Net effect of liming on soil organic carbon stocks: A review

• Published in: Agriculture, ecosystems & environment Vol. 202; pp. 98 - 107
• Main Authors: Paradelo, R., Virto, I., Chenu, C.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.04.2015; Elsevier
• Subjects: Acid soils; agricultural soils; aluminum; biological activity in soil; C stocks; carbon dioxide; carbon sinks; clay; exchangeable cations; Life Sciences; Liming; mineralization; nutrients; plant growth; soil organic carbon; Soil organic matter; soil structure; toxicity; C stocks; Soil organic matter; Liming; Acid soils; acid soils; liming; soil organic matter
• DOI: 10.1016/j.agee.2015.01.005
• ISSN: 0167-8809

•The effect of liming on soil organic carbon stocks is poorly known.•Liming increases SOC stocks in mineral soils due to higher C inputs and productivity.•Reductions in SOC could be temporary and due to initial increased SOC mineralization.•This initial trend should be reverted progressively due to increased C inputs.•We encourage scientists to synthesize unpublished data from existing experiments. Liming is a common agricultural practice worldwide, used for increasing productivity in acid agricultural soils. Liming reduces Al saturation and toxicity and/or increases pH up to values where the availability of nutrients is higher. The effect of this practice on soil properties has been extensively studied, with focus of most studies upon pH, exchangeable cations and productivity. In turn, the effects of liming on soil organic C (SOC) stocks still remain poorly known. The net effect on SOC can be the result of several factors: first, liming increases the soil biological activity, thus favoring the mineralization of organic matter, which should result in CO2 losses and a decrease of the SOC stocks. Second, liming ameliorates soil structure, increasing the stability of clay assemblages and clay-organic matter bonds, which should bring an increase in SOC physical and physicochemical protection. Finally, as liming ameliorates soil conditions to plant growth, plant productivity increases and also the return of C inputs to soil, thus potentially increasing SOC concentrations. The net effect of these processes is not well understood yet. Still, some overall trends can be deduced from data currently available in the literature. Liming does modify SOC stocks, increasing them in most cases, what seems to be caused by higher C inputs to limed soils due to increased productivity. Reductions in SOC have also been reported, probably in connexion with increased mineralization, whereas the role of improved soil structure remains unclear. Overall, these insights are deduced from published data which are still scarce, so we encourage the scientific community to synthesize unpublished SOC data from existing in situ experiments, in order to enlarge the span of experimental conditions and gain knowledge about the role of such a widespread agricultural practice on SOC stocks.