Ardemirio De Barros Silva’s scientific contributions

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Publications (2)


Figure 3 -Variation by Category between 1988 and 2003
Figure 6-Contributions to the variation of mangroves between 1988 and 2003
Figure 8 -Losses and gains between 2003 and 2017.
Figure 9 -Variation by Category between 2003 and 2017
Figure 13 -Losses and gains between 1988 and 2017.

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Assessment of conflicts between mangroves and human occupation in Subaé river outfall between the years 1988 to 2017
  • Article
  • Full-text available

November 2022

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29 Reads

International Journal for Innovation Education and Research

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Ardemirio De Barros Silva

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Ariston De Lima Cardoso

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[...]

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George De Lima Cardoso

Coastal zones fulfill important ecological, social and economic functions. Because soil flooded by tidal variations and due to great variation in salinity. Mangroves cover these regions. They are also a tropical coastal ecological system, always in the lowlands, at the mouths of rivers and estuaries. Despite their important environmental role, mangrove areas have been continuously decreasing worldwide, with an average reduction of 30% in the last 30 years. Thus, this research sought to determine land use and land cover change in low Subaé. With emphasis on Mangrove areas and urban occupation. We used supervised classifications of satellite images to evaluate the changes. We chose images from 1988, 2003, and 2017. And used images from the Landsat series (30m) and an image from the PlanetScope satellite (3m). We validated classifications through the Tau and Geographical Simultaneity concordance measures. We observed that performing the spatio-temporal analysis observing only the variation of areas may not represent the phenomena that occurred. The overall Tau index calculation for the ratings was 0.89. During the period 1988-2017 there was a significant reduction in Agricultural areas, corresponding to around 15% of the study area. Meanwhile, growth of pasture from 24km² to 48Km² and the Urban Zone, occurred over all classes, including mangroves.

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Figura 6 -Comportamento da Função Infiltração Cumulativa (A) e Influência de CN na Infiltração Cumulativa (B).
Figura 8 -Áreas inundáveis segundo CPRM.
Dinâmica hidrológica da Bacia hidrográfica do Rio Subaé-BA

October 2021

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64 Reads

Research Society and Development

Monitorar os processos hidrológicos em uma bacia hidrográfica apesar de ser fundamental, por vezes se torna bastante complexo, principalmente devido a escassez de dados. Nesse sentido, o presente estudo objetivou gerar modelos hidrológicos da Bacia Hidrográfica do Rio Subaé, Bahia, Brasil, em ambiente SIG, utilizando como base o método Curva Número (CN). Para tanto, foram utilizadas imagens do Satélite LandSat8 (30m), MDE do Satélite ALOS, sensor PALSAR (12,5m), arquivo vetorial de solos na escala 1:250.000 do IBGE e dados pluviométricos do INMET. Os dados adquiridos foram processados em ambiente SIG, utilizando o Classificador supervisionado Bhattacharya, o algoritmo r.watershed e o método SCS-CN. Os resultados foram mapas de Uso e Cobertura do Solo, Escoamento Superficial e Taxa de Escoamento. A partir dos resultados foi possível inferir que o somatório das características naturais, como Relevo, Solo e Precipitação em conjunto com fatores antrópicos, dentre os quais ressalta-se a ocupação urbana desordenada, proporcionam aumento do escoamento superficial que além de resultar em inundações no perímetro urbano, sugerem um maior risco quanto à erosão do solo e degradação hídrica na área de estudo.