Este estudo apresenta conhecimento geomorfológico sobre sistemas físicos meândricos e, em especial, busca o entendimento das atividades antrópicas sobre estes sistemas físicos, exemplificando assim um dos princípios fundamentais da Antropogeomorfologia ou Geomorfologia Antropogênica. A pesquisa tem como objetivo a análise qualitativa e quantitativa das mudanças produzidas pelas atividades de mineração de areia em um compartimento fluvial da planície meândrica do Rio Embu-Guaçu, setor sul do município de São Paulo (SP). O estudo das mudanças foi realizado com utilização da cartografia geomorfológica evolutiva como recurso analítico das condições do sistema físico em situação préintervenção e após 22 anos de extração de areia (situação durante intervenção). Para tanto, foram produzidos dois mapas geomorfológicos de detalhe da área de estudo: um, referente ao ano de 1981, e representa a morfologia original, o outro, referente à 2003, representa a morfologia antropogênica. A seleção e representação das formas, materiais e processos que constituem os mapas geomorfológicos, bem como sua análise comparativa baseiam-se em um conjunto de geoindicadores considerados como parâmetros para interpretação qualitativa e quantitativa. / This study presents the geomorphological knowledge about physical meandering systems and pursuits the understanding of the anthropic activities effects on these physical systems, so characterizing one of the main principles of a anthropogeomorphology and anthropogenic geomorphology. The main purpose of this research was the qualitative and quantitative analysis of the modifications performed by sand mining activities in a fluvial compartment of the meandering floodplain of the Embu-Guaçu river, in the southern sectin Sao Paulo county. This study was performed with the application of evolutionary geomorphological cartography mapping as analytical tool for the physical system conditions in a preintervention situation and after 22 year of sand extraction (state during intervention). Two detailed geomorphological maps were produced: one refers to 1981 and presents the original morphology and the other to 2003 including the anthropogenic morphology. The selection and representation of forms, materials and processes included in geomorphological maps as well as the comparative analysis were based upon a series of geoindicators considered as qualitative and quantitative interpretation parameters.

A recuperação ambiental de áreas exploradas pela mineração de areia na região do Vale do Paraíba, Estado de São Paulo, constitui anseio popular, obrigação constitucional e fator de diferenciação dentro da mais moderna visão empresarial. Este trabalho estuda a aplicação de turfa como um melhorador de solos na etapa final do processo de recuperação destas áreas: o restabelecimento da vegetação nativa. O interesse surgiu da experiência de trabalho do autor com pesquisa mineral e tecnológica desta substância, além da observação e acompanhamento de alguns projetos de revegetação nestas áreas, tidas como ambientalmente sensíveis e onde os solos apresentam-se, via de regra, improdutivos; sua utilização representou, nestes casos, a diferença entre o sucesso e a necessidade de replantio. Apresenta-se uma revisão bibliográfica sobre turfa e suas propriedades agronômicas, bem como acerca da utilização de matéria orgânica na revegetação de áreas degradadas. O estudo constituiu um comparativo entre resultados de ensaios efetuados em amostras de solo provenientes de área abandonada pela mineração de areia, homogeneizadas em laboratório em seu estado original (branco), de um lado, e com adição de turfa em diferentes proporções, de outro, visando aferir se alguma delas poderia adequar-se mais satisfatoriamente à melhoria das condições gerais do solo em questão. Foram analisadas variações em propriedades químicas e físicas como retenção de cátions, efeito tampão, densidade aparente, condutividade hidráulica e porosidade. Abre-se a possibilidade de os resultados deste projeto não se limitarem apenas à Indústria Mineral mas estenderem-se a outros setores onde haja a necessidade de recuperação de solos, fornecendo subsídios a eventuais modificações no manejo de solos agricultáveis, com perspectivas de geração de economia de recursos em irrigação, fertilizantes e defensivos agrícolas. / The environmental recuperation of areas explored by sand mining in the Vale do Paraíba region, in the State of São Paulo, is a popular aspiration, a constitutional obligation and constitutes a differentiating factor in the visions of modern enterprise. This work studies the utilization of peat as a soil conditioner in the final stage of the recuperation process for these areas: the revival of indigenous vegetation. This idea arose from the author's experience in technological and mineral research into peat, coupled with the observation and monitoring of these environmentally sensitive areas, whose soils were, from an agricultural stance, generally unproductive. The utilization of peat, in these cases, represented the difference between success and the necessity for a replantation process. This study presents a review of the agronomic properties of peat as well as the application of organic matter in the revegetation of damaged land. It is a comparative study between laboratory assay results from soil samples in their original state, and those where the soil has variable peat contents, seeking to ascertain which, if any, results in better general conditions for that particular soil. Both physical and chemical properties were analyzed, with an emphasis on cation exchange capacity, buffering, bulk density, hydraulic conductivity and porosity. There is a possibility that the results of this project can extended beyond the Mineral Industry to other sectors, where there are needs for soil recuperation, leading to cost savings for irrigation, fertilizers and agrotoxic compounds in food production areas.

Este estudo apresenta conhecimento geomorfológico sobre sistemas físicos meândricos e, em especial, busca o entendimento das atividades antrópicas sobre estes sistemas físicos, exemplificando assim um dos princípios fundamentais da Antropogeomorfologia ou Geomorfologia Antropogênica. A pesquisa tem como objetivo a análise qualitativa e quantitativa das mudanças produzidas pelas atividades de mineração de areia em um compartimento fluvial da planície meândrica do Rio Embu-Guaçu, setor sul do município de São Paulo (SP). O estudo das mudanças foi realizado com utilização da cartografia geomorfológica evolutiva como recurso analítico das condições do sistema físico em situação préintervenção e após 22 anos de extração de areia (situação durante intervenção). Para tanto, foram produzidos dois mapas geomorfológicos de detalhe da área de estudo: um, referente ao ano de 1981, e representa a morfologia original, o outro, referente à 2003, representa a morfologia antropogênica. A seleção e representação das formas, materiais e processos que constituem os mapas geomorfológicos, bem como sua análise comparativa baseiam-se em um conjunto de geoindicadores considerados como parâmetros para interpretação qualitativa e quantitativa. / This study presents the geomorphological knowledge about physical meandering systems and pursuits the understanding of the anthropic activities effects on these physical systems, so characterizing one of the main principles of a anthropogeomorphology and anthropogenic geomorphology. The main purpose of this research was the qualitative and quantitative analysis of the modifications performed by sand mining activities in a fluvial compartment of the meandering floodplain of the Embu-Guaçu river, in the southern sectin Sao Paulo county. This study was performed with the application of evolutionary geomorphological cartography mapping as analytical tool for the physical system conditions in a preintervention situation and after 22 year of sand extraction (state during intervention). Two detailed geomorphological maps were produced: one refers to 1981 and presents the original morphology and the other to 2003 including the anthropogenic morphology. The selection and representation of forms, materials and processes included in geomorphological maps as well as the comparative analysis were based upon a series of geoindicators considered as qualitative and quantitative interpretation parameters.

Thesis (M. Dev. (Planning and Management)) -- University of Limpopo, 2021 / Sand mining has grown popular in South African rural communities due to its increasing demand for building purposes in and around the surrounding villages as well as a source of income to the rural communities. Sand is an indispensable natural resource of any society around the world. For instance, the government has to deal with the frequent sand mining environmental effects and implement various strategies on how to deal with these effects to protect the environment. Although the National Environmental Management Act (NEMA) 107 of 1998 regulates sand mining, the illegal and unregulated rural sand mining is causing land degradation, creating unpleasant appearances, causing vulnerability to floods and pointing out the need for rehabilitation. Given the circumstances surrounding the issue of illegal sand mining in rural communities, this research is aimed at investigating the impact of illegal or legal sand mining on the environment looking at the land degradation and the importance of rehabilitating the area after use in Mentz village. The main objective of this research was to explore how sand mining causes land degradation and examining the significance of rehabilitation in sand mining. The methodology of the study was carried out using both quantitative and qualitative research design in a form of questionnaire surveys, oral interviews and field observations to collect the data. The sample was composed of the general members of the community, the chief and the sand miners. For data analysis, the study used the Statistical Package for the Social Sciences (SPSS), IBM SPSS Statistics 25. The results indicated that sand mining causes 54.76% of the land degradation in South Africa. Furthermore, the research revealed that 30.95% of the land degradation was due to deforestation and 11.90% of Mentz land degradation was caused by overgrazing. Besides, an overwhelming 76.58% of the respondents agreed that land should be rehabilitated after sand mining processes.

The recuperation of degraded areas due to mining activity namely sand mining is carried out by the forest recomposition with native species. In the present work the availability of nutrients along with amount of living matter cover accumulated in a native ciliary wood and in five fragments of forest recomposition of areas previously used for sand mining in the municipality of Tremembe SP. Such areas are currently at different phases of vegetative development process, ranging from 1, 5 and 11 years. The content of nutrient, organic matter, soil acidity and total production of living matter cover and coarse living matter leaves ,twigs and roots were analyzed .The living matter cover was sampled in 1 m2 fragments the 0-20 and 20-40 cm layers at five different random points in the beds and between the beds in all areas. The soil samples were analyzed in terms of the attributes pH, organic matter, P, K, Ca , Mg , H , Al , base aggregation , cation exchange capacity and base saturation percentage. The comparison of the living matter cover production and the chemical attributes between the areas were analyzed by means of variance analysis complemented by the Tukey test. A smaller production of total living matter cover was observed in the fragments over 6, 5 reforestation years. As from that period however, the relation between the content of the organic matter and the amount of living matter cover in the superficial layer of the soil tends to differ. There is an increase in the nature of organic matter and the reduction of the production of living matter cover possibly due to the cumulative effect of the organic matter in the soil through the organic composts that are more resistant to decomposition and respond for the humus formation. By means of the analyses of the chemical attributes the soils of the forest fragments were classified as dystrophic and moderately fertile. The nature and level of nutrients presented average values for Ca and Mg, high for P and low for K. The higher values for Ca, Mg and P may be a result of the residual effect of the fertilization carried out during the planting process. / A recuperação de áreas degradadas devido à exploração mineraria, notadamente pela extração de areia, é realizada pela recomposição florestal com espécies nativas. No presente trabalho analisou-se a disponibilidade de nutrientes e a quantidade de serapilheira acumulada em um fragmento de mata ciliar nativa e em cinco fragmentos de recomposição florestal de áreas anteriormente utilizadas para exploração de areia no município de Tremembé, SP. Estas áreas apresentam-se em processo de desenvolvimento vegetativo com períodos diferentes, variando de 1,5 a 11 anos. Foi analisado o teor de nutrientes, matéria orgânica, acidez do solo e a produção da serapilheira total e fracionada em folhas, ramos e raízes. As serapilheira foi amostrada em parcelas de 1m2, nas camadas 0-20 e 20-40 cm em cinco pontos escolhidos aleatoriamente nas leiras e entre leiras, em todas as áreas. Nas amostras de solo analisaram-se os atributos pH, matéria orgânica, Fósforo, Potássio, Cálcio, Magnésio, Hidrogênio, Alumínio, soma de bases, capacidade de troca catiônica e porcentagem de saturação de base. A comparação da produção de serapilheira e dos atributos químicos entre as áreas foi analisada por meio de análise de variância complementada pelo teste de Tukey. Observou-se menor produção de serapilheira total nos fragmentos a partir de 6,5 anos de reflorestamento. Entretanto, a partir deste período, a relação entre o teor de matéria orgânica e a quantidade de serapilheira da camada superficial do solo tende a diferir, com aumento no teor de matéria orgânica e redução da produção de serapilheira, decorrente, possivelmente, do efeito acumulativo da matéria orgânica no solo através de compostos orgânicos mais resistentes à decomposição responsáveis pela formação do húmus. Por meio das análises dos atributos químicos, os solos dos fragmentos florestais foram classificados como distróficos e de fertilidade moderada. Os teores dos nutrientes apresentaram valores médios para cálcio e magnésio, alto para o fósforo e baixo para o potássio. Os valores mais elevados de cálcio, magnésio e fósforo podem ser decorrentes do efeito residual da adubação realizada na época do plantio.

MENVSC / Department of Geography and Geo-Information Sciences

Ce travail de thèse a porté sur l’étude de littoraux sous l’influence de deux grands deltas, l’Amazone et le Mékong, avec un focus sur les plages et cheniers de Guyane intégrant le système de dispersion vaseuse de l’Amazone, et sur les liens entre la déstabilisation du littoral du delta du Mékong et les changements morpho-bathymétriques des chenaux deltaïques sous influence anthropique croissante. L’étude de la plage de Montjoly en Guyane a été conduite en combinant une approche innovante de photogrammétrie aéroportée SfM (Structure from Motion), des mesures hydrodynamiques, bathymétriques, et la modélisation de la propagation des houles à travers cette bathymétrie. Les résultats obtenus montrent le potentiel considérable de la technique de photogrammétrie SfM pour l’étude géomorphologique des plages, et confirment un modèle de rotation de la plage sous l'influence de banc de vase. Le suivi du second site d’étude, un chenier en recul sur un ancien polder rizicole vaseux, au travers d'une analyse multi décennale d’images satellites et des mesures de terrain, a démontré très finement les taux (atteignant 160 m par an) et mécanismes de recul du substrat vaseux en lien avec sa rhéologie.L’analyse de l'évolution de la bathymétrie des chenaux deltaïques du Mékong sur une décennie (1998 et 2008), conduite à travers une méthode sous SIG, a permis de quantifier une perte nette de 200 millions de m3 de sédiments et un approfondissement de chenaux ne relevant pas de processus naturels mais d'extraction de granulats.Ces prélèvements importants de sédiments ont des répercussions importantes sur les apports de sédiments au littoral du delta qui montre des taux d’érosion importants. / This thesis is a geomorphic study of two separate sites associated with two large deltas: the Amazon and the Mekong, with a focus on a beach and chenier in French Guiana integrated into the mud dispersal system of the Amazon, and on the links between destabilization of the Mekong delta shoreline and morpho-bathymetric changes in the deltaic channels under increasing human influence.The study of Montjoly beach in French Guiana was carried out using a combination of an innovative approach in SfM (Structure from Motion) airborne photogrammetry, hydrodynamic and bathymetric measurements, and wave propagation modelling over the nearshore bathymetry. The results show the strong potential of SfM photogrammetry in high-resolution morphometric and sediment budget surveys of sandy beach, and confirm a previously proposed model of beach rotation under mud-bank influence.The second field site in French Guiana, a retreating chenier over a muddy abandoned polder formerly a rice fields, work based on a multi-decadal analysis of satellite images combined with short-term field topographic and hydrodynamic measurements highlighted high rates of chenier migration (up to 160 m a year) and retreat mechanisms over the muddy substrate due to its rheology.A GIS-based analysis of bathymetric changes in the deltaic channels of the Mekong over a 10-year period (1998 to 2008) enabled the quantification of a net loss of 200 million m3 of sediments and an increase in the mean depth of the channels, which appears as unnatural and due to sand mining.These important sediment extractions have serious repercussions on sediment supply to the Mekong delta coast, which shows important rates of erosion.

This study aimed to evaluate the ecological impacts of sand mining on the Mokolo River, in Lephalale. The study focused on the water quality, macroinvertebrates and physical disturbances as indicators in order to determine the ecological im-pacts of sand mining on the Mokolo River. The water quality variables, which this study entailed, were related to sand mining and other sources of pollution such as coal mining, power station industries, agriculture and wastewater treatment works on the Mokolo River. The water quality results for pH, electrical conductivity (EC), total alkalinity (CaCO3), sodium (Na), calcium (Ca), magnesium (Mg), potassium (K), chloride (Cl), fluoride (F), sulphate (SO4) and nitrate (NO3-N) were not over the limits, however turbidity, total coliforms and E. coli were over the limits as per the Target Water Quality Guideline (TWQG). The River Health Programme (RHP) was done at upstream, sand mining and downstream areas in the Mokolo River using the South African Scoring System Version 5 (SASS5). The ecological status at the upstream and downstream areas changed from class C (March 2018) to class B (November 2018), indicating that the ecological status improved in those areas of the Mokolo River. However, at the sand mining area the ecological status has not improved and it was seriously modified due to the physical disturbance as a result of sand mining. Ecological impacts, such as the removal of marginal and riparian vegetation, erosion, disturbed riverbed, undercutting and collapse of riverbanks, loss of adjacent land, river deepened, river widened, water pools, in stream sand stockpiles and river diversions, were determined at the sand mining area. No physical disturbances at the upstream and downstream areas were determined. The findings of this study indicate that the ecological impacts of change in water quality at the upstream and downstream areas was due to high turbidity, Total coli-forms and E. coli. The absence of sensitive macroinvertebrates and loss of ma-croinvertebrates and the physical disturbances within the Mokolo River was be-cause of sand mining. The study indicates that sand mining has negative impacts on the water quality, water quantity, macroinvertebrates and physical characteris-tics of the Mokolo River. / Environmental Sciences / M. Sc. (Environmental Science)