Effects of hydromorphology and riparian vegetation on the sediment quality of agricultural low-order streams: consequences for stream restoration
Abstract Intensive agricultural land use imposes multiple pressures on streams. More specifically, the loading of streams with nutrient-enriched soil from surrounding crop fields may deteriorate the sediment quality. The current study aimed to find out whether stream restoration may be an effective...
Ausführliche Beschreibung
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| Autor*in: |
Teufl, Bernadette [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2012 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag 2012 |
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| Übergeordnetes Werk: |
Enthalten in: Environmental science and pollution research - Springer-Verlag, 1994, 20(2012), 3 vom: 04. Sept., Seite 1781-1793 |
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| Übergeordnetes Werk: |
volume:20 ; year:2012 ; number:3 ; day:04 ; month:09 ; pages:1781-1793 |
| Links: |
|---|
| DOI / URN: |
10.1007/s11356-012-1135-2 |
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OLC2040415513 |
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| 245 | 1 | 0 | |a Effects of hydromorphology and riparian vegetation on the sediment quality of agricultural low-order streams: consequences for stream restoration |
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| 520 | |a Abstract Intensive agricultural land use imposes multiple pressures on streams. More specifically, the loading of streams with nutrient-enriched soil from surrounding crop fields may deteriorate the sediment quality. The current study aimed to find out whether stream restoration may be an effective tool to improve the sediment quality of agricultural headwater streams. We compared nine stream reaches representing different morphological types (forested meandering reaches vs. deforested channelized reaches) regarding sediment structure, sedimentary nutrient and organic matter concentrations, and benthic microbial respiration. Main differences among reach types were found in grain sizes. Meandering reaches featured larger mean grain sizes (50–70 μm) and a thicker oxygenated surface layer (8 cm) than channelized reaches (40 μm, 5 cm). Total phosphorous amounted for up to 1,500 μg $ g^{−1} $ DW at retentive channelized reaches and 850–1,050 μg $ g^{−1} $ DW at the others. While N-$ NH_{4} $ accumulated in the sediments (60–180 μg $ g^{−1} $ DW), N-$ NO_{3} $ concentrations were generally low (2–5 μg $ g^{−1} $ DW). Benthic respiration was high at all sites (10–20 g $ O_{2} $ $ m^{−2} $ $ day^{−1} $). Our study shows that both hydromorphology and bank vegetation may influence the sediment quality of agricultural streams, though effects are often small and spatially restricted. To increase the efficiency of stream restoration in agricultural landscapes, nutrient and sediment delivery to stream channels need to be minimized by mitigating soil erosion in the catchment. | ||
| 650 | 4 | |a Agricultural streams | |
| 650 | 4 | |a Sediment structure | |
| 650 | 4 | |a Sedimentary nutrients | |
| 650 | 4 | |a Benthic microbial respiration | |
| 650 | 4 | |a Hydromorphology | |
| 650 | 4 | |a Stream restoration | |
| 700 | 1 | |a Weigelhofer, Gabriele |4 aut | |
| 700 | 1 | |a Fuchsberger, Jennifer |4 aut | |
| 700 | 1 | |a Hein, Thomas |4 aut | |
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10.1007/s11356-012-1135-2 doi (DE-627)OLC2040415513 (DE-He213)s11356-012-1135-2-p DE-627 ger DE-627 rakwb eng 570 360 333.7 VZ 690 333.7 540 VZ BIODIV DE-30 fid Teufl, Bernadette verfasserin aut Effects of hydromorphology and riparian vegetation on the sediment quality of agricultural low-order streams: consequences for stream restoration 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2012 Abstract Intensive agricultural land use imposes multiple pressures on streams. More specifically, the loading of streams with nutrient-enriched soil from surrounding crop fields may deteriorate the sediment quality. The current study aimed to find out whether stream restoration may be an effective tool to improve the sediment quality of agricultural headwater streams. We compared nine stream reaches representing different morphological types (forested meandering reaches vs. deforested channelized reaches) regarding sediment structure, sedimentary nutrient and organic matter concentrations, and benthic microbial respiration. Main differences among reach types were found in grain sizes. Meandering reaches featured larger mean grain sizes (50–70 μm) and a thicker oxygenated surface layer (8 cm) than channelized reaches (40 μm, 5 cm). Total phosphorous amounted for up to 1,500 μg $ g^{−1} $ DW at retentive channelized reaches and 850–1,050 μg $ g^{−1} $ DW at the others. While N-$ NH_{4} $ accumulated in the sediments (60–180 μg $ g^{−1} $ DW), N-$ NO_{3} $ concentrations were generally low (2–5 μg $ g^{−1} $ DW). Benthic respiration was high at all sites (10–20 g $ O_{2} $ $ m^{−2} $ $ day^{−1} $). Our study shows that both hydromorphology and bank vegetation may influence the sediment quality of agricultural streams, though effects are often small and spatially restricted. To increase the efficiency of stream restoration in agricultural landscapes, nutrient and sediment delivery to stream channels need to be minimized by mitigating soil erosion in the catchment. Agricultural streams Sediment structure Sedimentary nutrients Benthic microbial respiration Hydromorphology Stream restoration Weigelhofer, Gabriele aut Fuchsberger, Jennifer aut Hein, Thomas aut Enthalten in Environmental science and pollution research Springer-Verlag, 1994 20(2012), 3 vom: 04. Sept., Seite 1781-1793 (DE-627)171335805 (DE-600)1178791-0 (DE-576)038875101 0944-1344 nnns volume:20 year:2012 number:3 day:04 month:09 pages:1781-1793 https://doi.org/10.1007/s11356-012-1135-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-FOR SSG-OLC-DE-84 GBV_ILN_70 GBV_ILN_183 GBV_ILN_252 GBV_ILN_267 GBV_ILN_370 GBV_ILN_2018 GBV_ILN_2057 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4219 GBV_ILN_4266 GBV_ILN_4277 GBV_ILN_4302 AR 20 2012 3 04 09 1781-1793 |
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10.1007/s11356-012-1135-2 doi (DE-627)OLC2040415513 (DE-He213)s11356-012-1135-2-p DE-627 ger DE-627 rakwb eng 570 360 333.7 VZ 690 333.7 540 VZ BIODIV DE-30 fid Teufl, Bernadette verfasserin aut Effects of hydromorphology and riparian vegetation on the sediment quality of agricultural low-order streams: consequences for stream restoration 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2012 Abstract Intensive agricultural land use imposes multiple pressures on streams. More specifically, the loading of streams with nutrient-enriched soil from surrounding crop fields may deteriorate the sediment quality. The current study aimed to find out whether stream restoration may be an effective tool to improve the sediment quality of agricultural headwater streams. We compared nine stream reaches representing different morphological types (forested meandering reaches vs. deforested channelized reaches) regarding sediment structure, sedimentary nutrient and organic matter concentrations, and benthic microbial respiration. Main differences among reach types were found in grain sizes. Meandering reaches featured larger mean grain sizes (50–70 μm) and a thicker oxygenated surface layer (8 cm) than channelized reaches (40 μm, 5 cm). Total phosphorous amounted for up to 1,500 μg $ g^{−1} $ DW at retentive channelized reaches and 850–1,050 μg $ g^{−1} $ DW at the others. While N-$ NH_{4} $ accumulated in the sediments (60–180 μg $ g^{−1} $ DW), N-$ NO_{3} $ concentrations were generally low (2–5 μg $ g^{−1} $ DW). Benthic respiration was high at all sites (10–20 g $ O_{2} $ $ m^{−2} $ $ day^{−1} $). Our study shows that both hydromorphology and bank vegetation may influence the sediment quality of agricultural streams, though effects are often small and spatially restricted. To increase the efficiency of stream restoration in agricultural landscapes, nutrient and sediment delivery to stream channels need to be minimized by mitigating soil erosion in the catchment. Agricultural streams Sediment structure Sedimentary nutrients Benthic microbial respiration Hydromorphology Stream restoration Weigelhofer, Gabriele aut Fuchsberger, Jennifer aut Hein, Thomas aut Enthalten in Environmental science and pollution research Springer-Verlag, 1994 20(2012), 3 vom: 04. Sept., Seite 1781-1793 (DE-627)171335805 (DE-600)1178791-0 (DE-576)038875101 0944-1344 nnns volume:20 year:2012 number:3 day:04 month:09 pages:1781-1793 https://doi.org/10.1007/s11356-012-1135-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-FOR SSG-OLC-DE-84 GBV_ILN_70 GBV_ILN_183 GBV_ILN_252 GBV_ILN_267 GBV_ILN_370 GBV_ILN_2018 GBV_ILN_2057 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4219 GBV_ILN_4266 GBV_ILN_4277 GBV_ILN_4302 AR 20 2012 3 04 09 1781-1793 |
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10.1007/s11356-012-1135-2 doi (DE-627)OLC2040415513 (DE-He213)s11356-012-1135-2-p DE-627 ger DE-627 rakwb eng 570 360 333.7 VZ 690 333.7 540 VZ BIODIV DE-30 fid Teufl, Bernadette verfasserin aut Effects of hydromorphology and riparian vegetation on the sediment quality of agricultural low-order streams: consequences for stream restoration 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2012 Abstract Intensive agricultural land use imposes multiple pressures on streams. More specifically, the loading of streams with nutrient-enriched soil from surrounding crop fields may deteriorate the sediment quality. The current study aimed to find out whether stream restoration may be an effective tool to improve the sediment quality of agricultural headwater streams. We compared nine stream reaches representing different morphological types (forested meandering reaches vs. deforested channelized reaches) regarding sediment structure, sedimentary nutrient and organic matter concentrations, and benthic microbial respiration. Main differences among reach types were found in grain sizes. Meandering reaches featured larger mean grain sizes (50–70 μm) and a thicker oxygenated surface layer (8 cm) than channelized reaches (40 μm, 5 cm). Total phosphorous amounted for up to 1,500 μg $ g^{−1} $ DW at retentive channelized reaches and 850–1,050 μg $ g^{−1} $ DW at the others. While N-$ NH_{4} $ accumulated in the sediments (60–180 μg $ g^{−1} $ DW), N-$ NO_{3} $ concentrations were generally low (2–5 μg $ g^{−1} $ DW). Benthic respiration was high at all sites (10–20 g $ O_{2} $ $ m^{−2} $ $ day^{−1} $). Our study shows that both hydromorphology and bank vegetation may influence the sediment quality of agricultural streams, though effects are often small and spatially restricted. To increase the efficiency of stream restoration in agricultural landscapes, nutrient and sediment delivery to stream channels need to be minimized by mitigating soil erosion in the catchment. Agricultural streams Sediment structure Sedimentary nutrients Benthic microbial respiration Hydromorphology Stream restoration Weigelhofer, Gabriele aut Fuchsberger, Jennifer aut Hein, Thomas aut Enthalten in Environmental science and pollution research Springer-Verlag, 1994 20(2012), 3 vom: 04. Sept., Seite 1781-1793 (DE-627)171335805 (DE-600)1178791-0 (DE-576)038875101 0944-1344 nnns volume:20 year:2012 number:3 day:04 month:09 pages:1781-1793 https://doi.org/10.1007/s11356-012-1135-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-FOR SSG-OLC-DE-84 GBV_ILN_70 GBV_ILN_183 GBV_ILN_252 GBV_ILN_267 GBV_ILN_370 GBV_ILN_2018 GBV_ILN_2057 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4219 GBV_ILN_4266 GBV_ILN_4277 GBV_ILN_4302 AR 20 2012 3 04 09 1781-1793 |
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10.1007/s11356-012-1135-2 doi (DE-627)OLC2040415513 (DE-He213)s11356-012-1135-2-p DE-627 ger DE-627 rakwb eng 570 360 333.7 VZ 690 333.7 540 VZ BIODIV DE-30 fid Teufl, Bernadette verfasserin aut Effects of hydromorphology and riparian vegetation on the sediment quality of agricultural low-order streams: consequences for stream restoration 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2012 Abstract Intensive agricultural land use imposes multiple pressures on streams. More specifically, the loading of streams with nutrient-enriched soil from surrounding crop fields may deteriorate the sediment quality. The current study aimed to find out whether stream restoration may be an effective tool to improve the sediment quality of agricultural headwater streams. We compared nine stream reaches representing different morphological types (forested meandering reaches vs. deforested channelized reaches) regarding sediment structure, sedimentary nutrient and organic matter concentrations, and benthic microbial respiration. Main differences among reach types were found in grain sizes. Meandering reaches featured larger mean grain sizes (50–70 μm) and a thicker oxygenated surface layer (8 cm) than channelized reaches (40 μm, 5 cm). Total phosphorous amounted for up to 1,500 μg $ g^{−1} $ DW at retentive channelized reaches and 850–1,050 μg $ g^{−1} $ DW at the others. While N-$ NH_{4} $ accumulated in the sediments (60–180 μg $ g^{−1} $ DW), N-$ NO_{3} $ concentrations were generally low (2–5 μg $ g^{−1} $ DW). Benthic respiration was high at all sites (10–20 g $ O_{2} $ $ m^{−2} $ $ day^{−1} $). Our study shows that both hydromorphology and bank vegetation may influence the sediment quality of agricultural streams, though effects are often small and spatially restricted. To increase the efficiency of stream restoration in agricultural landscapes, nutrient and sediment delivery to stream channels need to be minimized by mitigating soil erosion in the catchment. Agricultural streams Sediment structure Sedimentary nutrients Benthic microbial respiration Hydromorphology Stream restoration Weigelhofer, Gabriele aut Fuchsberger, Jennifer aut Hein, Thomas aut Enthalten in Environmental science and pollution research Springer-Verlag, 1994 20(2012), 3 vom: 04. Sept., Seite 1781-1793 (DE-627)171335805 (DE-600)1178791-0 (DE-576)038875101 0944-1344 nnns volume:20 year:2012 number:3 day:04 month:09 pages:1781-1793 https://doi.org/10.1007/s11356-012-1135-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-ARC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-FOR SSG-OLC-DE-84 GBV_ILN_70 GBV_ILN_183 GBV_ILN_252 GBV_ILN_267 GBV_ILN_370 GBV_ILN_2018 GBV_ILN_2057 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4219 GBV_ILN_4266 GBV_ILN_4277 GBV_ILN_4302 AR 20 2012 3 04 09 1781-1793 |
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Enthalten in Environmental science and pollution research 20(2012), 3 vom: 04. Sept., Seite 1781-1793 volume:20 year:2012 number:3 day:04 month:09 pages:1781-1793 |
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effects of hydromorphology and riparian vegetation on the sediment quality of agricultural low-order streams: consequences for stream restoration |
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Effects of hydromorphology and riparian vegetation on the sediment quality of agricultural low-order streams: consequences for stream restoration |
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Abstract Intensive agricultural land use imposes multiple pressures on streams. More specifically, the loading of streams with nutrient-enriched soil from surrounding crop fields may deteriorate the sediment quality. The current study aimed to find out whether stream restoration may be an effective tool to improve the sediment quality of agricultural headwater streams. We compared nine stream reaches representing different morphological types (forested meandering reaches vs. deforested channelized reaches) regarding sediment structure, sedimentary nutrient and organic matter concentrations, and benthic microbial respiration. Main differences among reach types were found in grain sizes. Meandering reaches featured larger mean grain sizes (50–70 μm) and a thicker oxygenated surface layer (8 cm) than channelized reaches (40 μm, 5 cm). Total phosphorous amounted for up to 1,500 μg $ g^{−1} $ DW at retentive channelized reaches and 850–1,050 μg $ g^{−1} $ DW at the others. While N-$ NH_{4} $ accumulated in the sediments (60–180 μg $ g^{−1} $ DW), N-$ NO_{3} $ concentrations were generally low (2–5 μg $ g^{−1} $ DW). Benthic respiration was high at all sites (10–20 g $ O_{2} $ $ m^{−2} $ $ day^{−1} $). Our study shows that both hydromorphology and bank vegetation may influence the sediment quality of agricultural streams, though effects are often small and spatially restricted. To increase the efficiency of stream restoration in agricultural landscapes, nutrient and sediment delivery to stream channels need to be minimized by mitigating soil erosion in the catchment. © Springer-Verlag 2012 |
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Abstract Intensive agricultural land use imposes multiple pressures on streams. More specifically, the loading of streams with nutrient-enriched soil from surrounding crop fields may deteriorate the sediment quality. The current study aimed to find out whether stream restoration may be an effective tool to improve the sediment quality of agricultural headwater streams. We compared nine stream reaches representing different morphological types (forested meandering reaches vs. deforested channelized reaches) regarding sediment structure, sedimentary nutrient and organic matter concentrations, and benthic microbial respiration. Main differences among reach types were found in grain sizes. Meandering reaches featured larger mean grain sizes (50–70 μm) and a thicker oxygenated surface layer (8 cm) than channelized reaches (40 μm, 5 cm). Total phosphorous amounted for up to 1,500 μg $ g^{−1} $ DW at retentive channelized reaches and 850–1,050 μg $ g^{−1} $ DW at the others. While N-$ NH_{4} $ accumulated in the sediments (60–180 μg $ g^{−1} $ DW), N-$ NO_{3} $ concentrations were generally low (2–5 μg $ g^{−1} $ DW). Benthic respiration was high at all sites (10–20 g $ O_{2} $ $ m^{−2} $ $ day^{−1} $). Our study shows that both hydromorphology and bank vegetation may influence the sediment quality of agricultural streams, though effects are often small and spatially restricted. To increase the efficiency of stream restoration in agricultural landscapes, nutrient and sediment delivery to stream channels need to be minimized by mitigating soil erosion in the catchment. © Springer-Verlag 2012 |
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Abstract Intensive agricultural land use imposes multiple pressures on streams. More specifically, the loading of streams with nutrient-enriched soil from surrounding crop fields may deteriorate the sediment quality. The current study aimed to find out whether stream restoration may be an effective tool to improve the sediment quality of agricultural headwater streams. We compared nine stream reaches representing different morphological types (forested meandering reaches vs. deforested channelized reaches) regarding sediment structure, sedimentary nutrient and organic matter concentrations, and benthic microbial respiration. Main differences among reach types were found in grain sizes. Meandering reaches featured larger mean grain sizes (50–70 μm) and a thicker oxygenated surface layer (8 cm) than channelized reaches (40 μm, 5 cm). Total phosphorous amounted for up to 1,500 μg $ g^{−1} $ DW at retentive channelized reaches and 850–1,050 μg $ g^{−1} $ DW at the others. While N-$ NH_{4} $ accumulated in the sediments (60–180 μg $ g^{−1} $ DW), N-$ NO_{3} $ concentrations were generally low (2–5 μg $ g^{−1} $ DW). Benthic respiration was high at all sites (10–20 g $ O_{2} $ $ m^{−2} $ $ day^{−1} $). Our study shows that both hydromorphology and bank vegetation may influence the sediment quality of agricultural streams, though effects are often small and spatially restricted. To increase the efficiency of stream restoration in agricultural landscapes, nutrient and sediment delivery to stream channels need to be minimized by mitigating soil erosion in the catchment. © Springer-Verlag 2012 |
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