The Fate of Soil Organic Carbon from Compost: A Pot Test Study Using Labile Carbon and 13c Natural Abundance
Abstract Recycled organic waste (OW) can be a valuable nutrient source for plant cultivation; however, knowledge is poor regarding its effect on soil carbon conservation, especially in the frame of organic-mineral fertilisation succession. In this study, four composts, green waste (GWC), anaerobical...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Grigatti, Marco [verfasserIn] Ciavatta, Claudio [verfasserIn] Marzadori, Claudio [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) 2024 |
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| Übergeordnetes Werk: |
Enthalten in: Journal of soil science and plant nutrition - Springer International Publishing, 2010, 24(2024), 2 vom: 27. Feb., Seite 2589-2598 |
|---|---|
| Übergeordnetes Werk: |
volume:24 ; year:2024 ; number:2 ; day:27 ; month:02 ; pages:2589-2598 |
| Links: |
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| DOI / URN: |
10.1007/s42729-024-01680-6 |
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| Katalog-ID: |
SPR056602596 |
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| 520 | |a Abstract Recycled organic waste (OW) can be a valuable nutrient source for plant cultivation; however, knowledge is poor regarding its effect on soil carbon conservation, especially in the frame of organic-mineral fertilisation succession. In this study, four composts, green waste (GWC), anaerobically digested bio-waste (DC), sludge (SSC), and bio-waste (BWC), were compared (10 and 20 Mg volatile solids $ ha^{−1} $) in a ryegrass pot test over two growing cycles (112 + 112 days), along with an unamended control (Ctrl) and a chemical reference (Chem), with and without mineral nitrogen (N) fertilisation. At the end of the two growth cycles, the pot soil was analysed for total- (TOC) and labile-carbon ($ C_{L} $) as well as for 13C isotope natural abundance ($ δ^{13} $C and $ Δ^{13} $C vs. Chem). At day 112, the pot test showed that Ctrl and Chem gained poor TOC (8.48 g $ kg^{−1} $), lower than the compost at both 10 and 20 Mg volatile solids $ ha^{−1} $ (10.01 vs. 11.59 g $ kg^{−1} $). At day 224, a deep soil TOC depletion occurred in the pot soil treated with GWC, DC and BWC at both levels (-10 and -20). However, all the compost treatments showed more depleted soil $ d^{13} $C vs. the references, especially Chem, thus revealing relevant compost-derived carbon conservation. Regarding the compost treatments, the carbon management index (CMI) increased over time, indicating high soil functionality, also showing a good relationship with $ δ^{13} $C, suggesting a probable increase in relative lignin which could have been linked to carbon conservation and increased functionality. | ||
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| 700 | 1 | |a Marzadori, Claudio |e verfasserin |4 aut | |
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10.1007/s42729-024-01680-6 doi (DE-627)SPR056602596 (SPR)s42729-024-01680-6-e DE-627 ger DE-627 rakwb eng 630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl Grigatti, Marco verfasserin (orcid)0000-0001-6305-2391 aut The Fate of Soil Organic Carbon from Compost: A Pot Test Study Using Labile Carbon and 13c Natural Abundance 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2024 Abstract Recycled organic waste (OW) can be a valuable nutrient source for plant cultivation; however, knowledge is poor regarding its effect on soil carbon conservation, especially in the frame of organic-mineral fertilisation succession. In this study, four composts, green waste (GWC), anaerobically digested bio-waste (DC), sludge (SSC), and bio-waste (BWC), were compared (10 and 20 Mg volatile solids $ ha^{−1} $) in a ryegrass pot test over two growing cycles (112 + 112 days), along with an unamended control (Ctrl) and a chemical reference (Chem), with and without mineral nitrogen (N) fertilisation. At the end of the two growth cycles, the pot soil was analysed for total- (TOC) and labile-carbon ($ C_{L} $) as well as for 13C isotope natural abundance ($ δ^{13} $C and $ Δ^{13} $C vs. Chem). At day 112, the pot test showed that Ctrl and Chem gained poor TOC (8.48 g $ kg^{−1} $), lower than the compost at both 10 and 20 Mg volatile solids $ ha^{−1} $ (10.01 vs. 11.59 g $ kg^{−1} $). At day 224, a deep soil TOC depletion occurred in the pot soil treated with GWC, DC and BWC at both levels (-10 and -20). However, all the compost treatments showed more depleted soil $ d^{13} $C vs. the references, especially Chem, thus revealing relevant compost-derived carbon conservation. Regarding the compost treatments, the carbon management index (CMI) increased over time, indicating high soil functionality, also showing a good relationship with $ δ^{13} $C, suggesting a probable increase in relative lignin which could have been linked to carbon conservation and increased functionality. Organic waste (dpeaa)DE-He213 Recycling (dpeaa)DE-He213 Carbon storage (dpeaa)DE-He213 KMnO (dpeaa)DE-He213 oxidisable organic carbon (dpeaa)DE-He213 Soil functionality (dpeaa)DE-He213 Δ (dpeaa)DE-He213 C (dpeaa)DE-He213 Ciavatta, Claudio verfasserin aut Marzadori, Claudio verfasserin aut Enthalten in Journal of soil science and plant nutrition Springer International Publishing, 2010 24(2024), 2 vom: 27. Feb., Seite 2589-2598 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:24 year:2024 number:2 day:27 month:02 pages:2589-2598 https://dx.doi.org/10.1007/s42729-024-01680-6 X:SPRINGER Resolving-System kostenfrei 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 27 02 2589-2598 |
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10.1007/s42729-024-01680-6 doi (DE-627)SPR056602596 (SPR)s42729-024-01680-6-e DE-627 ger DE-627 rakwb eng 630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl Grigatti, Marco verfasserin (orcid)0000-0001-6305-2391 aut The Fate of Soil Organic Carbon from Compost: A Pot Test Study Using Labile Carbon and 13c Natural Abundance 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2024 Abstract Recycled organic waste (OW) can be a valuable nutrient source for plant cultivation; however, knowledge is poor regarding its effect on soil carbon conservation, especially in the frame of organic-mineral fertilisation succession. In this study, four composts, green waste (GWC), anaerobically digested bio-waste (DC), sludge (SSC), and bio-waste (BWC), were compared (10 and 20 Mg volatile solids $ ha^{−1} $) in a ryegrass pot test over two growing cycles (112 + 112 days), along with an unamended control (Ctrl) and a chemical reference (Chem), with and without mineral nitrogen (N) fertilisation. At the end of the two growth cycles, the pot soil was analysed for total- (TOC) and labile-carbon ($ C_{L} $) as well as for 13C isotope natural abundance ($ δ^{13} $C and $ Δ^{13} $C vs. Chem). At day 112, the pot test showed that Ctrl and Chem gained poor TOC (8.48 g $ kg^{−1} $), lower than the compost at both 10 and 20 Mg volatile solids $ ha^{−1} $ (10.01 vs. 11.59 g $ kg^{−1} $). At day 224, a deep soil TOC depletion occurred in the pot soil treated with GWC, DC and BWC at both levels (-10 and -20). However, all the compost treatments showed more depleted soil $ d^{13} $C vs. the references, especially Chem, thus revealing relevant compost-derived carbon conservation. Regarding the compost treatments, the carbon management index (CMI) increased over time, indicating high soil functionality, also showing a good relationship with $ δ^{13} $C, suggesting a probable increase in relative lignin which could have been linked to carbon conservation and increased functionality. Organic waste (dpeaa)DE-He213 Recycling (dpeaa)DE-He213 Carbon storage (dpeaa)DE-He213 KMnO (dpeaa)DE-He213 oxidisable organic carbon (dpeaa)DE-He213 Soil functionality (dpeaa)DE-He213 Δ (dpeaa)DE-He213 C (dpeaa)DE-He213 Ciavatta, Claudio verfasserin aut Marzadori, Claudio verfasserin aut Enthalten in Journal of soil science and plant nutrition Springer International Publishing, 2010 24(2024), 2 vom: 27. Feb., Seite 2589-2598 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:24 year:2024 number:2 day:27 month:02 pages:2589-2598 https://dx.doi.org/10.1007/s42729-024-01680-6 X:SPRINGER Resolving-System kostenfrei 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 27 02 2589-2598 |
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10.1007/s42729-024-01680-6 doi (DE-627)SPR056602596 (SPR)s42729-024-01680-6-e DE-627 ger DE-627 rakwb eng 630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl Grigatti, Marco verfasserin (orcid)0000-0001-6305-2391 aut The Fate of Soil Organic Carbon from Compost: A Pot Test Study Using Labile Carbon and 13c Natural Abundance 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2024 Abstract Recycled organic waste (OW) can be a valuable nutrient source for plant cultivation; however, knowledge is poor regarding its effect on soil carbon conservation, especially in the frame of organic-mineral fertilisation succession. In this study, four composts, green waste (GWC), anaerobically digested bio-waste (DC), sludge (SSC), and bio-waste (BWC), were compared (10 and 20 Mg volatile solids $ ha^{−1} $) in a ryegrass pot test over two growing cycles (112 + 112 days), along with an unamended control (Ctrl) and a chemical reference (Chem), with and without mineral nitrogen (N) fertilisation. At the end of the two growth cycles, the pot soil was analysed for total- (TOC) and labile-carbon ($ C_{L} $) as well as for 13C isotope natural abundance ($ δ^{13} $C and $ Δ^{13} $C vs. Chem). At day 112, the pot test showed that Ctrl and Chem gained poor TOC (8.48 g $ kg^{−1} $), lower than the compost at both 10 and 20 Mg volatile solids $ ha^{−1} $ (10.01 vs. 11.59 g $ kg^{−1} $). At day 224, a deep soil TOC depletion occurred in the pot soil treated with GWC, DC and BWC at both levels (-10 and -20). However, all the compost treatments showed more depleted soil $ d^{13} $C vs. the references, especially Chem, thus revealing relevant compost-derived carbon conservation. Regarding the compost treatments, the carbon management index (CMI) increased over time, indicating high soil functionality, also showing a good relationship with $ δ^{13} $C, suggesting a probable increase in relative lignin which could have been linked to carbon conservation and increased functionality. Organic waste (dpeaa)DE-He213 Recycling (dpeaa)DE-He213 Carbon storage (dpeaa)DE-He213 KMnO (dpeaa)DE-He213 oxidisable organic carbon (dpeaa)DE-He213 Soil functionality (dpeaa)DE-He213 Δ (dpeaa)DE-He213 C (dpeaa)DE-He213 Ciavatta, Claudio verfasserin aut Marzadori, Claudio verfasserin aut Enthalten in Journal of soil science and plant nutrition Springer International Publishing, 2010 24(2024), 2 vom: 27. Feb., Seite 2589-2598 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:24 year:2024 number:2 day:27 month:02 pages:2589-2598 https://dx.doi.org/10.1007/s42729-024-01680-6 X:SPRINGER Resolving-System kostenfrei 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 27 02 2589-2598 |
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10.1007/s42729-024-01680-6 doi (DE-627)SPR056602596 (SPR)s42729-024-01680-6-e DE-627 ger DE-627 rakwb eng 630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl Grigatti, Marco verfasserin (orcid)0000-0001-6305-2391 aut The Fate of Soil Organic Carbon from Compost: A Pot Test Study Using Labile Carbon and 13c Natural Abundance 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2024 Abstract Recycled organic waste (OW) can be a valuable nutrient source for plant cultivation; however, knowledge is poor regarding its effect on soil carbon conservation, especially in the frame of organic-mineral fertilisation succession. In this study, four composts, green waste (GWC), anaerobically digested bio-waste (DC), sludge (SSC), and bio-waste (BWC), were compared (10 and 20 Mg volatile solids $ ha^{−1} $) in a ryegrass pot test over two growing cycles (112 + 112 days), along with an unamended control (Ctrl) and a chemical reference (Chem), with and without mineral nitrogen (N) fertilisation. At the end of the two growth cycles, the pot soil was analysed for total- (TOC) and labile-carbon ($ C_{L} $) as well as for 13C isotope natural abundance ($ δ^{13} $C and $ Δ^{13} $C vs. Chem). At day 112, the pot test showed that Ctrl and Chem gained poor TOC (8.48 g $ kg^{−1} $), lower than the compost at both 10 and 20 Mg volatile solids $ ha^{−1} $ (10.01 vs. 11.59 g $ kg^{−1} $). At day 224, a deep soil TOC depletion occurred in the pot soil treated with GWC, DC and BWC at both levels (-10 and -20). However, all the compost treatments showed more depleted soil $ d^{13} $C vs. the references, especially Chem, thus revealing relevant compost-derived carbon conservation. Regarding the compost treatments, the carbon management index (CMI) increased over time, indicating high soil functionality, also showing a good relationship with $ δ^{13} $C, suggesting a probable increase in relative lignin which could have been linked to carbon conservation and increased functionality. Organic waste (dpeaa)DE-He213 Recycling (dpeaa)DE-He213 Carbon storage (dpeaa)DE-He213 KMnO (dpeaa)DE-He213 oxidisable organic carbon (dpeaa)DE-He213 Soil functionality (dpeaa)DE-He213 Δ (dpeaa)DE-He213 C (dpeaa)DE-He213 Ciavatta, Claudio verfasserin aut Marzadori, Claudio verfasserin aut Enthalten in Journal of soil science and plant nutrition Springer International Publishing, 2010 24(2024), 2 vom: 27. Feb., Seite 2589-2598 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:24 year:2024 number:2 day:27 month:02 pages:2589-2598 https://dx.doi.org/10.1007/s42729-024-01680-6 X:SPRINGER Resolving-System kostenfrei 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 27 02 2589-2598 |
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10.1007/s42729-024-01680-6 doi (DE-627)SPR056602596 (SPR)s42729-024-01680-6-e DE-627 ger DE-627 rakwb eng 630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl Grigatti, Marco verfasserin (orcid)0000-0001-6305-2391 aut The Fate of Soil Organic Carbon from Compost: A Pot Test Study Using Labile Carbon and 13c Natural Abundance 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2024 Abstract Recycled organic waste (OW) can be a valuable nutrient source for plant cultivation; however, knowledge is poor regarding its effect on soil carbon conservation, especially in the frame of organic-mineral fertilisation succession. In this study, four composts, green waste (GWC), anaerobically digested bio-waste (DC), sludge (SSC), and bio-waste (BWC), were compared (10 and 20 Mg volatile solids $ ha^{−1} $) in a ryegrass pot test over two growing cycles (112 + 112 days), along with an unamended control (Ctrl) and a chemical reference (Chem), with and without mineral nitrogen (N) fertilisation. At the end of the two growth cycles, the pot soil was analysed for total- (TOC) and labile-carbon ($ C_{L} $) as well as for 13C isotope natural abundance ($ δ^{13} $C and $ Δ^{13} $C vs. Chem). At day 112, the pot test showed that Ctrl and Chem gained poor TOC (8.48 g $ kg^{−1} $), lower than the compost at both 10 and 20 Mg volatile solids $ ha^{−1} $ (10.01 vs. 11.59 g $ kg^{−1} $). At day 224, a deep soil TOC depletion occurred in the pot soil treated with GWC, DC and BWC at both levels (-10 and -20). However, all the compost treatments showed more depleted soil $ d^{13} $C vs. the references, especially Chem, thus revealing relevant compost-derived carbon conservation. Regarding the compost treatments, the carbon management index (CMI) increased over time, indicating high soil functionality, also showing a good relationship with $ δ^{13} $C, suggesting a probable increase in relative lignin which could have been linked to carbon conservation and increased functionality. Organic waste (dpeaa)DE-He213 Recycling (dpeaa)DE-He213 Carbon storage (dpeaa)DE-He213 KMnO (dpeaa)DE-He213 oxidisable organic carbon (dpeaa)DE-He213 Soil functionality (dpeaa)DE-He213 Δ (dpeaa)DE-He213 C (dpeaa)DE-He213 Ciavatta, Claudio verfasserin aut Marzadori, Claudio verfasserin aut Enthalten in Journal of soil science and plant nutrition Springer International Publishing, 2010 24(2024), 2 vom: 27. Feb., Seite 2589-2598 (DE-627)661265102 (DE-600)2611093-3 0718-9516 nnns volume:24 year:2024 number:2 day:27 month:02 pages:2589-2598 https://dx.doi.org/10.1007/s42729-024-01680-6 X:SPRINGER Resolving-System kostenfrei 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 27 02 2589-2598 |
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English |
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Enthalten in Journal of soil science and plant nutrition 24(2024), 2 vom: 27. Feb., Seite 2589-2598 volume:24 year:2024 number:2 day:27 month:02 pages:2589-2598 |
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Enthalten in Journal of soil science and plant nutrition 24(2024), 2 vom: 27. Feb., Seite 2589-2598 volume:24 year:2024 number:2 day:27 month:02 pages:2589-2598 |
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Organic waste Recycling Carbon storage KMnO oxidisable organic carbon Soil functionality Δ C |
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Grigatti, Marco @@aut@@ Ciavatta, Claudio @@aut@@ Marzadori, Claudio @@aut@@ |
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In this study, four composts, green waste (GWC), anaerobically digested bio-waste (DC), sludge (SSC), and bio-waste (BWC), were compared (10 and 20 Mg volatile solids $ ha^{−1} $) in a ryegrass pot test over two growing cycles (112 + 112 days), along with an unamended control (Ctrl) and a chemical reference (Chem), with and without mineral nitrogen (N) fertilisation. At the end of the two growth cycles, the pot soil was analysed for total- (TOC) and labile-carbon ($ C_{L} $) as well as for 13C isotope natural abundance ($ δ^{13} $C and $ Δ^{13} $C vs. Chem). At day 112, the pot test showed that Ctrl and Chem gained poor TOC (8.48 g $ kg^{−1} $), lower than the compost at both 10 and 20 Mg volatile solids $ ha^{−1} $ (10.01 vs. 11.59 g $ kg^{−1} $). At day 224, a deep soil TOC depletion occurred in the pot soil treated with GWC, DC and BWC at both levels (-10 and -20). 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Grigatti, Marco |
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Grigatti, Marco ddc 630 ddc 580 bkl 48.30 bkl 58.52 misc Organic waste misc Recycling misc Carbon storage misc KMnO misc oxidisable organic carbon misc Soil functionality misc Δ misc C The Fate of Soil Organic Carbon from Compost: A Pot Test Study Using Labile Carbon and 13c Natural Abundance |
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630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl The Fate of Soil Organic Carbon from Compost: A Pot Test Study Using Labile Carbon and 13c Natural Abundance Organic waste (dpeaa)DE-He213 Recycling (dpeaa)DE-He213 Carbon storage (dpeaa)DE-He213 KMnO (dpeaa)DE-He213 oxidisable organic carbon (dpeaa)DE-He213 Soil functionality (dpeaa)DE-He213 Δ (dpeaa)DE-He213 C (dpeaa)DE-He213 |
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ddc 630 ddc 580 bkl 48.30 bkl 58.52 misc Organic waste misc Recycling misc Carbon storage misc KMnO misc oxidisable organic carbon misc Soil functionality misc Δ misc C |
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The Fate of Soil Organic Carbon from Compost: A Pot Test Study Using Labile Carbon and 13c Natural Abundance |
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Grigatti, Marco |
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Journal of soil science and plant nutrition |
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Journal of soil science and plant nutrition |
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2024 |
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Grigatti, Marco Ciavatta, Claudio Marzadori, Claudio |
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630 570 VZ 580 630 VZ 48.30 bkl 58.52 bkl |
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Elektronische Aufsätze |
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Grigatti, Marco |
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10.1007/s42729-024-01680-6 |
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the fate of soil organic carbon from compost: a pot test study using labile carbon and 13c natural abundance |
| title_auth |
The Fate of Soil Organic Carbon from Compost: A Pot Test Study Using Labile Carbon and 13c Natural Abundance |
| abstract |
Abstract Recycled organic waste (OW) can be a valuable nutrient source for plant cultivation; however, knowledge is poor regarding its effect on soil carbon conservation, especially in the frame of organic-mineral fertilisation succession. In this study, four composts, green waste (GWC), anaerobically digested bio-waste (DC), sludge (SSC), and bio-waste (BWC), were compared (10 and 20 Mg volatile solids $ ha^{−1} $) in a ryegrass pot test over two growing cycles (112 + 112 days), along with an unamended control (Ctrl) and a chemical reference (Chem), with and without mineral nitrogen (N) fertilisation. At the end of the two growth cycles, the pot soil was analysed for total- (TOC) and labile-carbon ($ C_{L} $) as well as for 13C isotope natural abundance ($ δ^{13} $C and $ Δ^{13} $C vs. Chem). At day 112, the pot test showed that Ctrl and Chem gained poor TOC (8.48 g $ kg^{−1} $), lower than the compost at both 10 and 20 Mg volatile solids $ ha^{−1} $ (10.01 vs. 11.59 g $ kg^{−1} $). At day 224, a deep soil TOC depletion occurred in the pot soil treated with GWC, DC and BWC at both levels (-10 and -20). However, all the compost treatments showed more depleted soil $ d^{13} $C vs. the references, especially Chem, thus revealing relevant compost-derived carbon conservation. Regarding the compost treatments, the carbon management index (CMI) increased over time, indicating high soil functionality, also showing a good relationship with $ δ^{13} $C, suggesting a probable increase in relative lignin which could have been linked to carbon conservation and increased functionality. © The Author(s) 2024 |
| abstractGer |
Abstract Recycled organic waste (OW) can be a valuable nutrient source for plant cultivation; however, knowledge is poor regarding its effect on soil carbon conservation, especially in the frame of organic-mineral fertilisation succession. In this study, four composts, green waste (GWC), anaerobically digested bio-waste (DC), sludge (SSC), and bio-waste (BWC), were compared (10 and 20 Mg volatile solids $ ha^{−1} $) in a ryegrass pot test over two growing cycles (112 + 112 days), along with an unamended control (Ctrl) and a chemical reference (Chem), with and without mineral nitrogen (N) fertilisation. At the end of the two growth cycles, the pot soil was analysed for total- (TOC) and labile-carbon ($ C_{L} $) as well as for 13C isotope natural abundance ($ δ^{13} $C and $ Δ^{13} $C vs. Chem). At day 112, the pot test showed that Ctrl and Chem gained poor TOC (8.48 g $ kg^{−1} $), lower than the compost at both 10 and 20 Mg volatile solids $ ha^{−1} $ (10.01 vs. 11.59 g $ kg^{−1} $). At day 224, a deep soil TOC depletion occurred in the pot soil treated with GWC, DC and BWC at both levels (-10 and -20). However, all the compost treatments showed more depleted soil $ d^{13} $C vs. the references, especially Chem, thus revealing relevant compost-derived carbon conservation. Regarding the compost treatments, the carbon management index (CMI) increased over time, indicating high soil functionality, also showing a good relationship with $ δ^{13} $C, suggesting a probable increase in relative lignin which could have been linked to carbon conservation and increased functionality. © The Author(s) 2024 |
| abstract_unstemmed |
Abstract Recycled organic waste (OW) can be a valuable nutrient source for plant cultivation; however, knowledge is poor regarding its effect on soil carbon conservation, especially in the frame of organic-mineral fertilisation succession. In this study, four composts, green waste (GWC), anaerobically digested bio-waste (DC), sludge (SSC), and bio-waste (BWC), were compared (10 and 20 Mg volatile solids $ ha^{−1} $) in a ryegrass pot test over two growing cycles (112 + 112 days), along with an unamended control (Ctrl) and a chemical reference (Chem), with and without mineral nitrogen (N) fertilisation. At the end of the two growth cycles, the pot soil was analysed for total- (TOC) and labile-carbon ($ C_{L} $) as well as for 13C isotope natural abundance ($ δ^{13} $C and $ Δ^{13} $C vs. Chem). At day 112, the pot test showed that Ctrl and Chem gained poor TOC (8.48 g $ kg^{−1} $), lower than the compost at both 10 and 20 Mg volatile solids $ ha^{−1} $ (10.01 vs. 11.59 g $ kg^{−1} $). At day 224, a deep soil TOC depletion occurred in the pot soil treated with GWC, DC and BWC at both levels (-10 and -20). However, all the compost treatments showed more depleted soil $ d^{13} $C vs. the references, especially Chem, thus revealing relevant compost-derived carbon conservation. Regarding the compost treatments, the carbon management index (CMI) increased over time, indicating high soil functionality, also showing a good relationship with $ δ^{13} $C, suggesting a probable increase in relative lignin which could have been linked to carbon conservation and increased functionality. © The Author(s) 2024 |
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| title_short |
The Fate of Soil Organic Carbon from Compost: A Pot Test Study Using Labile Carbon and 13c Natural Abundance |
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| score |
7.402237 |