current status of bni research at jircas
DESCRIPTION
A Collaborative effort with CIAT, ICRISAT and CIMMYT GV Subbarao, JIRCAS, JapanTRANSCRIPT
Current Status of BNI Research at JIRCAS
GV SubbaraoJIRCAS, Japan
A Collaborative effort with CIAT, ICRISAT and CIMMYT
Collaborators
CIATCIMMYTICRISAT
Tottori UniversityScottish Crops Research Institute
Colleagues contributed from JIRCAS1. T. Ando 2. K. Nakahara3. T. Yoshihashi4. T. Watanabe5. T. Ishikawa6. Y. Yamanaka7. H. Y. Wang (PDF)8. S. Gopalakrishnan (PDF)9. Stuart Pearse (PDF)10. A.K.M. Hussain (PDF)11. Yiyong Zhu (PDF)12. Zhu Yiyong (PDF)13. T. Tsehaye (PDF)
Nearly 70% of the N fertilizer applied is lost to the environment
Amounts to a direct annual economic loss of
US$ 90 billion* [*based on - a) world annual N fertilizer production is 150 million Mg; b) 0.45 US$ kg -1 urea]
Nitrogen fertilizer consumed in 1930s - < 1.0 Tg (million metric tons)
Nitrogen fertilizer consumed in 1960s – 10 Tg Nitrogen fertilizer consumption worldwide in 2010 – 150 Tg (million metric tons)
Energy cost of nitrogen fertilizer – 1.8 to 2 L diesel oil per kg N fertilizerTo produce 150 million metric tons of Nitrogen fertilizer requires
1.70 billion barrels of diesel oil (energy equivalent)
Nitrogen fertilizers – Some facts
Year
1950 1960 1970 1980 1990 2000 2010 2020
Nit
roge
n ef
fici
ency
in c
erea
l pro
duct
ion
(meg
a to
nnes
cer
eal g
rain
/meg
aton
ns f
erti
lize
r ap
plie
d)
20
30
40
50
60
70
80
Trends in N-fertilization efficiency in cereal production (annual global cereal production divided by annual global application of N-fertilizer) (Source: FAO 2012)
Global food production has tripled during this period, but N-fertilizer applications have increased 10-fold (Tilman et al.,
2001)
Why NUE is <30% in most agricultural systems?
Nitrification and denitrification processes associated with uncontrolled rapid nitrification are largely responsible for the
massive N leakage (>70% of the N fertilizers) and for the low-NUE
Nitrogen Cycle in Typical Agricultural Systems
Soil
OM
Organic N
NH4+
Microbial
N NO3-
>95% of the total soil inorganic N pool
Plant N uptake & Assimilation
Mineralization
Nitrification
Inorganic
N
Crop Residues
NFertilizer
Soil incubation period in days
0 10 20 30 40
Nitr
ific
atio
n (%
)
0
20
40
60
80
100
120
Intensively managed Alfisols
WatershedsConservatively managed Alfisols
Alfisol fields at ICRISAT
WS HP
Nitr
ific
atio
n ra
te ( g
NO
3- g-1
soi
l d-1
)
0
1
2
3
4
5
Alfisol fields at ICRISAT
WS HP
Nit
rifi
cati
on r
ate
(g
NO
3- g-1
soi
l d-1
)
0
1
2
3
4
5
Conservatively managedWatershed Alfisols
Intensively managedHigh-precision Alfisols
Agricultural intensification led to acceleration of nitrification in
intensively-managed production systems
How to achieve low-nitrifying agricultural soils?
Switch to low-nitrifying agricultural systems
Ammonium(NH4
+)Nitrite(NO2
-)
Leaching
Nitrate(NO3
-)
N2O, NO, N2
Greenhouse gasesGlobal warming
Nitrification
OMmineralization Denitrification
Ammonia-oxidizing Bacteria Nitrite-oxidizing Bacteria
Biological Nitrification Inhibition (BNI)
Brachiaria spp. root-produced
nitrificationinhibitors
Microbial Immobilization
of NH4+
Low-Nitrifying Natural Ecosystems High-Nitrifying Modern Agricultural Systems
BL
BL
BL
BL
BL
BL
BL
BL
BL
BL
BL
NFe
rtili
zer
BNI Function and its potential impacts to N-cycling
How to detect and quantify nitrification inhibitors ?
pHLUX209763 bp
(Bg/ II/BamHl)
kat
TrrnPhao
luxAB
PstI
(BamHI/Bg/ II) PstIPstI
BamHI
Physical map of pHLUX20(source: Iizumi et al. 1998)
OM
IM
NH2OH + H2O NO2- + 5H+ + 4e-
NH3 + O2
HAO
c554 c554
UQ
UQH2
NAD(P)H + H+ NAD(P)+
FMNH2FMN
H2O
hv RCOOH
RCHO
O2
Luciferase
NAD(P)+
reductaseCytaa3oxidase
NAD(P)H-FMN
AMO
oxidoreductase
Hypothetical model of interaction between the electron transfer pathways and the luciferasereaction in N. europaea (source Iizumi et al. 1998)
BNI activity is expressd in ‘ATU’
Inhibitory effect from 0.28 mM AT is defined as one
ATU
Pasture grasses
0 1 2 3 4 5 6 7
BN
I-ac
tivi
ty r
elea
sed
from
roo
ts
(AT
U g
-1 r
oot d
ry w
t. d-1
)
0
2
4
6
8
10
12
14
16
18
1. B. humidicola2. M. minutiflora3. P. maximum4. L. perenne5. A. gayanus6. B. brizantha
BNI capacity of pastures JIRCAS-CIAT partnership
Plants release two categories of BNIs
Hydrophobic Hydrophilic
BNI Activity
Mostly confined toRhizosphere
May move out of Rhizosphere
Plant -rootproduced
nitrificationinhibitors
BL
BL
BL
BL
BL
BL
BL
BL
BL
BL
BL
BL
BL
BLBL
BL
BL
BL
BL
Plant Species
BH Sorghum Wheat
BN
I ac
tiviit
y (%
of t
otal
BN
I ac
tivity
)
0
20
40
60
80
100
Hydrophobic-BNIHydrophilic-BNI
Relative importance of hydrophobic- and hydrophilic- BNI activity in three plant
species at 8 d old plants
40 d old plants
8 d old plants
BNI activity added to the soil (AT g-1 soil)
0 5 10 15 20 25
NO
3 co
nce
ntr
atio
n in
soi
l (p
pm
)
0
50
100
150
200
250
Threshold
Releases about 200 to 400 ATU hydrophilic BNI d-1
BNIs provide stable inhibitory effect on
soil nitrification
55 d soil incubation
14
A bioassay-guided purification of BNI activity led to isolation of
Brachialactone, identified as the major nitrification inhibitor
released from the roots of B. humidicola.
A tricyclic terpenoid with a unique 5-8-5 ring system and a g-lactone ring
Similar 5-8-5 ring system
Fusicoccins are produced in some fungi
(Geranylgeranyl diphosphate)
Patented by J IRCAS
GGDP is a precursor in the biosynthesis of terpenoids; also this is the precursor for the synthesis of carotenoids, gibberllins and chlorophylls in plants
11
Subbarao G V et al. PNAS 2009;106:17302-17307©2009 by National Academy of Sciences
0.0 2.5 5.0 7.5 10.0 12.5 15.0 min
0
5000
10000
15000
20000
25000
30000
35000
40000
45000
uV
sample: brachialactone standard (mixture of a and b), 75 μgcolumn: TSK gel super ODS (4.6 x 100 mm)mobile phase: water (A) – acetonitrile (B) flow rate: 1.0 ml/mingradient program: 23% - 43%B (10 min), 43% - 48%B (8 min)
Time (min)
Det
ecto
r res
pons
e
Brachialactone b
Purified Brachialactone HPLC chromatogram
GC-MS-SIM based brachialactone quantification
1617. 0 18. 0 19. 0 20. 0 21. 0 22. 0 23. 0 24. 0 25. 0
0. 1
0. 2
0. 3
0. 4
0. 5
0. 6
0. 7
0. 8
0. 9
1. 0
1. 1
1. 2
1. 3
1. 4(x100, 000)
314.00 (1.11)334.00 (100.00)
Progesterone (IS:1 ppm)
Brachialactone (48 ppm)
19.78minIdentification: m/z 334Quantification: m/z 137
18.65minIdentification: m/z 314Quantification: m/z 314
Quantification & identification was achieved.Brachialactone showed 2 peaks,
which might be caused by keto-enol tautomerism.
‘Keto’ form ‘Enol’ form
GC-MS-SIM based analytical methodology can have major implications to genetic improvement efforts directed at brachialactone-trait into root systems of Brachiaria sp.
Brachialactone is detected in root tissues and quantification using GC-MS-SIM analysis could be a possibility in future
Preliminary results suggest brachialactone concentration in root tissues can be as high as 0.27 0.01% (dry weight basis)
Brachialactone levels in root tissues could be up to 10 times higher than in root exudates (i.e. about 10% of brachialactone in the root tissues may be released per day from exudation)
GC-MS-SIM analysis improves the detection thresholds for brachialatone levels in the samples and may give better quantification in root tissues and root exudates.
Brachialactone release is highly influenced by growing season
Spring season in Japan appears to have a major influence on brachialactone release in B. humidicola
020
0040
0060
0080
0010
000
1200
0
11.0
1.04
(No.
31)
11.0
1.18
(No.
32)
11.0
2.01
(No.
33)
11.0
2.14
(No.
34)
11.0
3.03
(No.
35)
11.0
3.23
(No.
36)
11.0
3.26
(No.
36…
11.0
4.01
(A-1
)11
.04.
05 …
11.0
4.11
(A-3
)11
.04.
14(A
-5)
11.0
4.18
(A-6
)11
.04.
21(A
-7)
11.0
4.25
(A-8
)11
.05.
10(M
ay-1
)11
.05.
17(M
ay-2
)11
.05.
25(M
ay-3
)11
.06.
07(N
o.37
)11
.06.
21(N
o.38
)11
.07.
06(N
o.39
)11
.07.
25(N
o.40
)11
.08.
08(N
o.41
)11
.08.
23(N
o.42
)11
.09.
08(N
o.43
)11
.09.
26(N
o.44
)11
.10.
11(N
o.45
)11
.10.
24(N
o.46
)11
.11.
07(N
o.47
)11
.11.
25(N
o.48
)11
.12.
05(N
o.49
)11
.12.
19(N
o.50
)12
.01.
04(N
o.51
)12
.01.
16(N
o.52
)12
.01.
30(N
o.53
)12
.02.
16(N
o.54
)12
.02.
27(N
o.55
)12
.03.
05(M
arc…
12.0
3.14
(Mar
c…12
.03.
21(M
arc…
12.0
3.26
(Mar
c…12
.04.
02(A
pril-
1)12
.04.
09(A
pril-
2)12
.04.
13(A
pril-
3)12
.04.
18(A
pril-
4)12
.04.
23(A
pril-
5)12
.05.
8(M
ay-1
)12
.05.
18(M
ay-2
)12
.05.
29(M
ay-3
)12
.06.
05(j
une-
1)12
.06.
05(j
une-
2)12
.06.
18(j
une-
3)12
.06.
25(j
une-
4)12
.07.
06(j
uly-
1)12
.07.
24(j
uly-
2)12
.08.
06(a
ug-1
)12
.08.
20(a
ug-2
)12
.09.
03(s
ep-1
)12
.09.
18(s
ep-2
)12
.10.
11(o
ct-1
)12
.10.
16(o
ct-2
)12
.11.
06(n
ov-1
)12
.11.
19(n
ov-2
)12
.12.
03(d
ec-1
)12
.12.
18(d
ec-2
)13
.01.
07(ja
n-1)
13.0
1.22
(jan
-2)
13.0
2.04
(feb
-1)
13.0
2.18
(feb
-2)
13.0
3.05
(mar
-1)
13.0
3.18
(mar
-2)
13.0
3.25
(mar
-3)
13.0
4.01
(apr
-1)
13.0
4.08
(apr
-2)
13.0
4.22
(apr
-3)
13.0
5.08
(may
-1)
13.0
5.20
(may
-2)
13.0
6.03
(jun-
1)13
.06.
17(ju
n-2)
13.0
7.01
(july
-1)
13.0
7.16
(july
-2)
13.0
7.22
(july
-3)
13.0
8.20
(aug
-1)
13.0
9.03
(sep
-1)
13.0
9.17
(sep
-2)
peak
are
am
AU*s
ec.
date
Ann
ual fl
uctu
atio
n ro
ot e
xdat
e stan
dard
BH
high
BN
I BH
2011 20132012
We need to understand whether these seasonal influence on brachialactone release from root due to production in root tissues or only release from roots is influenced?
Brachialactone’s mode of inhibitory action on Nitrosomonas
CompoundConcentration in the in vitro assay, mM AMO pathway HAO pathway
Crude-root exudate (methanol extract) 63.4 + 0.8 63.8 + 0.8Brachialactone 5.0 59.7 + 0.9 37.7 + 0.9Nitrapyrin 3.0 82.3 + 1.5 8.1 + 1.2
Inhibition (%)
Outer Membrane
Inner Membrane
Periplasm
Nitrosomonas
Regulating factors for the Release of BNIs from roots
BNI synthesis and release from roots requires presence of NH4
+
N treatment (NO3-N vs NH4-N grown plants)
NO3-grown NH4-grown
BN
I ac
tivity
of
the
root
tiss
ue (
AT
uni
ts g
-1 r
oot d
ry w
t)
0
50
100
150
200
Root tissue from RE-water treatmentRoot tissue from RE-NH4 treatment
Nitrogen treatment (i.e. NH4-N vs. NO3) of the plants
NO3-grown NH4-grownTot
al B
NI
activ
ity r
elea
sed
duri
ng 1
0 d
peri
od (
AT
uni
ts)
0
200
400
600
800
1000
RE-collected using distilled waterRE-collected using 1 NH4Cl (1 mM)
Functional link between NH4+-uptake and BNI
release
A hypothesis
NH4+
Cytoplasm pH >7
NH4+ NH4
+
H+
H+ATP
ADP + Pi
BNIn-
BNIn-
BNI
Glutamine + H+
glutamate
Is there potential for genetic improvement of BNI capacity in
pastures?
Genetic variability is the primary requirement for genetic improvement in trait/s of interest using
traditional breeding
Is there a genetic variability for BNI capacity?
High-BNI and low-BNI genetic stocks in B. humidicola
B. humidicolaAccession
BNI releasedATU g-1 root dry wt. d-
1
CIAT 26159 46.3
CIAT 26427 31.6
CIAT 26430 24.1
CIAT 679 17.5
CIAT 26438 6.5
CIAT 26149 7.1
CIAT 682 7.5
Panicum maximum 0.1
LSD (0.05) 6.0
Based on evaluation of 40 germplasm accessions in B.humidicola
CIAT’s Collaboration
Note11 sexuals from a total of 40 germplasm accessions were evaluated for BNI capacity; Most sexuals evaluated have BNI capacity similar to the CIAT 679.
A bi-parental population using high-BNI (CIAT 16888) and low-BNI (CIAT 26146) has been developed to identify genetic regions associated with BNI-function using a mapping population derived from crosse between apomictic and sexual germplasm accession of BH that differ in BNI-capacity – CIAT-JIRCAS ongoing collaboration
Date of Root exudate collection during Spring 2012
2nd March 3rd March 4th March 1st April
Bra
chia
lact
one
rele
ase
per
plan
t (p
eak
area
)
0
2000
4000
6000
8000
10000
12000
CIAT 679CIAT 26159
CIAT 26159CIAT 679
Genetic differences in Brachialactone release
capacity High-BNI genotype releases several times higher
brachialactone than standard cultivar
25
Parental lines of RIL population
PVK 801 296-B
BN
I ac
tivity
/Sor
gole
one
rele
ase
per
plan
t
0
10
20
30
40
50
BNI activity (ATU)Sorgoleone (g)
Total BNI activity and sorgoleone levels in root-DCM wash after 8 d growth in root boxes with hydroponic system
(based on 6 times evaluation of 20 seed lings each over a 6 month period)
Parental lines of RIL population characterizationJIRCAS-ICRISAT
partnership
HPLC chromatogram of purified sorgoleone
BNI activity detected only in this peak
NO BNI activity detected in any of these peaks
O
O
OH
O
Chemical structure of sorgoleone, Molecular Weight - 358a P-benzoquinone exuded from sorghum roots
BNI activity released from sorghum roots
Hydrophobic BNIs
Hydrophilic BNIs
Isolation of the major BNI constituent of hydrophobic BNI activity
ED80 = 1.0 ppm
A droplet of sorgoleoneexuding from root tip
296B PVK 801
Sorgoleone-phenotyping system is now developedJIRCAS-ICRISAT
partnership
Bi-Parental Sorghum RIL population (PVK 801 x 296B)
0 50 100 150 200
Sor
gole
one
prod
uced
( g
pla
nt-1
)
0
10
20
30
40
50
PVK801
296B
RIL phenotyping for sorgoleone levels in root-DCM washJIRCAS-ICRISAT partnership
Introducing high-BNI capacity into wheat Is it possible or feasible?
JIRCAS-CIMMYT partnership
Plant species
0 1 2 3 4
BN
I ac
tivi
ty r
elea
sed
from
roo
ts
(AT
U g
-1 r
oot d
ry w
t. d-1
)
0
5
10
15
20
25
30
35
NH4-N grown
NO3-N grown
Nobeoka Chinese Spring
L. racemosus
Releases about 150 to 200 AT units of BNI da-1 under optimum conditions
Wild-wheat has high-BNI capacityJIRCAS-CIMMYT
partnership
Leymus racemosus2N=4X =28;
genome Ns NsXmXm
Triticum aestivum L. cv. Chinese Spring
2N=6X =42; genome AABBDD
F1 hybrid Triticum aestivum L. cv. Chinese Spring
2N=6X =42; genome AABBDD
BC1F1 hybrid
BC7F1 hybrid
Production of wheat-Leymus racemosus-addition lines
Two Lr#n L. racemosus chromosomes in wheat detected by florescence in situ hybridization with probe of L. racemosus genomic DNA (green color)
3.9LSD (0.05)
4.97Lr-1-2DtA7Lr-1-2
6.47Lr-1-1DtA7Lr-1-1
6.65Lr-1DA5Lr-1
3.22Lr-1DA2Lr-1
3.7Lr-HDALr-H
4.1Lr-FDALr-F
5.5Lr-kDALr-k
6.4Lr-1DALr-1
13.0Lr-IDALr-I
13.5Lr-jDALr-j
24.6Lr-nDALr-n
BNI released (ATU g-1 root dry wt d-1)
L. racemosuschromosome introduced
Genetic Stock
3.9LSD (0.05)
4.97Lr-1-2DtA7Lr-1-2
6.47Lr-1-1DtA7Lr-1-1
6.65Lr-1DA5Lr-1
3.22Lr-1DA2Lr-1
3.7Lr-HDALr-H
4.1Lr-FDALr-F
5.5Lr-kDALr-k
6.4Lr-1DALr-1
13.0Lr-IDALr-I
13.5Lr-jDALr-j
24.6Lr-nDALr-n
BNI released (ATU g-1 root dry wt d-1)
L. racemosuschromosome introduced
Genetic Stock
BNI released from Chromosome-addition lines derived fromL. racemosus and cultivated wheat (Chinese Spring)
Can the high-BNI capacity of wild-wheat be Transferred/Expressed in cultivated
wheat?Would this be the first step to develop low-nitrifying and low-
N2O emitting wheat production systems?
BA
JIRCAS-CIMMYT partnership
Lr#nS.3BL
Lr#nS.7BL
Leymus chromosome ‘N’
Transferred to
wheat 7B
ChromosomeBy
Kishii Masahiro
Transferred to wheat 3B
ChromosomeByKishii Masahiro
The short-arm of the Leymus ‘N’ chromosome is translocated to either 7B or 3B wheat chromosome (short-arm) for BNI evaluations
Short arm
long arm
centromere
Courtesy - Kishi
Courtesy - Kishi
JIRCAS-CIMMYT partnership
Lr#n addition
Lr#nS.3BL
Wheat-Leymus genetic stocks
CS N - add N - sub-3A N - Tr-3B N - Tr-7B
BN
I ac
tivity
rel
ease
d fr
om r
oots
(AT
U g
-1 r
oot d
ry w
t. d-1
)
0
100
200
300
400
500
RE-NH4+
BNI activity release from roots in the presence of
NH4+ in the collection solutions
Courtesy - Kishi
Courtesy - Kishi
BNI activity release is two-fold higher in Lr#N addition and Lr#N translocation line (on 3B wheat chromosome)
compared to Chinese Spring
The above results strongly confirm that BNI-capacity in Leymus is controlled by Lr#N and expressed in wheat background; further the BNI-trait is controlled by short-arm of Lr#n chromosome and its expression depends on the translocation position on wheat
JIRCAS-CIMMYT partnership
Can the BNI function be effective to control nitrification and nitrous
oxide emissions under field conditions?
JIRCAS-CIAT partnership
Roots of B. humidicola release a powerful nitrification inhibitor
Brachialactone
Ammonium(NH4
+)Nitrite(NO2
-)
Nitrate(NO3
-)Ammonia-oxidizing Bacteria Nitrite-oxidizing BacteriaBL
BL
BL BL
Microbial-N
Imm
obili
zatio
n
Min
eral
izat
ion
By blocking the Nitrosomonas function, B. humidicola facilitates NH4
+ to move into mocrobial pool and to remain in the soil system and act as a slow-releasing nitrogen source for Brachiaria growth
Estimations for the BNIs release from B. humidicola
• Active root biomass in a long-term BH pasture being 1.5 Mg ha-1
• (Root mass up to 9.0 Mg ha-1 has been reported in BH pastures)• BNI release rates can be 17 to 50 ATU g-1 root dry wt. d-1
• Estimated BNI activity release d-1 could be 2.6 x 106 to 7.5 x 106 ATU
(CIAT 679) (CIAT 26159)
•1 ATU being equal to 0.6 mg of nitrapyrin
• This amounts to an inhibitory potential equivalent to the application of 6.2 to 18 kg of nitrapyrin application ha-1 yr-1
38
Soil ammonium oxidation rates (mg of NO2− N per kg of soil per day) in field plots planted with tropical pasture grasses (differing in BNI capacity) and soybean (lacking BNI capacity in roots) [over 3 years from establishment of pastures
(September 2004 to November 2007); for soybean, two planting seasons every year and after six seasons of cultivation]
Brachiaria pastures suppressed soil ammonium oxidation
Subbarao G V et al. PNAS 2009;106:17302-17307©2009 by National Academy of Sciences
JIRCAS-CIAT partnership
CIAT-Palmira field study 2004-2007
0
0.5
1
1.5
2
2.5
3
3.5
4
Control - Bare soil BH- 16888
ppm
of
nitr
ate
prod
uced
day
-1
CIAT-Palmira field study 2013
39
Cumulative N2O emissions (mg of N2O N per m2 per year) from field plots of tropical pasture grasses (monitored monthly over a 3-year period, from September 2004 to November 2007)
Subbarao G V et al. PNAS 2009;106:17302-17307©2009 by National Academy of Sciences
Brachiaria pastures suppressed N2O emissions from the fieldCan BNI function in plants be exploited to develop low-N2O emitting systems then?
JIRCAS-CIAT partnership
BNI capacity of the species (ATU g-1 root dry wt. d-1)
0 10 20 30 40 50 60
Cum
ulat
ive
N2O
em
issi
on
(mg
N2O
-N m
2 y-1
)
0
100
200
300
400
500
Con
Soy
PMBHM
BH-679
BH-16888
High BNI capacity leads to low-N2O emitting systems?
A 3-year field study with soybean and pasture grasses with varying BNI capacities
Can we develop low-nitrifying and low-N2O emitting pasture-production systems through genetic exploitation of BNI trait?
The new MAFF-BNI project (starts from 2014) will test this hypothesis further using genetic stocks of B. humidicola with diverse BNI capacity in root systems
JIRCAS-CIAT partnership
Photo: J. W. MilesExploitation of BNI function in BH for the sustainable agro-pastoral systems?
Characterization of residual effect of BNI from B. humidicola pasture on maize productivity and
Nitrogen use efficiency
OngoingJIRCAS-CIAT partnership
How long the BNI-suppressive effect on nitrification persists?Ongoing
JIRCAS-CIAT partnership
Land Management
0 1 2
Nit
rifi
cati
on r
ate
(mg
NO
2-N
kg-
1 so
il d
-1)
0.00
0.02
0.04
0.06
0.08
0.10
0.12
Native savannaBH
Cultivated fields Maize
BH-BNI effect
Time in years
0 1 2 3 4 5 6A
mm
oniu
m o
xida
tion
rat
e in
soi
l
(mg
NO
2 kg-1
soi
l d-1
)
0.0
0.1
0.2
0.3
0.4
0.5
0.6
0.7Cultivated soils
control
BH-residualscenario-4
BH-residualscenario-3
BH-residualscenario-2
BH-residualscenario-1
Characterization of residual BNI impact on NUE in maize systems An agro-pastoral systems perspective
OngoingJIRCAS-CIAT partnership
Maize crop established in a high-BNI field by clearing B. humidicola
Field site – Taluma, Iianos, Colombia
JIRCAS – CIAT collaborative study – CIAT field site at Llanos
OngoingJIRCAS-CIAT partnership
120 kg N/ha 240 kg N/ha
B. humidicola field The BH-BNI benefits on Maize growth
Beneficial effects of BNI on subsequent maize crop
Land Management
0 1 2
Nit
rifi
cati
on r
ate
(mg
NO
2-N
kg-
1 so
il d
-1)
0.00
0.02
0.04
0.06
0.08
0.10
0.12
Native savannaBH
Cultivated fields Maize
BNI-Field
OngoingJIRCAS-CIAT partnership
120 kg N ha-1
Beneficial effects of BNI on subsequent maize cropA healthy maize crop in BNI-field with 120 kg N
application
Land Management
0 1 2
Nit
rifi
cati
on r
ate
(mg
NO
2-N
kg-
1 so
il d
-1)
0.00
0.02
0.04
0.06
0.08
0.10
0.12
Native savannaBH
Cultivated fields Maize
JIRCAS – CIAT collaborative study – CIAT field site at Llanos
BNI-Field
OngoingJIRCAS-CIAT partnership
120 kg N ha-1
Land Management
0 1 2
Nit
rifi
cati
on r
ate
(mg
NO
2-N
kg-
1 so
il d
-1)
0.00
0.02
0.04
0.06
0.08
0.10
0.12
Native savannaBH
Cultivated fields Maize
JIRCAS – CIAT collaborative study – CIAT field site at Llanos
Non-BNI-Field
Beneficial effects of BNI on subsequent maize crop
A nitrogen-deficient maize crop in non-BNI-field with 120 kg N application
OngoingJIRCAS-CIAT partnership
BNI-Field Non-BNI-Field
2012 Field study at Iianos, Colombia
Nitrogen fertilizer application (Kg ha-1)
40 60 80 100 120 140 160 180 200 220 240 260
Mai
ze g
rain
yie
ld (
t ha
-1)
0
1000
2000
3000
4000
5000
High nitrifying - cultivated fieldsLow nitrifying - BH-BNI
Beneficial effects of BNI on subsequent maize grain yields
BNI is more effective on maize yields at low to moderate N applications but not high-N environments
BNI function is effective in improving NUE only under low- to moderate-N environments and not at high-N environments
BNI-field
Non-BNI-field
OngoingJIRCAS-CIAT partnership
Maize plant tissues from various land-use systems
Ear Shoot Root
15N
/14N
rat
io in
pla
nt ti
ssue
s
4.5
5.0
5.5
6.0
6.5
BH-BNIcont.MaizeNative savannah
Beneficial effects of BNI on N recovery by Maize
BNI is effective in improving N recovery by maize in the field (from 15N studies)
BNI-Field
Non-BNI-Field
OngoingJIRCAS-CIAT partnership
Land use treatments on Maize
BH-BNI cont.Maize Native savannah
15N
/14N
rat
io in
soi
ls (
0-60
cm
s de
pth)
0.35
0.40
0.45
0.50
0.55
Beneficial effects of BNI on soil-N retention BNI is effective in improving soil-N retention after maize harvest (from 15N
studies)
BNI-Field
Non-BNI-Field
OngoingJIRCAS-CIAT partnership
CONCLUDING REMARKS
175 Tg NN-Fertilizer inputs
into Agriculture
53.5 Tg NPlant protein from
Agriculture
3.5 Tg NAnimal protein from Livestock
0.27Tg NHuman system
N-retention
123.5 Tg N LOST (70%)
From Agriculture
48.0 Tg N LOST(90%)
From Livestock
5.0 Tg N LOST(95%)
From Municipal Sewage systems
N-Fertilizer inputs into Agriculture
Plant protein-N
Animal protein-N
Human-N
Nitrogen flow in Human-centric Ecosystems
Annual
Nitrogen pollution epidemic in China
Nitrification facilitates movement of N from agricultural soils to water-bodies (ground water, freshwater lakes, rivers and to oceans) and cause algal
blooms Second Green Revolution?
NH4+
NO3-
Plant uptake
Soil-microbial
uptake
Nitrification
SOMMineralization
N-Fertilizers
Microbial-NImmobilization
Plant litter and
Root exudates
Nitrification opens several pathways in N-cycle for fertilizer-N to escape into the larger
Environment
A fundamental shift towards NH4
+-dominated crop nutrition is
possible?Retention of soil-N in
agricultural soils is critical for the sustainability of
production systems and to prevent N from entering into
water-bodies
Nature 2013, 501:291
BNI function in plants should be exploited to facilitate retention of soil-N within agricultural systems
We must develop new technologies to keep N to remain and recycle within the agricultural systems and not allow into water systems – Nitrification control is keyBNI function can be one such mechanism that can be exploited from a breeding perspective and from a system’s perspective
Take Home Message
Strategic Research Partner – CIAT(Drs. IM Rao; Manabu Ishitani; John Miles; Joe Tohme; Jacobo Arango, Marco Rondon; Maria Pilar Hurtado; Danillo Moreta; Gonzalo Borrero)
Other participating research institutesICRISAT (India)
CIMMYT (Mexico)Tottori University (Japan)
Yokohama City University (Japan)Scottish Crops Research Institute (UK)
Biogeochimieet ecologie des milieuxcontinentaux(France)
CIATTropical pastures-BNI
MAFFGTZ
Forage-CRP(?)
J IRCASBNI Research
CIMMYTWheat-BNI
MAFFWheat-CRP
ICRISATSorghum-BNI
MAFF (?)Dryland cereals-CRP(?)
Thank you for the attention