Removal of Mineral Components and Organic Matter by the Wetland Water over the Kola Peninsula
Abstract Removal of mineral components and organic matter by the wetland water is evaluated using the observations on the Pulozero oligotrophic bog (the Kola Peninsula). Precipitation is a source of mineral components for bogs, its mean annual mineralization is 26.8 mg/$ dm^{3} $. The average annual...
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Gespeichert in:
| Autor*in: |
Kalyuzhnyi, I. L. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2022 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2022 |
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| Übergeordnetes Werk: |
Enthalten in: Russian meteorology and hydrology - Pleiades Publishing, 1993, 47(2022), 9 vom: Sept., Seite 668-676 |
|---|---|
| Übergeordnetes Werk: |
volume:47 ; year:2022 ; number:9 ; month:09 ; pages:668-676 |
| Links: |
|---|
| DOI / URN: |
10.3103/S1068373922090047 |
|---|
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OLC2133008403 |
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| 520 | |a Abstract Removal of mineral components and organic matter by the wetland water is evaluated using the observations on the Pulozero oligotrophic bog (the Kola Peninsula). Precipitation is a source of mineral components for bogs, its mean annual mineralization is 26.8 mg/$ dm^{3} $. The average annual inflow of mineral components per bog unit area is 13.0 t/$ km^{2} $. Their mean annual channel flow modulus (14.8 t/$ km^{2} $) is 38% greater than the modulus of their total loss (10.7 t/$ km^{2} $) from the wetland (by infiltration, discharge, and accumulation). It is explained by the partial discharge of groundwater into the stream channel. The accumulation of mineral components within a peat deposit is equal to 2.3 t/$ km^{2} $ per year, or 17.7% of fallen ones. The concentration of organic matter in the water of a hummock-ridge complex is on average equal to 140.3 mg/$ dm^{3} $, varying from 68.2 to 200.8 mg/$ dm^{3} $. The modulus of organic substance loss within the complex is on average equal to 38.2 t/($ km^{2} $ year). Its annual channel flow is 12.5 t/($ km^{2} $ year). The accumulation of organic matter within the peat deposit reaches 25.7 t/($ km^{2} $ year), or 67.3% of the organic substance mass formed within the bog microlandscape during a year. | ||
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| 650 | 4 | |a organic matter discharge | |
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10.3103/S1068373922090047 doi (DE-627)OLC2133008403 (DE-He213)S1068373922090047-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Kalyuzhnyi, I. L. verfasserin aut Removal of Mineral Components and Organic Matter by the Wetland Water over the Kola Peninsula 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2022 Abstract Removal of mineral components and organic matter by the wetland water is evaluated using the observations on the Pulozero oligotrophic bog (the Kola Peninsula). Precipitation is a source of mineral components for bogs, its mean annual mineralization is 26.8 mg/$ dm^{3} $. The average annual inflow of mineral components per bog unit area is 13.0 t/$ km^{2} $. Their mean annual channel flow modulus (14.8 t/$ km^{2} $) is 38% greater than the modulus of their total loss (10.7 t/$ km^{2} $) from the wetland (by infiltration, discharge, and accumulation). It is explained by the partial discharge of groundwater into the stream channel. The accumulation of mineral components within a peat deposit is equal to 2.3 t/$ km^{2} $ per year, or 17.7% of fallen ones. The concentration of organic matter in the water of a hummock-ridge complex is on average equal to 140.3 mg/$ dm^{3} $, varying from 68.2 to 200.8 mg/$ dm^{3} $. The modulus of organic substance loss within the complex is on average equal to 38.2 t/($ km^{2} $ year). Its annual channel flow is 12.5 t/($ km^{2} $ year). The accumulation of organic matter within the peat deposit reaches 25.7 t/($ km^{2} $ year), or 67.3% of the organic substance mass formed within the bog microlandscape during a year. bog precipitation organic matter discharge accumulation Enthalten in Russian meteorology and hydrology Pleiades Publishing, 1993 47(2022), 9 vom: Sept., Seite 668-676 (DE-627)181990490 (DE-600)1180563-8 (DE-576)03887959X 1068-3739 nnns volume:47 year:2022 number:9 month:09 pages:668-676 https://doi.org/10.3103/S1068373922090047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-OEU SSG-OPC-GGO AR 47 2022 9 09 668-676 |
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10.3103/S1068373922090047 doi (DE-627)OLC2133008403 (DE-He213)S1068373922090047-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Kalyuzhnyi, I. L. verfasserin aut Removal of Mineral Components and Organic Matter by the Wetland Water over the Kola Peninsula 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2022 Abstract Removal of mineral components and organic matter by the wetland water is evaluated using the observations on the Pulozero oligotrophic bog (the Kola Peninsula). Precipitation is a source of mineral components for bogs, its mean annual mineralization is 26.8 mg/$ dm^{3} $. The average annual inflow of mineral components per bog unit area is 13.0 t/$ km^{2} $. Their mean annual channel flow modulus (14.8 t/$ km^{2} $) is 38% greater than the modulus of their total loss (10.7 t/$ km^{2} $) from the wetland (by infiltration, discharge, and accumulation). It is explained by the partial discharge of groundwater into the stream channel. The accumulation of mineral components within a peat deposit is equal to 2.3 t/$ km^{2} $ per year, or 17.7% of fallen ones. The concentration of organic matter in the water of a hummock-ridge complex is on average equal to 140.3 mg/$ dm^{3} $, varying from 68.2 to 200.8 mg/$ dm^{3} $. The modulus of organic substance loss within the complex is on average equal to 38.2 t/($ km^{2} $ year). Its annual channel flow is 12.5 t/($ km^{2} $ year). The accumulation of organic matter within the peat deposit reaches 25.7 t/($ km^{2} $ year), or 67.3% of the organic substance mass formed within the bog microlandscape during a year. bog precipitation organic matter discharge accumulation Enthalten in Russian meteorology and hydrology Pleiades Publishing, 1993 47(2022), 9 vom: Sept., Seite 668-676 (DE-627)181990490 (DE-600)1180563-8 (DE-576)03887959X 1068-3739 nnns volume:47 year:2022 number:9 month:09 pages:668-676 https://doi.org/10.3103/S1068373922090047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-OEU SSG-OPC-GGO AR 47 2022 9 09 668-676 |
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10.3103/S1068373922090047 doi (DE-627)OLC2133008403 (DE-He213)S1068373922090047-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Kalyuzhnyi, I. L. verfasserin aut Removal of Mineral Components and Organic Matter by the Wetland Water over the Kola Peninsula 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2022 Abstract Removal of mineral components and organic matter by the wetland water is evaluated using the observations on the Pulozero oligotrophic bog (the Kola Peninsula). Precipitation is a source of mineral components for bogs, its mean annual mineralization is 26.8 mg/$ dm^{3} $. The average annual inflow of mineral components per bog unit area is 13.0 t/$ km^{2} $. Their mean annual channel flow modulus (14.8 t/$ km^{2} $) is 38% greater than the modulus of their total loss (10.7 t/$ km^{2} $) from the wetland (by infiltration, discharge, and accumulation). It is explained by the partial discharge of groundwater into the stream channel. The accumulation of mineral components within a peat deposit is equal to 2.3 t/$ km^{2} $ per year, or 17.7% of fallen ones. The concentration of organic matter in the water of a hummock-ridge complex is on average equal to 140.3 mg/$ dm^{3} $, varying from 68.2 to 200.8 mg/$ dm^{3} $. The modulus of organic substance loss within the complex is on average equal to 38.2 t/($ km^{2} $ year). Its annual channel flow is 12.5 t/($ km^{2} $ year). The accumulation of organic matter within the peat deposit reaches 25.7 t/($ km^{2} $ year), or 67.3% of the organic substance mass formed within the bog microlandscape during a year. bog precipitation organic matter discharge accumulation Enthalten in Russian meteorology and hydrology Pleiades Publishing, 1993 47(2022), 9 vom: Sept., Seite 668-676 (DE-627)181990490 (DE-600)1180563-8 (DE-576)03887959X 1068-3739 nnns volume:47 year:2022 number:9 month:09 pages:668-676 https://doi.org/10.3103/S1068373922090047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-OEU SSG-OPC-GGO AR 47 2022 9 09 668-676 |
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10.3103/S1068373922090047 doi (DE-627)OLC2133008403 (DE-He213)S1068373922090047-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Kalyuzhnyi, I. L. verfasserin aut Removal of Mineral Components and Organic Matter by the Wetland Water over the Kola Peninsula 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2022 Abstract Removal of mineral components and organic matter by the wetland water is evaluated using the observations on the Pulozero oligotrophic bog (the Kola Peninsula). Precipitation is a source of mineral components for bogs, its mean annual mineralization is 26.8 mg/$ dm^{3} $. The average annual inflow of mineral components per bog unit area is 13.0 t/$ km^{2} $. Their mean annual channel flow modulus (14.8 t/$ km^{2} $) is 38% greater than the modulus of their total loss (10.7 t/$ km^{2} $) from the wetland (by infiltration, discharge, and accumulation). It is explained by the partial discharge of groundwater into the stream channel. The accumulation of mineral components within a peat deposit is equal to 2.3 t/$ km^{2} $ per year, or 17.7% of fallen ones. The concentration of organic matter in the water of a hummock-ridge complex is on average equal to 140.3 mg/$ dm^{3} $, varying from 68.2 to 200.8 mg/$ dm^{3} $. The modulus of organic substance loss within the complex is on average equal to 38.2 t/($ km^{2} $ year). Its annual channel flow is 12.5 t/($ km^{2} $ year). The accumulation of organic matter within the peat deposit reaches 25.7 t/($ km^{2} $ year), or 67.3% of the organic substance mass formed within the bog microlandscape during a year. bog precipitation organic matter discharge accumulation Enthalten in Russian meteorology and hydrology Pleiades Publishing, 1993 47(2022), 9 vom: Sept., Seite 668-676 (DE-627)181990490 (DE-600)1180563-8 (DE-576)03887959X 1068-3739 nnns volume:47 year:2022 number:9 month:09 pages:668-676 https://doi.org/10.3103/S1068373922090047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-OEU SSG-OPC-GGO AR 47 2022 9 09 668-676 |
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10.3103/S1068373922090047 doi (DE-627)OLC2133008403 (DE-He213)S1068373922090047-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Kalyuzhnyi, I. L. verfasserin aut Removal of Mineral Components and Organic Matter by the Wetland Water over the Kola Peninsula 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2022 Abstract Removal of mineral components and organic matter by the wetland water is evaluated using the observations on the Pulozero oligotrophic bog (the Kola Peninsula). Precipitation is a source of mineral components for bogs, its mean annual mineralization is 26.8 mg/$ dm^{3} $. The average annual inflow of mineral components per bog unit area is 13.0 t/$ km^{2} $. Their mean annual channel flow modulus (14.8 t/$ km^{2} $) is 38% greater than the modulus of their total loss (10.7 t/$ km^{2} $) from the wetland (by infiltration, discharge, and accumulation). It is explained by the partial discharge of groundwater into the stream channel. The accumulation of mineral components within a peat deposit is equal to 2.3 t/$ km^{2} $ per year, or 17.7% of fallen ones. The concentration of organic matter in the water of a hummock-ridge complex is on average equal to 140.3 mg/$ dm^{3} $, varying from 68.2 to 200.8 mg/$ dm^{3} $. The modulus of organic substance loss within the complex is on average equal to 38.2 t/($ km^{2} $ year). Its annual channel flow is 12.5 t/($ km^{2} $ year). The accumulation of organic matter within the peat deposit reaches 25.7 t/($ km^{2} $ year), or 67.3% of the organic substance mass formed within the bog microlandscape during a year. bog precipitation organic matter discharge accumulation Enthalten in Russian meteorology and hydrology Pleiades Publishing, 1993 47(2022), 9 vom: Sept., Seite 668-676 (DE-627)181990490 (DE-600)1180563-8 (DE-576)03887959X 1068-3739 nnns volume:47 year:2022 number:9 month:09 pages:668-676 https://doi.org/10.3103/S1068373922090047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-OEU SSG-OPC-GGO AR 47 2022 9 09 668-676 |
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Removal of Mineral Components and Organic Matter by the Wetland Water over the Kola Peninsula |
| abstract |
Abstract Removal of mineral components and organic matter by the wetland water is evaluated using the observations on the Pulozero oligotrophic bog (the Kola Peninsula). Precipitation is a source of mineral components for bogs, its mean annual mineralization is 26.8 mg/$ dm^{3} $. The average annual inflow of mineral components per bog unit area is 13.0 t/$ km^{2} $. Their mean annual channel flow modulus (14.8 t/$ km^{2} $) is 38% greater than the modulus of their total loss (10.7 t/$ km^{2} $) from the wetland (by infiltration, discharge, and accumulation). It is explained by the partial discharge of groundwater into the stream channel. The accumulation of mineral components within a peat deposit is equal to 2.3 t/$ km^{2} $ per year, or 17.7% of fallen ones. The concentration of organic matter in the water of a hummock-ridge complex is on average equal to 140.3 mg/$ dm^{3} $, varying from 68.2 to 200.8 mg/$ dm^{3} $. The modulus of organic substance loss within the complex is on average equal to 38.2 t/($ km^{2} $ year). Its annual channel flow is 12.5 t/($ km^{2} $ year). The accumulation of organic matter within the peat deposit reaches 25.7 t/($ km^{2} $ year), or 67.3% of the organic substance mass formed within the bog microlandscape during a year. © Pleiades Publishing, Ltd. 2022 |
| abstractGer |
Abstract Removal of mineral components and organic matter by the wetland water is evaluated using the observations on the Pulozero oligotrophic bog (the Kola Peninsula). Precipitation is a source of mineral components for bogs, its mean annual mineralization is 26.8 mg/$ dm^{3} $. The average annual inflow of mineral components per bog unit area is 13.0 t/$ km^{2} $. Their mean annual channel flow modulus (14.8 t/$ km^{2} $) is 38% greater than the modulus of their total loss (10.7 t/$ km^{2} $) from the wetland (by infiltration, discharge, and accumulation). It is explained by the partial discharge of groundwater into the stream channel. The accumulation of mineral components within a peat deposit is equal to 2.3 t/$ km^{2} $ per year, or 17.7% of fallen ones. The concentration of organic matter in the water of a hummock-ridge complex is on average equal to 140.3 mg/$ dm^{3} $, varying from 68.2 to 200.8 mg/$ dm^{3} $. The modulus of organic substance loss within the complex is on average equal to 38.2 t/($ km^{2} $ year). Its annual channel flow is 12.5 t/($ km^{2} $ year). The accumulation of organic matter within the peat deposit reaches 25.7 t/($ km^{2} $ year), or 67.3% of the organic substance mass formed within the bog microlandscape during a year. © Pleiades Publishing, Ltd. 2022 |
| abstract_unstemmed |
Abstract Removal of mineral components and organic matter by the wetland water is evaluated using the observations on the Pulozero oligotrophic bog (the Kola Peninsula). Precipitation is a source of mineral components for bogs, its mean annual mineralization is 26.8 mg/$ dm^{3} $. The average annual inflow of mineral components per bog unit area is 13.0 t/$ km^{2} $. Their mean annual channel flow modulus (14.8 t/$ km^{2} $) is 38% greater than the modulus of their total loss (10.7 t/$ km^{2} $) from the wetland (by infiltration, discharge, and accumulation). It is explained by the partial discharge of groundwater into the stream channel. The accumulation of mineral components within a peat deposit is equal to 2.3 t/$ km^{2} $ per year, or 17.7% of fallen ones. The concentration of organic matter in the water of a hummock-ridge complex is on average equal to 140.3 mg/$ dm^{3} $, varying from 68.2 to 200.8 mg/$ dm^{3} $. The modulus of organic substance loss within the complex is on average equal to 38.2 t/($ km^{2} $ year). Its annual channel flow is 12.5 t/($ km^{2} $ year). The accumulation of organic matter within the peat deposit reaches 25.7 t/($ km^{2} $ year), or 67.3% of the organic substance mass formed within the bog microlandscape during a year. © Pleiades Publishing, Ltd. 2022 |
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| title_short |
Removal of Mineral Components and Organic Matter by the Wetland Water over the Kola Peninsula |
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https://doi.org/10.3103/S1068373922090047 |
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2024-07-03T16:36:46.723Z |
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