Modelación de caudales en función de los macroporos del suelo en una microcuenca forestal de Durango, México

Návar, José; Lizárraga-Mendiola, Liliana; Gómez, Marco Aurelio Jiménez

doi:10.28940/terra.v35i2.265

Cited by 3 publications

(2 citation statements)

References 19 publications

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“…Many studies on infiltration have focused on the application of models for comparison or validation using data obtained through laboratory or field infiltrometry tests, including comparisons between different land uses (Mbagwu, 1995;Mishar et al, 2003;Shukla et al, 2003;Ghorbani Dashtaki et al, 2009;Haghighi et al, 2010;Duan et al, 2011;Robertson and Sharp, 2015). Despite the large number of studies on the effect of land use changes on infiltration rates (Malmer and Grip, 1990;Ghuman et al, 1991;Alegre and Cassel, 1996;Lal, 1996;Navar and Synnott, 2000;Martínez and Zinck, 2004;Ziegler et al, 2004;Zimmermann et al, 2006), additional information from studies comparing contrasting areas is still needed. In this study, we analysed a large data set of infiltration rates measured under several land use and vegetation cover situations in three study areas in northern Spain, in order to determine their effect on infiltration variability.…”

Section: Introductionmentioning

confidence: 99%

Analysing the effect of land use and vegetation cover on soil infiltration in three contrasting environments in northeast Spain

Regüés

Badía

Echeverría³

et al. 2017

CIG

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ABSTRACT. This study presents a joint analysis of the information from 195 field infiltration experiments, using double ring devices. The experiments were carried out in 20 contrasting types of land use, distributed across three geographic contexts (coast of NE Catalonia, an area of gentle relief in the centralPalabras clave: infiltración, ensayos con doble anillo, usos del suelo, cubierta vegetal, humedad del suelo, nordeste de España.

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Section: Introductionmentioning

confidence: 99%

Analysing the effect of land use and vegetation cover on soil infiltration in three contrasting environments in northeast Spain

Regüés

Badía

Echeverría³

et al. 2017

CIG

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“…The mean annual precipitation is about 805 mm. The type of soil under study is Vertisol with smectite and present structure of the prismatic type (Návar & Synnott, 2000), which has a deep grey colour, a clayey-silty texture, with high montmorillonite content, that contracts and expands significantly in response to changes in soil moisture (González et al, 2011).…”

Section: Description Of the Study Sitementioning

confidence: 99%

Effects of land use change and seasonal variation in the hydrophysical properties in Vertisols in northeastern Mexico

Yáñez-Díaz

Silva

González‐Rodríguez

et al. 2019

Soil Use and Management

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The impact of the use of natural resources associated with anthropogenic activities has increased evidently, mainly through land use changes which have altered hydrophysical properties of soils. We hypothesized that, in the same soil type (Vertisol), four types of land use system (grassland, agricultural, Eucalyptus plantation and thornscrub) and seasonal variation can modify the soil hydrophysical properties. Results showed significant differences between land use systems and seasons for hydraulic conductivity (K), infiltration capacity (fp) and cumulative infiltration (fc). There were no seasonal differences in soil penetration resistance (SPR), bulk density (ρd) and total porosity (φP). Grassland presented higher values for ρd (1.2 g cm−3) and SPR (5.3 kg cm−2) and lower for K (0.8 × 10−5 cm s−1) and φP (53%), unlike thornscrub. Agriculture presented lower SPR (0.4 kg cm−2), while plantation showed similar values when compared to the thornscrub. Kostiakov infiltration model was fitted to land use infiltration curves, showing differences between land use and season. The values for fp oscillated between 53.6 and 548.8 mm hr−1 and fc ranged from 105.3 to 1,061 mm. The order of the infiltration values goes as follows: agriculture > plantation > thornscrub > grassland. Land use changes in Vertisols induced modification of soil physical properties affecting processes like permeability, soil compaction and water availability.

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Análisis morfométrico de la cuenca El Salto, Durango, México

Méndez-Gutiérrez

Corral-Rivas

Luna

et al. 2021

Terra

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El manejo integral de las cuencas hidrográficas requiere una caracterización adecuada para identificar su problemática ambiental y consecuentemente establecer los lineamientos de solución pertinentes. El presente estudio describe detalladamente las características morfométricas e hipsométricas de la cuenca El Salto, Durango. A través de un Sistema de Información Geográfica y robustecido con datos de campo, se analizaron parámetros de forma, relieve y red hidrográfica; además, se realizó la curva hipsométrica y se calculó la integral hipsométrica para determinar la fase evolutiva de la cuenca. Los resultados sugieren que la cuenca es alargada, además el relieve evidencia un desnivel bajo (303 m) con una pendiente media de 2.23% considerada como moderadamente inclinada. La red de drenaje es considerada de cuarto orden, y está formada por 94 cauces cuya longitud total es 90.53 km. La densidad e intensidad de drenaje presentaron valores de 2.02 km/km2 y 1.04 km respectivamente, con una frecuencia de corrientes de 2.09 cauces/km2; éstos valores se consideran bajos para cuencas con estas dimensiones. De acuerdo al valor de la integral hipsométrica (0.5), la cuenca se encuentra en la fase de equilibrio o madurez. El orden de corrientes que predomina es 1, por lo que la cuenca es más susceptible a presentar erosión hídrica durante los eventos de lluvia. Por otro lado, debido a la forma alargada de la cuenca esta debería ser menos susceptible a presentar inundaciones; sin embargo, se observaron valores bajos de densidad e intensidad de drenaje y frecuencia de corrientes, lo cual sugiere que el escurrimiento no es eficiente. Este estudio será útil para el desarrollo de proyectos de manejo y conservación de los recursos naturales, en especial para aquellos cuyo objetivo sea reducir la pérdida de suelo por erosión y realizar acciones de captación de agua.

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Modelación de caudales en función de los macroporos del suelo en una microcuenca forestal de Durango, México

Abstract: Modelación de caudales en función de los macroporos del suelo en una microcuenca forestal de Durango, MéxicoModeling runoff components as a function of soil macropores in a forest watershed of Durango, Mexico

Cited by 3 publications

References 19 publications

Analysing the effect of land use and vegetation cover on soil infiltration in three contrasting environments in northeast Spain

Analysing the effect of land use and vegetation cover on soil infiltration in three contrasting environments in northeast Spain

Effects of land use change and seasonal variation in the hydrophysical properties in Vertisols in northeastern Mexico

Análisis morfométrico de la cuenca El Salto, Durango, México

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