Soil carbon dynamics during drying vs. rewetting: Importance of antecedent moisture conditions. (May 2021)

• Record Type: Journal Article
• Authors: Patel, Kaizad F.; Myers-Pigg, Allison; Bond-Lamberty, Ben; Fansler, Sarah J.; Norris, Cooper G.; McKever, Sophia A.; Zheng, Jianqiu; Rod, Kenton A.; Bailey, Vanessa L.
• Is Part Of: Soil biology and biochemistry. Volume 156(2021)
• Publication Date: 2021-05
• Subjects: Soil organic matter -- Carbon destabilization -- Adsorption and desorption -- Drying and rewetting; Soil biochemistry -- Periodicals; Soil biology -- Periodicals; Sols -- Biochimie -- Périodiques; Sols -- Biologie -- Périodiques; Sols -- Microbiologie -- Périodiques; Bodembiologie; Biochemie; 631.46
• DOI: 10.1016/j.soilbio.2021.108165
• Languages: English
• ISSNs: 0038-0717

Abstract

Abstract: Soil moisture influences soil carbon dynamics, including microbial growth and respiration. The response of such 'soil respiration' to moisture changes is generally assumed to be linear and reversible, i.e. to depend only on the current moisture state. Current models thus do not account for antecedent soil moisture conditions when determining soil respiration or the available substrate pool. We conducted a laboratory incubation to determine how the antecedent conditions of drought and flood influenced soil organic matter (SOM) chemistry, bioavailability, and respiration. We sampled soils from an upland coastal forest, Beaver Creek, WA USA, and subjected them to drying and rewetting treatments. For the drying treatment, field moist soils were saturated and then dried to 75, 50, 35, and 5% saturation. In the rewetting treatment, field moist soils were air-dried and then rewet to 35, 50, 75, and 100% saturation. We measured respiration and water extractable organic carbon (WEOC) concentrations and used 1 H-NMR and FT-ICR-MS to characterize the WEOC pool across the treatments. The drying vs. wetting treatment strongly influenced SOM bioavailability, as rewet soils (with antecedent drought) had greater WEOC concentrations and respiration fluxes compared to the drying soils (with antecedent flood). In addition, air-dry soils had the highest WEOC concentrations, and the NMR-resolved peaks showed a strong contribution of protein groups in these soils. Both NMR and FT-ICR-MS analyses indicated increased contribution of complex aromatic groups/molecules in the rewet soils, compared to the drying soils. We suggest that drying introduced organic matter into the WEOC pool via desorption of aromatic molecules and/or by microbial cell lysis, and this stimulated microbial mineralization rates. Our work indicates that even short-term shifts in antecedent moisture conditions can strongly influence soil C dynamics at the core scale. The predictive uncertainties in current soil models may be reduced by a more accurate representation of soil water and C persistence that includes a mechanistic and quantitative understanding of the impact of antecedent moisture conditions. Highlights: Antecedent moisture conditions influenced SOM response to moisture changes. Air-dry soils showed increased contribution of protein-like groups in the extractable SOM pool. Rewetting soils showed greater contribution of aromatic and complex groups in the extractable SOM pool. Rewetting soils showed greater respiration fluxes, compared to drying soils.