Abstract
Investigating microbial metabolic characteristics and soil organic carbon (SOC) within aggregates and their relationships under conservation tillage may be useful in revealing the mechanism of SOC sequestration in conservation tillage systems. However, limited studies have been conducted to investigate the relationship between SOC and microbial metabolic characteristics within aggregate fractions under conservation tillage. We hypothesized that close relationships can exist between SOC and microbial metabolic characteristics within aggregates under conservation tillage. In this study, a field experiment was conducted from June 2011 to June 2013 following a split-plot design of a randomized complete block with tillage practices [conventional intensive tillage (CT) and no tillage (NT)] as main plots and straw returning methods [preceding crop residue returning (S, 2100−2500 kg C ha−1) and removal (NS, 0 kg C ha-1)] as subplots with three replications. The objective of this study was to reveal the effects of tillage practices and residue-returning methods on topsoil microbial metabolic characteristics and organic carbon (SOC) fractions within aggregates and their relationships under a rice–wheat cropping system in central China. Microbial metabolic characteristics investigated using the Biolog system was examined within two aggregate fractions (>0.25 and <0.25 mm). NT treatments significantly increased SOC concentration of bulk soil, >0.25 aggregate, and <0.25 mm aggregate in the 0−5 cm soil layer by 5.8%, 6.8% and 7.9% relative to CT treatments, respectively. S treatments had higher SOC concentration of bulk soil (12.9%), >0.25 mm aggregate (11.3%), and <0.25 mm aggregate (14.1%) than NS treatments. Compared with CT treatments, NT treatments increased MBC by 11.2%, 11.5%, and 20%, and dissolved organic carbon (DOC) concentration by 15.5%, 29.5%, and 14.1% of bulk soil, >0.25 mm aggregate, and <0.25 mm aggregate in the 0−5 cm soil layer, respectively. Compared with NS treatments, S treatments significantly increased MBC by 29.8%, 30.2%, and 24.1%, and DOC concentration by 23.2%, 25.0%, and 37.5% of bulk soil, >0.25 mm aggregate, and <0.25 mm aggregate in the 0−5 cm soil layer, respectively. Conservation tillage (NT and S) increased microbial metabolic activities and Shannon index in >0.25 and <0.25 mm aggregates in the 0−5 cm soil layer. Redundancy analysis showed that the SOC and its fractions (DOC and MBC) were closely correlated with microbial metabolic activities. Structural equation modelling showed that the increase in microbial metabolic activities directly improved SOC by promoting DOC in >0.25 mm aggregate in the upper (0−5 cm) soil layer under conservation tillage systems, as well as directly and indirectly by promoting DOC and MBC in <0.25 mm aggregate. Our results suggested that conservation tillage increased SOC in aggregates in the topsoil by improving microbial metabolic activities.
Highlights
Anthropogenic carbon dioxide (CO2) emissions into the atmosphere have increased significantly by 39% from 6.3 Gt C in 1994 to 8.7 Gt C in 2009 [1]
Compared with NS treatments, S treatments significantly increased microbial biomass C (MBC) by 29.8%, 30.2%, and 24.1%, and dissolved organic carbon (DOC) concentration by 23.2%, 25.0%, and 37.5% of bulk soil, >0.25 mm aggregate, and
This study only investigated the effects of conservation tillage on microbial metabolic characteristics and the relationships between the metabolic characteristics and soil organic C (SOC) within aggregates in the 0−5 cm soil layer
Summary
Anthropogenic carbon dioxide (CO2) emissions into the atmosphere have increased significantly by 39% from 6.3 Gt C in 1994 to 8.7 Gt C in 2009 [1]. Reducing CO2 concentration to mitigate global climate change by carbon (C) sequestration has been a promising method [2]. Considerable attention has been given to the dynamics of soil organic C (SOC) stocks and its function in long-term C accumulation and sequestration of atmospheric CO2 for mitigating climate change, maintaining crop productivity sustainability, and increasing soil fertility [3]. Reasonable management practices, such as no tillage (NT) and residue returning (S), facilitate SOC sequestration in croplands [2]. Investigating the effects of conservation tillage on SOC is necessary for further understanding soil sequestration
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