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In this response to a letter to the editor, we provide evidence that the findings regarding a non‐detectable limit of mineral‐associated organic carbon as published in Begill et al. (2023) are robust. This is mainly done by showing that no methodological bias was present and that the main correlation was not driven by a few exceptional soils.
Soil organic carbon (SOC) sequestration is a promising climate change mitigation option. In this context, the formation of the relatively long‐lived mineral‐associated organic carbon (MAOC) is key. To date, soils are considered to be limited in their ability to accumulate MAOC, mainly by the amount of clay and silt particles present. Using the comprehensive German Agricultural Soil Inventory, we selected...
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