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Soil Aggregation and Carbon and Nitrogen Storage under Soybean Cropping Sequences
Author(s) -
Wright Alan L.,
Hons Frank M.
Publication year - 2004
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj2004.5070
Subject(s) - tillage , sorghum , monoculture , soil carbon , agronomy , carbon sequestration , soil water , cropping system , environmental science , conventional tillage , chemistry , nitrogen , soil science , biology , crop , organic chemistry
Management practices, such as no‐tillage (NT) and high‐intensity cropping sequences, have the potential to enhance C and N sequestration in agricultural soils. The objectives of this study were to investigate the impacts of conventional‐tillage (CT), NT, and multiple cropping sequences on soil organic carbon (SOC) and nitrogen (SON) sequestration and on distribution within aggregate‐size fractions in a southcentral Texas soil after 20 yr of treatment imposition. No‐tillage management increased soil aggregation compared with CT, with the bulk of SOC and SON storage present in larger aggregate‐size fractions (>2 mm, 250 μm to 2 mm) at both soil depths. Multiple cropping systems, such as a grain sorghum [ Sorghum bicolor (L.) Moench] / wheat ( Triticum aestivum L.)/soybean [ Glycine max (L.) Merr] (SWS) rotation and a wheat/soybean (WS) doublecrop had the highest SOC and SON storage, while the continuous monoculture soybean treatment had the lowest storage. Soil organic C and SON storage were significantly greater under NT than CT for all cropping sequences at 0 to 5 cm and for SWS and WS at 5 to 15 cm. At the 0‐ to 5‐cm depth, NT increased SOC storage by 64% and SON storage by 76% compared with CT. However, at 5 to 15 cm, NT only increased SOC storage by 28% and SON storage by 40%. The use of NT showed a greater impact for increasing SON storage than for SOC storage, suggesting that N cycling is an important factor related to soil C sequestration potential.