Keywords
micro-watershed
morphometric parameters
lama-bordo system
sediment transport
How to Cite
##article.highlights##
- Morphometric and hydrological parameters were determined in 27 sites with a lama-bordo system (LBS).
- The LBS studied correspond to micro-watersheds with area < 2 km 2 , altitude > 2 000 m, and slope > 10 %.
- The prediction model of soil volume captured by the LBS was obtained with multiple linear regression.
- Two morphological and two hydrological parameters explained 85 % of the cumulative sediment volume.
##article.graphical##
Abstract
Introduction: The lama-bordo systems (LBS) are built in natural watercourses and favor retention of sediment and runoff moisture for the development of agricultural activity.
Objective: To obtain a model for predicting the volume of soil permanently captured by LBS, based on the morphometric and hydrological characteristics of the micro-watersheds where they have prevailed in the Mixteca Alta of Oaxaca, Mexico
Materials and methods: The study was carried out in 27 sites where morphometric parameters and hydrological indexes were determined to obtain the volume prediction model by multiple linear regression (backward elimination technique).
Results and discussion: The systems studied were found in micro-watersheds under conditions that favor sediment transport: elongated shape, areas smaller than 2 km2 with 1st and 2nd order streams, at altitudes above 2 000 m and slopes greater than 10 %. Twelve morphometric parameters and three hydrological indexes characterize these micro-watersheds and explain the physical conditions that allow their establishment, but only four (micro-watershed area, average slope of the mainstream, topographic wetness index and sediment transport index) explain the cumulative sediment volume (R2 = 0.85, P < 0.001).
Conclusions: The model evaluated for volume estimation is reliable for application at sites under similar conditions.
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