Premium
Soil Compaction, Both an Environmental and Agronomic Culprit: Increased Nitrous Oxide Emissions and Reduced Plant Nitrogen Uptake
Author(s) -
Gregorich E.G.,
McLaughlin N.B.,
Lapen D.R.,
Ma B.L.,
Rochette P.
Publication year - 2014
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/sssaj2014.03.0117
Subject(s) - compaction , fertilizer , nitrous oxide , agronomy , soil water , environmental science , soil compaction , human fertilization , growing season , nitrogen , population , chemistry , soil science , biology , materials science , demography , organic chemistry , sociology , composite material
With a burgeoning world population and growing demand for agricultural products, it will be necessary to strike a judicious balance between maintaining adequate N inputs and minimizing gaseous N losses in farming systems. Our objective in this study was to quantify the effects of soil compaction, N fertilization, and clay content on N 2 O emission from soil. Soil cropped to maize ( Zea mays L.) was compacted by tractor wheel traffic or not compacted for consecutive years, and N fertilizer was applied at 0, 75, 150, and 300 kg N ha −1 to both compaction treatments. Variability in clay content across the experimental plots allowed us to assess of the effects of texture on N 2 O response to compaction and N fertilization. Compaction, increasing N fertilization, and their interaction all significantly increased cumulative emissions of N 2 O during the growing season. There was a significant carryover effect, with higher N 2 O emissions observed in previously compacted soils in a subsequent year when soybean [ Glycine max (L.) Merr.] was grown and no compaction or N fertilizer was applied. Nitrous oxide emissions scaled against plant N uptake showed significant positive response to both compaction and N fertilizer. Clay content did not significantly affect N 2 O emissions, but its role became apparent when the emissions were scaled by N uptake. This scaling amplified the deleterious effects of compaction on gaseous N losses from soil because compaction both increased N 2 O emissions and decreased yield and plant N uptake. In contrast, increasing N fertilizer increased both and therefore did not have as large an effect on the scaled N 2 O emissions.