Acidification and nutrient imbalance in forest soils subjected to nitrogen deposition
Abstract Emission of nitrogen oxides ($ NO_{x} $) and ammonia ($ NH_{3} $) from a fertilizer factory and the resulting input of nitrates ($ NO_{3} $−) and ammonium ($ NH_{4} $+) into the soil were the main reasons of nitrogen (N) cycle disturbance in forest ecosystems near Novgorod, North-Western Ru...
Ausführliche Beschreibung
Autor*in: |
Makarov, M. I. [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
1995 |
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Systematik: |
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Anmerkung: |
© Kluwer Academic Publishers 1995 |
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Übergeordnetes Werk: |
Enthalten in: Water, air & soil pollution - Kluwer Academic Publishers, 1971, 85(1995), 3 vom: Dez., Seite 1137-1142 |
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Übergeordnetes Werk: |
volume:85 ; year:1995 ; number:3 ; month:12 ; pages:1137-1142 |
Links: |
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DOI / URN: |
10.1007/BF00477134 |
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Katalog-ID: |
OLC2084461472 |
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245 | 1 | 0 | |a Acidification and nutrient imbalance in forest soils subjected to nitrogen deposition |
264 | 1 | |c 1995 | |
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520 | |a Abstract Emission of nitrogen oxides ($ NO_{x} $) and ammonia ($ NH_{3} $) from a fertilizer factory and the resulting input of nitrates ($ NO_{3} $−) and ammonium ($ NH_{4} $+) into the soil were the main reasons of nitrogen (N) cycle disturbance in forest ecosystems near Novgorod, North-Western Russia (50°31′ North, 31°17′ East). Total N atmospheric input was about 100 kg/ha annually. $ NH_{3} $ was a dominant pollutant, causing the increase of atmospheric precipitation pH within the polluted region compared to background territories (6.0–6.5 and 4.5–5.0, respectively). Soil acidification through $ NH_{4} $+ nitrification was observed. N-$ NO_{3} $− concentrations in soil solution reached 20–30 mg/l, and proton (H) production was equal to 4.1 keq/ha per warm season (from April to October). Compared with soil status in 1983, pH decrease by 0.2 pH units was found in A horizon. The content of exchangeable calcium (Ca) and magnesium (Mg) decreased by the factor of 2–3 and 1.5–2 in A and B horizons, respectively. Triple increase of exchangeable aluminium (Al) content was detected in A horizon. Through recent decrease of pollutant emission, the polluted territory is now a suitable subject for recovery studies. | ||
650 | 4 | |a Nitrogen Oxide | |
650 | 4 | |a Warm Season | |
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650 | 4 | |a Nitrogen Deposition | |
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700 | 1 | |a Kiseleva, V. V. |4 aut | |
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10.1007/BF00477134 doi (DE-627)OLC2084461472 (DE-He213)BF00477134-p DE-627 ger DE-627 rakwb eng 570 333.7 VZ 12 13 ssgn BIODIV DE-30 fid ZC 7520 VZ rvk ZC 7520 VZ rvk Makarov, M. I. verfasserin aut Acidification and nutrient imbalance in forest soils subjected to nitrogen deposition 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1995 Abstract Emission of nitrogen oxides ($ NO_{x} $) and ammonia ($ NH_{3} $) from a fertilizer factory and the resulting input of nitrates ($ NO_{3} $−) and ammonium ($ NH_{4} $+) into the soil were the main reasons of nitrogen (N) cycle disturbance in forest ecosystems near Novgorod, North-Western Russia (50°31′ North, 31°17′ East). Total N atmospheric input was about 100 kg/ha annually. $ NH_{3} $ was a dominant pollutant, causing the increase of atmospheric precipitation pH within the polluted region compared to background territories (6.0–6.5 and 4.5–5.0, respectively). Soil acidification through $ NH_{4} $+ nitrification was observed. N-$ NO_{3} $− concentrations in soil solution reached 20–30 mg/l, and proton (H) production was equal to 4.1 keq/ha per warm season (from April to October). Compared with soil status in 1983, pH decrease by 0.2 pH units was found in A horizon. The content of exchangeable calcium (Ca) and magnesium (Mg) decreased by the factor of 2–3 and 1.5–2 in A and B horizons, respectively. Triple increase of exchangeable aluminium (Al) content was detected in A horizon. Through recent decrease of pollutant emission, the polluted territory is now a suitable subject for recovery studies. Nitrogen Oxide Warm Season Pollutant Emission Nitrogen Deposition Atmospheric Precipitation Kiseleva, V. V. aut Enthalten in Water, air & soil pollution Kluwer Academic Publishers, 1971 85(1995), 3 vom: Dez., Seite 1137-1142 (DE-627)12929134X (DE-600)120499-3 (DE-576)014472643 0049-6979 nnns volume:85 year:1995 number:3 month:12 pages:1137-1142 https://doi.org/10.1007/BF00477134 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-TEC SSG-OLC-FOR SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_40 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2012 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4314 GBV_ILN_4315 GBV_ILN_4325 ZC 7520 ZC 7520 AR 85 1995 3 12 1137-1142 |
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10.1007/BF00477134 doi (DE-627)OLC2084461472 (DE-He213)BF00477134-p DE-627 ger DE-627 rakwb eng 570 333.7 VZ 12 13 ssgn BIODIV DE-30 fid ZC 7520 VZ rvk ZC 7520 VZ rvk Makarov, M. I. verfasserin aut Acidification and nutrient imbalance in forest soils subjected to nitrogen deposition 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1995 Abstract Emission of nitrogen oxides ($ NO_{x} $) and ammonia ($ NH_{3} $) from a fertilizer factory and the resulting input of nitrates ($ NO_{3} $−) and ammonium ($ NH_{4} $+) into the soil were the main reasons of nitrogen (N) cycle disturbance in forest ecosystems near Novgorod, North-Western Russia (50°31′ North, 31°17′ East). Total N atmospheric input was about 100 kg/ha annually. $ NH_{3} $ was a dominant pollutant, causing the increase of atmospheric precipitation pH within the polluted region compared to background territories (6.0–6.5 and 4.5–5.0, respectively). Soil acidification through $ NH_{4} $+ nitrification was observed. N-$ NO_{3} $− concentrations in soil solution reached 20–30 mg/l, and proton (H) production was equal to 4.1 keq/ha per warm season (from April to October). Compared with soil status in 1983, pH decrease by 0.2 pH units was found in A horizon. The content of exchangeable calcium (Ca) and magnesium (Mg) decreased by the factor of 2–3 and 1.5–2 in A and B horizons, respectively. Triple increase of exchangeable aluminium (Al) content was detected in A horizon. Through recent decrease of pollutant emission, the polluted territory is now a suitable subject for recovery studies. Nitrogen Oxide Warm Season Pollutant Emission Nitrogen Deposition Atmospheric Precipitation Kiseleva, V. V. aut Enthalten in Water, air & soil pollution Kluwer Academic Publishers, 1971 85(1995), 3 vom: Dez., Seite 1137-1142 (DE-627)12929134X (DE-600)120499-3 (DE-576)014472643 0049-6979 nnns volume:85 year:1995 number:3 month:12 pages:1137-1142 https://doi.org/10.1007/BF00477134 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-TEC SSG-OLC-FOR SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_40 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2012 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4314 GBV_ILN_4315 GBV_ILN_4325 ZC 7520 ZC 7520 AR 85 1995 3 12 1137-1142 |
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10.1007/BF00477134 doi (DE-627)OLC2084461472 (DE-He213)BF00477134-p DE-627 ger DE-627 rakwb eng 570 333.7 VZ 12 13 ssgn BIODIV DE-30 fid ZC 7520 VZ rvk ZC 7520 VZ rvk Makarov, M. I. verfasserin aut Acidification and nutrient imbalance in forest soils subjected to nitrogen deposition 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1995 Abstract Emission of nitrogen oxides ($ NO_{x} $) and ammonia ($ NH_{3} $) from a fertilizer factory and the resulting input of nitrates ($ NO_{3} $−) and ammonium ($ NH_{4} $+) into the soil were the main reasons of nitrogen (N) cycle disturbance in forest ecosystems near Novgorod, North-Western Russia (50°31′ North, 31°17′ East). Total N atmospheric input was about 100 kg/ha annually. $ NH_{3} $ was a dominant pollutant, causing the increase of atmospheric precipitation pH within the polluted region compared to background territories (6.0–6.5 and 4.5–5.0, respectively). Soil acidification through $ NH_{4} $+ nitrification was observed. N-$ NO_{3} $− concentrations in soil solution reached 20–30 mg/l, and proton (H) production was equal to 4.1 keq/ha per warm season (from April to October). Compared with soil status in 1983, pH decrease by 0.2 pH units was found in A horizon. The content of exchangeable calcium (Ca) and magnesium (Mg) decreased by the factor of 2–3 and 1.5–2 in A and B horizons, respectively. Triple increase of exchangeable aluminium (Al) content was detected in A horizon. Through recent decrease of pollutant emission, the polluted territory is now a suitable subject for recovery studies. Nitrogen Oxide Warm Season Pollutant Emission Nitrogen Deposition Atmospheric Precipitation Kiseleva, V. V. aut Enthalten in Water, air & soil pollution Kluwer Academic Publishers, 1971 85(1995), 3 vom: Dez., Seite 1137-1142 (DE-627)12929134X (DE-600)120499-3 (DE-576)014472643 0049-6979 nnns volume:85 year:1995 number:3 month:12 pages:1137-1142 https://doi.org/10.1007/BF00477134 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-TEC SSG-OLC-FOR SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_40 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2012 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4314 GBV_ILN_4315 GBV_ILN_4325 ZC 7520 ZC 7520 AR 85 1995 3 12 1137-1142 |
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10.1007/BF00477134 doi (DE-627)OLC2084461472 (DE-He213)BF00477134-p DE-627 ger DE-627 rakwb eng 570 333.7 VZ 12 13 ssgn BIODIV DE-30 fid ZC 7520 VZ rvk ZC 7520 VZ rvk Makarov, M. I. verfasserin aut Acidification and nutrient imbalance in forest soils subjected to nitrogen deposition 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1995 Abstract Emission of nitrogen oxides ($ NO_{x} $) and ammonia ($ NH_{3} $) from a fertilizer factory and the resulting input of nitrates ($ NO_{3} $−) and ammonium ($ NH_{4} $+) into the soil were the main reasons of nitrogen (N) cycle disturbance in forest ecosystems near Novgorod, North-Western Russia (50°31′ North, 31°17′ East). Total N atmospheric input was about 100 kg/ha annually. $ NH_{3} $ was a dominant pollutant, causing the increase of atmospheric precipitation pH within the polluted region compared to background territories (6.0–6.5 and 4.5–5.0, respectively). Soil acidification through $ NH_{4} $+ nitrification was observed. N-$ NO_{3} $− concentrations in soil solution reached 20–30 mg/l, and proton (H) production was equal to 4.1 keq/ha per warm season (from April to October). Compared with soil status in 1983, pH decrease by 0.2 pH units was found in A horizon. The content of exchangeable calcium (Ca) and magnesium (Mg) decreased by the factor of 2–3 and 1.5–2 in A and B horizons, respectively. Triple increase of exchangeable aluminium (Al) content was detected in A horizon. Through recent decrease of pollutant emission, the polluted territory is now a suitable subject for recovery studies. Nitrogen Oxide Warm Season Pollutant Emission Nitrogen Deposition Atmospheric Precipitation Kiseleva, V. V. aut Enthalten in Water, air & soil pollution Kluwer Academic Publishers, 1971 85(1995), 3 vom: Dez., Seite 1137-1142 (DE-627)12929134X (DE-600)120499-3 (DE-576)014472643 0049-6979 nnns volume:85 year:1995 number:3 month:12 pages:1137-1142 https://doi.org/10.1007/BF00477134 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-TEC SSG-OLC-FOR SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_40 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2012 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4314 GBV_ILN_4315 GBV_ILN_4325 ZC 7520 ZC 7520 AR 85 1995 3 12 1137-1142 |
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10.1007/BF00477134 doi (DE-627)OLC2084461472 (DE-He213)BF00477134-p DE-627 ger DE-627 rakwb eng 570 333.7 VZ 12 13 ssgn BIODIV DE-30 fid ZC 7520 VZ rvk ZC 7520 VZ rvk Makarov, M. I. verfasserin aut Acidification and nutrient imbalance in forest soils subjected to nitrogen deposition 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1995 Abstract Emission of nitrogen oxides ($ NO_{x} $) and ammonia ($ NH_{3} $) from a fertilizer factory and the resulting input of nitrates ($ NO_{3} $−) and ammonium ($ NH_{4} $+) into the soil were the main reasons of nitrogen (N) cycle disturbance in forest ecosystems near Novgorod, North-Western Russia (50°31′ North, 31°17′ East). Total N atmospheric input was about 100 kg/ha annually. $ NH_{3} $ was a dominant pollutant, causing the increase of atmospheric precipitation pH within the polluted region compared to background territories (6.0–6.5 and 4.5–5.0, respectively). Soil acidification through $ NH_{4} $+ nitrification was observed. N-$ NO_{3} $− concentrations in soil solution reached 20–30 mg/l, and proton (H) production was equal to 4.1 keq/ha per warm season (from April to October). Compared with soil status in 1983, pH decrease by 0.2 pH units was found in A horizon. The content of exchangeable calcium (Ca) and magnesium (Mg) decreased by the factor of 2–3 and 1.5–2 in A and B horizons, respectively. Triple increase of exchangeable aluminium (Al) content was detected in A horizon. Through recent decrease of pollutant emission, the polluted territory is now a suitable subject for recovery studies. Nitrogen Oxide Warm Season Pollutant Emission Nitrogen Deposition Atmospheric Precipitation Kiseleva, V. V. aut Enthalten in Water, air & soil pollution Kluwer Academic Publishers, 1971 85(1995), 3 vom: Dez., Seite 1137-1142 (DE-627)12929134X (DE-600)120499-3 (DE-576)014472643 0049-6979 nnns volume:85 year:1995 number:3 month:12 pages:1137-1142 https://doi.org/10.1007/BF00477134 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-TEC SSG-OLC-FOR SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_40 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2012 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4314 GBV_ILN_4315 GBV_ILN_4325 ZC 7520 ZC 7520 AR 85 1995 3 12 1137-1142 |
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570 333.7 VZ 12 13 ssgn BIODIV DE-30 fid ZC 7520 VZ rvk Acidification and nutrient imbalance in forest soils subjected to nitrogen deposition Nitrogen Oxide Warm Season Pollutant Emission Nitrogen Deposition Atmospheric Precipitation |
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Acidification and nutrient imbalance in forest soils subjected to nitrogen deposition |
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acidification and nutrient imbalance in forest soils subjected to nitrogen deposition |
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Acidification and nutrient imbalance in forest soils subjected to nitrogen deposition |
abstract |
Abstract Emission of nitrogen oxides ($ NO_{x} $) and ammonia ($ NH_{3} $) from a fertilizer factory and the resulting input of nitrates ($ NO_{3} $−) and ammonium ($ NH_{4} $+) into the soil were the main reasons of nitrogen (N) cycle disturbance in forest ecosystems near Novgorod, North-Western Russia (50°31′ North, 31°17′ East). Total N atmospheric input was about 100 kg/ha annually. $ NH_{3} $ was a dominant pollutant, causing the increase of atmospheric precipitation pH within the polluted region compared to background territories (6.0–6.5 and 4.5–5.0, respectively). Soil acidification through $ NH_{4} $+ nitrification was observed. N-$ NO_{3} $− concentrations in soil solution reached 20–30 mg/l, and proton (H) production was equal to 4.1 keq/ha per warm season (from April to October). Compared with soil status in 1983, pH decrease by 0.2 pH units was found in A horizon. The content of exchangeable calcium (Ca) and magnesium (Mg) decreased by the factor of 2–3 and 1.5–2 in A and B horizons, respectively. Triple increase of exchangeable aluminium (Al) content was detected in A horizon. Through recent decrease of pollutant emission, the polluted territory is now a suitable subject for recovery studies. © Kluwer Academic Publishers 1995 |
abstractGer |
Abstract Emission of nitrogen oxides ($ NO_{x} $) and ammonia ($ NH_{3} $) from a fertilizer factory and the resulting input of nitrates ($ NO_{3} $−) and ammonium ($ NH_{4} $+) into the soil were the main reasons of nitrogen (N) cycle disturbance in forest ecosystems near Novgorod, North-Western Russia (50°31′ North, 31°17′ East). Total N atmospheric input was about 100 kg/ha annually. $ NH_{3} $ was a dominant pollutant, causing the increase of atmospheric precipitation pH within the polluted region compared to background territories (6.0–6.5 and 4.5–5.0, respectively). Soil acidification through $ NH_{4} $+ nitrification was observed. N-$ NO_{3} $− concentrations in soil solution reached 20–30 mg/l, and proton (H) production was equal to 4.1 keq/ha per warm season (from April to October). Compared with soil status in 1983, pH decrease by 0.2 pH units was found in A horizon. The content of exchangeable calcium (Ca) and magnesium (Mg) decreased by the factor of 2–3 and 1.5–2 in A and B horizons, respectively. Triple increase of exchangeable aluminium (Al) content was detected in A horizon. Through recent decrease of pollutant emission, the polluted territory is now a suitable subject for recovery studies. © Kluwer Academic Publishers 1995 |
abstract_unstemmed |
Abstract Emission of nitrogen oxides ($ NO_{x} $) and ammonia ($ NH_{3} $) from a fertilizer factory and the resulting input of nitrates ($ NO_{3} $−) and ammonium ($ NH_{4} $+) into the soil were the main reasons of nitrogen (N) cycle disturbance in forest ecosystems near Novgorod, North-Western Russia (50°31′ North, 31°17′ East). Total N atmospheric input was about 100 kg/ha annually. $ NH_{3} $ was a dominant pollutant, causing the increase of atmospheric precipitation pH within the polluted region compared to background territories (6.0–6.5 and 4.5–5.0, respectively). Soil acidification through $ NH_{4} $+ nitrification was observed. N-$ NO_{3} $− concentrations in soil solution reached 20–30 mg/l, and proton (H) production was equal to 4.1 keq/ha per warm season (from April to October). Compared with soil status in 1983, pH decrease by 0.2 pH units was found in A horizon. The content of exchangeable calcium (Ca) and magnesium (Mg) decreased by the factor of 2–3 and 1.5–2 in A and B horizons, respectively. Triple increase of exchangeable aluminium (Al) content was detected in A horizon. Through recent decrease of pollutant emission, the polluted territory is now a suitable subject for recovery studies. © Kluwer Academic Publishers 1995 |
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