R. Tharindu Rambadagalla , Morgan P. Davis , Gurbir Singh , Timothy Reinbott , Biyensa Gurmessa , Ranjith P. Udawatta
{"title":"Long-term effects of cover crops on soil carbon forms and stocks in no-till corn-soybean rotations in midwest USA","authors":"R. Tharindu Rambadagalla , Morgan P. Davis , Gurbir Singh , Timothy Reinbott , Biyensa Gurmessa , Ranjith P. Udawatta","doi":"10.1016/j.soisec.2026.100230","DOIUrl":null,"url":null,"abstract":"<div><div>Anthropogenic activities have disrupted the natural carbon (C) balance, contributing to global climate change. Cover crops facilitate C sequestration, but their long-term impacts and deep soil C storage in Missouri remain unexplored. This study examined soil C forms to 100 cm depth under cover crop management in corn [<em>Zea mays</em> (L.)] - soybean [<em>Glycine max</em> (L.) Merr.] rotations. Soil from 5- and 10-year-old cover crop fields in Missouri were sampled to 100 cm depth under no-till cover crop (CC) and no-till no-cover crop (NCC) treatments, and analyzed for soil organic carbon (SOC), potentially mineralizable carbon (PMC), and permanganate oxidizable carbon (POXC). Cover crops increased SOC% and stocks in both fields, with the greatest concentration at 0–5 cm depth. Cumulative SOC stocks for 0–60 cm depth under CC were 10.3% greater in 10-year-old field and 1.63% greater in 5-year-old field than NCC. Interestingly, the 10-year-old field showed strong indicatations of stable C formation. Significantly greater POXC values under CC were observed at 0–5 cm and 45–60 cm depth than NCC in 5-year-old site. Additionally, PMC values were numerically greater under CC at 0–5 cm depth than NCC in both sites. Increased labile C (POXC and PMC) near the surface, suggests enhanced microbial activity and C mineralization. Greater parameter changes were notable in shallow depth (0–45 cm) but less pronounced at deeper depths (45–100 cm). These findings highlighted that long-term cover crop adoption can meaningfully enhance soil C storage in Missouri, including in sub-soils, providing valuable information for C accounting and the system's contribution to climate change mitigation.</div></div>","PeriodicalId":74839,"journal":{"name":"Soil security","volume":"22 ","pages":"Article 100230"},"PeriodicalIF":0.0000,"publicationDate":"2026-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Soil security","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2667006226000079","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2026/2/20 0:00:00","PubModel":"Epub","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Anthropogenic activities have disrupted the natural carbon (C) balance, contributing to global climate change. Cover crops facilitate C sequestration, but their long-term impacts and deep soil C storage in Missouri remain unexplored. This study examined soil C forms to 100 cm depth under cover crop management in corn [Zea mays (L.)] - soybean [Glycine max (L.) Merr.] rotations. Soil from 5- and 10-year-old cover crop fields in Missouri were sampled to 100 cm depth under no-till cover crop (CC) and no-till no-cover crop (NCC) treatments, and analyzed for soil organic carbon (SOC), potentially mineralizable carbon (PMC), and permanganate oxidizable carbon (POXC). Cover crops increased SOC% and stocks in both fields, with the greatest concentration at 0–5 cm depth. Cumulative SOC stocks for 0–60 cm depth under CC were 10.3% greater in 10-year-old field and 1.63% greater in 5-year-old field than NCC. Interestingly, the 10-year-old field showed strong indicatations of stable C formation. Significantly greater POXC values under CC were observed at 0–5 cm and 45–60 cm depth than NCC in 5-year-old site. Additionally, PMC values were numerically greater under CC at 0–5 cm depth than NCC in both sites. Increased labile C (POXC and PMC) near the surface, suggests enhanced microbial activity and C mineralization. Greater parameter changes were notable in shallow depth (0–45 cm) but less pronounced at deeper depths (45–100 cm). These findings highlighted that long-term cover crop adoption can meaningfully enhance soil C storage in Missouri, including in sub-soils, providing valuable information for C accounting and the system's contribution to climate change mitigation.