Actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop

Physical properties of soils have a significant influence on their water regime and should be considered when selecting suitable agricultural crops for particular sites, taking into account the crop productivity and its water requirements. Mean daily rates of actual evapotranspiration (ETa) were obtained by collation of measured or otherwise estimated 10-min values for the years 2004, 2006 and 2009 for a partially tile-drained agricultural experimental catchment in the Bohemo-Moravian Highland (Czech Republic). ETa was measured using the Bowen ratio (β) and energy balance (BREB) method at four weather stations located on different soil types (Stagnosols, Cambisols) and terrain relief positions (defined with respect to the groundwater recharge and discharge zones) over different crops (cereals, oil rape and permanent grassland). A systematic influence of soil properties on the evapotranspiration rate was more pronounced during the periods of limited transpiration (soil drought, crop maturity), when the average daily ETa was significantly lower and the corresponding β significantly higher over coarser-textured soils (shallow Haplic Cambisols), namely (year-ETa (mm/day)/β): 2004 - 1.75/1.66; 2006 - 2.44/0.93; 2009 - 2.60/0.81), than over finer-textured soils (Stagnic Cambisols and Haplic Stagnosols), namely: 2004 - 2.92/0.97; 2006 - 3.06/0.44; 2009 - 3.42/0.39). When the transpiration was not limited by soil water deficit, it acted as an equalizing factor smoothing down evapotranspiration from heterogeneous soil areas, whereby the effect of the soil physical properties was masked. With regard to soil water regime and evapotranspiration, the tile-drained Stagnic Cambisol lands behaved similarly as non-drained Haplic Cambisols. The effects of land use and of the terrain relief position could not be tracked independently, because the permanent grassland was situated in the wetter and texturally heavier parts of the catchment and the positions of the recharge/discharge zone coincided with the positions of texturally lighter/heavier soils, respectively. Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Renata DUFFKOVÁ [verfasserIn] Antonín ZAJÍČEK [verfasserIn] Eva NOVÁKOVÁ [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2011

Schlagwörter:	actual evapotranspiration bowen ratio cambisol cereals discharge zone energy balance grassland oil rape recharge zone soil physical properties stagnosol tile drainage transient zone

Übergeordnetes Werk:	In: Soil and Water Research - Czech Academy of Agricultural Sciences, 2016, 6(2011), 3, Seite 131-146
Übergeordnetes Werk:	volume:6 ; year:2011 ; number:3 ; pages:131-146

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.17221/20/2010-SWR

Katalog-ID:	DOAJ082812721

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publishDate	2011
allfields	10.17221/20/2010-SWR doi (DE-627)DOAJ082812721 (DE-599)DOAJ781481c2f3124512b004ef373e776380 DE-627 ger DE-627 rakwb eng Renata DUFFKOVÁ verfasserin aut Actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Physical properties of soils have a significant influence on their water regime and should be considered when selecting suitable agricultural crops for particular sites, taking into account the crop productivity and its water requirements. Mean daily rates of actual evapotranspiration (ETa) were obtained by collation of measured or otherwise estimated 10-min values for the years 2004, 2006 and 2009 for a partially tile-drained agricultural experimental catchment in the Bohemo-Moravian Highland (Czech Republic). ETa was measured using the Bowen ratio (β) and energy balance (BREB) method at four weather stations located on different soil types (Stagnosols, Cambisols) and terrain relief positions (defined with respect to the groundwater recharge and discharge zones) over different crops (cereals, oil rape and permanent grassland). A systematic influence of soil properties on the evapotranspiration rate was more pronounced during the periods of limited transpiration (soil drought, crop maturity), when the average daily ETa was significantly lower and the corresponding β significantly higher over coarser-textured soils (shallow Haplic Cambisols), namely (year-ETa (mm/day)/β): 2004 - 1.75/1.66; 2006 - 2.44/0.93; 2009 - 2.60/0.81), than over finer-textured soils (Stagnic Cambisols and Haplic Stagnosols), namely: 2004 - 2.92/0.97; 2006 - 3.06/0.44; 2009 - 3.42/0.39). When the transpiration was not limited by soil water deficit, it acted as an equalizing factor smoothing down evapotranspiration from heterogeneous soil areas, whereby the effect of the soil physical properties was masked. With regard to soil water regime and evapotranspiration, the tile-drained Stagnic Cambisol lands behaved similarly as non-drained Haplic Cambisols. The effects of land use and of the terrain relief position could not be tracked independently, because the permanent grassland was situated in the wetter and texturally heavier parts of the catchment and the positions of the recharge/discharge zone coincided with the positions of texturally lighter/heavier soils, respectively. actual evapotranspiration bowen ratio cambisol cereals discharge zone energy balance grassland oil rape recharge zone soil physical properties stagnosol tile drainage transient zone Agriculture S Antonín ZAJÍČEK verfasserin aut Eva NOVÁKOVÁ verfasserin aut In Soil and Water Research Czech Academy of Agricultural Sciences, 2016 6(2011), 3, Seite 131-146 (DE-627)585506779 (DE-600)2465020-1 18059384 nnns volume:6 year:2011 number:3 pages:131-146 https://doi.org/10.17221/20/2010-SWR kostenfrei https://doaj.org/article/781481c2f3124512b004ef373e776380 kostenfrei https://swr.agriculturejournals.cz/artkey/swr-201103-0003_actual-evapotranspiration-from-partially-tile-drained-fields-as-influenced-by-soil-properties-terrain-and-crop.php kostenfrei https://doaj.org/toc/1801-5395 Journal toc kostenfrei https://doaj.org/toc/1805-9384 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ 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_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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 6 2011 3 131-146
spelling	10.17221/20/2010-SWR doi (DE-627)DOAJ082812721 (DE-599)DOAJ781481c2f3124512b004ef373e776380 DE-627 ger DE-627 rakwb eng Renata DUFFKOVÁ verfasserin aut Actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Physical properties of soils have a significant influence on their water regime and should be considered when selecting suitable agricultural crops for particular sites, taking into account the crop productivity and its water requirements. Mean daily rates of actual evapotranspiration (ETa) were obtained by collation of measured or otherwise estimated 10-min values for the years 2004, 2006 and 2009 for a partially tile-drained agricultural experimental catchment in the Bohemo-Moravian Highland (Czech Republic). ETa was measured using the Bowen ratio (β) and energy balance (BREB) method at four weather stations located on different soil types (Stagnosols, Cambisols) and terrain relief positions (defined with respect to the groundwater recharge and discharge zones) over different crops (cereals, oil rape and permanent grassland). A systematic influence of soil properties on the evapotranspiration rate was more pronounced during the periods of limited transpiration (soil drought, crop maturity), when the average daily ETa was significantly lower and the corresponding β significantly higher over coarser-textured soils (shallow Haplic Cambisols), namely (year-ETa (mm/day)/β): 2004 - 1.75/1.66; 2006 - 2.44/0.93; 2009 - 2.60/0.81), than over finer-textured soils (Stagnic Cambisols and Haplic Stagnosols), namely: 2004 - 2.92/0.97; 2006 - 3.06/0.44; 2009 - 3.42/0.39). When the transpiration was not limited by soil water deficit, it acted as an equalizing factor smoothing down evapotranspiration from heterogeneous soil areas, whereby the effect of the soil physical properties was masked. With regard to soil water regime and evapotranspiration, the tile-drained Stagnic Cambisol lands behaved similarly as non-drained Haplic Cambisols. The effects of land use and of the terrain relief position could not be tracked independently, because the permanent grassland was situated in the wetter and texturally heavier parts of the catchment and the positions of the recharge/discharge zone coincided with the positions of texturally lighter/heavier soils, respectively. actual evapotranspiration bowen ratio cambisol cereals discharge zone energy balance grassland oil rape recharge zone soil physical properties stagnosol tile drainage transient zone Agriculture S Antonín ZAJÍČEK verfasserin aut Eva NOVÁKOVÁ verfasserin aut In Soil and Water Research Czech Academy of Agricultural Sciences, 2016 6(2011), 3, Seite 131-146 (DE-627)585506779 (DE-600)2465020-1 18059384 nnns volume:6 year:2011 number:3 pages:131-146 https://doi.org/10.17221/20/2010-SWR kostenfrei https://doaj.org/article/781481c2f3124512b004ef373e776380 kostenfrei https://swr.agriculturejournals.cz/artkey/swr-201103-0003_actual-evapotranspiration-from-partially-tile-drained-fields-as-influenced-by-soil-properties-terrain-and-crop.php kostenfrei https://doaj.org/toc/1801-5395 Journal toc kostenfrei https://doaj.org/toc/1805-9384 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ 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_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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 6 2011 3 131-146
allfields_unstemmed	10.17221/20/2010-SWR doi (DE-627)DOAJ082812721 (DE-599)DOAJ781481c2f3124512b004ef373e776380 DE-627 ger DE-627 rakwb eng Renata DUFFKOVÁ verfasserin aut Actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Physical properties of soils have a significant influence on their water regime and should be considered when selecting suitable agricultural crops for particular sites, taking into account the crop productivity and its water requirements. Mean daily rates of actual evapotranspiration (ETa) were obtained by collation of measured or otherwise estimated 10-min values for the years 2004, 2006 and 2009 for a partially tile-drained agricultural experimental catchment in the Bohemo-Moravian Highland (Czech Republic). ETa was measured using the Bowen ratio (β) and energy balance (BREB) method at four weather stations located on different soil types (Stagnosols, Cambisols) and terrain relief positions (defined with respect to the groundwater recharge and discharge zones) over different crops (cereals, oil rape and permanent grassland). A systematic influence of soil properties on the evapotranspiration rate was more pronounced during the periods of limited transpiration (soil drought, crop maturity), when the average daily ETa was significantly lower and the corresponding β significantly higher over coarser-textured soils (shallow Haplic Cambisols), namely (year-ETa (mm/day)/β): 2004 - 1.75/1.66; 2006 - 2.44/0.93; 2009 - 2.60/0.81), than over finer-textured soils (Stagnic Cambisols and Haplic Stagnosols), namely: 2004 - 2.92/0.97; 2006 - 3.06/0.44; 2009 - 3.42/0.39). When the transpiration was not limited by soil water deficit, it acted as an equalizing factor smoothing down evapotranspiration from heterogeneous soil areas, whereby the effect of the soil physical properties was masked. With regard to soil water regime and evapotranspiration, the tile-drained Stagnic Cambisol lands behaved similarly as non-drained Haplic Cambisols. The effects of land use and of the terrain relief position could not be tracked independently, because the permanent grassland was situated in the wetter and texturally heavier parts of the catchment and the positions of the recharge/discharge zone coincided with the positions of texturally lighter/heavier soils, respectively. actual evapotranspiration bowen ratio cambisol cereals discharge zone energy balance grassland oil rape recharge zone soil physical properties stagnosol tile drainage transient zone Agriculture S Antonín ZAJÍČEK verfasserin aut Eva NOVÁKOVÁ verfasserin aut In Soil and Water Research Czech Academy of Agricultural Sciences, 2016 6(2011), 3, Seite 131-146 (DE-627)585506779 (DE-600)2465020-1 18059384 nnns volume:6 year:2011 number:3 pages:131-146 https://doi.org/10.17221/20/2010-SWR kostenfrei https://doaj.org/article/781481c2f3124512b004ef373e776380 kostenfrei https://swr.agriculturejournals.cz/artkey/swr-201103-0003_actual-evapotranspiration-from-partially-tile-drained-fields-as-influenced-by-soil-properties-terrain-and-crop.php kostenfrei https://doaj.org/toc/1801-5395 Journal toc kostenfrei https://doaj.org/toc/1805-9384 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ 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_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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 6 2011 3 131-146
allfieldsGer	10.17221/20/2010-SWR doi (DE-627)DOAJ082812721 (DE-599)DOAJ781481c2f3124512b004ef373e776380 DE-627 ger DE-627 rakwb eng Renata DUFFKOVÁ verfasserin aut Actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Physical properties of soils have a significant influence on their water regime and should be considered when selecting suitable agricultural crops for particular sites, taking into account the crop productivity and its water requirements. Mean daily rates of actual evapotranspiration (ETa) were obtained by collation of measured or otherwise estimated 10-min values for the years 2004, 2006 and 2009 for a partially tile-drained agricultural experimental catchment in the Bohemo-Moravian Highland (Czech Republic). ETa was measured using the Bowen ratio (β) and energy balance (BREB) method at four weather stations located on different soil types (Stagnosols, Cambisols) and terrain relief positions (defined with respect to the groundwater recharge and discharge zones) over different crops (cereals, oil rape and permanent grassland). A systematic influence of soil properties on the evapotranspiration rate was more pronounced during the periods of limited transpiration (soil drought, crop maturity), when the average daily ETa was significantly lower and the corresponding β significantly higher over coarser-textured soils (shallow Haplic Cambisols), namely (year-ETa (mm/day)/β): 2004 - 1.75/1.66; 2006 - 2.44/0.93; 2009 - 2.60/0.81), than over finer-textured soils (Stagnic Cambisols and Haplic Stagnosols), namely: 2004 - 2.92/0.97; 2006 - 3.06/0.44; 2009 - 3.42/0.39). When the transpiration was not limited by soil water deficit, it acted as an equalizing factor smoothing down evapotranspiration from heterogeneous soil areas, whereby the effect of the soil physical properties was masked. With regard to soil water regime and evapotranspiration, the tile-drained Stagnic Cambisol lands behaved similarly as non-drained Haplic Cambisols. The effects of land use and of the terrain relief position could not be tracked independently, because the permanent grassland was situated in the wetter and texturally heavier parts of the catchment and the positions of the recharge/discharge zone coincided with the positions of texturally lighter/heavier soils, respectively. actual evapotranspiration bowen ratio cambisol cereals discharge zone energy balance grassland oil rape recharge zone soil physical properties stagnosol tile drainage transient zone Agriculture S Antonín ZAJÍČEK verfasserin aut Eva NOVÁKOVÁ verfasserin aut In Soil and Water Research Czech Academy of Agricultural Sciences, 2016 6(2011), 3, Seite 131-146 (DE-627)585506779 (DE-600)2465020-1 18059384 nnns volume:6 year:2011 number:3 pages:131-146 https://doi.org/10.17221/20/2010-SWR kostenfrei https://doaj.org/article/781481c2f3124512b004ef373e776380 kostenfrei https://swr.agriculturejournals.cz/artkey/swr-201103-0003_actual-evapotranspiration-from-partially-tile-drained-fields-as-influenced-by-soil-properties-terrain-and-crop.php kostenfrei https://doaj.org/toc/1801-5395 Journal toc kostenfrei https://doaj.org/toc/1805-9384 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ 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_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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 6 2011 3 131-146
allfieldsSound	10.17221/20/2010-SWR doi (DE-627)DOAJ082812721 (DE-599)DOAJ781481c2f3124512b004ef373e776380 DE-627 ger DE-627 rakwb eng Renata DUFFKOVÁ verfasserin aut Actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Physical properties of soils have a significant influence on their water regime and should be considered when selecting suitable agricultural crops for particular sites, taking into account the crop productivity and its water requirements. Mean daily rates of actual evapotranspiration (ETa) were obtained by collation of measured or otherwise estimated 10-min values for the years 2004, 2006 and 2009 for a partially tile-drained agricultural experimental catchment in the Bohemo-Moravian Highland (Czech Republic). ETa was measured using the Bowen ratio (β) and energy balance (BREB) method at four weather stations located on different soil types (Stagnosols, Cambisols) and terrain relief positions (defined with respect to the groundwater recharge and discharge zones) over different crops (cereals, oil rape and permanent grassland). A systematic influence of soil properties on the evapotranspiration rate was more pronounced during the periods of limited transpiration (soil drought, crop maturity), when the average daily ETa was significantly lower and the corresponding β significantly higher over coarser-textured soils (shallow Haplic Cambisols), namely (year-ETa (mm/day)/β): 2004 - 1.75/1.66; 2006 - 2.44/0.93; 2009 - 2.60/0.81), than over finer-textured soils (Stagnic Cambisols and Haplic Stagnosols), namely: 2004 - 2.92/0.97; 2006 - 3.06/0.44; 2009 - 3.42/0.39). When the transpiration was not limited by soil water deficit, it acted as an equalizing factor smoothing down evapotranspiration from heterogeneous soil areas, whereby the effect of the soil physical properties was masked. With regard to soil water regime and evapotranspiration, the tile-drained Stagnic Cambisol lands behaved similarly as non-drained Haplic Cambisols. The effects of land use and of the terrain relief position could not be tracked independently, because the permanent grassland was situated in the wetter and texturally heavier parts of the catchment and the positions of the recharge/discharge zone coincided with the positions of texturally lighter/heavier soils, respectively. actual evapotranspiration bowen ratio cambisol cereals discharge zone energy balance grassland oil rape recharge zone soil physical properties stagnosol tile drainage transient zone Agriculture S Antonín ZAJÍČEK verfasserin aut Eva NOVÁKOVÁ verfasserin aut In Soil and Water Research Czech Academy of Agricultural Sciences, 2016 6(2011), 3, Seite 131-146 (DE-627)585506779 (DE-600)2465020-1 18059384 nnns volume:6 year:2011 number:3 pages:131-146 https://doi.org/10.17221/20/2010-SWR kostenfrei https://doaj.org/article/781481c2f3124512b004ef373e776380 kostenfrei https://swr.agriculturejournals.cz/artkey/swr-201103-0003_actual-evapotranspiration-from-partially-tile-drained-fields-as-influenced-by-soil-properties-terrain-and-crop.php kostenfrei https://doaj.org/toc/1801-5395 Journal toc kostenfrei https://doaj.org/toc/1805-9384 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ 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_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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 6 2011 3 131-146
language	English
source	In Soil and Water Research 6(2011), 3, Seite 131-146 volume:6 year:2011 number:3 pages:131-146
sourceStr	In Soil and Water Research 6(2011), 3, Seite 131-146 volume:6 year:2011 number:3 pages:131-146
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	actual evapotranspiration bowen ratio cambisol cereals discharge zone energy balance grassland oil rape recharge zone soil physical properties stagnosol tile drainage transient zone Agriculture S
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container_title	Soil and Water Research
authorswithroles_txt_mv	Renata DUFFKOVÁ @@aut@@ Antonín ZAJÍČEK @@aut@@ Eva NOVÁKOVÁ @@aut@@
publishDateDaySort_date	2011-01-01T00:00:00Z
hierarchy_top_id	585506779
id	DOAJ082812721
language_de	englisch
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author	Renata DUFFKOVÁ
spellingShingle	Renata DUFFKOVÁ misc actual evapotranspiration misc bowen ratio misc cambisol misc cereals misc discharge zone misc energy balance misc grassland misc oil rape misc recharge zone misc soil physical properties misc stagnosol misc tile drainage misc transient zone misc Agriculture misc S Actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop
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topic_title	Actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop actual evapotranspiration bowen ratio cambisol cereals discharge zone energy balance grassland oil rape recharge zone soil physical properties stagnosol tile drainage transient zone
topic	misc actual evapotranspiration misc bowen ratio misc cambisol misc cereals misc discharge zone misc energy balance misc grassland misc oil rape misc recharge zone misc soil physical properties misc stagnosol misc tile drainage misc transient zone misc Agriculture misc S
topic_unstemmed	misc actual evapotranspiration misc bowen ratio misc cambisol misc cereals misc discharge zone misc energy balance misc grassland misc oil rape misc recharge zone misc soil physical properties misc stagnosol misc tile drainage misc transient zone misc Agriculture misc S
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title	Actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop
ctrlnum	(DE-627)DOAJ082812721 (DE-599)DOAJ781481c2f3124512b004ef373e776380
title_full	Actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop
author_sort	Renata DUFFKOVÁ
journal	Soil and Water Research
journalStr	Soil and Water Research
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author_browse	Renata DUFFKOVÁ Antonín ZAJÍČEK Eva NOVÁKOVÁ
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title_sort	actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop
title_auth	Actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop
abstract	Physical properties of soils have a significant influence on their water regime and should be considered when selecting suitable agricultural crops for particular sites, taking into account the crop productivity and its water requirements. Mean daily rates of actual evapotranspiration (ETa) were obtained by collation of measured or otherwise estimated 10-min values for the years 2004, 2006 and 2009 for a partially tile-drained agricultural experimental catchment in the Bohemo-Moravian Highland (Czech Republic). ETa was measured using the Bowen ratio (β) and energy balance (BREB) method at four weather stations located on different soil types (Stagnosols, Cambisols) and terrain relief positions (defined with respect to the groundwater recharge and discharge zones) over different crops (cereals, oil rape and permanent grassland). A systematic influence of soil properties on the evapotranspiration rate was more pronounced during the periods of limited transpiration (soil drought, crop maturity), when the average daily ETa was significantly lower and the corresponding β significantly higher over coarser-textured soils (shallow Haplic Cambisols), namely (year-ETa (mm/day)/β): 2004 - 1.75/1.66; 2006 - 2.44/0.93; 2009 - 2.60/0.81), than over finer-textured soils (Stagnic Cambisols and Haplic Stagnosols), namely: 2004 - 2.92/0.97; 2006 - 3.06/0.44; 2009 - 3.42/0.39). When the transpiration was not limited by soil water deficit, it acted as an equalizing factor smoothing down evapotranspiration from heterogeneous soil areas, whereby the effect of the soil physical properties was masked. With regard to soil water regime and evapotranspiration, the tile-drained Stagnic Cambisol lands behaved similarly as non-drained Haplic Cambisols. The effects of land use and of the terrain relief position could not be tracked independently, because the permanent grassland was situated in the wetter and texturally heavier parts of the catchment and the positions of the recharge/discharge zone coincided with the positions of texturally lighter/heavier soils, respectively.
abstractGer	Physical properties of soils have a significant influence on their water regime and should be considered when selecting suitable agricultural crops for particular sites, taking into account the crop productivity and its water requirements. Mean daily rates of actual evapotranspiration (ETa) were obtained by collation of measured or otherwise estimated 10-min values for the years 2004, 2006 and 2009 for a partially tile-drained agricultural experimental catchment in the Bohemo-Moravian Highland (Czech Republic). ETa was measured using the Bowen ratio (β) and energy balance (BREB) method at four weather stations located on different soil types (Stagnosols, Cambisols) and terrain relief positions (defined with respect to the groundwater recharge and discharge zones) over different crops (cereals, oil rape and permanent grassland). A systematic influence of soil properties on the evapotranspiration rate was more pronounced during the periods of limited transpiration (soil drought, crop maturity), when the average daily ETa was significantly lower and the corresponding β significantly higher over coarser-textured soils (shallow Haplic Cambisols), namely (year-ETa (mm/day)/β): 2004 - 1.75/1.66; 2006 - 2.44/0.93; 2009 - 2.60/0.81), than over finer-textured soils (Stagnic Cambisols and Haplic Stagnosols), namely: 2004 - 2.92/0.97; 2006 - 3.06/0.44; 2009 - 3.42/0.39). When the transpiration was not limited by soil water deficit, it acted as an equalizing factor smoothing down evapotranspiration from heterogeneous soil areas, whereby the effect of the soil physical properties was masked. With regard to soil water regime and evapotranspiration, the tile-drained Stagnic Cambisol lands behaved similarly as non-drained Haplic Cambisols. The effects of land use and of the terrain relief position could not be tracked independently, because the permanent grassland was situated in the wetter and texturally heavier parts of the catchment and the positions of the recharge/discharge zone coincided with the positions of texturally lighter/heavier soils, respectively.
abstract_unstemmed	Physical properties of soils have a significant influence on their water regime and should be considered when selecting suitable agricultural crops for particular sites, taking into account the crop productivity and its water requirements. Mean daily rates of actual evapotranspiration (ETa) were obtained by collation of measured or otherwise estimated 10-min values for the years 2004, 2006 and 2009 for a partially tile-drained agricultural experimental catchment in the Bohemo-Moravian Highland (Czech Republic). ETa was measured using the Bowen ratio (β) and energy balance (BREB) method at four weather stations located on different soil types (Stagnosols, Cambisols) and terrain relief positions (defined with respect to the groundwater recharge and discharge zones) over different crops (cereals, oil rape and permanent grassland). A systematic influence of soil properties on the evapotranspiration rate was more pronounced during the periods of limited transpiration (soil drought, crop maturity), when the average daily ETa was significantly lower and the corresponding β significantly higher over coarser-textured soils (shallow Haplic Cambisols), namely (year-ETa (mm/day)/β): 2004 - 1.75/1.66; 2006 - 2.44/0.93; 2009 - 2.60/0.81), than over finer-textured soils (Stagnic Cambisols and Haplic Stagnosols), namely: 2004 - 2.92/0.97; 2006 - 3.06/0.44; 2009 - 3.42/0.39). When the transpiration was not limited by soil water deficit, it acted as an equalizing factor smoothing down evapotranspiration from heterogeneous soil areas, whereby the effect of the soil physical properties was masked. With regard to soil water regime and evapotranspiration, the tile-drained Stagnic Cambisol lands behaved similarly as non-drained Haplic Cambisols. The effects of land use and of the terrain relief position could not be tracked independently, because the permanent grassland was situated in the wetter and texturally heavier parts of the catchment and the positions of the recharge/discharge zone coincided with the positions of texturally lighter/heavier soils, respectively.
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title_short	Actual evapotranspiration from partially tile-drained fields as influenced by soil properties, terrain and crop
url	https://doi.org/10.17221/20/2010-SWR https://doaj.org/article/781481c2f3124512b004ef373e776380 https://swr.agriculturejournals.cz/artkey/swr-201103-0003_actual-evapotranspiration-from-partially-tile-drained-fields-as-influenced-by-soil-properties-terrain-and-crop.php https://doaj.org/toc/1801-5395 https://doaj.org/toc/1805-9384
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up_date	2024-07-03T13:58:24.542Z
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