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Factors Contributing to Changes in Plant Available Nitrogen across a Variable Landscape
Author(s) -
Dharmakeerthi R. S.,
Kay B. D.,
Beauchamp E. G.
Publication year - 2005
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/sssaj2005.0453
Subject(s) - spatial variability , tillage , hordeum vulgare , agronomy , environmental science , plough , growing season , cover crop , soil water , geography , poaceae , agroforestry , soil science , biology , mathematics , statistics
The maximum benefits that may be obtained from site‐specific N management will not be realized until we improve our understanding of the spatial variability in plant available nitrogen (PAN) under different soil and crop management practices across the landscape. The objectives of this study were to quantify the influence of soil factors on the spatial and temporal variability of N availability to corn ( Zea mays L.) grown under different tillage and legume cover crop conditions. Three management treatments were established on a variable landscape in southern Ontario in 1999, 2000, and 2001: barley ( Hordeum vulgare L.) followed by corn under no‐tillage, barley followed by corn under spring plowing and secondary tillage, and barley underseeded with red clover ( Trifolium pratense L.) that was plowed down the next spring and followed by corn. The PAN contents were measured through the growing seasons and related to soil properties, management, and their interactions using regression analysis. The spatial patterns of PAN were temporally stable, suggesting a temporal consistency in the spatial patterns of factors influencing PAN. The variation in soil temperature among landscape positions was very small, often only 1 to 2°C, and its contribution to the spatial variation in PAN was considered negligible. Soil water made only a small contribution to the variability in PAN because the seasonal average water‐filled pore space (SAWFPS) exhibited little variation across the landscape and often fell within the nonlimiting water range (NLWR) for N mineralization. Most of the variation in PAN within a season in this landscape was accounted for by variation in organic carbon (OC) content.