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Eleven Years' Effect of Conservation Practices for Temperate Sandy Loams: I. Soil Physical Properties and Topsoil Carbon Content
Author(s) -
Abdollahi Lotfollah,
Getahun Gizachew Tarekegn,
Munkholm Lars Juhl
Publication year - 2017
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/sssaj2016.06.0161
Subject(s) - topsoil , tillage , environmental science , soil science , loam , soil structure , soil carbon , plough , agronomy , no till farming , soil water , soil fertility , biology
Core Ideas Moldboard plowing decreased VESS score and soil penetration resistance. Reduced tillage combined with residue retention enhanced soil structural stability. Residue retention alleviated unfavorable soil structure effects of reduced tillage. Clay and SOC were confirmed as key factors affecting soil structure. Combining minimal soil disturbance and residue retention improved soil structure. Conservation agriculture (CA) has been suggested as a means of making intensification of agriculture sustainable. The purpose of this study was to understand and quantify long‐term individual and combined effects of key conservation practices on soil physical properties and topsoil C content. Field experiments were conducted in 11‐ to 12‐yr‐old experiments on two Danish sandy loams at Foulum and Flakkebjerg. Three crop rotations/residue management treatments were compared and tillage was included as a split‐plot factor. The tillage systems were moldboard plowing to a depth of 20 cm (MP), direct drilling (D) and harrowing to a depth of 8 to 10 cm (H). Soil sampling and in‐field measurements were performed in autumn 2013 and spring 2014. In the field, soil structure was visually evaluated and penetration resistance (PR) measured. Soil C, wet stability (clay dispersion and wet aggregate stability), and soil strength were determined in the laboratory. The MP soil had a uniform soil organic carbon (SOC) content in the 0‐ to 20‐cm depth of topsoil, whereas H and D resulted in SOC accumulation near the soil surface. Plowing resulted in the best visually assessed topsoil structure and had the lowest PR. However, H and D in combination with residue retention gave the best structural stability. Residue retention alleviated negative effects of reduced tillage on PR and improved wet stability in the MP treatment at the Foulum site. Clay and SOC correlated well with soil physical parameters, confirming their important role in soil structure formation and stabilization. Our study showed benefits of combining key CA elements, although longer‐term studies are most likely needed to reveal the full potential.