RESUMO
Open-cast iron mining causes drastic disturbances in soil properties. Recovery of soil chemical and physical properties is essential for successful revegetation and landscape rehabilitation. To identify changes in soil properties during the mining and revegetation process, soil samples were collected from undisturbed sites represented by forest and ferriferous savannas stocking above iron outcrops, called "cangas," in open-pit benches, and in rehabilitation chronosequences of iron waste piles in the Carajás Mineral Province (CMP), Eastern Amazon, Brazil. The samples were analyzed for chemical and physical properties. Our results showed that iron mining operations resulted in significant alteration of the chemical soil properties when forest and canga vegetation are suppressed to form open-pit benches or waste piles in the CMP. Mining substrates showed lower contents of soil organic matter (SOM) and nutrients than undisturbed areas of forests and cangas. In order to achieve the success of revegetation, nutrients have been added prior to plant establishment. We have demonstrated how soil fertility changes along with mineland rehabilitation, and the variation among chronosequence was attributable mainly due to contents of SOM, K, and B in the soil. The slight improvement of SOM found in rehabilitated waste piles reinforces the notion that recovery of soil quality can be a slow process in iron minelands in the CMP.
Assuntos
Poluentes do Solo , Solo , Monitoramento Ambiental , Florestas , Ferro , Mineração , Solo/químicaRESUMO
Sediment transfer from land to ocean begins in coastal settings and, for large rivers such as the Amazon, has dramatic impacts over thousands of kilometers covering diverse environmental conditions. In the relatively natural Amazon tidal river, combinations of fluvial and marine processes transition toward the ocean, affecting the transport and accumulation of sediment in floodplains and tributary mouths. The enormous discharge of Amazon fresh water causes estuarine processes to occur on the continental shelf, where much sediment accumulation creates a large clinoform structure and where additional sediment accumulates along its shoreward boundary in tidal flats and mangrove forests. Some remaining Amazon sediment is transported beyond the region near the river mouth, and fluvial forces on it diminish. Numerous perturbations to Amazon sediment transport and accumulation occur naturally, but human actions will likely dominate future change, and now is the time to document, understand, and mitigate their impacts.
Assuntos
Monitoramento Ambiental/métodos , Sedimentos Geológicos/química , Rios/química , Movimentos da Água , Humanos , Oceanos e Mares , América do Sul , Ondas de Maré , Áreas AlagadasRESUMO
The fire frequency in the Amazon increased rapidly after the 1990s due to deforestation and forest degradation, and it is expected to increase in response to climate change. We analyzed the fire occurrence and assessed seven fire hazard indices in the municipality of Canaã dos Carajás, in the eastern Amazon, for different land use and land cover (LULC) types. We used data from three weather stations located at different heights to compare the performance of the indices using skill scores and success percentages for each LULC. Overall most hotspots occurred in deforested areas and native forests, which were the main LULC types, while few were observed in rupestrian fields, urban areas, and mining areas. However, forests presented the lowest number of hotspots per unit area, especially inside protected areas, and all hotspots in forest areas were observed after a severe drought in 2015. The performance of the fire indices varied as a function of the LULC class and the weather station considered, which indicates the importance of choosing the most appropriate location of the station according to the purpose of the monitoring. The Keetch-Byram Drought Index showed the best performance for predicting fire occurrence for all LULC classes, and forests and deforested areas individually. Despite its simplicity, the Angstrom index stood out due to its good performance in the prediction of days with more than six hotspots.
A frequência dos incêndios na Amazônia aumentou rapidamente após a década de 1990 devido ao desmatamento e degradação florestal, e espera-se que continue aumentando em resposta às mudanças climáticas. Analisamos a ocorrência de incêndios e avaliamos sete índices de perigo de incêndio no município de Canaã dos Carajás, na Amazônia oriental, para diferentes tipos de uso e cobertura do solo. Usamos dados de três estações meteorológicas situadas em diferentes altitudes para comparar o desempenho dos índices usando skill scores e porcentagens de sucesso para cada uso do solo. Em geral, a maior parte dos focos de calor ocorreu em áreas desmatadas e florestas nativas, que têm as maiores áreas de cobertura no município, enquanto poucos focos foram observados nas áreas de campo rupestre, urbanas e de mineração. No entanto, as florestas apresentaram o menor número de focos de calor por unidade de área, especialmente dentro de áreas protegidas, e todos os focos em floresta foram observados após uma seca severa em 2015. O desempenho dos índices de incêndio variou em função do uso do solo e da estação meteorológica utilizada, mostrando a importância da escolha da localização apropriada da estação, conforme o objetivo do monitoramento. O Índice de Seca Keetch-Byram apresentou o melhor desempenho para predizer a ocorrência de incêndios considerando todos os usos do solo, e para as áreas de floresta e desmatadas separadamente. Apesar de sua simplicidade, o índice de Angstrom se destacou por seu desempenho na predição de dias com mais de seis focos de calor detectados.
Assuntos
Conservação dos Recursos Naturais , Incêndios Florestais , Solo , Zonas Climáticas/análiseRESUMO
RESUMO A frequência dos incêndios na Amazônia aumentou rapidamente após a década de 1990 devido ao desmatamento e degradação florestal, e espera-se que continue aumentando em resposta às mudanças climáticas. Analisamos a ocorrência de incêndios e avaliamos sete índices de perigo de incêndio no município de Canaã dos Carajás, na Amazônia oriental, para diferentes tipos de uso e cobertura do solo. Usamos dados de três estações meteorológicas situadas em diferentes altitudes para comparar o desempenho dos índices usando skill scores e porcentagens de sucesso para cada uso do solo. Em geral, a maior parte dos focos de calor ocorreu em áreas desmatadas e florestas nativas, que têm as maiores áreas de cobertura no município, enquanto poucos focos foram observados nas áreas de campo rupestre, urbanas e de mineração. No entanto, as florestas apresentaram o menor número de focos de calor por unidade de área, especialmente dentro de áreas protegidas, e todos os focos em floresta foram observados após uma seca severa em 2015. O desempenho dos índices de incêndio variou em função do uso do solo e da estação meteorológica utilizada, mostrando a importância da escolha da localização apropriada da estação, conforme o objetivo do monitoramento. O Índice de Seca Keetch-Byram apresentou o melhor desempenho para predizer a ocorrência de incêndios considerando todos os usos do solo, e para as áreas de floresta e desmatadas separadamente. Apesar de sua simplicidade, o índice de Angstrom se destacou por seu desempenho na predição de dias com mais de seis focos de calor detectados.
ABSTRACT The fire frequency in the Amazon increased rapidly after the 1990s due to deforestation and forest degradation, and it is expected to increase in response to climate change. We analyzed the fire occurrence and assessed seven fire hazard indices in the municipality of Canaã dos Carajás, in the eastern Amazon, for different land use and land cover (LULC) types. We used data from three weather stations located at different heights to compare the performance of the indices using skill scores and success percentages for each LULC. Overall most hotspots occurred in deforested areas and native forests, which were the main LULC types, while few were observed in rupestrian fields, urban areas, and mining areas. However, forests presented the lowest number of hotspots per unit area, especially inside protected areas, and all hotspots in forest areas were observed after a severe drought in 2015. The performance of the fire indices varied as a function of the LULC class and the weather station considered, which indicates the importance of choosing the most appropriate location of the station according to the purpose of the monitoring. The Keetch-Byram Drought Index showed the best performance for predicting fire occurrence for all LULC classes, and forests and deforested areas individually. Despite its simplicity, the Angstrom index stood out due to its good performance in the prediction of days with more than six hotspots.
RESUMO
The fire frequency in the Amazon increased rapidly after the 1990s due to deforestation and forest degradation, and it is expected to increase in response to climate change. We analyzed the fire occurrence and assessed seven fire hazard indices in the municipality of Canaã dos Carajás, in the eastern Amazon, for different land use and land cover (LULC) types. We used data from three weather stations located at different heights to compare the performance of the indices using skill scores and success percentages for each LULC. Overall most hotspots occurred in deforested areas and native forests, which were the main LULC types, while few were observed in rupestrian fields, urban areas, and mining areas. However, forests presented the lowest number of hotspots per unit area, especially inside protected areas, and all hotspots in forest areas were observed after a severe drought in 2015. The performance of the fire indices varied as a function of the LULC class and the weather station considered, which indicates the importance of choosing the most appropriate location of the station according to the purpose of the monitoring. The Keetch-Byram Drought Index showed the best performance for predicting fire occurrence for all LULC classes, and forests and deforested areas individually. Despite its simplicity, the Angstrom index stood out due to its good performance in the prediction of days with more than six hotspots.(AU)
A frequência dos incêndios na Amazônia aumentou rapidamente após a década de 1990 devido ao desmatamento e degradação florestal, e espera-se que continue aumentando em resposta às mudanças climáticas. Analisamos a ocorrência de incêndios e avaliamos sete índices de perigo de incêndio no município de Canaã dos Carajás, na Amazônia oriental, para diferentes tipos de uso e cobertura do solo. Usamos dados de três estações meteorológicas situadas em diferentes altitudes para comparar o desempenho dos índices usando skill scores e porcentagens de sucesso para cada uso do solo. Em geral, a maior parte dos focos de calor ocorreu em áreas desmatadas e florestas nativas, que têm as maiores áreas de cobertura no município, enquanto poucos focos foram observados nas áreas de campo rupestre, urbanas e de mineração. No entanto, as florestas apresentaram o menor número de focos de calor por unidade de área, especialmente dentro de áreas protegidas, e todos os focos em floresta foram observados após uma seca severa em 2015. O desempenho dos índices de incêndio variou em função do uso do solo e da estação meteorológica utilizada, mostrando a importância da escolha da localização apropriada da estação, conforme o objetivo do monitoramento. O Índice de Seca Keetch-Byram apresentou o melhor desempenho para predizer a ocorrência de incêndios considerando todos os usos do solo, e para as áreas de floresta e desmatadas separadamente. Apesar de sua simplicidade, o índice de Angstrom se destacou por seu desempenho na predição de dias com mais de seis focos de calor detectados.(AU)
Assuntos
Solo , Zonas Climáticas/análise , Conservação dos Recursos Naturais , Incêndios FlorestaisRESUMO
Down-core changes in sedimentary facies, elemental geochemistry, pollen, spore, δ13C, δ15N and radiocarbon records from a filled lake, named R4, of the Serra Sul dos Carajás were used to study the relationship between the paleomorphological and paleoecological processes and their significance for Holocene paleoclimatology of the southeast Amazonia. The sediment deposition of the R4 lake started around 9500 cal yr BP. Increase of detrital components from 9500 to 7000 cal yr BP suggests high weathering of surrounding catchment rocks and soils, and deposition into the lake basin under mudflows. At that time, montane savanna and forest formation were already established suggesting predominance of wet climate. However, from 7000 to 3000 cal yr BP, a decline of detrital input occurred. Also, forest formation and pteridophytes were declined, while palms and macrophytes were remained relatively stable, indicating that water levels of the lake is likely dropped allowing the development of plants adapted to subaerial condition under drier climate conditions. After 3000 cal yr BP, eutrophication and low accommodation space lead to high lake productivity and the final stage of the lake filling respectively, and forest formation may has acquired its current structure, which suggests return of wetter climate conditions.
Assuntos
Radioisótopos de Carbono/análise , Sedimentos Geológicos/análise , Paleontologia/métodos , Pólen , Árvores , BrasilRESUMO
High-resolution satellite images, digital elevation models, bathymetric and sedimentological surveys coupled with statistical analysis were used to understand the physical environment and discuss their influence on water quality of the five upland lakes of Serra Sul dos Carajás, southeast Amazonia. The lakes have mid-altitude ranges (elevation), very small (catchment) and shallow to very shallow (central basins). Based on the length, area and volume, Violão and TI (Três Irmãs)-3 lakes may present large vertical movements of the water due to wind action and weakly stratified waters. Trophic conditions based on depth and shore development (Ld) parameters must be used with caution, since Amendoim Lake is relatively deep, but it is oligotrophic to ultra-oligotrophic. Ld values suggest that the lakes are circular to subcircular and are likely formed by solution process, as also suggested by volume development. TI-2 Lake is only presenting convex central basin and has highest dynamic ratio (DR), thus it may have high sedimentation and erosion rates. Based on the relationship between studied parameters, morphometric index and DR likely influence temperature and dissolved oxygen of waters of TI-2 Lake due to its depth profile and wind-induced surface mixing. Nevertheless, water quality parameters are controlled by catchment characteristics of the lakes.
RESUMO
The degradation of subterranean habitats is believed to represent a serious threat for the conservation of obligate subterranean dwellers (troglobites), many of which are short-range endemics. However, while the factors influencing cave biodiversity remain largely unknown, the influence of the surrounding landscape and patterns of subterranean connectivity of terrestrial troglobitic communities have never been systematically assessed. Using spatial statistics to analyze the most comprehensive speleological database yet available for tropical caves, we first assess the influence of iron cave characteristics and the surrounding landscape on troglobitic communities from the Eastern Amazon. We then determine the spatial pattern of troglobitic community composition, species richness, phylogenetic diversity, and the occurrence of frequent troglobitic species, and finally quantify how different landscape features influence the connectivity between caves. Our results reveal the key importance of habitat amount, guano, water, lithology, geomorphology, and elevation in shaping iron cave troglobitic communities. While mining within 250 m from the caves influenced species composition, increasing agricultural land cover within 50 m from the caves reduced species richness and phylogenetic diversity. Troglobitic species composition, species richness, phylogenetic diversity, and the occurrence of frequent troglobites showed spatial autocorrelation for up to 40 km. Finally, our results suggest that the conservation of cave clusters should be prioritized, as geographic distance was the main factor determining connectivity between troglobitic communities. Overall, our work sheds important light onto one of the most overlooked terrestrial ecosystems, and highlights the need to shift conservation efforts from individual caves to subterranean habitats as a whole.
RESUMO
This study estimated the reference evapotranspiration rate (ETo) for the Itacaiúnas River Watershed (IRW), Eastern Amazonia, and measured the accuracy of eight empirical equations: Penman-Monteith (PM), Priestley-Taylor (PT), Hargreaves and Samani (HS), Camargo (CAM), Thornthwaite (TH), Hamon (HM), Kharrufa (KF) and Turc (TC) using monthly data from 1980 to 2013. In addition, it verifies the regional applicability to the IRW using a for the Marabá-PA station. The methods TC and PM (FAO56) presented the best results, which demonstrate that radiation and higher temperatures are the dominant drivers in the Evapotranspiration process, while relative humidity and wind speed have a much smaller impact. The temporal and spatial variability of ETo for IRW show has strong seasonality, increasing during the dry season and decreasing during the rainy season. The statistical analyses at 1% level of significance, indicates that there is no correlation of the residuals between the dry and rainy seasons, and test of the physical parameters such as mean temperature, solar radiation and relative air humidity explains the variations of ETo.
RESUMO
ABSTRACT This study estimated the reference evapotranspiration rate (ETo) for the Itacaiúnas River Watershed (IRW), Eastern Amazonia, and measured the accuracy of eight empirical equations: Penman-Monteith (PM), Priestley-Taylor (PT), Hargreaves and Samani (HS), Camargo (CAM), Thornthwaite (TH), Hamon (HM), Kharrufa (KF) and Turc (TC) using monthly data from 1980 to 2013. In addition, it verifies the regional applicability to the IRW using a for the Marabá-PA station. The methods TC and PM (FAO56) presented the best results, which demonstrate that radiation and higher temperatures are the dominant drivers in the Evapotranspiration process, while relative humidity and wind speed have a much smaller impact. The temporal and spatial variability of ETo for IRW show has strong seasonality, increasing during the dry season and decreasing during the rainy season. The statistical analyses at 1% level of significance, indicates that there is no correlation of the residuals between the dry and rainy seasons, and test of the physical parameters such as mean temperature, solar radiation and relative air humidity explains the variations of ETo.