Interactive effects of initial pH and nitrogen status on soil organic carbon priming by glucose and lignocellulose
journal contributionposted on 06.01.2021, 01:12 authored by Nang Seng Aye, Clayton R Butterly, Peter SalePeter Sale, Caixian TangCaixian Tang
© 2018 Elsevier Ltd Soil pH and the availability of carbon (C) substrate and nutrients to microorganisms are well recognized to influence C priming. However, the mechanisms underpinning such interplay so far remain elusive. Given that liming acid soils, residue retention and fertilization are common agricultural practices, small changes in SOC content by these practices could have a big impact on the global C budget. This study aimed to gain insight into the impact of initial pH and mineral N availability on the priming effect of two C substrates with contrasting biodegradability. Stable 13C-labelled substrates, glucose and lignocellulose, were applied at the rate of 0.5 mg C g−1 soil with or without NH4NO3 to the same soil matrix with three different initial pH levels; pH 4.1 (strongly acidic), 4.7 (moderately acidic) and 6.6 (slightly acidic). The N treatment was based on a C:N of 10 of the added substrate (0.05 mg N g−1 soil) to ensure N was non-limiting. Interestingly, the priming effect was not linearly related to soil pH; greatest at pH 4.1, followed by pH 6.6 and lowest at pH 4.7. The greater net increase in microbial biomass upon C supply in strongly acidic soils compared to the moderately and slightly acidic soils would have enhanced co-metabolic decomposition of native soil organic C (SOC). The cumulative amount of primed SOC during the 30-day incubation period was greater in glucose- (21 μg C g−1) than lignocellulose-amended soils (13 μg C g−1). Nitrogen application reduced the C priming effect of both C substrates at all pH levels. This reduction was more prominent with lignocellulose and in the moderately acidic soils. The results suggest that maintaining optimal soil pH for nutrient availability and N application that exceeds the microbial N requirements in agricultural fields may minimize SOC loss via the priming effect in the short term.
JournalSoil Biology and Biochemistry
Pagination12p. (p. 33-44)
Rights StatementThe Author reserves all moral rights over the deposited text and must be credited if any re-use occurs. Documents deposited in OPAL are the Open Access versions of outputs published elsewhere. Changes resulting from the publishing process may therefore not be reflected in this document. The final published version may be obtained via the publisher’s DOI. Please note that additional copyright and access restrictions may apply to the published version.
Science & TechnologyLife Sciences & BiomedicineSoil ScienceAgricultureLimingAcidificationPriming effectsSubstrate decompositionMicrobial biomass CMicrobial biomass NMicrobial metabolic quotient (qCO(2))Soil organic matterMICROBIAL BIOMASSENZYME-ACTIVITIESMATTER DECOMPOSITIONCLIMATE-CHANGELITTER DECOMPOSITIONBACTERIAL-GROWTHLABILE CARBONTRACE AMOUNTSMINERALIZATIONAVAILABILITYAgronomy & Agriculture