the land, resulting in lower crop yields.
Ref ID : 1934
1016. Grindley, J. and Dudley, S. Estuaries of the Cape, Part 11. Report no. 28
Reitvlei (CW 24 and Diep (CW 25). CSIR research reports.Anonymous Pretoria:CSIR.
427, 1988.
Reprint : Not in File,
Ref ID : 815
1017. Grobler, D.C. and Silberbauer, M.J. Impact of eutrophication control
measures on the trophic status of South African impoundments.Anonymous
Pretoria:Water Research Commission. 130/1/84, 1984.
Reprint : Not in File,
Keywords : WATER QUALITY; POLLUTION
Ref ID : 1722
1018. Grossman, D. Primary production of rangeland: practical and interpretive
problems. Proceedings of the Grassland Society of southern Africa 17:76-78,
1982.
Reprint : In File,
Keywords : SOUTHERN AFRICA; METHODOLOGIES; VEGETATION DYNAMICS; AGRICULTURAL
PRODUCTION; LIVESTOCK PRODUCTION
Abstract : Primary production of rangeland has not been studied in southern
Africa to the extent that it has been in other biogeographical regions.
Ambiguity in terminology and in conceptualization of the process created
difficulties in interpreting and/or comparing production data within the region.
Certain difficulties inherent in estimating primary production of perennial
natural rangeland are discussed. Harvest data are utilized to illustrate how
methodology employed is critical to the estimate of primary production obtained.
A relationship is presented which accounts for the major losses pertinent to
most methods of estimating rangeland production.
Ref ID : 1291
1019. Grossman, D. Game ranching.Anonymous Anonymous Pretoria:Department of
Agriculture and water Supply. :1-3, 1989. 0 621 11412 X.
Reprint : In File,
Keywords : CONSERVATION
Notes : As a relatively young industry, a great opportunity exists to learn from
the mistakes of the past and to avoid the pitfalls which befell other farming
enterpresises. A vital game production industry, making wise use of the
country's natural resources, can contribute to the stability of rural areas,
provide sought-after products and add to the overall success of agriculture and
conservation.
Ref ID : 1334
1020. Grossman, D. Wildboerdery. Weading: 'n stategie vir die toekoms.Anonymous
Anonymous Pretoria:Departement van Landbou en Watervoorsiening. :1-4, 1989. 0
621 11411 1.
Reprint : In File,
Notes : See notes on the English translantion in ID no 1291 "Game Ranching".
Ref ID : 928
1021. Grossman, D. and Gandar, M.V. Land transformation in South African savanna
regions. South African Geographical Journal 71(1):38-45, 1989.
Reprint : In File,
Keywords : LAND DEGRADATION; BUSH ENCROACHMENT; SAVANNA; LAND USE
Abstract : The major form of land-use in savanna regions, which occupy about one
third of the surface area of SA, is pastoralism. Deterioration of the
herbaceous layer and an increase in bush density are regarded as the major
transformation processes in commercial ranching areas. In subsistence
economies, denudation of vegetation due to grazing and wood use are problems.
The socio-economic factors underlying these transformations are described.
Ref ID : 916
1022. Grut, M. Notes on the history of forestry in the Western Cape 1652-1872.
South African Forestry Journal (100):32-37, 1977.
Reprint : In File,
Keywords : FORESTRY; WESTERN CAPE; ENVIRONMENTAL HISTORY; FOREST
Abstract : A brief account is given of forestry history in the South Western
Cape Province from the time of the first permanent European settlement until the
granting of self-government. The demand and supply of wood, the indigenous
forests, forest law, and afforestation are dealt with. The scanty indigenous
forests were almost from the outset insufficient to meet the demands of the
settlement for firewood and building timber. The authorities therefore
immediately began trials with a view to finding exotic or indigenous tree
species suitable for afforestation. Exotic species used in these early trials
were, in chronological order: alder (Alnus glutinosa), Norway spruce (Picea
abies), Scots pine (Pinus sylvestris), ash (Fraxinus excelsior), oak (Quercus
robur), hazel (Corylus sp) and teak (Tectona grandis). Indigenous species were:
wild almond (Brabeium stellatifolium), "kreupelboom" (Leucospermum
conocarpodendron) and, probably, mountain cypress (Widdringtonia cupressoides).
Of all these, only the oak proved really successful, and was then extensively
planted in plantations, as a street tree, and singly, especially during the
period 1679 - 1706.
Ref ID : 1489
1023. Habitat Council The planning and conservation of the dry regions in South
Africa.Anonymous Anonymous , 1984.
Reprint : Not in File,
Keywords : CONSERVATION; DESERTIFICATION CONTROL; VELD MANAGEMENT; WATER
CONSERVATION; EROSION CONTROL
Ref ID : 1459
1024. Haigh, H. Grassing roads and eroded areas in the Drakensberg. South
African Forestry Journal 97:63, 1976.
Reprint : Not in File,
Keywords : EROSION; RESTORATION
Ref ID : 666
1025. Hakkeling, R.T.A. Global assessment of soil degradation - eastern and
southern Africa. Main Report (2 volumes).Anonymous Wageningen:STIBOKA. , 1989.
Reprint : Not in File,
Keywords : SOIL EROSION; LAND DEGRADATION; SOUTHERN AFRICA; STATISTICS
Ref ID : 166
1026. Hall, T.D. South African pastures: retrospective and prospective. South
African Journal of Science 31:59-97, 1934.
Reprint : In File,
Keywords : KAROO DESERTIFICATION; STOCKING RATE; DESERTIFICATION ASSESSMENT;
VEGETATION CHANGE; VELD MANAGEMENT; EROSION
Notes : The author writes that SA is at last realising that she is primarily a
pastoral country and is now almost quite disillusioned about her youthful
ambitions of becoming a second Argentine as regards maize production. Huge sums
of money have recently been appropriated by the government for pasture
investigations, veld management studies, erosion prevention and control, and the
eduction of farmers and the younger generation to the necessity of immediate and
vigorous action if SA is to be saved from becoming a desert. Little time will
be devoted to prospective pastures as the veld and the grasses composing it have
been ably dealt with by other writers from the ecological, phytogeographical and
taxonomic aspects. In this article, pastures will be dealt with more from the
point of view of their exploitation and mismanagement by man in his struggle for
existence.
Ref ID : 167
1027. Hallet, R. Reflections on a dust storm in the Free State. ?Cape Times ,
1990.
Reprint : In File,
Keywords : SOIL EROSION; DESERTIFICATION ASSESSMENT; FREE STATE; EROSION
Notes : The reporter agrees with the sentiments of a reader who wrote of the
tragedy of sand storms in the Free State being symptomatic of soil degradation.
He draws a parallel between these dust storms and the radioactive lichens in
Lappland as indicators of humans prioritising technological advance over the
survival of life. While he points out that philosophers like Heidegger may
argue for "existential revolutions" he prefers to support more practical tactics
like tree planting schemes to combat soil erosion.
Ref ID : 301
1028. Hallward, J.R. An investigation of the areas of potential wind erosion in
the Cape Province, Republic of South Africa.University of Cape Town. , 1988.
Master of Science.
Reprint : In File,
Keywords : SOIL EROSION; DESERTIFICATION ASSESSMENT; WESTERN CAPE; NORTHERN
CAPE; EASTERN CAPE; WIND EROSION; MAPS; EROSION; MODELS; RAINFALL; RUNOFF; VELD
CONDITION; CONSERVATION
Notes : Only a few pages have been copied. The conclusions reached are that
from the methods used in this study it is not possible to produce a clear map of
the wind erosion hazard in the Cape Province. It is of interest to note that
although neither of the models indicate that there is a severe wind erosion
hazard in the Cape Province, observations and reports indicate otherwise. The
author goes as far as to suggest that virtually the entire province, with the
possible exception of the all year rainfall zone and the forested areas, is
susceptible to wind erosion. This conclusion is based on observations made
while driving through various parts of the province and from comments made by
various individuals through the course of the research. For example, the
susceptibility of the Cape Flats area to the east of Cape Town has been clearly
illustrated by the problems of blowing sand during the extensive road
construction that has been ongoing for the past few years. The complaints of
the residents of Khayalitsha and of communities on the western side of Cape Town
will also attest to the problems of wind erosion. This, however, need not be an
ongoing problem, as once construction has been completed and vegetation has been
established, much of the blowing sand should be controlled. A close examination
of many parts of the Karoo, on the other hand, will reveal ripple marks on
exposed areas, the accumulation of sand and debris at the base of bushes and
where sand blasting is severe the loss of bark on the downwind side of some
bushes. This is evidence that wind erosion has been a long term problem. That
the problem goes unnoticed by people in many areas including the Karoo is not
surprising due to the insidious nature in which the effects of wind erosion
accumulate. Nonetheless it is surprising that the models fail to adequately
reflect actual conditions. It is for this reason that the author concludes that
in the Karoo and inland areas of Namaqualand, management is the primary factor
responsible for wind erosion. Acocks (1953, 5 - 6), in his oft quoted treatise
on the Veld types of SA discusses the effect of improper management. He regards
continuous selective grazing as having had three main impacts on the Karoo.
Firstly, it has changed the species composition of the veld so that good grazing
species have been replaced by less useful ones. Secondly, soil cover has been
reduced giving rise to a loss of water through run-off, sheet erosion and wind
erosion. The net result is a silting of rivers and a scouring of channels which
has increased donga formation. It thus appears that the effects of improper
management have long been an issue of concern and that even in the 1950's it was
apparent that management was a significant factor in giving rise to erosion and
veld degradation. SA is an arid country. Most of the Cape Province falls into
either a summer or winter rainfall zone and as a result different parts of the
province are particularly arid at different times during the year. It is during
the dry season that the wind erosion hazard is most severe. SA also experiences
a cyclical rainfall pattern of 18-20 years duration. It is during the 9-10 year
dry period that the wind erosion hazard is greatest. Climatic data are
notoriously poorly behaved in their statistical properties. As a result they
should be regarded with caution and not used for predictive purposes.
Nonetheless as veld conditions cannot be changed immediately it seems important
that management guidelines be based on maintaining an adequate ground cover
during the drier years so as to avoid excessive erosion during these periods.
It is suggested that further research is required with regard to grazing
management in the Karoo. It is essential that one of the goals of management be
veld conservation in order to improve and retain the productivity of the Karoo.
It is only by doing so, that the threat of increasing desertification of which
wind erosion is only a part, can be brought under control.
Ref ID : 453
1029. Hanbidge, G. A study of gully erosion: a Natal donga. Unpublished third
year student report. Geographical & Environmental Sciences, University of Natal,
Durban. 1983.
Reprint : Not in File,
Keywords : SOIL EROSION; KWAZULU NATAL
Ref ID : 1936
1030. Hanbidge, G. A study of gully erosion: a KZN donga. 1983.
Reprint : Not in File,
Keywords : EROSION
Notes : An unpublished third year student report, Geographical and Environmental
Sciences, University of KZN, Durban.
Ref ID : 1419
1031. Hanekom, F. Draft national enviromental management bill. Government
Gazette 397(19031):1-48, 1998.
Reprint : In File,
Keywords : POLICY; GOVERNMENT INITIATIVES; LEGISLATION; ENVIRONMENTAL POLICY
Ref ID : 850
1032. Hanvey, P.M., Dardis, G.F., and Beckedahl, H.R. Soil erosion on a
subtropical coastal dune complex, Transkei, southern Africa. Geojournal
23(1):41-48, 1991.
Reprint : In File,
Keywords : SOIL EROSION; TRANSKEI
Ref ID : 849
1033. Hanvey, P.M., Dardis, G.P., and Beckedahl, H.R. Gully development in
coastal dune systems, Mbolompo Point, Transkei, Southern Africa. Geojournal
23(1):41-48, 1990.
Reprint : Not in File,
Keywords : TRANSKEI; SOIL EROSION
Ref ID : 2017
1034. Harding, G.B. and Bate, G.C. The occurrence of invasive Prosopis species
in the north-western Cape, South Africa. South African Journal of Science
87:188-192, 1991.
Reprint : Not in File,
Ref ID : 1174
1035. Harding, G.H. The genus prosopis as an invasive alien in South
Africa.University of Port Elizabeth. :i-195, 1988. Prosopis species are thicket
forming trees or multi-stemmed shrubs belonging to Fabaceae. They were
introduced into southern Africa in 1894 as fodder and shade plants but have
since invaded vast areas of the arid north-western Cape. The taxonomy of the
species found in SA is discussed, suggesting that there are two distinct groups
present, namely invasive and non-invasive forms. The invasive group consists of
P. Velutina, P. glandulosa var. torreyana and P. juliflora. The non-invasive
group consists of P. chilensis and P. glandulosa var. glandulosa. The
possibility of hybridization between these species is mentioend but not
confirmed. The distribution of the species was determined by a postal survey,
herbarium specimens and a limited collection. This showed that the centre of
spread is the Kenhardt/Carnarvon district but that there is a large area over
which the trees are scattered. The actual area estimated to be covered with
Prosopis is 20 000 ha. The area of potential spread and the pattern of spread
were determined from Landsat Images. This showed that the potential area
available for Prosopis is about 935 000 ha. The pattern of spread was
determined using aerial photographs of the farm Humansdam and was found to be
directly related to above-normal rainfall events. The type of soil does not
influence the distribution of the trees but the soil depth and availability of
ground water does. Boreholes were used to collect sediment samples while a
hammer seismograph was used to determine sediment depth. This showed that
Prosopis has a phraetophytic habit and can be expected to be a problem in areas
with either shallow groundwater and deep sediment or areas with high rainfall.
The germinability of the seeds was investigated using acid and boiling water
scarification. This showed a requirement for scarification and that acid was
more effective than boiling water. Once scarified the seeds germinate readily,
have no light requirement but do have a temperature requirement with 30/20oC
(day/night) being most effective. Seeds exposed in the field were found to
decay rapidly when buried at 10 cm., with 98% damage being recorded after 18
months. Damage to seeds on the soil surface was considerably lower with only
58% of the seeds being destroyed in that time period. The effect that domestic
and wild animals have on seed dispersal was investigated over a 1 km2 plot.
These data suggest that porcupine and bat-eared fox with 7,38 and 2,53 seeds g-1
dung respectively are the major distributors of seeds. However the distance
over which they spread the seed is limited. Domestic stock have only 0,0335
seeds g-1 dung but their range is considerably greater. The potential of
Prosopis pods as a sheep feed was investigated. Sheep mass gains were monitored
as well as the number of undamaged seeds passed in the faeces. This showed that
although Prosopis pods are suitable as a feed, they should not be used
continuously as this resulted in fluctuating mass gain and decreased seed
damage. The extent of damage to seeds varied between sheep and with time, with
a mean of 92,5% seeds being rendered non-viable. Chemical control was
investigated using aerial foliar-applied herbicides, with Knapsacks and with a
high pressure, low volume foam applicator. Cut-stump and soil application were
also included. Cut-stump proved the most effective while extreme climatic
conditions made foliar application difficult and only moderately successful.
The efficacy of herbicides applied to the soil is erratic because of limited and
erratic rainfall. Trees that have rooted into the groundwater i.e. those
growing as phraetophytes are not as stressed as those growing on the fringes of
the Carnarvon Leegte. Pre-dawn water potential values of phraetophytic trees
were found to be about -1,0 MPa and dropped to -2,7 MPa at midday. Trees with
water potential values as slow as -5,5 MPa were presumed to be growting non-
phraetophytically. Photosynthetic studes showed that Prosopis has a light
compensation point of more than 80 micro-mols m-2s-1. The daily photosynthetic
pattern of Prosopis showed a midday peak of 14 micro mols CO2 m-2s-1. The
status of Prosopis as a weed is discussed and the data used to determine whether
Prosopis is an undesirable or economic plant.Doctoral Dissertation.
Reprint : In File,
Keywords : ALIEN PLANTS; SOUTHERN AFRICA; RAINFALL
Ref ID : 2147
1036. Harding, W.R. The ecology of some urban-impacted coastal vleis on the Cape
Flats near Cape Town, with special reference to phytoplankton
periodicity.University of Cape Town. , 1992.
Reprint : Not in File,
Notes : Unpublished M.Sc. thesis, Freshwater Research Unit, Zoology Department,
University of Cape Town.
Ref ID : 1831
1037. Hardy, M.B. Short-term effects of cattle-to-sheep ratio and stocking rate
on patch grazing in sour grassveld. African Journal of Range and Forage Science
12(3):121-127, 1995.
Reprint : In File,
Keywords : STOCKING RATE
Abstract : The short-term effects of stocking rate (AUE ha-1) and cattle-to-
sheep ratio on the extent and severity of patch grazing and on patch size were
evaluated. The extent of patch grazing was proprotional to stocking rate, and
livestock species had a small but significant effect. Patch size was also a
function of size distribution when stocked at the same number of AUE ha-1. The
severity of grazing within a patch was influenced by both stocking rate and
cattle-to-sheep ratio. Recommendations that cattle should be in greater
proportion (in terms of AUE ha-1) than sheep, which are aimed at limiting the
severity of grazing by sheep, are supported. However, severe grazing within
patches is an inevitable consequence of sheep grazing irrespective of the
stocking rate or cattle-to-sheep ratio implied.
Ref ID : 1059
1038. Hardy, M.B. and Hurt, C.R. An evaluation of veld condition assessment
techniques in Highland Sourveld. Journal of the Grassland Society of southern
Africa 6(2):51-58, 1989.
Reprint : In File,
Keywords : VELD CONDITION; GRASSLAND; KWAZULU NATAL
Abstract : An evaluation of six methods used to index veld condition showed that
the majority provided indices that were insensitive to long-term grazing impact.
However, certain species were found to either increase or decrease in relative
abundance with an increase in grazing intensity. A key species method is
therefore suggested to be a potentially sensitive approach for indexing veld
condition in relation to grazing management in the Highland Sourveld.
Ref ID : 1788
1039. Hardy, M.B. and Mentis, M.T. Grazing dynamics in sour grassveld. South
African Journal of Science 82:566-572, 1986.
Reprint : In File,
Keywords : MODELS; LIVESTOCK PRODUCTION; CARRYING CAPACITY; STOCKING RATE
Abstract : Present understanding of local grazing ecosystems is based on studies
focused on single components and processes in relative isolation. The
mathematical stimulation presented here is intended to relate components and
improve the testability and predictive capacity of theory. The model simulates
(1) the response of the species composition of the veld to grazing livestock,
and (2) livestock production from veld. It is assumed that grazing intensity
affects floristics because of the variable tolerance of plant species to
grazing. Further, animal performance is assumed to depend partly on floristics,
since plant species differ in palatability and nutritive value. Modelled animal
production per hectare is not universally better under rotational than under
continuous grazing, the latter being of merit for veld in 'poor' condition.
Both commercial and subsistence graziers are locked into 'overgrazing'. The
seasonal production of forage sensitively affects animal performance, implying
the importance to modelling of grass growth and its response to grazing. A
single value for the carrying capacity of veld for livestock is not evident.
The optimal stocking rate, the determination of which the model can facilitate,
depends on the grazier's objectives, the starting state of his veld, his
management system and economic circumstances.
Ref ID : 1062
1040. Hardy, M.B. and Walker, R.S. Determining sample size for assessing species
composition in grassland. Journal of the Grassland Society of southern Africa
8(2):70-73, 1991.
Reprint : In File,
Keywords : VELD CONDITION; GRASSLAND; MONITORING
Abstract : Species composition is measured in grasslands for a variety of
reasons. Commonly, observations are made using the wheel-point apparatus.
However, the problem of determining optimum sample size has not yet been
satisfactorily resolved. In this study the wheel-point apparatus was used to
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