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Please use this identifier to cite or link to this item: http://dspace.ucuenca.edu.ec/handle/123456789/22092
Title: Land use change impacts on the hydrology of wet Andean páramo ecosystems
Authors: Crespo Sanchez, Patricio Xavier
Borja Ramón, Pablo Marcelo
Celleri Alvear, Rolando Enrique
Feyen, Jean
Buytaert, Wouter
De Bievre, Bert
Iñiguez Moran, Vicente Mauricio
metadata.dc.ucuenca.correspondencia: Crespo Sanchez, Patricio Xavier, patricio.crespo@ucuenca.edu.ec
Keywords: Land use
Hydrology
Paramo
metadata.dc.ucuenca.areaconocimientofrascatiamplio: 1. Ciencias Naturales y Exactas
metadata.dc.ucuenca.areaconocimientofrascatidetallado: 1.5.10 Recursos Hídricos
metadata.dc.ucuenca.areaconocimientofrascatiespecifico: 1.5 Ciencias de la Tierra y el Ambiente
metadata.dc.ucuenca.areaconocimientounescoamplio: 05 - Ciencias Físicas, Ciencias Naturales, Matemáticas y Estadísticas
metadata.dc.ucuenca.areaconocimientounescodetallado: 0521 - Ciencias Ambientales
metadata.dc.ucuenca.areaconocimientounescoespecifico: 052 - Medio Ambiente
Issue Date: 2009
metadata.dc.ucuenca.volumen: Volúmen 336
metadata.dc.source: IAHS-AISH Publication
Publisher: International Association of Hydrological Sciences
metadata.dc.description.city: 
Koblenz
metadata.dc.type: ARTÍCULO DE CONFERENCIA
Abstract: 
This paper presents the research performed in the wet Andean páramo ecosystem in order to study the land use change impacts on its hydrology, using small paired catchments. The research results revealed that pine plantations produce a decrease of annual water yield as a consequence of increased evapotranspiration. On the other hand, livestock grazing does not seem to affect the hydrological response, primarily due to the low animal density. The main impact of cultivation is the reduction in the regulating function of the catchment, with a large increase in the magnitude of peak flows and a reduction of base flows. Furthermore, research results revealed that vertical infiltration through the soil is dominant under wet conditions, whereas preferential flow within the organic horizon to the underlying mineral horizon is dominant during low intensity rains. Saturated excess surface flow is observed only during long rain events; otherwise near surface lateral flow in the organic layer occurs. There is no evidence of Hortonian flow
URI: https://www.scopus.com/record/display.uri?eid=2-s2.0-79551505851&origin=resultslist&sort=plf-f&src=s&sid=2bff71f65af8351641b6cdf0bbff15c7&sot=b&sdt=b&s=TITLE-ABS-KEY%28Land+use+change+impacts+on+the+hydrology+of+wet+Andean+p%C3%A1ramo+ecosystems%29&sl=87&sessionSearchId=2bff71f65af8351641b6cdf0bbff15c7
metadata.dc.ucuenca.urifuente: https://iahs.info/Publications-News.do
ISBN: 978-190716108-7
ISSN: 01447815
Appears in Collections:Artículos

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