Abstract

Biochar has important biogeochemical functions in soil—first as a means to sequester carbon, and second as a soil conditioner to potentially enhance soil quality and fertility. Volatile matter (VM) content is a property of biochar that describes its degree of thermal alteration, which can have a direct influence on carbon and nitrogen dynamics in soil. In this study, we characterized the VM in biochars derived from two locally sourced feedstocks (corncob and kiawe wood) and evaluated the relationship of VM content to nitrogen transformations and culturable fungal biomass. Using 13C nuclear magnetic resonance (NMR) spectroscopy, we found that the VM content of biochar primarily consisted of alkyl (5.1–10.1%), oxygen-substituted alkyl (2.2–6.7%), and phenolic carbon (9.4–11.6%). In a series of laboratory incubations, we demonstrated that corncob biochars with high VM (23%) content provide a source of bioavailable carbon that appeared to support enhanced viable, culturable fungi (up to 8 fold increase) and cause nitrogen immobilization in the short-term. Corncob biochar with bioavailable VM was nitrogen-limited, and the addition of nitrogen fertilizer resulted in a four-fold increase in total hydrolytic enzyme activity and the abundance of culturable fungal colonies. In contrast, kiawe biochar with an equivalent VM content differed substantially in its composition and effect on these same biological parameters. Therefore, the rapid measurement of VM content is too coarse to differentiate chemical composition and to predict the behavior of biochars across feedstocks and production methods.

Highlights

  • Our 13 C CPMAS nuclear magnetic resonance (NMR) data indicate that biochar chemical and structural composition varies depending upon both Volatile matter (VM) content and feedstock

  • Similar shifts in structure between high and low temperature maize charcoal were reported by Wang et al (2015), which we attribute to VM content

  • We have shown that VM content is related to changes in chemical structure and composition of biochar due to increasing pyrolysis severity for a corncob biochar produced by flash carbonization

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Summary

Introduction

Biochar is widely considered to be a source of stable carbon (C) that can be applied as a soil amendment, a broad range of turnover times have been reported, depending upon biochar properties and emergent behavior of the soil to which it is applied [1,2,3,4,5,6,7,8]. Biochar has the potential to sequester carbon in soil, but newly produced biochar can initially undergo decomposition upon its addition to soil [9,10] resulting in the immobilization of nutrients and the decline of plant growth [11,12,13]. The bioavailability of biochar C is a function of feedstock and pyrolysis conditions to the extent that they control chemical structure and composition [9,14,15,16,17,18,19], and energy return-on-investment to the microbial community [20], which depends upon soil nutrient availability, structure, and redox conditions

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