Adriano Marlison Leão De de Sousa

Prof. Dr. Adriano Marlison Leão De de Sousa


Research Focus & Metrics

Academic Career Length

19Years (2008-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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29 June 2024 in Climate
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Everaldo Barreiros de SouzaEveraldo Barreiros de Souza
Everaldo Barreiros de Souza
BSBrenda C. S. Silva
Brenda C. S. Silva
ESEmilene Monteiro Furtado Serra
Emilene Monteiro Furtado Serra
MBMelgris José Becerra
Melgris José Becerra
ACAlan Cavalcanti Cunha
Alan Cavalcanti Cunha
TATercio Ambrizzi
Tercio Ambrizzi
The focus of this work is on small municipalities (population below 50 thousand inhabitants) that cover around 87% of the territory of the Brazilian Legal Amazon (BLA). Based on a comprehensive integrated analysis approach using the three components hazard (climate extremes from CMIP6 future scenarios), exposure (directly affected population), and vulnerability (subdimensions of susceptibility and coping/adaptive capacity by using multidimensional indicators), the latter two using current datasets provided by the official Census IBGE 2022, we document a quantitative assessment of the risk R of natural disasters in the BLA region. We evidenced a worrying and imminent intensification of the curve of R in most Amazonian municipalities over the next two 25-year periods. The overall results of the highest proportions of R (total municipalities affected) pointed out the Amazonas, Roraima, Pará, and Maranhão as the main states, presenting projected categories of R high in the near future (2015 to 2039) and very high in the far future (2040 to 2064). The detailed assessment of the susceptibility and coping/adaptive capacity allowed us to elucidate the principal indicators that aggravate the degree of vulnerability: economy, the precariousness of urban infrastructure, medical services, communication, and urban mobility, whose combined factors, unfortunately, reveal a widespread poverty profile along the small Amazonian municipalities. Our scientific findings can assist decision makers in targeted strategies planning and public policies to minimize and mitigate ongoing and future climate change.

1 September 2017 in Revista Caatinga
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PSPaulo Jorge Souza
Paulo Jorge Souza
VFVivian Dielly DA Silva Farias
Vivian Dielly DA Silva Farias
MLMarcus José Alves de Lima
Marcus José Alves de Lima
TRThaynara Fernandes Ramos
Thaynara Fernandes Ramos
ASAdriano Marlison Leão De de Sousa
Adriano Marlison Leão De de Sousa
This work evaluated the effect of soil water availability on growth and productivity variables of cowpea in northeastern Pará, Brazil. The experiment was carried out in a field of 2,100 m2 at the experimental site of the Federal Rural University of Amazon, during the driest season of the years 2011, 2012 and 2013, in a completely randomised design with two treatments (irrigated and non-irrigated), both with 12 replications in the reproductive phase (2012 and 2013). Growth and productivity data were submitted to analysis of variance with two variation factors (water regime and experimental year) at 5% probability. Student's t -test at 5% probability was used in the means of the stomatal conductance data, since this was monitored only in 2012. Final biomass production presented a reduction of 54.3% in 2012 and 26.4% in 2013 as a result of water deficit (DEF) of 76 and 26 mm, respectively. Mean stomatal conductance was reduced by 73% in the grain-filling stage as a result of the lower water availability during this period. Average cowpea productivity under water deficit reached 1,257 kg ha-1 in 2012 and 1,396 kg ha-1 in 2013. The reduction in water supply over the reproductive period significantly decreased production by 72 and 41% (F test, p < 0.05) in 2012 and 2013, respectively. An accumulated water deficit during the reproductive phase caused a maximum LAI reduction of 47% in 2012 (DEF of 76 mm) and of 13% in 2013 (DEF of 26 mm).

18 May 2021 in Horticulturae
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DFDenilson Pontes Ferreira
Denilson Pontes Ferreira
DSDenis De Pinho Sousa
Denis De Pinho Sousa
HNHILDO GIUSEPPE GARCIA CALDAS NUNES
HILDO GIUSEPPE GARCIA CALDAS NUNES
JPJoao Vitor de Nóvoa Pinto
Joao Vitor de Nóvoa Pinto
VFVivian D. S. Farias
Vivian D. S. Farias
PSPaulo Jorge Souza
Paulo Jorge Souza
Cowpea (Vigna unguiculata (L.) Walp.) is a leguminous species widely cultivated in northern and northeastern Brazil. In the state of Pará, this crop still has low productivity due to several factors, such as low soil fertility and climatic adversity, especially the water deficiency. Therefore, the present study aimed at evaluating the physiological parameters and the productivity of cowpea plants under different water depths. The experiment was conducted in Castanhal/Pará between 2015 and 2016. A randomized block design was applied with six replications and four treatments, represented by the replacement of 100%, 50%, 25% and 0% of the water lost during crop evapotranspiration (ETc), starting from the reproductive stage. The rates of net photosynthesis (A), stomatal conductance (gs), leaf transpiration (Eleaf), substomatal CO2 concentration (Ci), leaf temperature (Tleaf) and leaf water potential (Ψw) were determined in four measurements at the R5, R7, R8 and R9 phenological stages. Cowpea was sensitive to the water availability in the soil, showing a significant difference between treatments for physiological variables and productivity. Upon reaching a Ψw equal to −0.88 MPa, the studied variables showed important changes, which allows establishing this value as a threshold for the crop regarding water stress under such experimental conditions. The different water levels in the soil directly influenced productivity for both years, indicating that the proper water supply leads to better crop growth and development, increasing productivity.

1 May 2018 in Revista Brasileira de Engenharia Agrícola E Ambiental
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ASAntonio K. L. Silva
Antonio K. L. Silva
ASAdriano Marlison Leão De de Sousa
Adriano Marlison Leão De de Sousa
JSJoyse Tatiane Souza dos Santos
Joyse Tatiane Souza dos Santos
JVJoão M. Villela
João M. Villela
Lucietta Guerreiro MartoranoLucietta Guerreiro Martorano
Lucietta Guerreiro Martorano
Silvio CrestanaSilvio Crestana
Silvio Crestana
Currently, an activity that has become strategic at a national level is the cultivation of oil palm (Elaeis guineensis) in the northeast region of the Pará State, in eastern Brazilian Amazon. However, the impacts of this crop expansion on the hydro-sedimentological cycle are still unknown. Therefore, this study estimated the impacts of oil palm crop expansion on sediment production in a sub-basin under consolidated use of this crop. The Soil and Water Assessment Tool (SWAT) model was applied in the Mariquita sub-basin, calibrated by the flow regionalization technique, using data measured in the field with a current meter. Simulation results indicated an increase in sediment production between the years 2008 and 2013, which can be attributed to the large reduction of areas of secondary vegetation that were replaced by pasture, oil palm and general agriculture. Oil palm areas had a lower average monthly sediment yield in the rainiest period in all simulated years, compared with areas of general agriculture and pasture.

20 March 2018 in Ambiente e Agua - An Interdisciplinary Journal of Applied Science
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RSRégia Simony Braz Da Silva
Régia Simony Braz Da Silva
ASAdriano Marlison Leão De de Sousa
Adriano Marlison Leão De de Sousa
SSSilvana Do Socorro Veloso Sodré
Silvana Do Socorro Veloso Sodré
MVMaria Isabel Vitorino
Maria Isabel Vitorino
O objetivo deste trabalho foi avaliar a sazonalidade da qualidade da água superficial e subterrânea nas proximidades do lixão de Salinópolis, situado na Vila de Cuiarana, por meio da caracterização da precipitação da região e da sua influência na composição físico-química e microbiológica das águas locais. Para isso, foram observados os dados dos acumulados mensais da precipitação local, medição da velocidade de infiltração no solo e medição da vazão dos rios Cachoeira e Teixeira. Foram selecionados os parâmetros físico-químicos e bacteriológicos: pH, oxigênio dissolvido (OD), temperatura da água, sólidos totais dissolvidos (TDS), turbidez, condutividade elétrica (CE), salinidade, amônia, nitrato, coliformes totais e Escherichia coli; e os metais: alumínio, cádmio, chumbo, cobre, cromo, ferro, manganês, mercúrio, níquel e zinco. Tanto as águas superficiais quanto as subterrâneas se apresentaram inadequadas para uso e consumo humano. Parâmetros como OD, ferro, alumínio, chumbo, mercúrio, coliformes totais e E. coli estão em desconformidade com as legislações vigentes. O período chuvoso influenciou negativamente a qualidade em águas superficiais. Em águas subterrâneas, parâmetros como amônia, nitrato, ferro, mercúrio e chumbo estiveram em maiores concentrações no período menos chuvoso; enquanto, CE, E. coli, coliformes totais e alumínio aumentaram suas concentrações no período chuvoso.

1 January 2016 in Revista Brasileira de Fruticultura
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PSPaulo Jorge Souza
Paulo Jorge Souza
JRJuliana Chagas Rodrigues
Juliana Chagas Rodrigues
ASAdriano Marlison Leão De de Sousa
Adriano Marlison Leão De de Sousa
RLRenata Trindade DE Lima
Renata Trindade DE Lima
EREdson José Paulino DA Rocha
Edson José Paulino DA Rocha
Samuel Ortega-FariasSamuel Ortega-Farias
Samuel Ortega-Farias
The aim of this study was to estimate the water consumption in mango orchard during its phenological stages in the northeastern of the State of Pará, Brazil. For this purpose, it was installed and instrumented a micrometeorological tower in a mango orchard, cv. Tommy Atkins, of 22 years old, with data collected during the crops of 2010/2011 and of 2011/2012. The actual crop evapotranspiration was estimated from the energy balance using the Bowen ratio technique. The crops were subjected to different weather conditions, consequently, some differences in the Bowen ration values were observed. The evapotranspiration suffered influences of meteorological conditions during the period. The actual crop evapotranspiration during its reproductive period ranged between 402.9 and 420 mm with a mean daily water consumption of 3.8 mm at flowering, of 4.25 mm at fruit fall, of 3.56 mm at fruit formation, of 3.0 mm at fruit maturation and of 3.73 mm for the whole period.