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Amino acid-sulphur decomposition in agricultural soil profile along a long-term recultivation chronosequence.

Authors :
Wang Q
Bauke SL
Wang D
Zhao Y
Reichel R
Jones DL
Chadwick DR
Tietema A
Bol R
Source :
The Science of the total environment [Sci Total Environ] 2024 Nov 15; Vol. 951, pp. 175409. Date of Electronic Publication: 2024 Aug 13.
Publication Year :
2024

Abstract

The significance of sulphur (S) availability for crop yield and quality is highlighted under the global S deficiency scenario. However, little is known about the temporal trend in belowground organic S mineralisation when restoring land to productive agricultural systems, particularly for the deeper soil parts. Therefore, we investigated the decomposition of <superscript>35</superscript> S-labelled methionine in surface (0-30 cm) and subsurface soil (30-60 cm and 60-90 cm) over a 48-year recultivation chronosequence (sampled after1, 8, 14, 24 and 48 years). Soil total sulphur (TS) significantly (p < 0.05) increased in surface soil but not in subsurface soils after 48 years of recultivation. Overall, the immobilisation of <superscript>35</superscript> S-methionine ( <superscript>35</superscript> S-MB) in subsurface soils relative to year 1 significantly decreased over the chronosequence but did not change in the surface samples. The <superscript>35</superscript> S-MB values in subsurface soils were positively corrected with soil carbon (C) stoichiometry (Pearson correlation, p < 0.05), suggesting the immobilisation of methionine was likely constrained by microbial C demand in deep soil. Compared to year 1, <superscript>35</superscript> S-SO <subscript>4</subscript> <superscript>2-</superscript> released from <superscript>35</superscript> S-methionine significantly declined throughout the older (≥ 8 years) soil profiles. Significant (p < 0.05) changes in the organic <superscript>35</superscript> S partition ( <superscript>35</superscript> S immobilisation and <superscript>35</superscript> S released as sulphate) were observed in year 8 after the soil was recultivated with N-fixing alfalfa or fertilisers. Whereas, after that (≥ 14 years), soil organic S partition remained affected when conventional tillage and agricultural crops dominated this site. Indicating that the effect of recultivation on organic S decomposition depends on the manner of recultivation management. Our study contributes to an improved understanding of amino acid S and organic S mineralisation under severe anthropogenic disturbance.<br />Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.<br /> (Copyright © 2024 The Authors. Published by Elsevier B.V. All rights reserved.)

Details

Language :
English
ISSN :
1879-1026
Volume :
951
Database :
MEDLINE
Journal :
The Science of the total environment
Publication Type :
Academic Journal
Accession number :
39142402
Full Text :
https://doi.org/10.1016/j.scitotenv.2024.175409