scholarly journals Flow-velocity model for hydrokinetic energy availability assessment in the Amazon

2019 ◽  
Vol 42 ◽  
pp. e45703
Author(s):  
Josias da Silva Cruz ◽  
Claudio José Cavalcante Blanco ◽  
Antônio César Pinho Brasil Junior

The Brazilian hydrological information network does not provide data series of daily velocities. The river velocities are important for the study of hydrokinetic potential. Therefore, the work proposes a model called flow-velocity that estimates the average daily velocity and the distribution of the velocity profile of the cross section of rivers. The model was applied to the Amazon basin, using the highest and lowest flow rates of the historical series. The highest and lowest average velocities found in the Amazon River were 2.27 m s-1 and 0.735 m s-1, respectively. The main contributors to the Amazon River presented average daily velocities close to 2.0 ms-1 for the flood period, but in the dry season these velocities did not exceed 0.5 m s-1. Thus, it was verified that the Amazon River has hydrokinetic potential throughout the year and its tributaries during the flood period.

2019 ◽  
Vol 12 (3) ◽  
pp. 988
Author(s):  
Rogério Souza Aguiar ◽  
Edson José Paulino da Rocha ◽  
José Augusto de Souza Junior ◽  
Joyse Tatiane Souza dos Santos ◽  
Josiane Sarmento Dos Santos

As cheias e vazantes do rio Amazonas passaram a ser mais persistentes ao longo dos anos. Este estudo busca analisara influência da variabilidade temporal em escala de bacia hidrográfica sobre o regime do rio Amazonas, a partir das vazões da estação hidrológica da Agência Nacional de Águas – ANA, localizada em Óbidos, no Estado do Pará em uma série histórica de janeiro/1970 a dezembro/2013. Além do tempo, o estudo analisou a intensidade do El Niño e La Niña. Como esperado, o tempo influenciou na vazão média interanual encontrada de 98.723 m3/s para os 44 anos da série analisada. Porém com variabilidade anual do regime do rio Amazonas de intensas proporções temporais, com a vazão variando de ordem de 72.380 m3/s (como em 1997) no regime de vazante até uma ordem de 131.620 m3/s (como em 1974) no regime de cheia. Também foi identificado que fenômenos de El Niño e La Niña modularam eventos climáticos extremos sobre as vazões da Bacia Amazônica em cada ano. A análise interanual mostrou que os anos de baixas vazões, possuíam a característica de persistência de ocorrência em relação às altas vazões. A partir de 1989, houve um aumento em relação à amplitude média da vazão de 87.727 m3/s devido a fortes níveis mínimos registrados. Ao analisar a vazão normalizada percebeu-se que na maioria dos anos de baixa vazão foram também anos do fenômeno El Niño. Constatado esta persistência de baixas vazões, investigaram-se os fatores de armazenamento e disponibilidade do rio Amazonas.   Analysis of Hydrological Regime Componentof the Amazonas River Basin in Years of Climate Events. ABSTRACTThe floods and drains of the Amazon River have become more persistent over the years. This study seeks to analyze the influence of the temporal variability in the basin scale on the Amazon river regime, from the flows of the hydrological station of the National Water Agency - ANA, located in Óbidos, State of Pará, in a historical series from January/1970 to December /2013. Besides time, the study analyzed the intensity of El Niño and La Niña. As expected, time influenced the annual interannual flow rate of 98,723 m3/s for the 44 years of the analyzed series. However, with an annual variability of the Amazon river regime of intense flows, with an increase of 72,380 m3/s (as in 1997) in the effluent regime up to an order of 131,620 m3/s (as in 1974) in the flood regime. It was also identified that El Niño and La Niña phenomena modulated extreme climatic events on the Amazon Basin flows each year. The year-on-year analysis showed that the years of low flows had a persistence of occurrence in relation to high flows. As of 1989, there was an increase in relation to the average flow amplitude of 87,727 m3/s due to the strong minimum levels recorded. Analyzing the normalized flow rate, it was observed that in most of the years of low flow there were also years of the El Niño phenomenon. Considering this persistence of low flows, we investigated the storage and availability factors of the Amazon River.Keywords: Time flows. Ecological Maintenance.Amazonriver. 


2019 ◽  
Vol 20 (72) ◽  
pp. 360-374 ◽  
Author(s):  
Maria do Socorro Rocha da Silva ◽  
Eduardo Antonio Ríos-Villamizar ◽  
Hillândia Brandão da Cunha ◽  
Sebastião Átila Fonseca Miranda ◽  
Sávio José Filgueiras Ferreira ◽  
...  

The geological diversity of the Amazon Basin, as well as the pluvial regime, influences the characteristics of the waters. To know the water types of the rivers of the Amazon basin, 288 superficial water samples were collected, 94 of them along the Amazon River and 194 in their tributaries, from March 2009 to September 2012. The physical, chemical, and physicochemical properties were analyzed. Rivers with pH between 6.5 and 7.6 and electrical conductivity (40.00 - 80.00 μS cm-1) are water bodies that are influenced by the Andean region (e.g., the Amazon River and some of its right bank tributaries). On the other hand, the rivers with pH in the range of 3.5 to 5.5 and conductivity <30.00 μS cm-1, which are Amazon River’s left bank tributaries, reflect the characteristics of the Guiana Shield. The rivers with pH (6.0 to 7.0), low ionic charge, and conductivity <40.0 μS cm-1, such as the lower Amazon River’s right bank tributaries (Tapajos and Xingu) which are influenced by the Central Brazilian Shield, and also the middle/upper Amazon River’s right bank tributaries (Tefé, Coari and Jutaí).


Check List ◽  
2010 ◽  
Vol 6 (3) ◽  
pp. 397 ◽  
Author(s):  
Bradley J. W. Davis ◽  
Scott T. Olmstead

We present new distribution records for Topaza pella (Linnaeus, 1758) in the southern reaches of the Amazon Basin in Brazil. The two new localities presented for the species elucidate its range in southern Pará and northern Mato Grosso states, and in consideration of recent records elsewhere south of the Amazon River, suggest that the species is widely distributed across suitable habitat throughout the Brazilian Amazon.


Oryx ◽  
2019 ◽  
Vol 54 (5) ◽  
pp. 696-698 ◽  
Author(s):  
Marcelo Oliveira-da-Costa ◽  
Miriam Marmontel ◽  
Daiane S. X. da-Rosa ◽  
André Coelho ◽  
Serge Wich ◽  
...  

AbstractQuantifying the abundance of species is essential for their management and conservation. Much effort has been invested in surveys of freshwater dolphins in the Amazon basin but river dimensions and complex logistics limit replication of such studies across the region. We evaluated the effectiveness of using unmanned aerial vehicles (UAVs) for surveying two Amazon dolphin species, the tucuxi Sotalia fluviatilis and pink river dolphin Inia geoffrensis, in tropical rivers. In 2016 we conducted drone and visual surveys over 80 km of the Juruá River in Brazil. The aerial surveys provided higher accuracy than human observers in counting individuals detected in groups. Compared to estimates derived from visual surveys, the use of UAVs could provide a more feasible, economical and accurate estimate of Amazon river dolphin populations. The method could potentially be replicated in other important areas for the conservation of these species, to generate an improved index of river dolphin populations in the Amazon.


2019 ◽  
Vol 2019 ◽  
pp. 1-20 ◽  
Author(s):  
Bin Wang ◽  
Chuan-xin Rong ◽  
Jian Lin ◽  
Hua Cheng ◽  
Hai-bing Cai

Taking into account moisture migration and heat change during the soil freezing process, as well as the influence of absolute porosity reduction on seepage during the freezing process, we construct a numerical model of hydrothermal coupling using laws of conservation of energy and mass. The model is verified by the results of large-scale laboratory tests. By applying the numerical calculation model to the formation of artificial shaft freezing temperature fields under the action of large-flow groundwater, we conclude that groundwater with flow rates of less than 5 m/d will not have a significant impact on the artificial freezing temperature field. The maximum flow rates that can be handled by single-row freezing pipes and double-row freezing pipes are 10 m/d and 20 m/d, respectively, during the process of freezing shaft sinking. By analyzing the variation of groundwater flow rate during freezing process, we find that the groundwater flow velocity can reach 5–7 times the initial flow velocity near the closure moment of the frozen wall. Finally, in light of the action characteristics of groundwater on the freezing temperature field, we make suggestions for optimal pipe and row spacing in freezing pipe arrangement.


Author(s):  
Kenneth D. LeBay ◽  
Marc D. Polanka ◽  
Richard D. Branam

The Ultra Compact Combustor (UCC) has shown viable merit for significantly improving gas turbine combustor performance. UCC models for small engines can provide centrifugal loading up to 4,000 gs. However, as the scale of the combustor increases, the g-load will necessarily decrease and the radial vane height will increase. Thus, the importance of understanding flame migration over increasing radial vane heights is pivotal to the applicability of this design to larger engine diameters. The Air Force Institute of Technology’s Combustion Optimization and Analysis Laser laboratory studied this effect with a sectional UCC model using three different vane heights. By varying the mass flow rates of the circumferential UCC section, the g-loading was varied from 500–2,000 gs. Two-line Planar Laser Induced Fluorescence at 10Hz was used for 2D temperature profiles. High-speed video at 2kHz was also used for qualitative flame migration characterization. Several cases were studied varying the radial vane height, the circumferential g-load, and the UCC/core mass flow ratio but specifically focusing on the interaction between matching the core mass flow and the core freestream velocity among the different vane heights. Finally, the decreased core flow velocity for the same mass flow weakened the shear layer between the main and cavity flows and this allowed deeper flame migration into the core flow from the UCC. Control of the overall flame migration is the key to produce desirable combustor exit temperature profiles. Increased spans lead to higher velocity gradients and increased flame injection angles at the same mass flow rates. However, at the same core flow velocities and UCC to core flow velocity ratios the flame injection angle was relatively independent of the radial vane height and almost entirely dependent on the core flow velocity alone.


2016 ◽  
Vol 6 (1) ◽  
Author(s):  
Cedric Blatter ◽  
Eelco F. J. Meijer ◽  
Ahhyun S. Nam ◽  
Dennis Jones ◽  
Brett E. Bouma ◽  
...  

Author(s):  
Joana Maria Pujadas-Mora ◽  
Gabriel Brea-Martínez

Unequal distribution of wealth is a matter of growing concern in contemporary society, but it is also one with deep roots in the past. Several authors have traced the origins of this inequality by reconstructing historical series and collecting and harmonising data from sources and records with uneven territorial and temporal cover (Milanovic et al. (2011), Alfani (2015) Piketty (2014 and 2020)). Few places in the world have data series that make it possible to reconstruct the patterns of socioeconomic inequality by drawing on a single source. Barcelona, including its hinterland, is one of these places. The Barcelona Historical Marriage Database, which was created under the auspices of the Advanced Grant project Five Centuries of Marriages headed by Professor Anna Cabré, has made it possible to analyse, over a period of five centuries, the distribution of wealth by studying the taxes levied on marriages held in the Diocese from 1451 to 1880. This number of Perspectives Demogràfiques offers an account of the evolution of inequality from the ancien régime through to the consolidation of industrialisation, the concentration of wealth, and the composition and replacement of economic elites in the Barcelona area.


2020 ◽  
Author(s):  
Danilo Rabino ◽  
Marcella Biddoccu ◽  
Giorgia Bagagiolo ◽  
Guido Nigrelli ◽  
Luca Mercalli ◽  
...  

&lt;p&gt;Historical weather data represent an extremely precious resource for agro-meteorology for studying evolutionary dynamics and for predictive purposes, to address agronomical and management choices, that have economic, social and environmental effect. The study of climatic variability and its consequences starts from the observation of variations over time and the identification of the causes, on the basis of historical series of meteorological observations. The availability of long-lasting, complete and accurate datasets is a fundamental requirement to predict and react to climate variability. Inter-annual climate changes deeply affect grapevine productive cycle determining direct impact on the onset and duration of phenological stages and, ultimately, on the grape harvest and yield. Indeed, climate variables, such as air temperature and precipitation, affect evapotranspiration rates, plant water requirements, and also the vine physiology. In this respect, the observed increase in the number of warm days poses a threat to grape quality as it creates a situation of imbalance at maturity, with respect to sugar content, acidity and phenolic and aromatic ripeness.&lt;/p&gt;&lt;p&gt;A study was conducted to investigate the relationships between climate variables and harvest onset dates to assess the responses of grapevine under a global warming scenario. The study was carried out in the &amp;#8220;Monferrato&amp;#8221; area, a rainfed hillslope vine-growing area of NW Italy. In particular, the onset dates of harvest of different local wine grape varieties grown in the Vezzolano Experimental Farm (CNR-IMAMOTER) and in surrounding vineyards (affiliated to the Terre dei Santi Cellars) were recorded from 1962 to 2019 and then related to historical series of climate data by means of regression analysis. The linear regression was performed based on the averages of maximum and minimum daily temperatures and sum of precipitation (1962&amp;#8211;2019) calculated for growing and ripening season, together with a bioclimatic heat index for vineyards, the Huglin index. The climate data were obtained from two data series collected in the Experimental farm by a mechanical weather station (1962-2002) and a second series recorded (2002-2019) by an electro-mechanical station included in Piedmont Regional Agro-meteorological Network. Finally, a third long-term continuous series covering the period from 1962 to 2019, provided by Italian Meteorological Society was considered in the analysis.&lt;/p&gt;&lt;p&gt;The results of the study highlighted that inter-annual climate variability, with a general positive trend of temperature, significantly affects the ripening of grapes with a progressive anticipation of the harvest onset dates. In particular, all the considered variables excepted precipitation, resulted negatively correlated with the harvest onset date reaching a high level of significance (up to P&lt; 0.001). Best results have been obtained for maximum temperature and Huglin index, especially by using the most complete dataset. The change ratios obtained using datasets including last 15 years were greater (in absolute terms) than results limited to the period 1962-2002, and also correlations have greater level of significance. The results indicated clearly the relationships between the temperature trend and the gradual anticipation of harvest and the importance of having long and continuous historical weather data series available.&lt;/p&gt;


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