Abstract

Soil management practices, such as tillage method or straw return, could alter soil organic carbon (C) contents. However, the effects of tillage method or straw return on soil organic C (SOC) have showed inconsistent results in different soil/climate/cropping systems. The Yangtze River Delta of China is the main production region of rice and wheat, and rice-wheat rotation is the most important cropping system in this region. However, few studies in this region have been conducted to assess the effects of different tillage methods combined with straw return on soil labile C fractions in the rice-wheat rotation system. In this study, a field experiment was used to evaluate the effects of different tillage methods, straw return and their interaction on soil total organic C (TOC) and labile organic C fractions at three soil depths (0–7, 7–14 and 14–21 cm) for a rice-wheat rotation in Yangzhong of the Yangtze River Delta of China. Soil TOC, easily oxidizable C (EOC), dissolved organic C (DOC) and microbial biomass C (MBC) contents were measured in this study. Soil TOC and labile organic C fractions contents were significantly affected by straw returns, and were higher under straw return treatments than non-straw return at three depths. At 0–7 cm depth, soil MBC was significantly higher under plowing tillage than rotary tillage, but EOC was just opposite. Rotary tillage had significantly higher soil TOC than plowing tillage at 7–14 cm depth. However, at 14–21 cm depth, TOC, DOC and MBC were significantly higher under plowing tillage than rotary tillage except for EOC. Consequently, under short-term condition, rice and wheat straw both return in rice-wheat rotation system could increase SOC content and improve soil quality in the Yangtze River Delta.

Highlights

  • Soil organic carbon (C) has profound effects on soil physical, chemical and biological properties [1]

  • Soil labile organic C fractions (i.e., microbial biomass C (MBC), dissolved organic C (DOC), and oxidizable C (EOC)) that turn over quickly can respond to soil disturbance more rapidly than total organic C (TOC) [1,3,4]

  • PN had significantly lower TOC, DOC, MBC and easily oxidizable C (EOC) at 0–7 cm and 7– 14 cm, and RN had the lowest TOC and MBC at 14–21 cm compared to other treatments (Fig. 1)

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Summary

Introduction

Soil organic carbon (C) has profound effects on soil physical, chemical and biological properties [1]. Soil labile organic C fractions (i.e., microbial biomass C (MBC), dissolved organic C (DOC), and oxidizable C (EOC)) that turn over quickly can respond to soil disturbance more rapidly than total organic C (TOC) [1,3,4]. These fractions have been suggested as early sensitive indicators of the effects of land use change on soil quality Numerous studies have indicated that tillage methods combined with straw return had a significant effect on labile SOC fractions, the results varied under different soil/climate conditions. The investigation on soil labile organic C for specific soil, climate, and cropping system is necessary to improve the soil quality

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