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A long‐term nitrogen fertilizer gradient has little effect on soil organic matter in a high‐intensity maize production system
Author(s) -
Brown Kimberly H.,
Bach Elizabeth M.,
Drijber Rhae A.,
Hofmockel Kirsten S.,
Jeske Elizabeth S.,
Sawyer John E.,
Castellano Michael J.
Publication year - 2014
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/gcb.12519
Subject(s) - fertilizer , environmental science , agronomy , organic matter , crop residue , agroecosystem , nitrogen , mineralization (soil science) , soil organic matter , chemistry , soil science , ecology , soil water , biology , agriculture , organic chemistry
Global maize production alters an enormous soil organic C ( SOC ) stock, ultimately affecting greenhouse gas concentrations and the capacity of agroecosystems to buffer climate variability. Inorganic N fertilizer is perhaps the most important factor affecting SOC within maize‐based systems due to its effects on crop residue production and SOC mineralization. Using a continuous maize cropping system with a 13 year N fertilizer gradient (0–269 kg N ha −1 yr −1 ) that created a large range in crop residue inputs (3.60–9.94 Mg dry matter ha −1 yr −1 ), we provide the first agronomic assessment of long‐term N fertilizer effects on SOC with direct reference to N rates that are empirically determined to be insufficient, optimum, and excessive. Across the N fertilizer gradient, SOC in physico‐chemically protected pools was not affected by N fertilizer rate or residue inputs. However, unprotected particulate organic matter ( POM ) fractions increased with residue inputs. Although N fertilizer was negatively linearly correlated with POM C/N ratios, the slope of this relationship decreased from the least decomposed POM pools (coarse POM ) to the most decomposed POM pools (fine intra‐aggregate POM ). Moreover, C/N ratios of protected pools did not vary across N rates, suggesting little effect of N fertilizer on soil organic matter ( SOM ) after decomposition of POM . Comparing a N rate within 4% of agronomic optimum (208 kg N ha −1 yr −1 ) and an excessive N rate (269 kg N ha −1 yr −1 ), there were no differences between SOC amount, SOM C/N ratios, or microbial biomass and composition. These data suggest that excessive N fertilizer had little effect on SOM and they complement agronomic assessments of environmental N losses, that demonstrate N 2 O and NO 3 emissions exponentially increase when agronomic optimum N is surpassed.