Global stocks and capacity of mineral-associated soil organic carbon
Soil is the largest terrestrial reservoir of organic carbon and is central for climate change mitigation and carbon-climate feedbacks. Chemical and physical associations of soil carbon with minerals play a critical role in carbon storage, but the amount and global capacity for storage in this form r...
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| Vydáno v: | Nature communications Ročník 13; číslo 1; s. 3797 |
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| Hlavní autoři: | , , , , , , , , , , , |
| Médium: | Journal Article |
| Jazyk: | angličtina |
| Vydáno: |
London
Nature Publishing Group UK
01.07.2022
Nature Publishing Group Nature Portfolio |
| Témata: | |
| ISSN: | 2041-1723, 2041-1723 |
| On-line přístup: | Získat plný text |
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| Abstract | Soil is the largest terrestrial reservoir of organic carbon and is central for climate change mitigation and carbon-climate feedbacks. Chemical and physical associations of soil carbon with minerals play a critical role in carbon storage, but the amount and global capacity for storage in this form remain unquantified. Here, we produce spatially-resolved global estimates of mineral-associated organic carbon stocks and carbon-storage capacity by analyzing 1144 globally-distributed soil profiles. We show that current stocks total 899 Pg C to a depth of 1 m in non-permafrost mineral soils. Although this constitutes 66% and 70% of soil carbon in surface and deeper layers, respectively, it is only 42% and 21% of the mineralogical capacity. Regions under agricultural management and deeper soil layers show the largest undersaturation of mineral-associated carbon. Critically, the degree of undersaturation indicates sequestration efficiency over years to decades. We show that, across 103 carbon-accrual measurements spanning management interventions globally, soils furthest from their mineralogical capacity are more effective at accruing carbon; sequestration rates average 3-times higher in soils at one tenth of their capacity compared to soils at one half of their capacity. Our findings provide insights into the world’s soils, their capacity to store carbon, and priority regions and actions for soil carbon management.
Mineral-organic associations play a key role in soil carbon preservation. Here, Georgiou et al. produce global estimates of mineral-associated soil carbon, providing insight into the world’s soils and their capacity to store carbon |
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| AbstractList | Soil is the largest terrestrial reservoir of organic carbon and is central for climate change mitigation and carbon-climate feedbacks. Chemical and physical associations of soil carbon with minerals play a critical role in carbon storage, but the amount and global capacity for storage in this form remain unquantified. Here, we produce spatially-resolved global estimates of mineral-associated organic carbon stocks and carbon-storage capacity by analyzing 1144 globally-distributed soil profiles. We show that current stocks total 899 Pg C to a depth of 1 m in non-permafrost mineral soils. Although this constitutes 66% and 70% of soil carbon in surface and deeper layers, respectively, it is only 42% and 21% of the mineralogical capacity. Regions under agricultural management and deeper soil layers show the largest undersaturation of mineral-associated carbon. Critically, the degree of undersaturation indicates sequestration efficiency over years to decades. We show that, across 103 carbon-accrual measurements spanning management interventions globally, soils furthest from their mineralogical capacity are more effective at accruing carbon; sequestration rates average 3-times higher in soils at one tenth of their capacity compared to soils at one half of their capacity. Our findings provide insights into the world’s soils, their capacity to store carbon, and priority regions and actions for soil carbon management.Mineral-organic associations play a key role in soil carbon preservation. Here, Georgiou et al. produce global estimates of mineral-associated soil carbon, providing insight into the world’s soils and their capacity to store carbon Soil is the largest terrestrial reservoir of organic carbon and is central for climate change mitigation and carbon-climate feedbacks. Chemical and physical associations of soil carbon with minerals play a critical role in carbon storage, but the amount and global capacity for storage in this form remain unquantified. Here, we produce spatially-resolved global estimates of mineral-associated organic carbon stocks and carbon-storage capacity by analyzing 1144 globally-distributed soil profiles. We show that current stocks total 899 Pg C to a depth of 1 m in non-permafrost mineral soils. Although this constitutes 66% and 70% of soil carbon in surface and deeper layers, respectively, it is only 42% and 21% of the mineralogical capacity. Regions under agricultural management and deeper soil layers show the largest undersaturation of mineral-associated carbon. Critically, the degree of undersaturation indicates sequestration efficiency over years to decades. We show that, across 103 carbon-accrual measurements spanning management interventions globally, soils furthest from their mineralogical capacity are more effective at accruing carbon; sequestration rates average 3-times higher in soils at one tenth of their capacity compared to soils at one half of their capacity. Our findings provide insights into the world's soils, their capacity to store carbon, and priority regions and actions for soil carbon management. Mineral-organic associations play a key role in soil carbon preservation. Here, Georgiou et al. produce global estimates of mineral-associated soil carbon, providing insight into the world’s soils and their capacity to store carbon Soil is the largest terrestrial reservoir of organic carbon and is central for climate change mitigation and carbon-climate feedbacks. Chemical and physical associations of soil carbon with minerals play a critical role in carbon storage, but the amount and global capacity for storage in this form remain unquantified. Here, we produce spatially-resolved global estimates of mineral-associated organic carbon stocks and carbon-storage capacity by analyzing 1144 globally-distributed soil profiles. We show that current stocks total 899 Pg C to a depth of 1 m in non-permafrost mineral soils. Although this constitutes 66% and 70% of soil carbon in surface and deeper layers, respectively, it is only 42% and 21% of the mineralogical capacity. Regions under agricultural management and deeper soil layers show the largest undersaturation of mineral-associated carbon. Critically, the degree of undersaturation indicates sequestration efficiency over years to decades. We show that, across 103 carbon-accrual measurements spanning management interventions globally, soils furthest from their mineralogical capacity are more effective at accruing carbon; sequestration rates average 3-times higher in soils at one tenth of their capacity compared to soils at one half of their capacity. Overall, our findings provide insights into the world’s soils, their capacity to store carbon, and priority regions and actions for soil carbon management. Soil is the largest terrestrial reservoir of organic carbon and is central for climate change mitigation and carbon-climate feedbacks. Chemical and physical associations of soil carbon with minerals play a critical role in carbon storage, but the amount and global capacity for storage in this form remain unquantified. Here, we produce spatially-resolved global estimates of mineral-associated organic carbon stocks and carbon-storage capacity by analyzing 1144 globally-distributed soil profiles. We show that current stocks total 899 Pg C to a depth of 1 m in non-permafrost mineral soils. Although this constitutes 66% and 70% of soil carbon in surface and deeper layers, respectively, it is only 42% and 21% of the mineralogical capacity. Regions under agricultural management and deeper soil layers show the largest undersaturation of mineral-associated carbon. Critically, the degree of undersaturation indicates sequestration efficiency over years to decades. We show that, across 103 carbon-accrual measurements spanning management interventions globally, soils furthest from their mineralogical capacity are more effective at accruing carbon; sequestration rates average 3-times higher in soils at one tenth of their capacity compared to soils at one half of their capacity. Our findings provide insights into the world's soils, their capacity to store carbon, and priority regions and actions for soil carbon management.Soil is the largest terrestrial reservoir of organic carbon and is central for climate change mitigation and carbon-climate feedbacks. Chemical and physical associations of soil carbon with minerals play a critical role in carbon storage, but the amount and global capacity for storage in this form remain unquantified. Here, we produce spatially-resolved global estimates of mineral-associated organic carbon stocks and carbon-storage capacity by analyzing 1144 globally-distributed soil profiles. We show that current stocks total 899 Pg C to a depth of 1 m in non-permafrost mineral soils. Although this constitutes 66% and 70% of soil carbon in surface and deeper layers, respectively, it is only 42% and 21% of the mineralogical capacity. Regions under agricultural management and deeper soil layers show the largest undersaturation of mineral-associated carbon. Critically, the degree of undersaturation indicates sequestration efficiency over years to decades. We show that, across 103 carbon-accrual measurements spanning management interventions globally, soils furthest from their mineralogical capacity are more effective at accruing carbon; sequestration rates average 3-times higher in soils at one tenth of their capacity compared to soils at one half of their capacity. Our findings provide insights into the world's soils, their capacity to store carbon, and priority regions and actions for soil carbon management. Soil is the largest terrestrial reservoir of organic carbon and is central for climate change mitigation and carbon-climate feedbacks. Chemical and physical associations of soil carbon with minerals play a critical role in carbon storage, but the amount and global capacity for storage in this form remain unquantified. Here, we produce spatially-resolved global estimates of mineral-associated organic carbon stocks and carbon-storage capacity by analyzing 1144 globally-distributed soil profiles. We show that current stocks total 899 Pg C to a depth of 1 m in non-permafrost mineral soils. Although this constitutes 66% and 70% of soil carbon in surface and deeper layers, respectively, it is only 42% and 21% of the mineralogical capacity. Regions under agricultural management and deeper soil layers show the largest undersaturation of mineral-associated carbon. Critically, the degree of undersaturation indicates sequestration efficiency over years to decades. We show that, across 103 carbon-accrual measurements spanning management interventions globally, soils furthest from their mineralogical capacity are more effective at accruing carbon; sequestration rates average 3-times higher in soils at one tenth of their capacity compared to soils at one half of their capacity. Our findings provide insights into the world’s soils, their capacity to store carbon, and priority regions and actions for soil carbon management. Mineral-organic associations play a key role in soil carbon preservation. Here, Georgiou et al. produce global estimates of mineral-associated soil carbon, providing insight into the world’s soils and their capacity to store carbon |
| ArticleNumber | 3797 |
| Author | Abramoff, Rose Z. Polley, H. Wayne Feng, Wenting Pellegrini, Adam F. A. Georgiou, Katerina Soong, Jennifer L. Riley, William J. Torn, Margaret S. Vindušková, Olga Jackson, Robert B. Harden, Jennifer W. Ahlström, Anders |
| Author_xml | – sequence: 1 givenname: Katerina orcidid: 0000-0002-2819-3292 surname: Georgiou fullname: Georgiou, Katerina email: georgiou1@llnl.gov organization: Physical and Life Sciences Directorate, Lawrence Livermore National Laboratory, Department of Earth System Science, Stanford University – sequence: 2 givenname: Robert B. orcidid: 0000-0001-8846-7147 surname: Jackson fullname: Jackson, Robert B. organization: Department of Earth System Science, Stanford University, Woods Institute for the Environment, Stanford University, Precourt Institute for Energy, Stanford University – sequence: 3 givenname: Olga orcidid: 0000-0002-7060-2459 surname: Vindušková fullname: Vindušková, Olga organization: Department of Biology, University of Antwerp, Institute for Environmental Studies, Charles University – sequence: 4 givenname: Rose Z. surname: Abramoff fullname: Abramoff, Rose Z. organization: Laboratoire des Sciences du Climat et de l’Environnement, Environmental Sciences Division, Oak Ridge National Laboratory – sequence: 5 givenname: Anders orcidid: 0000-0003-1642-0037 surname: Ahlström fullname: Ahlström, Anders organization: Deptartment of Physical Geography and Ecosystem Science, Lund University – sequence: 6 givenname: Wenting orcidid: 0000-0002-3189-3687 surname: Feng fullname: Feng, Wenting organization: Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences – sequence: 7 givenname: Jennifer W. surname: Harden fullname: Harden, Jennifer W. organization: Department of Earth System Science, Stanford University, U.S. Geological Survey – sequence: 8 givenname: Adam F. A. orcidid: 0000-0003-0418-4129 surname: Pellegrini fullname: Pellegrini, Adam F. A. organization: Department of Plant Sciences, University of Cambridge, Cambridge Conservation Institute, University of Cambridge – sequence: 9 givenname: H. Wayne orcidid: 0000-0002-1197-8800 surname: Polley fullname: Polley, H. Wayne organization: Agricultural Research Service, U.S. Department of Agriculture – sequence: 10 givenname: Jennifer L. surname: Soong fullname: Soong, Jennifer L. organization: Department of Ecosystem Science and Sustainability, Colorado State University, Granular, Inc – sequence: 11 givenname: William J. orcidid: 0000-0002-4615-2304 surname: Riley fullname: Riley, William J. organization: Climate and Ecosystem Sciences, Lawrence Berkeley National Laboratory – sequence: 12 givenname: Margaret S. orcidid: 0000-0002-8174-0099 surname: Torn fullname: Torn, Margaret S. organization: Climate and Ecosystem Sciences, Lawrence Berkeley National Laboratory, Energy and Resources Group, University of California, Berkeley |
| BackLink | https://insu.hal.science/insu-03824369$$DView record in HAL https://www.osti.gov/biblio/1874618$$D View this record in Osti.gov |
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| CorporateAuthor | Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States) Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States) Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States) MERGE: ModElling the Regional and Global Earth system Strategiska forskningsområden (SFO) Dept of Physical Geography and Ecosystem Science Strategic research areas (SRA) Lunds universitet Naturvetenskapliga fakulteten Profile areas and other strong research environments BECC: Biodiversity and Ecosystem services in a Changing Climate Faculty of Science Lund University Profilområden och andra starka forskningsmiljöer Institutionen för naturgeografi och ekosystemvetenskap |
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| Snippet | Soil is the largest terrestrial reservoir of organic carbon and is central for climate change mitigation and carbon-climate feedbacks. Chemical and physical... Mineral-organic associations play a key role in soil carbon preservation. Here, Georgiou et al. produce global estimates of mineral-associated soil carbon,... |
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| SubjectTerms | 704/106/47/4113 704/106/694/1108 704/106/694/682 704/47/4113 Agricultural and Veterinary sciences Agricultural management Agriculture, Forestry and Fisheries Carbon carbon cycle Carbon sequestration climate and Earth system modeling Climate change Climate change mitigation Earth Sciences ENVIRONMENTAL SCIENCES Estimates GEOSCIENCES Humanities and Social Sciences Jordbruk, skogsbruk och fiske Lantbruksvetenskap och veterinärmedicin Markvetenskap Mineralogy Minerals multidisciplinary Organic carbon Permafrost Science Science (multidisciplinary) Sciences of the Universe soil Soil analysis Soil layers soil organic carbon Soil profiles Soil properties Soil Science Soils Storage capacity |
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| Title | Global stocks and capacity of mineral-associated soil organic carbon |
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