made of the feeding behaviour of tame animals in the Nylsvley Nature Reserve in
northern Transvaal bushveld. Seasonal variations in acceptance / rejection
frequencies were used to assign plant species to palatability categores,
allowing for the effects of thorns on leaf accessibility. Palatable species
remained highly acceptable year-round, while unpalatable species were eaten
during restricted time periods. The design of appropriate acceptability indices
for particular animal species is discussed. Interrelationships between
palatability and leaf chemistry, soil nutrient status and inherent plant growth
rates are indicated.
Ref ID : 1944
1565. Paling, W., Stephenson, D., and James, C. Modular rainfall-runoff and
erosion modelling. Water Systems Research Group. Johannesburg:Wits University. ,
1989.
Reprint : Not in File,
Keywords : EROSION
Ref ID : 1013
1566. Palmer, A.R. A qualitative model of vegetation history in the eastern Cape
midlands, South Africa. Journal of Biogeography 17:35-46, 1990.
Reprint : In File,
Keywords : ENVIRONMENTAL HISTORY; EASTERN CAPE; VEGETATION CHANGE; MODELS;
GRASSLAND; SAVANNA; NAMA KAROO; PALAEOENVIRONMENTS; SUCCULENT KAROO
Abstract : A qualitative model of the vegetation history during the glacial-
interglacial sequence in the Graaff-Reinet region of the eastern Cape is
presented. Using a descriptive approach, the distribution patterns of sixty-
eight taxa, which are differential species for Karoo Shrublands, Succulent
Thicket and Karoo Dwarf Shrublands, are investigated relative to the major
southern African biomes. The results indicate that a large proportion of the
differential species in the phytosociological classification show strong
affinity with Grassland and Savanna Biomes. Three species groups found in the
Dwarf Shrublands show strong affinities with the Nama-Karoo biome. The
differential species of the Succulent Thicket have a predominantly subtropical
distribution. Using an historical approach the palaeoenvironment of the region
during the past 20 000 years is discussed briefly. On the basis of the
descriptive and historical perspectives, the following hypothesis is presented.
The general vegetation history of the eastern Cape midlands is a product of
comparatively recent climatic change The Succulent Thicket may have become
established on edaphically favourable sites in the ameliorating conditions of
the warmer, wetter Holocene subsequent to the Last Glacial Maximum. The Dwarf
Shrubland and Succulent Dwarf Shrubland are depauperate in relation to
communities in other southern African biomes, but the relatively large number of
endemics suggests a long history in the region. Their differential species
groups occur under arid conditions, accompanied by soils with high base and
fertility status. The Dwarf Shrublands may have been more extensive during the
drier glacial times on those sites currently occupied by Shrubland. The
Shrublands display the expected affinity with the Grassland and Savanna Biomes.
The small number of endemics suggest that these communities may have occupied
the region in the period since the Last Glacial Maximum. Species with Succulent
Karoo Biome affinity are poorly represented.
Ref ID : 2439
1567. Palmer, A.R. Grazing capacity information system (GCIS).
Grahamstown:Agricultural Research Council. , 1999.
Reprint : In File,
Keywords : MODELS; RAINFALL; CARRYING CAPACITY; CLIMATE CHANGE; AGRICULTURAL
PRODUCTION
Notes : The Grazing Capacity Information System (GCIS) is based on a production
model originally developed by Le Houerou, Bingham and Skerbek(1988) and
described by the formula: P = (1 + B. (r-R) /R ).r.RUE, where P = production for
the given year (kg DM per ha per year); r = rainfall in a given year; R = median
annual rainfall, long term; B = CVP/CVR (coefficient of variation in production
over coefficient of variation in rainfall); and RUE = rain use efficiency.
Primary production and hence short term carrying capacity depends on a number of
local climatic conditions, including rainfall. Variation in primary production
is linked to variation in rainfall amount and distribution. Variability in both
is directly related to aridity. Le Houerou et al, (1988) relate mean annual
primary production to three important indices namely; annual rainfall; rain use
efficiency (RUE) and the ratio of variability in production to variability in
rainfall (B).
Ref ID : 2371
1568. Palmer, A.R., Crook, B.J.S., and Lulke, R.A. Aspects of vegetation and
soil relationships in the Andries Vosloo Kudu Reserve, Cape Province. South
African Journal of Botany , 1988.
Reprint : Not in File,
Keywords : METHODOLOGIES; GRASSLAND; EASTERN CAPE; SOIL PROPERTIES; VEGETATION
DYNAMICS; SUCCULENT KAROO
Notes : The objectives of the research were to examine vegetation aspects and
soil relationships in the Andries Vosloo Kudu reserve in the Cape Province. 1.
Soil samples were collected from 31 permanent 100-m2 quadrats in single
operation in August 1981. 2. The samples were placed in separate watertight
bags for transfer to the laboratory. Other specific details of the methodology
can be seen in the main paper. Grassland samples in the dwarf shrub land and in
the succulent bush clump Portulacaria afra - Ruellia cordata were in a separate
subset. Other specific details of the results are found in the main paper. This
article can be obtained at Rhodes University, Grahamstown. See ref. I.D. no:
2339.
Ref ID : 203
1569. Palmer, A.R., Hobson, C.G., and Hoffman, M.T. Vegetation change in a semi-
arid succulent dwarf shrubland in the eastern Cape, South Africa. South African
Journal of Science 86:392-396, 1990.
Reprint : In File,
Keywords : VEGETATION CHANGE; MONITORING; VEGETATION DYNAMICS; KAROO
DESERTIFICATION; NAMA KAROO; VELD MANAGEMENT
Abstract : A model of vegetation change in the succulent dwarf shrublands of the
Camdebo plain, eastern Cape, is presented using the results of eight 2000-point
samples collected from 1950 to 1988. Three models are developed using reciprocal
averaging, two-way indicator species analysis and trend analysis. All the models
suggest a gradient of change from 1950 to 1988. This gradient is examined for
trend using component line charts of basal cover with 95% confidence limits. The
analysis shows an increase in annual and perennial grasses (Poaceae),
fluctuations in perennial dwarf shrubs, returning to the 1956 levels in 1988,
and stability in succulent dwarf shrubs (Aizoaceae and Mesembryanthemaceae).
Comparison with an adjacent paired plot, subjected to short-duration grazing,
suggests that these changes are a consequence of favourable management by the
grazier. Changes in rainfall seasonality did not provide an explanation for the
fluctuations in grasses and perennial dwarf shrubs. Time series analysis of
rainfall data confirmed the presence of a wet-dry oscillation.
Ref ID : 244
1570. Palmer, A.R. and Hoffman, M.T. Nama-karoo. In: Vegetation of Southern
Africa. edited by Cowling, R.M., Richardson, D.M., and Pierce,
S.M.Cambridge:Cambridge University Press, 1997,p. 167-188.
Reprint : In File,
Keywords : NAMA KAROO; KAROO DESERTIFICATION; BOTANICAL SURVEY; SOUTHERN AFRICA;
POLICY; LAND DEGRADATION; CLIMATE CHANGE; VEGETATION CHANGE
Notes : The authors conclude that the Nama-karoo biome has not attracted the
same level of ecological interest as have the other biomes of southern Africa.
Efforts to focus on the biome by research agencies (notably the Foundation for
Research Development) were short-lived. Although the contributions from the
agricultural institutes in the region have been considerable, their research has
seldom been published in the primary literature. Where they have made important
ecological contributions is in describing the composition and structure of the
vegetation of the region. Despite this work, however, and despite more than a
century of scientific investigation, the functioning of Nama-karoo communities
and ecosystems is still poorly developed. This paucity of ecological knowledge
of the region is regrettable for a number of reasons. The Nama-karoo biome
covers an extensive area on the subcontinent and, largely as a result of its
size and central location, it abuts on all the other major biomes of the
subcontient. It also exists at the arid end of a moisture gradient which extends
into adjacent, more productive vegetation types, especially on its southern and
eastern margins. Degradation of these more mesic regions is thought to
facilitate the expansion of typical Nama-karoo species and a general 'expanding
karoo' hypothesis has had a profound influence on agricultural policy and
financial commitment in the past and continues to do so today. Despite recent
attempts to discount the severity and extent of land degradation in the Karoo
the matter has not been laid to rest. It is crucial that there is renewed
ecological interest in the region, not only to develop a deeper ecological
understanding of the Nama-karoo biome itself but also to understand its dynamics
in relation to the vegetation of the rest of the subcontinent. Extensive
pastoralism and wildlife ranching continue to be the major economic activities
in the biome. Future research priorities should focus on these activities and
include a re-assessment of herbivore preference tables, which have been
presented for the dominant taxa in the biome. Preliminary results suggest that
taxa vary both in photosynthetic rate and palatability, depending on substratum.
Patchiness in the distribution of resources in the landscape appears to impact
on the productivity and dynamics of the ecosystem, with both wild and domestic
herbivores showing seasonal and spatial preferences for patches. Elucidation of
these trends will impact significantly on the rangeland condition assessment
techniques currently being applied by pastoralists. Within the framework of
global climate-change scenarios, testable predictions should be made on the
direction that vegetation changes will take in the biome. Long-term climatic
records in the biome are vital to our continued understanding of climatic
processes, and with the reduction in the number of manned recording stations,
due to de-population, the time length and spatial extent of records is
declining.
Ref ID : 1167
1571. Palmer, A.R., Tanser, F., and Hintsa, M.D. Using satellite imagery to map
and inventorize vegetation status for the Eastern Cape Province. 1997.
Reprint : In File,
Keywords : REMOTE SENSING; SATELLITE IMAGERY; EASTERN CAPE
Ref ID : 2309
1572. Palmer, A.R., Tanser, F., and Hintsa, M.D. Using satellite imagery to map
and inventorize vegetation status for the eastern Cape province. ARC-Range &
Forest Institute. Grahamstown:ARC-Range & Forest Institute. , 1997.
Reprint : In File,
Keywords : SATELLITE IMAGERY; MAPS; EASTERN CAPE; MODELS
Notes : The authors conclude that the veld types in the region are generally in
a moderate to poor condition. The model of Tongway & Ludwig (1997) has
generally been confirmed for the condition of veld in the eastern Cape. The
technique has provided a method which is not dependent upon the vegetation type
being explored. This means that the stratification of the rangeland on the
basis of vegetation types is not necessary, and the same technique can be
applied across the landscape. The technique also permits us to evaluate the
rate at which desertification is taking place in the province. This is
accompanied by a loss of production from the rangeland. Tanser (1997) and
Palmer & Van Rooyen (1997) confirmed this more fully after exploring the MSDI
and NDVI in five different images from five different regions. In the shallow
soils of the eastern Cape, Karoo, Drakensberg and Namaqualand, there was a
negative relationship between MSDI and NDVI i.e. as MSDI increased (condition
declined) the NDVI increased. The NDVI is a satellite derived index of
photosynthetic activity, and can be equated to production. The increase in MSDI
in natural rangeland can be confidently equated with a decrease in annual
production. The technique is extremely cost-effective, as only one band (R1600
per band in 1996) had to be purchased for each scene, and processing was
completed on a Pentium with IDRISI.
Ref ID : 329
1573. Palmer, D.L. and Griffiths, P.G. The erosion problem on chicory lands.
Dohne Agric 6(1):34-35, 1984.
Reprint : In File,
Keywords : SOIL EROSION; CULTIVATION; EROSION; FLOODS
Notes : The authors note that with good, but not abnormal rains in July 1983, it
was once again revealed that serious erosion is taking place on chicory lands.
Soil losses are far exceeding the soil formation process and are thus considered
to be beyond all reasonably acceptable limits. However, as long as virgin soil
is available and the bush clearing process continues, the trend could continue
without adversely affecting the economics of the industry in the short term.
This can only lead the chicory industry into disrepute. The authors suggest
that, although contouring is not in itself a solution to the problem, it does go
some way to improving matters if a few rules are adhered to, such as: (1)
natural watercourses must be retained and established to good grass cover; (2)
no flood water must be allowed to enter the land from adjacent fields and
satisfactory stormwater drains must be constructed; (3) with the present
cultivation practices water will inevitably be silt-laden at times and this silt
must not be allowed to deposit in the contour canals; (4) contours should be
short and not exceed 200 metres' flow in any direction; (5) ridges should be
parallel to the upper contour; (6) canals should be cleared in the annual soil
preparation process; (7) a crop rotation system must be followed; and (8) lands
with slopes exceeding 12% should not be used for chicory production, but be
under permanent plant cover.
Ref ID : 2525
1574. Palmer, R. Rural adaptations in the Eastern Cape, South Africa. Working
Paper no. 11, published in ISBN 99911-31-24-8.Anonymous Working Paper no. 11,
1997.
Reprint : Not in File,
Keywords : EASTERN CAPE; CISKEI; CULTIVATION; LESOTHO; GENDER ASPECTS;
SETTLEMENT IMPACTS; LIVESTOCK PRODUCTION
Notes : The study focuses on two villages, Gwabeni and Gcinisa in the Ciskei
"homeland". It investigates the interplay between gender, household and
environmental change in a specific national context at the grass roots level.
It also highlights an "alien" method of environmental control, behaviour and
perceptions at village level in an underdeveloped area. Data was collected by
primary qualitative methods, in the field or villages where respondents or
participants held discussions with research groups. Data was also collected by
secondary sources through desktop studies. Given the use of resources, the most
conveniently situated location differed for people living in different parts of
the village. Scattered settlement patterns made sense in practical and
environmental terms where natural resources were widely distributed. Field
cultivation was found to be sharply decreasing in both Gwabeni and Gcinisa.
There are several other findings in the study related to field cultivation,
stock farming, and garden cultivation. This working paper is obtainable from
the Institute of Southern African Studies, National University of Lesotho, Roma,
and ISER, Rhodes. See also ID ref. no. 2339.
Ref ID : 2170
1575. Palmer, R.W. Invertebrates in the Orange River, with emphasis on
conservation and management. South African Journal of Aquatic Sciences
22(1/2):3-51, 1996.
Reprint : Not in File,
Keywords : CONSERVATION
Ref ID : 2171
1576. Palmer, R.W. and O'Keeffe, J.H. Transported material in a small river with
multiple impoundments. Freshwater Biology 24:563-575, 1990.
Reprint : Not in File,
Ref ID : 1945
1577. Park, S.W., Mitchel, J.K., and Scarborough, J.N. Soil erosion simulation
on small watersheds: a modified ANSWERS model. Transactions of the ASAE
25(6):1581-1588, 1982.
Reprint : Not in File,
Keywords : SOIL EROSION; EROSION; MODELS
Ref ID : 908
1578. Parker, D. The western Cape lowland fynbos: What is there left to
conserve?! Veld & Flora 68(4):98-101, 1982.
Reprint : In File,
Keywords : FYNBOS; WESTERN CAPE; CONSERVATION; DESERTIFICATION ASSESSMENT
Notes : The area in question, which was the subject of the Lowlands Symposium,
stretches from the Olifants River in the north to the False Bay coast in the
south. The variation of the fynbos over this region is so marked that plant
geographers have subdivided it into three principal groups for the purposes of
establishing truly representative areas for conservation needs. Data which have
been collected by the Threatened Plants Group of the National Programme for
Environmental Sciences have shown that this area carries a total of 270
critically rare, threatened or recently extinct taxa of flowering plants and
ferns. The article describes most serious regional loss of plants in the area;
important ecotonal zones; and ignorance, obstinancy and errors.
Ref ID : 2302
1579. Parsons, R. and Jolly, J. The development of a systematic method for
evaluating site suitability for waste disposal based on geohydrological
criteria.Anonymous Pretoria:Water Research Commission. 485/1/94, 1994.
Reprint : In File,
Notes : The authors conclude that, based on all the reliable waste disposal site
data currently available in SA and the work performed during the research
programme, WASP was found to be capable of providing an accurate and quantified
assessment of a site's suitability for waste disposal, based on geohydrological
criteria. WASP now needs to be applied to a wide range of waste and
geohydrological conditions. Once applied, the performance of the procedure can
then be re-assessed. The objectives of the research project have been achieved
by the development, verification and validation of the Waste-Aquifer Separation
Principle, abbreviated as WASP. The method was based on 29 methods used
throughout the world, but was developed to suit South African conditions. All
reliable waste disposal site data currently available were used in the
verification of the method while the validation of WASP was based on information
from ten well-studied facilities spread throughout the country. A data
reliability rating is coupled to the WASP Index and this allows the value and
reliability of the obtained Index to be readily apparent. A degree of
flexibility is allowed for in the procedure in order to accommodate special or
unique considerations and circumstances. WASP does not, however, replace the
need for appropriate data nor the need for the assessor to be suitably qualified
and experienced in geohydrology.
Ref ID : 809
1580. Parsons, R. and Tredoux, G. The development of a strategy to monitor
groundwater on a national scale.Anonymous Pretoria:Water Research Commission.
482/1/93, 1993.
Reprint : Not in File,
Keywords : HYDROLOGY
Ref ID : 418
1581. Parsons, R. and Tredoux, G. Monitoring groundwater quality in South
Africa: Development of a national strategy. Water SA 21(2):113-116, 1995.
Reprint : In File,
Keywords : HYDROLOGY; MONITORING
Abstract : Little is known about the temporal distribution of groundwater
quality on a national scale in SA. The effective management of the country's
groundwater resources is thus difficult and the need exists for a national
network for monitoring groundwater. A literature-based project was initiated
with the aim of identifying practical strategies to be used in the establishment
of the desired network. Prior to identifying possible strategies, a statement
on monitoring network objectives was developed. Cognisance of special
constraints and considerations such as responsibility and funding was also
taken. Various approaches and strategies for establishing national or regional
monitoring networks were evaluated, the most appropriate of which were proposed
for use in the establishment of a South African network. The strategies
considered aspects such as information needs, available resources, monitoring
frequencies, funding and the use of a pilot-scale study to initiate the network.
A network manager and a Review Committee should be appointed and be responsible
for the establishment of the network. Some technical issues had to be
considered owing to their impact on the strategies to be adopted. Empirical and
hierarchical approaches to the development of the network were considered
essential. Work on the network has subsequently started and many of the
proposed strategies have been adopted.
Ref ID : 1716
1582. Partridge, T.C. Origin and peopling of the Kalahari. South African Journal
of Science 88:119-120, 1992.
Reprint : In File,
Keywords : POPULATION; MONITORING
Notes : This is a book review. The book is titled: The Kalahari Environment and
its author is S.G. Thomas and P.A. Shaw. The author says that few areas of
Africa have seized the imagination of explorers and writers as persistently as
the Kalahari, but no comprehensive treatment of its landscape and people has, in
fact, been attempted since the appearance of Siegfried Passarge's Die Kalahari
in 1904. The present volume is said to be handsomely produced and goes far
towards providing an up-to-date and broad-ranging scientific account of this
fascinating area.
Ref ID : 2228
1583. Partridge, T.C. Evolution of landscapes. In: Vegetation of southern
Africa, edited by Cowling, R.M., Richardson, D.M., and Pierce,
S.M.Cambridge:Cambridge University Press, 1997,p. 5-20.
Reprint : In File,
Keywords : SOUTHERN AFRICA
Ref ID : 1255
1584. Peard, R.H. A tribute to the Soil Conservation Committees of Natal: a
review of their achievments date, Natal:Department of Agriculture & Fisheries,
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