Quantifying soil organic matter stock distribution and origin following over a century of maize-based cropping in the former tallgrass prairie region of central USA

Tallgrass prairie conversion to maize-based agriculture in central North America has resulted in substantial loss of soil organic carbon (SOC) in less than two centuries. However, evaluations of how management practices may mitigate SOC losses are generally limited in soil depth and/or duration, missing long-term SOC stock outcomes that manifest over timescales of decades or longer. To address this, we sampled soils in year 145 of the Morrow Plots experiment to (i) evaluate effects of crop rotation and fertility management on SOC stocks and (ii) distinguish prairie- versus maize-derived SOC after continuous maize cropping since 1876 using stable carbon isotope ( 13 C) natural abundance. Soil organic carbon stock by equivalent soil mass (ESM) was + 30.7 Mg C ha −1 (+31.7 %) higher under maize-oat-alfalfa than continuous maize, but similar between maize-soybean and continuous maize. NPK fertilization and manuring did not influence SOC stocks by ESM. Response of SOC stocks at 15 cm depth intervals to NPK fertilization varied by depth and crop rotation, with lower SOC stocks at 30–45 cm under continuous maize and maize-soybean. Maize-derived C ranged 19.5–59.6 % of SOC stock across depths, indicating the majority of SOC was still derived from tallgrass prairie even after 145 years of continuous maize cropping. Our results confirm the potential of diversified crop rotation for minimizing SOC losses relative to tallgrass prairie at the supracentennial scale, and highlight the importance of relic prairie soil organic matter for future crop production in central North America. • Evaluated centennial-scale crop rotation and fertilization effect on soil organic C. • Higher soil organic C stocks under maize-oat-alfalfa than continuous maize. • Limited effect of NPK fertilization and manuring on soil organic C stocks. • Lower subsoil organic C stock with NPK fertilization under simplified maize rotations. • Prairie-derived organic C still dominated after 145 years of continuous maize.

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Publication Details

Journal
Agriculture Ecosystems & Environment
Published
2025-12-31
DOI
https://doi.org/10.1016/j.agee.2025.110195
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
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article

Quantifying soil organic matter stock distribution and origin following over a century of maize-based cropping in the former tallgrass prairie region of central USA

Yuhei Nakayama, Michael D. Masters, Andrew J. Margenot, Evan H. DeLucia
Agriculture Ecosystems & Environment
Soil Carbon and Nitrogen Dynamics
article

Quantifying soil organic matter stock distribution and origin following over a century of maize-based cropping in the former tallgrass prairie region of central USA

Yuhei Nakayama, Michael D. Masters, Andrew J. Margenot, Evan H. DeLucia
article en

Abstract

Tallgrass prairie conversion to maize-based agriculture in central North America has resulted in substantial loss of soil organic carbon (SOC) in less than two centuries. However, evaluations of how management practices may mitigate SOC losses are generally limited in soil depth and/or duration, missing long-term SOC stock outcomes that manifest over timescales of decades or longer. To address this, we sampled soils in year 145 of the Morrow Plots experiment to (i) evaluate effects of crop rotation and fertility management on SOC stocks and (ii) distinguish prairie- versus maize-derived SOC after continuous maize cropping since 1876 using stable carbon isotope ( 13 C) natural abundance. Soil organic carbon stock by equivalent soil mass (ESM) was + 30.7 Mg C ha −1 (+31.7 %) higher under maize-oat-alfalfa than continuous maize, but similar between maize-soybean and continuous maize. NPK fertilization and manuring did not influence SOC stocks by ESM. Response of SOC stocks at 15 cm depth intervals to NPK fertilization varied by depth and crop rotation, with lower SOC stocks at 30–45 cm under continuous maize and maize-soybean. Maize-derived C ranged 19.5–59.6 % of SOC stock across depths, indicating the majority of SOC was still derived from tallgrass prairie even after 145 years of continuous maize cropping. Our results confirm the potential of diversified crop rotation for minimizing SOC losses relative to tallgrass prairie at the supracentennial scale, and highlight the importance of relic prairie soil organic matter for future crop production in central North America. • Evaluated centennial-scale crop rotation and fertilization effect on soil organic C. • Higher soil organic C stocks under maize-oat-alfalfa than continuous maize. • Limited effect of NPK fertilization and manuring on soil organic C stocks. • Lower subsoil organic C stock with NPK fertilization under simplified maize rotations. • Prairie-derived organic C still dominated after 145 years of continuous maize.

Agriculture Ecosystems & EnvironmentVol. 399
University of Illinois Urbana-Champaign (US)
Zero hunger
Openalex Percentile: Top 32%
Soil Carbon and Nitrogen Dynamics
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