TY - JOUR A1 - Coetzee-Van Rooy, Susan A1 - Peters, Arne T1 - A portrait-corpus study of language attitudes towards Afrikaans and English JF - Language matters : studies in the languages of Africa N2 - Language portraits are useful instruments to elicit speakers' reflections on the languages in their repertoires. In this study, we implement a "portrait-corpus approach" (Peters and Coetzee-Van Rooy 2020) to investigate the conceptualisations of the languages Afrikaans and English in 105 language portraits. In this approach, we use participants' reflections about their placement of the two languages on a human silhouette as a linguistic corpus. Relying on quantitative and qualitative analyses using WordSmith, Statistica and Atlas.ti, our study shows that Afrikaans is mainly conceptualised as a language that is located in more peripheral areas of the body (for example, the hands and feet) and, hence, is perceived as less important in participants' repertoires. The central location of English in the head reveals its status as an important language in the participants' multilingual repertoires. We argue that these conceptualisations of Afrikaans and English provide additional insight into the attitudes towards these languages in South Africa. KW - language attitudes KW - language portraits KW - portrait-corpus approach KW - multilingualism KW - South Africa KW - Afrikaans KW - English Y1 - 2021 U6 - https://doi.org/10.1080/10228195.2021.1942167 SN - 1022-8195 SN - 1753-5395 VL - 52 IS - 2 SP - 3 EP - 28 PB - Routledge, Taylor & Francis Group CY - Abingdon ER - TY - JOUR A1 - Hickmann, Thomas A1 - Stehle, Fee T1 - The Embeddedness of Urban Climate Politics in Multilevel Governance BT - a Case Study of South Africa’s Major Cities JF - The journal of environment & development : a review of international policy N2 - Numerous scholars have lately highlighted the importance of cities in the global response to climate change. However, we still have little systematic knowledge on the evolution of urban climate politics in the Global South. In particular, we lack empirical studies that examine how local climate actions arise in political-administrative systems of developing and emerging economies. Therefore, this article adopts a multilevel governance perspective to explore the climate mitigation responses of three major cities in South Africa by looking at their vertical and horizontal integration in the wider governance framework. In the absence of a coherent national climate policy, Johannesburg, Cape Town, and Durban have developed distinct climate actions within their jurisdictions. In their effort to address climate change, transnational city networks have provided considerable technical support to these cities. Yet, substantial domestic political-economic obstacles hinder the three cities to develop a more ambitious stance on climate change. KW - climate change KW - developing and emerging economies KW - local climate policy making KW - multilevel governance KW - South Africa KW - transnational city networks Y1 - 2018 U6 - https://doi.org/10.1177/1070496518819121 SN - 1070-4965 SN - 1552-5465 VL - 28 IS - 1 SP - 54 EP - 77 PB - Sage Publ. CY - Thousand Oaks ER - TY - JOUR A1 - Fairey, Brenton J. A1 - Timmerman, Martin Jan A1 - Sudo, Masafumi A1 - Tsikos, Harilaos T1 - The role of hydrothermal activity in the formation of Karst-hosted manganese deposits of the Postmasburg Mn Field, Northern Cape Province, South Africa JF - Minerals N2 - The Postmasburg Manganese Field (PMF), Northern Cape Province, South Africa, once represented one of the largest sources of manganese ore worldwide. Two belts of manganese ore deposits have been distinguished in the PMF, namely the Western Belt of ferruginous manganese ores and the Eastern Belt of siliceous manganese ores. Prevailing models of ore formation in these two belts invoke karstification of manganese-rich dolomites and residual accumulation of manganese wad which later underwent diagenetic and low-grade metamorphic processes. For the most part, the role of hydrothermal processes and metasomatic alteration towards ore formation has not been adequately discussed. Here we report an abundance of common and some rare Al-, Na-, K- and Ba-bearing minerals, particularly aegirine, albite, microcline, banalsite, serandite-pectolite, paragonite and natrolite in Mn ores of the PMF, indicative of hydrothermal influence. Enrichments in Na, K and/or Ba in the ores are generally on a percentage level for most samples analysed through bulk-rock techniques. The presence of As-rich tokyoite also suggests the presence of As and V in the hydrothermal fluid. The fluid was likely oxidized and alkaline in nature, akin to a mature basinal brine. Various replacement textures, particularly of Na- and K- rich minerals by Ba-bearing phases, suggest sequential deposition of gangue as well as ore-minerals from the hydrothermal fluid, with Ba phases being deposited at a later stage. The stratigraphic variability of the studied ores and their deviation from the strict classification of ferruginous and siliceous ores in the literature, suggests that a re-evaluation of genetic models is warranted. New Ar-Ar ages for K-feldspars suggest a late Neoproterozoic timing for hydrothermal activity. This corroborates previous geochronological evidence for regional hydrothermal activity that affected Mn ores at the PMF but also, possibly, the high-grade Mn ores of the Kalahari Manganese Field to the north. A revised, all-encompassing model for the development of the manganese deposits of the PMF is then proposed, whereby the source of metals is attributed to underlying carbonate rocks beyond the Reivilo Formation of the Campbellrand Subgroup. The main process by which metals are primarily accumulated is attributed to karstification of the dolomitic substrate. The overlying Asbestos Hills Subgroup banded iron formation (BIF) is suggested as a potential source of alkali metals, which also provides a mechanism for leaching of these BIFs to form high-grade residual iron ore deposits. KW - manganese ore KW - Postmasburg manganese field KW - hydrothermal KW - karst KW - South Africa Y1 - 2019 U6 - https://doi.org/10.3390/min9070408 SN - 2075-163X VL - 9 IS - 7 PB - MDPI CY - Basel ER - TY - JOUR A1 - Mielke, Christian A1 - Bösche, Nina Kristine A1 - Rogass, Christian A1 - Kaufmann, Hermann A1 - Gauert, Christoph A1 - de Wit, Maarten T1 - Spaceborne mine waste mineralogy monitoring in South Africa, applications for modern push-broom missions: Hyperion/OLI and EnMAP/Sentinel-2 JF - Remote sensing N2 - Remote sensing analysis is a crucial tool for monitoring the extent of mine waste surfaces and their mineralogy in countries with a long mining history, such as South Africa, where gold and platinum have been produced for over 90 years. These mine waste sites have the potential to contain problematic trace element species (e. g., U, Pb, Cr). In our research, we aim to combine the mapping and monitoring capacities of multispectral and hyperspectral spaceborne sensors. This is done to assess the potential of existing multispectral and hyperspectral spaceborne sensors (OLI and Hyperion) and future missions, such as Sentinel-2 and EnMAP (Environmental Mapping and Analysis Program), for mapping the spatial extent of these mine waste surfaces. For this task we propose a new index, termed the iron feature depth (IFD), derived from Landsat-8 OLI data to map the 900-nm absorption feature as a potential proxy for monitoring the spatial extent of mine waste. OLI was chosen, because it represents the most suitable sensor to map the IFD over large areas in a multi-temporal manner due to its spectral band layout; its (183 km x 170 km) scene size and its revisiting time of 16 days. The IFD is in good agreement with primary and secondary iron-bearing minerals mapped by the Material Identification and Characterization Algorithm (MICA) from EO-1 Hyperion data and illustrates that a combination of hyperspectral data (EnMAP) for mineral identification with multispectral data (Sentinel-2) for repetitive area-wide mapping and monitoring of the IFD as mine waste proxy is a promising application for future spaceborne sensors. A maximum, absolute model error is used to assess the ability of existing and future multispectral sensors to characterize mine waste via its 900-nm iron absorption feature. The following sensor-signal similarity ranking can be established for spectra from gold mining material: EnMAP 100% similarity to the reference, ALI 97.5%, Sentinel-2 97%, OLI and ASTER 95% and ETM+ 91% similarity. KW - mine waste KW - spatial extent KW - gold KW - platinum KW - South Africa KW - EnMAP KW - OLI KW - Hyperion KW - Sentinel-2 KW - iron feature depth (IFD) Y1 - 2014 U6 - https://doi.org/10.3390/rs6086790 SN - 2072-4292 VL - 6 IS - 8 SP - 6790 EP - 6816 PB - MDPI CY - Basel ER - TY - JOUR A1 - Paasche, Hendrik A1 - Eberle, Detlef T1 - Automated compilation of pseudo-lithology maps from geophysical data sets a comparison of Gustafson-Kessel and fuzzy c-means cluster algorithms JF - Exploration geophysics : the bulletin of the Australian Society of Exploration Geophysicists N2 - The fuzzy partitioning Gustafson-Kessel cluster algorithm is employed for rapid and objective integration of multi-parameter Earth-science related databases. We begin by evaluating the Gustafson-Kessel algorithm using the example of a synthetic study and compare the results to those obtained from the more widely employed fuzzy c-means algorithm. Since the Gustafson-Kessel algorithm goes beyond the potential of the fuzzy c-means algorithm by adapting the shape of the clusters to be detected and enabling a manual control of the cluster volume, we believe the results obtained from Gustafson-Kessel algorithm to be superior. Accordingly, a field database comprising airborne and ground-based geophysical data sets is analysed, which has previously been classified by means of the fuzzy c-means algorithm. This database is integrated using the Gustafson-Kessel algorithm thus minimising the amount of empirical data processing required before and after fuzzy c-means clustering. The resultant zonal geophysical map is more evenly clustered matching regional geology information available from the survey area. Even additional information about linear structures, e. g. as typically caused by the presence of dolerite dykes or faults, is visible in the zonal map obtained from Gustafson-Kessel cluster analysis. KW - cluster analysis KW - data integration KW - airborne KW - South Africa KW - Gustafson-Kessel KW - fuzzy c-means Y1 - 2011 U6 - https://doi.org/10.1071/EG11014 SN - 0812-3985 VL - 42 IS - 4 SP - 275 EP - 285 PB - CSIRO CY - Collingwood ER -