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Benchmarking soil organic carbon to support agricultural carbon management: A German case study

Background Soil organic carbon (SOC) storage is highly variable across sites and primarily depends on site properties and land use. It is therefore difficult for farmers to evaluate the actual SOC status of a site. To aid the interpretation of measured SOC contents, easy‐to‐use frameworks for the as...

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Published in:Journal of plant nutrition and soil science 2022-06, Vol.185 (3), p.427-440
Main Authors: Drexler, Sophie, Broll, Gabriele, Flessa, Heinz, Don, Axel
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creator Drexler, Sophie
Broll, Gabriele
Flessa, Heinz
Don, Axel
description Background Soil organic carbon (SOC) storage is highly variable across sites and primarily depends on site properties and land use. It is therefore difficult for farmers to evaluate the actual SOC status of a site. To aid the interpretation of measured SOC contents, easy‐to‐use frameworks for the assessment of SOC contents are needed. Aims The aim of this study was to derive site‐specific SOC benchmarks for German mineral soils under agricultural use based on the dataset of the first German Agricultural Soil Inventory. Methods The dataset was stratified into 33 strata by land use, soil texture, C/N ratio and mean annual precipitation. Lower and upper SOC benchmarks were calculated for all strata (0.125 and the 0.875 quantile). Results The SOC benchmark value ranges were lower for cropland (6.8–48.9 g kg–1) than for grassland (14.1–76.6 g kg–1), and increased with rising clay content and precipitation. Sandy soils with a wide C/N ratio and high SOC content due to their heathland or peatland history were divided into separate strata. The number of strata only decreased the SOC benchmark ranges slightly. Around 15–20 sites were required as a minimum to quantify SOC benchmarks for one stratum. Conclusions The presented framework is easy to use, requiring only four readily available stratification factors to perform a comparative classification of SOC contents. It allows farmers and extension services to compare where their measured SOC contents fall within the expected SOC value range for their site, and can thus help develop an initial evaluation of the SOC status of a site with regard to soil‐specific differences.
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It is therefore difficult for farmers to evaluate the actual SOC status of a site. To aid the interpretation of measured SOC contents, easy‐to‐use frameworks for the assessment of SOC contents are needed. Aims The aim of this study was to derive site‐specific SOC benchmarks for German mineral soils under agricultural use based on the dataset of the first German Agricultural Soil Inventory. Methods The dataset was stratified into 33 strata by land use, soil texture, C/N ratio and mean annual precipitation. Lower and upper SOC benchmarks were calculated for all strata (0.125 and the 0.875 quantile). Results The SOC benchmark value ranges were lower for cropland (6.8–48.9 g kg–1) than for grassland (14.1–76.6 g kg–1), and increased with rising clay content and precipitation. Sandy soils with a wide C/N ratio and high SOC content due to their heathland or peatland history were divided into separate strata. The number of strata only decreased the SOC benchmark ranges slightly. Around 15–20 sites were required as a minimum to quantify SOC benchmarks for one stratum. Conclusions The presented framework is easy to use, requiring only four readily available stratification factors to perform a comparative classification of SOC contents. 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It is therefore difficult for farmers to evaluate the actual SOC status of a site. To aid the interpretation of measured SOC contents, easy‐to‐use frameworks for the assessment of SOC contents are needed. Aims The aim of this study was to derive site‐specific SOC benchmarks for German mineral soils under agricultural use based on the dataset of the first German Agricultural Soil Inventory. Methods The dataset was stratified into 33 strata by land use, soil texture, C/N ratio and mean annual precipitation. Lower and upper SOC benchmarks were calculated for all strata (0.125 and the 0.875 quantile). Results The SOC benchmark value ranges were lower for cropland (6.8–48.9 g kg–1) than for grassland (14.1–76.6 g kg–1), and increased with rising clay content and precipitation. Sandy soils with a wide C/N ratio and high SOC content due to their heathland or peatland history were divided into separate strata. The number of strata only decreased the SOC benchmark ranges slightly. 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Around 15–20 sites were required as a minimum to quantify SOC benchmarks for one stratum. Conclusions The presented framework is easy to use, requiring only four readily available stratification factors to perform a comparative classification of SOC contents. It allows farmers and extension services to compare where their measured SOC contents fall within the expected SOC value range for their site, and can thus help develop an initial evaluation of the SOC status of a site with regard to soil‐specific differences.</abstract><cop>Weinheim</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1002/jpln.202200007</doi><tpages>14</tpages><orcidid>https://orcid.org/0000-0002-7232-1650</orcidid><orcidid>https://orcid.org/0000-0001-7046-3332</orcidid><oa>free_for_read</oa></addata></record>
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subjects Agricultural land
Annual precipitation
Benchmarks
best agricultural practice
Bundes‐Bodenschutzgesetz
Carbon
carbon farming
Carbon/nitrogen ratio
Clay minerals
climate‐smart agriculture
Datasets
Evaluation
Farmers
Grasslands
Land use
Mathematical analysis
Organic carbon
Organic soils
Peatlands
Precipitation
Sandy soils
site‐specific soil organic carbon content
soil health
Soil properties
Soil texture
Strata
Texture
title Benchmarking soil organic carbon to support agricultural carbon management: A German case study
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