Runoff estimation in small rural watersheds using DEMS in North West of Argentina

Basic information from analytical-descriptive methodologies on the relief of watersheds provides the necessary physical parameters for studying natural resources for, e.g., integrated management of watersheds, environmental impact, soil degradation, deforestation, conservation of water resources, and so forth. Geographic information systems can be used for all of these processes, which are linked to a strong spatial component. Digital elevation models [DEM] and their derivatives are a relevant component of these data sources. The parameters found from these models, such as the slope, are used directly or indirectly [as a component of these factors] in many surface runoff estimation equations. In Latin America, the Rational Method has been and continues to be one of the most widely used for the study of microdrainage in small watersheds. The experiment was conducted in the Yatasto district of the Province of Salta, North West Argentina and has an approximate surface of 270 hectares. This zone is located on the piedmont plain of the Metán sierra, where crops are grown, with relatively high slopes and high potential of soil erosion. In this area were studied five small rural watersheds all of them within the total DEM study area and none of them over 81 hectares. This work studied whether potential surface runoff found from the Rational Method [RAMSER] in small rural watersheds shows significant differences depending on whether the mean slopes are found from the DEM derived model or by the usual field methodology. We found that the small-sized grids increase the average slope [between 045 percent and 0.79 percent] found over those found from field data. The differences observed in volume of the peak runoff [between 0.003m3s-1 and 0.062m3s-1] were not significant. The results assure that there are no differences in the parameter evaluated [average slope] under the studied methodology and conditions.

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Bibliographic Details
Main Authors: Rosatto, Héctor Gustavo, Tolón Becerra, Alfredo, Botta, Guido Fernando, Presutti, Miriam Elisabeth
Format: Texto biblioteca
Language:eng
Subjects:AVERAGE SLOPE, BASIS, LEVEL, TOPOGRAPHIC PARAMETERS, DATA SOURCE, DIGITAL ELEVATION MODEL, FIELD DATA, HIGH POTENTIAL, HIGH SLOPES, INTEGRATED MANAGEMENT, LATIN AMERICA, PHYSICAL PARAMETERS, POTENTIAL SURFACES, RATIONAL METHODS, RELEVANT COMPONENTS, RUNOFF ESTIMATION, RURAL WATERSHEDS, SMALL WATERSHEDS, SOIL DEGRADATION, SOIL EROSION, STUDY AREAS, SURFACE RUNOFFS, DEFORESTATION, ENVIRONMENTAL IMPACT, GEOGRAPHIC INFORMATION SYSTEMS, NATURAL RESOURCES MANAGEMENT, RUNOFF, SOIL CONSERVATION, SOILS, SURVEYING, WATER CONSERVATION, WATER RESOURCES, WATERSHEDS, LANDFORMS, DRAINAGE, EXPERIMENTAL STUDY, GIS, PHYSICAL PROPERTY, PIEDMONT, RURAL AREA, TOPOGRAPHY, ARGENTINA,
Online Access:http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=46679
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id KOHA-OAI-AGRO:46679
record_format koha
institution UBA FA
collection Koha
country Argentina
countrycode AR
component Bibliográfico
access En linea
En linea
databasecode cat-ceiba
tag biblioteca
region America del Sur
libraryname Biblioteca Central FAUBA
language eng
topic AVERAGE SLOPE
BASIS
LEVEL
TOPOGRAPHIC PARAMETERS
DATA SOURCE
DIGITAL ELEVATION MODEL
FIELD DATA
HIGH POTENTIAL
HIGH SLOPES
INTEGRATED MANAGEMENT
LATIN AMERICA
PHYSICAL PARAMETERS
POTENTIAL SURFACES
RATIONAL METHODS
RELEVANT COMPONENTS
RUNOFF ESTIMATION
RURAL WATERSHEDS
SMALL WATERSHEDS
SOIL DEGRADATION
SOIL EROSION
STUDY AREAS
SURFACE RUNOFFS
TOPOGRAPHIC PARAMETERS
DEFORESTATION
ENVIRONMENTAL IMPACT
GEOGRAPHIC INFORMATION SYSTEMS
NATURAL RESOURCES MANAGEMENT
RUNOFF
SOIL CONSERVATION
SOILS
SURVEYING
WATER CONSERVATION
WATER RESOURCES
WATERSHEDS
LANDFORMS
DRAINAGE
EXPERIMENTAL STUDY
GIS
PHYSICAL PROPERTY
PIEDMONT
RURAL AREA
SOIL EROSION
TOPOGRAPHY
ARGENTINA
AVERAGE SLOPE
BASIS
LEVEL
TOPOGRAPHIC PARAMETERS
DATA SOURCE
DIGITAL ELEVATION MODEL
FIELD DATA
HIGH POTENTIAL
HIGH SLOPES
INTEGRATED MANAGEMENT
LATIN AMERICA
PHYSICAL PARAMETERS
POTENTIAL SURFACES
RATIONAL METHODS
RELEVANT COMPONENTS
RUNOFF ESTIMATION
RURAL WATERSHEDS
SMALL WATERSHEDS
SOIL DEGRADATION
SOIL EROSION
STUDY AREAS
SURFACE RUNOFFS
TOPOGRAPHIC PARAMETERS
DEFORESTATION
ENVIRONMENTAL IMPACT
GEOGRAPHIC INFORMATION SYSTEMS
NATURAL RESOURCES MANAGEMENT
RUNOFF
SOIL CONSERVATION
SOILS
SURVEYING
WATER CONSERVATION
WATER RESOURCES
WATERSHEDS
LANDFORMS
DRAINAGE
EXPERIMENTAL STUDY
GIS
PHYSICAL PROPERTY
PIEDMONT
RURAL AREA
SOIL EROSION
TOPOGRAPHY
ARGENTINA
spellingShingle AVERAGE SLOPE
BASIS
LEVEL
TOPOGRAPHIC PARAMETERS
DATA SOURCE
DIGITAL ELEVATION MODEL
FIELD DATA
HIGH POTENTIAL
HIGH SLOPES
INTEGRATED MANAGEMENT
LATIN AMERICA
PHYSICAL PARAMETERS
POTENTIAL SURFACES
RATIONAL METHODS
RELEVANT COMPONENTS
RUNOFF ESTIMATION
RURAL WATERSHEDS
SMALL WATERSHEDS
SOIL DEGRADATION
SOIL EROSION
STUDY AREAS
SURFACE RUNOFFS
TOPOGRAPHIC PARAMETERS
DEFORESTATION
ENVIRONMENTAL IMPACT
GEOGRAPHIC INFORMATION SYSTEMS
NATURAL RESOURCES MANAGEMENT
RUNOFF
SOIL CONSERVATION
SOILS
SURVEYING
WATER CONSERVATION
WATER RESOURCES
WATERSHEDS
LANDFORMS
DRAINAGE
EXPERIMENTAL STUDY
GIS
PHYSICAL PROPERTY
PIEDMONT
RURAL AREA
SOIL EROSION
TOPOGRAPHY
ARGENTINA
AVERAGE SLOPE
BASIS
LEVEL
TOPOGRAPHIC PARAMETERS
DATA SOURCE
DIGITAL ELEVATION MODEL
FIELD DATA
HIGH POTENTIAL
HIGH SLOPES
INTEGRATED MANAGEMENT
LATIN AMERICA
PHYSICAL PARAMETERS
POTENTIAL SURFACES
RATIONAL METHODS
RELEVANT COMPONENTS
RUNOFF ESTIMATION
RURAL WATERSHEDS
SMALL WATERSHEDS
SOIL DEGRADATION
SOIL EROSION
STUDY AREAS
SURFACE RUNOFFS
TOPOGRAPHIC PARAMETERS
DEFORESTATION
ENVIRONMENTAL IMPACT
GEOGRAPHIC INFORMATION SYSTEMS
NATURAL RESOURCES MANAGEMENT
RUNOFF
SOIL CONSERVATION
SOILS
SURVEYING
WATER CONSERVATION
WATER RESOURCES
WATERSHEDS
LANDFORMS
DRAINAGE
EXPERIMENTAL STUDY
GIS
PHYSICAL PROPERTY
PIEDMONT
RURAL AREA
SOIL EROSION
TOPOGRAPHY
ARGENTINA
Rosatto, Héctor Gustavo
Tolón Becerra, Alfredo
Botta, Guido Fernando
Presutti, Miriam Elisabeth
Runoff estimation in small rural watersheds using DEMS in North West of Argentina
description Basic information from analytical-descriptive methodologies on the relief of watersheds provides the necessary physical parameters for studying natural resources for, e.g., integrated management of watersheds, environmental impact, soil degradation, deforestation, conservation of water resources, and so forth. Geographic information systems can be used for all of these processes, which are linked to a strong spatial component. Digital elevation models [DEM] and their derivatives are a relevant component of these data sources. The parameters found from these models, such as the slope, are used directly or indirectly [as a component of these factors] in many surface runoff estimation equations. In Latin America, the Rational Method has been and continues to be one of the most widely used for the study of microdrainage in small watersheds. The experiment was conducted in the Yatasto district of the Province of Salta, North West Argentina and has an approximate surface of 270 hectares. This zone is located on the piedmont plain of the Metán sierra, where crops are grown, with relatively high slopes and high potential of soil erosion. In this area were studied five small rural watersheds all of them within the total DEM study area and none of them over 81 hectares. This work studied whether potential surface runoff found from the Rational Method [RAMSER] in small rural watersheds shows significant differences depending on whether the mean slopes are found from the DEM derived model or by the usual field methodology. We found that the small-sized grids increase the average slope [between 045 percent and 0.79 percent] found over those found from field data. The differences observed in volume of the peak runoff [between 0.003m3s-1 and 0.062m3s-1] were not significant. The results assure that there are no differences in the parameter evaluated [average slope] under the studied methodology and conditions.
format Texto
topic_facet AVERAGE SLOPE
BASIS
LEVEL
TOPOGRAPHIC PARAMETERS
DATA SOURCE
DIGITAL ELEVATION MODEL
FIELD DATA
HIGH POTENTIAL
HIGH SLOPES
INTEGRATED MANAGEMENT
LATIN AMERICA
PHYSICAL PARAMETERS
POTENTIAL SURFACES
RATIONAL METHODS
RELEVANT COMPONENTS
RUNOFF ESTIMATION
RURAL WATERSHEDS
SMALL WATERSHEDS
SOIL DEGRADATION
SOIL EROSION
STUDY AREAS
SURFACE RUNOFFS
TOPOGRAPHIC PARAMETERS
DEFORESTATION
ENVIRONMENTAL IMPACT
GEOGRAPHIC INFORMATION SYSTEMS
NATURAL RESOURCES MANAGEMENT
RUNOFF
SOIL CONSERVATION
SOILS
SURVEYING
WATER CONSERVATION
WATER RESOURCES
WATERSHEDS
LANDFORMS
DRAINAGE
EXPERIMENTAL STUDY
GIS
PHYSICAL PROPERTY
PIEDMONT
RURAL AREA
SOIL EROSION
TOPOGRAPHY
ARGENTINA
author Rosatto, Héctor Gustavo
Tolón Becerra, Alfredo
Botta, Guido Fernando
Presutti, Miriam Elisabeth
author_facet Rosatto, Héctor Gustavo
Tolón Becerra, Alfredo
Botta, Guido Fernando
Presutti, Miriam Elisabeth
author_sort Rosatto, Héctor Gustavo
title Runoff estimation in small rural watersheds using DEMS in North West of Argentina
title_short Runoff estimation in small rural watersheds using DEMS in North West of Argentina
title_full Runoff estimation in small rural watersheds using DEMS in North West of Argentina
title_fullStr Runoff estimation in small rural watersheds using DEMS in North West of Argentina
title_full_unstemmed Runoff estimation in small rural watersheds using DEMS in North West of Argentina
title_sort runoff estimation in small rural watersheds using dems in north west of argentina
url http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=46679
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AT tolonbecerraalfredo runoffestimationinsmallruralwatershedsusingdemsinnorthwestofargentina
AT bottaguidofernando runoffestimationinsmallruralwatershedsusingdemsinnorthwestofargentina
AT presuttimiriamelisabeth runoffestimationinsmallruralwatershedsusingdemsinnorthwestofargentina
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spelling KOHA-OAI-AGRO:466792022-02-18T16:06:12Zhttp://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=46679AAGRunoff estimation in small rural watersheds using DEMS in North West of ArgentinaRosatto, Héctor GustavoTolón Becerra, AlfredoBotta, Guido FernandoPresutti, Miriam Elisabethtextengapplication/pdfBasic information from analytical-descriptive methodologies on the relief of watersheds provides the necessary physical parameters for studying natural resources for, e.g., integrated management of watersheds, environmental impact, soil degradation, deforestation, conservation of water resources, and so forth. Geographic information systems can be used for all of these processes, which are linked to a strong spatial component. Digital elevation models [DEM] and their derivatives are a relevant component of these data sources. The parameters found from these models, such as the slope, are used directly or indirectly [as a component of these factors] in many surface runoff estimation equations. In Latin America, the Rational Method has been and continues to be one of the most widely used for the study of microdrainage in small watersheds. The experiment was conducted in the Yatasto district of the Province of Salta, North West Argentina and has an approximate surface of 270 hectares. This zone is located on the piedmont plain of the Metán sierra, where crops are grown, with relatively high slopes and high potential of soil erosion. In this area were studied five small rural watersheds all of them within the total DEM study area and none of them over 81 hectares. This work studied whether potential surface runoff found from the Rational Method [RAMSER] in small rural watersheds shows significant differences depending on whether the mean slopes are found from the DEM derived model or by the usual field methodology. We found that the small-sized grids increase the average slope [between 045 percent and 0.79 percent] found over those found from field data. The differences observed in volume of the peak runoff [between 0.003m3s-1 and 0.062m3s-1] were not significant. The results assure that there are no differences in the parameter evaluated [average slope] under the studied methodology and conditions.Basic information from analytical-descriptive methodologies on the relief of watersheds provides the necessary physical parameters for studying natural resources for, e.g., integrated management of watersheds, environmental impact, soil degradation, deforestation, conservation of water resources, and so forth. Geographic information systems can be used for all of these processes, which are linked to a strong spatial component. Digital elevation models [DEM] and their derivatives are a relevant component of these data sources. The parameters found from these models, such as the slope, are used directly or indirectly [as a component of these factors] in many surface runoff estimation equations. In Latin America, the Rational Method has been and continues to be one of the most widely used for the study of microdrainage in small watersheds. The experiment was conducted in the Yatasto district of the Province of Salta, North West Argentina and has an approximate surface of 270 hectares. This zone is located on the piedmont plain of the Metán sierra, where crops are grown, with relatively high slopes and high potential of soil erosion. In this area were studied five small rural watersheds all of them within the total DEM study area and none of them over 81 hectares. This work studied whether potential surface runoff found from the Rational Method [RAMSER] in small rural watersheds shows significant differences depending on whether the mean slopes are found from the DEM derived model or by the usual field methodology. We found that the small-sized grids increase the average slope [between 045 percent and 0.79 percent] found over those found from field data. The differences observed in volume of the peak runoff [between 0.003m3s-1 and 0.062m3s-1] were not significant. The results assure that there are no differences in the parameter evaluated [average slope] under the studied methodology and conditions.AVERAGE SLOPEBASISLEVELTOPOGRAPHIC PARAMETERSDATA SOURCEDIGITAL ELEVATION MODELFIELD DATAHIGH POTENTIALHIGH SLOPESINTEGRATED MANAGEMENTLATIN AMERICAPHYSICAL PARAMETERSPOTENTIAL SURFACESRATIONAL METHODSRELEVANT COMPONENTSRUNOFF ESTIMATIONRURAL WATERSHEDSSMALL WATERSHEDSSOIL DEGRADATIONSOIL EROSIONSTUDY AREASSURFACE RUNOFFSTOPOGRAPHIC PARAMETERSDEFORESTATIONENVIRONMENTAL IMPACTGEOGRAPHIC INFORMATION SYSTEMSNATURAL RESOURCES MANAGEMENTRUNOFFSOIL CONSERVATIONSOILSSURVEYINGWATER CONSERVATIONWATER RESOURCESWATERSHEDSLANDFORMSDRAINAGEEXPERIMENTAL STUDYGISPHYSICAL PROPERTYPIEDMONTRURAL AREASOIL EROSIONTOPOGRAPHYARGENTINASoil and Tillage Research