Bibliografías temáticas / Amazonian Andes

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Literatura académica sobre el tema "Amazonian Andes"

Autor: Grafiati
Publicado: 25 de mayo de 2024
Última modificación: 31 de julio de 2025

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Artículos de revistas sobre el tema "Amazonian Andes"

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Bush, M. B., M. R. Silman, C. McMichael, and S. Saatchi. "Fire, climate change and biodiversity in Amazonia: a Late-Holocene perspective." Philosophical Transactions of the Royal Society B: Biological Sciences 363, no. 1498 (2008): 1795–802. http://dx.doi.org/10.1098/rstb.2007.0014.

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Fire is an important and arguably unnatural component of many wet Amazonian and Andean forest systems. Soil charcoal has been used to infer widespread human use of landscapes prior to European Conquest. An analysis of Amazonian soil carbon records reveals that the records have distinct spatial and temporal patterns, suggesting that either fires were only set in moderately seasonal areas of Amazonia or that strongly seasonal and aseasonal areas are undersampled. Synthesizing data from 300 charcoal records, an age–frequency diagram reveals peaks of fire apparently coinciding with some periods of
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Nores, Manuel. "The Western Amazonian Boundary for Avifauna Determined by Species Distribution Patterns and Geographical and Ecological Features." International Journal of Ecology 2011 (2011): 1–7. http://dx.doi.org/10.1155/2011/958684.

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In northern South America, an extensive tropical lowland runs 5,000 km from the Atlantic coast to the foot of the Andes. The slope is gentle until about 500 m where the eastern Andes rise abruptly. The lowland supports Amazonia, which is the most extensive tract of tropical rainforest on the planet. Most of its boundaries are well defined, but the boundary between Amazonia and the forest of the eastern slopes of the Andes has not been clearly defined. To determine for avifauna whether Amazonia is restricted to the lowland of northern South America or whether it also extends up into the eastern
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Borda, Víctor, Isabela Alvim, Marla Mendes, et al. "The genetic structure and adaptation of Andean highlanders and Amazonians are influenced by the interplay between geography and culture." Proceedings of the National Academy of Sciences 117, no. 51 (2020): 32557–65. http://dx.doi.org/10.1073/pnas.2013773117.

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Western South America was one of the worldwide cradles of civilization. The well-known Inca Empire was the tip of the iceberg of an evolutionary process that started 11,000 to 14,000 years ago. Genetic data from 18 Peruvian populations reveal the following: 1) The between-population homogenization of the central southern Andes and its differentiation with respect to Amazonian populations of similar latitudes do not extend northward. Instead, longitudinal gene flow between the northern coast of Peru, Andes, and Amazonia accompanied cultural and socioeconomic interactions revealed by archeology.
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Stanfield-Mazzi, Maya. "Inka Bird Idiom: Amazonian Feathers in the Andes." Ethnohistory 72, no. 1 (2025): 121–22. https://doi.org/10.1215/00141801-11472796.

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Guayasamin, Juan M. "A new yellow species of glassfrog (Centrolenidae: Nymphargus) from the Amazonian slopes of the Ecuadorian Andes." Zootaxa 3651, no. 1 (2013): 193–200. https://doi.org/10.11646/zootaxa.3652.1.8.

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STURARO, MARCELO JOSÉ, and TERESA C. S. AVILA-PIRES. "Taxonomic revision of the geckos of the Gonatodes concinnatus complex (Squamata: Sphaerodactylidae), with description of two new species." Zootaxa 2869, no. 1 (2011): 1. http://dx.doi.org/10.11646/zootaxa.2869.1.1.

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The Gonatodes concinnatus complex, as here considered, consists of Gonatodes species characterized by a white suprahumeral spot with black margins; vermiculations or not on back; and transversely enlarged scales under the tail, showing the sequence 1’1’1”, and in some specimens 1’1’2” on the anterior portion. Two species are presently recognized in this Amazonian complex: G. concinnatus and G. tapajonicus. New material collected in eastern Amazonia (states of Pará and Amapá, Brazil) made it necessary to review these species. We analyzed several populations within this complex, from Colombia, E
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Bahamonde-Vinueza, Daniela, Hector Cadena-Ortiz, Carlos Cajas-Bermeo, and Elisa Bonaccorso. "Unusual records of Cochlearius cochlearius (Linnaeus, 1766) (Aves: Ardeidae) in the Andes of Ecuador." Check List 10, no. (3) (2014): 687–88. https://doi.org/10.15560/10.3.687.

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We report two high altitude sightings of Boat-billed Heron in the Andes of Ecuador. Based on identification and the localities were the sightings were reported, we suggest that both individuals belong to the Amazonian population of this species.
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Harvey, Michael B., Ana Almendáriz, Jorge Brito, and Diego Batallas. "A new species of Noblella (Anura: Craugastoridae) from the Amazonian Slopes of the Ecuadorian Andes with Comments on Noblella lochites (Lynch)." Zootaxa 3635, no. 1 (2013): 1–14. https://doi.org/10.11646/zootaxa.3635.1.1.

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Harvey, Michael B., Almendáriz, Ana, Brito, Jorge, Batallas, Diego (2013): A new species of Noblella (Anura: Craugastoridae) from the Amazonian Slopes of the Ecuadorian Andes with Comments on Noblella lochites (Lynch). Zootaxa 3635 (1): 1-14, DOI: 10.11646/zootaxa.3635.1.1
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Arteaga-Chávez, William Andrés, José María Loaiza, Daniel Valencia, et al. "DIVERSIDAD DE AVES DEL OESTE DE LA PROVINCIA DE CARCHI, ECUADOR." Revista Ecuatoriana de Ornitología 11, no. 1 (2025): 1–49. https://doi.org/10.18272/reo.v11i1.3315.

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Describing bird diversity patterns in complex biogeographic regions such as the Andes Mountains is crucial for understanding their biogeography and evolution. In Northern Ecuador lies the province of Carchi, geographically located in the inter-Andean valley, over the Pasto massif, where the western and eastern Ecuadorian branches diverge southward. Western Carchi, settled on the western Andean Cordillera, exhibits a wide altitudinal gradient and vegetation turnover from lowlands to high Andes. Although the area is part of the Chocó bioregion, a global biodiversity and endemism hotspot, knowled
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Guayasamin, Juan M., José Vieira, Richard E. Glor, and Carl R. Hutter. "A new glassfrog (Centrolenidae: Hyalinobatrachium) from the Topo River Basin, Amazonian slopes of the Andes of Ecuador." Amphibian & Reptile Conservation 13, no. 2 (2019): 133–44. https://doi.org/10.5281/zenodo.11405283.

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Guayasamin, Juan M., Vieira, José, Glor, Richard E., Hutter, Carl R. (2019): A new glassfrog (Centrolenidae: Hyalinobatrachium) from the Topo River Basin, Amazonian slopes of the Andes of Ecuador. Amphibian & Reptile Conservation (e194) 13 (2): 133-144, DOI: 10.5281/zenodo.11405283
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Tesis sobre el tema "Amazonian Andes"

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Andriolli, Custodio Michele. "Evolution du système Andes-Amazonie-Océan Atlantique au cours du Cénozoïque." Electronic Thesis or Diss., Toulouse 3, 2023. http://www.theses.fr/2023TOU30262.

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Le système "source to sink" (S2S) Andes-Amazone-Marge équatoriale sud-américaine (AAMESA) qui s'étend sur environ 3 200 km et est situé au nord de la plate-forme sud-américaine, un des plus grands systèmes S2S au monde. Actuellement, le système AAMESA est contrôlé par les Andes d'un point de vue sédimentaire, car 95 % du flux annuel moyen de sédiments en suspension fournis par l'Amazone à l'océan Atlantique provient d'affluents andins. Malgré de récents progrès détaillant les influences des processus de construction et d'érosion des Andes sur l'origine et l'évolution et l'enregistrement sédime
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2

Calderón, Ysabel. "Architecture structurale, bilans sédimentaires et potentiel hydrocarburifère d'une zone de transition "wedgetop-foredeep" de rétro-bassin d'avant-pays : exemple des bassins Marañon et Huallaga du Nord-Pérou." Thesis, Toulouse 3, 2018. http://www.theses.fr/2018TOU30038/document.

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Cette thèse, par son approche multidisciplinaire et l'interprétation d'une quantité importante de données industrielles, apporte de nouveaux éléments dans la compréhension des systèmes de bassin d'avant-pays, en particulier dans le domaine andino-amazonien du nord-Pérou. Elle propose un nouveau modèle stratigraphique et structural de cette région, et reconstitue l'histoire de la déformation et de la sédimentation tout en les quantifiant, données indispensables pour modéliser les systèmes pétroliers et réduire les risques en exploration. Les résultats montrent que l'architecture structurale du
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Hermoza, Wilber. "Dynamique tectono-sédimentaire et restauration séquentielle du rétro-bassin d'avant-pays des Andes centrales." Toulouse 3, 2004. http://www.theses.fr/2004TOU30134.

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Le bassin d'avant-pays rétro-arc des Andes Centrales est considéré comme un exemple typique de système de bassin d'avant-pays (Horton et DeCelles, 1997). Les trois régions étudiées sont le bassin nord-amazonien (3ʿ-8ʿS), le bassin sud-amazonien (11ʿ-12ʿS) et le bassin sud est bolivien (19ʿ-20ʿS). Le système de bassin d'avant-pays des Andes Centrales constitue un domaine privilégié où l'analyse de la déformation peut se faire de façon concomitante avec l'étude du remplissage sédimentaire. Cette étude nous a permis de mieux comprendre la variabilité de l'évolution longitudinale et latitudinale,
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Guibovich, Pérez Pedro M. "Monnier, Marcel. De los Andes hasta Pará. Ecuador - Perú - Amazonas." Pontificia Universidad Católica del Perú, 2012. http://repositorio.pucp.edu.pe/index/handle/123456789/122181.

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Filizola, Naziano. "Transfert sédimentaire actuel par les fleuves amazoniens." Toulouse 3, 2003. http://www.theses.fr/2003TOU30162.

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Roddaz, Martin. "Transition des stades alimentés à suralimentés dans les systèmes de rétro-bassin d'avant-pays : du bassin amazonien." Toulouse 3, 2004. http://www.theses.fr/2004TOU30133.

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Contrairement aux retro-bassins d'avant-pays des Andes du Sud, le bassin d'avant-pays amazonien est caractérisé par une sédimentation tidale au Miocène. Cette thèse montre que le bassin amazonien " marin " peu profond miocène ne formait qu'un seul et même bassin (stade alimenté du bassin). Au Miocène Supérieur, une transgression marine causée par une augmentation de la charge tectonique affecte le bassin amazonien. Au Pliocène, la sédimentation devient continentale (stade suralimenté du bassin). La propagation du prisme chevauchant en est la principale cause. Elle permet une augmentation de l'
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Bes, de Berc Séverine. "Tectonique de chevauchement, surrection et incision fluviatile : (exemple de la zone subandine équatorienne, Haut bassin amazonien)." Toulouse 3, 2003. http://www.theses.fr/2003TOU30072.

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Espinoza, Villar Jhan Carlo. "Impact de la variabilité climatique sur l'hydrologie du bassin amazonien." Paris 6, 2009. https://tel.archives-ouvertes.fr/tel-00379116.

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La variabilité hydro-climatique du bassin amazonien est analysée pour la première fois à partir de données in situ provenant de cinq pays, pendant les 40 dernières années. Une diminution des débits d’étiage et le maintien de forts débits de crues dans le cours principal de l’Amazone, en particulier depuis le début des années 1990, sont liées à une forte diminution des pluies et des débits annuels dans le sud-ouest du bassin et à une augmentation des pluies et des crues dans le nord-ouest, c’est-à-dire essentiellement à la variabilité des régions andines. Pour expliquer la variabilité hydrologi
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Louterbach, Mélanie. "Propagation du front orogénique Subandin et réponse sédimentaire associée dans le bassin d'avant-pays amazonien (Madre de Dios, Pérou)." Toulouse 3, 2014. http://thesesups.ups-tlse.fr/2530/.

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Ce travail s'inscrit dans le cadre de l'étude des chaînes de montagnes et des bassins sédimentaires d'avant-pays rétro-arc associés à une subduction océanique. Il s'intéresse plus particulièrement aux facteurs qui contrôlent la croissance du prisme orogénique oriental andin et à la dynamique de remplissage du bassin d'avant-pays amazonien. La zone d'étude de cette thèse concerne le bassin de Madre de Dios (12º-14ºS) situé au sud du Pérou dans la zone Subandine (ZSA) actuelle, entre la Cordillère Orientale (CO) à l'Ouest et le bassin Amazonien à l'Est. L'approche de la thèse est multidisciplina
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Maurice, Laurence. "Sur les traces du mercure au fil de l'eau, des Andes à l'Amazone." Habilitation à diriger des recherches, Université Paul Sabatier - Toulouse III, 2008. http://tel.archives-ouvertes.fr/tel-00288015.

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Libros sobre el tema "Amazonian Andes"

1

Denevan, William M. Cultivated landscapes of native Amazonia and the Andes. Oxford University Press, 2002.

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2

R, Chuquimamani V. Nonato, Godenzzi Juan Carlos, and Centro de Estudios Regionales Andinos "Bartolomé de las Casas.", eds. Educación e interculturalidad en los Andes y la Amazonía. Centro de Estudios Regionales Andinos "Bartolomé de Las Casas", 1996.

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3

1950-, Monnier Alain, ed. L' Amazonie d'une Baronne russe: Des Andes à l'Atlantique en 1903. Musée d'ethnographie de Genève, 1994.

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1949-, García Alan, ed. Agua madre: Verdades e imágenes : Andes, Amazonía, Centroamérica, Antártida = Mother water truths and images : Andes, Amazon, Central America, Antarctica. Graph Ediciones, 2007.

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5

Kroeger, Axel. La lucha por la salud en el alto Amazonas y en los Andes. Abya-Yala, 1992.

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6

Luna, Carmen. Volkskunst aus Peru: Lebendige Traditionen der Küste der Anden und Amazoniens. Das Museum, 1992.

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7

M, Jones David. Mythology of the Incas: Myths and legends of the ancient Andes, Western Valleys, desert and Amazonia. Southwater, 2003.

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Samper, Diego. Las voces de la tierra: Paisajes sonoros del Amazonas, los Andes y el Caribe. Diego Samper Ediciones, 1999.

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9

Heinrich, Goldschmid, and Goldschmid Archive, eds. De los Andes a la Amazonía del Ecuador: Diario de un explorador, 1939-1946 = Von den Anden in das Amazonasgebiet Ecuadors : Tagebuch eines Forschers, 1939-1946 = From the Andes to the Amazon basin in Ecuador: diary of an explorer, 1939-1946. Trama, 2005.

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10

Pärssinen, Martti. Andes orientales y Amazonía occidental: Ensayos entre la historia y la arqueología de Bolivia, Brasil y Perú. Postgrado de la Carrera de Historia, Universidad Mayor de San Andrés, Colegio Nacional de Historiadores de Bolivia, 2003.

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Capítulos de libros sobre el tema "Amazonian Andes"

1

Sabogal, Ana. "Biodiversity and Endemism of the Andes." In Ecosystem and Species Adaptations in the Andean-Amazonian Region. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-44385-5_5.

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Wanderley, Fernanda, Horacio Vera Cossio, and Jean Paul Benavides. "Paradoxes of development in the Andes and Amazonia." In Buen Vivir and the Challenges to Capitalism in Latin America. Routledge, 2020. http://dx.doi.org/10.4324/9781003091516-11.

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Mora, Andres, Patrice Baby, Martin Roddaz, et al. "Tectonic History of the Andes and Sub-Andean Zones: Implications for the Development of the Amazon Drainage Basin." In Amazonia: Landscape and Species Evolution. Wiley-Blackwell Publishing Ltd., 2011. http://dx.doi.org/10.1002/9781444306408.ch4.

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4

Howard, Rosaleen. "Language ideologies and the Quechuan family." In The Oxford Guide to the Languages of the Central Andes. Oxford University PressOxford, 2024. https://doi.org/10.1093/oso/9780198849926.003.0028.

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Abstract The linguistic panorama of the Central Andes is interwoven with that of Western Amazonia. This chapter explores three related aspects of that relationship. First, we describe areal typological patterns that can be detected across the whole region and that reflect the deepest time depth available to our current methods. Second, we turn to the linguistic geography of the Andean–Amazonian transitional zone, both historically and in the present, revealing a more recent picture of the region’s languages. Third, we present two case studies of Andean–Amazonian linguistic connections: the Aym
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Emlen, Nicholas Q., Rik van Gijn, and Sietze Norder. "The Andean–Amazonian interface." In The Oxford Guide to the Languages of the Central Andes. Oxford University PressOxford, 2024. https://doi.org/10.1093/oso/9780198849926.003.0029.

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Abstract The chapter examines the language ideologies–ways in which value is brought to bear upon the form and use of language in society–in relation to the use of the Quechuan languages in highland Peru and Bolivia, in contemporary times and based on the author’s field research. After a brief synopsis of language ideologies in colonial times and an overview of the sociolinguistic context of Quechuan languages in relation to other Central Andean Indigenous languages, the study takes discourse as its object, both at the “micro” level as people reflect on their own language use and that of other
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6

Tyuleneva, Vera. "The Amazonian Indians as viewed by three Andean chroniclers." In Rethinking the Andes–Amazonia Divide, translated by Adrian J. Pearce. UCL Press, 2020. http://dx.doi.org/10.2307/j.ctv13xps7k.30.

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Kaulicke, Peter. "Early social complexity in northern Peru and its Amazonian connections." In Rethinking the Andes–Amazonia Divide. UCL Press, 2020. http://dx.doi.org/10.2307/j.ctv13xps7k.17.

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Adelaar, Willem F. H. "Linguistic connections between the Altiplano region and the Amazonian lowlands." In Rethinking the Andes–Amazonia Divide. UCL Press, 2020. http://dx.doi.org/10.2307/j.ctv13xps7k.26.

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Hastings, Charles M. "Herders in the Jungle." In The Archaeology of the Upper Amazon. University Press of Florida, 2021. http://dx.doi.org/10.5744/florida/9780813066905.003.0010.

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The Chinchaycocha, a people described by sixteenth century sources as herders of a high Central Andean plateau, may also have been part of the Andean-Amazonian frontier. A combination of archaeological, ethnohistoric, and ethnographic information in support of this argument is presented from eastern valleys below this plateau. A long ridge beside one of these valleys descends to a small basin nestled at the foot of the Andes, at times home to one or more indigenous populations of Amazonian cultural affiliation. An ancient trail along this ridge connected one relatively large Late Intermediate
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Denevan, William M. "Pre-European Forest Cultivation." In Cultivated Landscapes of Native Amazonia And the Andes. Oxford University PressOxford, 2001. http://dx.doi.org/10.1093/oso/9780198234074.003.0007.

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Abstract The forms of Amazonian Indian forest farming examined in Chapters 4 and 5 are mostly recent. It is tempting to believe that pre-European field practices were similar; however, we do not know this. We can only speculate as to what fields may have been like, based on limited evidence. A common assumption is that shifting cultivation was the dominant form of prehistoric cultivation, with forms of intensive (permanent or semipermanent) agriculture being absent or rare (Meggers 1957; 1993-5; 1995; Steward and Faron 1959: 292; Willey 1971: 339; D. J. Wilson 1999: 63). However, there is no a
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Actas de conferencias sobre el tema "Amazonian Andes"

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Pettinger, Alfred M., and Robert Montgomery. "Project Management Considerations of Pipelines Crossing the Andes." In 2010 8th International Pipeline Conference. ASMEDC, 2010. http://dx.doi.org/10.1115/ipc2010-31303.

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Pipeline operators, contractors and governments face important challenges when planning, designing, constructing and operating pipelines which connect the hydrocarbon reserves in the Amazonian basin with population and shipping centers on the Pacific coast. These pipelines cross portions of the Amazonian rainforest, the mountain rainforest along the eastern flank of the Andes, the Andean plateau, and the rural and urban low lying desert areas along the Pacific coast. The need for these pipelines will continue and offers a tremendous opportunity to promote sustainable economic development. Howe
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Moya, John Malpartida, Edward Francisco Oliveros Montes, and Giancarlo Massucco De la Sota. "Integration of Monitoring and Inspection Systems for Geohazard Assessment on Pipelines That Cross Amazonian Jungles and the Andes." In 2012 9th International Pipeline Conference. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/ipc2012-90501.

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As a part of the Integrity Management System, TgP/COGA has identified the weather and outside forces as main threats that increase the risk of the integrity of its pipelines in jungle and mountains areas. In pipelines with particular characteristics such as pipelines that cross the Andes and the Amazonian jungle, this threat can cause even a greater number of failures than other threats such as corrosion or third party damage (TPD). Given this situation, the TgP’s Pipeline Integrity Management System has made a significant development in the use and management of the information provided by th
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Moya, John Erick Malpartida. "Managing Geohazards in Hard Conditions: Monitoring and Risk Assessment of Pipelines That Crosses Amazonian Jungles and the Andes." In ASME 2015 International Pipeline Geotechnical Conference. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/ipg2015-8532.

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The hydrocarbon transmission system that belongs to Transportadora de Gas del Perú (TGP), comprise two parallel pipelines: a natural gas (NG) pipeline, which runs from the upstream facilities at Malvinas, in the Amazonian jungle of Cusco-Peru, to a reception station at Lurín (south of Lima); and a natural gas liquid (NGL) pipeline, which transports the condensed liquids from Malvinas to Pisco, on the coast of Peru. The right-of-way (ROW) crosses the Peruvian jungle with both pipelines in its first 200 kilometers, after climbs over the Andes Mountains at an elevation of 4860 masl, and descends
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Ribera Torró, Esteve. "KUÉLAP VIRTUAL: VIRTUALIZACIÓN DE UNA CIUDADELA PREINCA EN LOS ANDES AMAZÓNICOS DEL PERÚ MEDIANTE FOTOGRAFÍA ESFÉRICA, MODELADO 3D E IMPRESIÓN 3D." In ARQUEOLÓGICA 2.0 - 8th International Congress on Archaeology, Computer Graphics, Cultural Heritage and Innovation. Universitat Politècnica València, 2016. http://dx.doi.org/10.4995/arqueologica8.2016.3567.

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Between 2010 and 2012, under the International Cooperation for Development, a virtual archeology project was realized in Amazonian Andes of Peru. The project was carried out with collaboration from Universitat Politécnica de València (UPV) and the Agencia Española de Cooperación Internacional al Desarrollo (AECID), with archeologists taking part in Proyecto Especial Kuélap (PEK). The goal was to create a virtualization of Kuélap, an important monumental citadel constructed by the ancient Chachapoya society. The fruits of the project was the website “kuelapvirtual.com", that offers an interacti
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Malpartida Moya, John. "Integrity Management System Based on Risk Analysis: A Tool To Prevent Failures on Pipelines Which Crossing Amazonian Jungles and the Andes." In SPE Latin-American and Caribbean Health, Safety, Environment and Social Responsibility Conference. Society of Petroleum Engineers, 2013. http://dx.doi.org/10.2118/165601-ms.

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Gaibor, Janeth, Santiago Guerrero, Martina Grefa, Anne Valdez, and Angel Villavicencio. "High-Resolution Resistivity Image Interpretation to Improve Stratigraphic Model of the ITT Field – Oriente Basin, Ecuador." In SPE Annual Technical Conference and Exhibition. SPE, 2022. http://dx.doi.org/10.2118/210088-ms.

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Abstract The Oriente Basin is an oil-rich province located in Ecuador, where the main reservoirs were deposited during the Late Cretaceous. The distribution and thickness of the sandy reservoirs vary from East to West of the basin. For that, most of the reservoirs are amalgamated to the East and the definition of the contacts between them are difficult. The ITT oil field is located in this area and the main reservoir correspond to M1 Sandstone Member of the Napo Formation. However, in certain areas, the contact between M1 Sandstone Member of Napo Formation and the Basal Tena Member of the Tena
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7

Moya, John Malpartida, and Giancarlo Massucco De la Sota. "Alternative Geohazard Risk Assessment and Monitoring for Pipelines With Limited Access: Amazon Jungle Example." In 2014 10th International Pipeline Conference. American Society of Mechanical Engineers, 2014. http://dx.doi.org/10.1115/ipc2014-33628.

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The Pipeline Integrity Management System (PIMS) of Transportadora de Gas del Peru (TgP) has identified the Weather and Outside Forces such as main threat which increases the risk of the integrity of its pipelines in jungle and mountains areas. In pipelines with particular characteristics such as pipeline which crosses the Andes and the Amazonian jungle, this threat can cause even a greater number of failures than other threats such as Corrosion or Third Party Damage (TPD). Given this situation, the TgP’s PIMS has made a significant development in the use and management of the information provi
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Montes, Edward Francisco Oliveros. "Unprovoked Errors in Geotechnical Monitoring Activities in an RoW." In ASME 2015 International Pipeline Geotechnical Conference. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/ipg2015-8518.

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The Camisea Pipeline Transmission System (PTS), owned by Transportadora de Gas del Perú (TgP) in Peru, consists of two parallel pipelines, a Natural Gas (NG) pipeline and a Liquefied Natural Gas (LNG) pipeline. The NG pipeline is 834 km in length, including a 105 km loop. The LNG pipeline is 557 km in length. The first 210 km, are defined as having Amazonian geotechnical characteristics, with the presence of sedimentary and metamorphic rocks and a deposit of materials that are easily altered, which are associated with the transition between the Amazon plain and the Andes mountains. The area be
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Lopez, Byron G. "Implications of Reduced Heating of Heavy Crude Pipeline on Pump Lubrication Systems." In 2012 9th International Pipeline Conference. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/ipc2012-90315.

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OCP Ecuador S.A. was designed for transporting heavy crude oil from the Ecuadorian Amazonian forest to the Pacific Ocean, crossing the Andes (highest point @ 4060 masl). OCP have four pumping stations PS1, PS2, PS3, PS4 located across the first 182km. Main pumps were designed with an inherent product circulation from pressure connection via orifice to mechanical seal (API Plan 11) for lubricating and cooling. In order to achieve required viscosity, crude oil from the main line must be heated. Low sulfur crude oil (LSCO) is burned for this purpose. In order to optimize fuel consumption, some ef
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Miola, Evandro Carlos. "O auxílio-doença acidentário no Amazonas, antes e depois do FAP/NTEP." In 17º Congresso da Associação Nacional de Medicina do Trabalho. 17 - Supl.1, 2019. http://dx.doi.org/10.5327/z16794435201917s1tl084.

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Informes sobre el tema "Amazonian Andes"

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Flores, Bernardo M., Adriane Esquivel-Muelbert, Marco Ehrlich, et al. NUEVE MANERAS DE EVITAR EL PUNTO DE NO RETORNO EN LA AMAZONÍA. Sustainable Development Solutions Network (SDSN), 2023. http://dx.doi.org/10.55161/oqrm8068.

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Las emisiones globales de gases de efecto invernadero, combinadas con la deforestación y degradación forestal local, están empujando al sistema Amazónico más cerca de un punto de un punto de no retorno. Las sinergias entre perturbaciones pueden provocar un comportamiento de ión inesperado, incluso en regiones forestales que antes se consideraban resilientes al cambio climático, como la Amazonia central u occidental.
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Diversidad Biológica de Tres Tipos de Vertebrados en Cinco Paisajes de Conservación de los Andes-Amazonía Apoyados por Wildlife Conservation Society. Wildlife Conservation Society, 2020. http://dx.doi.org/10.19121/2020.report.42014.

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