Soil carbon change in intensive agriculture after 25 years of conservation management
[1];
[2];
[3];
[4]
- Michigan State University, Hickory Corners, MI (United States); Michigan State University, East Lansing, MI (United States); University of Nebraska–Lincoln, NE (United States)
- Michigan State University, East Lansing, MI (United States)
- Michigan State University, East Lansing, MI (United States); University of Idaho, Moscow, ID (United States)
- Michigan State University, Hickory Corners, MI (United States); Michigan State University, East Lansing, MI (United States)
Changes in soil organic carbon (SOC) and nitrogen (SON) are strongly affected by land management but few long-term comparative studies have surveyed changes throughout the whole soil profile. We quantified 25-year SOC and SON changes to 1 m in 10 replicate ecosystems at an Upper Midwest, USA site. We compared four annual cropping systems in maize (Zea mays)-soybean (Glycine max)-winter wheat (Triticum aestivum) rotations, each managed differently (Conventional, No-till, Reduced input, and Biologically based); in three managed perennial systems (hybrid Poplar (Populus × euramericana), Alfalfa (Medicago sativa), and Conifer (Pinus spp.); and in three successional systems (Early, Mid- and Late succession undergoing a gradual change in species composition and structure over time). Both Reduced input and Biologically based systems included winter cover crops. Neither SOC nor SON changed significantly in the Conventional or Late successional systems over 25 years. All other systems gained SOC and SON to different degrees. SOC accrual was fastest in the Early successional system (0.8 ± 0.1 Mg C ha–1 y–1) followed by Alfalfa and Conifer (avg. 0.7 ± 0.1 Mg C ha–1 y–1), Poplar, Reduced input, and Biologically based systems (avg. 0.4 ± 0.1 Mg C ha–1 y–1), and Mid-successional and No-till systems (0.3 and 0.2 Mg C ha–1 y–1, respectively). Over the most recent 12 years, rates of SOC accrual slowed in all systems except Reduced input and Mid-successional. There was no evidence of SOC loss at depth in any system, including No-till. Rates of SON accrual ranged from 64.7 to 0.8 kg N ha–1 y–1 in the order Alfalfa ≥ Early successional > Reduced input and Biologically based ≥ Poplar > No-till and Conifer > Mid-successional systems. Pyrogenic C levels in the Conventional, Early, and Late successional systems were similar despite 17 years of annual burning in the Early successional system (~ 15 % of SOC to 50 cm, on average, and ~40 % of SOC from 50 to 100 cm). Results underscore the importance of cover crops, perennial crops, and no-till options for sequestering whole profile C in intensively managed croplands.
- Research Organization:
- Great Lakes Bioenergy Research Center (GLBRC), Madison, WI (United States)
- Sponsoring Organization:
- USDOE Office of Science (SC), Biological and Environmental Research (BER)
- Grant/Contract Number:
- SC0018409
- OSTI ID:
- 2481378
- Journal Information:
- Geoderma, Journal Name: Geoderma Vol. 453; ISSN 0016-7061
- Publisher:
- ElsevierCopyright Statement
- Country of Publication:
- United States
- Language:
- English
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