Short-Term Impact of Tillage on Soil and the Hydrological Response within a Fig (<i<Ficus Carica</i<) Orchard in Croatia
Tillage is well known to have impacts on soil properties and hydrological responses. This work aims to study the short-term impacts of tillage (0–3 months) on soil and hydrological responses in fig orchards located in Croatia. Understanding the soil hydrological response in the study area is crucial...
Ausführliche Beschreibung
Autor*in: |
Leon Josip Telak [verfasserIn] Paulo Pereira [verfasserIn] Carla S. S. Ferreira [verfasserIn] Vilim Filipovic [verfasserIn] Lana Filipovic [verfasserIn] Igor Bogunovic [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2020 |
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Schlagwörter: |
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Übergeordnetes Werk: |
In: Water - MDPI AG, 2010, 12(2020), 11, p 3295 |
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Übergeordnetes Werk: |
volume:12 ; year:2020 ; number:11, p 3295 |
Links: |
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DOI / URN: |
10.3390/w12113295 |
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Katalog-ID: |
DOAJ039591301 |
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10.3390/w12113295 doi (DE-627)DOAJ039591301 (DE-599)DOAJd592ab2bcf0c4da6862b6828e4da6838 DE-627 ger DE-627 rakwb eng TC1-978 TD201-500 Leon Josip Telak verfasserin aut Short-Term Impact of Tillage on Soil and the Hydrological Response within a Fig (<i<Ficus Carica</i<) Orchard in Croatia 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Tillage is well known to have impacts on soil properties and hydrological responses. This work aims to study the short-term impacts of tillage (0–3 months) on soil and hydrological responses in fig orchards located in Croatia. Understanding the soil hydrological response in the study area is crucial for soil management due to frequent autumn floods. The hydrological response was investigated using rainfall simulation experiments (58 mm h<sup<−1</sup<, for 30 min, over 0.785 m<sup<2</sup< plots). The results show that the bulk density was significantly higher 3 months after tillage than at 0 and 1 months. The water holding capacity and amount of soil organic matter decreased with time. The water runoff and phosphorous loss (P loss) increased over time. The sediment concentration (SC) was significantly higher 3 months after tillage than in the previous monitoring periods, while sediment loss (SL) and carbon loss (C loss) were significantly lower 0 months after tillage than 3 months after tillage. Overall, there was an increase in soil erodibility with time (high SC, SL, C loss, and P loss), attributed to the precipitation patterns that increase the soil water content and therefore the hydrological response. Therefore, sustainable agricultural practices are needed to avoid sediment translocation and to mitigate floods and land degradation. soil properties erosion nutrient loss undeveloped soil Hydraulic engineering Water supply for domestic and industrial purposes Paulo Pereira verfasserin aut Carla S. S. Ferreira verfasserin aut Vilim Filipovic verfasserin aut Lana Filipovic verfasserin aut Igor Bogunovic verfasserin aut In Water MDPI AG, 2010 12(2020), 11, p 3295 (DE-627)611729008 (DE-600)2521238-2 20734441 nnns volume:12 year:2020 number:11, p 3295 https://doi.org/10.3390/w12113295 kostenfrei https://doaj.org/article/d592ab2bcf0c4da6862b6828e4da6838 kostenfrei https://www.mdpi.com/2073-4441/12/11/3295 kostenfrei https://doaj.org/toc/2073-4441 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 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_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4367 GBV_ILN_4700 AR 12 2020 11, p 3295 |
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10.3390/w12113295 doi (DE-627)DOAJ039591301 (DE-599)DOAJd592ab2bcf0c4da6862b6828e4da6838 DE-627 ger DE-627 rakwb eng TC1-978 TD201-500 Leon Josip Telak verfasserin aut Short-Term Impact of Tillage on Soil and the Hydrological Response within a Fig (<i<Ficus Carica</i<) Orchard in Croatia 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Tillage is well known to have impacts on soil properties and hydrological responses. This work aims to study the short-term impacts of tillage (0–3 months) on soil and hydrological responses in fig orchards located in Croatia. Understanding the soil hydrological response in the study area is crucial for soil management due to frequent autumn floods. The hydrological response was investigated using rainfall simulation experiments (58 mm h<sup<−1</sup<, for 30 min, over 0.785 m<sup<2</sup< plots). The results show that the bulk density was significantly higher 3 months after tillage than at 0 and 1 months. The water holding capacity and amount of soil organic matter decreased with time. The water runoff and phosphorous loss (P loss) increased over time. The sediment concentration (SC) was significantly higher 3 months after tillage than in the previous monitoring periods, while sediment loss (SL) and carbon loss (C loss) were significantly lower 0 months after tillage than 3 months after tillage. Overall, there was an increase in soil erodibility with time (high SC, SL, C loss, and P loss), attributed to the precipitation patterns that increase the soil water content and therefore the hydrological response. Therefore, sustainable agricultural practices are needed to avoid sediment translocation and to mitigate floods and land degradation. soil properties erosion nutrient loss undeveloped soil Hydraulic engineering Water supply for domestic and industrial purposes Paulo Pereira verfasserin aut Carla S. S. Ferreira verfasserin aut Vilim Filipovic verfasserin aut Lana Filipovic verfasserin aut Igor Bogunovic verfasserin aut In Water MDPI AG, 2010 12(2020), 11, p 3295 (DE-627)611729008 (DE-600)2521238-2 20734441 nnns volume:12 year:2020 number:11, p 3295 https://doi.org/10.3390/w12113295 kostenfrei https://doaj.org/article/d592ab2bcf0c4da6862b6828e4da6838 kostenfrei https://www.mdpi.com/2073-4441/12/11/3295 kostenfrei https://doaj.org/toc/2073-4441 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 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_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4367 GBV_ILN_4700 AR 12 2020 11, p 3295 |
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Short-Term Impact of Tillage on Soil and the Hydrological Response within a Fig (<i<Ficus Carica</i<) Orchard in Croatia |
abstract |
Tillage is well known to have impacts on soil properties and hydrological responses. This work aims to study the short-term impacts of tillage (0–3 months) on soil and hydrological responses in fig orchards located in Croatia. Understanding the soil hydrological response in the study area is crucial for soil management due to frequent autumn floods. The hydrological response was investigated using rainfall simulation experiments (58 mm h<sup<−1</sup<, for 30 min, over 0.785 m<sup<2</sup< plots). The results show that the bulk density was significantly higher 3 months after tillage than at 0 and 1 months. The water holding capacity and amount of soil organic matter decreased with time. The water runoff and phosphorous loss (P loss) increased over time. The sediment concentration (SC) was significantly higher 3 months after tillage than in the previous monitoring periods, while sediment loss (SL) and carbon loss (C loss) were significantly lower 0 months after tillage than 3 months after tillage. Overall, there was an increase in soil erodibility with time (high SC, SL, C loss, and P loss), attributed to the precipitation patterns that increase the soil water content and therefore the hydrological response. Therefore, sustainable agricultural practices are needed to avoid sediment translocation and to mitigate floods and land degradation. |
abstractGer |
Tillage is well known to have impacts on soil properties and hydrological responses. This work aims to study the short-term impacts of tillage (0–3 months) on soil and hydrological responses in fig orchards located in Croatia. Understanding the soil hydrological response in the study area is crucial for soil management due to frequent autumn floods. The hydrological response was investigated using rainfall simulation experiments (58 mm h<sup<−1</sup<, for 30 min, over 0.785 m<sup<2</sup< plots). The results show that the bulk density was significantly higher 3 months after tillage than at 0 and 1 months. The water holding capacity and amount of soil organic matter decreased with time. The water runoff and phosphorous loss (P loss) increased over time. The sediment concentration (SC) was significantly higher 3 months after tillage than in the previous monitoring periods, while sediment loss (SL) and carbon loss (C loss) were significantly lower 0 months after tillage than 3 months after tillage. Overall, there was an increase in soil erodibility with time (high SC, SL, C loss, and P loss), attributed to the precipitation patterns that increase the soil water content and therefore the hydrological response. Therefore, sustainable agricultural practices are needed to avoid sediment translocation and to mitigate floods and land degradation. |
abstract_unstemmed |
Tillage is well known to have impacts on soil properties and hydrological responses. This work aims to study the short-term impacts of tillage (0–3 months) on soil and hydrological responses in fig orchards located in Croatia. Understanding the soil hydrological response in the study area is crucial for soil management due to frequent autumn floods. The hydrological response was investigated using rainfall simulation experiments (58 mm h<sup<−1</sup<, for 30 min, over 0.785 m<sup<2</sup< plots). The results show that the bulk density was significantly higher 3 months after tillage than at 0 and 1 months. The water holding capacity and amount of soil organic matter decreased with time. The water runoff and phosphorous loss (P loss) increased over time. The sediment concentration (SC) was significantly higher 3 months after tillage than in the previous monitoring periods, while sediment loss (SL) and carbon loss (C loss) were significantly lower 0 months after tillage than 3 months after tillage. Overall, there was an increase in soil erodibility with time (high SC, SL, C loss, and P loss), attributed to the precipitation patterns that increase the soil water content and therefore the hydrological response. Therefore, sustainable agricultural practices are needed to avoid sediment translocation and to mitigate floods and land degradation. |
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