Navegando por Orientadores "RANIERI, Leilanhe Almeida"

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Acesso aberto (Open Access)
Análise de intrusão salina e qualidade de água em aquífero costeiro na Vila de Algodoal (Ilha de Maiandeua, Pará)
(Universidade Federal do Pará, 2023-09-22) PEREIRA, Lucas Yan de Oliveira; KAWAKAMI, Silvia Keiko; http://lattes.cnpq.br/5306256489815710; https://orcid.org/0000-0002-0548-7976; RANIERI, Leilanhe Almeida; http://lattes.cnpq.br/3129401501809850; https://orcid.org/0000-0002-9870-4879
The increasing urbanization of coastal areas increases the demand for water resources and consequently leads to intensive exploitation of groundwater and anthropogenic impacts that result in groundwater quality degradation. The objective of this research was to assess potential saline intrusion and groundwater contamination in a marine protected area of sustainable use, Algodoal Village (Maiandeua, PA). For the first stage of the research, the quality of groundwater used for human consumption was evaluated based on current regulations (CONAMA Resolution 396/2008; Ministry of Health Ordinance 888/2021). Groundwater characterization was carried out using well water collected during rainy and less rainy periods (between 2021 and 2023), with in-situ physicochemical, microbiological, and major ion parameter analyses by chromatography. Topographic measurements and water table level measurements were also conducted. For the second stage, the results of a socio-environmental questionnaire applied to village residents were analyzed to ascertain their perception of water quality-related issues. Samples from the coastal aquifer presented average electrical conductivity (EC) values of 453 ± 1 µS/cm and total dissolved solids (TDS) of 225.8 ± 1 mg/L. The Cl⁻ ion showed an average concentration of 60 ± mg/L, with several wells exceeding the acceptable potability limit. Significant differences were observed for data collected in the first rainy period (March 2022), where EC averaged 290 µS/cm and TDS was 145 mg/L. The relationship between redox potential, ranging from 0.14 to 0.54 mV, and pH, ranging from 3.2 to 6.7, indicated a tendency toward a reducing acidic environment, typical of a subterranean transitional environment. All analyzed wells were contaminated with total and thermotolerant coliforms. Out of the 34 administered questionnaires, 52% indicated perception of some water quality problem, such as brackish water, for example. Poor water quality is locally associated with the process of saline intrusion and bacterial contamination due to proximity to septic tanks. The shallow depth of the wells (average of 12 m) exacerbates the poor groundwater quality in the village. It is concluded that the aquifer water is not recommended for human consumption, and saline intrusion occurs throughout the year, being more intense in the dry period.
Acesso aberto (Open Access)
Análise multitemporal da linha de costa e indicadores de erosão na praia da Ponta D’Areia, ilha do Maranhão: diagnóstico dos impactos de obras costeiras
(Universidade Federal do Pará, 2024-08-29) SANTOS, Alessandro Ferreira dos; LIMA, Leonardo Gonçalves de; http://lattes.cnpq.br/5984899472616752; RANIERI, Leilanhe Almeida; http://lattes.cnpq.br/3129401501809850; https://orcid.org/0000-0002-9870-4879
The coastal zone is defined as the geographical transition space between the ocean and the continent. In the state of Maranhão, it comprises five sectors, including the Maranhão Golfão. Ponta D’Areia beach is located northwest of the Maranhão Island, making up this sector where tides can reach up to 7.2 meters in height. The beach is approximately 2.5 km long, bounded by the Anil River and São Marcos Beach. In 2014, the construction of a coastal groin was completed at Ponta D’Areia beach, aimed at containing erosion and preventing sedimentation towards the Anil River. In this context, the research addressed the following questions: (a) How did the shoreline change over 27 years? (b) What are the erosional, depositional, and stable sectors from a morphodynamic perspective, considering the period before and after the construction of the coastal groin at the beach? It was believed that the rigid engineering structure was intended to stop the sedimentation at the mouth of the Anil river, which did not occur. As a result, it was necessary to extend the groin to an "L" shape to attempt to curb sedimentation, but this led to continued erosional activity at the northeastern end of the beach. Therefore, the objective of this research was to conduct a multitemporal analysis of the Ponta D’Areia shoreline from 1996 to 2022 and assess its current vulnerability to erosion. The methodology included: (1) on-site observational analysis to fill out pre-defined tables related to coastal erosion geoindicators and collection of surface beach sediments in November 2022 and April 2023, during the dry and rainy seasons, respectively; (2) beach topography survey and orthophoto acquisition through drone flights in April 2023; (3) multitemporal shoreline analysis from 1996 to 2022 using Landsat satellite images, ArcGIS software, and the Digital Shoreline Analysis System (DSAS) extension, as well as shoreline projections for 10 and 20 years into the future; (4) application of the Coastal Erosion Vulnerability Index (CEVI) in three coastal sectors, through the evaluation of natural and anthropogenic parameters; and (5) assessment of the impacts of coastal engineering works on Ponta D’Areia beach. Results showed variations in the shoreline from -64.63 meters (-3.46 m/year: erosion) to 32.15 meters (2.39 m/year: acretion) from 1996 to 2022, with a projected advance of 157.76 meters (4.94 m/year) and retreat of -123.26 meters (-3.68 m/year) by 2032, and a projected advance of 101.93 meters (1.48 m/year) and retreat of -141.35 meters (-1.63 m/year) by 2042. The morphodynamic state of the beach was identified as dissipative through topographic mapping with a drone, and moderate vulnerability to coastal erosion in Sector I, the marina sector, which had the lowest CEVI of 4. Sector II, the groin sector, had CEVI of 6.37 (moderate vulnerability), while Sector III, the Lighthouse sector, had a CEVI of 6.8, indicating high vulnerability to coastal erosion. It was possible to observe how meteo-oceanographic processes (waves, littoral drift, tidal currents, winds, and estuarine discharge) are influencing shoreline variation, as well as human interventions (coastal occupation and construction of rigid structures). Coastal accretion intensified at the beach after the anthropogenic intervention with the groin construction. It is concluded that the multitemporal analysis of the shoreline in the study area between 1996 and 2022 revealed significant variations influenced by natural and anthropogenic factors. Even with human interventions to alter the resulting sedimentation caused by meteo-oceanographic agents, these natural processes continue to intensely shape the region's coastal dynamics and are mainly responsible for variations in the shoreline.
Acesso aberto (Open Access)
Caracterização dos padrões morfodinâmicos em cristas de praias na costa amazônica
(Universidade Federal do Pará, 2023-09-29) ROSÁRIO, Edineuza dos Santos; SANTOS, Valdenira Ferreira dos; http://lattes.cnpq.br/1395198888623953; HTTPS://ORCID.ORG/0000-0002-5038-4191; RANIERI, Leilanhe Almeida; http://lattes.cnpq.br/3129401501809850; https://orcid.org/0000-0002-9870-4879
Knowledge of beach environments requires an integrated morphodynamic approach using different spatio-temporal scales, in order to understand the role of coastal and marine processes in modifying beach morphology. There are some important peculiarities about these processes on the beaches of the Amazon region, such as the large hydro-sedimentary discharge from the estuaries, high rainfall rates and the high amplitude and intensity of the tidal currents, which shape the often complex beach systems, such as beach ridges. The objective of this research was to analyze the morphological dynamics of a beach ridge segment located north of the mouth of the Amazon River, in Goiabal (city of Calçoene), in the coastal ocean sector of the state of Amapá.The hypothesis is that the morphological changes in the segment of beach crest under study are influenced by the hydrosedimentary dynamics of the Amazon River. The research methodology was based on three stages: (1) determining the morphology of beach ridges and their changes (beach profile variation, sedimentary deposits and beach classification); (2) analysis of morphosedimentary processes (physical coastal agents such as tides, waves and currents, and sediment supply such as sediment plumes; (3) data integration (correlation between the processes analyzed in stage one and two). The results indicate significant average variations in the morphosedimentation of the Goiabal beach ridge system, with seasonal migration (~24 to ~42 meters) towards the mainland. Erosion and deposition on the ridges and subsequent channels averaged less than 0.30 m along the beach profiles during the seasonal cycle. The oceanographic parameters indicate an average wave height of 0.25 m and an average tidal range of 5 m. Coastal currents are directed west-southwest and there is a predominance of ebb tide currents during the rainy season. The sediment plume of the Amazon River was closer to the study area during the rainy season (~15 to 25 km), with a predominance of ebb tide currents. Thus, it can be concluded that the segment of beach crest studied has a greater influence from the Amazon River sediment plume during the rainy season, intensifying the deposition of fine sediments. The displacement of beach ridges and the supply of sediment have a strong relationship with tidal dynamics in the region.
Acesso aberto (Open Access)
Caracterização morfossedimentar da Praia do Caripi (Barcarena/PA) antes e após a construção da nova orla
(Universidade Federal do Pará, 2021-12-29) SOUSA, Bianca Abraham de Assis; RANIERI, Leilanhe Almeida; http://lattes.cnpq.br/3129401501809850; https://orcid.org/0000-0002-9870-4879
Acesso aberto (Open Access)
Geoindicadores de vulnerabilidade à erosão em praias estuarinas, costa amazônica, Pará.
(Universidade Federal do Pará, 2022-04-19) NOVAES, Gabriela de Oliveira; RANIERI, Leilanhe Almeida; http://lattes.cnpq.br/3129401501809850; https://orcid.org/0000-0002-9870-4879
The coastal zone (CZ) is a region responsible for various ecological functions, and also object of concern due to its uses and anthropic pressures, which affect its balance and environmental integrity. The beach is one of the most important environments in CZ, due to its intense use by the human population, having ecological function for many organisms and being a natural protection against physical forcers (waves, tides and chains). The anthropogenic occupation on a particular beach can aggravate coastal erosion (natural process of the morphological amendment of the environment, due to the interaction with physical agents). This occurs on the island of Mosqueiro, object of study of this work, where erosive processes have been intensified in recent decades, combined with urbanization. Observing this problem, the present research aims to analyze vulnerability to erosion on the Amazonian estuarine beaches of the Mosqueiro Island, well as evaluating the degree of coastal risk to which they are exposed. Using geoindicators, index and classification of local vulnerability were obtained. Being the index composed of coastal variables: morphology and granulometry of the beach, sedimentary swing, variation of the coast line, cliffs, natural barriers; and continental variables: land elevation, vegetation, coastal engineering structures, percentage of occupation and soil permeability. Then it was carried out: (a) collection of topographic data and sealing samples on 16 beaches; (b) observational analysis with Checklist of geoindicators of coastal erosion in loco and through satellite images; c) treatment of data collected in the field and by remote sensing; d) Use of the coastal vulnerability index to evaluate erosion on the beaches; and, e) identification of risk degree in these beaches. The results demonstrate that 8 of the 16 analyzed beaches are classified with high vulnerability (IVC: 5,0-7,4) and accentuated coastal risk, and that the presence of active cliffs, wall of arrimation and high occupation next the beaches stood out as favoring ones for this result. The data indicated high human occupation (> 70% on most beaches), since several forms of land use are frequent on the island, whether for homes or establishments (shops, restaurants, inns), which raises local risk for the occurrence of damage caused by erosion. In general, the adapted method of this study for Amazonian estuarine beaches, proved to be an interesting tool to be used in urban planning and to minimize future impacts of coastal erosion. It provides information that can aid in decision-making focused on coastal management and choosing which mitigatory measures can be carried out. Thus, the importance of this analysis and continuous coastal monitoring is reinforced through the use of geoindicators.
Acesso aberto (Open Access)
Morfodinâmica de praias estuarinas da vila de Jubim (ilha do Marajó-Pa)
(Universidade Federal do Pará, 2025-04-25) RODRIGUES, Mayara de Souza; RANIERI, Leilanhe Almeida; http://lattes.cnpq.br/3129401501809850; https://orcid.org/0000-0002-9870-4879
The Brazilian Amazon Coastal Zone (states of Amapá, Pará and Maranhão) has environmental characteristics such as a humid tropical climate (high temperatures, low thermal and rainfall variation) and important oceanographic conditions (hyper to mesotidal), in addition to extensive mangroves and sandy beaches, including estuarine beaches. These are vulnerable to seasonal changes in river discharge, in addition to current climate change, the consequent rise in sea level and the resulting coastal erosion, which causes negative consequences for the goods and services originating from this coastal ecosystem. The objective of this study was to analyze the changes in the morphology and sediment dynamics of the estuarine beaches of Jubim and adjacent areas, during a complete seasonal cycle (March 2023 to March 2024). Jubim is a district located in the municipality of Salvaterra, State of Pará, on the east bank of Marajó Island, under oceanographic conditions of the Pará River estuary. Data collection was carried out on four specific beaches, namely: Salazar Beach, Meninas Beach, Baleia Beach and Curuanã Beach. To characterize the morphodynamic state of the beaches, the slope (β) and relative tidal variation (RTR) parameters, derived from the treatment of physical and topographic data (beach profiles), were used as reference. For granulometric analysis, surface sediment samples were subjected to dry sieving in order to obtain the average size, grain selection and sedimentary balance of the beaches. The results showed that the beaches of the village of Jubim have sedimentation ranging from medium to fine sand 1 ɸ and 2 ɸ, with moderately well-sorted grains. The beaches presented quite varied morphometric parameters: topographic elevation from 5.6 m to 2.7 m, and beach width ranging from 79 m to 550 m, thus classifying them into dissipative to intermediate morphodynamic stages (beach slope from 0.2° to 2.6°), with tidal dominance (RTR = 44). The seasonal sedimentary variation was both positive and negative, indicating that the variability index alternate along the beaches and climatic seasons, showing both erosive and depositional tendencies. Erosive processes were observed mainly in the rainy season and greater sedimentary deposition in the dry season. The morphological behavior of the beaches studied on the eastern shore of Marajó Island is directly influenced by estuarine hydrodynamics, where the distinct sedimentary changes are due to the interation that hidrodynamics with the differentiated geology along the coast, and the respective material that constitutes the substrate of the beaches and backwaters.
Acesso aberto (Open Access)
Mudanças morfológicas em praias da costa Leste da ilha do Marajó e os níveis de vulnerabilidade à erosão
(Universidade Federal do Pará, 2021-06-29) SOUSA, Maria Bárbara Pereira de; RANIERI, Leilanhe Almeida; http://lattes.cnpq.br/3129401501809850; https://orcid.org/0000-0002-9870-4879
The coastal zone is a transition area between the sea and the continent, being one of the most vulnerable geographic spaces on the planet. In view of this, the assessment of morphological changes and coastal vulnerability to erosion is essential, as it contributes to the planning of protective and mitigating actions against impacts that occur on the environment, whether natural or anthropic. Thus, the work aims to verify the morphological changes in beaches on the east coast of Ilha de Marajó/PA and their levels of vulnerability to erosion at different time scales. For this purpose, two field campaigns (dry and rainy seasons) were carried out at Barra Velha beach (municipality of Soure) and Praia Grande (municipality of Salvaterra). The methodology consisted of a semi-quantitative analysis, determined by parameters of human and natural occupation evaluated on the beaches. Remote sensing techniques (medium period data) and in situ data collection (short period data) were used. According to the results obtained, Barra Velha beach was classified as dissipative in the two periods studied and most profiles topographic showed an erosive trend from the dry to the rainy period. Praia Grande showed behavior of intermediate to reflective beaches in both the dry and rainy seasons. The sedimentary accretion phase of this beach occurred during the rainy season, reflecting an atypical pattern for beach morphodynamics. Barra Velha beach exhibited moderate erosion vulnerability in the northwest sector and high vulnerability in the southeast sector, mainly due to the high erosion rate over the 16 years studied. Praia Grande, on the other hand, presented a moderate degree of vulnerability to erosion, being considered a more stable beach, combined with coastal protection works. On both beaches, the coastal risk was low due to the low level of occupation close to the coastline. It is believed that the results of this research can contribute to future studies on the theme of vulnerability to erosion in areas that are little or very anthropized and, for possible actions of coastal management in the Amazon region, considering their environmental particularities.
Acesso aberto (Open Access)
Vulnerabilidade costeira em uma comunidade tradicional amazônica: estudo de caso na vila de Jubim, Salvaterra - PA
(Universidade Federal do Pará, 2025-04-16) FIGUEIREDO, Fabrício de Sousa; RANIERI, Leilanhe Almeida; http://lattes.cnpq.br/3129401501809850; https://orcid.org/0000-0002-9870-4879
Coastal vulnerability is a topic of great relevance on a global scale due to current climate issues and rising ocean levels. Understanding the degree of coastal vulnerability is essential to prevent socioeconomic and environmental losses, such as those resulting from erosive processes. This study aimed to quantitatively assess the conditions of vulnerability to coastal erosion in a traditional community on Marajó Island: Jubim, located in the municipality of Salvaterra, state of Pará. To achieve this objective, a Coastal Vulnerability Index (CVI) was used, considering two projections of sea-level rise proposed by the Intergovernmental Panel on Climate Change (IPCC): one with a rise of 4 mm/year and the other with 15 mm/year until 2100. To identify coastal vulnerability under the two sea-level rise scenarios, they were associated with geomorphological and physical characteristics along the estuarine coast of Jubim. Oceanographic variables (tidal range, significant wave height, and sea-level variation) and geological variables (coastal geomorphology, beach slope, and shoreline erosion/accretion rate) were analyzed and classified, with vulnerability indices ranging from very low to very high. The determination of the shoreline erosion/accretion rate was carried out through multispectral and multitemporal analysis (33 years) using Landsat satellite images and the Digital Shoreline Analysis System (DSAS) tool. The spatialization and integration of the data, based on the CVI, were performed using Geographic Information System (GIS) software. The study area was segmented into three sectors: North (Salazar Beach), Central (Meninas Beach), and South (Baleia and Curuanã Beaches). Between 1990 and 2023, the average linear retreat recorded for the entire study area was -35.24 m (NSM), while the average linear advance was 15.10 m (NSM), highlighting the predominance of coastal erosion. The North sector, with the lowest topographic gradient, showed a maximum retreat of 170 meters and an average retreat of 1.99 m/year (EPR), revealing the retreat of mangrove vegetation and the overlapping of Salazar Beach over this ecosystem. The CVI revealed that, under both sea-level rise projections, Jubim's coastline tends to present moderate to high vulnerability (30.3% and 27.3%) in areas with cliffs and extensive sandy stretches, respectively. The map developed based on the CVI proved to be a useful tool to support coastal management on the Amazonian coast and decision-making in the face of advancing erosion caused by estuarine hydrodynamics, associated with rising sea levels.