4.7 Article

Root exudates shift how N mineralization and N fixation contribute to the plant-available N supply in low fertility soils

Journal

SOIL BIOLOGY & BIOCHEMISTRY
Volume 165, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2021.108541

Keywords

Marginal lands; Root exudates; N fixation; Gross N mineralization; Plant-microbe interactions

Categories

Funding

  1. Department of Energy (DOE) Biological and Environmental Research (BER) , Office of Science [DE-SC0014108]
  2. DOE Great Lakes Bioenergy Research Center (DOE BER Office of Science) [DE-SC0018409, DE-FC02-07ER64494]
  3. National Science Foun-dation Long-Term Ecological Research Program at the Kellogg Biological Station [DEB 1832042]
  4. U.S. Department of Energy (DOE) [DE-SC0014108] Funding Source: U.S. Department of Energy (DOE)

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This study investigated the effects of root exudates on microbial-mediated nitrogen transformations in low fertility soils through laboratory incubation. The results showed that different root exudates influenced soil respiration, dissolved organic carbon, and dissolved organic nitrogen concentrations. Analysis of measured pools revealed that the recovery of root exudate carbon was lower in sandy loam soil. Additionally, organic acids had a greater impact on nitrogen mineralization and fixation rates. Root exudate addition also altered soil pH and organic nitrogen concentrations.
Nitrogen (N) availability is a primary constraint to plant productivity, especially in marginal lands with inherently low fertility. Root exudates change with plant nutrient status, and are expected to affect the microbiallymediated N transformations (gross N mineralization vs N fixation) in low fertility soil (low soil organic matter). To explore this possibility, we sampled soils from two monoculture switchgrass (var. Cave-In-Rock) plot with and without N addition at two marginal land sites in Michigan, USA. In a two-week lab incubation, we quantified the effect of different root exudates on gross N mineralization and N fixation by adding simulated root exudates (carbohydrates, organic acids) at a rate of 100 mu g C g(-1) day(-1). On average, adding carbohydrates to low fertility soil increased the soil respiration by 254%, the dissolved organic carbon (DOC) by 366% and reduced dissolved organic N (DON) by 40%. In contrast, soils receiving organic acids had 159% more soil respiration, 163% higher DOC concentration and the DON concentration increased by 49%. Analysis of the C recovery in measured pools revealed that root exudates C inputs were nearly equivalent to the DOC, microbial biomass carbon (MBC), and soil respiration in sandy soil, but only 45-74% of the root exudate C was recovered in these pools in the sandy loam soil. This suggests that root exudate C may be adsorbed to mineral particles in the sandy loam soil. Soil treated with organic acids had higher gross N mineralization and N immobilization rates than soil with carbohydrates addition. Adding carbohydrates significantly increased the free-living N fixation rates, compared to organic acid addition. Changes in soil pH, and DON induced by root exudate addition had strong association with N transformation rates and N availability. Gross N mineralization produced more plant-available N than N fixation, as evidenced by higher inorganic N concentration in soils receiving organic acids than carbohydrates. By quantifying how different root exudates affect the contribution of N mineralization and N fixation to the plant available N pool in low fertility soils, this study enhances our understanding of the C for N exchange in the plant rhizosphere.

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