Characterization of Mollisols after Long-Term N Fertilization at Successive Rates in Continuous and Rotated Corn Systems

Modern agricultural systems rely on inorganic nitrogen (N) fertilization to enhance crop yields, but its overuse may negatively impact soil properties. Soil properties to a depth of 90 cm were studied after 36 years of inorganic N fertilization at successive rates of 0, 202, and 269 kg N ha<sup&g...

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Glavni autori: Nakian Kim, Gevan D. Behnke, María B. Villamil
Format: Članak
Jezik:English
Izdano: MDPI AG 2022-03-01
Serija:Agronomy
Teme:
Online pristup:https://www.mdpi.com/2073-4395/12/3/625
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author Nakian Kim
Gevan D. Behnke
María B. Villamil
author_facet Nakian Kim
Gevan D. Behnke
María B. Villamil
author_sort Nakian Kim
collection DOAJ
description Modern agricultural systems rely on inorganic nitrogen (N) fertilization to enhance crop yields, but its overuse may negatively impact soil properties. Soil properties to a depth of 90 cm were studied after 36 years of inorganic N fertilization at successive rates of 0, 202, and 269 kg N ha<sup>−1</sup> (N0, N202, and N269) in continuous corn production [<i>Zea mays</i> L.] (CCC), and the corn (Cs) and soybean [<i>Glycine max</i> (L.) Merr.] (Sc) phases of a corn-soybean (CS) rotation. Experimental plots were arranged as a split-plot in a randomized complete block design with three replications. High levels of N fertilization under CCC acidified the topsoil (N0 pH 6.6 vs. N269 pH 4.9), and increased the nitrate level eight-fold compared to unfertilized controls. Under CCC, N0 had more than twice the available phosphorus level (P) and 40% more potassium (K) than the fertilized soils. Though treatments did not impact the soil organic carbon (SOC) content, water aggregate stability (WAS) decreased during the soybean phase of the rotated treatment (Sc) when compared to CCC. Fertilization affected soil bulk density (BD), which decreased by 5% from N0 to N269 across rotations. Averaged since the start of the study, corn yields increased by 60% with N fertilizer use compared to the unfertilized controls (N0). The corn grain yield benefited from the rotation with soybeans rendering 17% more grain yield in Cs than in CCC. Yet this benefit rose to 45% more grain yield on average, when no N fertilizer was used in Cs. Our results showed that there are important trade-offs with N fertilization and long-term use of corn monocultures, as its long-term use, even in the fertile and resilient soils on the Midwestern U.S., has led to P and K depletion, soil acidification, and potentially exacerbated N losses to the environment.
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spelling doaj.art-1592460c43484991a48b126a97ef29fa2023-11-30T20:44:14ZengMDPI AGAgronomy2073-43952022-03-0112362510.3390/agronomy12030625Characterization of Mollisols after Long-Term N Fertilization at Successive Rates in Continuous and Rotated Corn SystemsNakian Kim0Gevan D. Behnke1María B. Villamil2Department of Crop Sciences, University of Illinois, 1102 S. Goodwin Ave., Urbana, IL 61801, USADepartment of Crop Sciences, University of Illinois, 1102 S. Goodwin Ave., Urbana, IL 61801, USADepartment of Crop Sciences, University of Illinois, 1102 S. Goodwin Ave., Urbana, IL 61801, USAModern agricultural systems rely on inorganic nitrogen (N) fertilization to enhance crop yields, but its overuse may negatively impact soil properties. Soil properties to a depth of 90 cm were studied after 36 years of inorganic N fertilization at successive rates of 0, 202, and 269 kg N ha<sup>−1</sup> (N0, N202, and N269) in continuous corn production [<i>Zea mays</i> L.] (CCC), and the corn (Cs) and soybean [<i>Glycine max</i> (L.) Merr.] (Sc) phases of a corn-soybean (CS) rotation. Experimental plots were arranged as a split-plot in a randomized complete block design with three replications. High levels of N fertilization under CCC acidified the topsoil (N0 pH 6.6 vs. N269 pH 4.9), and increased the nitrate level eight-fold compared to unfertilized controls. Under CCC, N0 had more than twice the available phosphorus level (P) and 40% more potassium (K) than the fertilized soils. Though treatments did not impact the soil organic carbon (SOC) content, water aggregate stability (WAS) decreased during the soybean phase of the rotated treatment (Sc) when compared to CCC. Fertilization affected soil bulk density (BD), which decreased by 5% from N0 to N269 across rotations. Averaged since the start of the study, corn yields increased by 60% with N fertilizer use compared to the unfertilized controls (N0). The corn grain yield benefited from the rotation with soybeans rendering 17% more grain yield in Cs than in CCC. Yet this benefit rose to 45% more grain yield on average, when no N fertilizer was used in Cs. Our results showed that there are important trade-offs with N fertilization and long-term use of corn monocultures, as its long-term use, even in the fertile and resilient soils on the Midwestern U.S., has led to P and K depletion, soil acidification, and potentially exacerbated N losses to the environment.https://www.mdpi.com/2073-4395/12/3/625soil acidificationnitrificationsoil organic carbon
spellingShingle Nakian Kim
Gevan D. Behnke
María B. Villamil
Characterization of Mollisols after Long-Term N Fertilization at Successive Rates in Continuous and Rotated Corn Systems
Agronomy
soil acidification
nitrification
soil organic carbon
title Characterization of Mollisols after Long-Term N Fertilization at Successive Rates in Continuous and Rotated Corn Systems
title_full Characterization of Mollisols after Long-Term N Fertilization at Successive Rates in Continuous and Rotated Corn Systems
title_fullStr Characterization of Mollisols after Long-Term N Fertilization at Successive Rates in Continuous and Rotated Corn Systems
title_full_unstemmed Characterization of Mollisols after Long-Term N Fertilization at Successive Rates in Continuous and Rotated Corn Systems
title_short Characterization of Mollisols after Long-Term N Fertilization at Successive Rates in Continuous and Rotated Corn Systems
title_sort characterization of mollisols after long term n fertilization at successive rates in continuous and rotated corn systems
topic soil acidification
nitrification
soil organic carbon
url https://www.mdpi.com/2073-4395/12/3/625
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AT gevandbehnke characterizationofmollisolsafterlongtermnfertilizationatsuccessiveratesincontinuousandrotatedcornsystems
AT mariabvillamil characterizationofmollisolsafterlongtermnfertilizationatsuccessiveratesincontinuousandrotatedcornsystems