Benchmarking soil organic carbon (SOC) concentration provides more robust soil health assessment than the SOC/clay ratio at European scale
Feeney, Christopher J. 
ORCID: https://orcid.org/0000-0003-2175-1842; Bentley, Laura ORCID: https://orcid.org/0000-0001-5055-7673; De Rosa, Daniele; Panagos, Panos; Emmett, Bridget A. ORCID: https://orcid.org/0000-0002-2713-4389; Thomas, Amy ORCID: https://orcid.org/0000-0002-4929-7285; Robinson, David A. ORCID: https://orcid.org/0000-0001-7290-4867.
2024
Benchmarking soil organic carbon (SOC) concentration provides more robust soil health assessment than the SOC/clay ratio at European scale.
Science of The Total Environment, 951, 175642.
13, pp.
https://doi.org/10.1016/j.scitotenv.2024.175642
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Text
N537884JA.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (5MB) | Preview |
Abstract/Summary
Increasing soil organic carbon (SOC) confers benefits to soil health, biodiversity, underpins carbon sequestration and ameliorates land degradation. One recommendation is to increase SOC such that the SOC to clay ratio (SOC/clay) exceeds 1/13, yet normalising SOC levels based on clay alone gives misleading indications of soil structure and the potential to store additional carbon. Building on work by Poeplau & Don (2023) to benchmark observed against predicted SOC, we advance an alternative indicator: the ratio between observed and “typical” SOC (O/T SOC) for pan-European application. Here, “typical” SOC is the average concentration in different pedo-climate zones, PCZs (which, unlike existing SOC indicators, incorporate land cover and climate, alongside soil texture) across Europe, determined from mineral (<20 % organic matter) topsoils (0–20 cm) sampled during 2009–2018 in LUCAS, Europe's largest soil monitoring scheme (n = 19,855). Regression tree modelling derived 12 PCZs, with typical SOC values ranging 5.99–39.65 g kg−1. New index classes for comparison with SOC/clay grades were established from the quartiles of each PCZ's O/T SOC distribution; these were termed: “Low” (below the 25th percentile), “Intermediate” (between the 25th and 50th percentiles), “High” (between the 50th and 75th percentiles), and “Very high” (above the 75th percentile). Compared with SOC/clay, O/T SOC was less sensitive to clay content, land cover, and climate, less geographically skewed, and better reflected differences in soil porosity and SOC stock, supporting 2 EU Soil Health Mission objectives (consolidating SOC stocks; improving soil structure for crops and biota). These patterns held for 2 independent datasets, and O/T SOC grades were sensitive enough to reflect land management differences across several long-term field experiments. O/T SOC used in conjunction with several other physical, chemical and biological soil health indicators can help support the EU Soil Monitoring Law and achieve several United Nations Sustainable Development Goals.
| Item Type: | Publication - Article |
|---|---|
| Digital Object Identifier (DOI): | https://doi.org/10.1016/j.scitotenv.2024.175642 |
| UKCEH and CEH Sections/Science Areas: | Soils and Land Use (Science Area 2017-) |
| ISSN: | 0048-9697 |
| Additional Information. Not used in RCUK Gateway to Research.: | Open Access paper - full text available via Official URL link. |
| Additional Keywords: | soil carbon, clay, pedo-climate zones, soil structure, soil monitoring, sustainable development goals |
| NORA Subject Terms: | Ecology and Environment Agriculture and Soil Science |
| Related URLs: | |
| Date made live: | 21 Aug 2024 10:06 +0 (UTC) |
| URI: | https://nora.nerc.ac.uk/id/eprint/537884 |
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