result was obtained in Texas. In both
studies, cluster formation and survival were greatest during wet periods with
severe mortality of small bush clusters occurring during periods of long-term
drought. Larger bush clusters continued to increase in size in both studies
during drought periods and were difficult to identify individually in the
sequence of aerial photographs used. The latter observation suggests that the
estimates of the rate of closure of the bush cluster phase are lower than they
actually are. Third, most of the species that occur in the Natal bushveld seem
to be dependent on the clustered structure of woody vegetation for establishment
and survival. Very few of the species found in the interstices of bush cluster
phase are present within the bush clusters. Those species that are present in
both situations are primarily members of the genus, Acacia, or are understory
shrubs which rarely reach tree size. A similar result was reached in the Texas
study where Prosopis glandulosa is the dominant woody species found in the open
grassland stage. It also serves as foci for the establishment of other woody
species, which are rarely found in the open, under their canopies. As a
consequnce, the cluster phase in Natal bushveld vegetation is important for the
maintenance of species diversity and ecosystem resilience at the landscape
scale. The bush cluster phase is particularly important where different types of
land use are employed on the landscape. The effects of these land-use practices
can (i) result in local extinction of species and loss of ecosystem resilience
and (ii) retard the development of closed-canopy woodland. Fourth, a
'successional gradient', which is likely the result of biotic interaction among
individual plants over a 'successional time scale' can be used to explain the
pattern of species distribution in a Natal bushveld community to a large degree.
As a consequence, species reponses to such a 'successional gradient' can be used
to describe the temporal range of individual species, and to group these species
into functional classes. In this study, as in the La Copita study, the early
successional species are aggressive invaders of the grassland phase and are not
easily removed once established. These species are primarily responsible for
our 'bush encroachment' problems in southern Africa and in many other parts of
the world. In all cases, the propagules of these early successional species are
dispersed into grasslands by large vertebrates. The propagules of later
successional species are dispersed by birds, monkeys and, rarely, wind. These
species are generally broad-leafed and appear to be dependent on bush clusters
to facilitate their successful establishment. Next, models based upon the above
methods and results can be constructed which describe species turn-over in
bushveld communities along a continuum of 'successional' development. Such a
model can be used to classify different communities or sites on the basis of
their species composition according to their previous land-use history and their
successional status. Such a model would be a potentially useful management and
planning tool. Finally, the phenomenon of 'bush encroachment' in southern Africa
is the result of natural events in which man has interceeded. Unless a clear
understanding is obtained of the dynamics underlying the ecological processes
and the environmental forces involved in causing the transition from one state
of vegetation to another within these rangelands, no attempts to manage this
vegetation to a desired endpoint will be successful in the long term. At
present, bush clusters in Natal bushveld continue to grow and coalesce in
moderately disturbed veld, slowly reverting to closed-canopy woodland. The
future of Natal bushveld under higher levels of disturbance is still an
unanswered question.
Ref ID : 648
1269. Le Roux, J.S. Spatial variations in the rate of fluvial erosion (sediment
production) over South Africa. Water SA 16(3):185-194, 1990.
Reprint : In File,
Keywords : SOIL EROSION; SEDIMENTATION
Abstract : The rate of denudation of the past ten to fifty years was calculated
from sediment accumulated in man-made reservoirs. The rate of surface lowering
generally increases from west to east over the subcontinent. This increase more
or less coincides with both an increase in annual precipitation and an increase
in the number of storms of high intensity. On the whole there is an increase in
relief from west to east, but relief seems to be only a secondary factor in the
explanation of denudation rate. No conclusive evidence could be found (from
reservoir sedimentation rates) that denudation rates have either decreased or
increased over the last ten to fifty years.
Ref ID : 312
1270. Le Roux, J.S. and Roos, Z.N. Rate of erosion in the catchment of the
Bulbergfontein dam near Reddersburg in the Orange Free State. J.Limnol Soc.S.A.
5(2):89-93, 1979.
Reprint : In File,
Keywords : SOIL EROSION; FREE STATE; SEDIMENTATION; CULTIVATION; RAINFALL;
EROSION
Notes : The volume of sediment in the Bulbergfontein Dam was computed after
mapping the area of the dam and ascertaining the depth of the sediment by
digging and augering. The watershed of the impoundment had been delimited by
means of aerial photographs and fieldwork. The catchment has a mean slope of
1,9o which is mostly covered by perennial grasses and xerophytic shrublets.
Approximately 75 per cent of the area is natural pasture and the rest under
maize and wheat cultivation. The mean annual rainfall is 471 mm. The
fortuitous presence of a fine sand layer (marker) in the sediments made it
possible to compute not only the total accumulation of sediment, but also the
accumulation since 1971. From these figures the rates of erosion were found to
be 27,5 mm 10-3 years for the period 1942 to 1971 and 34,6 mm 10-3 year for the
period 1972 to 1978.
Ref ID : 313
1271. Le Roux, J.S. and Roos, Z.N. The rate of soil erosion in the Wuras dam
catchment calculated from sediment trapped in the dam. Annals of Geomorph.
26(3):315-329, 1982.
Reprint : In File,
Keywords : SOIL EROSION; SEDIMENTATION; FREE STATE; EROSION
Abstract : The volume of sediment trapped in Wuras dam was obtained by
calculating the present capacity from numerous depth measurements and
subtracting this value from the original capacity of the dam. In order to
calculate the mass of the trapped sediment eleven core samples were taken and
the average density determined (0,97 g cm-3). The denudation rate was
calculated in terms of ground lowering and for this the average density of the
rocks underlying the catchment area was necessary. This was found to be 2,5 g
cm-3. From these figures in addition to the catchment area and the age of the
dam the rate of erosion was found to be 2.06 cm 10-3 years. As some of the
sediment is lost by overflow during wet spells (about 12%) the absolute rate is
about 2,3 cm 10-3 years.
Ref ID : 314
1272. Le Roux, J.S. and Roos, Z.N. Surface wash on a low-angled slope near
Bloemfontein. South African Geographical Journal 64(2):114-124, 1982.
Reprint : In File,
Keywords : SOIL EROSION; SEDIMENTATION; RUNOFF; FREE STATE; EROSION; RAINFALL
Abstract : Surface wash was measured for three consecutive years on a fairly
low-angled slope by means of 6 pairs of wash-traps. The erosion rate was found
to be more or less constant over the whole slope. This implies that, for the
period under observation, the slope retreated parallel to itself. Multiple
regression analysis of erosion (dependent variable), rainfall, rainfall
intensity and product of rainfall and rainfall intensity indicated that the only
truly significant variable was the product of rainfall and rainfall intensity.
The three variables together accounted for 58 percent of the variance in
erosion. The rate of soil loss calculated from the wash-trap data for 37 run-
off events was 46 g m-2 per year or, calculated as a ground lowering, 18 mm 1000
yr-1 at rock density, or 34 mm 1000 yr-1 at soil density.
Ref ID : 641
1273. Le Roux, J.S. and Roos, Z.N. The relationship between the size of
particles in surface wash sediment and rainfall characteristics on a low angle
slope in a semi-arid climate. Zeitschrift fur Geomorphologie N.F. 30(3):357-362,
1986.
Reprint : In File,
Keywords : SOIL EROSION; RAINFALL EROSIVITY; SEDIMENTATION; RAINFALL
Notes : In this investigation the amount of rainfall proved to be positively
correlated to the relative amounts of the sand fraction and negatively
correlated to the clay fraction being entrained and transported by surface wash.
Rainfall intensity showed the opposite trend, negative correlation to the sand
fraction and positive correlation to the clay fraction. The product of rainfall
intensity - the better indicator of overall soil loss - (Le Roux & Roos 1982:
120), provided to be negatively correlated to the relative amounts of sand and
positively to the clay fraction. The rather low correlations of precipitation
variables to the different mass percentage particle size categories indicate the
importance of other internal and external factors of the soil.
Ref ID : 2283
1274. Lehman, T. Public values, private lands, London:The University of the
North Carolina Press, 1995.
Reprint : In File,
Keywords : POLICY; LAND USE; SOIL CONSERVATION; CONSERVATION; POPULATION; ENERGY
Notes : The author examines the political battles over public policies to
protect farmland from urban sprawl. His detailed account clarifies three larger
themes: the ongoing struggle over land use planning in this country, the
emerging environmental critique of modern agriculture, and the use of social
science expertise in policymaking. Federal efforts to preserve private
farmlands began during the New Deal with modest soil conservation and land use
initiatives, but stalled with the agricultural surpluses of the postwar decades.
Land conservation interests re-emerged during the 1970s as productivity
plateaus, population growth, and the energy crisis heightened concern about the
loss of high-quality farmland. Bureaucrats and social scientists were divided
on the seriousness of the land problem. According to Lehman, the debate pitted
a conservation mentality against a production mentality, virtually guaranteeing
that consensus would be impossible. Land preservation initiatives of the 1970s
achieved a belated and partial success with the conservation measures of the
1985 farm bill, the author says, but the ecological constraints on agriculture
remain significant.
Ref ID : 2521
1275. Leibbrandt, M. and Sperber, F. Income and economic welfare. ISER Research
Report.Anonymous Grahamstown:ISER, Rhodes University. , 1997.
Reprint : Not in File,
Keywords : CISKEI; ECONOMIC ASPECTS; SOCIOECONOMIC ASPECTS; LABOUR; AGRICULTURAL
DEVELOPMENT
Notes : The purpose was to look at the structure of rural household income in
the Keiskammahoek district to identify important trends since 1949, and
isolating the factors that have affected each village's relative development. A
survey was conducted between September 1990 and February 1991 involving
interviews with 98 households taken from Rabula, Burnshill and Chatha. The
survey indicates that the three villages differ in sources of income and access
of employment. Burnshill is fast becoming functionally urbanised, in terms of
activities and aspirations. Chatha continues to conform more to the stereotype
of a poor rural village dependent on long term migrants, while Rabula falls
somewhere in between the two, showing characteristics of both. The survey shows
employment to be important in the Ciskei health, educational, agricultural and
administrative bureaucracies. As of 1990, the unemployment rate was 39%, 23%
and 42% respectively amongst rural households in Rabula, Burnshill and Chatha.
This report is obtainable from the Border Rural Committee, East London. See
also ID no. 2339.
Ref ID : 2519
1276. Leibbrandt, M. and Sperber, F. From reserve to region. Apartheid and
social change in the Keiskammahoek district of (former) Ciskei, 1950 to 1990,
Grahamstown:ISER, 1997.
Reprint : Not in File,
Keywords : CISKEI; POVERTY; POLICY; ECONOMIC ASPECTS; AGRICULTURAL PRODUCTION
Notes : The purpose of the study was to look at the structure of rural household
incomes in three villages of Keiskammahoek. Quantitative data collection in the
form of a survey was used for the study. The findings reveal different degrees
of reliance on agriculture, and different levels of integration into urban
economies. The second section extends the average income comparison of three
villages by documenting the extent of unemployment, poverty and inequality
within each village. The third section strengthens the static, survey-based
picture of previous sections by detailing the process that reproduces such a
static snapshot overtime. The fourth section returns to the policy issues
raised in the introduction. By seeking to understand the resilience of
oscillating migration, some of the crucial behavioural issues surrounding the
framing of regional and urbanization policy are raised. This book is obtainable
from the Border Rural Committee, East London. See also ID ref. no. 2339.
Ref ID : 959
1277. Leistner, G.M.E. International aid and African development. Paper
presented at a meeting of the Bophuthatswana Institute of International Affairs,
Mafikeng, 26 June 1986. 1986.
Reprint : In File,
Keywords : RURAL DEVELOPMENT; INTERNATIONAL ASPECTS; AID
Notes : The author notes that the correlation between the amount of aid received
and a particular country's economic progress is, at best, tenuous. He suggests
that the adverse factors associated with the provision of aid outnumber the
benefits. However, equally strong arguments in favour of aid are adduced by the
immensely powerful interest groups whose very existence is based on provision of
aid. The history of provision of aid is discussed, but the author suggests that
aid in post-war Europe was aimed primarily at reconstruction rather than
development. The author concludes by saying that the benefits as well as the
drawbacks of economic interdependence cannot be detailed in this review.
However, it is important to remember that ties of other countries with the South
African economy can act as growth stimuli for neighbouring countries, an
advantage which Black states further to the north do not enjoy, and are not able
to import through foregn aid. Under certain conditions, aid can facilitate the
process of development, but there is no doubt that normal commercial exchange
across international boundaries can do far more to promote economic progress
than any hand-outs doubtfully termed as 'aid'.
Ref ID : 1323
1278. LeMaitre, D.C., Van Wilgen, B.W., Chapman, R.A., and McKelly, D.H.
Invasive plants and water resouces in the Western Cape Province, South Africa:
modelling the consequences of a lack of management. 1998.
Reprint : In File,
Keywords : WESTERN CAPE; FYNBOS; FIRE; ALIEN PLANTS; RAINFALL; RUNOFF; MODELS;
EROSION; WATER QUALITY
Notes : (1) The invasion of fynbos shrublands by woody weed species can reduce
the water yield from catchment areas dramatically. We modelled the consequences
of uncontrolled invasion on water yield using a geographical information system
(Arc/Info). (2) Five important processes were recognised: the occurrence of
fire; the spread and establishment of alien plants after fire; rainfall to
runoff ratios; growth and changes in biomass between fires; and effects of these
changes on streamflow. (3) The simulations of water yield were modelled with
the Arc/Info GRID module using a 200 x 200 m grid. Fire interval was assumed to
be 15 years, and proliferation and dispersal of alien plants took place only
after fires. (4) Between fires, the model simulated the growth of the
vegetation and its effects on streamflow, using relationships between rainfall
and runoff, and runoff and above-ground biomass. (5) Results for the Kogelberg
area in the Western Cape Province showed that alien plants invaded about 40% of
the grid cells within 50 years. Cover of alien plants increased from an initial
estimate of 5.4% to 80% after 100 years. (6) Invasion of catchment areas would
result in an average decrease of 347 cubic metres of water per hectare per year
over 100 years, resulting in average losses of more than 30% of the water supply
to the city of Cape Town. In individual years, where large areas would be
covered by mature trees, losses would be much greater. (7) In addition,
invasion of fynbos by alien plants will result in the extinction of many plant
species, increase the intensity of fires, destabilise catchment areas with
resultant erosion and decreased water quality, and decrease the aesthetic appeal
of mountain areas. (8) Control of alien weed species is necessary to avert the
above impacts, and the costs of control operations could be justified by
maintaining good levels of water runoff from stable catchments in the long term.
Ref ID : 1203
1279. Lenta, G. Development or stagnation? Agriculture in KwaZulu.Anonymous
Durban:Department of Economics, University of Natal. No. 7:1-55, 1978.
Occasional Paper.
Reprint : In File,
Keywords : AGRICULTURAL PRODUCTION; COMMUNAL AREA; CULTIVATION; ECONOMIC
ASPECTS; KWAZULU; LAND USE; LIVESTOCK PRODUCTION; STOCKING RATE; FORESTRY;
POPULATION
Notes : It is commonly believed that agricultural methods in KwaZulu, as in the
case of most SA homelands, are primitive and output and yields low. It is the
purpose of this study to review the agricultural production of KwaZulu and to
determine to what extent this generally held opinion reflects the actual
situation. Part 1 concerns itself with the state of field production, forestry
activities and animal husbandry over the 16 year period 1957 - 1973. In part 2
the findings of the two analyses are collated in a systematic form so as to
provide an estimate of income originating in the agricultural sector over the
period under review. At the same time the size of the agricultural output is
tested against the food requirements of the local population so as to guage the
performance of acgriculture in the homeland. Finally, the quantitative and
qualitative endowment of factors of production which characterises KwaZulu's
agriculture will be compared with that of White agricuture.
Ref ID : 595
1280. Lenta, G. Land shortage and land unused: the paradoxical patterns of
KwaZulu, Durban:Economic Research Unit: University of Natal, 1981.
Reprint : In File,
Keywords : AGRICULTURAL PRODUCTION; COMMUNAL AREA; KWAZULU; KWAZULU NATAL; LAND
REFORM; LAND USE; POLITICAL ASPECTS; POPULATION; LAND TENURE
Notes : The need for this study arises from the particular situation in SA where
land is divided between Africans and Whites in such a way that the different
tribal groups each receive their separate parts of the 14 per cent allocated to
Africans out of the total area of the country. Moreover, a further puzzle is
that a comparatively large proportion of arable land (20 - 30 per cent) is left
uncultivated every year. The main intention of this study is to attempt to
explain this puzzle. A few questions on the matter will be answered including
the following: In what sense is there a shortage of arable land in KwaZulu?
Why is land left uncultivated? The intention, therefore, is not to investigate
the ways in which land at present cultivated could be made to produce higher
yields, but to try to indicate how a larger extent of land could be cultivated.
The discussion is preceded by an historical review of the way in which the
concept of the Reserves developed and altered from their inceptions until the
present day (section 2), the object being to throw light on the principles on
which, at different times, land was allocated to Africans and to allow some
judgments to be made, in later sections and in the conclusion, on the justice of
those principles. With the exception of Section 2, the study restricts itself
to KwaZulu, or rather to that part of SA at present so called. In Section 3,
trends in crop production during the period 1867 - 1977 are examined. The
amount of land available at different periods is compared with population
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