Runoff response of a small agricultural basin in the argentine Pampas considering connectivity aspects

Our manuscript analyses the surface runoff variability, and its controlling factors in a small basin with gentle slopes, at the headwaters of a flat catchment, to improve the knowledge of the hydrology of plain areas under agriculture. We study runoff, rainfall and antecedent conditions in the argentine Pampas region. We use correlations, regressions and quantitative and qualitative descriptive information of the system: erosion signs, ground cover by crops, groundwater depth data and temporal changes in the drainage network, to discuss and understand the complexity of the runoff process by frameworks to study (dis)connectivity. The analysis of 56 events evidenced a nonlinear rainfall–runoff relationship. In contrast with other works, we identified clear upper limit events, under which hydrological responses emerge, as a result of combinations of antecedent wetness, rainfall erosivity, ground cover and referential drainage paths. We separated the nonlinear rainfall–runoff response in three linear relationships according to differences in antecedent wetness conditions. We found differences in runoff responses under wet and dry antecedent conditions, but complex responses under medium antecedent conditions. The analyses of the inputs, the structural and the functional elements of the (dis)connectivity frameworks, were key in the understanding of the temporal changes of runoff, and its complex responses. Temporal coincidences of connectivity components and their feedbacks appear to be strongly ssociated with the runoff dynamics. Highmagnitude hydrological responses occur with complete coincidences, while partial coincidences between the components reduce connectivity and low magnitude and/or heterogeneous responses prevail. Thus, these analyses suggest that runoff is controlled by (dis)connectivity in this basin with gentle slopes. Our work contributes to the understanding of the process of surface runoff in the context of humid flatlands under agricultural land use, by the identification of the complex combinations of factors which regulate/control the (dis)connectivity that helps to interpret the nonlinearities of runoff.

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Bibliographic Details
Main Authors: Ares, María Guadalupe, Varni, Marcelo, Chagas, Celio Ignacio
Format: Texto biblioteca
Language:eng
Subjects:AGRICULTURAL BASIN, ANTECEDENT WETNESS CONDITIONS, EROSION SIGNS, GENTLE HILLS AND SLOPES, HYDROLOGICAL (DIS)CONNECTIVITY, PAMPAS REGION, RAINFALL, RUNOFF RESPONSE, ,
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id KOHA-OAI-AGRO:54357
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 AGRICULTURAL BASIN
ANTECEDENT WETNESS CONDITIONS
EROSION SIGNS
GENTLE HILLS AND SLOPES
HYDROLOGICAL (DIS)CONNECTIVITY
PAMPAS REGION
RAINFALL
RUNOFF RESPONSE

AGRICULTURAL BASIN
ANTECEDENT WETNESS CONDITIONS
EROSION SIGNS
GENTLE HILLS AND SLOPES
HYDROLOGICAL (DIS)CONNECTIVITY
PAMPAS REGION
RAINFALL
RUNOFF RESPONSE
spellingShingle AGRICULTURAL BASIN
ANTECEDENT WETNESS CONDITIONS
EROSION SIGNS
GENTLE HILLS AND SLOPES
HYDROLOGICAL (DIS)CONNECTIVITY
PAMPAS REGION
RAINFALL
RUNOFF RESPONSE

AGRICULTURAL BASIN
ANTECEDENT WETNESS CONDITIONS
EROSION SIGNS
GENTLE HILLS AND SLOPES
HYDROLOGICAL (DIS)CONNECTIVITY
PAMPAS REGION
RAINFALL
RUNOFF RESPONSE
Ares, María Guadalupe
Varni, Marcelo
Chagas, Celio Ignacio
Runoff response of a small agricultural basin in the argentine Pampas considering connectivity aspects
description Our manuscript analyses the surface runoff variability, and its controlling factors in a small basin with gentle slopes, at the headwaters of a flat catchment, to improve the knowledge of the hydrology of plain areas under agriculture. We study runoff, rainfall and antecedent conditions in the argentine Pampas region. We use correlations, regressions and quantitative and qualitative descriptive information of the system: erosion signs, ground cover by crops, groundwater depth data and temporal changes in the drainage network, to discuss and understand the complexity of the runoff process by frameworks to study (dis)connectivity. The analysis of 56 events evidenced a nonlinear rainfall–runoff relationship. In contrast with other works, we identified clear upper limit events, under which hydrological responses emerge, as a result of combinations of antecedent wetness, rainfall erosivity, ground cover and referential drainage paths. We separated the nonlinear rainfall–runoff response in three linear relationships according to differences in antecedent wetness conditions. We found differences in runoff responses under wet and dry antecedent conditions, but complex responses under medium antecedent conditions. The analyses of the inputs, the structural and the functional elements of the (dis)connectivity frameworks, were key in the understanding of the temporal changes of runoff, and its complex responses. Temporal coincidences of connectivity components and their feedbacks appear to be strongly ssociated with the runoff dynamics. Highmagnitude hydrological responses occur with complete coincidences, while partial coincidences between the components reduce connectivity and low magnitude and/or heterogeneous responses prevail. Thus, these analyses suggest that runoff is controlled by (dis)connectivity in this basin with gentle slopes. Our work contributes to the understanding of the process of surface runoff in the context of humid flatlands under agricultural land use, by the identification of the complex combinations of factors which regulate/control the (dis)connectivity that helps to interpret the nonlinearities of runoff.
format Texto
topic_facet
AGRICULTURAL BASIN
ANTECEDENT WETNESS CONDITIONS
EROSION SIGNS
GENTLE HILLS AND SLOPES
HYDROLOGICAL (DIS)CONNECTIVITY
PAMPAS REGION
RAINFALL
RUNOFF RESPONSE
author Ares, María Guadalupe
Varni, Marcelo
Chagas, Celio Ignacio
author_facet Ares, María Guadalupe
Varni, Marcelo
Chagas, Celio Ignacio
author_sort Ares, María Guadalupe
title Runoff response of a small agricultural basin in the argentine Pampas considering connectivity aspects
title_short Runoff response of a small agricultural basin in the argentine Pampas considering connectivity aspects
title_full Runoff response of a small agricultural basin in the argentine Pampas considering connectivity aspects
title_fullStr Runoff response of a small agricultural basin in the argentine Pampas considering connectivity aspects
title_full_unstemmed Runoff response of a small agricultural basin in the argentine Pampas considering connectivity aspects
title_sort runoff response of a small agricultural basin in the argentine pampas considering connectivity aspects
url http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=54357
http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=
http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=
http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=
http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=
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AT varnimarcelo runoffresponseofasmallagriculturalbasinintheargentinepampasconsideringconnectivityaspects
AT chagascelioignacio runoffresponseofasmallagriculturalbasinintheargentinepampasconsideringconnectivityaspects
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spelling KOHA-OAI-AGRO:543572021-12-28T10:20:07Zhttp://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=54357http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=AAGRunoff response of a small agricultural basin in the argentine Pampas considering connectivity aspectsAres, María GuadalupeVarni, MarceloChagas, Celio Ignaciotextengapplication/pdfOur manuscript analyses the surface runoff variability, and its controlling factors in a small basin with gentle slopes, at the headwaters of a flat catchment, to improve the knowledge of the hydrology of plain areas under agriculture. We study runoff, rainfall and antecedent conditions in the argentine Pampas region. We use correlations, regressions and quantitative and qualitative descriptive information of the system: erosion signs, ground cover by crops, groundwater depth data and temporal changes in the drainage network, to discuss and understand the complexity of the runoff process by frameworks to study (dis)connectivity. The analysis of 56 events evidenced a nonlinear rainfall–runoff relationship. In contrast with other works, we identified clear upper limit events, under which hydrological responses emerge, as a result of combinations of antecedent wetness, rainfall erosivity, ground cover and referential drainage paths. We separated the nonlinear rainfall–runoff response in three linear relationships according to differences in antecedent wetness conditions. We found differences in runoff responses under wet and dry antecedent conditions, but complex responses under medium antecedent conditions. The analyses of the inputs, the structural and the functional elements of the (dis)connectivity frameworks, were key in the understanding of the temporal changes of runoff, and its complex responses. Temporal coincidences of connectivity components and their feedbacks appear to be strongly ssociated with the runoff dynamics. Highmagnitude hydrological responses occur with complete coincidences, while partial coincidences between the components reduce connectivity and low magnitude and/or heterogeneous responses prevail. Thus, these analyses suggest that runoff is controlled by (dis)connectivity in this basin with gentle slopes. Our work contributes to the understanding of the process of surface runoff in the context of humid flatlands under agricultural land use, by the identification of the complex combinations of factors which regulate/control the (dis)connectivity that helps to interpret the nonlinearities of runoff.Our manuscript analyses the surface runoff variability, and its controlling factors in a small basin with gentle slopes, at the headwaters of a flat catchment, to improve the knowledge of the hydrology of plain areas under agriculture. We study runoff, rainfall and antecedent conditions in the argentine Pampas region. We use correlations, regressions and quantitative and qualitative descriptive information of the system: erosion signs, ground cover by crops, groundwater depth data and temporal changes in the drainage network, to discuss and understand the complexity of the runoff process by frameworks to study (dis)connectivity. The analysis of 56 events evidenced a nonlinear rainfall–runoff relationship. In contrast with other works, we identified clear upper limit events, under which hydrological responses emerge, as a result of combinations of antecedent wetness, rainfall erosivity, ground cover and referential drainage paths. We separated the nonlinear rainfall–runoff response in three linear relationships according to differences in antecedent wetness conditions. We found differences in runoff responses under wet and dry antecedent conditions, but complex responses under medium antecedent conditions. The analyses of the inputs, the structural and the functional elements of the (dis)connectivity frameworks, were key in the understanding of the temporal changes of runoff, and its complex responses. Temporal coincidences of connectivity components and their feedbacks appear to be strongly ssociated with the runoff dynamics. Highmagnitude hydrological responses occur with complete coincidences, while partial coincidences between the components reduce connectivity and low magnitude and/or heterogeneous responses prevail. Thus, these analyses suggest that runoff is controlled by (dis)connectivity in this basin with gentle slopes. Our work contributes to the understanding of the process of surface runoff in the context of humid flatlands under agricultural land use, by the identification of the complex combinations of factors which regulate/control the (dis)connectivity that helps to interpret the nonlinearities of runoff.AGRICULTURAL BASINANTECEDENT WETNESS CONDITIONSEROSION SIGNSGENTLE HILLS AND SLOPESHYDROLOGICAL (DIS)CONNECTIVITYPAMPAS REGIONRAINFALLRUNOFF RESPONSEHydrological Processes