Impact of Changes in Soil Attributes and Composition following Anthropization Related to Agricultural Practices in the Amazon Region
Abstract In response to the ongoing expansion of agriculture and land use changes in the Amazon region, new studies are necessary to understand the impacts of agricultural practices on Amazonian soils. The objective was to assess the changes induced in soil horizons by different management practices...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Paes da Silva, Rosa de Nazaré [verfasserIn] de Souza Mateus, Nikolas [verfasserIn] dos Santos, Cássio Rafael Costa [verfasserIn] Costa, Milton Garcia [verfasserIn] de Oliveira Ferreira, Eric Victor [verfasserIn] Viégas, Ismael de Jesus Matos [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2024 |
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| Schlagwörter: |
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| Anmerkung: |
© The Author(s) under exclusive licence to Sociedad Chilena de la Ciencia del Suelo 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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| Übergeordnetes Werk: |
Enthalten in: Journal of soil science and plant nutrition - Springer International Publishing, 2010, 24(2024), 2 vom: 22. März, Seite 2898-2909 |
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| Übergeordnetes Werk: |
volume:24 ; year:2024 ; number:2 ; day:22 ; month:03 ; pages:2898-2909 |
| Links: |
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| DOI / URN: |
10.1007/s42729-024-01716-x |
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SPR056602952 |
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| 520 | |a Abstract In response to the ongoing expansion of agriculture and land use changes in the Amazon region, new studies are necessary to understand the impacts of agricultural practices on Amazonian soils. The objective was to assess the changes induced in soil horizons by different management practices. The research was conducted in the National Forest of Caxiuanã, located in the municipality of Melgaço, Pará State, Brazil. A completely randomized 3 × 4 factorial design was employed, incorporating three types of vegetation (20-year-old secondary forest—$ Soil_{FS20} $, 5-year-old secondary forest—$ Soil_{FS5} $, and coivara—cutting and burning of native vegetation—$ Soil_{LTM} $) and four effective soil depths (0–5 cm, 5–10 cm, 10–20 cm, and 20–30 cm), with nine replicates for each combination. To enhance accuracy of the required assessment of the modifications induced in the physical and chemical attributes of the soil, isotopic composition of $ δ^{13} $C and $ δ^{15} $N was utilized. In areas subjected to clearing ($ Soil_{FS5} $ and $ Soil_{LTM} $), significant concentrations of carbon (C) and nitrogen (N) were observed in the 20–30 cm depth due to soil disturbance, which incorporated the litter into the deeper horizons. However, no significant differences in the C/N ratio were detected among the studied areas at the effective soil depth. Regardless of soil depth, $ Soil_{FS20} $ exhibited lower acidity, $ δ^{13} $C, $ δ^{15} $N, sandy and clay content, as well as iron (Fe) content, while displaying higher levels of SOM, zinc (Zn), calcium (Ca), manganese (Mn), potassium (K), silt, sodium (Na), copper (Cu), and phosphorus (P) content compared to the other sites. The results showed significant variations in the chemical and physical properties of the soil among the study sites, with $ Soil_{FS20} $ standing out in several characteristics. The increase in carbon stock in $ Soil_{FS20} $ indicated positive responses to specific management practices. Analyses of carbon, nitrogen concentrations, and stable isotopes highlighted $ Soil_{FS5} $ as distinctly different from the others. These findings contribute to the understanding of soil dynamics under different management practices, providing valuable insights for sustainable natural resource management in the region. | ||
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| 650 | 4 | |a Soil management |7 (dpeaa)DE-He213 | |
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| 700 | 1 | |a dos Santos, Cássio Rafael Costa |e verfasserin |4 aut | |
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| 700 | 1 | |a de Oliveira Ferreira, Eric Victor |e verfasserin |4 aut | |
| 700 | 1 | |a Viégas, Ismael de Jesus Matos |e verfasserin |4 aut | |
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10.1007/s42729-024-01716-x doi (DE-627)SPR056602952 (SPR)s42729-024-01716-x-e DE-627 ger DE-627 rakwb eng 630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl Paes da Silva, Rosa de Nazaré verfasserin aut Impact of Changes in Soil Attributes and Composition following Anthropization Related to Agricultural Practices in the Amazon Region 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) under exclusive licence to Sociedad Chilena de la Ciencia del Suelo 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract In response to the ongoing expansion of agriculture and land use changes in the Amazon region, new studies are necessary to understand the impacts of agricultural practices on Amazonian soils. The objective was to assess the changes induced in soil horizons by different management practices. The research was conducted in the National Forest of Caxiuanã, located in the municipality of Melgaço, Pará State, Brazil. A completely randomized 3 × 4 factorial design was employed, incorporating three types of vegetation (20-year-old secondary forest—$ Soil_{FS20} $, 5-year-old secondary forest—$ Soil_{FS5} $, and coivara—cutting and burning of native vegetation—$ Soil_{LTM} $) and four effective soil depths (0–5 cm, 5–10 cm, 10–20 cm, and 20–30 cm), with nine replicates for each combination. To enhance accuracy of the required assessment of the modifications induced in the physical and chemical attributes of the soil, isotopic composition of $ δ^{13} $C and $ δ^{15} $N was utilized. In areas subjected to clearing ($ Soil_{FS5} $ and $ Soil_{LTM} $), significant concentrations of carbon (C) and nitrogen (N) were observed in the 20–30 cm depth due to soil disturbance, which incorporated the litter into the deeper horizons. However, no significant differences in the C/N ratio were detected among the studied areas at the effective soil depth. Regardless of soil depth, $ Soil_{FS20} $ exhibited lower acidity, $ δ^{13} $C, $ δ^{15} $N, sandy and clay content, as well as iron (Fe) content, while displaying higher levels of SOM, zinc (Zn), calcium (Ca), manganese (Mn), potassium (K), silt, sodium (Na), copper (Cu), and phosphorus (P) content compared to the other sites. The results showed significant variations in the chemical and physical properties of the soil among the study sites, with $ Soil_{FS20} $ standing out in several characteristics. The increase in carbon stock in $ Soil_{FS20} $ indicated positive responses to specific management practices. Analyses of carbon, nitrogen concentrations, and stable isotopes highlighted $ Soil_{FS5} $ as distinctly different from the others. These findings contribute to the understanding of soil dynamics under different management practices, providing valuable insights for sustainable natural resource management in the region. Soil anthropization (dpeaa)DE-He213 Soil chemical attributes (dpeaa)DE-He213 Stable isotope analysis (dpeaa)DE-He213 Soil organic matter (dpeaa)DE-He213 Soil management (dpeaa)DE-He213 de Souza Mateus, Nikolas verfasserin aut dos Santos, Cássio Rafael Costa verfasserin aut Costa, Milton Garcia verfasserin (orcid)0000-0003-0105-8792 aut de Oliveira Ferreira, Eric Victor verfasserin aut Viégas, Ismael de Jesus Matos verfasserin aut Enthalten in Journal of soil science and plant nutrition Springer International Publishing, 2010 24(2024), 2 vom: 22. März, Seite 2898-2909 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:24 year:2024 number:2 day:22 month:03 pages:2898-2909 https://dx.doi.org/10.1007/s42729-024-01716-x X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OLC-PHA SSG-OPC-FOR SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 48.30 VZ 58.52 VZ AR 24 2024 2 22 03 2898-2909 |
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10.1007/s42729-024-01716-x doi (DE-627)SPR056602952 (SPR)s42729-024-01716-x-e DE-627 ger DE-627 rakwb eng 630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl Paes da Silva, Rosa de Nazaré verfasserin aut Impact of Changes in Soil Attributes and Composition following Anthropization Related to Agricultural Practices in the Amazon Region 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) under exclusive licence to Sociedad Chilena de la Ciencia del Suelo 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract In response to the ongoing expansion of agriculture and land use changes in the Amazon region, new studies are necessary to understand the impacts of agricultural practices on Amazonian soils. The objective was to assess the changes induced in soil horizons by different management practices. The research was conducted in the National Forest of Caxiuanã, located in the municipality of Melgaço, Pará State, Brazil. A completely randomized 3 × 4 factorial design was employed, incorporating three types of vegetation (20-year-old secondary forest—$ Soil_{FS20} $, 5-year-old secondary forest—$ Soil_{FS5} $, and coivara—cutting and burning of native vegetation—$ Soil_{LTM} $) and four effective soil depths (0–5 cm, 5–10 cm, 10–20 cm, and 20–30 cm), with nine replicates for each combination. To enhance accuracy of the required assessment of the modifications induced in the physical and chemical attributes of the soil, isotopic composition of $ δ^{13} $C and $ δ^{15} $N was utilized. In areas subjected to clearing ($ Soil_{FS5} $ and $ Soil_{LTM} $), significant concentrations of carbon (C) and nitrogen (N) were observed in the 20–30 cm depth due to soil disturbance, which incorporated the litter into the deeper horizons. However, no significant differences in the C/N ratio were detected among the studied areas at the effective soil depth. Regardless of soil depth, $ Soil_{FS20} $ exhibited lower acidity, $ δ^{13} $C, $ δ^{15} $N, sandy and clay content, as well as iron (Fe) content, while displaying higher levels of SOM, zinc (Zn), calcium (Ca), manganese (Mn), potassium (K), silt, sodium (Na), copper (Cu), and phosphorus (P) content compared to the other sites. The results showed significant variations in the chemical and physical properties of the soil among the study sites, with $ Soil_{FS20} $ standing out in several characteristics. The increase in carbon stock in $ Soil_{FS20} $ indicated positive responses to specific management practices. Analyses of carbon, nitrogen concentrations, and stable isotopes highlighted $ Soil_{FS5} $ as distinctly different from the others. These findings contribute to the understanding of soil dynamics under different management practices, providing valuable insights for sustainable natural resource management in the region. Soil anthropization (dpeaa)DE-He213 Soil chemical attributes (dpeaa)DE-He213 Stable isotope analysis (dpeaa)DE-He213 Soil organic matter (dpeaa)DE-He213 Soil management (dpeaa)DE-He213 de Souza Mateus, Nikolas verfasserin aut dos Santos, Cássio Rafael Costa verfasserin aut Costa, Milton Garcia verfasserin (orcid)0000-0003-0105-8792 aut de Oliveira Ferreira, Eric Victor verfasserin aut Viégas, Ismael de Jesus Matos verfasserin aut Enthalten in Journal of soil science and plant nutrition Springer International Publishing, 2010 24(2024), 2 vom: 22. März, Seite 2898-2909 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:24 year:2024 number:2 day:22 month:03 pages:2898-2909 https://dx.doi.org/10.1007/s42729-024-01716-x X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OLC-PHA SSG-OPC-FOR SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 48.30 VZ 58.52 VZ AR 24 2024 2 22 03 2898-2909 |
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10.1007/s42729-024-01716-x doi (DE-627)SPR056602952 (SPR)s42729-024-01716-x-e DE-627 ger DE-627 rakwb eng 630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl Paes da Silva, Rosa de Nazaré verfasserin aut Impact of Changes in Soil Attributes and Composition following Anthropization Related to Agricultural Practices in the Amazon Region 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) under exclusive licence to Sociedad Chilena de la Ciencia del Suelo 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract In response to the ongoing expansion of agriculture and land use changes in the Amazon region, new studies are necessary to understand the impacts of agricultural practices on Amazonian soils. The objective was to assess the changes induced in soil horizons by different management practices. The research was conducted in the National Forest of Caxiuanã, located in the municipality of Melgaço, Pará State, Brazil. A completely randomized 3 × 4 factorial design was employed, incorporating three types of vegetation (20-year-old secondary forest—$ Soil_{FS20} $, 5-year-old secondary forest—$ Soil_{FS5} $, and coivara—cutting and burning of native vegetation—$ Soil_{LTM} $) and four effective soil depths (0–5 cm, 5–10 cm, 10–20 cm, and 20–30 cm), with nine replicates for each combination. To enhance accuracy of the required assessment of the modifications induced in the physical and chemical attributes of the soil, isotopic composition of $ δ^{13} $C and $ δ^{15} $N was utilized. In areas subjected to clearing ($ Soil_{FS5} $ and $ Soil_{LTM} $), significant concentrations of carbon (C) and nitrogen (N) were observed in the 20–30 cm depth due to soil disturbance, which incorporated the litter into the deeper horizons. However, no significant differences in the C/N ratio were detected among the studied areas at the effective soil depth. Regardless of soil depth, $ Soil_{FS20} $ exhibited lower acidity, $ δ^{13} $C, $ δ^{15} $N, sandy and clay content, as well as iron (Fe) content, while displaying higher levels of SOM, zinc (Zn), calcium (Ca), manganese (Mn), potassium (K), silt, sodium (Na), copper (Cu), and phosphorus (P) content compared to the other sites. The results showed significant variations in the chemical and physical properties of the soil among the study sites, with $ Soil_{FS20} $ standing out in several characteristics. The increase in carbon stock in $ Soil_{FS20} $ indicated positive responses to specific management practices. Analyses of carbon, nitrogen concentrations, and stable isotopes highlighted $ Soil_{FS5} $ as distinctly different from the others. These findings contribute to the understanding of soil dynamics under different management practices, providing valuable insights for sustainable natural resource management in the region. Soil anthropization (dpeaa)DE-He213 Soil chemical attributes (dpeaa)DE-He213 Stable isotope analysis (dpeaa)DE-He213 Soil organic matter (dpeaa)DE-He213 Soil management (dpeaa)DE-He213 de Souza Mateus, Nikolas verfasserin aut dos Santos, Cássio Rafael Costa verfasserin aut Costa, Milton Garcia verfasserin (orcid)0000-0003-0105-8792 aut de Oliveira Ferreira, Eric Victor verfasserin aut Viégas, Ismael de Jesus Matos verfasserin aut Enthalten in Journal of soil science and plant nutrition Springer International Publishing, 2010 24(2024), 2 vom: 22. März, Seite 2898-2909 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:24 year:2024 number:2 day:22 month:03 pages:2898-2909 https://dx.doi.org/10.1007/s42729-024-01716-x X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OLC-PHA SSG-OPC-FOR SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 48.30 VZ 58.52 VZ AR 24 2024 2 22 03 2898-2909 |
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10.1007/s42729-024-01716-x doi (DE-627)SPR056602952 (SPR)s42729-024-01716-x-e DE-627 ger DE-627 rakwb eng 630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl Paes da Silva, Rosa de Nazaré verfasserin aut Impact of Changes in Soil Attributes and Composition following Anthropization Related to Agricultural Practices in the Amazon Region 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) under exclusive licence to Sociedad Chilena de la Ciencia del Suelo 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract In response to the ongoing expansion of agriculture and land use changes in the Amazon region, new studies are necessary to understand the impacts of agricultural practices on Amazonian soils. The objective was to assess the changes induced in soil horizons by different management practices. The research was conducted in the National Forest of Caxiuanã, located in the municipality of Melgaço, Pará State, Brazil. A completely randomized 3 × 4 factorial design was employed, incorporating three types of vegetation (20-year-old secondary forest—$ Soil_{FS20} $, 5-year-old secondary forest—$ Soil_{FS5} $, and coivara—cutting and burning of native vegetation—$ Soil_{LTM} $) and four effective soil depths (0–5 cm, 5–10 cm, 10–20 cm, and 20–30 cm), with nine replicates for each combination. To enhance accuracy of the required assessment of the modifications induced in the physical and chemical attributes of the soil, isotopic composition of $ δ^{13} $C and $ δ^{15} $N was utilized. In areas subjected to clearing ($ Soil_{FS5} $ and $ Soil_{LTM} $), significant concentrations of carbon (C) and nitrogen (N) were observed in the 20–30 cm depth due to soil disturbance, which incorporated the litter into the deeper horizons. However, no significant differences in the C/N ratio were detected among the studied areas at the effective soil depth. Regardless of soil depth, $ Soil_{FS20} $ exhibited lower acidity, $ δ^{13} $C, $ δ^{15} $N, sandy and clay content, as well as iron (Fe) content, while displaying higher levels of SOM, zinc (Zn), calcium (Ca), manganese (Mn), potassium (K), silt, sodium (Na), copper (Cu), and phosphorus (P) content compared to the other sites. The results showed significant variations in the chemical and physical properties of the soil among the study sites, with $ Soil_{FS20} $ standing out in several characteristics. The increase in carbon stock in $ Soil_{FS20} $ indicated positive responses to specific management practices. Analyses of carbon, nitrogen concentrations, and stable isotopes highlighted $ Soil_{FS5} $ as distinctly different from the others. These findings contribute to the understanding of soil dynamics under different management practices, providing valuable insights for sustainable natural resource management in the region. Soil anthropization (dpeaa)DE-He213 Soil chemical attributes (dpeaa)DE-He213 Stable isotope analysis (dpeaa)DE-He213 Soil organic matter (dpeaa)DE-He213 Soil management (dpeaa)DE-He213 de Souza Mateus, Nikolas verfasserin aut dos Santos, Cássio Rafael Costa verfasserin aut Costa, Milton Garcia verfasserin (orcid)0000-0003-0105-8792 aut de Oliveira Ferreira, Eric Victor verfasserin aut Viégas, Ismael de Jesus Matos verfasserin aut Enthalten in Journal of soil science and plant nutrition Springer International Publishing, 2010 24(2024), 2 vom: 22. März, Seite 2898-2909 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:24 year:2024 number:2 day:22 month:03 pages:2898-2909 https://dx.doi.org/10.1007/s42729-024-01716-x X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OLC-PHA SSG-OPC-FOR SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 48.30 VZ 58.52 VZ AR 24 2024 2 22 03 2898-2909 |
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10.1007/s42729-024-01716-x doi (DE-627)SPR056602952 (SPR)s42729-024-01716-x-e DE-627 ger DE-627 rakwb eng 630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl Paes da Silva, Rosa de Nazaré verfasserin aut Impact of Changes in Soil Attributes and Composition following Anthropization Related to Agricultural Practices in the Amazon Region 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) under exclusive licence to Sociedad Chilena de la Ciencia del Suelo 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract In response to the ongoing expansion of agriculture and land use changes in the Amazon region, new studies are necessary to understand the impacts of agricultural practices on Amazonian soils. The objective was to assess the changes induced in soil horizons by different management practices. The research was conducted in the National Forest of Caxiuanã, located in the municipality of Melgaço, Pará State, Brazil. A completely randomized 3 × 4 factorial design was employed, incorporating three types of vegetation (20-year-old secondary forest—$ Soil_{FS20} $, 5-year-old secondary forest—$ Soil_{FS5} $, and coivara—cutting and burning of native vegetation—$ Soil_{LTM} $) and four effective soil depths (0–5 cm, 5–10 cm, 10–20 cm, and 20–30 cm), with nine replicates for each combination. To enhance accuracy of the required assessment of the modifications induced in the physical and chemical attributes of the soil, isotopic composition of $ δ^{13} $C and $ δ^{15} $N was utilized. In areas subjected to clearing ($ Soil_{FS5} $ and $ Soil_{LTM} $), significant concentrations of carbon (C) and nitrogen (N) were observed in the 20–30 cm depth due to soil disturbance, which incorporated the litter into the deeper horizons. However, no significant differences in the C/N ratio were detected among the studied areas at the effective soil depth. Regardless of soil depth, $ Soil_{FS20} $ exhibited lower acidity, $ δ^{13} $C, $ δ^{15} $N, sandy and clay content, as well as iron (Fe) content, while displaying higher levels of SOM, zinc (Zn), calcium (Ca), manganese (Mn), potassium (K), silt, sodium (Na), copper (Cu), and phosphorus (P) content compared to the other sites. The results showed significant variations in the chemical and physical properties of the soil among the study sites, with $ Soil_{FS20} $ standing out in several characteristics. The increase in carbon stock in $ Soil_{FS20} $ indicated positive responses to specific management practices. Analyses of carbon, nitrogen concentrations, and stable isotopes highlighted $ Soil_{FS5} $ as distinctly different from the others. These findings contribute to the understanding of soil dynamics under different management practices, providing valuable insights for sustainable natural resource management in the region. Soil anthropization (dpeaa)DE-He213 Soil chemical attributes (dpeaa)DE-He213 Stable isotope analysis (dpeaa)DE-He213 Soil organic matter (dpeaa)DE-He213 Soil management (dpeaa)DE-He213 de Souza Mateus, Nikolas verfasserin aut dos Santos, Cássio Rafael Costa verfasserin aut Costa, Milton Garcia verfasserin (orcid)0000-0003-0105-8792 aut de Oliveira Ferreira, Eric Victor verfasserin aut Viégas, Ismael de Jesus Matos verfasserin aut Enthalten in Journal of soil science and plant nutrition Springer International Publishing, 2010 24(2024), 2 vom: 22. März, Seite 2898-2909 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:24 year:2024 number:2 day:22 month:03 pages:2898-2909 https://dx.doi.org/10.1007/s42729-024-01716-x X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OLC-PHA SSG-OPC-FOR SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 48.30 VZ 58.52 VZ AR 24 2024 2 22 03 2898-2909 |
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Paes da Silva, Rosa de Nazaré @@aut@@ de Souza Mateus, Nikolas @@aut@@ dos Santos, Cássio Rafael Costa @@aut@@ Costa, Milton Garcia @@aut@@ de Oliveira Ferreira, Eric Victor @@aut@@ Viégas, Ismael de Jesus Matos @@aut@@ |
| publishDateDaySort_date |
2024-03-22T00:00:00Z |
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661265102 |
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3630 |
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SPR056602952 |
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englisch |
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Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract In response to the ongoing expansion of agriculture and land use changes in the Amazon region, new studies are necessary to understand the impacts of agricultural practices on Amazonian soils. The objective was to assess the changes induced in soil horizons by different management practices. The research was conducted in the National Forest of Caxiuanã, located in the municipality of Melgaço, Pará State, Brazil. A completely randomized 3 × 4 factorial design was employed, incorporating three types of vegetation (20-year-old secondary forest—$ Soil_{FS20} $, 5-year-old secondary forest—$ Soil_{FS5} $, and coivara—cutting and burning of native vegetation—$ Soil_{LTM} $) and four effective soil depths (0–5 cm, 5–10 cm, 10–20 cm, and 20–30 cm), with nine replicates for each combination. To enhance accuracy of the required assessment of the modifications induced in the physical and chemical attributes of the soil, isotopic composition of $ δ^{13} $C and $ δ^{15} $N was utilized. In areas subjected to clearing ($ Soil_{FS5} $ and $ Soil_{LTM} $), significant concentrations of carbon (C) and nitrogen (N) were observed in the 20–30 cm depth due to soil disturbance, which incorporated the litter into the deeper horizons. However, no significant differences in the C/N ratio were detected among the studied areas at the effective soil depth. Regardless of soil depth, $ Soil_{FS20} $ exhibited lower acidity, $ δ^{13} $C, $ δ^{15} $N, sandy and clay content, as well as iron (Fe) content, while displaying higher levels of SOM, zinc (Zn), calcium (Ca), manganese (Mn), potassium (K), silt, sodium (Na), copper (Cu), and phosphorus (P) content compared to the other sites. The results showed significant variations in the chemical and physical properties of the soil among the study sites, with $ Soil_{FS20} $ standing out in several characteristics. The increase in carbon stock in $ Soil_{FS20} $ indicated positive responses to specific management practices. Analyses of carbon, nitrogen concentrations, and stable isotopes highlighted $ Soil_{FS5} $ as distinctly different from the others. 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|
| author |
Paes da Silva, Rosa de Nazaré |
| spellingShingle |
Paes da Silva, Rosa de Nazaré ddc 630 ddc 580 bkl 48.30 bkl 58.52 misc Soil anthropization misc Soil chemical attributes misc Stable isotope analysis misc Soil organic matter misc Soil management Impact of Changes in Soil Attributes and Composition following Anthropization Related to Agricultural Practices in the Amazon Region |
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Paes da Silva, Rosa de Nazaré |
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electronic Article |
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630 - Agriculture & related technologies 570 - Life sciences; biology 580 - Plants (Botany) |
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keep |
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aut aut aut aut aut aut |
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springer |
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true |
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Not Illustrated |
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0718-9516 |
| topic_title |
630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl Impact of Changes in Soil Attributes and Composition following Anthropization Related to Agricultural Practices in the Amazon Region Soil anthropization (dpeaa)DE-He213 Soil chemical attributes (dpeaa)DE-He213 Stable isotope analysis (dpeaa)DE-He213 Soil organic matter (dpeaa)DE-He213 Soil management (dpeaa)DE-He213 |
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impact of changes in soil attributes and composition following anthropization related to agricultural practices in the amazon region |
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Impact of Changes in Soil Attributes and Composition following Anthropization Related to Agricultural Practices in the Amazon Region |
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Abstract In response to the ongoing expansion of agriculture and land use changes in the Amazon region, new studies are necessary to understand the impacts of agricultural practices on Amazonian soils. The objective was to assess the changes induced in soil horizons by different management practices. The research was conducted in the National Forest of Caxiuanã, located in the municipality of Melgaço, Pará State, Brazil. A completely randomized 3 × 4 factorial design was employed, incorporating three types of vegetation (20-year-old secondary forest—$ Soil_{FS20} $, 5-year-old secondary forest—$ Soil_{FS5} $, and coivara—cutting and burning of native vegetation—$ Soil_{LTM} $) and four effective soil depths (0–5 cm, 5–10 cm, 10–20 cm, and 20–30 cm), with nine replicates for each combination. To enhance accuracy of the required assessment of the modifications induced in the physical and chemical attributes of the soil, isotopic composition of $ δ^{13} $C and $ δ^{15} $N was utilized. In areas subjected to clearing ($ Soil_{FS5} $ and $ Soil_{LTM} $), significant concentrations of carbon (C) and nitrogen (N) were observed in the 20–30 cm depth due to soil disturbance, which incorporated the litter into the deeper horizons. However, no significant differences in the C/N ratio were detected among the studied areas at the effective soil depth. Regardless of soil depth, $ Soil_{FS20} $ exhibited lower acidity, $ δ^{13} $C, $ δ^{15} $N, sandy and clay content, as well as iron (Fe) content, while displaying higher levels of SOM, zinc (Zn), calcium (Ca), manganese (Mn), potassium (K), silt, sodium (Na), copper (Cu), and phosphorus (P) content compared to the other sites. The results showed significant variations in the chemical and physical properties of the soil among the study sites, with $ Soil_{FS20} $ standing out in several characteristics. The increase in carbon stock in $ Soil_{FS20} $ indicated positive responses to specific management practices. Analyses of carbon, nitrogen concentrations, and stable isotopes highlighted $ Soil_{FS5} $ as distinctly different from the others. These findings contribute to the understanding of soil dynamics under different management practices, providing valuable insights for sustainable natural resource management in the region. © The Author(s) under exclusive licence to Sociedad Chilena de la Ciencia del Suelo 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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Abstract In response to the ongoing expansion of agriculture and land use changes in the Amazon region, new studies are necessary to understand the impacts of agricultural practices on Amazonian soils. The objective was to assess the changes induced in soil horizons by different management practices. The research was conducted in the National Forest of Caxiuanã, located in the municipality of Melgaço, Pará State, Brazil. A completely randomized 3 × 4 factorial design was employed, incorporating three types of vegetation (20-year-old secondary forest—$ Soil_{FS20} $, 5-year-old secondary forest—$ Soil_{FS5} $, and coivara—cutting and burning of native vegetation—$ Soil_{LTM} $) and four effective soil depths (0–5 cm, 5–10 cm, 10–20 cm, and 20–30 cm), with nine replicates for each combination. To enhance accuracy of the required assessment of the modifications induced in the physical and chemical attributes of the soil, isotopic composition of $ δ^{13} $C and $ δ^{15} $N was utilized. In areas subjected to clearing ($ Soil_{FS5} $ and $ Soil_{LTM} $), significant concentrations of carbon (C) and nitrogen (N) were observed in the 20–30 cm depth due to soil disturbance, which incorporated the litter into the deeper horizons. However, no significant differences in the C/N ratio were detected among the studied areas at the effective soil depth. Regardless of soil depth, $ Soil_{FS20} $ exhibited lower acidity, $ δ^{13} $C, $ δ^{15} $N, sandy and clay content, as well as iron (Fe) content, while displaying higher levels of SOM, zinc (Zn), calcium (Ca), manganese (Mn), potassium (K), silt, sodium (Na), copper (Cu), and phosphorus (P) content compared to the other sites. The results showed significant variations in the chemical and physical properties of the soil among the study sites, with $ Soil_{FS20} $ standing out in several characteristics. The increase in carbon stock in $ Soil_{FS20} $ indicated positive responses to specific management practices. Analyses of carbon, nitrogen concentrations, and stable isotopes highlighted $ Soil_{FS5} $ as distinctly different from the others. These findings contribute to the understanding of soil dynamics under different management practices, providing valuable insights for sustainable natural resource management in the region. © The Author(s) under exclusive licence to Sociedad Chilena de la Ciencia del Suelo 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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Abstract In response to the ongoing expansion of agriculture and land use changes in the Amazon region, new studies are necessary to understand the impacts of agricultural practices on Amazonian soils. The objective was to assess the changes induced in soil horizons by different management practices. The research was conducted in the National Forest of Caxiuanã, located in the municipality of Melgaço, Pará State, Brazil. A completely randomized 3 × 4 factorial design was employed, incorporating three types of vegetation (20-year-old secondary forest—$ Soil_{FS20} $, 5-year-old secondary forest—$ Soil_{FS5} $, and coivara—cutting and burning of native vegetation—$ Soil_{LTM} $) and four effective soil depths (0–5 cm, 5–10 cm, 10–20 cm, and 20–30 cm), with nine replicates for each combination. To enhance accuracy of the required assessment of the modifications induced in the physical and chemical attributes of the soil, isotopic composition of $ δ^{13} $C and $ δ^{15} $N was utilized. In areas subjected to clearing ($ Soil_{FS5} $ and $ Soil_{LTM} $), significant concentrations of carbon (C) and nitrogen (N) were observed in the 20–30 cm depth due to soil disturbance, which incorporated the litter into the deeper horizons. However, no significant differences in the C/N ratio were detected among the studied areas at the effective soil depth. Regardless of soil depth, $ Soil_{FS20} $ exhibited lower acidity, $ δ^{13} $C, $ δ^{15} $N, sandy and clay content, as well as iron (Fe) content, while displaying higher levels of SOM, zinc (Zn), calcium (Ca), manganese (Mn), potassium (K), silt, sodium (Na), copper (Cu), and phosphorus (P) content compared to the other sites. The results showed significant variations in the chemical and physical properties of the soil among the study sites, with $ Soil_{FS20} $ standing out in several characteristics. The increase in carbon stock in $ Soil_{FS20} $ indicated positive responses to specific management practices. Analyses of carbon, nitrogen concentrations, and stable isotopes highlighted $ Soil_{FS5} $ as distinctly different from the others. These findings contribute to the understanding of soil dynamics under different management practices, providing valuable insights for sustainable natural resource management in the region. © The Author(s) under exclusive licence to Sociedad Chilena de la Ciencia del Suelo 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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| score |
7.4018955 |