Integrating straw return and tillage practices to enhance soil organic carbon sequestration in wheat–maize rotation systems in the North China Plain

Abstract

Straw return is a crucial strategy for enhancing soil organic carbon (SOC) sequestration in winter wheat–summer maize rotation systems in the North China Plain. However, the effects of straw return combined with different tillage practices on SOC sequestration under different environmental and management conditions across the soil profile remain unclear. A meta-analysis was conducted based on 2525 pairs of observations to investigate the effects of straw return combined with no tillage (NT), reduced tillage (RT), and conventional tillage (CT) on SOC content in wheat–maize rotation systems in the North China Plain. The results indicated that, compared with straw removal, straw return with NT and RT significantly increased the SOC content in the 0–40 cm layer, which was attributed to reduced soil disturbance and promoted SOC surface accumulation. The largest increase was observed in the 0–20 cm layer under NT (12.7 %) and in the 20–40 cm layer under RT (12.7 %). CT showed the greatest increase in SOC content below 40 cm (10.0 %), and RT did not affect SOC below the 40 cm layer relative to CT because deep tillage increased inputs of straw C and transferred topsoil with higher SOC to the subsoil layer. Mean annual precipitation, initial SOC content, and straw quantity were the major drivers regulating the response of SOC sequestration to straw return. Specifically, regions with mean annual temperatures above 15℃ and precipitation over 700 mm had a greater increase in SOC under straw return. Straw return under NT and RT led to the largest increase in SOC content when initial SOC was between 5 and 10 g kg −1 or with a straw return duration of 16–20 years. Straw return under CT showed the greatest increase when initial SOC exceeded 10 g kg −1 or with a straw return duration of 6–10 years. SOC content reached the highest level under RT and CT with a straw quantity of 10–15 t ha −1 and under NT with a straw quantity of less than 10 t ha −1 . Structural equation modeling showed that climatic conditions were positively correlated with the response of SOC to straw return and that soil properties and management practices exhibited a negative correlation. The effects of straw return combined with different tillage practices on the C footprint of agricultural systems should be explored in further research. • Straw return effects on SOC in soil profile of wheat–summer systems were assessed. • Straw return under NT/RT and CT significantly increased SOC in topsoil and subsoil, respectively. • MAP, initial SOC content, and straw quantity were the major drivers of SOC response to straw return. • Climate and management affected straw return impacts on SOC directly or indirectly via MBC and LOC.