Comparison of two methods to assess heterogeneity of water flow in soils
The heterogeneity of water flow and solute transport was assessed during radioactive tracer infiltration experiment in a black clay loam soil using modified methods to estimate the effective cross section (ECS) and the degree of preferential flow (DPF). The results of field and numerical experiments...
Ausführliche Beschreibung
Autor*in: |
Lichner Ľubomír [verfasserIn] Dušek Jaromír [verfasserIn] Dekker Louis W. [verfasserIn] Zhukova Natalia [verfasserIn] Faško Pavol [verfasserIn] Holko Ladislav [verfasserIn] Šír Miloslav [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2013 |
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Übergeordnetes Werk: |
In: Journal of Hydrology and Hydromechanics - Sciendo, 2015, 61(2013), 4, Seite 299-304 |
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Übergeordnetes Werk: |
volume:61 ; year:2013 ; number:4 ; pages:299-304 |
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DOI / URN: |
10.2478/johh-2013-0038 |
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Katalog-ID: |
DOAJ077837142 |
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10.2478/johh-2013-0038 doi (DE-627)DOAJ077837142 (DE-599)DOAJac17b9f136c149229bd97289d634902a DE-627 ger DE-627 rakwb eng TC1-978 Lichner Ľubomír verfasserin aut Comparison of two methods to assess heterogeneity of water flow in soils 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The heterogeneity of water flow and solute transport was assessed during radioactive tracer infiltration experiment in a black clay loam soil using modified methods to estimate the effective cross section (ECS) and the degree of preferential flow (DPF). The results of field and numerical experiments showed that these parameters characterized the heterogeneity of water flow in the soils unequivocally. The ECS decreases non-linearly and the DPF increases linearly with an increase of the bypassing ratio (ratio of macropore flow rate to total flow rate). The ECS decreased and the DPF increased with depth, which suggests an increase in the heterogeneity of water flow with depth. The plot of the DPF against ECS values calculated from the tracer experiment data was consistent with the relationship obtained by the numerical simulation assuming preferential flow in the neighbourhood of three probes. degree of preferential flow effective cross section preferential flow in soil infiltration experiment radioactive tracer technique Hydraulic engineering Dušek Jaromír verfasserin aut Dekker Louis W. verfasserin aut Zhukova Natalia verfasserin aut Faško Pavol verfasserin aut Holko Ladislav verfasserin aut Šír Miloslav verfasserin aut In Journal of Hydrology and Hydromechanics Sciendo, 2015 61(2013), 4, Seite 299-304 (DE-627)604801416 (DE-600)2503779-1 13384333 nnns volume:61 year:2013 number:4 pages:299-304 https://doi.org/10.2478/johh-2013-0038 kostenfrei https://doaj.org/article/ac17b9f136c149229bd97289d634902a kostenfrei https://doi.org/10.2478/johh-2013-0038 kostenfrei https://doaj.org/toc/0042-790X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4700 AR 61 2013 4 299-304 |
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10.2478/johh-2013-0038 doi (DE-627)DOAJ077837142 (DE-599)DOAJac17b9f136c149229bd97289d634902a DE-627 ger DE-627 rakwb eng TC1-978 Lichner Ľubomír verfasserin aut Comparison of two methods to assess heterogeneity of water flow in soils 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The heterogeneity of water flow and solute transport was assessed during radioactive tracer infiltration experiment in a black clay loam soil using modified methods to estimate the effective cross section (ECS) and the degree of preferential flow (DPF). The results of field and numerical experiments showed that these parameters characterized the heterogeneity of water flow in the soils unequivocally. The ECS decreases non-linearly and the DPF increases linearly with an increase of the bypassing ratio (ratio of macropore flow rate to total flow rate). The ECS decreased and the DPF increased with depth, which suggests an increase in the heterogeneity of water flow with depth. The plot of the DPF against ECS values calculated from the tracer experiment data was consistent with the relationship obtained by the numerical simulation assuming preferential flow in the neighbourhood of three probes. degree of preferential flow effective cross section preferential flow in soil infiltration experiment radioactive tracer technique Hydraulic engineering Dušek Jaromír verfasserin aut Dekker Louis W. verfasserin aut Zhukova Natalia verfasserin aut Faško Pavol verfasserin aut Holko Ladislav verfasserin aut Šír Miloslav verfasserin aut In Journal of Hydrology and Hydromechanics Sciendo, 2015 61(2013), 4, Seite 299-304 (DE-627)604801416 (DE-600)2503779-1 13384333 nnns volume:61 year:2013 number:4 pages:299-304 https://doi.org/10.2478/johh-2013-0038 kostenfrei https://doaj.org/article/ac17b9f136c149229bd97289d634902a kostenfrei https://doi.org/10.2478/johh-2013-0038 kostenfrei https://doaj.org/toc/0042-790X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4700 AR 61 2013 4 299-304 |
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10.2478/johh-2013-0038 doi (DE-627)DOAJ077837142 (DE-599)DOAJac17b9f136c149229bd97289d634902a DE-627 ger DE-627 rakwb eng TC1-978 Lichner Ľubomír verfasserin aut Comparison of two methods to assess heterogeneity of water flow in soils 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The heterogeneity of water flow and solute transport was assessed during radioactive tracer infiltration experiment in a black clay loam soil using modified methods to estimate the effective cross section (ECS) and the degree of preferential flow (DPF). The results of field and numerical experiments showed that these parameters characterized the heterogeneity of water flow in the soils unequivocally. The ECS decreases non-linearly and the DPF increases linearly with an increase of the bypassing ratio (ratio of macropore flow rate to total flow rate). The ECS decreased and the DPF increased with depth, which suggests an increase in the heterogeneity of water flow with depth. The plot of the DPF against ECS values calculated from the tracer experiment data was consistent with the relationship obtained by the numerical simulation assuming preferential flow in the neighbourhood of three probes. degree of preferential flow effective cross section preferential flow in soil infiltration experiment radioactive tracer technique Hydraulic engineering Dušek Jaromír verfasserin aut Dekker Louis W. verfasserin aut Zhukova Natalia verfasserin aut Faško Pavol verfasserin aut Holko Ladislav verfasserin aut Šír Miloslav verfasserin aut In Journal of Hydrology and Hydromechanics Sciendo, 2015 61(2013), 4, Seite 299-304 (DE-627)604801416 (DE-600)2503779-1 13384333 nnns volume:61 year:2013 number:4 pages:299-304 https://doi.org/10.2478/johh-2013-0038 kostenfrei https://doaj.org/article/ac17b9f136c149229bd97289d634902a kostenfrei https://doi.org/10.2478/johh-2013-0038 kostenfrei https://doaj.org/toc/0042-790X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4700 AR 61 2013 4 299-304 |
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10.2478/johh-2013-0038 doi (DE-627)DOAJ077837142 (DE-599)DOAJac17b9f136c149229bd97289d634902a DE-627 ger DE-627 rakwb eng TC1-978 Lichner Ľubomír verfasserin aut Comparison of two methods to assess heterogeneity of water flow in soils 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The heterogeneity of water flow and solute transport was assessed during radioactive tracer infiltration experiment in a black clay loam soil using modified methods to estimate the effective cross section (ECS) and the degree of preferential flow (DPF). The results of field and numerical experiments showed that these parameters characterized the heterogeneity of water flow in the soils unequivocally. The ECS decreases non-linearly and the DPF increases linearly with an increase of the bypassing ratio (ratio of macropore flow rate to total flow rate). The ECS decreased and the DPF increased with depth, which suggests an increase in the heterogeneity of water flow with depth. The plot of the DPF against ECS values calculated from the tracer experiment data was consistent with the relationship obtained by the numerical simulation assuming preferential flow in the neighbourhood of three probes. degree of preferential flow effective cross section preferential flow in soil infiltration experiment radioactive tracer technique Hydraulic engineering Dušek Jaromír verfasserin aut Dekker Louis W. verfasserin aut Zhukova Natalia verfasserin aut Faško Pavol verfasserin aut Holko Ladislav verfasserin aut Šír Miloslav verfasserin aut In Journal of Hydrology and Hydromechanics Sciendo, 2015 61(2013), 4, Seite 299-304 (DE-627)604801416 (DE-600)2503779-1 13384333 nnns volume:61 year:2013 number:4 pages:299-304 https://doi.org/10.2478/johh-2013-0038 kostenfrei https://doaj.org/article/ac17b9f136c149229bd97289d634902a kostenfrei https://doi.org/10.2478/johh-2013-0038 kostenfrei https://doaj.org/toc/0042-790X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4700 AR 61 2013 4 299-304 |
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The heterogeneity of water flow and solute transport was assessed during radioactive tracer infiltration experiment in a black clay loam soil using modified methods to estimate the effective cross section (ECS) and the degree of preferential flow (DPF). The results of field and numerical experiments showed that these parameters characterized the heterogeneity of water flow in the soils unequivocally. The ECS decreases non-linearly and the DPF increases linearly with an increase of the bypassing ratio (ratio of macropore flow rate to total flow rate). The ECS decreased and the DPF increased with depth, which suggests an increase in the heterogeneity of water flow with depth. The plot of the DPF against ECS values calculated from the tracer experiment data was consistent with the relationship obtained by the numerical simulation assuming preferential flow in the neighbourhood of three probes. |
abstractGer |
The heterogeneity of water flow and solute transport was assessed during radioactive tracer infiltration experiment in a black clay loam soil using modified methods to estimate the effective cross section (ECS) and the degree of preferential flow (DPF). The results of field and numerical experiments showed that these parameters characterized the heterogeneity of water flow in the soils unequivocally. The ECS decreases non-linearly and the DPF increases linearly with an increase of the bypassing ratio (ratio of macropore flow rate to total flow rate). The ECS decreased and the DPF increased with depth, which suggests an increase in the heterogeneity of water flow with depth. The plot of the DPF against ECS values calculated from the tracer experiment data was consistent with the relationship obtained by the numerical simulation assuming preferential flow in the neighbourhood of three probes. |
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The heterogeneity of water flow and solute transport was assessed during radioactive tracer infiltration experiment in a black clay loam soil using modified methods to estimate the effective cross section (ECS) and the degree of preferential flow (DPF). The results of field and numerical experiments showed that these parameters characterized the heterogeneity of water flow in the soils unequivocally. The ECS decreases non-linearly and the DPF increases linearly with an increase of the bypassing ratio (ratio of macropore flow rate to total flow rate). The ECS decreased and the DPF increased with depth, which suggests an increase in the heterogeneity of water flow with depth. The plot of the DPF against ECS values calculated from the tracer experiment data was consistent with the relationship obtained by the numerical simulation assuming preferential flow in the neighbourhood of three probes. |
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