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A meta-evaluation of nitrapyrin agronomic and environmental effectiveness with emphasis on corn production in Midwestern USA

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The effectiveness of nitrification inhibitors for abatement of N loss from the agroecosystem is difficult to measure at typical agronomic scales, since performance varies at the research-field scale due to complex interactions among crop management, soil properties, length of the trial, and environmental factors. The environmental impact of the nitrification inhibitor nitrapyrin on N losses from agronomic ecosystems was considered with emphasis on the Midwestern USA. A meta-evaluation approach considered the integrated responses to nitrification inhibition found across research trials conducted in diverse environments over many years as measured in side-by-side comparisons of fertilizer N or manure applied with and without nitrapyrin. The resulting distributions of response indices were evaluated with respect to the magnitude and variance of the agronomic and environmental effects that may be achieved when nitrification inhibitors are used regionally over time. The indices considered (1) crop yield, (2) annual or season-long maintenance of inorganic N within the crop root zone, (3) NO3-N leached past the crop root zone, and (4) greenhouse gas emission from soil. Results showed that on average, the crop yield increased (relative to N fertilization without nitrapyrin) 7% and soil N retention increased by 28%, while N leaching decreased by 16% and greenhouse gas emissions decreased by 51%. In more than 75% of individual comparisons, use of a nitrification inhibitor increased soil N retention and crop yield, and decreased N leaching and volatilization. The potential of nitrification inhibitors for reducing N loss needs to be considered at the scale of a sensitive region, such as a watershed, over a prolonged period of use as well as within the context of overall goals for abatement of N losses from the agroecosystem to the environment.
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A meta-evaluation of nitrapyrin agronomic and environmental
effectiveness with emphasis on corn production in the Midwestern USA
Jeffrey D. Wolt
Research and Development Laboratories, Dow AgroSciences LLC, Indianapolis, IN 46262, USA; present
address: 164 Seed Science Center, Iowa State University, Ames, IA 50011-3228, USA; (fax: +1-515-294-2014;
e-mail: jdwolt@iastate.edu)
Received 3 April 2003; accepted in revised form 19 December 2003
Key words: Inorganic nitrogen, Leaching, Nitrification inhibitor, Nitrous oxide
Abstract
The effectiveness of nitrification inhibitors for abatement of N loss from the agroecosystem is difficult to mea-
sure at typical agronomic scales, since performance varies at the research-field scale due to complex interactions
among crop management, soil properties, length of the trial, and environmental factors. The environmental im-
pact of the nitrification inhibitor nitrapyrin on N losses from agronomic ecosystems was considered with empha-
sis on the Midwestern USA. A meta-evaluation approach considered the integrated responses to nitrification
inhibition found across research trials conducted in diverse environments over many years as measured in side-
by-side comparisons of fertilizer N or manure applied with and without nitrapyrin. The resulting distributions of
response indices were evaluated with respect to the magnitude and variance of the agronomic and environmental
effects that may be achieved when nitrification inhibitors are used regionally over time. The indices considered
1crop yield, 2annual or season-long maintenance of inorganic N within the crop root zone, 3NO
3
-N leached
past the crop root zone, and 4greenhouse gas emission from soil. Results showed that on average, the crop
yield increased relative to N fertilization without nitrapyrin7% and soil N retention increased by 28%, while N
leaching decreased by 16% and greenhouse gas emissions decreased by 51%. In more than 75% of individual
comparisons, use of a nitrification inhibitor increased soil N retention and crop yield, and decreased N leaching
and volatilization. The potential of nitrification inhibitors for reducing N loss needs to be considered at the scale
of a sensitive region, such as a watershed, over a prolonged period of use as well as within the context of overall
goals for abatement of N losses from the agroecosystem to the environment.
Introduction
The use of nitrification inhibitors is an established
agronomic practice for conservation of fertilizer ni-
trogen in the root zone where it may be utilized by a
crop. A side effect of this practice is environmental
protection afforded by the reduction of N loss from
the agroecosystem. A substantial amount of literature
details the environmental and agronomic performance
of nitrification inhibitors when used in combination
with N fertilizer or manure see Meisinger et al. 1980;
Wolt 2000. Even though most published data focuses
on nitrification inhibition as a crop production tool
see, for instance, Meisinger et al. 1980, this same
body of information provides considerable insight as
to N stabilization through application of nitrification
inhibitors, with the consequences of altered move-
ment of N from the root zone by either leaching or
volatilization.
Nutrient Cycling in Agroecosystems 69: 23–41, 2004.
© 2004 Kluwer Academic Publishers. Printed in the Netherlands.
23
Nitrification inhibitor performance and variability
in response
As with any technology aimed at nutrient manage-
ment, nitrification inhibitor performance in reducing
N losses through leaching or volatilization will be
variable at the field level due to complex interactions
among crop management, soil, and environmental
factors. The microbial ecology of bacterial nitrifiers
is considerably influenced by multiple factors that
confound interpretations of nitrification inhibitor per-
formance Keeney 1980. The persistence and activ-
ity of nitrification inhibitors in the soil will also be
affected by many of these same factors Touchton et
al. 1978b; Wolt 2000. Thus, the year-to-year
performance of a nitrification inhibitor in a given field
or research plot may vary, even though the perform-
ance attributes of the nitrification inhibitor may be
evident when considered across a larger region, such
as a watershed or ecoregion, over time.
Nitrification inhibitors have been shown under a
variety of field and laboratory conditions to reduce
nitrate-N leaching as compared to fertilizer-only
treatments Wolt 2000. Reduced leaching is achieved
when nitrification inhibition in the crop root zone al-
lows for N to be retained in the upper soil profile and
utilized by the crop. This effect is best documented in
long-term lysimeter studies where annual reduction in
N loss is observed. For instance, Owens 1987
showed that with 6 years continuous use of the nitri-
fication inhibitor nitrapyrin for corn production in
Ohio, USA, cumulative N leaching was reduced an
average of 20% in comparison to fertilizer application
without a nitrification inhibitor. Similar effects have
been shown in other environments Yadav 1997;
Randall 2000, but in contrast there are instances
where a variable benefit of nitrification inhibition is
observed see, for example, Timmons 1984.
The greenhouse gas nitrous oxide is produced in
soils during both nitrification of ammonium-N and
denitrification of nitrate-N, with the greater level be-
ing produced by denitrification. Accelerated nitrous
oxide fluxes from annual cropping systems are likely
a consequence of high N availability Robertson et al.
2000. There appears to be a direct effect of nitrifica-
tion inhibitors on reducing nitrous oxide produced
during nitrification, while the effect on denitrification
appears to be indirect from lower soil nitrate levels.
Bronson and Mosier 1993reported that nitrification
inhibitors applied with N fertilizer decreased nitrous
oxide emissions by 43 to 71% when periodic
measurements were taken from time of fertilization to
harvest in a field trial of irrigated corn. In addition to
the effect on nitrous oxide loss from soil, there is
some evidence to indicate that nitrification inhibitors
also reduce the efflux of methane from soil, perhaps
through an indirect effect on methanotroph ecology
Arif et al. 1996. The environmental benefit of
reduced greenhouse gas emissions may be offset by
efflux of acid-forming NH
3
in situations where nitri-
fication inhibitor use occurs in conjunction with sur-
face-applied urea or ammonium fertilizers in warm,
moist soils Harrison and Webb 2001.
Nitrification inhibitor performance in soils is most
effective and consistent when conditions favor slower
biological degradation of the inhibitor and reduced
Nitroso-group bacterial activity. Thus, optimal per-
formance is more common with late fall or early
spring application when soil temperatures are low.
These periods are associated with increased ground-
water recharge and runoff in continental temperate
climates due to lower evapotranspiration and seasonal
precipitation patterns. As a consequence of the tem-
perature effect, historical nitrification inhibitor per-
formance has generally been best in the upper
Midwestern USA as compared to more southerly cli-
mates. Nitrification inhibitor performance is best es-
tablished for corn, since this crop has an especially
high N requirement and is frequently grown on soils
with high N-loss potential, namely, poorly drained
soils, tile-drained soils, and irrigated sandy soils. The
efficacy and environmental effects of nitrification in-
hibition are best documented for the intense corn
production region of the upper Midwest. The greatest
environmental benefits of nitrification inhibitors nor-
mally occur when used with rates of N fertilization
that are well matched to crop N demand Wolt 2000;
therefore, nitrification inhibitor use is compatible with
other nutrient management technologies that improve
N-use efficiency.
Meta-effects evaluation of nitrification inhibitor
performance
The published literature regarding nitrification inhibi-
tor performance in the field focuses nearly exclu-
sively on the effects achieved at the research scale;
that is, individually, the data reflect performance at
the field or research-plot scale and over typical time
spans of one to three years. In contrast, any environ-
mental effect of nitrification inhibition on N loss will
be of consequence at the scale of a vulnerable water-
24
shed or larger over a period of many years. Crop
environment management factors contribute to
variability at the field scale that lends uncertainty to
the annual realization of microeconomic benefits
from nitrification inhibitors when used for yield en-
hancement Nelson and Huber 1980, even though
there may be societal benefits of nitrification inhibi-
tor use over broader scales of space and time for re-
duction of N loss from agroecosystems to the
environment. The research reported herein considers
comprehensively the environmental effect of nitrifi-
cation inhibition using a meta-evaluation approach
that probabilistically treats the distribution in out-
comes found across studies conducted in diverse en-
vironments over many years. The meta-evalution
approach entails integrated description of heteroge-
neous data. In the present case, data from short-dura-
tion agronomic trails conducted under diverse condi-
tions were integrated to allow for a generalized
assessment of agronomic and environmental effec-
tiveness. Such an approach provides insight in to the
environmental benefit that may be achieved when ni-
trification inhibition is used regionally over time.
Data detailing the effectiveness of the product
nitrapyrin 2-chloro-6-trichloro-methylpyridineare
considered here, since this product has been used for
nitrification inhibition in the intense corn production
regions of the Midwestern USA for over 25 years and
its efficacy in controlling N loss is well documented
in the published literature.
Methods
A detailed review of published literature was con-
ducted to identify research trials where indices of ef-
fectiveness of nitrification inhibition were measured
in side-by-side comparisons of N fertilizer or manure
with and without added nitrapyrin. The indices
selected for consideration were 1grain yield
indicative of N availability and retention in the crop
root zone,2annual or season-long maintenance of
inorganic N typically, NH
4
-N plus NO
3
-Nwithin
the crop root zone, 3N leached past the crop root
zone, and 4gaseous flux typically N
2
O volatiliza-
tionfrom soil.
For those trials where relevant data were identified,
the relative effect of nitrapyrin was calculated as the
difference in effect observed for the comparable
treatment without nitrapyrin, expressed as a percent-
age of the effect without nitrapyrin 关共effect with ni-
trapyrin effect without nitrapyrin100/effect
without nitrapyrin, for a given location and year.
When the study design involved multiple compari-
sons, such as the effect of nitrapyrin over a range of
N levels or N sources, the average effect across these
treatments was determined. The intention of this
analysis is to consider the effects of nitrification inhi-
bition that may be expected with typical grower prac-
tice; therefore, control treatments receiving no N or
treatments using N fertilization rates well in excess
of crop N demand were typically not considered.
Treatments using nitrapyrin well in excess of the
maximum recommended use rate 1.12 kg ai ha
–1
;
Dow AgroSciences 1999were also excluded from
consideration.
For many of the studies reported, the original re-
sults were summarized in figures. In these instances,
the relevant information for comparisons of nitrapy-
rin effect were translated from graphical to tabular
form by scanning the figures and extracting the data
using UnGraph version 4.0 BIOSOFT, Cambridge,
UK.
The data from the literature were used to develop a
statistical distribution of relative effect of nitrapyrin
on the indices of interest, from which the grand mean
and standard error in response across studies were
developed and probabilities of nitrification inhibitor
effectiveness were determined.
Results
Grain yield
The database developed describing the effect of
nitrapyrin on grain yield consists of 189 observations
comprising 437 mean comparisons across 158 loca-
tion–years of experiments Table 1. The preponder-
ance of data are for field corn yield, but yields of
wheat, grain sorghum, and sweet corn are also
included. These data reflect studies conducted princi-
pally in the Midwestern USA, but also include results
from transitional climate zones in the Southeastern
USA and from Europe. The distribution in mean re-
sponse for a given yield comparison ranges from
20.1 to 60.9%, with 141 of 189 observations
showing a positive effect of nitrapyrin on yield Fig-
ure 1. The grand mean standard error of the
meaneffect represents a relative yield increase from
nitrapyrin of 7.0% 0.8%. Although the data de-
scribing the effect of nitrapyrin on yield do not de-
25
Table 1. Relative crop yield from nitrapyrin when applied with sources of fertilizer or manurial N.
Nitrogen fertilization practice
Relative
effect
%
a
Identity Crop Time Method Rate
kg ha
–1
Form
b
Soil subgroupReference
3.0 Ames IA 1982 Corn Spring Inject 112, 224 AA Nicollet Aquic Hapludollsand Webster Typic
Hapludolls
Blackmer and Sanchez
1988
0.0 Ames IA 1983
5.1 Ames IA 1984
1.9 Nashua IA 1982 Readlyn fAquic Hapludolls
20.1 Nashua IA 1983
0.3 Nashua IA 1984
1.9 Ames #1 IA 1985 Corn Spring Incorp 56, 112, 168 AS Nicollett Aquic HapludollsCerrato and Blackmer
1990
1.7 Ames #1 IA 1986
5.1 Ames #1 IA 1987
5.2 Ames #2 IA 1985 Canisteo Typic Haplaquolls
5.5 Ames #2 IA 1986
4.9 Ames #2 IA 1987
7.9 Holestein IA 1986 Galva Typic Hapludolls
0.5 Holestein IA 1987
2.0 Ida Grove IA 1986 Marshall Typic Hapludols
7.7 Ida Grove IA 1987
0.3 Iowa City IA 1985 Mahaska Aquic Agriudolls
5.0 Kalona IA 1985 Bremer Typic Agriaquolls
1.4 Kalona IA 1986
8.2 Kalona IA 1987
0.7 Marengo IA 1985 Nevin Aquic Agriudolls
3.9 Marengo IA 1986
4.8 Marengo IA 1997
1.2 Williamsburg IA 1985 Mahaska Aquic Agriudolls
11.3 Bath Co. KY 1976 Corn Spring Surface 85, 170 AN Lowell silt loam Typic HapludaflsFrye et al. 1981
19.6 Lee Co. KY 1978 85, 170 Monongahela silt loam Typic Paleudalfs
11.8 Lewis Co. KY 1977 85 Cavode silt loam Aeric Ochraquults
17.4 Princeton KY 1974 140 Tilsit silt loam Johnsburg silt loam intergrade
Typic Fragiudults
21.8 Princeton KY 1975 140
42.4 Princeton KY 1976 110
7.9 Princeton KY 1977 90, 135, 180
4.6 Princeton KY 1978 90, 135, 180
22.8 Buffalo ND 1997 Wheat Fall Inject 84 AA Gardena loam Pachic HapludollsGoos and Johnson 1999
5.3 Knox Co. IN 1974 Wheat Fall Surface 44, 88 Urea Patton silty clay loam Typic HaplaquollsHuber et al. 1980
4.7 Knox Co. IN 1975 Fall Surface Urea Alford silty loam Typic Haplualfs
0.0 Knox Co. IN 1977 Fall Inject AA
26
Table 1. Continued.
Nitrogen fertilization practice
Relative
effect
%
a
Identity Crop Time Method Rate
kg ha
–1
Form
b
Soil subgroupReference
8.2 LaGrange Co. IN
1973
Fall Inject, sur-
face
AA, Urea
17.6 LaGrange Co. IN
1973
Fall,
spring
Surface Urea Elston sandy loam Typic Agriudolls
16.1 LaGrange Co. IN
1977
Fall Inject, sur-
face
AA, Urea Ockley silty loam Typic Haplualfs
17.5 Sullivan Co. IN 1973 Fall Surface Urea, AS, CN Elston sandy loam Typic Agriudolls
1.5 Sullivan Co. IN 1973 Fall,
spring
Surface Urea, AS, CN
20.0 Sullivan Co. IN 1974 Fall Surface AS, CN Patton silty clay loam Typic Haplaquolls
21.5 Sullivan Co. IN 1975 Fall Surface AS, CN
8.4 Sullivan Co. #2 IN
1975
Fall Surface AS, CN Elston sandy loam Typic Agriudolls
44.4 Sullivan Co. IN 1976 Fall Surface AS Patton silty clay loam Typic Haplaquolls
11.2 Sullivan Co. IN 1976 Fall,
spring
Surface AS
7.2 Buttlerville IN 1992 Corn Spring Inject 67, 174, 280 AA Silty clay loam Huber et al. 1993
6.6 Buttlerville IN 1992 67, 174, 280 SM
2.8 Lafayette IN 1992 84, 168 AA Silt loam
6.0 Lafayette IN 1992 84, 168 SM
1.8 Pinney #3 IN 1992 112, 224 AA Tracy sandy loam Ultic Hapludalfs
4.1 Pinney #3 IN 1992 112, 224 SM
7.3 Vincennes IN 1992 67, 123 SM Fine sandy loam
3.0 Brookston OH Corn Fall Inject 90, 112 AA, UAN Brookston silty clay loam Typic AgriaquollsJohnson 1995
7.5 Brookston OH Spring 90, 112
10.7 Crosby OH Fall 112, 180 Crosby silt loam Aeric Epiaqualfs
7.2 Crosby OH Spring 112, 180
3.1 Hoytville OH Fall 180 Hoytville silty clay loam Mollic Epiaqualfs
3.8 Hoytville OH Spring 180
2.2 Scioto OH 1994 Corn Spring Inject 134 AA, UAN Kokomo silty clay loam Typic ArgiaquollsJohnson 1997
8.7 Scioto OH 1995
8.4 Scioto OH 1996
17.6 Germany 1977-81 Various Fall NR 65 338 Urea Sand-Rosterden Katzur et al. 1984
5.6 Germany 1977-81 Fall,
spring
65 338
12.9 Germany 1977-81 Spring 65 338
15.3 Germany 1982-87 Fall 108 280
21.6 Germany 1982-87 Fall,
spring
108 280
0.2 Belleville IL 1977 Wheat Fall Incorporate 45, 90, 135 Urea Weir silt loam Typic OrchaqualfsLiu et al. 1984
27
Table 1. Continued.
Nitrogen fertilization practice
Relative
effect
%
a
Identity Crop Time Method Rate
kg ha
–1
Form
b
Soil subgroupReference
3.3 Belleville IL 1977 Incorporate 45, 90, 135 UAN
7.0 Belleville IL 1977 Inject 45, 90, 135 AA
12.5 Belleville IL 1979 Incorporate 45, 90, 135 Urea
3.4 Belleville IL 1979 Incorporate 45, 90, 135 UAN
23.0 Belleville IL 1979 Inject 45, 90, 135 AA
5.4 Carbondale IL 1977 Incorporate 45, 90, 135 Urea Stoy silt loam Aquic Hapludalfs
1.7 Carbondale IL 1977 Incorporate 45, 90, 135 UAN
0.5 Carbondale IL 1977 Inject 45, 90, 135 AA
18.1 Carbondale IL 1979 Incorporate 45, 90, 135 Urea
23.5 Carbondale IL 1979 Incorporate 45, 90, 135 UAN
23.0 Carbondale IL 1979 Inject 45, 90, 135 AA
4.0 Carbondale IL 1980 Incorporate 50, 100, 150 Urea
1.6 Rossville KS 1978 Corn Spring Inject 84, 168, 252 AA Eudora fine sandy loam Fleuventic HapluquollsMaddux et al. 1985
0.1 Rossville KS 1979 Fall,
spring
84, 168
1.6 Rossville KS 1979
#III
Spring 84, 168
3.4 Scandia KS 1979 Fall,
spring
84, 168 Crete silty loam Pachic Argiustolls
10.1 St John KS 1979 Fall,
spring
84, 168 Pratt loamy fine sand Psammentic Haplustalfs
9.1 Becker MN Corn Spring Incorporate 134 Urea, UAN Hubbard lomy coarse sand Udorthentic Hap-
loborolls
Malzer 1989
4.5 IA 1987 Spring Inject 157 AA, Urea Webster clay loam Typic Hapudolls
3.9 MN 1982 Fall,
Spring
Inject 134 AA
0.5 MN #2 1982 Spring Inject, In-
corp
157 168 AA, UAN,
Urea
Coarse-textured soil
26.7 MN 1982,83 Spring Inject, In-
corp
157 168 AA, UAN,
Urea
0.0 MN 1983 Spring Inject 134 AA Webster clay loam Typic Hapudolls
1.3 MN 1985, 86, 87 Spring Inject, In-
corp
157 168 AA, UAN,
Urea
Coarse-textured soil
20.0 Northern IL 1983 Spring Inject, In-
corp
NR SM Derinda silt loam Oxyaquic Hapludalfs
10.5 Northern IL 1984 Spring Inject, In-
corp
NR SM
0.1 Northern IL 1985 Spring Inject, In-
corp
NR SM
28
Table 1. Continued.
Nitrogen fertilization practice
Relative
effect
%
a
Identity Crop Time Method Rate
kg ha
–1
Form
b
Soil subgroupReference
7.5 Northern IL 1986 Spring Inject, In-
corp
NR SM
1.4 WI 1984, 85, 86 Spring Inject, In-
corp
157 168 AA, UAN,
Urea
Coarse-textured soil
0.3 WI 1987 Spring Inject, In-
corp
134 AA, UAN,
Urea
23.5 Becker MN Spring Incorp 134 Urea Hubbard loamy coarse sand Udorthentic Hap-
loborolls
15.2 Becker MN Spring Incorp 134 UAN
3.7 West Lafayette IN
1978
Corn Spring Inject 154, 345 SM Chalmers silty clay loam Typic HaplaquollsMcCormick et al. 1984
60.0 West Lafayette IN
1979
Fall 75, 144 SM
1.7 West Lafayette IN
1979
Fall 168 AA
4.3 West Lafayette IN
1979
Spring 161 SM
0.9 West Lafayette IN
1979
Spring 168 AA
27.9 West Lafayette IN
1980
Fall 104, 166 SM
1.4 West Lafayette IN
1980
Fall 168 AA
12.7 West Lafayette IN
1980
Spring 159, 286 SM
11.5 West Lafayette IN
1980
Spring 168 AA
15.6 GA 1978 Sweet
corn
Spring Surface 40 AS CN Cecil clay loam McElhannon and Mills
1981
19.9 GA 1979
3.2 Marna G MN Corn Fall,
spring
Inject 170, 340 SM Marna silty clay loam Typic HapludollsRandall et al. 1999
7.9 Nicollet A MN 64, 127 DM Nicollet clay loam Aquic Halludolls
0.9 Nicollet C MN 59, 118 DM
7.3 Nicollet E MN 113, 226 SM
2.6 Nicollet F MN 215, 431 SM
3.4 Port Bryan B MN 59, 118 DM Port Bryan silt loam Typic Hapludolls
0.5 Webster D MN 66, 133 DM Webster clay loam Typic Endoaquolls
23.9 El Reno OK 1991-94 Wheat Fall Surface 60 Urea Renfrow silt loam, pH 4.8, 1% OC Rao 1996
1.6 El Reno OK 1991-94 Incorporate
29
Table 1. Continued.
Nitrogen fertilization practice
Relative
effect
%
a
Identity Crop Time Method Rate
kg ha
–1
Form
b
Soil subgroupReference
6.8 Hamerly A MN 1992 Corn Spring Inject 93 DM Hamerly clay loam Aeric CalciaquollsSchmitt et al. 1995
19.4 Maxcreek C MN
1992
69 DM Maxcreek silty clay loam Typic Endoaquolls
3.5 Maxfield D MN 1992 119 DM Maxfield silty clay loam Typic Endoaquolls
2.7 Maxfield F MN 1993 129 SM
5.8 Racine B MN 1992 106 SM Racine silt loam Mollic Haplualfs
6.5 Schley G MN 1993 80 SM Schley silt loam Udollic Ochraqualfs
4.1 Webster E MN 1993 63 SM Webster clay loam Typic Haplaquolls
2.0 Springfield OH 1978 Corn Fall Inject 90, 180 AA Crosby silt loamAeric EpiaqualfsStehouwer and Johnson
1990
3.5 Springfield OH 1978 Spring
16.1 Springfield OH 1979 Fall
2.4 Springfield OH 1979 Spring
22.2 Springfield OH 1980 Fall
0.6 Springfield OH 1980 Spring
5.4 Springfield OH 1981 Fall
14.1 Springfield OH 1981 Spring
0.8 Springfield OH 1982 Fall
12.5 Springfield OH 1982 Spring
3.9 Springfield OH 1983 Spring
2.2 Springfield OH 1983 Spring
0.0 Springfield OH 1984 Fall
0.7 Springfield OH 1984 Spring
8.2 Springfield OH 1985 Fall
5.6 Springfield OH 1985 Spring
6.5 Crawfordsville IN
1982
Corn Spring Inject 238 AA SM Odell silt loam Aquic AgridollsSutton et al. 1985, 1986
5.9 Crawfordsville IN
1982
Winter 211
5.1 Crawfordsville IN
1983
Late fall 193
11.7 Crawfordsville IN
1983
Spring 122
5.4 Crawfordsville IN
1984
Late fall 214
0.6 Crawfordsville IN
1984
Spring 271
0.0 Brownstown IL 1976 Corn Fall Inject 67, 134 AA Cisne silt loam Mollic AlbaqualfsTouchton et al. 1979a
0.1 Brownstown IL 1976 Spring
14.6 Urbana IL #2 1976 Corn Fall Incorp 67, 134 Urea Flanagan silt loam Typic HapludollsTouchton et al. 1979b
30
Table 1. Continued.
Nitrogen fertilization practice
Relative
effect
%
a
Identity Crop Time Method Rate
kg ha
–1
Form
b
Soil subgroupReference
2.0 Urbana IL 1975 Spring Inject 67, 134, 268 AA Drummer clay loam Typic Haplaquolls
12.1 Urbana IL 1976 Fall Inject 67, 134, 268 AA
3.6 Urbana IL 1976 Spring Inject 67, 134, 268 AA
0.1 Bonanza Farm MN
1980
Corn Spring Incorp 90, 180 Urea Estherville sandy loam Typic HapludollsWalters and Malzer
1990a
1.5 Bonanza Farm MN
1981
2.2 Bonanza Farm MN
1982
206.9 Sullivan Co. #1 IN
1973
Corn Late fall Inject 134 AA Kings silty clay Vertic EndoaquollsWarren et al. 1975
1.3 Sullivan Co. #2 IN
1973
200 Elston fine sandy loam Typic Agriudolls
30.7 Sullivan Co. #2 IN
1974
134, 224
8.7 Pinney #1 IN Corn Fall Inject 83, 166 AA Runnymede loam Typic ArgiaguollsWarren et al. 1980
0.6 Pinney #1 IN Spring 83, 166
18.8 Pinney #2 IN Fall 83, 166 Tracy sandy loam Ultic Hapludalfs
1.7 Pinney #2 IN Spring 83, 166
9.8 West Lafayette IN Fall 66, 132 Chalmers silty clay loam Typic Haplaquolls
1.0 West Lafayette IN Spring 66. 132
13.1 Hix IN 1982 Corn Spring Inject 175 DM Blount clay Aeric OchraqualfsWelty et al. 1986
2.1 Hix IN 1983 143
21.5 Hix IN 1984 349
16.8 Jackson IN 1982 349
60.9 Jackson IN 1983 349
25.4 Jackson IN 1984 349
0.3 Altus OK 1976 Grain
sorghum
Late
spring
Inject, In-
corp
45, 90, 180 AA, Urea Holister clay loam Pachic PaleustollsWesterman et al. 1981
0.8 Altus OK 1978 67, 134, 201 UAN
8.4 Altus OK 1979
1.6 Haskell OK 1979 Taloka silt loam Mollic Albaqualfs
7.4 Tipton OK 1977 Urea, UAN Tipton fine sandy loam Pachic Agriustolls
3.5 Lewisburg TN 1982 Corn Fall Surface 376 DM Huntington silt loam Fluvaquentic EutrochreptsWolt 1985
4.1 Lewisburg TN 1982 Spring Inject 376 DM
3.9 Lewisburg TN 1982 Spring Incorp 140 AN
14.5 Lewisburg TN 1983 Fall Surface 341 DM
17.4 Lewisburg TN 1983 Spring Inject 341 DM
7.4 Lewisburg TN 1983 Spring Incorp 140 AN
9.1 Blackville SC 1981 Corn Spring Incorp 168 UAN Varina loamy sand Plinthic PaleudultsZublena 1984
31
scribe an effect on reduced environmental loss of
fertilizer N per se, they are an integrated measure of
N availability during the crop cycle and, therefore, are
directionally indicative of N lost from the agroeco-
system increased N availability to the crop represents
N which was not lost from the root zone.
Inorganic N in the root zone
In comparison to the database for yield response, that
for inorganic N in the root zone is somewhat more
limited 50 observations comprising 43 location–
years of experimental results reflecting varied annual
or season-long sampling strategies; Table 2. Results
are also more variable, ranging from 39.8 to
135.3%. The grand mean standard erroreffect
for nitrapyrin to increase inorganic N retained in the
root zone is 28.2% 5.4%relative to N retention
in the absence of a nitrification inhibitor Figure 2.
Thirty-nine of 50 observations show a benefit from
nitrapyrin in terms of increased year-long or seasonal
inorganic N retention in the root zone and, conse-
quently, reduced N loss from agroecosystems. These
data largely represent soil N retention during the crop
cycle in which nitrapyrin is applied; therefore, they
do not indicate the long-term fate of seasonally
retained N within the agroecosystem.
N leached from the root zone
The database for N leached from the root zone con-
firms the trend for nitrapyrin application with fertil-
izer or manurial N to increase yield and root zone N
retention Table 3. Twenty-four observations com-
prising 26 location–years of experimental results de-
scribe N occurrence in percolates or in soil sampled
from below the root zone. As with measurements of
inorganic N within the root zone, these data largely
reflect the leaching of N that occurs within the crop
cycle when a nitrification inhibitor is used. The rela-
tive percent N leached when nitrapyrin was used
ranges from 42.6 to 31.7. The grand mean
standard erroreffect is 15.8% 3.8%, indica-
tive of reduced N transport in soil percolates. Nine-
teen of 24 observations show a benefit from nitrapyrin
in terms of decreased year-long or seasonal inorganic
N loss out of the root zone Figure 3.
Table 1. Continued.
Nitrogen fertilization practice
Relative
effect
%
a
Identity Crop Time Method Rate
kg ha
–1
Form
b
Soil subgroupReference
6.7 Blackville SC 1982
4.5 Florence SC 1981 Bonneau sand Arenic Paleudults
3.4 Florence SC 1982 Goldsboro loamy sand Aquic Paleudult
3.1 Sumter SC 1981 Dothan sandy loam Plinthic Paleudults
23.0 Sumter SC 1982
a
关共effect with nitrapyrin effect without nitrapyrin100/effect without nitrapyrin;
b
AA, anhydrous ammonia; AN, ammonium nitrate; AS, ammonium sulfate; CN, calcium nitrate;
DM, dairy manure, SM, swine manure; UAN, uryl ammonium nitrate.
32
Volatilization of greenhouse gases
A somewhat more limited set of data describes the
relative impact of nitrapyrin use on N loss to the at-
mosphere Table 4. Nitrapyrin may contribute to re-
duced emission of gases from agricultural soils
through a variety of direct and indirect mechanisms
and, therefore, the nature and the particular volatile
compound that is considered governs the magnitude
of the effect attributed to nitrapyrin. Denitrification
losses of N in the form of N
2
O are the most directly
attributable to inhibition of nitrification, whereas ef-
fects on CH
4
emission will be more indirect through
shifts in microbial processes in the agroecosystems
13 of the comparisons summarized in Table 4
describe NO
2
efflux and 1 describes CH
4
efflux.In
any event, overall these data demonstrate an effect of
nitrapyrin to reduce atmospheric emission of green-
house gases with an overall mean standard error
effect of 51.2% 4.0%兲共
Figure 4.
Discussion
A large body of literature describes the performance
of nitrification inhibitors in terms of crop response
Figure 1. Frequency distributions describing the relative change in crop yield attributable to nitrification inhibition for comparisons of N
fertilization with and without nitrapyrin mean ————; standard error ···············.
Figure 2. Frequency distributions describing the relative change in root zone N retention attributable to nitrapyrin for comparisons of N
fertilization with and without nitrapyrin mean ————; standard error ···············.
33
and N fate within agronomic ecosystems. Consider-
able variability in response is reported from individ-
ual research findings and is anticipated based on the
numerous crop, environment, and management fac-
tors that in combination contribute variability to the
processes whereby N is cycled and utilized within
crop production systems. When described in terms of
relative responses among diverse experiments, indi-
ces of N loss indicate a consistent effect of nitrifica-
tion inhibitor use in conjunction with N fertilization.
The distributions of effects when compared across
various indices of N loss Figure 5show that for
75% of the comparisons considered, nitrapyrin in-
creased annual or season-long N retention in the crop
root zone, increased crop yield, decreased N leaching
from the root zone, and decreased volatilization of
greenhouse gases.
On a regional basis over time, factors such as ni-
trogen fertilization practice rate, timing, source,
placement, soil factors texture, organic matter con-
tent, pH, and environmental conditions soil cover,
temperature, moisturecombine to influence the
overall performance of a nitrification inhibitor. The
integrated effect of these factors on nitrapyrin
performance is represented by the meta-evaluation of
diverse studies that in combination describe the an-
ticipated effect of sustained use of nitrification inhibi-
tors in a region over time. The observed variance in
Figure 3. Frequency distributions describing the relative change in N leached from the root zone attributable to nitrapyrin for comparisons of
N fertilization with and without nitrapyrin mean ————; standard error ···············.
Figure 4. Frequency distributions describing the relative change in greenhouse gas emissions attributable to nitrapyrin for comparisons of N
fertilization with and without nitrapyrin mean ————; standard error ···············.
34
Table 2. Relative amount of inorganic N retained within the crop root zone as affected by nitrapyrin applied with sources of fertilizer or manurial N.
Nitrogen fertilization practice
Relative
effect %
a
Identity Crop Time Method Rate
kg ha
–1
Form
b
Soil subgroupReference
15.8 Marengo IA 1986 Corn Spring Incorporate 56, 112,
178
AS Nevin Aquic AgriudollsCerrato and Blackmer
1990
0.9 Kalona IA 1986 Bremer Typic Agriaquolls
4.9 Ames #1 IA 1986 Nicollett Aquic Hapludolls
5.7 Ames #2 IA 1986 Canisteo Typic Haplaquolls
6.0 Ida Grove IA 1986 Marshall Typic Hapludols
1.7 Holestein IA 1986 Galva Typic Hapludolls
21.5 Narrabri #1 NSW Uncropped Fall Incorporate 120 Urea Fine-textured grey clay Typic PellustertsChen et al. 1994
31.8 Narrabri #2 NSW
84.7 Buffalo ND 1997 Wheat Fall Inject 84 AA Gardena loam Pachic HapludollsGoos and Johnson 1999
38.7 Fargo ND 1997 Fargo silty clay Typic Epiaquerts
2.0 Benerembah NSW Rice Incorporate 80 Urea Grey clay Typic PelloxerertsKeerthisinghe et al.
1993
35.4 Columbia, MO 91 Wheat Fall Inject 56, 112 AA Mexico silt loam Udollic OchraqualfKidwaro and Kephart
1998
19.5 Columbia, MO 92
8.7 Bellville IL 1977 Wheat Fall Incorporate 152 Urea Weir silt loam Typic OrchaqualfsLiu et al. 1984
18.2 UAN
115.7 Bellville IL 1979 100, 151 Urea
78.9 UAN
17.3 Carbondale IL 1980 112 Urea Stoy silt loam Aquic Hapludalfs
46.3 Rossville KS 1979 #III Corn Spring Inject 84, 168,
260
AA Eudora fine sandy loam Fleuventic Haplu-
quolls
Maddux et al. 1985
111.5 West Lafayette IN 1979 Fallow Spring Inject 157 SM Chalmers silty clay loam Typic HaplaquollsMcCormick et al. 1983
3.5 Edinburgh UK Grassland Spring Surface 120 AS, Urea Winton clay loam McTaggart et al. 1997
38.5 Nicollet A MN Corn Fall, spring Inject 116, 234 DM Nicollet clay loam Aquic HapludollsRandall et al. 1999
41.2 Port Bryan B MN 108, 215 Port Bryan silt loam Typic Hapludolls
11.1 Nicollet C MN Nicollet clay loam Aquic Halludolls
13.8 Webster D MN 121, 241 Webster clay loam Typic Endoaquolls
3.5 Nicollet E MN 175, 350 SM Nicollet clay loam Aquic Hapludolls
15.5 Nicollet F MN 331, 662
7.2 Marna G MN 262, 524 Marna silty clay loam Typic Hapludolls
135.3 El Reno OK 1991 Wheat Fall Surface,
incorp.
60 Urea Renfrow silt loam Udertic PaleustollsRao 1996
32.3 El Reno OK 1992
36.9 El Reno OK 1993
6.5 El Reno OK 1994
7.1 Northwest IL 1986 #1 Corn Spring Inject 302 BM Derinda silt loam Oxyaquic HaplualfsSawyer et al. 1990
65.6 Northwest IL 1986 #2
20.1 Crawfordsville IN 1982 Corn Fall Inject 235 AA SM Odell silt loam Aquic AgridollsSutton et al. 1986
35
Table 2. Continued.
Nitrogen fertilization practice
Relative
effect %
a
Identity Crop Time Method Rate
kg ha
–1
Form
b
Soil subgroupReference
10.4 Crawfordsville IN 1983 228
22.3 Crawfordsville IN 1983 183
0.2 Crawfordsville IN 1982 Spring 295
16.7 Crawfordsville IN 1983 133
39.8 Crawfordsville IN 1983 239
55.3 Urbana IL 1975 Corn Fall Inject 67, 134 AA Drummer silty clay loam Typic HaplaquollsTouchton et al. 1978a
93.0 Urbana IL 1976 Spring
14.0 Urbana IL 1975 Spring
7.1 Brownstown IL 1976 Spring
73.4 Fall
11.2 Bonanza Farm MN
1980
Corn Spring Incorporate 90, 180 Urea Estherville sandy loam Typic HapludollsWalters and Malzer
1990b
104.6 Bonanza Farm MN
1981
52.4 Altus OK 1976 Grain sor-
ghum
Spring Incorporate,
inject
45, 90, 180 AA Holister clay loam Pachic PaleustollsWesterman et al. 1981
7.1 Tipton OK 1977 67, 134,
202
Urea, UAN Tipton fine sandy loam Pachic Agriustolls
2.7 Altus OK 1978 UAN Holister clay loam Pachic Paleustolls
a
关共effect with nitrapyrin effect without nitrapyrin100/effect without nitrapyrin;
b
AA, anhydrous ammonia; AS, ammonium sulfate; BM, beef manure; DM, dairy manure, SM, swine
manure; UAN, uryl ammonium nitrate.
36
Table 3. Relative quantity of N leached from the crop root zone as affected by nitrapyrin applied with sources of fertilizer or manurial N.
Nitrogen fertilization practice
Relative effect
%
a
Identity Crop Time Method Rate
kg ha
–1
Form
b
Soil subgroupReference
20.6 Germany 1977-81 Various Spring NR Various Urea Sand-Rosterden Katzur and Zietz 1984
29.9 Fall
17.6 Fall,
Spring
22.6 Germany 1982-87 Various Spring NR Various Urea Sand-Rosterden Katzur et al. 1984
15.8 Fall
12.1 Fall,
Spring
15.5 Coshocton OH 1977-78 Corn Spring Incorpo-
rate
300 Urea Rayne silt loam Typic HapludultsOwens 1987
8.4 Coshocton OH 1978-79
16.5 Coshocton OH 1979-80
42.1 Coshocton OH 1980-81
35.3 Coshocton OH 1981-82
24.5 Coshocton OH 1982-83
25.4 Coshocton OH 1983-84 Wheat, rye
40.4 Hurley UK Perennial
ryegrass
Winter Inject 221 DM Frilsam loam Thompson et al. 1987
42.6 Huley UK Spring 234
10.7 Lab column #1 None N/A Surface 200 AA Estherville sandy loam Typic Haplu-
dolls
Timmons 1984
31.7 Lab column #2 Urea
23.7 Westport MN 1977 Corn Spring Incorpo-
rate
Urea
2.5 Westport MN 1978
11.8 Wesport MN 1979
1.6 Bonanza Farm MN 1980 Corn Spring Incorpo-
rate
80 & 160 Urea Estherville sandy loam Typic Haplu-
dolls
Walters and Malzer
1990b
1.0 Bonanza Farm MN 1981
24.5 Olmsted Co. MN Corn Various NR Various Vari-
ous
NR Yadav 1997
25.4 Goodhue Co. MN
a
关共effect with nitrapyrin effect without nitrapyrin100/effect without nitrapyrin;
b
AA, anhydrous ammonia; DM, dairy manure.
37
Table 4. Relative amount of greenhouse gas forced from agricultural soils as affected by nitrapyrin applied with sources of fertilizer or manurial N.
Nitrogen fertilization practice
Relative
effect %
a
Identity Crop Time Method Rate
kg ha
–1
Form
b
Soil subgroupReference
51.9 Ames IA 1979 Fallow Fall Injection 180 AA Webster clay loam Typic HaplaquollsBremner et al. 1981
59.9 Ames IA 1980 Spring
65.1 Ft Collins CO 1989 #1 Corn Early sum-
mer
Incorporated 195 Urea Nunn clay loam Aridic ArgiustollsBronson et al. 1992
65.6 Ft Collins CO 1989 #2
40.6 Ft Collins CO 1990
27.4 Benerembah NSW Dry-seeded
flooded rice
Incorporated 0 & 71 Urea Grey clay Typic PelloxerertsKeerthisinghe et al. 1993
69.8
56.9 Hurley UK Perennial
ryegrass
Winter Inject 221 DM Frilsam loam Thompson et al. 1987
20.9 Spring 234
58.8 Darling Downs QLD
1982 #1
Fallow Spring Injection 80 AA Mywybilla clay Typic PellustertsMagalhaes et al. 1984
66.0 Darling Downs QLD
1982 #2
60 Anchorfield clay Typic Chromus-
tersts
51.8 Darling Downs QLD
1982 #3
Norilee clay Typic Chromusterts
38.1 Edinburgh UK Grassland Spring Surface 120 AS, Urea Winton clay loam McTaggart et al. 1997
44.2 GA 1979 Sweet corn Spring Surface 40 AS CN Cecil clay loam Typic KanhapludultsMcElhannon and Mills
1981
a
关共effect with nitrapyrin effect without nitrapyrin100/effect without nitrapyrin;
b
AA, anhydrous ammonia; AS, ammonium sulfate; CN, calcium nitrate; DM, dairy manure;
c
N
2
O.
d
CH
4
.
38
the response elements considered reflects the varied
source data representing a wide range of environ-
ments and management scenarios where a nitrifica-
tion inhibitor may be used. Conditions of use
including fertilizer timing, source, and placement as
well as environmental properties such as soil cover,
temperature, and moisture content affect the physico-
chemical and biological performance of the nitrifica-
tion inhibitor Wolt 1999as well as the overall
nitrogen cycle.
In approximately 25% of the instances considered,
use of a nitrification inhibitor did not positively affect
agronomic or environmental performance. These in-
stances may represent situations where environmen-
tal conditions were not conducive to N losses from
the agroecosystem Blackmer and Sanchez 1988,or
they may represent situations where nitrification in-
hibitor use in conjuction with fertilization practice re-
sults in N loss through ammonia volatilization
Thompson et al. 1987. Examples of the latter would
be fertilization strategies involving N forms urea or
ammonium fertilizers, placements surface applica-
tion, and timings fall applicationsas well as pro-
longed periods where soils are warm and moist,
allowing for ammonia volatilization Brink et al.
2000; Harrison and Webb 2001. As a consequence,
the positive aspects of nitrification inhibition in
reducing N leaching and reduced greenhouse gas
evolution must be balanced against the potential
negative effects of environmental acidification
through soil ammonia efflux.
This analysis has considered the agronomic and
environmental effectiveness of nitrapyrin, a widely
studied product with a long history of use for nitro-
gen inhibition in the intense corn production regions
of the Midwestern USA. Nitrapyrin is representative
of a broad class of compounds that act as nitrification
inhibitors and that appear to affect the initial rate lim-
iting step of nitrification involving NH
4
oxidation:
2NH4
3O2
Nitrosomonas
2NO2
4H2H2O.
Alternative forms of nitrification inhibitors for ex-
ample, dicyandiamide, ammonium thiosulfate, and
etridiazolcan be expected to have similar relative
responses as has been considered here for nitrapyrin.
The performance of any of these, as compared to ni-
trapyrin, will vary dependent on considerations of
physico-chemical properties, efficacy, and persistence
in various environments and management regimes.
For instance, comparative differences in field per-
formance of different nitrification inhibitors have
been attributed to physical volatilityand biological
efficacy and persistenceproperties as affected by
factors such as surface cover, timing of application,
and method of placement Malzer 1989; McTaggart
et al. 1997; Goos and Johnston 1999.
Figure 5. Comparative distribution of nitrapyrin effect, expressed as relative percent of the change attributable to nitrapyrin, for four indices
of N mobility. Box plots represent the 10, 25, 50, 75, and 90
th
percentile effect with mean dotted lineand outliers upper and lower 10
percentile of distribution.
39
Conclusions
A comprehensive assessment of nitrapyrin effect on
indices of N loss from agricultural ecosystems shows
that despite the anticipated variability in response
there is a positive impact on N use efficiency and
consequently N loss when viewed from the perspec-
tive of impact within a region over time. These find-
ings are of special consequence to the potential for
nitrification inhibitors to be effectively employed for
mitigating the adverse consequences of N loss from
soils receiving inputs of N fertilizer or manure. Field
research to date has focused primarily on the impact
of nitrification inhibition at the agronomic scale over
rather short timeframes, whereas the potential benefits
of nitrification inhibitor use in relation to N loss to
ground and surface water or to the atmosphere need
to be considered at the scale of a sensitive region,
such as a watershed, over a prolonged period of use.
The results reported here suggest that nitrification in-
hibition when considered within this context can
positively contribute to reduced NO
3
and greenhouse
gas losses from agricultural lands. These benefits
must be considered within the context of overall goals
for abatement of N losses through agricultural best
management practices.
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... Another method to synchronize crop N uptake with inorganic N availability in the soil can include using a controlled-release enhanced efficiency fertilizer technology. Nitrapyrin is a nitrification inhibitor (NI) that can be applied with ammonium (NH 4 + )-containing fertilizers that limits the conversion of NH 4 + to NO 3 − , which is susceptible to leaching and denitrification losses [19,20]. Numerous studies in Midwest corn-soybean cropping systems reported variable results from nitrapyrin application on water quality with an increase or no effect on flow-weighted NO 3 -N concentration in subsurface drainage water flow [21,22]. ...
... Numerous studies in Midwest corn-soybean cropping systems reported variable results from nitrapyrin application on water quality with an increase or no effect on flow-weighted NO 3 -N concentration in subsurface drainage water flow [21,22]. Several comprehensive meta-analyses and studies have observed that nitrapyrin reduces gas emission losses in corn and other cereal grain systems compared to N fertilizer without nitrapyrin [20,[23][24][25]. While the use of nitrapyrin in the fall is a BMP, no knowledge is available compared to other practices such as spring AA or an enhanced efficiency urea fertilizer application on gaseous losses [26,27]. ...
Article
Full-text available
Sustainable nitrogen (N) fertilizer management practices in the Midwest U.S. strive to optimize crop production while minimizing N gas emission losses and nitrate-N (NO3-N) losses in subsurface drainage water. A replicated site in upstate Missouri from 2018 to 2020 investigated the influence of different N fertilizer management practices on nutrient concentrations in drainage water, nitrous oxide (N2O) emissions, and ammonia (NH3) volatilization losses in a corn (Zea mays, 2018, 2020)–soybean (Glyince max, 2019) rotation. Four N treatments applied to corn included fall anhydrous ammonia with nitrapyrin (fall AA + NI), spring anhydrous ammonia (spring AA), top dressed SuperU and ESN as a 25:75% granular blend (TD urea), and non-treated control (NTC). All treatments were applied to subsurface-drained (SD) and non-drained (ND) replicated plots, except TD urea, which was only applied with SD. Across the years, NO3-N concentration in subsurface drainage water was similar for fall AA + NI and spring AA treatments. The NO3-N concentration in subsurface drainage water was statistically (p < 0.0001) lower with TD urea (9.1 mg L⁻¹) and NTC (8.9 mg L⁻¹) compared to fall AA + NI (14.6 mg L⁻¹) and spring AA (13.8 mg L⁻¹) in corn growing years. During corn years (2018 and 2020), cumulative N2O emissions were significantly (p < 0.05) higher with spring AA compared to other fertilizer treatments with SD and ND. Reduced corn growth and plant N uptake in 2018 caused greater N2O loss with TD urea and spring AA compared to the NTC and fall AA + NI in 2019. Cumulative NH3 volatilization was ranked as TD urea > spring AA > fall AA + NI. Due to seasonal variability in soil moisture and temperature, gas losses were higher in 2018 compared to 2020. There were no environmental benefits to applying AA in the spring compared to AA + NI in the fall on claypan soils. Fall AA with a nitrification inhibitor is a viable alternative to spring AA, which maintains flexible N application timings for farmers.
... The effectiveness of BNIs may be impacted by a range of soil and environmental factors [13,49,[80][81][82] including soil type, chemical properties, pH levels, organic matter content, and microbial activity, among others [80][81][82][83][84][85]. Understanding and considering these factors is crucial for determining applicability, considering how BNIs can fluctuate depending on soil type, with instances where they might prove ineffective in alkaline soils. ...
... The effectiveness of BNIs may be impacted by a range of soil and environmental factors [13,49,[80][81][82] including soil type, chemical properties, pH levels, organic matter content, and microbial activity, among others [80][81][82][83][84][85]. Understanding and considering these factors is crucial for determining applicability, considering how BNIs can fluctuate depending on soil type, with instances where they might prove ineffective in alkaline soils. ...
Article
Full-text available
To meet the growing population’s demand for food, humans have introduced large amounts of nitrogen fertilizers into agricultural systems, resulting in highly nitrified environments in most farmland soils. In highly nitrified environments, the application of nitrogen fertilizer easily leads to the formation of nitrate (NO3⁻) and subsequent leaching, resulting in very low utilization rates. Moreover, nitrogen loss can cause harm to both the environment and human health, making it necessary to inhibit the nitrification process. Nitrification inhibitors can suppress nitrification, and inhibitors derived biologically from plant roots are gaining attention due to their low cost and environmental friendliness. Sorghum, as a crop capable of growing in arid environments, holds economic value and also possesses the ability to secrete biological nitrification inhibitors. This article utilizes sorghum as a case study to review different types of BNIs (MHPP, sorgoleone, and sakuranetin), their mechanisms of inhibition, and influencing factors. This article summarizes the contributions of these inhibitors in reducing N2O emissions and increasing food production, while also providing insight into future research directions for sorghum’s biological nitrification inhibitors in terms of agricultural production efficiency. BNIs are expected to play an important role in improving agricultural production and reducing environmental pollution.
... This could be attributed to variable N availability with nitrapyrin or relative loss of available N during winter or early spring. In addition, nitrapyrin performance is influenced by soil factors (organic matter, pH, and texture) and environmental conditions (soil cover, temperature, and moisture) (Wolt, 2004). This shows that inconsistent weather conditions and drainage water management systems can influence AE among different fertilizer sources and are associated with application timing and dynamic fluctuations of plant N uptake relative to soil available N (Congreves et al., 2021). ...
Article
Full-text available
Nitrogen (N) and subsurface drainage water management are crucial and challenging components of sustainable crop production on poorly drained claypan soils. During extreme precipitation events, N fertilizer management is difficult in a corn (Zea mays L.)–soybean (Glycine max L.) rotation that balances productivity and environmental quality. This 4‐year (2018–2021) experiment was conducted on a poorly drained soil to examine the interactive effects of drainage (subsurface tile drainage [SD] and no drainage [ND]) and corn N fertilizer treatments (non‐treated control [NTC], fall‐applied anhydrous ammonia [AA] at 190 kg N ha⁻¹ with nitrapyrin [fall AA + NI], pre‐plant AA [spring AA] at 190 kg N ha⁻¹, and top‐dressed urea [TD urea] as 42 kg N ha⁻¹ SuperU and 126 kg N ha⁻¹ ESN as a 25:75% granular blend) on yield and nutrient uptake. Corn grain yield was 1.22–1.53 Mg ha⁻¹ greater with fertilizer treatments in SD compared to ND. Drought conditions in 2018 lowered corn grain yield compared to 2020. Average over 2 years, corn yield in SD soils was ranked as spring AA > fall AA + NI > TD urea > NTC. While soybean yield following corn was 13% greater in the NTC compared to TD urea. The SD treatment increased soybean yield by 0.6–2 Mg ha⁻¹ compared to ND. This study results showed that fall AA + NI produced corn yields similar to spring AA in SD and ND soils in temperate humid climatic conditions.
... The oxidation of ammonium (NH 4 + ) to nitrite (NO 2 − ) can be delayed by applying NIs, which act to inhibit ammonia-oxidizing bacteria (AOB) activity (Ruser and Schulz 2015;Hayden et al. 2021). Dicyandiamide (DCD), 3,4-Dimethylpyrazole phosphate (DMPP), and 2-chloro-6-(trichloromethyl) pyridine (Nitrapyrin) are the most widely investigated and commercially utilized NIs (Zerulla et al. 2001;Wolt 2004;Yang et al. 2016). Guo et al. (2022) indicated that DCD and DMPP can reduce N 2 O emissions by up to 85% and 99%, respectively, under a range of temperature and moisture levels. ...
Article
Full-text available
Extensive research has been performed into the effectiveness of nitrification inhibitors (NIs) in preventing N losses; however, tropical agriculture has been underrepresented in recent meta-analyses. Here, we apply a meta-analytic approach using data from 50 articles to identify the impact of NIs (DMPP, DCD, and DCD + NBPT) on crop yield, N2O emissions , soil NH4+ and NO3− concentrations, and NH3 volatilization in subtropical and tropical regions of Brazil. In addition, the survey includes information about location; climate zone; cultivated crops; soil pH; soil organic carbon; soil texture; experimental method; soil management; irrigation; fertilizer source, rate, and type; and NI type and rate. Overall, the data set showed that NIs increased crop yield and soil NH4+ concentrations by 3 and 60%, respectively, whereas N2O emissions and soil NO3− concentrations were reduced by 62 and 31%, respectively. Ammonia volatilization was not changed by NI application. However, the combination of a NI with a urease inhibitor decreased such losses by 39%. The effectiveness of the NIs was highest in irrigated fields, fine-textured soils, and mineral N sources. Moreover, NI performance in Brazil was found to be similar in tropical and subtropical climates, and was also comparable to values previously reported in meta-analyses , including those conducted in temperate climates. Therefore, NI application is indicated to be an efficient strategy to delay nitrification and mitigate N2O emissions in tropical agroecosystems.
... In some regional trials, adding CP significantly increased yield and NUE (Sun et al., 2015). However, a meta-analysis showed that the addition of CP changed the crop yield by -20∼207% (Wolt, 2004). It can be seen that the effectiveness of CP is variable. ...
Article
Full-text available
The application of nitrogen (N) fertilizer combined with nitrification inhibitor is considered to be one of the effective strategies to improve N efficiency and reduce N loss. While the chemical and physical properties of nitrapyrin (CP) in fertilizers have been evaluated to increase N efficiency, a lack of comprehensive evaluation of the effects of adding CP on summer maize yield, environmental benefits and economic income under different fertilization methods. In this study, two fertilization methods were used: split-N application and one-time basal N fertilizer before sowing. The comprehensive effects of N fertilizer with CP on N loss (NH3 volatilization, NO3– leaching, and N2O emissions), N efficiency, yield and profit under two N application methods were explored. Results showed that under the two N application methods, N fertilizer with CP treatment increased the N efficiency and yield (+3.4%∼+5.7%), significantly reduced the soil NO3–-N content and N2O emissions, while increased NH3 volatilization. Especially, the increase amplitude of NH3 was much less than the decrease amplitude of N2O induced by adding CP. Although split-N application could achieve higher yield and N efficiency, N2O emissions and NH3 volatilization also increased. However, the T1 + N (one-time basal N fertilizer before sowing mixed with CP) achieved the same yield level as T2 treatment (split-N application). Taking agronomic, economic and environmental benefits into consideration, one-time basal N fertilizer before sowing mixed with CP could ensure the target yield, increase economic benefits, maintain soil N content, and reduce N losses. Therefore, optimizing N management is essential to the sustainable development of agriculture.
Article
Full-text available
The use of nitrification inhibitors (NIs) with nitrogen fertilizers represents an effective strategy to reduce nitrogen loss. In addition, nitrification inhibitors are widely applied to improve agricultural yield. However, it is necessary to continue investigating the crop-specific agricultural practice. In this study, a nitrapyrin-based nitrification inhibitor was used to assess its effects on Brassica oleracea L. var. botrytis growth and on the environment. In a pot experiment, cauliflower plants were grown in fertilized soils based on calcium nitrate (SF) and SF + nitrapyrin. At the end of the experiment, the content of nitrogen compounds in soil and percolation water and the cauliflower yield were determined, and the plant tissues were characterized by Fourier-transform infrared spectroscopy. The application of the NI significantly reduced nitrogen losses, increasing nutrient availability in the soil and the element’s absorption in the plant. Co-application of fertilizers and NIs reduced NO3− leaching from 925 to 294 mg/L. Plant tissue characterization by FTIR spectroscopy highlighted variations in the functional groups in response to the application of NIs. These results suggest that applying nitrogen fertilizer in combination with nitrapyrin can mitigate nitrate pollution and improve element absorption and plant growth. Our research has shown that application methods and cropping systems need to be studied to maximize the effectiveness of nitrapyrin-based NIs.
Article
The microbial conversion of ammonia to nitrite in soils involves three enzymatic steps. Nitrification inhibitors (NIs) are designed to inhibit ammonia monooxygenase (AMO), the enzyme performing the initial oxidation of ammonia to hydroxylamine, to mitigate excessive nitrogen fertilizer losses in agricultural systems. Because the efficiency of the current commercial NIs is highly unreliable, novel, better performing compounds need to be developed. Previously, time-consuming soil incubation studies were required as the first step to test new potential NIs. We present here a simple and cost-efficient colorimetric assay that has been developed for the rapid assessment of the efficiency of new synthetic NIs to identify the most promising compounds for subsequent soil studies. This protocol enables screening of the inhibitor activity of multiple compounds at the same time with high reproducibility and can be manipulated to determine pH and temperature-dependent effects on NIs.
Article
Nitrification inhibitors (NIs) affect nitrogen (N) cycle and crop yield, but how the combinations of NIs influence N transformation and maize yield remains unclear. An outdoor pot experiment was performed to explore the effect of three NIs (nitrapyrin (CP), 3, 4-dimethylpyrazole phosphate (DMPP) and dicyandiamide (DCD)) and their combinations on mineral N transformation, yield and N use efficiency (NUE) of maize in a brown soil and a cinnamon soil from northeast China. Higher yield and NUE were obtained in the brown soil than that in the cinnamon soil. All treatments with NIs significantly increased NH4+-N content, grain yield and NUE in both soils, especially for NIs combination (DMPP + DCD in the brown soil and CP + DCD in the cinnamon soil). These two treatments significantly increased yield and apparent nitrogen recovery by 1.84 and 2.31 times, 10.24 and 6.39 times, respectively, compared with N fertilizer treatment. They also showed lower apparent nitrification rates (17.2% and 53.7%, respectively) compared with single NIs treatments. Considering both the inorganic N supply and agronomic effect of NIs, DMPP + DCD and CP + DCD are the best strategies for the application of NIs in the brown soil and cinnamon soil.
Chapter
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Agricultural systems contribute a large proportion of the global emissions of methane (CH4) and nitrous oxide (N2O) to the atmosphere. Nitrogen (N) fertilizer influences the flux rates of these gases in agroecosystems. Methane and nitrous oxide fluxes were measured periodically in an irrigated corn (Zea mays L.) field from time of fertilization to harvest. Fertilizer treatments included 0 and 218 kg urea-N ha-1, as well as applications of the nitrification inhibitors (NIs), nitrapyrin [2-chloro-6-(trichloromethyl)-pyridine], and encapsulated calcium carbide (ECC). Brief periods of CH4 emissions were observed after irrigations, with no effect of N or NIs. Methane consumption was not affected by urea fertilization, but was reduced 43% by the addition of ECC. The contribution, however, of changes in the consumption of CH4 as a result of ECC addition to the net greenhouse effect was negligible (<0.1%) compared to the reduction in N2O emissions. Nitrous oxide emissions were 16 times greater in urea-fertilized plots than in unfertilized soils. The application of NIs with urea decreased N2O emissions 43–71%.
Article
Full-text available
A commercial formulation of 2-chloro-6-(trichloromethyl)-pyridine (nitrapyrin) was incorporated within the N-fertilizer band in 2 consecutive years under widely different environmental conditions to evaluate the effect of nitrapyrin on denitrification occurring with field-grown sweet corn ( Zea mays L.). Nitrapyrin significantly increased soil NO ⁻ 3 –N levels, total plant N, and yield; decreased rates of N 2 O evolved from the soil with both NH ⁺ 4 and NO ⁻ 3 forms of N-fertilizer. Denitrification appears to be a significant factor influencing the growth of sweet corn under field conditions, and nitrapyrin effectively inhibits the denitrification process.
Article
Maximum manure N use efficiency by corn (Zea mays L.) requires that N mineralization and subsequent plant availability coincide with N uptake demand. Information regarding the effects of time of manure application and use of a nitrification inhibitor on manure mineralization and corn yield is needed for producers to make sound manure management decisions. Studies were conducted at seven southern Minnesota sites over 3 yr to determine the effects of three manure application times (mid-September, mid-October, and late April), two manure rates, and a nitrification inhibitor, (nitrapyrin [NP] 1.0 lb a.i./acre), on corn yield and soil nitrate N concentration (0 to 12 in.) at the V4 growth stage, Application rates ranged from 3000 to 4000 gal/acre for the low rate and from 6000 to 8000 gal/acre for the high rate. For the four sites receiving liquid dairy (Bos taurus) manure, soil nitrate N was greatest when manure was applied in April and lowest when applied the previous September. The addition of NP increased soil nitrate N at three sites but affected grain yields at only one site when averaged across time and rate of manure application. Grain yields for the April, October, and September applications averaged 146, 142, and 139 bu/acre, respectively, across manure rates and NP treatments, with April exceeding the September application time (P < 0.10). When liquid swine (Sus scrofa domesticus) manure was used, the effects of application time and NP on soil nitrate N concentration and grain yield depended on climatic conditions. At one site where 8.5 in. of rain fell in a 5-wk period in the spring, NP significantly increased both soil nitrate N concentration and grain yield for the October application but had no effect with the April application. Similar effects of NP on soil nitrate N were found at the other sites, but grain yields were not increased. Results from the seven site-yr support about a 5% yield increase with April application compared with fall applications. However, it is unlikely that many farmers will consider this an economic advantage because of logistical challenges often faced with spring applications of manure in the Northern Corn Belt.
Article
A three year study was conducted to determine the fertilizer value of liquid swine and dairy manure stored in above-ground steel structures. The magnitude of nitrogen losses from dairy manure stored in above-ground systems was determined. Randomized complete block design agronomic experiments were conducted on experimental corn plots at two swine and two dairy farms in east central Indiana. A nitrification inhibitor, nitrapyrin, was added to another group of manure plots. Corn yields fluctuated due to stressful weather conditions during the study, although in general, yields increased as manure application rates increased for both swine and dairy manure. Adding the nitrification inhibitor to spring injected dairy manure increased yields but not when applied with swine manure. Soil nutrients showed evidence of P build-up in plots where high manure rates were applied. Additional study results are discussed in the paper.
Article
Nitrapyrin [2-chloro-6-(trichloromethyl) pyridine] is a nitrification inhibitor frequently used to prevent losses of N fertilizer during corn (Zea Mays L.) production. Although many studies have shown that nitrapyrin inhibits nitrification in soils, it has not been established that use of nitrapyrin is cost effective for corn producers in the western portion of the Corn Belt. Field experiments were conducted at 18 site-years from 1985 through 1987 to determine the effects of nitrapyrin on corn yields and recovery of spring-applied fertilizer. Ammonium sulfate was broadcast at four rates (0, 50, 100, and 150 lb N/acre), with and without nitrapyrin, and replicated three times. ¹⁵N-labeled (NH4)2 SO4 was substituted for unlabeled (NH4)2 SO4 on subplots within yield plots at eight of the site-years. Statistically significant (P < 0.05) grain yield responses to fertilizer N were observed at 17 of the 18 site-years. Nitrapyrin significantly increased yields only at two of the 72 rate-site-years. Nitrapyrin did not influence recovery of labeled N in grain at 22 of the 24 rate-site-years having labeled fertilizer. It decreased recovery at the two other rate-site-years. Nitrapyrin had no significant effect on recovery of labeled N in the soils 8 wk and 14 mo after application. The results suggest that use of nitrapyrin was not cost effective at any of the sites studied. Please view the pdf by using the Full Text (PDF) link under 'View' to the left. Copyright © 1990. . Copyright © 1990 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America, 5585 Guilford Rd., Madison, WI 53711 USA
Article
Nitrogen management for conventional tillage (CT) corn (Zea mays L.) production is highly dependent on local soil and climatic conditions. Nitrogen fertilizer source, time of application, and use of nitrification inhibitors (NI) are components of an N management program which easily can be varied by the producer. An 8-yr study was undertaken in Ohio to assess N fertilizer management for CT corn production on a Crosby silt loam soil (fine, mixed, mesic Aerie Ochraqualf). Nitrogen fertilizer treatments compared in the study were fall and spring-preplant broadcast and incorporated urea, and fall and spring-preplant anhydrous ammonia (AA), with and without the NI, nitrapyrin [2-chloro-6-(trichloromethyl) pyridine]. Each N treatment was applied at rates of 80 and 160 lb/acre. Spring urea also was applied at 240 and 320 lb N/acre. Both grain yield and percent N in the ear leaf at tasseling were increased with increases in N rate for all N source × application time × NI treatments. For increasing rates of N, anhydrous ammonia produced higher yields and gave greater increases in percent ear-leaf N than did urea. Spring-preplant application of both N sources gave higher yields than fall application. Nitrapyrin with spring-applied AA gave no yield or percent ear-leaf N increases. However, NI with fall-applied AA did increase grain yield over fall-applied AA without NI. While significant year-to-year and treatment year variability was present in the study, the 8-yr average results can be used in formulating N management recommendations for CT corn production in similar soils in the North Central USA. Please view the pdf by using the Full Text (PDF) link under 'View' to the left. Copyright © 1990. . Copyright © 1990 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America, 5585 Guilford Rd., Madison, WI 53711 USA