Document Type

Article

Publication Version

Version of Record

Publication Date

5-2026

Abstract

No-till systems improve soil functions and are widely adopted in South Dakota cropping systems. However, these cropping systems have become increasingly simplified due to reduced small grain adoption, potentially reducing carbon inputs and microbial diversity. Therefore, this study aimed to (i) quantify the effects of crop rotations and cover cropping on soil organic carbon (SOC), total nitrogen (TN), and their labile fractions across the 0–80 cm soil profile, and (ii) assess how these management practices affect microbial properties in the topsoil (0–7.5 cm), using a long-term no-till (>30 years) field experiment in South Dakota. Main treatments included a corn (Zea mays L.)–soybean [Glycine max L. (Merr)]–oat (Avena sativa L.)–rye (Secale cereale L.) rotation (CSOR) and a corn–soybean rotation (CS) in a randomized complete block design with four replicates. Each rotation plot was split into cover crops (CC) and no cover crops (NCC). Near-surface SOC concentrations, microbial biomass carbon, and enzyme activities were increased by CC but showed little response to rotations. Both CSOR and CC increased TN, water-extractable carbon and nitrogen, and permanganate-oxidizable carbon in the topsoil. The CSOR promoted bacterial and total microbial phospholipid fatty acid abundance during the corn phase in fall and promoted arbuscular mycorrhiza fungi in spring under CC. In the fall, CC increased all microbial groups in both rotations, with greater benefits under CSOR in spring. Overall, at this long-term no-till site, cover crops and, to a lesser extent diversified rotations, can improve near-surface SOC concentrations, labile carbon, and microbial indicators.

Publication Title

Geoderma

Volume

469

First Page

117808

DOI of Published Version

10.1016/j.geoderma.2026.117808

Publisher

South Dakota State University

Creative Commons License

Creative Commons Attribution 4.0 International License
This work is licensed under a Creative Commons Attribution 4.0 International License.

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