Please use this identifier to cite or link to this item: http://dspace.ucuenca.edu.ec/handle/123456789/22137
Title: The use of the linear reservoir concept to quantify the impact of changes in land use on the hydrology of catchments in the Andes
Other Titles: Hydrology and Earth System Sciences
Authors: Buytaert, Wouter
Wyseure, Guido
Deckers, Jozef
De Bièvre, Bert
Keywords: LINEAR RESERVOIR
ECUADOR
PARAMO
MOUNTAIN HYDROLOGY
LAND USE CHANGES
Issue Date: 2004
metadata.dc.ucuenca.paginacion: pp. 108-114
metadata.dc.type: Article
Abstract: 
The high Andes region of South Ecuador (The Paramo) is characterized by a cold and wet climate. Most soils of the Páramo region are Andosols and Histosols, with a very high water retention capacity that is affected irreversibly by drying. This key property of Páramo soils buffers catchment outflow, resulting in an almost uniform outflow pattern which, notwithsyanding the variability in rainfall, can be very variable in space and time. These soils serve as the most important reservoir of drinking and irrigation water for the densely populated inter-Andean depression region. The Páramo has long served only as an extensive grazing area but recent population pressure and land scarcity have increased cultivation. Two small Páramo catchments (about 2 km2) were monitored intensively for precipitation and discharge for over a year to assess the effect of such land-use changes on the hydrological properties. One catchment is in an undisturbed area and grazed intensively while in the other, local farmers started intensive drainage for cultivation of potatoes about five years ago. The linear reservoir concept has been used to assess the overall retention capacity of the catchment in terms of both peak response and base flow. In this model, every catchment is considered as a series if independent parallel reservoirs, each characterized by mean residence times (T). In every catchment, three major mean residence time can be distinguished. In the undisturbed catchment, an immediate response. characterized by a T of 5.4 hours, is followed by a slower response with a T of 44.3h. The base flow has mean T value of 360 h. The response of the cultivated catchment is similar with T values of 3.6 h., 27.2 h and 175 h, respectively. As a result, in the disturbed catchment, water release is about 40% faster than in the undisturbed catchment, so that the base flow falls rapidly to lower levels. The linear reservoir model is a simple way of quantifying the impact of land use changes on the water regulation capacity of Páramo catchments.
URI: http://dspace.ucuenca.edu.ec/handle/123456789/22137
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