Thesis (MSc)--University of Stellenbosch, 2002. / ENGLISH ABSTRACT: Arid lands comprise some 47.2 % of the world's land surface. Between 32 % and 35 % of these drylands are subject to some form of desertification and land degradation. South Africa is an arid country with water being a major limiting resource. The Nama-Karoo biome is an extensive tract of semi-arid vegetation comprising some 22.7 % of South Africa, characterised by low rainfall and high temperatures. Grazing is the most common form of land use in the country, and particularly in this biome. Aridity and grazing are two factors that make large areas of South Africa (including the Nama-karoo) susceptible to land degradation. The Nama-Karoo biome has been neglected in past research and is an understudied part of South Africa's vegetation. This study is a component of a bigger umbrella project entitled "Restoration of degraded Nama-karoo rangelands: the role of conservation islands". The aim of this project was to assess the role played by isolated hills and mountains (mesas, inselbergs, etc.) in conserving the remnant biological diversity of the Nama-karoo rangelands of Namibia and South Africa. Vegetation composition, seed banks, seedling recruitment, pollination and grazing patterns and intensity on and off isolated mesas in the eastern parts of the Nama-karoo were investigated in the South African component of this project. I report on patterns of 1) plant species diversity and 2) plant communities across the Middelburg District, Eastern Cape, South Africa. Three isolated mesas (Tafelberg, Folminkskop and Buffelskop) and their surrounding plains were selected for this study. Permanent plots were established in broad transects extending from the plains to southeastern slopes, plateaux, north-western slopes and north-western plains of each mesa. Plots were 25 m2 in size, and ten 1 m2 blocks within the 25 m2 plot were randomly selected and sampled. Species composition was recorded and cover values determined for all plants in every subplot. In the eastern Nama-karoo mesas were not found to be higher in Alpha Diversity than their surrounding plains. Plains habitats were mostly equally as diverse as mesa habitats, with some plains habitats being higher in diversity than mesa habitats. Greater differences between mesas and their surroundings were found in a parallel study in the northern parts of the Nama-karoo in Namibia, indicating that mesas are more distinct islands of diversity with an increase in aridity. In the Middelburg District, a greater presence of woody phanerophytes occurred on mesa habitats in comparison with plains habitats, a possible result of the more moist microhabitats on mesas. Cooler, moister conditions on the south-eastern slopes of the mesas led to higher Alpha Diversity there in comparison with the warmer and drier north-western slopes, a phenomenon commonly found in arid areas. In terms of Alpha Diversity, the largest mesa sampled, Tafelberg (450 m above surroundings), was not significantly more diverse than the two smaller mesas (Folminkskop and Buffelskop both being 200 m above surroundings). Tafelberg and Buffelskop were equally high in Beta Diversity, with Folminkskop being much less diverse. Increased Beta Diversity for Tafelberg was explained by the increased size of the mesa (providing a more diverse microhabitat) relative to Folminkskop, which has the same shape and geology but is much smaller in size. High Beta Diversity values for Buffelskop were explained by the presence of degraded communities on the northwestern slopes and plains, while the south-eastern slopes were some of the most diverse habitats sampled in the landscape. Mesas and plains shared few species. Proportionally fewer species were shared between the plateau and slopes of the larger Tafelberg in comparison with the smaller two mesas. Isolation of the plateau could possibly become more distinct with an increase in size of the mesa. However, Tafelberg had more species in common with the surrounding plains than did the smaller mesas. It is suggested that bigger mesas support a more diverse array of microhabitats enabling plains species to occupy selective sites on the slopes of the mesa. Average Shannon-Wiener Alpha Diversity Indices for Middelburg were higher than that of the Nama-karoo in general. This could be explained by the higher precipitation in the eastern parts of the Nama-karoo relative to the rest. Diversity in Middelburg compared favourably with that in other arid lands of North America and Australia and was found to be similar in patterns and determinants of diversity compared to arid lands such as those of the New World. Regarding plant community composition, mesas were found to be distinctly different from their surrounding plains, with no shared communities between mesas and plains. The distribution of communities across the landscape was mainly attributed to a soilmoisture gradient. Mesas, compared to plains, have shallower, rockier soils coupled with very little run-off and naturally higher precipitation due to elevation. This results in a more mesic habitat. Plains, compared with mesas, have little rock cover, high percentages of bare soil and higher run-off rates than mesas, resulting in a more xeric habitat. Habitat differences such as these probably existed before the impact of domestic livestock but overgrazing has probably exacerbated the differences. The dominance structure of plant communities on the plains has probably changed in favour of toxic, spinescent or unpalatable plant species due to selective grazing by livestock. For the two dolerite-capped mesas (Tafelberg and Folminkskop) aspect and the expected cooler, moister conditions on south-eastern slopes as factors determining community composition were overridden by soil type and associated nutrient status. On Buffelskop (sandstone mesa), aspect and slope overrode soil type and associated nutrient status as determinants of community compositions. The potential to use mesas as a source of seeds and propagules to restore degraded plains habitats is low. Approximately 28 % of species were shared between mesas and their surroundings, and not all of these species could be regarded as good colonisers. Generalist, palatable species occurring across the landscape, such as Eragrostis obtusa, Felicia muricata, F. ovata, Fingerhuthia africana, Jamesbrittenia tysonii, Limeum aethiopicum, Pentzia incana and Selago albida could have some potential for future restoration attempts. Mesas are distinct in composition and can be regarded as islands of one vegetation type (mesas) in a sea of a different vegetation type (plains). Mesa habitats are not generally used for grazing by livestock, due to their general inaccessibility, and are not threatened by development. Plant communities in the Middelburg area were very similar In composition to communities identified in other parts of the Nama-karoo. Results from this study suggest that the plains are at present more degraded than the mesa habitats, but it is impossible to conclude whether or not these rangelands have stabilised given current stocking rates and climatic conditions. The Braun-Blanquet classification system proved an effective method to describe plant communities in the semi-arid Nama-karoo. All the plots used during the duration of the study were marked by metal stakes and are therefore of a permanent nature, so that they can be resampled in future. This might possibly shed some light on questions related to resilience, stability and degradation of the karoo. Restoring rangeland in the future is an important option, however, few farmers would, in the short term, be able to afford costly restoration techniques. It is recommended that farmers inspect the condition of their veld on a regular basis, and adjust stocking rates accordingly. Veld should be rested on a regular basis, and assessment should precede the movement of stock to a camp. Most farmers plough denuded areas of veld to encourage restoration, and it is recommended that this practice be combined with reseeding, followed by rest during and shortly after germination of the seed. / AFRIKAANSE OPSOMMING: Ariede areas beslaan tans 47 % van die aarde se land oppervlak. Tussen 32 % en 35 % van hierdie areas is onderworpe aan een of ander vorm van land degredasie. Die Nama- Karoo bioom is 'n ekstensiewe semi-ariede area wat naastenby 47 % van Suid-Afrika beslaan. Die karoo word gekenmerk deur hoë temperature en lae reënval. Suid-Afrika is 'n ariede land en water is 'n beperkende faktor. Weiding is die algemeenste boerderypraktyk, en meer so in ariede areas soos bv. in die karoo. Die droë klimaat en hoë voorkoms van weiding as boerderypraktyk maak ekstensiewe areas (insluitende die karoo) van Suid-Afrika vatbaar vir land degredasie. Hierdie studie is deel van 'n breër projek genaamd: "Restorasie van gedegradeerde Nama-karoo veld: Die rol van bewaringseilande". Die doel van hierdie projek was om die rol te bepaal van ge-isoleerde koppies en berge (mesas, inselberge, ens.) in die bewaring van biologiese diversiteit in die Nama-karoo van Suid-Afrika en Namibië. Plantegroeisamestelling, saadbanke, saailing oorlewing, bestuiwing en weidingsintensiteitlpatrone op koppies en hulle omringende vlaktes in die oostelike dele van die Nama-karoo is ondersoek in die Suid-Afrikaanse komponent van die studie. Ek rapporteer oor patrone van 1) plant diversiteit en 2) plantegroeigemeenskappe in die Middelburg Distrik, Oos-Kaap, Suid-Afrika. Drie ge-isoleerde koppies (Tafelberg, Folminkskop en Buffelskop) en hulle omliggende vlaktes is geselekteeer vir die doel van die studie. Permanente persele is uitgelê in 'n breë lyn vanaf die suid-oostelike vlaktes na die suid-oostelike hang, oor die plato's, noord-westelike hange en noord-westelike vlaktes vir al drie koppies. Persele was 25 m2 in grootte, waarvan tien 1 m2 sub-persele geselekteer is binne die groter 25 m2 blok. Spesies samestelling en bedekkingswaardes is bepaal vir alle plante in al die sub-persele. Mesas was nie hoër in Alpha Diversiteit as hulle omringende vlaktes nie. Vlaktes was meestal net so hoog in diversiteit as die mesas, en somtyds selfs hoër. Groter verskille in diversiteit is gevind in 'n paralelle studie in die noordelike dele van die Nama-karoo in Namibië. Dit dui aan dat mesas moontlik meer definitiewe eilande van diversiteit is in droër gebiede. Meer houtagtige fanerofiete het voorgekom op die mesas in vergelyking met die omliggende vlaktes, 'n moontlike gevolg van 'n natter habitat op die mesas. Suid-oostelike hange was hoër in alfa-diversiteit in vergelyking met noord-westelike hange. Dit is toegeskryf aan die koeler, natter mikrohabitat van die suid-oostelike hange. Die groter mesa (Tafelberg - 450 m bo die vlakte), was nie meer divers as die twee kleiner mesas nie (Folminkskop en Buffelskop is sowat 200 m bo die vlakte). Tafelberg en Buffelskop was ewe hoog in Beta Diversiteit, terwyl Folminkskop heelwat laer was. Hoër Beta Diversiteit vir Tafelberg kan verklaar word deur die groter oppervlak en hoogte van die mesa (voorsien 'n meer diverse mikrohabitat) in vergelyking met Folminkskop. Folminkskop het dieselfde vorm en geologiese geskiedenis as Tafelberg, maar is veel kleiner. Buffelskop was hoog in Beta Diversiteit as gevolg van 'n gedegradeerde gemeenskap op die noord-westelike hang en vlaktes, terwyl die suidoostelike hang baie hoog was in diversiteit. Min spesies kom op beide mesas en vlaktes voor. Minder spesies is gedeel deur die plato en hange van Tafelberg in vergelyking met die plato's en hange van Folminkskop en Buffelskop. Isolasie van die plato kan moontlik hoër wees in groter mesas. Tafelberg (slegs mesa) het meer spesies in gemeen met sy omliggende vlakte as die ander twee mesas. Groter mesas soos Tafelberg kan moontlik 'n meer diverse spektrum van mikrohabitatte bevat, wat sekere vlakte spesies in staat stel om te oorleef op mesa hange. Gemiddelde alfa diversiteit vir die Middelburg Distrik was hoër as die van die res van die karoo. Dit kan verklaar word deur die hoër reënval in die oostelike dele van die karoo relatief tot die meer westelike dele. Diversiteit in Middelburg vergelyk goed met die van ander ariede lande in Noord-Amerika en Australie, terwyl patrone en faktore wat diversiteit bepaal soortgelyk was aan die van gemeenskappe in ariede lande van die Nuwe Wêreld. Mesas en vlaktes het drasties verskil in die samestelling van hulle onderskeie plantegroeigemeenskappe, alhoewel hulle soortgelyk was in diversiteit. Geen plantegroeigemeenskappe het voorgekom op beide mesas en vlaktes nie (gedeelde plantegroeigemeenskappe). Die verspreiding van plantegroeigemeenskappe oor die landskap was toegeskryf aan 'n grond-water gradient. Mesas het, oor die algemeen, vlakker, meer rotsagtige grond en 'n hoër reënval met minder afloop as vlaktes. Vlaktes het minder rotse, 'n hoër persentasies kaal grond en vinniger afloop tempo's na reën as mesas. Hierdie faktore het tot gevolg dat mesas 'n natter habitat verteenwoordig in vergelyking met die meer ariede vlaktes. Habitatsverskille soos dié het heel moontlik klaar bestaan voor die aankoms van vee, maar oorbeweiding het die verskille in habitat tussen mesas en vlaktes groter gemaak. Selektiewe beweiding deur vee het waarskynlik tot gevolg gehad dat plante wat giftig, doringagtig of onsmaaklik is, toegeneem het in plantegroeigemeenskappe, ten koste van meer smaaklike spesies. Grondtipe en grondsamestelling het aspek en verwagte koeler kondisies op die suidoostelike hange onderdruk as bepalende faktore vir plantegroeigemeenskap samestelling op Tafelberg en Folminkskop (beide bedek met 'n doleriet laag). Aspek en steilte van die hange het grondtipe en grondsamestelling onderdruk as bepalende faktore vir plantegroeigemeenskappe op Buffelskop. Die potensiaal om mesas te gebruik as bronne van saad vir die rehabilitasie van die vlaktes was laag. Mesas en hulle omliggende vlaktes het naastenby 28 % van spesies in gemeen gehad, maar nie al hierdie spesies was goeie koloniseerders nie. Sekere smaaklike plante wat op beide mesas en vlaktes voorgekom het, kan potensiaal hê vir toekomstige restorasie doeleindes, bv. Eragrostis obtusa, Felicia muricata, F. ovata, Fingerhuthia Africana, Jamesbrittenia tysonii, Limeum aethiopicum, Pentzia incana en Selago albida. Mesas is uniek in samestelling en kan beskou word as een plantegroeitipe in 'n see van 'n ander tipe (vlaktes). Mesas word nie oor die algemeen bewei nie (as gevolg van hulle steil hange en bergagtigheid) en word gevolglik nie bedreig deur huidige ontwikkeling nie. Plantegroeigemeenskappe in Middelburg is soortgelyk aan die van ander dele van die Nama-Karoo bioom. Resultate van die studie dui aan dat die vlaktes huidiglik meer gedegradeer is as mesas, maar dit is onbekend of die veld gestabiliseer het of steeds besig is om verder te degradeer in huidige weidings- en klimaatskondisies. Die Braun-Blanquet klassifikasiemetode IS effektief vir die beskrywing van plantegroeigemeenskappe in ariede areas. Al die persele in die studie area is gemerk met metaal paaltjies en is dus permanent. Dit maak dit moontlik om in die toekoms die persele weer te ondersoek. 'n Langtermyn datastel kan moontlik lig werp op die stabiliteit en degredasie van karoo veld. Restorasie van veld is 'n moontlikheid vir die toekoms, maar min boere kan duur restorasie metodes bekostig in die kort termyn. Boere moet hulle lande gereeld ondersoek en drakrag aanpas by die kondisie van die veld. Baie boere ploeg kaal kolle in die veld op 'n gereelde basis, en daar word voorgestel dat die praktyk gekombineer word met die saai van geskikte saad, gevolg deur 'n rusperiode tydens en na ontkieming daarvan.

A dissertation submitted to the Faculty of Science, University of the Witwatersrand, Johannesburg, in fulfilment of the requirements for the degree of Master of Science. Johannesburg, 2016. / The Jacomynspan Ni-Cu sulphide mineralisation is hosted within a 100m thick steeply dipping tabular, differentiated, sill of mafic to ultramafic composition intruded into country gneissic rocks of the Namaqualand Metamorphic complex. This sill is predominantly composed of tremolite schist (metamorphosed pyroxenite) containing lenticular bodies of harzburgite. The harzburgite generally hosts net-textured mineralisation with up to 50% by volume of the rock. Massive sulphide veins and stringers are occasionally present within the harzburgite. The sulphide minerals are a typical magmatic assemblage of pyrrhotite, chalcopyrite and pentlandite. The sill covers an approximate strike length of about 5km but only a small portion covering 1km x 1km was selected for this study. Physical property studies carried out on the drill core (magnetic susceptibility and conductivity) indicate that the country gneissic rocks are not conductive and neither are they magnetically susceptible. However, the mineralized sill has elevated values of both magnetic susceptibility and relative conductivity compared to its host making it a suitable target for both magnetic and electromagnetic inversion. Drilling done so far on the study area has shown that the well-mineralised harzburgite (hosted within the poorly mineralised ultramafic sill) is not a continuous body but occurs in ‘pockets’. There is therefore need to use the available geophysical and geological datasets to derive a model of these well mineralised pods. This study is therefore intended to assess the feasibility of using electromagnetic (EM) methods together with other geophysical methods and geology in obtaining a model of the harzburgite pods hosted within the less conductive poorly mineralised ultramafic sill in order to guide further drilling. Geosoft’s VOXI Earth Modelling software was used to model the high resolution airborne magnetic data for this study. Cooper’s Mag2dc (www.wits.ac.za) and Stettler’s Magmodintrp software (personal communication, 2015) was also used during modelling of the magnetic data to compliment the modelling from VOXI. The mineralised ultramafic sill was clearly mapped in both the 3D model representation from Mag2dc modelling and VOXI’s 3D unconstrained smooth model inversion for the study area. Based on the physical properties studies carried out on the study area, EM data (both ground and downhole EM) were modelled using Maxwell software. The poorly mineralised tremolite schist was clearly modelled. In order to better constrain the targets, an assumption was made that at late decay times the currents would be focused in the centre of the large EM plate probably giving an indication of the most conductive part of the intrusion. Smaller ‘Resultant EM plates’ of dimensions, 300mx300m that coincide with the centre of the large EM plates (with a conductance above 100S) were constructed in iv Maxwell software and integrated with the DXF file of the Micromine geology model of the well mineralised harzburgite clearly mapping the well-mineralised harzburgite and showing its possible extensions. 2D inversion modelling was conducted on all audio-frequency magnetotelluric (AMT) data for this study area. The modelling results clearly mapped the mineralised intrusion.

The Namaqua Province of southwestern Africa is comprised of a number of distinct tectonostratigraphic subprovinces and terranes, which have in common a 1100-1200Ma structural and metamorphic imprint. In the western Bushmanland Subprovince, E-Wtrending belts of supracrustal gneisses are intruded by and infolded with granitic gneisses of varying ages. A central zone of rocks metamorphosed in the granulite facies is bordered to the north and south by amphibolite facies rocks. A portion of the Garies-Platbakkies supracrustal gneiss belt has been mapped on a 1:15 000 scale. The supracrustal succession was deposited on an unconfirmed basement. It is structurally juxtaposed and infolded with three different granitic augen gneisses. Large bodies of orthopyroxene-bearing granite are syntectonically emplaced in the succession. A wide variety of anatectic granites crop out as sills, dykes and pods varying in size between a few metres and a few hundred metres. These bodies commonly truncate pre-existing foliations. The metamorphosed supracrustal succession contains gneissic equivalents of felsic, mafic and intermediate volanics; pelitic, semi-pelitic, magnesian and granitic composition sediments; feldspathic quartzites; and subordinate quartzites, banded iron formation and calc-silicates. The mineral assemblages of all the rocks indicate metamorphism in the granulite facies. A variety of field evidence exists which suggests that the metamorphic peak was responsible for generating significant quantities of partial melt. The rocks of the study area contain an early Dl fabric. This is refolded in tight, E-plunging D2 crenulation folds. D2 mineral fabrics pre-date the metamorphic peak. D3 open, asymmetric folds are N-vergent and fold the crystalline products partial melting. The southern limbs of D3-folds are attenuated in 04 shear zones. The whole belt is cut by steep, N-S-trending faults. A wide variety of thermobarometers are tested for their applicability to mineral assemblages in the supracrustal rocks. The results of this application suggest that the metamorphic peak occurred at 780 ± 30°C and 5.0 ± 0.4 kbar. Assemblages in shear zones indicate an isobaric retrograde cooling path. The phase relations of melting near the solidus are reviewed with reference to common assemblages in the leucosomes of rocks with granitic and peraluminous bulk compositions. Isobaric T-a(H₂O) sections are constructed from available experimental and thermochemical data. Biotite dehydration and dehydration melting reactions are balanced using natural mineral compositions. The predicted results are compared with the modal abundances of natural product assemblages. The results suggest that dehydration melting was responsible for migmatization, and the consequent reduction of water activity. The amount of melt produced was controlled by the amount of water available from the dehydration of biotite. There is no evidence for the control of water activity by an external fluid reservoir. Limited amounts of water-undersaturated melts were extracted from their sites of generation. This process was responsible for the depletion of some leucosome assemblages with respect to K₂O, H₂O and in peraluminous rocks Na₂O. The partial melts were emplaced locally in developing shear zones.

Thesis (MSc (Botany and Zoology)--University of Stellenbosch, 2006. / Parts of the West Coast Strandveld and adjacent Succulent Karoo on the arid coast of Namakwaland in the Western Cape of South Africa are subject to surface mining. An understanding of mycorrhizal association of plants in the natural vegetation of this area could contribute to the improvement of post-mining re-vegetation of the area. This study investigated mycorrhizal association of plants in the West Coast Strandveld, and compared mycorrhizal infection rates of soils taken from natural vegetation to soils from post-mined rehabilitated vegetations. The study was divided into two components. In the first component a pot experiment was conducted in the greenhouse to assess vesicular-arbuscular mycorrhiza (AM) infectivity of post-mined rehabilitated areas of Brand se Baai in Namakwa Sands mining areas. Rehabilitated areas used in this study included sites that has been strip mined for heavy minerals and then progressively backfilled with sub-soil sand remaining after mineral extraction (tailings), topsoil and translocated plants in an effort to restore the structure and functional aspects of the mined site to its original (pre-mining) ecosystem. Rehabilitated sites 1 assessed in this study included sites backfilled with: tailings + translocated plants (TP); tailing + topsoil + translocated plants (TSP) and tailings + topsoil only (TS). Natural sites (N) were also assessed to serve as reference points. AM infection was evaluated as percent root colonization on wheat planted as bioassay on sterilised sand and inoculum from rehabilitated sites in the ratio of 3:1 respectively. Results of this study component showed that mycorrhiza infectivity of rehabilitated soils was high on TSP and TS because mining disturbance has been remedied by topsoil with or without translocated plant replacement. The structural and chemical components of topsoil used as rehabilitation material favoured re-establishment of microbial activities. Infectivity was however low on soils rehabilitated with tailings and translocated plants (TP) because this treatment lacked topsoil which is a major source of infective mycorrhizal propagules. Infectivity was also low in soils from undisturbed sites (N) probably high phosphorus concentration or presence of perennial vegetation led to low mycorrhiza infection. Results showed that there was no significant effect of mycorrhiza on plant growth rate, nutrient uptake or carbon cost of mycorrhizal plants when related to non-mycorrhizal plants, instead the biomass production and nutrient contents of plants were determined by chemical properties of treatment soils. The second component of the study investigated presence of mycorrhiza on randomly selected common indigenous species of Aizoaceae, Asparagaceae, Asteraceae, Chenopodiaceae, Fabaceae, Lamiaceae, Mesembryanthemaceae, Restionaceae, families growing on unmined areas of the study site. Total mycorrhiza infection was recorded on 85% of the assessed species with percent infection level ranging from 8% in Atriplex lindleyi and Drosanthemum hispidum to 98% in Salvia lanceolata. Functional mycorrhizal association with arbuscule structures were however only observed on 15% of all species assessed. Low arbuscules infection observed in indigenous species assessed in this study could be associated with the timing of mycorrhiza infection assessment and root competition in the soil. There was no infection observed on four species belonging to Chenopodiaceae, Zygophyllaceae, Sterculiaceae, and Asteraceae families, which represented 15% of all species assessed. Most species belonging to Chenopodiaceae and Zygophyllaceae have been reported as non-mycorrhizal in other studies, absence of mycorrhiza on the remaining three families species observed in this study require further confirmation.

Thesis (MSc)--Stellenbosch University, 2015. / ENGLISH ABSTRACT: Several areas in Namaqualand are affected by elevated levels of salinity; including the shallow alluvial aquifers along the Buffels River catchment. The chemistry of rainwater that recharges these aquifers has low salt-loads, but the groundwater system is very saline. The shallow alluvial aquifers are an important source of water for several communal areas along the river both for domestic and agricultural purposes. Groundwater is also used for the copper and diamond mining activities along the river. Prior to this study, the sources of salinity to the alluvial aquifers and whether salinity can be remediated has not been determined. Possible salinity sources included seawater intrusion, evaporitic salts dissolution, concentrations by evaporation, deep aquifer brines, dissolution of minerals from the aquifer geology as well as salts from anthropogenic activities (i.e. mining). The source(s) of salinity to the groundwater has been determined using the geochemical as well as the isotopic tracers. The ratios of major ions (i.e. Na/Cl) as well the oxygen (18O), hydrogen (2H), 36Cl/Cl, and 87Sr/86Sr isotopes were used in determining the possible solute sources. In addition to these, the chloride mass balance (CMB) method was used to determine the recharge rates to the alluvial aquifers. Furthermore, the groundwater age of the alluvial aquifers was determined using the tritium (3H) isotope. The groundwater samples have high 87Sr/86Sr ratios, which are in the same ranges as the 87Sr/86Sr ratios in the surrounding granitic rocks indicating water-rock interactions. The 36Cl/Cl ratios are low and indicate the dissolution of old salts. The 18O and 2H stable isotopes of groundwater show an evaporative trend with respect to the LMWL, which indicate that groundwater has been evaporated before or during infiltration. Salinity to the shallow alluvial aquifers was found to be mainly derived from the dissolution of rock mass and concentration by evaporation process. The groundwater is relatively young, but there is mixing between old water recharged prior to bomb testing and recently recharged groundwater in some boreholes. The Chloride mass balance (CMB) method assumes atmospheric chloride is the only source of chloride to the aquifers. However, there is additional chloride to these alluvial aquifers from rock mass dissolution. The estimated recharge rates by CMB method (0.1-3.4mm/a) are therefore underestimated. A simulation model was used to determine the recharge rates based on the annual precipitation that will yield the current measured chloride concentrations in the groundwater. Recharge was found to range from 1-5% of the annual precipitation, which is also low. The CMB method therefore gives significant recharge rate estimates, but they are not accurate and need to be supported by another method. / AFRIKAANSE OPSOMMING: Geen opsomming beskikbaar.

Thesis (Ph.D.)--University of the Witwatersrand, Faculty of Science, 1997.

The Mesoproterozoic rocks of the Bysteek and Koenap Formations of the Arribees Group are exposed within a NW-SE striking antiformal structure comprised of mafic granulites and metapelitic diatexites, and a number of marble and calc-silicate rock layers. The mafic granulites of the Bysteek Formation show a typological variety of anatectic features, including nebulitic, stromatitic mesosomes, melanosomes, quartz syenitic leucocratic vein networks and syenitic pools. Melanosomes consist of hedenbergitic to diopside-rich clinopyroxene (XMg: 0.40), anorthitic plagioclase (An90), with some quartz, minor apatite and titanite. Anatexis was caused by biotite dehydration melting and formed a melt of probably granitic composition. The leucosome composition ranges from either alkali-feldspar-granitic to plagioclase rich or granitic. This variation is interpreted as a result of variable extraction of melt from the source to granitic pools. The diatexites of the Koenap Formation are most likely of metapelitic or meta-greywacke origin. They are texturally variable but always contain high modal contents of alkali feldspar and quartz which generally form magmatic textures. Almandine-rich garnet (XMg: 0.18-0.25), cordierite (XMg: 0.71) form secondary biotite, sillimanite and magnetite during retrograde breakdown. Thermodynamic modelling of mafic granulite compositions suggests peak P-T conditions of ~865 °C and 8.6 kbar. Occasionally, garnet rich in ferric iron (XAdr: 0.55) forms by plagioclase-clinopyroxene breakdown under oxidising conditions at ~6 kilobar and ~ 800 °C. At the same stage amphibole forms in some melanosomes. P-T estimations for the diatexites based on thermodynamic modelling suggest the equilibration of the assemblage garnet, cordierite, alkali feldspar and melt at ~860 °C and 5.5 kbar. Conditions comparable to the peak pressure in the mafic granulites could not be established. However, since the diatexites and the mafic granulites are closely related in the field and no evidence of juxtaposition after the thermal peak exists, the P-T record of the diatexites might be incomplete

Magister Philosophiae - MPhil / This thesis provides a detailed examination of the development and implementation of a commonage management system on newly acquired municipal commonage in the Leliefontien communal area of Namaqualand, South Africa. This commonage has been acquired ostensibly for use by all of the Leliefontien's residents. A Commonage Committee made up of community members and state representatives manages this land on behalf of the municipality. / South Africa

Magister Artium - MA / The aim of this research is firstly, to determine the impact of the current practiced tenure system in the Leliefontein Rural Area on the use of the natural resources and secondly, to devise and establish the most appropriate tenure system that will ensure the sustainable natural resource management on the communal and commonage land of the mentioned area. Quantitative questionnaires, review of relevant literature from documentation, research studies and reports were used to gather information and provide contextual insights. A wide spectrum from the Leliefontein Rural area specifically, Namaqualand in general and other semi-arid and communal areas in Southern Africa were covered with the gathering of the secondary data. / South Africa

Scheelite, wolfram Ite and cassIterIte mIneralizat ion is hosted wIthin numerous quartz-tourmaline-feldspar-fluorite veins at Van Rooi's Vley, N.W. Cape Province . MineralizatIon and hydrothermal alteration within, and around, these veins is hIghly complex and reflects the intricate interaction of hydrotherma l activity upon a structurally deformed sequence of ProterozoIc med ium to high-grade gneisses. Four distinct stages of alteration and mineralization occurred, including a l ate 'epithermal stage'. Although the location of mineralization was strongly controlled by st ructure, the concentration of mineralizati on was controlled by physicochemical variables, of which host-rock geochemistry was particularly important . Further W/Sn mineralization occurs on a local scale, some of which is spatia lly related to minor leucogranite dykes. Leucogranite bodies are not uncommon within the region and some are enriched in Wand Sn. By comparing FIB ra tio s,W/Sn ratios, the alteration mineralogy, the ore mineralogy and the Fe-content of tourmaline, the deposits within the Van Rooi's Vley area can be placed into a 'proximal' to 'distal' classification, with respect to a common source of mineralizing hydrothermal fluids. The Van Rooi's Vley deposit, whilst affiliated to greisen-style deposits, represents a ' distal' quartz-vein lode deposit. / KMBT_363 / Adobe Acrobat 9.53 Paper Capture Plug-in