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Journal of Plant Nutrition and Soil Science· 2026Q1

Organic Matter Quality and Microbial Activity in Soils Managed With Brachiaria Succession

Siro Paulo Moreira, Vanessa Maria de Souza Barros, David Gabriel Campos Pereira, Humberto Josué de Oliveira Ramos et al.

Short summary

Brachiaria succession systems, particularly B6D, significantly altered soil organic matter fractions and microbial enzyme activity, though total C and N stocks at 1m depth decreased compared to no-brachiaria systems (NB).

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Key points

  • Total C and N stocks at 1m depth decreased by 15-32% for C and 14-27% for N in brachiaria systems (B24, B6D) compared to no-brachiaria (NB).
  • The B6D system exhibited the highest N stocks in the particulate organic matter fraction and the highest arylsulfatase activity (37.6 mg p-nitrophenol kg−1 soil h−1).
  • β-Glucosidase activity correlated with readily available C in the dissolved SOM fraction.
  • Bacterial biomass was higher in some brachiaria systems at greater soil depths.

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Abstract

ABSTRACT Background Although succession systems and brachiaria improve soil quality, gaps remain in microbial community dynamics, activity, and soil organic matter stocks. Methods The objective was to evaluate the carbon (C) and nitrogen (N) stocks of soil organic matter fractions and their distribution, molecular characterization, enzyme activity associated with the C, sulfur (S), and phosphorus (P) cycles, and microbial composition in succession crops of corn, soybeans, and cotton without prior use of brachiaria in succession (NB) and with brachiaria planted 24 months ago (B24), 6 months ago and desiccated (B6D), and 2 months ago and still alive (B2L), at different depths. Results Stocks decreased by 15% and 14% for B24, 32% and 27% for B6D, and 7% and 3% for B2L, respectively, for C and N at a depth of 1 m, when compared to NB. The B6D system had the highest N stocks in the particulate fraction of organic matter at depth, as well as the highest arylsulfatase activity (37.6 mg p ‐nitrophenol kg −1 soil h −1 ). β‐Glucosidase activity was driven by the supply of particulate material and readily available C to microorganisms, as observed by C stocks in the dissolved fraction. There was no difference between treatments for acid phosphatase activity. The stabilization of soil organic matter is directly associated with the presence of recalcitrant compounds, such as lipids, lignin, and alkanes (14–26). Conclusions Microbial attributes varied across land‐use systems and soil depths, with higher bacterial biomass observed in some brachiaria ‐based systems at greater depths. However, these responses were not accompanied by increases in total C and N stocks or in soil organic matter fractions, and their implications for C sequestration require further evaluation in long‐term studies.

The authors' abstract, as published at the source. Journal of Plant Nutrition and Soil Science, 2026 · DOI ↗

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Soil ScienceAgricultural and Biological Sciences