Spelling suggestions: "subject:"south africa"" "subject:"south affrica""
21 |
Privatisation and deregulation policies in South Africa.Mfuku, Nkosana January 2006 (has links)
<p>This research report examined the key policies of globalisation namely, privatisation and deregulation of services and also their implication on the Tri-partite alliance. Because they have impacted negatively on major economic sectors, particularly to those that help the needy. Therefore, the study explores these initiatives, which has been debatable in South Africa under the dominant understanding of &lsquo / progress&rsquo / or &lsquo / development&rsquo / .</p>
<p><br />
The Objective of the study is to lay the basis for the examination and evaluation of policy option with regard to privatisation and deregulation of services in South Africa and to engage South Africa effectively in global policy debates and adjust in global trends and negotiations within the region (SADC) and other international countries. It examines global challenges and opportunities / threats for South Africa as a developing country in the emerging global order.</p>
<p><br />
This study also attempts to provide answers to several questions concerning privatisation and deregulation of public services in South Africa. To the poor, is deregulation and privatisation of state assets threatening to become the new apartheid, which is an instrument of exclusion, not just from a better life but even from the very basic services? How are workers and including the poorest of the poor affected by the status of deregulation and privatisation? Do the timing and specifics of these processes matter? Who should attempt to regulate the auction, as some of government officials seems to be corrupt? And which prior restructuring policies are worth implementing?</p>
|
22 |
Petrographic characterization of sandstones in borehole E-BA1, Block 9, Bredasdorp Basin, Off-Shore South Africa.Van Bloemenstein, Chantell Berenice January 2006 (has links)
<p>The reservoir quality (RQ) of well E-BA1 was characterized using thin sections and core samples in a petrographic study. Well E-BA1 is situated in the Bredasdorp Basin, which forms part of the Outeniqua Basin situated in the Southern Afircan offshore region. Rifting as a result of the break up of Gondwanaland formed the Outeniqua Basin. The Bredasorp Basin is characterized by half-graben structures comprised of Upper Jurassic, Lower Cretaceous and Cenozoic rift to drift strata. The current research within the thesis has indicated that well E-BA1 is one of moderate to good quality having a gas-condensate component.</p>
|
23 |
Private padvragvervoer in Suid-Afrika18 February 2014 (has links)
M.Com. (Economics) / The objective of this study was to obtain information that will enable the identification of the role, nature and magnitude of private road freight transport in the South African economy. The underlying rationale was the lack of information in this regard in South Africa. Information about private road freight transport was obtained on a sectoral basis by means of a literature analysis and an empirical investigation.
|
24 |
The contribution of agriculture to the economic growth of South Africa31 August 2011 (has links)
M.Comm. / The agricultural sector is important in South Africa, because it contributes approximately 4 percent to the country’s Gross Domestic Product. Agriculture can contribute significantly to economic growth, by means of food production and job creation, and thereby it can play an important role in reducing poverty. This paper examines the contribution of agriculture to economic growth in South Africa, and its possible role in poverty alleviation. It begins by conducting a literature review of the contribution of agriculture to economic growth. In particular, it examines two stages of farming, namely, the subsistence and commercial stages, to determine how each of these contributes to economic growth and poverty alleviation. It finds that both of these stages have undergone little improvement over the years and have performed poorly. Next, the challenges that prevent the farming sector from performing better are described and investigated in detail. Importantly, unavailability of the data in the subsistence sector makes it harder to arrive at a conclusion as to whether agriculture contributes to poverty alleviation. Despite these challenges, the study finds that agriculture remains the key to survival for most of the rural poor. Finally the paper draws conclusions and makes recommendations for policy measures to increase growth in the agricultural sector based on the findings of the research. The key conclusion emanating from this study is that agriculture does not indeed contribute to economic growth and that it is able to alleviate poverty. However, resources such as land, skilled labour, machinery and capitals are a major limiting factor. As for recommendations, a critical strategy must be to recapitalise agriculture, investing more heavily in this sector and in programmes to develop rural economic and social infrastructure. Public investment needs to be directed in particular towards promoting agricultural research and extension, improving access to financial services, providing investment incentives, and increasing access of the poor to support services and productive resources. The study concludes that data and information should be separated between subsistence and commercial farmers to be able to determine whether agriculture contributes to poverty alleviation.
|
25 |
Analysis of the determinants of poverty in South AfricaKgaphola, Hlali Kemedi January 2016 (has links)
A research dissertation submitted in partial fulfilment of a Master of Management in
Public Policy (MMPP)
The University of Witwatersrand
Wits School of Governance
26 February 2015 / This research dissertation investigates what factors drive poverty in South Africa using annual data from 1996 to 2013. In an attempt to contribute towards a better understanding of what contributes to poverty in South Africa, the researcher adopted three types of research questions: a contextual research question, a main research question and an applied research question. The central questions of this study was “what drives poverty in South Africa?” and “how do these drivers influence poverty trends in South Africa?” The study recognises poverty as a multi-dimensional phenomenon, in addition to the unidimensional money-metric definition of poverty for analysis purposes. Consequently although the study adopts the monetary definition of poverty as a framework to poverty analysis; it also incorporates other variables that capture the multi-dimensional nature of poverty relevant to the South African context. The study uses various data analysis tools including descriptive statistics, line graphs, bivariate analysis, and trend analysis to investigate the relationship between poverty and the variables in this study. Consistent with Klasen (2000) and Finn et al. (2013), the main findings were that there is a negative relationship between poverty and government expenditure on health, housing, energy, public order and safety, and access to credit in South Africa. On the contrary, government expenditure on education is found not to reduce poverty in South Africa, neither is unemployment found to increase poverty in South Africa. The research concluded that although certain variables are expected to reduce or increase poverty, remedial policy interventions by Government and country specific economic structure mitigate these a prior expectations. From these findings the researcher makes recommendations, contributing to how scholars (and government) can further their attempt to alleviate poverty in South Africa. / MT 2018
|
26 |
Middle Permian continental biodiversity changes as reflected in the Beaufort Group of South Africa: a bio-and lithostratigraphic review of the Eodicynodon, Tapinocephalus and Pristerognathus assemblage zonesDay, Michael Oliver 04 March 2014 (has links)
The fluvio-lacustrine rocks of the Beaufort Group, South Africa have long been
known for their tetrapod fossil record, which is the richest and most complete
Middle Permian to Middle Triassic record for any terrestrial sequence in the world.
The abundance of fossil material has enabled the Beaufort Group to be
biostratigraphically subdivided into between 8 and 10 tetrapod assemblage zones, of
which the lowest three (Eodicynodon, Tapinocephalus and Pristerognathus) are attributed to
the Middle Permian. These lower assemblage zones record the earliest therapsiddominated
faunas and, because they were recorded during a largely uninterrupted
period of deposition, make the Beaufort Group the only place in the world where
biodiversity change through the terrestrial Middle Permian can be effectively studied.
In the last two decades, much interest has focused on an extinction of marine
invertebrates at or close to the end of the Middle Permian (Guadalupian epoch), but
the existence of a concurrent extinction in the terrestrial realm is contentious. The
Beaufort Group is already well known to record the Permo-Triassic Mass Extinction
but it also records an earlier extinction at the top of the Tapinocephalus Assemblage
Zone (AZ). This extinction is very poorly understood but recent radiometric dates
for many Permian assemblage zones of the Beaufort Group have confirmed a Middle
Permian age for Eodicynodon, Tapinocephalus and Pristerognathus assemblage zones and
suggest that the end-Tapinocephalus AZ extinction may coincide with the marine
extinctions.
A recently produced GIS database that accommodates all Beaufort Group fossil
material curated in South Africa formed the basis on which the stratigraphic range of
individual specimens was calculated. To put the fossil localities in a stratigraphic
context, lithostratigraphic information was retrieved from the literature and extensive
fieldwork was conducted, which measured stratigraphic sections in key areas and
traced the surface outcrop of lithostratigraphic units. In order to compensate for
lateral variations in lithostratigraphy, the basin was split into sectors, each
represented by a stratigraphic section. The stratigraphic ranges of fossil specimens
and, subsequently, of genera and families could then be calculated and a workable
biostratigraphic subdivision of the Middle Permian Beaufort Group proposed.
The Abrahamskraal Formation, which forms the majority of the Middle Permian
Beaufort sequence, can be divided into six lithostratigraphic members based on the
occurrence of sandstone ‘packages’. These members were traced laterally across the
Basin and their correspondence with fining-upwards cycles was refined and
correlated with the newly defined biostratigraphic units. This refined two-pronged
stratigraphic subdivision allowed the recognition of a waning period of subsidence in
the proximal sector of the Karoo Basin during the Middle Permian.
Stratigraphic ranges of individual genera were found to be far more heterogeneous
than previously recognised. Dicynodont genera are useful biostratigraphic indicators
due to their relative abundance and well-defined stratigraphic ranges, while
dinocephalians and pareiasaurs are clustered in the upper part of the Abrahamskraal
Formation. The stratigraphic range of Eodicynodon extends further up in the
Abrahamskraal Formation than was previously recognised. The Tapinocephalus AZ is
restricted to approximately the upper fifth of the Abrahamskraal Formation and is
characterised by advanced tapinocephalid dinocephalians and the pareiasaur
Bradysaurus. Between these two biozones is a stratigraphic interval dubbed the mid-
Abrahamskraal Formation Transition Zone, where both Eodicynodon and advanced
tapinocephalids coexisted.
A 75 % loss of generic diversity occurred between the upper Tapinocephalus AZ and
the base of the Pristerognathus AZ, which corresponds to a stratigraphic interval
between the mid-Karelskraal Member of the Abrahamskraal Formation and the mid-
Poortjie Member of the Teekloof Formation. Several taxa that survive the end-
Tapinocephalus AZ extinction, and are relatively common in the overlying
Pristerognathus AZ (scylacosaurid therocephalians, the dicynodont genus Eosimops and
the parareptile Eunotosaurus), all became extinct in the upper Poortjie Member at a
time when generic originations are increasing. This suggests a second wave of
extinctions in a similar fashion to that recorded at the Permo-Triassic boundary.
|
27 |
A profile of rape during residential robberies in Gauteng, South Africa between 2002 and 2012Chowles, Jacqui 27 July 2016 (has links)
A research report submitted to the Faculty of Humanities, University of the Witwatersrand, Johannesburg in partial fulfilment of the requirements for the degree of Masters in Community-based Counselling Psychology on 15 March 2016 / Despite the often publicised occurrence of residential robberies being accompanied with additional forms of violence there is a limited amount of research exploring these forms of intersecting violence, specifically within the South African context. The latest statistics released by the South African Police Service (2015) indicate that residential robberies are continuing to increase. The co-occurrence of rape in such residential robberies is under-studied. Therefore, the aim of this study was to explore and describe a profile of residential robberies that are accompanied by rape in Gauteng, South Africa between 2002 and 2012. This was done by exploring the temporal, sociodemographic and situational factors related to reported instances of this crime. The study consisted of cases obtained by the Crime Administration System (CAS). The study focused specifically on instances of reported residential robbery, in Gauteng. Overall there were 68178 cases analysed, with 1104 cases containing instances of reported co-occurring rape. The initial descriptive results indicated that specific variables significantly influence the co-occurrence of rape during a residential robbery. Whereby, there has been a significant increase in the proportion of rapes co-occurring within the 2002 to 2012 period Additionally, binary logistic regression analysis showed that Black females between the ages of 12 and 17 years are the demographic group most at risk when other situational factor are additionally present. Other findings of the regression indicate that there is an increased risk of a rape co-occurring during the residential robbery; over the weekend, between the hours of 00:00 and 06:59 and when no firearm is used as the method of entry or during the residential robbery. Overall, the study present significant findings related to this specific co-occurring crime and a number of areas that can be further explored in relation to the co-occurrence of rape during residential robbery and other forms of co-occurring violence, specifically in the context of South Africa
|
28 |
Private sector investment in development: prospects and obstacles.Fraser, Fraser Dugan January 1994 (has links)
A research report submitted in partial fulfilment of the requirements for a Master of Arts
degree in the Faculty of Arts, University of the Witwatersrand, Johannesburg. / This report is an exploratory discussion of the prospects for private sector investment in
development initiatives. Based on a set of structured and unstructured interviews, a press review
and a survey of the relevant literature, the report paints to a growth in the areas of commonality
between the worlds of investment and development, in that there is increasing recogniticm of the
need to direct resources to South Africa's poor at the same time as market forces are starting to
play an enlarged role in development. The report argues however, that the social context in which
investors are 'embedded' is very different from that of development practitioners, leading to a
situation in which development projects are seen as risky investments. The difficulty experienced
by private investors in understanding the world of development is identified by the report as the
single largest obstacle to private sector investment in development. The report draws the
conclusion that mediating institutions are required to structure relationships between
development agents and investors. / Andrew Chakane 2018
|
29 |
Privatisation and deregulation policies in South Africa.Mfuku, Nkosana January 2006 (has links)
<p>This research report examined the key policies of globalisation namely, privatisation and deregulation of services and also their implication on the Tri-partite alliance. Because they have impacted negatively on major economic sectors, particularly to those that help the needy. Therefore, the study explores these initiatives, which has been debatable in South Africa under the dominant understanding of &lsquo / progress&rsquo / or &lsquo / development&rsquo / .</p>
<p><br />
The Objective of the study is to lay the basis for the examination and evaluation of policy option with regard to privatisation and deregulation of services in South Africa and to engage South Africa effectively in global policy debates and adjust in global trends and negotiations within the region (SADC) and other international countries. It examines global challenges and opportunities / threats for South Africa as a developing country in the emerging global order.</p>
<p><br />
This study also attempts to provide answers to several questions concerning privatisation and deregulation of public services in South Africa. To the poor, is deregulation and privatisation of state assets threatening to become the new apartheid, which is an instrument of exclusion, not just from a better life but even from the very basic services? How are workers and including the poorest of the poor affected by the status of deregulation and privatisation? Do the timing and specifics of these processes matter? Who should attempt to regulate the auction, as some of government officials seems to be corrupt? And which prior restructuring policies are worth implementing?</p>
|
30 |
Petrographic characterization of sandstones in borehole E-BA1, Block 9, Bredasdorp Basin, Off-Shore South Africa.Van Bloemenstein, Chantell Berenice January 2006 (has links)
<p>The reservoir quality (RQ) of well E-BA1 was characterized using thin sections and core samples in a petrographic study. Well E-BA1 is situated in the Bredasdorp Basin, which forms part of the Outeniqua Basin situated in the Southern Afircan offshore region. Rifting as a result of the break up of Gondwanaland formed the Outeniqua Basin. The Bredasorp Basin is characterized by half-graben structures comprised of Upper Jurassic, Lower Cretaceous and Cenozoic rift to drift strata. The current research within the thesis has indicated that well E-BA1 is one of moderate to good quality having a gas-condensate component.</p>
|
Page generated in 0.107 seconds