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Litter quality and living roots affected the formation of new mineral-associated organic carbon but did not affect total mineral-associated organic carbon in a short-term incubation

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35 Scopus citations

Abstract

Storing carbon (C) in soil organic matter (SOM) is critical for mitigating climate change as well as for providing food security under extreme weather events. Mineral-associated organic matter (MAOM), which is the organic matter attached to silt and clay, has a longer residence time than the light, sand-sized particulate organic matter (POM). Hence, increasing the C in this fraction is thought to be important for long-term C storage. However, the influence of litter quality and living plants on new MAOM formation and MAOM turnover is unclear. We hypothesized that lower C:N litter would form MAOM more efficiently and result in more MOAM than higher C:N litter because lower C:N litter favors biomass production of microbes, which are thought to be an important precursor of MAOM. In addition, we hypothesized that living plants would amplify the effect of litter quality on MAOM formation and turnover because roots growing with low C:N litter would be less N-stressed and rely less on MAOM turnover to access N than roots growing in high C:N litter. We conducted a greenhouse study where soil was mixed with four different plant litter treatments: a control without litter, soybean (Glycine max) with C:N = 21, buckwheat (Fagopyrum esculentum) with C:N = 35, and sudex (Sorghum bicolor [L.] Moench × S. sudanense [P.] Staph.) with C:N = 65. The four litter treatments were incubated with and without living oats (Avena sativa). The incubation was maintained for 40 days, and over this period soybean and buckwheat lost 89 % of their initial dry matter while sudex lost 69 % of its initial dry matter. Contrary to our expectation, the litter with the higher C:N (sudex) had the greatest proportion of degraded C transferred to MAOM (i.e., the litter MAOM-C transfer efficiency). However, the litter MAOM-C transfer efficiency was not associated with the total MAOM-C at the end of the incubation. The presence of living plants increased the amount of MAOM-C derived from soybean and sudex litter, but it did not increase the total MAOM-C. Thus, our results demonstrate that high C:N litter can efficiently form new MAOM-C, which can be enhanced by the presence of living plants, but the greater MAOM-C formation may be accompanied by a loss of pre-existing MAOM-C.

Original languageEnglish
Article number116302
JournalGeoderma
Volume430
DOIs
StatePublished - Feb 2023

Bibliographical note

Publisher Copyright:
© 2022 The Authors

Funding

This work is supported by the University of Kentucky College of Agriculture, Food, and Environment, the University of Kentucky Department of Plant and Soil Sciences, Agriculture and Food Research Initiative’s Sustainable Agricultural Systems Coordinated Agricultural Projects [award no. 2019–68012-29818] from the United States Department of Agriculture (USDA) National Institute of Food and Agriculture (NIFA), USDA NIFA Grant No 2020–67013-30860, the Foundation for Food and Agriculture Research Grant Number FF-NIA21-0000000058, and the USDA NIFA Multistate project NC1195.

FundersFunder number
University of Kentucky College of Agriculture Food and the Environment
University of Kentucky Department of Plant and Soil Sciences, Agriculture and Food Research Initiative’s Sustainable Agricultural Systems Coordinated Agricultural Projects2019–68012-29818
U.S. Department of Agriculture
National Institute of Food and Agriculture2020–67013-30860
Foundation for Food and Agriculture ResearchNC1195, FF-NIA21-0000000058

    UN SDGs

    This output contributes to the following UN Sustainable Development Goals (SDGs)

    1. SDG 2 - Zero Hunger
      SDG 2 Zero Hunger
    2. SDG 13 - Climate Action
      SDG 13 Climate Action

    Keywords

    • Carbon transfer efficiency
    • Mineral-associated organic matter
    • Particulate organic matter
    • Soil organic matter

    ASJC Scopus subject areas

    • Soil Science

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