Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events

Operative distributed/semi-distributed rainfall-runoff formulations need a mathematically tractable component for estimating the expected areal-average infiltration rate, I...
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Gespeichert in:

Autor*in:	Flammini, Alessia [verfasserIn] Morbidelli, Renato [verfasserIn] Saltalippi, Carla [verfasserIn] Picciafuoco, Tommaso [verfasserIn] Corradini, Corrado [verfasserIn] Govindaraju, Rao S. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2018

Schlagwörter:	Areal infiltration Infiltration modelling Rainfall-runoff experiments

Übergeordnetes Werk:	Enthalten in: Journal of hydrology - Amsterdam [u.a.] : Elsevier, 1963, 565, Seite 835-845
Übergeordnetes Werk:	volume:565 ; pages:835-845

DOI / URN:	10.1016/j.jhydrol.2018.08.073

Katalog-ID:	ELV00072761X

Internformat


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520			\|a Operative distributed/semi-distributed rainfall-runoff formulations need a mathematically tractable component for estimating the expected areal-average infiltration rate, I , while point infiltration models are usually adopted for this purpose. A model for I , suitable for hydrological applications, was proposed by Morbidelli et al. (2006, Hydrological Processes, 20: 1465–1481). The main model tenet is the use of cumulative infiltration as an independent variable and replacement of time by its expected value. While this model - as with many other models for field-scale infiltration - was tested through Monte Carlo methods, it remains untested with experimental observations. In this study, a reassessment of the model’s applicability is conducted through experimental evidence from several rainfall-runoff events observed under natural conditions at the plot scale over a slight slope characterized by a silty loam soil. During each experiment rainfall rate, surface runoff at the plot outlet and soil water content vertical profiles were monitored at short time intervals. An overall analysis of our results suggests that the model reliably simulates I and surface runoff as functions of time and is also suitable for applications under time-dependent rainfall events. The process of redistribution under rainfall hiatus is not addressed by this model.
650		4	\|a Areal infiltration
650		4	\|a Infiltration modelling
650		4	\|a Rainfall-runoff experiments
700	1		\|a Morbidelli, Renato \|e verfasserin \|0 (orcid)0000-0001-8388-2149 \|4 aut
700	1		\|a Saltalippi, Carla \|e verfasserin \|0 (orcid)0000-0002-5868-6442 \|4 aut
700	1		\|a Picciafuoco, Tommaso \|e verfasserin \|4 aut
700	1		\|a Corradini, Corrado \|e verfasserin \|0 (orcid)0000-0002-7297-6665 \|4 aut
700	1		\|a Govindaraju, Rao S. \|e verfasserin \|4 aut
773	0	8	\|i Enthalten in \|t Journal of hydrology \|d Amsterdam [u.a.] : Elsevier, 1963 \|g 565, Seite 835-845 \|h Online-Ressource \|w (DE-627)268761817 \|w (DE-600)1473173-3 \|w (DE-576)077610628 \|x 1879-2707 \|7 nnns
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912			\|a GBV_ILN_63
912			\|a GBV_ILN_65
912			\|a GBV_ILN_69
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912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_702
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912			\|a GBV_ILN_2014
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912			\|a GBV_ILN_2020
912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2027
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2038
912			\|a GBV_ILN_2044
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912			\|a GBV_ILN_2049
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912			\|a GBV_ILN_2056
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
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936	b	k	\|a 38.85 \|j Hydrologie: Allgemeines
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Indexfelder

author_variant	a f af r m rm c s cs t p tp c c cc r s g rs rsg
matchkey_str	article:18792707:2018----::esesetfsmaayiafedcliflrtomdlhogeprmns
hierarchy_sort_str	2018
bklnumber	38.85
publishDate	2018
allfields	10.1016/j.jhydrol.2018.08.073 doi (DE-627)ELV00072761X (ELSEVIER)S0022-1694(18)30672-3 DE-627 ger DE-627 rda eng 690 DE-600 38.85 bkl Flammini, Alessia verfasserin (orcid)0000-0002-9823-3413 aut Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Operative distributed/semi-distributed rainfall-runoff formulations need a mathematically tractable component for estimating the expected areal-average infiltration rate, I , while point infiltration models are usually adopted for this purpose. A model for I , suitable for hydrological applications, was proposed by Morbidelli et al. (2006, Hydrological Processes, 20: 1465–1481). The main model tenet is the use of cumulative infiltration as an independent variable and replacement of time by its expected value. While this model - as with many other models for field-scale infiltration - was tested through Monte Carlo methods, it remains untested with experimental observations. In this study, a reassessment of the model’s applicability is conducted through experimental evidence from several rainfall-runoff events observed under natural conditions at the plot scale over a slight slope characterized by a silty loam soil. During each experiment rainfall rate, surface runoff at the plot outlet and soil water content vertical profiles were monitored at short time intervals. An overall analysis of our results suggests that the model reliably simulates I and surface runoff as functions of time and is also suitable for applications under time-dependent rainfall events. The process of redistribution under rainfall hiatus is not addressed by this model. Areal infiltration Infiltration modelling Rainfall-runoff experiments Morbidelli, Renato verfasserin (orcid)0000-0001-8388-2149 aut Saltalippi, Carla verfasserin (orcid)0000-0002-5868-6442 aut Picciafuoco, Tommaso verfasserin aut Corradini, Corrado verfasserin (orcid)0000-0002-7297-6665 aut Govindaraju, Rao S. verfasserin aut Enthalten in Journal of hydrology Amsterdam [u.a.] : Elsevier, 1963 565, Seite 835-845 Online-Ressource (DE-627)268761817 (DE-600)1473173-3 (DE-576)077610628 1879-2707 nnns volume:565 pages:835-845 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.85 Hydrologie: Allgemeines AR 565 835-845
spelling	10.1016/j.jhydrol.2018.08.073 doi (DE-627)ELV00072761X (ELSEVIER)S0022-1694(18)30672-3 DE-627 ger DE-627 rda eng 690 DE-600 38.85 bkl Flammini, Alessia verfasserin (orcid)0000-0002-9823-3413 aut Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Operative distributed/semi-distributed rainfall-runoff formulations need a mathematically tractable component for estimating the expected areal-average infiltration rate, I , while point infiltration models are usually adopted for this purpose. A model for I , suitable for hydrological applications, was proposed by Morbidelli et al. (2006, Hydrological Processes, 20: 1465–1481). The main model tenet is the use of cumulative infiltration as an independent variable and replacement of time by its expected value. While this model - as with many other models for field-scale infiltration - was tested through Monte Carlo methods, it remains untested with experimental observations. In this study, a reassessment of the model’s applicability is conducted through experimental evidence from several rainfall-runoff events observed under natural conditions at the plot scale over a slight slope characterized by a silty loam soil. During each experiment rainfall rate, surface runoff at the plot outlet and soil water content vertical profiles were monitored at short time intervals. An overall analysis of our results suggests that the model reliably simulates I and surface runoff as functions of time and is also suitable for applications under time-dependent rainfall events. The process of redistribution under rainfall hiatus is not addressed by this model. Areal infiltration Infiltration modelling Rainfall-runoff experiments Morbidelli, Renato verfasserin (orcid)0000-0001-8388-2149 aut Saltalippi, Carla verfasserin (orcid)0000-0002-5868-6442 aut Picciafuoco, Tommaso verfasserin aut Corradini, Corrado verfasserin (orcid)0000-0002-7297-6665 aut Govindaraju, Rao S. verfasserin aut Enthalten in Journal of hydrology Amsterdam [u.a.] : Elsevier, 1963 565, Seite 835-845 Online-Ressource (DE-627)268761817 (DE-600)1473173-3 (DE-576)077610628 1879-2707 nnns volume:565 pages:835-845 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.85 Hydrologie: Allgemeines AR 565 835-845
allfields_unstemmed	10.1016/j.jhydrol.2018.08.073 doi (DE-627)ELV00072761X (ELSEVIER)S0022-1694(18)30672-3 DE-627 ger DE-627 rda eng 690 DE-600 38.85 bkl Flammini, Alessia verfasserin (orcid)0000-0002-9823-3413 aut Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Operative distributed/semi-distributed rainfall-runoff formulations need a mathematically tractable component for estimating the expected areal-average infiltration rate, I , while point infiltration models are usually adopted for this purpose. A model for I , suitable for hydrological applications, was proposed by Morbidelli et al. (2006, Hydrological Processes, 20: 1465–1481). The main model tenet is the use of cumulative infiltration as an independent variable and replacement of time by its expected value. While this model - as with many other models for field-scale infiltration - was tested through Monte Carlo methods, it remains untested with experimental observations. In this study, a reassessment of the model’s applicability is conducted through experimental evidence from several rainfall-runoff events observed under natural conditions at the plot scale over a slight slope characterized by a silty loam soil. During each experiment rainfall rate, surface runoff at the plot outlet and soil water content vertical profiles were monitored at short time intervals. An overall analysis of our results suggests that the model reliably simulates I and surface runoff as functions of time and is also suitable for applications under time-dependent rainfall events. The process of redistribution under rainfall hiatus is not addressed by this model. Areal infiltration Infiltration modelling Rainfall-runoff experiments Morbidelli, Renato verfasserin (orcid)0000-0001-8388-2149 aut Saltalippi, Carla verfasserin (orcid)0000-0002-5868-6442 aut Picciafuoco, Tommaso verfasserin aut Corradini, Corrado verfasserin (orcid)0000-0002-7297-6665 aut Govindaraju, Rao S. verfasserin aut Enthalten in Journal of hydrology Amsterdam [u.a.] : Elsevier, 1963 565, Seite 835-845 Online-Ressource (DE-627)268761817 (DE-600)1473173-3 (DE-576)077610628 1879-2707 nnns volume:565 pages:835-845 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.85 Hydrologie: Allgemeines AR 565 835-845
allfieldsGer	10.1016/j.jhydrol.2018.08.073 doi (DE-627)ELV00072761X (ELSEVIER)S0022-1694(18)30672-3 DE-627 ger DE-627 rda eng 690 DE-600 38.85 bkl Flammini, Alessia verfasserin (orcid)0000-0002-9823-3413 aut Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Operative distributed/semi-distributed rainfall-runoff formulations need a mathematically tractable component for estimating the expected areal-average infiltration rate, I , while point infiltration models are usually adopted for this purpose. A model for I , suitable for hydrological applications, was proposed by Morbidelli et al. (2006, Hydrological Processes, 20: 1465–1481). The main model tenet is the use of cumulative infiltration as an independent variable and replacement of time by its expected value. While this model - as with many other models for field-scale infiltration - was tested through Monte Carlo methods, it remains untested with experimental observations. In this study, a reassessment of the model’s applicability is conducted through experimental evidence from several rainfall-runoff events observed under natural conditions at the plot scale over a slight slope characterized by a silty loam soil. During each experiment rainfall rate, surface runoff at the plot outlet and soil water content vertical profiles were monitored at short time intervals. An overall analysis of our results suggests that the model reliably simulates I and surface runoff as functions of time and is also suitable for applications under time-dependent rainfall events. The process of redistribution under rainfall hiatus is not addressed by this model. Areal infiltration Infiltration modelling Rainfall-runoff experiments Morbidelli, Renato verfasserin (orcid)0000-0001-8388-2149 aut Saltalippi, Carla verfasserin (orcid)0000-0002-5868-6442 aut Picciafuoco, Tommaso verfasserin aut Corradini, Corrado verfasserin (orcid)0000-0002-7297-6665 aut Govindaraju, Rao S. verfasserin aut Enthalten in Journal of hydrology Amsterdam [u.a.] : Elsevier, 1963 565, Seite 835-845 Online-Ressource (DE-627)268761817 (DE-600)1473173-3 (DE-576)077610628 1879-2707 nnns volume:565 pages:835-845 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.85 Hydrologie: Allgemeines AR 565 835-845
allfieldsSound	10.1016/j.jhydrol.2018.08.073 doi (DE-627)ELV00072761X (ELSEVIER)S0022-1694(18)30672-3 DE-627 ger DE-627 rda eng 690 DE-600 38.85 bkl Flammini, Alessia verfasserin (orcid)0000-0002-9823-3413 aut Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Operative distributed/semi-distributed rainfall-runoff formulations need a mathematically tractable component for estimating the expected areal-average infiltration rate, I , while point infiltration models are usually adopted for this purpose. A model for I , suitable for hydrological applications, was proposed by Morbidelli et al. (2006, Hydrological Processes, 20: 1465–1481). The main model tenet is the use of cumulative infiltration as an independent variable and replacement of time by its expected value. While this model - as with many other models for field-scale infiltration - was tested through Monte Carlo methods, it remains untested with experimental observations. In this study, a reassessment of the model’s applicability is conducted through experimental evidence from several rainfall-runoff events observed under natural conditions at the plot scale over a slight slope characterized by a silty loam soil. During each experiment rainfall rate, surface runoff at the plot outlet and soil water content vertical profiles were monitored at short time intervals. An overall analysis of our results suggests that the model reliably simulates I and surface runoff as functions of time and is also suitable for applications under time-dependent rainfall events. The process of redistribution under rainfall hiatus is not addressed by this model. Areal infiltration Infiltration modelling Rainfall-runoff experiments Morbidelli, Renato verfasserin (orcid)0000-0001-8388-2149 aut Saltalippi, Carla verfasserin (orcid)0000-0002-5868-6442 aut Picciafuoco, Tommaso verfasserin aut Corradini, Corrado verfasserin (orcid)0000-0002-7297-6665 aut Govindaraju, Rao S. verfasserin aut Enthalten in Journal of hydrology Amsterdam [u.a.] : Elsevier, 1963 565, Seite 835-845 Online-Ressource (DE-627)268761817 (DE-600)1473173-3 (DE-576)077610628 1879-2707 nnns volume:565 pages:835-845 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.85 Hydrologie: Allgemeines AR 565 835-845
language	English
source	Enthalten in Journal of hydrology 565, Seite 835-845 volume:565 pages:835-845
sourceStr	Enthalten in Journal of hydrology 565, Seite 835-845 volume:565 pages:835-845
format_phy_str_mv	Article
bklname	Hydrologie: Allgemeines
institution	findex.gbv.de
topic_facet	Areal infiltration Infiltration modelling Rainfall-runoff experiments
dewey-raw	690
isfreeaccess_bool	false
container_title	Journal of hydrology
authorswithroles_txt_mv	Flammini, Alessia @@aut@@ Morbidelli, Renato @@aut@@ Saltalippi, Carla @@aut@@ Picciafuoco, Tommaso @@aut@@ Corradini, Corrado @@aut@@ Govindaraju, Rao S. @@aut@@
publishDateDaySort_date	2018-01-01T00:00:00Z
hierarchy_top_id	268761817
dewey-sort	3690
id	ELV00072761X
language_de	englisch
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author	Flammini, Alessia
spellingShingle	Flammini, Alessia ddc 690 bkl 38.85 misc Areal infiltration misc Infiltration modelling misc Rainfall-runoff experiments Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events
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topic_title	690 DE-600 38.85 bkl Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events Areal infiltration Infiltration modelling Rainfall-runoff experiments
topic	ddc 690 bkl 38.85 misc Areal infiltration misc Infiltration modelling misc Rainfall-runoff experiments
topic_unstemmed	ddc 690 bkl 38.85 misc Areal infiltration misc Infiltration modelling misc Rainfall-runoff experiments
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title	Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events
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title_full	Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events
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author_browse	Flammini, Alessia Morbidelli, Renato Saltalippi, Carla Picciafuoco, Tommaso Corradini, Corrado Govindaraju, Rao S.
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title_sort	reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events
title_auth	Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events
abstract	Operative distributed/semi-distributed rainfall-runoff formulations need a mathematically tractable component for estimating the expected areal-average infiltration rate, I , while point infiltration models are usually adopted for this purpose. A model for I , suitable for hydrological applications, was proposed by Morbidelli et al. (2006, Hydrological Processes, 20: 1465–1481). The main model tenet is the use of cumulative infiltration as an independent variable and replacement of time by its expected value. While this model - as with many other models for field-scale infiltration - was tested through Monte Carlo methods, it remains untested with experimental observations. In this study, a reassessment of the model’s applicability is conducted through experimental evidence from several rainfall-runoff events observed under natural conditions at the plot scale over a slight slope characterized by a silty loam soil. During each experiment rainfall rate, surface runoff at the plot outlet and soil water content vertical profiles were monitored at short time intervals. An overall analysis of our results suggests that the model reliably simulates I and surface runoff as functions of time and is also suitable for applications under time-dependent rainfall events. The process of redistribution under rainfall hiatus is not addressed by this model.
abstractGer	Operative distributed/semi-distributed rainfall-runoff formulations need a mathematically tractable component for estimating the expected areal-average infiltration rate, I , while point infiltration models are usually adopted for this purpose. A model for I , suitable for hydrological applications, was proposed by Morbidelli et al. (2006, Hydrological Processes, 20: 1465–1481). The main model tenet is the use of cumulative infiltration as an independent variable and replacement of time by its expected value. While this model - as with many other models for field-scale infiltration - was tested through Monte Carlo methods, it remains untested with experimental observations. In this study, a reassessment of the model’s applicability is conducted through experimental evidence from several rainfall-runoff events observed under natural conditions at the plot scale over a slight slope characterized by a silty loam soil. During each experiment rainfall rate, surface runoff at the plot outlet and soil water content vertical profiles were monitored at short time intervals. An overall analysis of our results suggests that the model reliably simulates I and surface runoff as functions of time and is also suitable for applications under time-dependent rainfall events. The process of redistribution under rainfall hiatus is not addressed by this model.
abstract_unstemmed	Operative distributed/semi-distributed rainfall-runoff formulations need a mathematically tractable component for estimating the expected areal-average infiltration rate, I , while point infiltration models are usually adopted for this purpose. A model for I , suitable for hydrological applications, was proposed by Morbidelli et al. (2006, Hydrological Processes, 20: 1465–1481). The main model tenet is the use of cumulative infiltration as an independent variable and replacement of time by its expected value. While this model - as with many other models for field-scale infiltration - was tested through Monte Carlo methods, it remains untested with experimental observations. In this study, a reassessment of the model’s applicability is conducted through experimental evidence from several rainfall-runoff events observed under natural conditions at the plot scale over a slight slope characterized by a silty loam soil. During each experiment rainfall rate, surface runoff at the plot outlet and soil water content vertical profiles were monitored at short time intervals. An overall analysis of our results suggests that the model reliably simulates I and surface runoff as functions of time and is also suitable for applications under time-dependent rainfall events. The process of redistribution under rainfall hiatus is not addressed by this model.
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title_short	Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events
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author2	Morbidelli, Renato Saltalippi, Carla Picciafuoco, Tommaso Corradini, Corrado Govindaraju, Rao S.
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up_date	2024-07-06T18:58:06.167Z
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Reassessment of a semi-analytical field-scale infiltration model through experiments under natural rainfall events

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