Ayala M.,University of Barcelona |
Maldonado J.,National University of Loja |
Paccha E.,University of Chile |
Riba C.,University of Barcelona
Energy Procedia | Year: 2017
This paper describes a complex terrain wind farm case study in the Ecuadorian Andes. The Windfarm Villonaco is located in southern Ecuador, 640km of Quito, 2700 m a.s.l. with 16.5 MW power output. The objective is to compare actual power production from an existing wind farm with power production predicted by Meteodyn WT, which is a CFD tool based on a nonlinear flow model. The results of this work show that the calculation of the annual energy production of the Villonaco Wind Farm using Meteodyn WT is equal to 69.0 GWh / year, with a capacity factor of 53%. © 2017 The Authors.
Lattke J.E.,National University of Loja |
Delsinne T.,Technical University of Loja
Myrmecological News | Year: 2016
Taxonomic clarifications and natural history data dealing with some species of the genus Gnamptogenys are offered: Gnamptogenys bufonis (MANN, 1926) is synonymized under G. simulans (EMERY, 1896); G. vriesi BRANDÃO & LATTKE, 1990 is redescribed and illustrated with SEM and montage images, the peculiar morphology of its compound eye is discussed. Also, an updated key for the G. minuta group species is presented and a nest of G. minuta (EMERY, 1896) is described. The species known up to now as G. costata (EMERY, 1889) is renamed G. coxalis (F. SMITH, 1857), and the species misidentified up to now as G. coxalis (ROGER, 1860) is renamed G. Sinhala LATTKE sp.n.
Larrea M.I.P.,Technical University of Loja |
Daniela Calva Cabrera K.,National University of Loja
Iberian Conference on Information Systems and Technologies, CISTI | Year: 2016
The approval of the Communication law in Ecuador (LOC-2013), alerted to the journalists. In article number 42, related to the professionalization, is considered harmful to the right to the communication and will push the journalist, to return to the classrooms. This article analyzes the university offer related to the communication sciences, and the geographical coverage, showing the universities concentration in the province capitals of Ecuador, and this become in a difficult to be a professional in communication sciences. In Ecuador, the mass communication is deeply marked with the lack ot a professional title, strong critics to the mass media and negative reports about the freedom of speech, mostly in the last 5 years. What the universities have to offer, also have some deficiencies. © 2016 AISTI.
Wilcke W.,University of Bern |
Leimer S.,University of Bern |
Peters T.,Friedrich - Alexander - University, Erlangen - Nuremberg |
Emck P.,Friedrich - Alexander - University, Erlangen - Nuremberg |
And 4 more authors.
Global Biogeochemical Cycles | Year: 2013
Water-bound nitrogen (N) cycling in temperate terrestrial ecosystems of the Northern Hemisphere is today mainly inorganic because of anthropogenic release of reactive N to the environment. In little-industrialized and remote areas, in contrast, a larger part of N cycling occurs as dissolved organic N (DON). In a north Andean tropical montane forest in Ecuador, the N cycle changed markedly during 1998-2010 along with increasing N deposition and reduced soil moisture. The DON concentrations and the fractional contribution of DON to total N significantly decreased in rainfall, throughfall, and soil solutions. This inorganic turn of the N cycle was most pronounced in rainfall and became weaker along the flow path of water through the system until it disappeared in stream water. Decreasing organic contributions to N cycling were caused not only by increasing inorganic N input but also by reduced DON production and/or enhanced DON decomposition. Accelerated DON decomposition might be attributable to less waterlogging and higher nutrient availability. Significantly increasing NO 3-N concentrations and NO3-N/NH4-N concentration ratios in throughfall and litter leachate below the thick organic layers indicated increasing nitrification. In mineral soil solutions, in contrast, NH4-N concentrations increased and NO3-N/NH 4-N concentration ratios decreased significantly, suggesting increasing net ammonification. Our results demonstrate that the remote tropical montane forests on the rim of the Amazon basin experienced a pronounced change of the N cycle in only one decade. This change likely parallels a similar change which followed industrialization in the temperate zone of the Northern Hemisphere more than a century ago. ©2013. American Geophysical Union. All Rights Reserved.
Neill D.A.,Amazonian State University |
Beltran H.,National Major San Marcos University |
Quizhpe W.,National University of Loja
Novon | Year: 2012
Clethra concordia D. A. Neill, H. Beltrán & Quizhpe (Clethraceae), a thin-stemmed shrub or treelet from the sandstone Machinaza plateau in the Cordillera del Cóndor region on the Peru-Ecuador border, is described and illustrated. The new species is distinct from other species of Clethra L. in its small stature and its very small, thick sclerophyllous leaves, which are evidently an ecological adaptation to the highly acidic, nutrient-poor sandstone substrate where it occurs.
Rehmus A.,University of Bern |
Bigalke M.,University of Bern |
Valarezo C.,National University of Loja |
Castillo J.M.,TU Munich |
Wilcke W.,University of Bern
Plant and Soil | Year: 2014
Aims: In acid tropical forest soils (pH <5.5) increased mobility of aluminum might limit aboveground productivity. Therefore, we evaluated Al phytotoxicity of three native tree species of tropical montane forests in southern Ecuador. Methods: An hydroponic dose-response experiment was conducted. Seedlings of Cedrela odorata L., Heliocarpus americanus L., and Tabebuia chrysantha (Jacq.) G. Nicholson were treated with 0, 300, 600, 1200, and 2400 μ M Al and an organic layer leachate. Dose-response curves were generated for root and shoot morphologic properties to determine effective concentrations (EC). Results: Shoot biomass and healthy leaf area decreased by 44 % to 83 % at 2400 μ M Al, root biomass did not respond (C. odorata), declined by 51 % (H. americanus), or was stimulated at low Al concentrations of 300 μ M (T. chrysantha). EC10 (i.e. reduction by 10 %) values of Al for total biomass were 315 μ M (C. odorata), 219 μ M (H. americanus), and 368 μ M (T. chrysantha). Helicarpus americanus, a fast growing pioneer tree species, was most sensitive to Al toxicity. Negative effects were strongest if plants grew in organic layer leachate, indicating limitation of plant growth by nutrient scarcity rather than Al toxicity. Conclusions: Al toxicity occurred at Al concentrations far above those in native organic layer leachate. © 2014 Springer International Publishing Switzerland.
Wullaert H.,Johannes Gutenberg University Mainz |
Homeier J.,University of Gottingen |
Valarezo C.,National University of Loja |
Wilcke W.,University of Bern
Forest Ecology and Management | Year: 2010
Atmospheric nitrogen (N) and phosphorus (P) depositions are expected to increase in the tropics as a consequence of increasing human activities in the next decades. In the literature, it is frequently assumed that tropical montane forests are N-limited, while tropical lowland forests are P-limited. In a low-level N and P addition experiment, we determined the short-term response of N and P cycles in a north Andean montane forest on Palaeozoic shists and metasandstones at an elevation of 2100m a.s.l. to increased N and P inputs. We evaluated experimental N, P and N+P additions (50kgha-1yr-1 of N, 10kgha-1yr-1 of P and 50kg+10kgha-1yr-1 of N and P, respectively) and an untreated control in a fourfold replicated randomized block design. We collected litter leachate, mineral soil solution (0.15 and 0.30m depths), throughfall and litterfall before the treatment began (August 2007) until 16 months after the first nutrient application (April 2009). Less than 10 and 1% of the applied N and P, respectively, leached below the organic layer which contained almost all roots and no significant leaching losses of N and P occurred to below 0.15m mineral soil depth. Deposited N and P from the atmosphere in dry and wet form were retained in the canopy of the control treatment using a canopy budget model. Nitrogen and P retention by the canopy were reduced and N and P fluxes in throughfall and litterfall increased in their respective treatments. The increase in N and P fluxes in throughfall after fertilization was equivalent to 2.5% of the applied N and 2% of the applied P. The fluxes of N and P in litterfall were up to 15% and 3%, respectively, higher in the N and N+P than in the control treatments. We conclude that the expected elevated N and P deposition in the tropics will be retained in the ecosystem, at least in the short term and hence, N and P concentrations in stream water will not increase. Our results suggest that in the studied tropical montane forest ecosystem on Palaeozoic bedrock, N and P are co-limiting the growth of organisms in the canopy and organic layer. © 2010 Elsevier B.V.
Mazon M.,University of Los Andes, Venezuela |
Mazon M.,University of Alicante |
Mazon M.,National University of Loja
Biodiversity and Conservation | Year: 2016
When trying to assess entomological diversity, identifying taxa at levels higher than species is much easier and may provide a wider vision of other ecological features. In this work, we used the data from several samplings made in across six cacao farms in Mérida state (Venezuela). Farms fell into two categories according to intensity of perturbation. In these samplings we identified all parasitoid Hymenoptera families. All individuals belonging to families Ichneumonidae, Braconidae and Chalcididae were sorted to subfamilies and then to morphospecies. The accuracy of subfamilies richness to predict the species richness and to detect differences in the conservation status of plantations was tested. The species aggregation according to the sampling size was also explored. The three families this study was focused on represented 23 % of the total sampling, comprising 40 subfamilies and 393 morphospecies. Results showed a significant high positive correlation between subfamilies and species richness, and species/subfamilies ratio was about 4.5:1, with logarithmic relationship with sampling size tending to stabilisation at sizes greater than 15 individuals per sampling day. Subfamily richness detected the nearly-significant differences in plantations with the same accuracy as species richness, and therefore surrogacy effectiveness of parasitoid Hymenoptera subfamilies richness may be accepted for cacao plantations. © 2015, Springer Science+Business Media Dordrecht.
Volland F.,Friedrich - Alexander - University, Erlangen - Nuremberg |
Pucha D.,National University of Loja |
Brauning A.,Friedrich - Alexander - University, Erlangen - Nuremberg
Erdkunde | Year: 2016
Variations of stable oxygen isotopes in tree-ring cellulose are a widely used proxy to reconstruct hydro-climate variability in tropical and subtropical regions. We present the first δ18O chronology from annual tree rings in tropical Cedrela montana trees growing in the mountain rain forest of the Podocarpus National Park (PNP) in southern Ecuador. The more than a century long data record (1885-2011) comes from up to 15 individual trees (1980-2005) and represents the best- replicated isotope tree-ring chronology from the tropics. In comparison with tree-ring width, stable isotope variations show considerably higher correlations between individuals and thus represent a more reliable climate proxy in this very humid environment. High teleconnections to other stable isotope chronologies from the Amazon lowland indicate a high degree of consistency of regional hydro-climate variations. The PNP δ18O record is correlated with seasonal precipitation (January to April, CRU TS 3.21), frequency of wet days, and cloud cover over the Andean Cordillera Real. Spatial correlations indicate that the El Niño-Southern Oscillation (ENSO) has strong impact on tree-ring δ18O variations. Sea Surface Temperatures (SSTs) of the Niño 3.4 region and Niño 4 region, and the Oceanic Niño Index (ONI) show strong positive correlations with Cedrela oxygen isotope ratios, whereas the ENSO precipitation index correlates negatively. The Niño 3.4 and 4 SST influence is stronger after 1960 than before, indicating a shift in the influence of the Pacific Ocean on moisture variations in the Ecuadorian Andes. In the same period, the positive correlation with oxygen isotope signals from Andean glacier ice cores (r=0.2; p<0.05, 1894-1993) increased strongly (r=0.51; p<0.01, 1960-1993). In conclusion, stable oxygen isotope series from tropical tree species can help reconstruct variations in the hydroclimate of the Andean mountains and their surrounding areas. © 2016, Erdkunde. All rights reserved.
Volland-Voigt F.,Friedrich - Alexander - University, Erlangen - Nuremberg |
Brauning A.,Friedrich - Alexander - University, Erlangen - Nuremberg |
Ganzhi O.,National University of Loja |
Peters T.,Friedrich - Alexander - University, Erlangen - Nuremberg |
Maza H.,National University of Loja
Trees - Structure and Function | Year: 2011
Stem diameter increments of the broadleaved deciduous tree species Tabebuia chrysantha were measured with high-resolution dendrometers in a tropical lower montane forest and in a dry forest in southern Ecuador, the latter showing a distinct dry season. Those analyses were complemented by wood anatomical studies on regularly collected microcores to determine the season of active cambial growth and the time of formation of annual growth boundaries. The length of the cambial active period varied between 3 and 7 months at the tropical lower montane forest and 2 and 4 months in the dry forest, respectively. During dry days, amplitudes of daily stem diameter variations correlated with vapour pressure deficit. During October and November, inter-annual climate variations may lead to dry and sunny conditions in the tropical lower montane forest, causing water deficit and stem diameter shrinkage in T. chrysantha. The results of the climate-growth analysis show a positive relationship between tree growth and rainfall as well as vapour pressure deficit in certain periods of the year, indicating that rainfall plays a major role for tree growth. © 2010 Springer-Verlag.