Knowledge management is largely a social process. It is more about the community‘s understanding, skills and values in relation to their practices than technology. Knowledge is generated and shared through social interaction of people. Exploring the community‘s acts of communication and interaction can help to understand the knowledge they have as well as the knowledge gaps that are apparent. It can also aid in discovering ways in which their practices are shaped and constrained by the knowledge they have. The purpose of this study was to determine the optimal means of knowledge sharing and knowledge distribution in an open system using the Eastern Cape Tyolomnqa Estuary as a case study. Different scholars stated in their different works that sharing knowledge is problematic in most organizations, whether they are formal or informal organizations. There are several reasons that have been identified as to why people do not want to share their knowledge. To achieve the objectives of this study, both secondary and primary sources of data were used. This included literature from various sources, such as books, journal articles and information from the Internet that has been reviewed and analyzed. Interviews and focus groups were used to collect data. Interviews were conducted with 16 people who were purposively selected from the Buffalo City Council, Tyolomnqa Conservancy, Tyolomnqa Estates, Tyolomnqa Forum, and Phozi, Ncera, Sandile and Xhama communities. The key informants were people with management positions, and community leaders. The interviews were unstructured. After collecting data by means of face-to-face interviews focus groups, workshops were convened with the Tyolomnqa Forum, and Phozi, Ncera, Sandile and Xhama communities. The self-administered questionnaire was additionally used as a data collection technique for researchers. Data were analyzed through content analysis and the use of SPSS, and presented in the form of tables and figures. It was identified that their knowledge sharing was fragmented and there was no formal organisational structure to bring communities along the Tyolomnqa Estuary to work together as one would do in bureaucratic organizations like companies. The Tyolomnqa Estuary Forum, which has vested interests in estuary management, could be used as model to provide the organisational infrastructure to facilitate the acquisition and sharing of knowledge on the management of estuaries. It is envisaged that such forums can be a viable mechanism of facilitating the harnessing and sharing of knowledge on the sustainable use of estuaries at the local level. / Thesis (M.I.S.)-University of Natal, Pietermaritzburg, 2003.

Thesis (MSc (Geography and Environmental Studies))--University of Stellenbosch, 2007. / In South Africa, as a result of limited resources and capacity, the governance and management of estuaries occur on an ad hoc basis, with decisions about an estuary’s freshwater-flow requirements, water quality, living-resources management, mouth management and protection status being made on a largely uncoordinated and non-strategic basis. This study is aimed at developing an understanding of the opportunities and constraints affecting estuarine management at a regional scale. The objectives of this study were to: 􀂃 Review relevant policy and legislation governing estuarine management in South Africa; 􀂃 Discuss the current status of regional estuarine management in South Africa; 􀂃 Review international literature for potentially applicable management guidelines; 􀂃 Construct a management protocol for estuarine management in South Africa; 􀂃 Apply this protocol in a South African setting; and 􀂃 Recommend improved measures for regional estuarine management. The main outcome of the study was the development of the proposed National Estuarine Management Protocol, which is currently in the process of being incorporated into the National Environmental Management: Coastal Zone Bill. The CAPE Estuaries Programme was developed to test the proposed Protocol in a regional setting. The study concluded that there was an urgent need for a more holistic regional approach to estuarine management but that the proposed framework and protocol would be successful only if, in addition, they were supported by an understanding of the biophysical estuarine processes and management constraints operating at the local level.

An estuary, according to the National Water Act of 1998, is a partially or fully enclosed body of water which is open periodically or permanently to the sea within which the sea water can be diluted, to an extent that is measurable with freshwater from inland. Estuaries and the lands surrounding them are places of transition from land to sea, and from freshwater to saltwater. Although influenced by the tides, estuaries are protected from the full force of ocean waves, winds, and storms by the reefs, barrier islands, or fingers of land, mud, or sand that surround them. South Africa’s estuaries are important and irreplaceable habitats, especially for prawns, fish, wading birds and mangroves. They are home to numerous plants and animals that live in water that is partly fresh and partly salty. Estuaries are also homes to growing coastal communities as increasing number of people occupy watersheds. However, estuaries are also threatened. One of the threats is reduced river water inflow. This study applies the contingent valuation method (CVM) to elicit user’s willingness to pay to mitigate the negative impacts of reduced freshwater inflow into selected five Eastern Cape and Kwazulu-Natal estuaries: the Sundays, Gamtoos, Mdloti, Mgeni and Mvoti estuaries. In addition to the contingent valuation method, the travel cost method was used to generate comparative values. The contingent valuation method is a technique to establish the value of a good (or service) that is not bought or sold in an actual market. The CVM establishes the economic value of the good by asking the users of an environmental good to state their willingness to pay (WTP) for a hypothetical project to prevent, or bring about, a change in the current condition of the environmental good. The users’ WTP is aggregated to establish a total willingness to pay (TWTP) for the population of the users of the environmental good.

Details are given herein of the development, refinement and application of a higher-order accurate 3-D finite difference model for non-cohesive suspended sediment transport processes, in non-stratified estuarine and coastal waters. The velocity fields are computed using a 2-D horizontal depth-integrated model, in combination with either an assumed logarithmic velocity profile or a velocity profile obtained from field data. Also, for convenience in handling variable bed topographies and for better vertical resolution, a δ-stretching co-ordinate system has been used. In order to gain insight into the relative merits of various numerical schemes for modelling the convection of high concentration gradients, in terms of both accuracy and efficiency, thirty six existing finite difference schemes and two splitting techniques have been reviewed and compared by applying them to the following cases: i) 1-D and 2-D pure convection, ii) 1-D and 2-D convection and diffusion, and iii) 1-D non-linear Burger's equation. Modifications to some of the considered schemes have also been proposed, together with two new higher-order accurate finite difference schemes for modelling the convection of high concentration gradients. The schemes were derived using a piecewise cubic interpolation and an universal limiter (proposed scheme 1) or a modified form of the TVD filter (proposed scheme 2). The schemes have been tested for: i) 1-D and 2-D pure convection, and ii) 2-D convection and diffusion problems. The schemes have produced accurate, oscillation-free and non-clipped solutions, comparable with the ULTIMATE fifth- and sixth-order schemes. However, the proposed schemes need only three (proposed scheme 1) or five cell stencils. Hence, they are very attractive and can be easily implemented to solve convection dominated problems for complex bathymetries with flooding and drying. The 3-D sediment transport equation was solved using a splitting technique, with two different techniques being considered. With this technique the 3-D convective-diffusion equation for suspended sediment fluxes was split into consecutive 1-D convection, diffusion and convective-diffusion equations. The modified and proposed higher-order accurate finite difference schemes mentioned above were then used to solve the consecutive 1-D equations. The model has been calibrated and verified by applying it to predict the development of suspended sediment concentration profiles under non-equilibrium conditions in three test flumes. The results of numerical predictions were compared with existing analytical solutions and experimental data. The numerical results were in excellent agreement with the analytical solutions and were in reasonable agreement with the experimental data. Finally, the model has also been applied to predict sediment concentration and velocity profiles in the Humber Estuary, UK. Reasonable agreement was obtained between the model predictions and the corresponding field measurements, particularly when considered in the light of usual sediment transport predictions. The model is therefore thought to be a potentially useful tool for hydraulic engineers involved in practical case studies

No description available.

Estuaries in South Africa are important nursery areas for the juveniles of many fish species. The condition of many of these systems has, however, deteriorated as a result of degradation caused by urban, industrial and agricultural development. An assessment of the role of harbours, particularly in KwaZulu Natal, as nursery grounds has therefore become an important issue. Durban Bay has undergone considerable changes since the mid-1800s and further developments are proposed. If these developments continue, they will result in the loss of large areas of the sandbanks, but Portnet has recognised the need to integrate environmental considerations into future port developments and operations. It was the overall aim of this study to establish the nature of the association of the juveniles of four common fish species viz. Pomadasys commersonnii, Gerres filamentosus, Liza dumerilii and Leiognathus equula with these sandbanks and, thereby assess the impact of their removal. It was found that all species were abundant on the sandbanks and that the diets of P. commersonnii, G. fiiamentosus and L. equuia were very similar, consisting primarily of bivalve siphon tips, benthic crustaceans and polychaetes. The respective contributions of each food type to the diet varied with species. The diet of L. dumerilii differed from that of the other three species, consisting primarily of benthic floc, foraminiferans, ostracods and sponge spicules. Despite differences in selectivity, it was concluded, from studies of the benthos in the harbour, that all four species, irrespective of size, were feeding on these sandbanks, as opposed to in the channels, throughout the year. Removal of the sandbanks for the construction of a new pier would, thus, result in the elimination of important feeding grounds for the juveniles of these four species. / Thesis (M.Sc.)-University of Natal, 1994.

Investigating linkages between the compositions of suspended (seston) and benthic particulate matter is important to the understanding of organic matter (OM) cycling and nutrient retention in aquatic systems. We compared the quantity and quality of the truly suspended (TS) and settleable (SB) fractions of seston as well as benthic particulate matter in the tidal freshwater James River, Virginia. The mass of seston and OM was consistently higher in the TS fraction compared to the SB fraction. OM was preferentially retained in the TS fraction relative to seston. The proportional contribution of OM constituents (chlorophyll a, particulate organic carbon and nitrogen) to the two fractions was consistent across observed concentrations whereas increases in seston concentration resulted in decreased proportions in the TS fraction. Benthic constituent reservoirs were large relative to the SB fraction but the higher proportion of OM in the SB fraction suggests that the settleable material was more labile.

Aquatic bacteria respond to changing environmental conditions through a variety of mechanisms including changes in abundance, shifts in community composition and variable activity states. In the tidal-freshwater James River, variation in bacterial abundance was linked to nutrient availability and autochthonous production with highest bacterial densities associated with low-nutrient, high-chlorophyll a conditions. Laboratory experiments revealed that bacterial growth rates were nutrient limited at the low-nutrient site, while co-limitation (nutrients, glucose, light) was apparent at the high nutrient site. Despite large differences in abundance, community composition was similar based on TRFLP and 16S rDNA pyrosequencing. Community similarity was lower among rRNA libraries suggesting that variable activity states are prevalent in natural communities. Rare taxa were more likely to be metabolically active and were capable of dramatic growth under microcosm conditions.

A maioria dos hidrozoários é marinha, mas eles também são frequentemente encontrados em estuários. Estes ambientes são considerados um dos principais em número de invasões biológicas. A fauna brasileira de hidrozoários estuarinos é praticamente desconhecida, exceto por alguns registros esparsos. Os objetivos deste estudo são (1) inventariar a fauna de hidroides planctônicos e bentônicos em quarto estuários, Cananéia, Paranaguá, Guaratuba e Babitonga das regiões Sudeste e Sul do Brasil, investigando as afinidades entre os estuários e também a relação entre pólipos estuarinos e seus substratos; (2) caracterizar e comparar as comunidades de hidrozoários planctônicos e bentônicos no gradiente salino (3) e entre o verão (estação chuvosa) e o inverno (estação seca); e (4) inferir padrões que possam auxiliar no entendimento das invasões dos medusozoários. As amostras foram realizadas nos verões e invernos de 2007, 2008 e 2009, em seis isohalinas, sempre que possível. Nós também copilamos dados da literatura com registros de espécies invasoras e criptogênicas e contrastamos estes registros com as características biológicas das espécies. Nós identificamos 37 espécies de hidrozoários (21 medusas e 17 pólipos). Liriope tetraphylla foi a medusa mais frequente em amostras nos estuários de Cananéia e Guaratuba, mas Clytia spp. e Blackfordia virginica foram as medusas mais abundantes nas baías de Paranaguá e Babitonga, respectivamente. Bougainvillia muscus, Clytia gracilis e Obelia bidentata foram as espécies de pólipos mais frequentes em todos os estuários. Os pólipos frequentemente utilizaram cracas, bivalves, hidrozoários e partes de mangue como substrato. Clytia gracilis foi a espécie encontrada sobre maior número de substratos diferentes, enquanto Acharadria crocea foi encontrada mais frequentemente sobre substratos artificiais. Entre as Entre as medusas, Ectopleura dumortieri foi encontrada apenas na salinidade mais alta (30) em todos os estuários, enquanto Moerisia inkermanica foi encontrada apenas nas salinidades 10 e 15. Entre os pólipos A. crocea restringiu-se a salinidade 30 em todos os estuários. A maioria das espécies de medusas (67%) e de pólipos (65%) amostrada era eurialina, ocorrendo em pelo menos quatro salinidades diferentes. As comunidades das medusas variaram sazonalmente, principalmente pela variação na abundância das espécies mais ubíquas. Enquanto as comunidades de pólipos parecem ter sido menos influenciadas pelas estações, exceto por A. crocea que ocorreu apenas no inverno. Nós listamos 43 (37 Hydrozoa e 6 Scyphozoa) como invasoras e 15 espécies de Hydrozoa como criptogênicas. Nós observamos que alguns padrões de invasão nos Medusozoa podem estar relacionados à biologia das espécies e com a filogenia dos grupos. / The majority of the hydrozoans is marine, but they are also often recorded in estuaries. This environment is considered one of the most important in number of biological invasions. The Brazilian brackish hydrozoan fauna is practically unknown, except for some scattered records. The goals of this study are (1) to survey the planktonic and benthic hydrozoans fauna in four estuaries, Cananéia, Paranaguá, Guaratuba e Babitonga, from southern Brazil, investigating the affinities among these estuaries and also the relationship between estuarine polyps and their substrates; (2) characterize and compare the planktonic and benthonic hydrozoan communities in salinity gradients (3) and between summer (raining station) and winter (dry station); and (4) infer patterns that might help to understand Medusozoan invasion. Samplings were carried out during summer and winter of 2007, 2008 and 2009, at six isohalines for each estuary, whenever it was possible. We also compiled data of literature records of invasive and cryptogenic species and contrasted those records with biological features of these species. We have recorded 37 species of hydrozoans (21 medusa and 17 polyps). Liriope tetraphylla was the most abundant and frequent medusa in the samples of Cananéia and Guaratuba estuaries, but Clytia spp. and Blackfordia virginica were the most abundant medusae in Paranaguá and Babitonga bays, respectively. Bougainvillia muscus, Clytia gracilis and Obelia bidentata were the most frequent polyps in all estuaries. Polyps frequently used barnacles, hydrozoans, mussels shells and mangrove parts as substrates. Clytia gracilis was the species recorded in the largest number of substrates, while Acharadria crocea was recorded more often on artificial substrates. Among the medusae, Ectopleura dumortieri was found only in the highest salinity (30) in all estuaries, while Moerisia inkermanica was recorded in the salinities 10 and 15. Among the polyps, A. crocea was constrained to salinity 30 in all estuaries. The majority of the species of medusa (67%) and polyp (65%) sampled was euryhaline, occurring in at least four different salinities. Communities of medusae vary seasonally, mainly by the abundance variation of the most ubiquitous species. Whilst the community of polyps seems to be less influenced by season, except for A. crocea that occurred only in winter. We have listed 43 (37 Hydrozoa and 6 Scyphozoa) species recorded as invaders and 15 hydrozoan species record as cryptogenic. We have observed that some patterns of invasion in Medusozoa may be related with the species\' biology and with the phylogeny of the group

O complexo estuarino-lagunar de Cananéia-Iguape, localizado na porção sul do litoral do Estado de São Paulo, integra uma importante reserva ambiental e um ecossistema costeiro extremamente produtivo. A região abriga o canal do Valo Grande, construído há mais de 160 anos, o qual favorece a introdução água doce do rio Ribeira de Iguape diretamente no sistema estuarino contribuindo à importantes alterações biogeoquímicas como o aporte de nutrientes, metais e outros elementos pouco solúveis, que acabam tendo como destino os sedimentos. No presente trabalho foi realizada a coleta de amostras da coluna de água e de sedimentos de superfície ao longo do complexo estuarino-lagunar de Cananéia-Iguape e ambientes contíguos. Também houve a realização de perfis de sedimento na região sul do estuário, considerada mais preservada. O objetivo principal foi avaliar os processos que regem a distribuição dos Elementos Terras Raras (ETR) nos sedimentos do sistema, conhecendo as propriedades hidroquímicas do sistema, associando e comparando os ETR a outros elementos presentes em baixas concentrações, de modo natural ou resultantes de alterações de origem antrópica, utilizando padrões de fracionamento, anomalias e assinatura geoquímica de minerais que atuam na distribuição dos ETR verificando seu potencial para evidenciar a origem e interpretar níveis naturais e efeitos antrópicos aos quais o Complexo está submetido. Os resultados mostraram que as características hidroquímicas na região norte do Complexo encontram-se fortemente influenciadas pelo aporte de águas fluviais via Valo Grande e pelos processos biogeoquímicos associados a ele, enquanto a região sul apresentou-se mais conservada, mostrando equilíbrio biogeoquímico natural de sistemas estuarinos, oferecendo maior suporte à produção primária. Nos sedimentos de superfície, as concentrações elementares de Al, As, Ba, Ca, Cd, Co, Cr, Cs, Fe, Hg, Hf, P, Pb, Rb, Sb, Sc, Th, U, Zn, Zr e ETR* apresentaram distribuição bastante relacionada às características deposicionais/texturais, de forma que a maioria destes elementos tiveram maiores concentrações em regiões de baixa energia hidrodinâmica, no interior do rio Ribeira de Iguape e no mar Pequeno. Considerando como referência os valores guias de qualidade dos sedimentos canadenses (TEL e PEL), os elementos As, Cd, Pb, Cr, Hg e Zn apresentaram concentração abaixo dos valores que indicam frequente ocorrência de efeitos adversos nos organismos aquáticos (PEL), mas foi observado que em alguns locais, As, Cr, Pb e Zn superaram os valores de concentração que indicam uma baixa probabilidade de ocorrência de efeitos adversos à biota (TEL). Fatores de enriquecimento calculados com relação à crosta continental superior (FEUCC) e ao background geoquímico regional (FEBG) apontaram regiões onde ocorrem concentrações de Pb, P e Sb acima dos níveis considerados naturais, entretanto evidenciaram que os altos valores de As e Cr estariam relacionados a um enriquecimento natural dos sedimentos na região. No caso dos ETR, o FEUCC e FEBG indicaram enriquecimento na região do mar adjacente ao estuário e em estações no rio Ribeira e no Valo Grande. A aplicação de modelagem através da regressão múltipla linear mostrou que os valores, que seriam normalmente considerados anômalos, são naturais e refletem a presença de minerais pesados nestes locais. Outros elementos que parecem naturalmente enriquecidos onde há ocorrência minerais pesados são: As, Ca, Cr, Th, U, além dos elementos ditos sinalizadores, como Hf e Zr. Anomalias de Ce mostraram a possível relação com processos de oxidação de Ce+3 a Ce+4 mediada biológicamente nas zonas mais produtivas do estuário. Dos quatro perfis de sedimento obtidos na região sul do estuário, três mostraram seções com valores de FEUCC e FEBG para Pb que sugerem contribuição antrópica. Tais padrões decrescem em direção ao sul do sistema, porém praticamente não mostram variação temporal. Nenhuma concentração de Pb superou o valor de TEL nos testemunhos estudados. Zn e Hg mostraram enriquecimentos pontuais em diferentes seções do testemunho T3. Com relação aos ETR, houve novamente a observação de enriquecimento causado por minerais pesados, e os teores modelados parecem refletir níveis naturais para estes elementos nos quatro testemunhos. Tais informações podem ser utilizadas na ampliação do uso de ferramentas biogeoquímicas de avaliação e prevenção de riscos aos quais o sistema estudado está sujeito, e na tomada de decisão pelo poder público no sentido da conservação ambiental da região. / The estuary-lagoon complex of Cananéia-Iguape, in the southern portion of the coast of São Paulo state, is part of an important environmental reserve and an extremely productive coastal ecosystem. The region encloses the Valo Grande channel, built more than 160 years ago, which favors the introduction of fresh water from Ribeira de Iguape river directly into the estuarine system contributing to important biogeochemical changes in the region. Through this channel, many nutrients arrive at the estuary, as well as, metals and other slightly soluble elements, that end up as sediments. In this research, samples of the water column and surface sediments were collected in the estuary-lagoon complex of Cananéia-Iguape and contiguous environments, as well as, sediment profiles in the south of the estuary, considered to be the most conserved region. The main objective of this study was to evaluate the processes that govern the distribution of rare earth elements (REE) in the sediments of the system, associating and comparing them to other elements, both essential and toxic, using fractionation patterns, anomalies and the geochemical signature of minerals that act in the distribution of REE to evaluate the origin and interpret natural levels and the amplitude of possible anthropic effects to which the Complex is submitted. The results show that the hydrochemical characteristics in the northern region of the complex are strongly influenced by the provision of fresh water through Valo Grande channel and its resulting biogeochemical processes, while the southern region is more conserved, showing the natural biogeochemical balance of estuarine systems, offering greater support to primary production. The elemental concentrations of Al, As, Ba, Ca, Cd, Co, Cr, Cs, Fe, Hg, Hf, P, Pb, Rb, Sb, Sc, Th, U, Zn, Zr and REE* in the surface sediments, show distribution related to depositional/textural characteristics, in such a way most of these elements presented their highest concentrations in regions of recognized low hydrodynamic energy, in the Ribeira de Iguape river and Mar Pequeno region. A comparison of the values obtained for As, Cd, Pb, Cr, Hg and Zn with the Canadian sediment quality guidelines (TEL and PEL) shows that none of the evaluated elements reached concentrations indicating a frequent occurrence of negative effects on aquatic organisms (PEL), however, As, Cr, Pb and Zn have sometimes exceeded concentration values indicating a low probability of occurrence of adverse effects on biota (TEL). Enrichment factors calculated in relation to the upper continental crust (FEUCC) and the regional geochemical background (FEBG) pointed out regions where Pb, P and Sb accumulated above the levels considered natural, however have shown that the high values of As and Cr are related to a natural enrichment of the sediments in the region. For the REE, FEUCC and FEBG indicated enrichment in the sea region adjacent to the estuary and at stations in Ribeira de Iguape river and Valo Grande. Data modeling through linear multiple regression showed that the values, which would normally be considered anomalous, are natural and reflect the presence of heavy minerals at these sites. Other elements that appear to be naturally enriched where there is the indication of occurrence of such minerals are As, Ca, Cr, Th, U, in addition to the signaling elements Hf and Zr. Ce anomalies showed a possible relationship with biologically mediated Ce+3 to Ce+4 oxidation processes in the most productive areas of the estuary. Out of the four sediment profiles obtained in the southern region of the estuary, three showed sections with FEUCC and FEBG values for Pb suggesting anthropogenic contribution. Such values decrease towards the south of the system, however showed a small time variation. None of the obtained Pb values overcame the values of TEL for such sediment profiles. Zn and Hg showed one-off enrichments in different sections of T3 sediment core. Regarding REE, there was again the observation of enrichment caused by heavy minerals in one of the sediment cores, and the modeled contents seem to reflect natural levels for these elements in the four cores. Such information can be used in the expansion of the biogeochemical tools for assessment and prevention of the risks to which the studied system is subject and in the decision making by the public sector towards the environmental preservation of the region.