Soil type and moisture regime control microbial C and N mineralization in grassland soils more than atmospheric CO2-induced changes in litter quality

Authors

• Virginia L. Jin, USDA - Agricultural Research ServiceFollow
• Richard L. Haney, USDA - Agricultural Research Service
• Philip A. Fay, USDA-ARSFollow
• H. Wayne Polley, USDA-ARSFollow

Document Type

Article

Date of this Version

2013

Citation

Soil Biology & Biochemistry 58 (2013) 172-180; http://dx.doi.org/10.1016/j.soilbio.2012.11.024

Abstract

Global change-induced alterations in litter quality and soil moisture regime will likely impact grassland C and N dynamics, but how these changes interact with edaphic properties across the landscape is unclear. We measured the effects of litter quality, soil type, soil moisture level, and soil drying-rewetting frequency (D-RW) on microbial C and N mineralization of litter and soil organic matter (SOM) in a full-factorial, controlled incubation experiment. Four levels of litter quality (no litter; or litter from Bouteloua curtipendula grown under 280, 380, 500 μL L^‒1 CO₂) were surface-applied to three contrasting soils common to Blackland Prairie landscapes: an upland Mollisol, a lowland Vertisol, and a fluvial Alfisol. Different soil moisture regimes were tested by incubating soils at four moisture levels (air-dry, 25%, 35%, or 50% water-holding capacity, WHC) and by drying-rewetting soils 0, 1, 2, 4 or 8 times over the 112- d incubation period. Litter additions stimulated microbial activity, increasing total CO₂ production (i.e. C mineralized from litter + SOM decomposition) up to 17x more than no-litter controls (average 3x) and decreasing net N mineralization up to ‒3x less (average ‒0.5x) due to greater microbial N immobilization. Neither C nor N mineralization, however, was affected by litter quality. For all soils, litter decomposition increased with increasing WHC and D-RW frequency, but the average percent of total CO₂ derived from litter was a negative function of SOM content. Similarly, net N mineralization also was positively correlated with soil WHC and affected most strongly by soil type (Alfisol < Mollisol < Vertisol). Net N mineralization responses to D-RW events was also soil-specific, with Alfisol soils showing no response and Mollisol and Vertisol soils decreasing after 4 D-RW events. Our results suggest that predicted changes in rainfall patterns and its interactions with soil type across the landscape will control short-term C and N mineralization responses in grasslands to a greater extent than atmospheric CO₂- induced changes in litter C:N ratio for this common species of prairie grass.