Water infiltration affected by different land use types and soil texture in temperate climate
Аутори
Gajić, BoškoKresović, Branka
Životić, Ljubomir
Dugalić, Goran
Tomić, Zorica
Sredojević, Zorica
Конференцијски прилог (Објављена верзија)
Метаподаци
Приказ свих података о документуАпстракт
Surface soil hydrological properties like water infiltration and hydraulic conductivity have important
consequences for hydrological properties of soils in river basins and their knowledge is needed for
sound land management, as well as flood risk prevention. They are very dynamic properties due to
varying land use management practices. The objective of this study was to evaluate the effects of two land uses (native meadow and arable) on surface (0–30 cm) infiltration characteristics of a silty clay loam and sandy loam soils at three sites in the Kolubara river valley and the Nišava river valley, respectivelly, with temperate climate, Serbia. A site consisted of two adjacent but different land uses on the same soil types. For each land use, water infiltration rates were measured in triplicate using double ring infiltrometer. Particle size distribution, bulk density and soil organic matter content of the surface soil were determined. Experimental measurements in the field indicated t...hat treatments significantly influenced water infiltration characteristics on both locations. At both site the infiltration rates showed a decrease as a function of elapsed time. Steady state infiltration rate and cumulative infiltration of sandy loam-textured soils under the meadows were much lower than that for the arable soils. By contrast, the infiltration capacity and cumulative infiltration of silty clay loam soils under the meadows was significantly (P < 0.05) higher compared to arable soils. Increase in infiltration capacity of arable soils were related to decrease in bulk density. In addition, in tilled sandy loam soil infiltration was much higher than in silty clay loam soil. However, infiltration in a silty clay loam under meadow was lower compared with sandy loam soil. According to the results of our study it could be concluded that the land use change infiltration properties of surface soil and consequently may alter the water balance of the area by
changing the amount of surface runoff and soil water retention. Knowledge of how management
practices affect infiltration capacity can aid growers in reducing soil quality and degradation.
Кључне речи:
vegetation change / meadow / arable land / Fluvisols / surface soilИзвор:
2nd International and 14th National Congress of Soil Science Society of Serbia "Solutions and Projections for Sustainable Soil Management", Novi Sad, Serbia, 2017, 228-234Издавач:
- Srpsko društvo za proučavanje zemljišta
Финансирање / пројекти:
- Идентификација специфичних гена за терапију канцера (RS-MESTD-MPN2006-2010-143009)
Институција/група
Poljoprivredni fakultetTY - CONF AU - Gajić, Boško AU - Kresović, Branka AU - Životić, Ljubomir AU - Dugalić, Goran AU - Tomić, Zorica AU - Sredojević, Zorica PY - 2017 UR - http://aspace.agrif.bg.ac.rs/handle/123456789/6752 AB - Surface soil hydrological properties like water infiltration and hydraulic conductivity have important consequences for hydrological properties of soils in river basins and their knowledge is needed for sound land management, as well as flood risk prevention. They are very dynamic properties due to varying land use management practices. The objective of this study was to evaluate the effects of two land uses (native meadow and arable) on surface (0–30 cm) infiltration characteristics of a silty clay loam and sandy loam soils at three sites in the Kolubara river valley and the Nišava river valley, respectivelly, with temperate climate, Serbia. A site consisted of two adjacent but different land uses on the same soil types. For each land use, water infiltration rates were measured in triplicate using double ring infiltrometer. Particle size distribution, bulk density and soil organic matter content of the surface soil were determined. Experimental measurements in the field indicated that treatments significantly influenced water infiltration characteristics on both locations. At both site the infiltration rates showed a decrease as a function of elapsed time. Steady state infiltration rate and cumulative infiltration of sandy loam-textured soils under the meadows were much lower than that for the arable soils. By contrast, the infiltration capacity and cumulative infiltration of silty clay loam soils under the meadows was significantly (P < 0.05) higher compared to arable soils. Increase in infiltration capacity of arable soils were related to decrease in bulk density. In addition, in tilled sandy loam soil infiltration was much higher than in silty clay loam soil. However, infiltration in a silty clay loam under meadow was lower compared with sandy loam soil. According to the results of our study it could be concluded that the land use change infiltration properties of surface soil and consequently may alter the water balance of the area by changing the amount of surface runoff and soil water retention. Knowledge of how management practices affect infiltration capacity can aid growers in reducing soil quality and degradation. PB - Srpsko društvo za proučavanje zemljišta C3 - 2nd International and 14th National Congress of Soil Science Society of Serbia "Solutions and Projections for Sustainable Soil Management", Novi Sad, Serbia T1 - Water infiltration affected by different land use types and soil texture in temperate climate EP - 234 SP - 228 UR - https://hdl.handle.net/21.15107/rcub_agrospace_6752 ER -
@conference{ author = "Gajić, Boško and Kresović, Branka and Životić, Ljubomir and Dugalić, Goran and Tomić, Zorica and Sredojević, Zorica", year = "2017", abstract = "Surface soil hydrological properties like water infiltration and hydraulic conductivity have important consequences for hydrological properties of soils in river basins and their knowledge is needed for sound land management, as well as flood risk prevention. They are very dynamic properties due to varying land use management practices. The objective of this study was to evaluate the effects of two land uses (native meadow and arable) on surface (0–30 cm) infiltration characteristics of a silty clay loam and sandy loam soils at three sites in the Kolubara river valley and the Nišava river valley, respectivelly, with temperate climate, Serbia. A site consisted of two adjacent but different land uses on the same soil types. For each land use, water infiltration rates were measured in triplicate using double ring infiltrometer. Particle size distribution, bulk density and soil organic matter content of the surface soil were determined. Experimental measurements in the field indicated that treatments significantly influenced water infiltration characteristics on both locations. At both site the infiltration rates showed a decrease as a function of elapsed time. Steady state infiltration rate and cumulative infiltration of sandy loam-textured soils under the meadows were much lower than that for the arable soils. By contrast, the infiltration capacity and cumulative infiltration of silty clay loam soils under the meadows was significantly (P < 0.05) higher compared to arable soils. Increase in infiltration capacity of arable soils were related to decrease in bulk density. In addition, in tilled sandy loam soil infiltration was much higher than in silty clay loam soil. However, infiltration in a silty clay loam under meadow was lower compared with sandy loam soil. According to the results of our study it could be concluded that the land use change infiltration properties of surface soil and consequently may alter the water balance of the area by changing the amount of surface runoff and soil water retention. Knowledge of how management practices affect infiltration capacity can aid growers in reducing soil quality and degradation.", publisher = "Srpsko društvo za proučavanje zemljišta", journal = "2nd International and 14th National Congress of Soil Science Society of Serbia "Solutions and Projections for Sustainable Soil Management", Novi Sad, Serbia", title = "Water infiltration affected by different land use types and soil texture in temperate climate", pages = "234-228", url = "https://hdl.handle.net/21.15107/rcub_agrospace_6752" }
Gajić, B., Kresović, B., Životić, L., Dugalić, G., Tomić, Z.,& Sredojević, Z.. (2017). Water infiltration affected by different land use types and soil texture in temperate climate. in 2nd International and 14th National Congress of Soil Science Society of Serbia "Solutions and Projections for Sustainable Soil Management", Novi Sad, Serbia Srpsko društvo za proučavanje zemljišta., 228-234. https://hdl.handle.net/21.15107/rcub_agrospace_6752
Gajić B, Kresović B, Životić L, Dugalić G, Tomić Z, Sredojević Z. Water infiltration affected by different land use types and soil texture in temperate climate. in 2nd International and 14th National Congress of Soil Science Society of Serbia "Solutions and Projections for Sustainable Soil Management", Novi Sad, Serbia. 2017;:228-234. https://hdl.handle.net/21.15107/rcub_agrospace_6752 .
Gajić, Boško, Kresović, Branka, Životić, Ljubomir, Dugalić, Goran, Tomić, Zorica, Sredojević, Zorica, "Water infiltration affected by different land use types and soil texture in temperate climate" in 2nd International and 14th National Congress of Soil Science Society of Serbia "Solutions and Projections for Sustainable Soil Management", Novi Sad, Serbia (2017):228-234, https://hdl.handle.net/21.15107/rcub_agrospace_6752 .