Effect of reduction of aggregate size on the priming effect in a Mollisol under different soil managements

Abstract

Summary The priming effect (PE) is influenced by the amount and quality of soil organic carbon (SOC) held in different soil aggregates sizes. We examined the PE in Mollisols managed for >30 years as a grassland, farmland and bare fallow with 51, 32 and 27 g of SOC kg−1 soil, respectively, in a 60‐day incubation. Grassland soil contained 75% of aggregates in the macro size fractions >0.25 mm compared to <32% in farmland and bare fallow. Farmland and bare fallow soils contained proportionately more micro size fractions. The effect of aggregate size on the PE was assessed by comparing soils with intact aggregates to those where macroaggregates were reduced to microaggregate size fractions. In the grassland soil, cumulative CO2 mineralization increased by 20% in the reduced aggregate‐size treatment with no effect on farmland or bare fallow soils. Substrate additions to examine the PE included 13C‐glucose and 13C‐alanine (0.4 g C kg−1 dry soil), and inorganic N (2 mg N kg−1 dry soil). The PE was in the order glucose > alanine > (NH4)2SO4 and was most intense at day 3 of the incubation. Aggregate‐size reduction did not affect the PE within soil management treatments regardless of substrate addition. Most of the CO2 produced was derived from SOC rather than substrate addition and peaked at day 3. There was an interaction between microbial biomass C and dissolved organic C on the PE in the grassland soil only. The results suggested that the PE is an intrinsic characteristic of soils that are more affected by available C than the SOC in different aggregate fractions. Highlights The priming effect from added C substrates was examined in relation to aggregate size. Reducing macroaggregates to <0.25 mm increased CO2 production in a grassland but not agricultural Mollisol. The positive priming effect was proportionately reduced in soil dominated by macroaggregates. The priming effect is an intrinsic characteristic affected by C additions and less so by aggregate protected C.

Keystone Microbiomes Revealed by 14 Years of Field Restoration of the Degraded Agricultural Soil Under Distinct Vegetation Scenarios

“…The physicochemical properties of black soil, however, have changed drastically, especially SOC depletion, because agricultural land was reclaimed in the last hundred years. Numerous studies have shown significant deterioration of agricultural soils due to intensified anthropogenic interference, which poses great challenges for sustainable agriculture in China (Hao et al, 2017;You et al, 2019). Nonetheless, the microbial mechanisms underlying the restoration of agriculturally important lands are poorly understood.…”

Editorial for soil organic matter 2019 special issue

“…Five papers investigate the effects of management on SOM. You et al () report greater initial SOM, greater SOM mineralization when aggregates were disturbed, and a greater priming effect of native SOM after the addition of substrates to soil under grassland management, compared to arable or fallow management, confirming how management affects soil physical properties, and the nature and vulnerability to loss of the SOM that is protected within structures. Paddy rice systems are examined in two papers.…”