Nitrogen Fertilizer Suppresses Mineralization of Soil Organic Matter in Maize Agroecosystems

被引:112
作者
Mahal, Navreet K. [1 ,3 ]
Osterholz, William R. [1 ,4 ]
Miguez, Fernando E. [1 ]
Poffenbarger, Hanna J. [1 ,5 ]
Sawyer, John E. [1 ]
Olk, Daniel C. [2 ]
Archontoulis, Sotirios, V [1 ]
Castellano, Michael J. [1 ]
机构
[1] Iowa State Univ, Dept Agron, Ames, IA 50011 USA
[2] USDA ARS, Natl Lab Agr & Environm, Ames, IA USA
[3] South Dakota State Univ, Dept Agron Hort & Plant Sci, Brookings, SD 57007 USA
[4] USDA ARS, Soil Drainage Res Unit, Columbus, OH USA
[5] Univ Kentucky, Dept Plant & Soil Sci, Lexington, KY USA
基金
美国农业部;
关键词
fertilizer nitrogen use efficiency; N mineralization; priming effect; agronomic optimum N rate; synthetic N fertilizer; continuous maize system; USE EFFICIENCY; N MINERALIZATION; DECOMPOSITION; FATE; CORN; AVAILABILITY; TEMPERATURE; DECREASES; GRASSLAND; TURNOVER;
D O I
10.3389/fevo.2019.00059
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The possibility that N fertilizer increases soil organic matter (SOM) mineralization and, as a result, reduces SOM stocks has led to a great debate about the long-term sustainability of maize-based agroecosystems as well as the best method to estimate fertilizer N use efficiency (FNUE). Much of this debate is because synthetic N fertilizer can positively or negatively affect SOM mineralization via several direct and indirect pathways. Here, we test a series of hypotheses to determine the direction, magnitude, and mechanism of N fertilizer effect on SOM mineralization and discuss the implications for methods to estimate FNUE. We measured the effect of synthetic N fertilizer on SOM mineralization via gross ammonification at two long-term experiments in central and southern Iowa, USA with replicated plots of continuous maize that received one of three "historical" N fertilizer rates (zero, moderate or high) from 1999 to 2014. In 2015, prior to our measurements, we split the historical N fertilizer rate plots into two subplots that received either the site-specific agronomic optimum N rate or zero N fertilizer. At the onset of rapid maize N uptake, N fertilizer reduced gross ammonification by 13-21% (2-5 kg NH4-N ha(-1) d(-1)). A companion laboratory experiment rejected the hypothesis that differences in net primary productivity between fertilized and unfertilized treatments explained the negative effect of N fertilizer on SOM mineralization. Moreover, the NH4+ pool size was negatively correlated with the gross ammonification rate (r(2) = 0.85, p < 0.001). Thus, we conclude that NH4+-N fertilizer had a direct suppressive effect on SOM mineralization. These results demonstrate that the direct effect of N fertilizer on microbial activity can exceed the indirect effects of N fertilizer via large changes in NPP that alter organic matter inputs, soil temperature and moisture content. The magnitude of this effect and specificity to NH4+-N has significant implications for fertilizer management as well as the measurement and modeling of agroecosystem N dynamics including FNUE.
引用
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页数:12
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