Long-term retention of 137Cs in three forest soil types with different soil properties
Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gap...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Suchara, Ivan [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2016transfer abstract |
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| Schlagwörter: |
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| Umfang: |
12 |
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| Übergeordnetes Werk: |
Enthalten in: Acute caffeine ingestion improves 3-km run performance, cognitive function, and psychological state of young recreational runners - Khcharem, Amir ELSEVIER, 2021, New York, NY [u.a.] |
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| Übergeordnetes Werk: |
volume:158 ; year:2016 ; pages:102-113 ; extent:12 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.jenvrad.2016.04.010 |
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ELV029665701 |
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| 245 | 1 | 0 | |a Long-term retention of 137Cs in three forest soil types with different soil properties |
| 264 | 1 | |c 2016transfer abstract | |
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| 520 | |a Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. | ||
| 520 | |a Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. | ||
| 650 | 7 | |a 137Cs activity concentrations |2 Elsevier | |
| 650 | 7 | |a Soil properties |2 Elsevier | |
| 650 | 7 | |a Soil horizons |2 Elsevier | |
| 650 | 7 | |a 137Cs vertical migration rate |2 Elsevier | |
| 650 | 7 | |a 137Cs inventory |2 Elsevier | |
| 700 | 1 | |a Sucharová, Julie |4 oth | |
| 700 | 1 | |a Holá, Marie |4 oth | |
| 700 | 1 | |a Pilátová, Helena |4 oth | |
| 700 | 1 | |a Rulík, Petr |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier |a Khcharem, Amir ELSEVIER |t Acute caffeine ingestion improves 3-km run performance, cognitive function, and psychological state of young recreational runners |d 2021 |g New York, NY [u.a.] |w (DE-627)ELV006295479 |
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10.1016/j.jenvrad.2016.04.010 doi GBVA2016008000022.pica (DE-627)ELV029665701 (ELSEVIER)S0265-931X(16)30100-X DE-627 ger DE-627 rakwb eng 690 540 690 DE-600 540 DE-600 540 VZ 15,3 ssgn PHARM DE-84 fid 44.00 bkl 44.38 bkl 42.66 bkl 44.40 bkl Suchara, Ivan verfasserin aut Long-term retention of 137Cs in three forest soil types with different soil properties 2016transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. 137Cs activity concentrations Elsevier Soil properties Elsevier Soil horizons Elsevier 137Cs vertical migration rate Elsevier 137Cs inventory Elsevier Sucharová, Julie oth Holá, Marie oth Pilátová, Helena oth Rulík, Petr oth Enthalten in Elsevier Khcharem, Amir ELSEVIER Acute caffeine ingestion improves 3-km run performance, cognitive function, and psychological state of young recreational runners 2021 New York, NY [u.a.] (DE-627)ELV006295479 volume:158 year:2016 pages:102-113 extent:12 https://doi.org/10.1016/j.jenvrad.2016.04.010 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-PHARM SSG-OLC-PHA SSG-OPC-PHA 44.00 Medizin: Allgemeines VZ 44.38 Pharmakologie VZ 42.66 Ethologie Biologie VZ 44.40 Pharmazie Pharmazeutika VZ AR 158 2016 102-113 12 045F 690 |
| spelling |
10.1016/j.jenvrad.2016.04.010 doi GBVA2016008000022.pica (DE-627)ELV029665701 (ELSEVIER)S0265-931X(16)30100-X DE-627 ger DE-627 rakwb eng 690 540 690 DE-600 540 DE-600 540 VZ 15,3 ssgn PHARM DE-84 fid 44.00 bkl 44.38 bkl 42.66 bkl 44.40 bkl Suchara, Ivan verfasserin aut Long-term retention of 137Cs in three forest soil types with different soil properties 2016transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. 137Cs activity concentrations Elsevier Soil properties Elsevier Soil horizons Elsevier 137Cs vertical migration rate Elsevier 137Cs inventory Elsevier Sucharová, Julie oth Holá, Marie oth Pilátová, Helena oth Rulík, Petr oth Enthalten in Elsevier Khcharem, Amir ELSEVIER Acute caffeine ingestion improves 3-km run performance, cognitive function, and psychological state of young recreational runners 2021 New York, NY [u.a.] (DE-627)ELV006295479 volume:158 year:2016 pages:102-113 extent:12 https://doi.org/10.1016/j.jenvrad.2016.04.010 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-PHARM SSG-OLC-PHA SSG-OPC-PHA 44.00 Medizin: Allgemeines VZ 44.38 Pharmakologie VZ 42.66 Ethologie Biologie VZ 44.40 Pharmazie Pharmazeutika VZ AR 158 2016 102-113 12 045F 690 |
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10.1016/j.jenvrad.2016.04.010 doi GBVA2016008000022.pica (DE-627)ELV029665701 (ELSEVIER)S0265-931X(16)30100-X DE-627 ger DE-627 rakwb eng 690 540 690 DE-600 540 DE-600 540 VZ 15,3 ssgn PHARM DE-84 fid 44.00 bkl 44.38 bkl 42.66 bkl 44.40 bkl Suchara, Ivan verfasserin aut Long-term retention of 137Cs in three forest soil types with different soil properties 2016transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. 137Cs activity concentrations Elsevier Soil properties Elsevier Soil horizons Elsevier 137Cs vertical migration rate Elsevier 137Cs inventory Elsevier Sucharová, Julie oth Holá, Marie oth Pilátová, Helena oth Rulík, Petr oth Enthalten in Elsevier Khcharem, Amir ELSEVIER Acute caffeine ingestion improves 3-km run performance, cognitive function, and psychological state of young recreational runners 2021 New York, NY [u.a.] (DE-627)ELV006295479 volume:158 year:2016 pages:102-113 extent:12 https://doi.org/10.1016/j.jenvrad.2016.04.010 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-PHARM SSG-OLC-PHA SSG-OPC-PHA 44.00 Medizin: Allgemeines VZ 44.38 Pharmakologie VZ 42.66 Ethologie Biologie VZ 44.40 Pharmazie Pharmazeutika VZ AR 158 2016 102-113 12 045F 690 |
| allfieldsGer |
10.1016/j.jenvrad.2016.04.010 doi GBVA2016008000022.pica (DE-627)ELV029665701 (ELSEVIER)S0265-931X(16)30100-X DE-627 ger DE-627 rakwb eng 690 540 690 DE-600 540 DE-600 540 VZ 15,3 ssgn PHARM DE-84 fid 44.00 bkl 44.38 bkl 42.66 bkl 44.40 bkl Suchara, Ivan verfasserin aut Long-term retention of 137Cs in three forest soil types with different soil properties 2016transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. 137Cs activity concentrations Elsevier Soil properties Elsevier Soil horizons Elsevier 137Cs vertical migration rate Elsevier 137Cs inventory Elsevier Sucharová, Julie oth Holá, Marie oth Pilátová, Helena oth Rulík, Petr oth Enthalten in Elsevier Khcharem, Amir ELSEVIER Acute caffeine ingestion improves 3-km run performance, cognitive function, and psychological state of young recreational runners 2021 New York, NY [u.a.] (DE-627)ELV006295479 volume:158 year:2016 pages:102-113 extent:12 https://doi.org/10.1016/j.jenvrad.2016.04.010 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-PHARM SSG-OLC-PHA SSG-OPC-PHA 44.00 Medizin: Allgemeines VZ 44.38 Pharmakologie VZ 42.66 Ethologie Biologie VZ 44.40 Pharmazie Pharmazeutika VZ AR 158 2016 102-113 12 045F 690 |
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10.1016/j.jenvrad.2016.04.010 doi GBVA2016008000022.pica (DE-627)ELV029665701 (ELSEVIER)S0265-931X(16)30100-X DE-627 ger DE-627 rakwb eng 690 540 690 DE-600 540 DE-600 540 VZ 15,3 ssgn PHARM DE-84 fid 44.00 bkl 44.38 bkl 42.66 bkl 44.40 bkl Suchara, Ivan verfasserin aut Long-term retention of 137Cs in three forest soil types with different soil properties 2016transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. 137Cs activity concentrations Elsevier Soil properties Elsevier Soil horizons Elsevier 137Cs vertical migration rate Elsevier 137Cs inventory Elsevier Sucharová, Julie oth Holá, Marie oth Pilátová, Helena oth Rulík, Petr oth Enthalten in Elsevier Khcharem, Amir ELSEVIER Acute caffeine ingestion improves 3-km run performance, cognitive function, and psychological state of young recreational runners 2021 New York, NY [u.a.] (DE-627)ELV006295479 volume:158 year:2016 pages:102-113 extent:12 https://doi.org/10.1016/j.jenvrad.2016.04.010 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-PHARM SSG-OLC-PHA SSG-OPC-PHA 44.00 Medizin: Allgemeines VZ 44.38 Pharmakologie VZ 42.66 Ethologie Biologie VZ 44.40 Pharmazie Pharmazeutika VZ AR 158 2016 102-113 12 045F 690 |
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long-term retention of 137cs in three forest soil types with different soil properties |
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Long-term retention of 137Cs in three forest soil types with different soil properties |
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Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. |
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Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. |
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Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies. |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV029665701</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230625175056.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">180603s2016 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.jenvrad.2016.04.010</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBVA2016008000022.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV029665701</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0265-931X(16)30100-X</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">690</subfield><subfield code="a">540</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">690</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">540</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">540</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">15,3</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">PHARM</subfield><subfield code="q">DE-84</subfield><subfield code="2">fid</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">44.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">44.38</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">42.66</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">44.40</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Suchara, Ivan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Long-term retention of 137Cs in three forest soil types with different soil properties</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016transfer abstract</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">12</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing 137Cs from the surrounding plots situated below neighbouring canopies.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Current 137Cs activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 × 20 × 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 × 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of 137Cs accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of 137Cs into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total 137Cs activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of 137Cs in the soils was found to be in accordance with the estimated 137Cs inputs from the Chernobyl fallout and from global fallout. The low amounts of 137Cs found accumulated in the aboveground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of 137Cs in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current 137Cs activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q4/6). However, this was not confirmed. Similarly, we observed a weak tendency toward higher 137Cs activity in soils below the canopy than in soils below canopy gaps. 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