Long-term analysis of soil water regime and nitrate dynamics at agricultural experimental site : field-scale monitoring and numerical modeling using HYDRUS-1D
- Krevh, Vedran, Filipović, Lana, Petošić, Dragutin, Mustać, Ivica, Bogunović, Igor, Butorac, Jaminka, Kisić, Ivica, Defterdarović, Jasmina, Nakić, Zoran, Kovač, Zoran, Pereira, Paulo, He, Hailong, Chen, Rui, Toor, Gurpal, Versini, Antoine, Baumgartl, Thomas, Filipović, Vilim
- Authors: Krevh, Vedran , Filipović, Lana , Petošić, Dragutin , Mustać, Ivica , Bogunović, Igor , Butorac, Jaminka , Kisić, Ivica , Defterdarović, Jasmina , Nakić, Zoran , Kovač, Zoran , Pereira, Paulo , He, Hailong , Chen, Rui , Toor, Gurpal , Versini, Antoine , Baumgartl, Thomas , Filipović, Vilim
- Date: 2023
- Type: Text , Journal article
- Relation: Agricultural Water Management Vol. 275, no. (2023), p.
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- Description: Intensive agricultural practices increase agrochemical pollution, particularly nitrogen (N) based fertilizers, which present an environmental risk. This study aims to evaluate long-term (2009–2020) data on soil water regime and nitrate dynamics at an agricultural experimental site on fine-textured soils and to better understand the implications of N management in relation to groundwater pollution. The field site is located in the Biđ field (eastern Croatia), in the proximity of the Sava river. Zero-tension lysimeters were installed at six selected locations. Lysimeters were used to monitor the water regime, i.e., outflows in which nitrate concentration was measured, while additional soil-water samples were collected via 4 and 15-meter-deep monitoring wells. Soil hydraulic parameters were estimated by combining the laboratory measurements, and estimation in RETC software. Water regime and nitrate leaching in lysimeters were simulated using HYDRUS-1D for each year to allow crop rotation and to evaluate their effects individually. The HYDRUS-1D model successfully reproduced lysimeter outflows and nitrate dynamics, which was confirmed with high R2 values (water: 93% above 0.7, and nitrate: 73% above 0.7) indicating the good performance of the model simulating nitrification chain reactions. Principal component analysis (PCA) was performed to identify the relationships among all soil properties and environmental characteristics. The results showed the complex interaction of soil hydraulic properties, precipitation patterns, plant uptake, and N application. All locations have a decreasing trend of nitrate leaching over the investigation period. Most of the lysimeter outflows and elevated nitrate concentrations were connected to the wet period of the year when the soil was saturated, and evapotranspiration was low. The results of this study show that it is important to optimize N fertilizer applications for each particular environmental condition to reduce nitrate loss. The study indicates the importance of long-term field studies, key for agro-hydrological modeling and the improvement of agricultural practices. © 2022 The Authors
- Authors: Krevh, Vedran , Filipović, Lana , Petošić, Dragutin , Mustać, Ivica , Bogunović, Igor , Butorac, Jaminka , Kisić, Ivica , Defterdarović, Jasmina , Nakić, Zoran , Kovač, Zoran , Pereira, Paulo , He, Hailong , Chen, Rui , Toor, Gurpal , Versini, Antoine , Baumgartl, Thomas , Filipović, Vilim
- Date: 2023
- Type: Text , Journal article
- Relation: Agricultural Water Management Vol. 275, no. (2023), p.
- Full Text:
- Reviewed:
- Description: Intensive agricultural practices increase agrochemical pollution, particularly nitrogen (N) based fertilizers, which present an environmental risk. This study aims to evaluate long-term (2009–2020) data on soil water regime and nitrate dynamics at an agricultural experimental site on fine-textured soils and to better understand the implications of N management in relation to groundwater pollution. The field site is located in the Biđ field (eastern Croatia), in the proximity of the Sava river. Zero-tension lysimeters were installed at six selected locations. Lysimeters were used to monitor the water regime, i.e., outflows in which nitrate concentration was measured, while additional soil-water samples were collected via 4 and 15-meter-deep monitoring wells. Soil hydraulic parameters were estimated by combining the laboratory measurements, and estimation in RETC software. Water regime and nitrate leaching in lysimeters were simulated using HYDRUS-1D for each year to allow crop rotation and to evaluate their effects individually. The HYDRUS-1D model successfully reproduced lysimeter outflows and nitrate dynamics, which was confirmed with high R2 values (water: 93% above 0.7, and nitrate: 73% above 0.7) indicating the good performance of the model simulating nitrification chain reactions. Principal component analysis (PCA) was performed to identify the relationships among all soil properties and environmental characteristics. The results showed the complex interaction of soil hydraulic properties, precipitation patterns, plant uptake, and N application. All locations have a decreasing trend of nitrate leaching over the investigation period. Most of the lysimeter outflows and elevated nitrate concentrations were connected to the wet period of the year when the soil was saturated, and evapotranspiration was low. The results of this study show that it is important to optimize N fertilizer applications for each particular environmental condition to reduce nitrate loss. The study indicates the importance of long-term field studies, key for agro-hydrological modeling and the improvement of agricultural practices. © 2022 The Authors
Characterising soil physical properties of selected temperate highland peat swamps on sandstone in the Sydney basin bioregion
- Shaygan, Mandana, Baumgartl, Thomas, McIntyre, Neil
- Authors: Shaygan, Mandana , Baumgartl, Thomas , McIntyre, Neil
- Date: 2022
- Type: Text , Journal article
- Relation: Journal of Hydrology: Regional Studies Vol. 40, no. (2022), p.
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- Reviewed:
- Description: Study region: Sydney Basin, New South Wales, Australia. Study focus: Some of Temperate Highland Peat Swamps on Sandstone of Sydney Basin overlie existing underground mining areas, which may impact the hydrological fluxes into and out of the swamps. Understanding and predicting these potential impacts and their consequences for swamps’ vegetation requires knowledge of the relevant physical properties of the soil, however such knowledge is almost completely absent from the literature. This study addresses this gap, and provides new insight into the degree and nature of variability between swamp sites, and between groups of swamps, the soil properties controlling these variabilities and the classification of these swamps in the context of peatland. Soil samples were collected up to a depth of 750 mm from ten sites in Upper Nepean and Newnes Plateau swamps. Samples were analysed for organic matter, bulk density, texture, saturated hydraulic conductivity and water retention characteristics. New hydrological insights: Not only the organic matter, but also bulk density and sand content control soil physical properties of the swamps. Soil properties vary between swamps; however, the variabilities were not large relative to those found in peatlands globally. These THPSS of the Sydney Basin cannot be classified as peatland and so their soil parameters cannot be estimated through the generalisation of peatland soil physical properties. It is concluded that the insights into soil properties provide new scope for developing hydrological models to assist in hydrological and ecological impacts analysis of the swamps. © 2022 The Authors
- Authors: Shaygan, Mandana , Baumgartl, Thomas , McIntyre, Neil
- Date: 2022
- Type: Text , Journal article
- Relation: Journal of Hydrology: Regional Studies Vol. 40, no. (2022), p.
- Full Text:
- Reviewed:
- Description: Study region: Sydney Basin, New South Wales, Australia. Study focus: Some of Temperate Highland Peat Swamps on Sandstone of Sydney Basin overlie existing underground mining areas, which may impact the hydrological fluxes into and out of the swamps. Understanding and predicting these potential impacts and their consequences for swamps’ vegetation requires knowledge of the relevant physical properties of the soil, however such knowledge is almost completely absent from the literature. This study addresses this gap, and provides new insight into the degree and nature of variability between swamp sites, and between groups of swamps, the soil properties controlling these variabilities and the classification of these swamps in the context of peatland. Soil samples were collected up to a depth of 750 mm from ten sites in Upper Nepean and Newnes Plateau swamps. Samples were analysed for organic matter, bulk density, texture, saturated hydraulic conductivity and water retention characteristics. New hydrological insights: Not only the organic matter, but also bulk density and sand content control soil physical properties of the swamps. Soil properties vary between swamps; however, the variabilities were not large relative to those found in peatlands globally. These THPSS of the Sydney Basin cannot be classified as peatland and so their soil parameters cannot be estimated through the generalisation of peatland soil physical properties. It is concluded that the insights into soil properties provide new scope for developing hydrological models to assist in hydrological and ecological impacts analysis of the swamps. © 2022 The Authors
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