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“Effect of Chemical Composition of Plant
Residues on Nitrogen Mineralization in
Soil”
Presented By:
Vikram Singh
M.Sc. (Agri.) Soil Science student
Reg. No: 2010115095
Presented By:
Vikram Singh
M.Sc. (Agri.) Soil Science student
Reg. No: 2010115095
Major Guide :
Dr. J. N. Nariya
Professor
Dept. of Agril. Chem. and Soil
Science
JAU , Amreli
Major Guide :
Dr. J. N. Nariya
Professor
Dept. of Agril. Chem. and Soil
Science
JAU , Amreli
Minor Guide:
Dr. P. K. Chovatia
Associate Professor
Department of Agronomy
JAU , Junagadh
Minor Guide:
Dr. P. K. Chovatia
Associate Professor
Department of Agronomy
JAU , Junagadh
3
Contents…
Introduction
Facts about nitrogen
Transformation of nitrogen in soil
Chemical composition of plant residues
Decomposition rates of crop residues
Research finding
Conclusion
Use of plant residues as organic nutrient source is
relatively simple for the farmers compared to the application of
manure. Incorporating plant residues into agricultural soils can
sustain organic carbon content, improve soil physical
properties, enhance biological activities and increase nutrient
availability.
In the short-term, incorporation of plant residues provides
the energy and nutrients for microbial growth and activity, acts
as a driving force for the mineralization-immobilization
processes in the soil and is a source of nitrogen (N) for plants
.In the long-term, incorporation of crop residues is important for
the maintenance of organic C and N stocks in the nutrient pool
of arable soils. The N availability from these residues depends
on the amount of N mineralized or immobilized during
decomposition. 4
Introduction
Residues: Whatever remains after something else has been taken,
separated, removed, or designated; remnant; remainder.
Crop/Plant residues: Defined as the vegetative plant(crop/trees/shrubs)
material left on a ground after its harvesting, pruning or processing or
grazing. Ex: stalks, stems, leaves, roots, penicles and weeds.
5
Crop residues
Field residues Process residues
Types of crop residues
Stalks and Stubble
Leaves, and Seed pods.
Husks, Seeds, Bagasse and
Roots.
6
Nitrogen
 Nitrogen is most important primary nutrient which is
required in large quantity for plant growth.
 Most widely distributed element in atmosphere.
Preferred as nitrate (NO3
-
) and ammoniacal (NH4
+
)
Nitrogen by plants.
Nitrogen makes up 78 % of atmospheric air
N N
7
Very small amount of soil nitrogen is available to
plants. Total nitrogen in furrow slice(0-15 cm) soils generally varies
from 0.02 to 0.44 per cent by weight.
Role of Nitrogen
An essential constituent of proteins and is present in many compounds of great
physiological importance in plant metabolism
 Is an integral part of chlorophyll.
 Imparts vigorous vegetative growth and dark green colour to plants.
 Governs utilization of potassium, phosphorus and other elements.
Facts about nitrogen
8
Sources of Nitrogen :
• Fertilizers
• Organic manures
• Plant residues
• Bio-fertilizers
• Green manure
• Rain water
• Bacterial nitrogen fixation
9
Transformation of Nitrogen in soils
Various pathways of N transformation
 Mineralization
 Immobilization
 Fixation in soil
 Losses of N( Volatilization)
• Nitrogen in crop residue become available after
mineralization
• Available nitrogen includes NH4
+
and NO3
-
10
Mineralization
“Process by which nitrogen in organic
compounds is converted to inorganic ammonium and
nitrate ions carried out by micro-organisms.”
11
Mineralization process operates through three reactions
namely:
1.Aminisation
2.Ammonification , and
3.Nitrification
1. Aminisation:
Process of release of amines and amino acids from combined N
compounds (proteins).
Proteins R-NH2 + CO2 + Energy + Other products
(Amines)
Heterotrophic
Micro-organisms
12
Organic N
R-NH2
(Amine)
NH4
+
(Ammonium)
NO2
-
(Nitrite)
NO3
-
(Nitrate)
Aminization Ammonification Nitrification
Aminisation occurs both in aerobic and anaerobic condition
End products
(NH4)2 SO4 H2O, and CO2Under aerobic condition
Under anaerobic condition
NH3, NH2
-
, CO2
,
organic acids, H2S etc
13
2.Ammonification
Process of reduction of amines to ammonical
compounds.
R-NH2 + HOH
NH3 + R-OH + energy
H2O
NH4 + OH-
14
 Under anaerobic condition (due to more
hydrogen)Org.N NH4
+
-N
Lack of O2 in soil
 Under aerobic condition the process continues
NH4
+
-N NO3
-
-N
NO2
-
-N
Nitrification
3. Nitrification
15
Process of microbial oxidation of
ammonical nitrogen to nitrate form of
nitrogen.
16
Fig. 01: Sketch of three different process types regarding the effects
of returning plant residues on soil inorganic nitrogen over the
limited experimental period.
Chen et al. (2014) France
17
Fig. 2. Diagram illustrating some processes in the nitrogen cycle in
soils.
HawaiiJonathan (2006)
Plant residues /material may be classified under three major chemical
groups:
Polysaccharides: These are large group of carbon compounds, and
made up of simple monosaccharides units like glucose etc. cellulose
and hemicellulose are most important polysaccharides and they
accumulate in plants tissues. They form the skelton of plant tissues.
Lignins: These are complex carbon compounds. They are found in
woody tissue. It is binding material and covers the cell walls and fibro-
vascular bundles. Lignin is one of the most abundant organic polymers
in plants, just behind cellulose. It is the exclusive chemical composition
of gymnosperm and angiosperm. The content of lignin in wood and
Gramineae is 20–40% and 15–20 %, respectively.
Proteins :They are nitrogenous substances, it`s predominant in cell
protoplasm. Simple forms of protein is amino acids.
18
Chemical composition of plant residues:
19
Fig 3: Composition of Plant Materials
Source: Brady And Wail (2012)
Rapid
Very slow
Sugars ,Starch and simple protiens
Crude proteins
Hemicellulose
Cellulose
Fats, Waxes and Oils
Lignins and phenolic compounds
20
Decomposition Rates of Crop residues
Resource
quality category
Resource quality
parameters (g kg-1
)
Nitrogen supplying
capacity
High quality N >25
Lignin <150
Polyphenol <40
High and immediate
Intermediate-high
quality
N >25
Lignin >150
Polyphenol >40
Delayed, short or long term
Intermediate-low
quality
(Short-term)
N<25
lignin<150
polyphenol <40
Low–short term
immobilization
Low quality
(Long-term)
N <25
Lignin >150
Polyphenol >40
Very low and possible long
term immobilization
Mohanty et al. (2013)
21
NAAS, New Delhi
22
Source: Brady And Wail (2012)
Research findings
23
24
Carbon and nitrogen mineralization
potential of biofuel crop(Jatropha curcas L.)
residues in soil
CASE STUDY- 01
Soil location pH EC(ds/m) CaCO3
(%)
O.C C/N Total N
(g/kg)
Available
N (mg/kg)
Texture
Inside –canopy soil 7.41 0.14 0.92 0.67 9.57 0.72 47.6 Loam
Outside –canopy
soil
7.31 0.11 0.92 0.60 8.57 0.72 41.3 Loam
TABLE:2..Characteristics of soil used for incubation study
Chaudhary et al.(2014) 25
Bhavnagar ,Gujarat
26
Jatropha
residues
C (%) N (%) C/N Cellulose
(%)
Hemi
cellulos
e (%)
Lignin
(%)
Phenolics
(mg/g)
Cake 46 3.30 13.94 14.44 12.46 1.25 1.91
Leaf 43 1.22 35.25 8.96 17.71 5.48 3.32
Fruit shell 42 0.98 42.86 6.85 15.78 1.82 0.46
Chaudhary et al.
(2014)
Bhavnagar ,Gujarat
Chaudhary et al. (2014) 27Bhavnagar ,Gujarat
Chaudhary et al. 28Bhavnagar ,Gujarat
Rate at
day
C N Cellulose Hemicellulose Lignin Phenolic C/N
ratio
1 0.95 0.97 0.94 -0.91 -0.59 0.01 -0.94
9 0.95 0.97 0.94 -0.92 -0.61 -0.02 -0.94
21 0.96 0.99 0.95 -0.93 -0.61 -0.01 -0.96
33 0.97 0.99 0.96 -0.93 -0.61 0.01 -0.96
64 0.98 0.99 0.98 -0.88 -0.52 0.11 -0.98
94 0.99 0.99 0.98 -0.85 -0.48 0.17 -0.98
29
Chaudhary et al. (2014) Bhavnagar ,Gujarat
30
Case Study- 02
Effect of organic matter and soil fertility on nitrogen
mineralization and its uptake by cassava (Manihot
esculenta Crantz).
Andy , 2015 Java,Indonesia
Treatments 20 o
C 25 o
C 30 o
C
Soil that planted with cassava less than 10 years
Only Groundnut (G) 550.6 773.8 1015.6
Only Maize (M) 435.2 704.9 872.3
G : M (1:1) 533.8 943.0 1036.0
G : M (2:1) 589.6 1011.8 1086.2
G : M (1:2) 459.4 710.5 851.9
Control (Without
Organic Matter)
347.8 459.4 450.1
TABLE 05: Cumulative nitrogen mineralization (mg kg-1
) for 12
weeks at various temperatures and biomasses application.
Andy (2015) Java,Indonesia 31
32
Treatments 20 o
C 25 o
C 30 o
C
Soil that planted with cassava more than 30 years
Only Groundnut
(G)
496.6 738.4 747.7
Only Maize (M) 388.7 556.1 638.0
G : M (1:1) 444.5 634.3 638.0
G : M (2:1) 526.4 738.4 783.1
G : M (1:2) 375.7 647.3 758.9
Control (Without
Organic Matter)
264.1 437.1 394.3
TABLE:6..Cumulative nitrogen mineralization (mg kg-1
) for 12
weeks at various temperatures and biomasses application.
TABLE:6..Cumulative nitrogen mineralization (mg kg-1
) for 12
weeks at various temperatures and biomasses application.
Andy (2015) Java,Indonesia
33
Case Study-03
Effect of Chemical Composition of Plant Residues
on Nitrogen Mineralization
Srinivas et al.(2006) CRIDA, Hyderabad
Srinivas et al.(2006) CRIDA, Hyderabad 34
TABLE 07: Chemical composition of different tree residues.
Plant residues C(%) N% Ligni
n
%
Polyphen
ol
%
C/N Ligni
n/N
Polyphen
ol/N
Lignin+Polyph
enol/N
C.calothyrsus 41.5 2.46 7.21 7.04 a 16.9 2.93 2.86 5.79
C.siamea 42.1 2.07 7.64 3.88 20.3 3.69 1.88 5.57
D.sissoo 40.1 2.42 8.69 2.44 16.6 3.59 1.01 4.60
G.sepium 40.9 3.16 6.84 2.02 12.9 2.16 0.64 2.80
H.binata 40.1 1.91 10.21 3.74 21.0 5.35 1.96 7.31
L.leucocephala 39.5 3.59 6.87 3.10 11.0 1.92 0.87 2.78
P.juliflora 40.7 1.96 8.29 4.02 20.7 4.23 2.05 6.28
T. indica 41.3 1.62 10.15 4.83 b 25.6 6.29 2.99 9.28
35
Plant
residues
C % N % Lignin
%
Polyphenol
%
C/N Lignin/
N
Polyphenol/
N
Lignin+Polyphenl/
N
Caster 41.2 0.95 6.07 0.74 43.4 6.39 0.78 7.17
Horse gram 39.5 1.22 5.36 1.68 32.4 4.39 1.38 5.77
Paddy 40.4 0.48 5.19 0.61 84.2 10.81 1.27 12.08
Pearl millet 42.1 0.84 6.24 0.49 50.1 7.43 0.58 8.01
Sorghum 39.8 0.55 6.81 0.55 72.4 12.38 1.00 13.38
Sugarcane 43.0 0.51 7.54 0.37 84.3 14.78 0.73 15.51
Sunflower 40.2 1.06 8.10 0.82 37.9 7.64 0.77 8.42
TABLE 08: Chemical composition of different crop residues
Srinivas et al.(2006) CRIDA,Hyderabad
Fig:6..Plant residue quality and nitrogen mineralization
36
G.sepium
C. siamea
Paddy
Sugarcane
L.leucocephala C. cajan
Srinivas et al.(2006) CRIDA,Hyderabad
FIG:7.. Relationships between residue quality parameters and N mineralization
for All residues
37
Srinivas et al.(2006) CRIDA,Hyderabad
38
Case Study-04
Impact of the addition of different plant residues on
nitrogen mineralization–immobilization turnover and
carbon content of a soil incubated under laboratory
conditions
Abbasi et al. (2015) (PAKISTAN)
g kg-1
Plant residues
(Treatments)
Plant
organs
Total
N
Total
C
Lignin
(LG)
Polyphen
ols(PP)
C /N LG /
N
PP /
N
LG+PP
/N
Glycine max shoot 35.2 447 11 13.1 12.7 0.3 0.4 0.7
Glycine max Root 12.8 466 29 26.9 36.4 2.3 2.1 4.4
Zea mays Shoot 9.6 472 41 29.5 49.2 4.3 3.1 7.3
Zea mays Root 4.0 486 48 31.4 121.5 12.0 7.9 19.9
Trifolium repens Shoot 27.4 397 13 18.0 14.4 0.4 0.6 1.1
Trifolium repens Root 16.0 423 21 20.2 26.4 1.3 1.2 2.5
Populus euramericana Leaves 20.8 435 34
53.8
20.9 1.6 2.6 4.2
Robinia pseudoacacia Leaves 33.3 404 28 32.3 12.1 0.8 1.0 1.8
Elaeagnus umbellata leaves 34.7 418 32 38.7 12.1 0.9 1.1 2.0
LSD (p= 0.05) - 3.14 14.16 4.53 3.77
TABLE:9..Mean biochemical composition of the plant residues used
in the experiment
39
Abbasi et al. (2015) Pakistan
Days after plant-residue addition
Treatments 0 7 14 21 28 42 60 80 100 120 CD
(p=0.05)
mg Nkg-1
soil
Control 13.7 13.9 12.9 17.1 30.9 65.9 63.1 75.6 77.7 51.7 2.88
T1 14.8 39.2 49.2 76.8 96.7 158.1 165.2 174.1 188.7 160.9 7.90
T2 13.7 8.1 5.2 8.3 11.8 13.8 28.4 50.4 49.4 27.7 8.15
T3 13.7 7.4 6.2 6.9 10.5 23.1 21.2 36.1 46.7 21.0 5.34
T4 14.3 7.4 9.4 7.7 8.8 15.3 22.2 21.4 32.4 26.4 4.30
T5 14.1 19.0 21.6 55.5 62.5 86.8 127.6 150.8 145.8 93.3 7.31
T6 15.5 8.2 5.2 23.9 34.0 85.3 98.0 149.9 130.2 85.8 9.46
T7 13.0 5.7 4.1 8.6 22.6 55.5 73.1 106.8 87.3 66.9 8.39
T8 13.9 7.4 9.2 23.6 46.6 91.3 111.0 138.9 127.8 93.7 7.83
T9 12.9 9.4 14.5 25.3 51.1 80.1 92.7 140.0 116.4 93.5 6.88
CD (p
=0.05)
2.43 4.77 3.12 5.11 7.63 8.23 6.37 9.23 8.27 7.34
TABLE:10..Mean changes in the concentration of total mineral N of a soil
amended with different plant residues and incubated at 25 0
C under controlled
laboratory conditions during a 120-day period .
40
T1-Glycine max shoot,
T2-Glycine max root;
T3-Zea mays shoot,
T4-Zea mays root;
T5-Trifolium repens shoot;
T6 -Trifolium repens root
T7 -Populus euramericana leaves;
T8-Robinia pseudoacacia leaves;
T9-Elaeagnus umbellata leaves.
Abbasi et al. (2015) Pakistan
FIG:8..Net cumulative N mineralized from the added plant residues at different incubation
periods.
41
T1-Glycine max shoot
T2-Glycine max root
T3-Zea mays shoot
T4-Zea mays root
T5-Trifolium repens shoot
T6 -Trifolium repens root
T7 -Populus euramericana leaves
T8-Robinia pseudoacacia leaves
T9-Elaeagnus umbellata leaves
Days after residues amendments
Abbasi et al. (2015) Pakistan
42
Singh And Kumar (2006) HAU, Hisar
Case Study-05
Legumes
residues
OC (g/kg) Total N g/kg C:N ratio Lignin
(g/kg)
Polyphenols
(g/kg)
Black gram 428 23.3 18.4 75.0 22.4
Cluster bean 452 18.2 24.8 80.0 44.4
Cowpea 446 21.4 20.8 71.2 27.6
Green gram 416 26.0 16.0 54.1 30.9
Sesbania 440 22.6 19.5 73.9 26.7
Soyabean 462 21.4 21.6 61.2 35.7
Sunhemp 438 20.1 21.8 64.3 32.2
43Singh And Kumar (2006) HAU, Hisar
TABLE:11..Characteristics of legumes residues
FIG:9..Commulative Nitrogen MineralizationFIG:9..Commulative Nitrogen Mineralization
44
Singh And Kumar (2006) HAU, Hisar
TABLE:12..Cumulative net N mineralized and amounts of added
N mineralized from legume residues after 56 days of incubation
period
Legumes residues Net N mineralized (mg/kg) Amount of added N
mineralized (%)
Hisar Karnal Hisar Karnal
Black gram 84 87 72.1 74.7
Cluster bean 53 55 58.2 60.4
Cowpea 71 73 66.4 68.2
Green gram 96 99 73.8 76.1
Sesbania 74 76 65.5 67.3
Soyabean 75 77 70.1 72
sunhemp 65 67 64.7 66.7
45
Singh And Kumar (2006) HAU, Hisar
46
Oglesby And Fownes (2002) Hawaii
Case Study-06
TABLE:13..Characteristics of green manures used in the
experiment
Species Polyphenols (%) N (%) Lignin
(%)
Leaves Twigs Average
Calliandra calothyrsus 4.99 1.95 4.06 2.85 13.4
Cassia reticulata 2.10 0.89 1.99 2.65 9.9
Cassia siamea 4.60 1.27 3.92 2.31 10.3
Gliricidia sepiurn 2.07 0.35 1.84 3.43 8.6
lnga edulis 4.71 1.70 3.83 2.51 18.3
Leucaena leucocephala 3.52 1.49 2.93 3.74 11.1
Sesbania sesban 2.60 0.56 1.38 1.39 14.5
47
Oglesby And Fownes (2002) Hawaii
Week N (%) Polyphenols (%) Lignin (%) Polyphenol:N Lignin:N
1 0.24 -0.78 -0.13 -0.89 0.00
2.5 0.29 -0.80 -0.48 -0.94 -0.21
4 0.44 -0.71 -0.80 -0.88 -0.56
8 0.37 -0.79 -0.79 -0.90 -0.46
12 0.11 -0.59 -0.79 -0.53 -0.32
TABLE:14.Correlation coefficients of cumulative % N mineralized at
each time interval versus initial green manure properties.
48
Oglesby And Fownes (2002) Hawaii
49
FIG:10..N Mineralization pattern
Oglesby And Fownes (2002) Hawaii
50
FIG:11..Relationship between N mineralized at 8 weeks and Polyphenol
: N ratio (Y = 79.4 - 39.5X, n = 7, r 2 = 0.81).
Oglesby And Fownes (2002) Hawaii
51
Mafongoya et al. (2008) Florida
Case Study-07
Mineralization of nitrogen from decomposing leaves
of multipurpose trees as affected by their chemical
composition
TABLE:15..Chemical composition of leaves of MPT species (on
oven-dry matter basis).
Mafongoya et al. Florida 52
Treatment N
g/Kg
NDF-N
g/Kg
Lignin
g/Kg
SP phenol
g/Kg
Acacia angustissima 25b 19a 143b 122b
Gliricidia sepium 18c 9d 111c 23d
Flemingia macrophylla 18c 11c 193a 105b
Sesbania sesban 28ab 5c 67d 112b
Calliandra calothyrsus 27ab 12b 114c 154a
Cajanus cajan 31a 12b 140b 42d
Leucaena leucocephala 31a 11c 120c 122b
Acacia+sesbania 27b 12b 105c 117b
Cajanus+sesbania 30a 9d 104c 77c
Values followed by different letters in each column are significantly different from each other at P~0.05 using
Duncan’s Multiple Range Test.
NDF-N=neutral detergent fraction),
SP= Soluble polyphenols
53
FIG:12.. N mineralization pattern
Mafongoya et al. (2008) Florida
TABLE:16..Correlation coefficients relating the cumulative amount of net N mineralized
to initial chemical properties of multi purpose tree (MPT) leaves during incubation with
soil.
TABLE:16..Correlation coefficients relating the cumulative amount of net N mineralized
to initial chemical properties of multi purpose tree (MPT) leaves during incubation with
soil.
54
Times
(weeks)
NDF-N Lignin SPphenol Tannins L/N P/N L+P/N NDF-N/N
1 -0.64 -0.78 -0.39 -0.01 -0.68 -0.59 -0.78 -0.73
2 -0.70 -0.75 -0.53 -0.23 -0.51 -0.64 -0.68 -0.61
3 -0.61 -0.70 -0.44 -0.06 -0.59 -0.59 -0.72 -0.68
4 -0.66 -0.73 -0.54 0.10 -0.61 -0.71 -0.79 -0.71
5 -0.65 -0.75 -0.53 0.07 -0.64 -0.71 -0.81 -0.72
6 -0.62 -0.73 -0.55 0.07 -0.62 -0.72 -0.80 -0.68
7 -0.63 -0.68 -0.57 0.19 -0.54 -0.71 -0.74 -0.62
8 -0.68 -0.71 -0.56 0.33 -049 -0.67 -0.68 -0.59
Mafongoya et al. (2008) Florida
55
Nitrogen Mineralization from Soil Amended with Gliricidia andNitrogen Mineralization from Soil Amended with Gliricidia and
Sorghum Residues:Sorghum Residues:
Case Study-08
ICRISAT, HydrabadSridevi et al. (2006)
TABLE:17..Residue fractionation:
Residue Soluble fractions
(% )
Fiber
(%)
N g kg-1
C/N
Sorghum straw 21.4 78.6 5.32 77.3
Glyricidia prunings 53.3 46.7 28.60 13.4
56
ICRISAT, HydrabadSridevi et al. (2006)
Amendment N
added
(mg/
kg)
Incubation period in days N
mineralized
after 90
days
(% of
added)
0 5 15 30 45 60 75 90
Control - 7.8
4
14.4
6
24.
31
31.
44
35.2
8
37.6
3
39.
19
40.
42
-
Sorghum
straw
24.39 7.8
4
4.52 12.
41
19.
91
25.1
5
30.3
3
34.
17
39.
06
5.6
Gliricidia
prunings
24.39 7.8
4
12.5
8
32.
5
44.
86
51.2
9
56.7
5
60.
31
62.
04
88.6
57
ICRISAT, HydrabadSridevi et al. (2006)
Table:18..Nitrogen mineralization
58
 N concentration and C:N ratio are sound criteria for predicting
nitrogen release in few crop residues while in other residues
polyphenol/N ratio, ( lignin + polyphenol ) to N ratio play a role in
percent N mineralized.
 The composition of residues in terms of soluble and fiber fractions
determines whether and to what extent, N is immobilized or
mineralized.
 The decomposition and nutrient release rates of residues are often
regulated by environmental factors, such as temperature and soil
moisture, and biochemical composition of plant materials and their
interaction. The biochemical composition or quality parameters such as
total N concentration, lignin (LG), polyphenols (PP), carbon : nitrogen
(C/N) ratio, LG/ N, PP /N and (LG, C, PP) /N ratios are useful
indicators that control decomposition and N release of added plant
residues.
Conclusion of seminar
59

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Ppt seminar

  • 1.
  • 2. “Effect of Chemical Composition of Plant Residues on Nitrogen Mineralization in Soil” Presented By: Vikram Singh M.Sc. (Agri.) Soil Science student Reg. No: 2010115095 Presented By: Vikram Singh M.Sc. (Agri.) Soil Science student Reg. No: 2010115095 Major Guide : Dr. J. N. Nariya Professor Dept. of Agril. Chem. and Soil Science JAU , Amreli Major Guide : Dr. J. N. Nariya Professor Dept. of Agril. Chem. and Soil Science JAU , Amreli Minor Guide: Dr. P. K. Chovatia Associate Professor Department of Agronomy JAU , Junagadh Minor Guide: Dr. P. K. Chovatia Associate Professor Department of Agronomy JAU , Junagadh
  • 3. 3 Contents… Introduction Facts about nitrogen Transformation of nitrogen in soil Chemical composition of plant residues Decomposition rates of crop residues Research finding Conclusion
  • 4. Use of plant residues as organic nutrient source is relatively simple for the farmers compared to the application of manure. Incorporating plant residues into agricultural soils can sustain organic carbon content, improve soil physical properties, enhance biological activities and increase nutrient availability. In the short-term, incorporation of plant residues provides the energy and nutrients for microbial growth and activity, acts as a driving force for the mineralization-immobilization processes in the soil and is a source of nitrogen (N) for plants .In the long-term, incorporation of crop residues is important for the maintenance of organic C and N stocks in the nutrient pool of arable soils. The N availability from these residues depends on the amount of N mineralized or immobilized during decomposition. 4 Introduction
  • 5. Residues: Whatever remains after something else has been taken, separated, removed, or designated; remnant; remainder. Crop/Plant residues: Defined as the vegetative plant(crop/trees/shrubs) material left on a ground after its harvesting, pruning or processing or grazing. Ex: stalks, stems, leaves, roots, penicles and weeds. 5
  • 6. Crop residues Field residues Process residues Types of crop residues Stalks and Stubble Leaves, and Seed pods. Husks, Seeds, Bagasse and Roots. 6
  • 7. Nitrogen  Nitrogen is most important primary nutrient which is required in large quantity for plant growth.  Most widely distributed element in atmosphere. Preferred as nitrate (NO3 - ) and ammoniacal (NH4 + ) Nitrogen by plants. Nitrogen makes up 78 % of atmospheric air N N 7
  • 8. Very small amount of soil nitrogen is available to plants. Total nitrogen in furrow slice(0-15 cm) soils generally varies from 0.02 to 0.44 per cent by weight. Role of Nitrogen An essential constituent of proteins and is present in many compounds of great physiological importance in plant metabolism  Is an integral part of chlorophyll.  Imparts vigorous vegetative growth and dark green colour to plants.  Governs utilization of potassium, phosphorus and other elements. Facts about nitrogen 8
  • 9. Sources of Nitrogen : • Fertilizers • Organic manures • Plant residues • Bio-fertilizers • Green manure • Rain water • Bacterial nitrogen fixation 9
  • 10. Transformation of Nitrogen in soils Various pathways of N transformation  Mineralization  Immobilization  Fixation in soil  Losses of N( Volatilization) • Nitrogen in crop residue become available after mineralization • Available nitrogen includes NH4 + and NO3 - 10
  • 11. Mineralization “Process by which nitrogen in organic compounds is converted to inorganic ammonium and nitrate ions carried out by micro-organisms.” 11 Mineralization process operates through three reactions namely: 1.Aminisation 2.Ammonification , and 3.Nitrification
  • 12. 1. Aminisation: Process of release of amines and amino acids from combined N compounds (proteins). Proteins R-NH2 + CO2 + Energy + Other products (Amines) Heterotrophic Micro-organisms 12 Organic N R-NH2 (Amine) NH4 + (Ammonium) NO2 - (Nitrite) NO3 - (Nitrate) Aminization Ammonification Nitrification
  • 13. Aminisation occurs both in aerobic and anaerobic condition End products (NH4)2 SO4 H2O, and CO2Under aerobic condition Under anaerobic condition NH3, NH2 - , CO2 , organic acids, H2S etc 13
  • 14. 2.Ammonification Process of reduction of amines to ammonical compounds. R-NH2 + HOH NH3 + R-OH + energy H2O NH4 + OH- 14  Under anaerobic condition (due to more hydrogen)Org.N NH4 + -N Lack of O2 in soil
  • 15.  Under aerobic condition the process continues NH4 + -N NO3 - -N NO2 - -N Nitrification 3. Nitrification 15 Process of microbial oxidation of ammonical nitrogen to nitrate form of nitrogen.
  • 16. 16 Fig. 01: Sketch of three different process types regarding the effects of returning plant residues on soil inorganic nitrogen over the limited experimental period. Chen et al. (2014) France
  • 17. 17 Fig. 2. Diagram illustrating some processes in the nitrogen cycle in soils. HawaiiJonathan (2006)
  • 18. Plant residues /material may be classified under three major chemical groups: Polysaccharides: These are large group of carbon compounds, and made up of simple monosaccharides units like glucose etc. cellulose and hemicellulose are most important polysaccharides and they accumulate in plants tissues. They form the skelton of plant tissues. Lignins: These are complex carbon compounds. They are found in woody tissue. It is binding material and covers the cell walls and fibro- vascular bundles. Lignin is one of the most abundant organic polymers in plants, just behind cellulose. It is the exclusive chemical composition of gymnosperm and angiosperm. The content of lignin in wood and Gramineae is 20–40% and 15–20 %, respectively. Proteins :They are nitrogenous substances, it`s predominant in cell protoplasm. Simple forms of protein is amino acids. 18 Chemical composition of plant residues:
  • 19. 19 Fig 3: Composition of Plant Materials Source: Brady And Wail (2012)
  • 20. Rapid Very slow Sugars ,Starch and simple protiens Crude proteins Hemicellulose Cellulose Fats, Waxes and Oils Lignins and phenolic compounds 20 Decomposition Rates of Crop residues
  • 21. Resource quality category Resource quality parameters (g kg-1 ) Nitrogen supplying capacity High quality N >25 Lignin <150 Polyphenol <40 High and immediate Intermediate-high quality N >25 Lignin >150 Polyphenol >40 Delayed, short or long term Intermediate-low quality (Short-term) N<25 lignin<150 polyphenol <40 Low–short term immobilization Low quality (Long-term) N <25 Lignin >150 Polyphenol >40 Very low and possible long term immobilization Mohanty et al. (2013) 21 NAAS, New Delhi
  • 22. 22 Source: Brady And Wail (2012)
  • 24. 24 Carbon and nitrogen mineralization potential of biofuel crop(Jatropha curcas L.) residues in soil CASE STUDY- 01
  • 25. Soil location pH EC(ds/m) CaCO3 (%) O.C C/N Total N (g/kg) Available N (mg/kg) Texture Inside –canopy soil 7.41 0.14 0.92 0.67 9.57 0.72 47.6 Loam Outside –canopy soil 7.31 0.11 0.92 0.60 8.57 0.72 41.3 Loam TABLE:2..Characteristics of soil used for incubation study Chaudhary et al.(2014) 25 Bhavnagar ,Gujarat
  • 26. 26 Jatropha residues C (%) N (%) C/N Cellulose (%) Hemi cellulos e (%) Lignin (%) Phenolics (mg/g) Cake 46 3.30 13.94 14.44 12.46 1.25 1.91 Leaf 43 1.22 35.25 8.96 17.71 5.48 3.32 Fruit shell 42 0.98 42.86 6.85 15.78 1.82 0.46 Chaudhary et al. (2014) Bhavnagar ,Gujarat
  • 27. Chaudhary et al. (2014) 27Bhavnagar ,Gujarat
  • 28. Chaudhary et al. 28Bhavnagar ,Gujarat
  • 29. Rate at day C N Cellulose Hemicellulose Lignin Phenolic C/N ratio 1 0.95 0.97 0.94 -0.91 -0.59 0.01 -0.94 9 0.95 0.97 0.94 -0.92 -0.61 -0.02 -0.94 21 0.96 0.99 0.95 -0.93 -0.61 -0.01 -0.96 33 0.97 0.99 0.96 -0.93 -0.61 0.01 -0.96 64 0.98 0.99 0.98 -0.88 -0.52 0.11 -0.98 94 0.99 0.99 0.98 -0.85 -0.48 0.17 -0.98 29 Chaudhary et al. (2014) Bhavnagar ,Gujarat
  • 30. 30 Case Study- 02 Effect of organic matter and soil fertility on nitrogen mineralization and its uptake by cassava (Manihot esculenta Crantz). Andy , 2015 Java,Indonesia
  • 31. Treatments 20 o C 25 o C 30 o C Soil that planted with cassava less than 10 years Only Groundnut (G) 550.6 773.8 1015.6 Only Maize (M) 435.2 704.9 872.3 G : M (1:1) 533.8 943.0 1036.0 G : M (2:1) 589.6 1011.8 1086.2 G : M (1:2) 459.4 710.5 851.9 Control (Without Organic Matter) 347.8 459.4 450.1 TABLE 05: Cumulative nitrogen mineralization (mg kg-1 ) for 12 weeks at various temperatures and biomasses application. Andy (2015) Java,Indonesia 31
  • 32. 32 Treatments 20 o C 25 o C 30 o C Soil that planted with cassava more than 30 years Only Groundnut (G) 496.6 738.4 747.7 Only Maize (M) 388.7 556.1 638.0 G : M (1:1) 444.5 634.3 638.0 G : M (2:1) 526.4 738.4 783.1 G : M (1:2) 375.7 647.3 758.9 Control (Without Organic Matter) 264.1 437.1 394.3 TABLE:6..Cumulative nitrogen mineralization (mg kg-1 ) for 12 weeks at various temperatures and biomasses application. TABLE:6..Cumulative nitrogen mineralization (mg kg-1 ) for 12 weeks at various temperatures and biomasses application. Andy (2015) Java,Indonesia
  • 33. 33 Case Study-03 Effect of Chemical Composition of Plant Residues on Nitrogen Mineralization Srinivas et al.(2006) CRIDA, Hyderabad
  • 34. Srinivas et al.(2006) CRIDA, Hyderabad 34 TABLE 07: Chemical composition of different tree residues. Plant residues C(%) N% Ligni n % Polyphen ol % C/N Ligni n/N Polyphen ol/N Lignin+Polyph enol/N C.calothyrsus 41.5 2.46 7.21 7.04 a 16.9 2.93 2.86 5.79 C.siamea 42.1 2.07 7.64 3.88 20.3 3.69 1.88 5.57 D.sissoo 40.1 2.42 8.69 2.44 16.6 3.59 1.01 4.60 G.sepium 40.9 3.16 6.84 2.02 12.9 2.16 0.64 2.80 H.binata 40.1 1.91 10.21 3.74 21.0 5.35 1.96 7.31 L.leucocephala 39.5 3.59 6.87 3.10 11.0 1.92 0.87 2.78 P.juliflora 40.7 1.96 8.29 4.02 20.7 4.23 2.05 6.28 T. indica 41.3 1.62 10.15 4.83 b 25.6 6.29 2.99 9.28
  • 35. 35 Plant residues C % N % Lignin % Polyphenol % C/N Lignin/ N Polyphenol/ N Lignin+Polyphenl/ N Caster 41.2 0.95 6.07 0.74 43.4 6.39 0.78 7.17 Horse gram 39.5 1.22 5.36 1.68 32.4 4.39 1.38 5.77 Paddy 40.4 0.48 5.19 0.61 84.2 10.81 1.27 12.08 Pearl millet 42.1 0.84 6.24 0.49 50.1 7.43 0.58 8.01 Sorghum 39.8 0.55 6.81 0.55 72.4 12.38 1.00 13.38 Sugarcane 43.0 0.51 7.54 0.37 84.3 14.78 0.73 15.51 Sunflower 40.2 1.06 8.10 0.82 37.9 7.64 0.77 8.42 TABLE 08: Chemical composition of different crop residues Srinivas et al.(2006) CRIDA,Hyderabad
  • 36. Fig:6..Plant residue quality and nitrogen mineralization 36 G.sepium C. siamea Paddy Sugarcane L.leucocephala C. cajan Srinivas et al.(2006) CRIDA,Hyderabad
  • 37. FIG:7.. Relationships between residue quality parameters and N mineralization for All residues 37 Srinivas et al.(2006) CRIDA,Hyderabad
  • 38. 38 Case Study-04 Impact of the addition of different plant residues on nitrogen mineralization–immobilization turnover and carbon content of a soil incubated under laboratory conditions Abbasi et al. (2015) (PAKISTAN)
  • 39. g kg-1 Plant residues (Treatments) Plant organs Total N Total C Lignin (LG) Polyphen ols(PP) C /N LG / N PP / N LG+PP /N Glycine max shoot 35.2 447 11 13.1 12.7 0.3 0.4 0.7 Glycine max Root 12.8 466 29 26.9 36.4 2.3 2.1 4.4 Zea mays Shoot 9.6 472 41 29.5 49.2 4.3 3.1 7.3 Zea mays Root 4.0 486 48 31.4 121.5 12.0 7.9 19.9 Trifolium repens Shoot 27.4 397 13 18.0 14.4 0.4 0.6 1.1 Trifolium repens Root 16.0 423 21 20.2 26.4 1.3 1.2 2.5 Populus euramericana Leaves 20.8 435 34 53.8 20.9 1.6 2.6 4.2 Robinia pseudoacacia Leaves 33.3 404 28 32.3 12.1 0.8 1.0 1.8 Elaeagnus umbellata leaves 34.7 418 32 38.7 12.1 0.9 1.1 2.0 LSD (p= 0.05) - 3.14 14.16 4.53 3.77 TABLE:9..Mean biochemical composition of the plant residues used in the experiment 39 Abbasi et al. (2015) Pakistan
  • 40. Days after plant-residue addition Treatments 0 7 14 21 28 42 60 80 100 120 CD (p=0.05) mg Nkg-1 soil Control 13.7 13.9 12.9 17.1 30.9 65.9 63.1 75.6 77.7 51.7 2.88 T1 14.8 39.2 49.2 76.8 96.7 158.1 165.2 174.1 188.7 160.9 7.90 T2 13.7 8.1 5.2 8.3 11.8 13.8 28.4 50.4 49.4 27.7 8.15 T3 13.7 7.4 6.2 6.9 10.5 23.1 21.2 36.1 46.7 21.0 5.34 T4 14.3 7.4 9.4 7.7 8.8 15.3 22.2 21.4 32.4 26.4 4.30 T5 14.1 19.0 21.6 55.5 62.5 86.8 127.6 150.8 145.8 93.3 7.31 T6 15.5 8.2 5.2 23.9 34.0 85.3 98.0 149.9 130.2 85.8 9.46 T7 13.0 5.7 4.1 8.6 22.6 55.5 73.1 106.8 87.3 66.9 8.39 T8 13.9 7.4 9.2 23.6 46.6 91.3 111.0 138.9 127.8 93.7 7.83 T9 12.9 9.4 14.5 25.3 51.1 80.1 92.7 140.0 116.4 93.5 6.88 CD (p =0.05) 2.43 4.77 3.12 5.11 7.63 8.23 6.37 9.23 8.27 7.34 TABLE:10..Mean changes in the concentration of total mineral N of a soil amended with different plant residues and incubated at 25 0 C under controlled laboratory conditions during a 120-day period . 40 T1-Glycine max shoot, T2-Glycine max root; T3-Zea mays shoot, T4-Zea mays root; T5-Trifolium repens shoot; T6 -Trifolium repens root T7 -Populus euramericana leaves; T8-Robinia pseudoacacia leaves; T9-Elaeagnus umbellata leaves. Abbasi et al. (2015) Pakistan
  • 41. FIG:8..Net cumulative N mineralized from the added plant residues at different incubation periods. 41 T1-Glycine max shoot T2-Glycine max root T3-Zea mays shoot T4-Zea mays root T5-Trifolium repens shoot T6 -Trifolium repens root T7 -Populus euramericana leaves T8-Robinia pseudoacacia leaves T9-Elaeagnus umbellata leaves Days after residues amendments Abbasi et al. (2015) Pakistan
  • 42. 42 Singh And Kumar (2006) HAU, Hisar Case Study-05
  • 43. Legumes residues OC (g/kg) Total N g/kg C:N ratio Lignin (g/kg) Polyphenols (g/kg) Black gram 428 23.3 18.4 75.0 22.4 Cluster bean 452 18.2 24.8 80.0 44.4 Cowpea 446 21.4 20.8 71.2 27.6 Green gram 416 26.0 16.0 54.1 30.9 Sesbania 440 22.6 19.5 73.9 26.7 Soyabean 462 21.4 21.6 61.2 35.7 Sunhemp 438 20.1 21.8 64.3 32.2 43Singh And Kumar (2006) HAU, Hisar TABLE:11..Characteristics of legumes residues
  • 44. FIG:9..Commulative Nitrogen MineralizationFIG:9..Commulative Nitrogen Mineralization 44 Singh And Kumar (2006) HAU, Hisar
  • 45. TABLE:12..Cumulative net N mineralized and amounts of added N mineralized from legume residues after 56 days of incubation period Legumes residues Net N mineralized (mg/kg) Amount of added N mineralized (%) Hisar Karnal Hisar Karnal Black gram 84 87 72.1 74.7 Cluster bean 53 55 58.2 60.4 Cowpea 71 73 66.4 68.2 Green gram 96 99 73.8 76.1 Sesbania 74 76 65.5 67.3 Soyabean 75 77 70.1 72 sunhemp 65 67 64.7 66.7 45 Singh And Kumar (2006) HAU, Hisar
  • 46. 46 Oglesby And Fownes (2002) Hawaii Case Study-06
  • 47. TABLE:13..Characteristics of green manures used in the experiment Species Polyphenols (%) N (%) Lignin (%) Leaves Twigs Average Calliandra calothyrsus 4.99 1.95 4.06 2.85 13.4 Cassia reticulata 2.10 0.89 1.99 2.65 9.9 Cassia siamea 4.60 1.27 3.92 2.31 10.3 Gliricidia sepiurn 2.07 0.35 1.84 3.43 8.6 lnga edulis 4.71 1.70 3.83 2.51 18.3 Leucaena leucocephala 3.52 1.49 2.93 3.74 11.1 Sesbania sesban 2.60 0.56 1.38 1.39 14.5 47 Oglesby And Fownes (2002) Hawaii
  • 48. Week N (%) Polyphenols (%) Lignin (%) Polyphenol:N Lignin:N 1 0.24 -0.78 -0.13 -0.89 0.00 2.5 0.29 -0.80 -0.48 -0.94 -0.21 4 0.44 -0.71 -0.80 -0.88 -0.56 8 0.37 -0.79 -0.79 -0.90 -0.46 12 0.11 -0.59 -0.79 -0.53 -0.32 TABLE:14.Correlation coefficients of cumulative % N mineralized at each time interval versus initial green manure properties. 48 Oglesby And Fownes (2002) Hawaii
  • 50. 50 FIG:11..Relationship between N mineralized at 8 weeks and Polyphenol : N ratio (Y = 79.4 - 39.5X, n = 7, r 2 = 0.81). Oglesby And Fownes (2002) Hawaii
  • 51. 51 Mafongoya et al. (2008) Florida Case Study-07 Mineralization of nitrogen from decomposing leaves of multipurpose trees as affected by their chemical composition
  • 52. TABLE:15..Chemical composition of leaves of MPT species (on oven-dry matter basis). Mafongoya et al. Florida 52 Treatment N g/Kg NDF-N g/Kg Lignin g/Kg SP phenol g/Kg Acacia angustissima 25b 19a 143b 122b Gliricidia sepium 18c 9d 111c 23d Flemingia macrophylla 18c 11c 193a 105b Sesbania sesban 28ab 5c 67d 112b Calliandra calothyrsus 27ab 12b 114c 154a Cajanus cajan 31a 12b 140b 42d Leucaena leucocephala 31a 11c 120c 122b Acacia+sesbania 27b 12b 105c 117b Cajanus+sesbania 30a 9d 104c 77c Values followed by different letters in each column are significantly different from each other at P~0.05 using Duncan’s Multiple Range Test. NDF-N=neutral detergent fraction), SP= Soluble polyphenols
  • 53. 53 FIG:12.. N mineralization pattern Mafongoya et al. (2008) Florida
  • 54. TABLE:16..Correlation coefficients relating the cumulative amount of net N mineralized to initial chemical properties of multi purpose tree (MPT) leaves during incubation with soil. TABLE:16..Correlation coefficients relating the cumulative amount of net N mineralized to initial chemical properties of multi purpose tree (MPT) leaves during incubation with soil. 54 Times (weeks) NDF-N Lignin SPphenol Tannins L/N P/N L+P/N NDF-N/N 1 -0.64 -0.78 -0.39 -0.01 -0.68 -0.59 -0.78 -0.73 2 -0.70 -0.75 -0.53 -0.23 -0.51 -0.64 -0.68 -0.61 3 -0.61 -0.70 -0.44 -0.06 -0.59 -0.59 -0.72 -0.68 4 -0.66 -0.73 -0.54 0.10 -0.61 -0.71 -0.79 -0.71 5 -0.65 -0.75 -0.53 0.07 -0.64 -0.71 -0.81 -0.72 6 -0.62 -0.73 -0.55 0.07 -0.62 -0.72 -0.80 -0.68 7 -0.63 -0.68 -0.57 0.19 -0.54 -0.71 -0.74 -0.62 8 -0.68 -0.71 -0.56 0.33 -049 -0.67 -0.68 -0.59 Mafongoya et al. (2008) Florida
  • 55. 55 Nitrogen Mineralization from Soil Amended with Gliricidia andNitrogen Mineralization from Soil Amended with Gliricidia and Sorghum Residues:Sorghum Residues: Case Study-08 ICRISAT, HydrabadSridevi et al. (2006)
  • 56. TABLE:17..Residue fractionation: Residue Soluble fractions (% ) Fiber (%) N g kg-1 C/N Sorghum straw 21.4 78.6 5.32 77.3 Glyricidia prunings 53.3 46.7 28.60 13.4 56 ICRISAT, HydrabadSridevi et al. (2006)
  • 57. Amendment N added (mg/ kg) Incubation period in days N mineralized after 90 days (% of added) 0 5 15 30 45 60 75 90 Control - 7.8 4 14.4 6 24. 31 31. 44 35.2 8 37.6 3 39. 19 40. 42 - Sorghum straw 24.39 7.8 4 4.52 12. 41 19. 91 25.1 5 30.3 3 34. 17 39. 06 5.6 Gliricidia prunings 24.39 7.8 4 12.5 8 32. 5 44. 86 51.2 9 56.7 5 60. 31 62. 04 88.6 57 ICRISAT, HydrabadSridevi et al. (2006) Table:18..Nitrogen mineralization
  • 58. 58  N concentration and C:N ratio are sound criteria for predicting nitrogen release in few crop residues while in other residues polyphenol/N ratio, ( lignin + polyphenol ) to N ratio play a role in percent N mineralized.  The composition of residues in terms of soluble and fiber fractions determines whether and to what extent, N is immobilized or mineralized.  The decomposition and nutrient release rates of residues are often regulated by environmental factors, such as temperature and soil moisture, and biochemical composition of plant materials and their interaction. The biochemical composition or quality parameters such as total N concentration, lignin (LG), polyphenols (PP), carbon : nitrogen (C/N) ratio, LG/ N, PP /N and (LG, C, PP) /N ratios are useful indicators that control decomposition and N release of added plant residues. Conclusion of seminar
  • 59. 59