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Role of microbes in nutrient mobilization, transformation in fertilizer use effic
1. Name of Speaker : Jayvirsinh P. Solanki
Degree : M. Sc. Agri. (Agril. Microbiology)
Major Advisor : Dr. R. V. Vyas
Minor Advisor : Dr. S. N. Shah
Course No. : MICRO. 591
Reg. No. : 04-2917-2016
Date : 19/10/2017
Time : 3:30 p.m.
Microbes role for nutrient mobilization,
transformation and in fertilizer use efficiency
4. The fertility of the soil depends
upon
ďˇ Quantitative nature of the
microorganisms
ďˇ Organic matter content
ďˇ Nature of microbial products which
bind the soil particle together
ďˇ Humus content
4
5. Mobilization
⢠Basic mechanism through which microbes promote nutrients
bioavailability includes nutrient fixation, mobilization and
transformation
⢠Nutrient mobilization is the process of making nutrients
movable or capable of moving by the physiochemical or
biochemical ways
⢠Microbes play a very important role in nutrient mobilization
through the biochemical actions like release of organic
acids, proton extrusion and lowering pH
⢠Bacterial, fungal inocula and organic amendments can
mobilize nutrient reserves
5
7. Phosphorus Mobilization
⢠Microbes play a fundamental role in mobilizing organic, native or
inherited P that unavailable for plants
⢠The total P acquired by plants through bacteria and fungus (75%)
⢠Biochemical processes operating in the rhizosphere determine the
mobilization and acquisition of soil nutrients
⢠Wide variety of bacteria, fungi and endophytes solubilize insoluble P
through the production of organic acids, a feature which is genetically
controlled
⢠Such type of inocula are termed as P-mobilizing microbes, as these
inocula do not only solubilize P, but they also mobilize its organic form
through mineralization and facilitate the translocation of phosphate
7
8. P mobilization mechanism & Microorganisms
Organic P
mobilization
Direct way
Lowering pH
Hydrolyze
organic P
Indirect way
Release of
CO2
Release of
Protons
Bacillus Beijernckia Burkholderia Enterobacter Flavobacterium Microbacterium
Pseudomons
Mesorhizobium
cicero
Mesorhizobium
mediterraneum
Aspergillus Penicillium
8
9. ⢠K is present in very small amount ranging from 0.04 to 3.00%
⢠Despite of being in limited amount, 98% of this K is bound within the
Phyllosilicates structures
⢠The remaining 2% exists in soil solution or on exchange sites to become
available for the plants
⢠Hence, soil fertility is decreased due to low availability of this nutrient
⢠Many microorganism in the soil are able to solubilize unavailable forms of K-
bearing minerals, such as micas, feldspar, illite and orthoclases by
excreting organic acids which either directly dissolves rock K or chelate
silicon ions to bring the K into solution
K mobilization
9
12. Fe mobilization
⢠Iron is the fourth most abundant element available on earth and predominantly exits in nature in
ferric (Fe3+) form
⢠It is sparingly soluble, therefore not readily available for plant
⢠Iron limitation is a problem for plants on as much as 30% worldwide
⢠Iron tends to form insoluble complexes in aerobic soils of neutral to basic pH
⢠In soil ferrous (Fe2+) is oxidized to ferric (Fe3+) thereby forming insoluble compounds and leaving
a very low amount of iron for plant assimilation
⢠Some strains of bacteria synthesize low molecular mass proteins known as siderophores
⢠Siderophores have high affinity to chelate and solubilize iron from mineral or organic compounds
⢠Generally siderophores have high affinity to form complexes with ferric (Fe3+) uptake of the
complexes by the cell membrane of both gram positive and negative bacteria reduces ferric (Fe3+) â
ferrous (Fe2+)
12
13. Siderophore producing bacteria for iron chelation
Bradyrhizobium
japonicum
Rhizobium
leguminosarum
Sinorhizobium
meliloti
Pseudomonas
Enterobacter
genera
Bacillus
rhodococcus
13
14. Zinc mobilization
⢠Zinc is required in relatively small concentration although
prevalence of Zn deficiency in crop is due to low solubility of Zn
rather than low Zn availability
⢠50% of Indian soils are Zinc deficient
⢠Solubility of Zn decrease with
ďź Increase in pH
ďź High organic matter
ďź Bicarbonate content
ďź High magnesium to calcium ratio
ďź High availability of P and Fe
14
15. ⢠The Zinc applied to agriculture fields as Zinc sulphate (Soluble) get converted to
different insoluble forms like:
ďź Zinc hydroxide [Zn(OH)2] at high soil pH,
ďź Zinc Carbonate [ZnCo3 ] in calcium rich alkali soils,
ďź Zinc phosphate [Zn3(PO4)2] in near neutral to alkali soil with large application of
P fertilizers and
ďź Zinc sulfide [ZnS] under reducing conditions particularly during flooding
⢠The soluble form of Zn fertilizers applied to the fields become readily insoluble forms
that cannot be assimilated by plants which leads to the Zn deficiency in crops
⢠The microbes solubilize the Zn by lowering the pH by gluconic acid and indole acetic
acid production
⢠Example:
Acinetobacter sp. Burkholderia sp.
15
16. Sulphur mobilization
⢠In agricultural soil, most of the Sulphur (>95%) is present as
sulphate esters or as carbon bounded Sulphur rather than inorganic
Sulphur
⢠The two major form of organo-S, Sulphur-esters and sulfonates are
not directly available to plants which rely upon microbes in soil and
rhizosphere for organo- S mobilization
⢠Different Sulphur forms are interconverted and immobilized Sulphur
is mineralized to yield plant available inorganic Sulphur
⢠Organic form of Sulphur is metabolized by soil microorganism to
make it available for plant in an inorganic form like mineralization,
immobilization, oxidation and reduction
16
27. Fertilizer use efficiency (FUE)
⢠Its an estimate of the productivity per unit of nutrient uptake or loss
⢠It depends upon the ability of efficient uptake, transport, storage,
mobilization, usage within the plant and even on the environment of
nutrient from the soil
⢠The FUE/NUE is an important ecological measure as it integrates a
variety of physiological processes in how nutrients taken up by plants
are generally used for the production of biomass
27
28. Table 2. Current status of nutrient use efficiency (NUE) of agricultural ecosystem
Nutrients Nutrient use efficiency
(NUE%)
Nitrogen (N) 30-50
Phosphorus (P) 10-20
Potassium (K) 70-80
Sulphur (S) 8-12
Zinc (Zn) 2-5
Iron (Fe) 1-2
Copper (Cu) 1-2
Manganese (Mn) 1-2
28
29. Why fertilizer use efficiency is important �??
⢠Improving FUE is an important goal to harvest better crop yield on sustained
basis
⢠Overall the nutrient use efficiency by crop plant is ~50% under all agro-
ecological conditions
⢠Hence, large part of the applied nutrients is lost in the soil-plant system
⢠To check the nutrient loss and their adverse effect due to excess usage and
diminish the cost in crop production
⢠To minimize the pollution hazard due to increasing use of chemical fertilizer
29
30. Integrated Nutrient Supply for FUE
ONLYSOILNUTRIENT
SOILNUTRIENTS+
ORGANICMANURES
SOILNUTRIENTS+
ORGANICMANURES+
CHEMICALFERTILISERS
SOILNUTRIENTS+
ORGANICMANURES+
CHEMICALFERTILISERS+
BIOFERTILISER
YEILD
BENEFITS :
⢠MAXIMUM PRODUCTIVITY
⢠ECONOMIC CULTIVATION
⢠SUSTAINED SOIL FERTILITY
30
40. Fig. 3 Effect of AMF and KMB on cured leaf yield of tobacco (P = 0.05)
40
41. Treatment
No.
Treatment Nicotine(%) Reducing sugar(%)
1 NPK 1.45 20.37
2 Absolute control 0.95 6.81
3 AMF+NPK 1.52 21.46
4 AMF alone 0.93 14.51
5 KMB + NPK 1.48 21.32
6 KMB alone 1.01 18.45
7 KMB + AMF + NPK 1.72 22.90
8 KMB + AMF 1.13 17.22
CD at 5% 0.17 1.07
Table 10 . Effect of AMF and KMB on the quality parameters of FCV tobacco leaf
41
42. Table 11. The interactive effects of N chemical fertilizer and bio-fertilizer on the nutrient content of rice grain
Treatment
no.
Chemical N
fertilization
Microbial
inoculation
N (%) P (%) Fe (%) Zn (mg kg-1) NUE (%)
1 N1 M 1.81 c 0.68 c 23.77 b 29.26 abc 0.71
2 N1 H 1.85 bc 0.61 d 35.66 a 35.02 a 0.73
3 N1 C 1.71 d 0.39 e 14.22 c 11.22 d 0.67
4 N2 M 1.83 c 0.76 ab 21.88 c 31.48 ab 0.96
5 N2 H 2.01 a 0.81 a 17.88 c 35.38 a 1.04
6 N2 C 1.70 d 0.38 e 22.88 d 10.77 d 0.89
7 N3 M 1.80 c 0.70 bc 21.77 b 27.60 bc 1.38
8 N3 H 1.91 b 0.68 c 26.11 b 24.76 c 1.46
9 N3 C 1.40 e 0.38 e 6 d 7.66 d 1.07
Case 4: Rice nutrient management using mycorrhizal fungi and endophytic
Herbaspirilum seropedicae
Iran Hoseinzad et al., 2016
P = 0.05, M = Mycorrhizal fungi, H = Herbaspirilium seropedicae, C = control,
NUE = Nutrient use efficiency
42
43. Table 12. The interactive effects of P fertilizer and bio-fertilizer on soil and plant nutrient content
Treatmen
t no.
Chemical P
fertilization
Microbial
inoculation
Straw P
(%)
Straw Fe (mg
Kg-1)
Soil K (mg kg-1) Soil Fe (mg kg-1)
1 P1 M 0.52 d 21 c 228 ab 237.30 bc
2 P1 H 0.67 c 20 c 227 bc 246.38 ab
3 P1 C 0.38 e 21 c 228 ab 214.96 d
4 P2 M 0.77 b 33 a 229 ab 235.27c
5 P2 H 0.77 b 14 d 206 c 232.80 c
6 P2 C 0.42 e 9 e 230 a 215.08 d
7 P3 M 0.86 a 34 a 228 ab 253.84 a
8 P3 H 0.66 c 30 b 228 ab 229.72 c
9 P3 C 0.36 e 8 e 280 ab 213.90 d
43Values in the same column followed by different letters are significantly different at P = 0.05
44. Figure 4. Effect of ZnO nanoparticles on plants
phenological parameter stems height, root length,
root area, root diameter and root nodule.
Observations are also compared with bulk ZnO
nanoparticles
Figure 5. Effect of ZnO particles (bulk and
nano) on p-mobilizing enzymes (acid P, alkaline
P, phytase) and soil microbial population
indicator enzyme (dehydrogenase)
Raliya et al., 2016St. Louis, USA
Case 5: Enhancing the mobilization of native phosphorus in mung bean rhizosphere using ZnO
nanoparticles synthesized by soil fungi
44
45. Figure 6. Effect of ZnO nanoparticles on plant P uptake
from rhizosphere in mung bean plant
Figure 8. Accumulation of metal
ion in leaf, stem, root and seeds:
ICP-MS analyses of ZnO particles
(bulk and nano) treated plants
Figure 7. Influence of bulk and synthesized ZnO
nanoparticles on chlorophyll and protein content in the
leaves of mung bean
45
46. Table 13. Effect of inoculated KMB strains in available soil potash at different incubation period
Treatment
no.
Treatments
Incubation periods (Days) Mean
30 60 90 120 150
Available Potash (mg/kg of soil)
1 Control 90 90 90 91 90 90
2 TKMB 3 100 124 127 125 124 120
3 TKMB 6 101 124 128 125 125 121
4 TKMB 8 93 111 115 113 113 109
5 TKMB 11 118 122 128 127 127 124
Mean 125.58 142.50 164.92 145.17 144.92
S. Em 1.281
For comparing
two
at 5%
Strains 1.13
Time 0.90
Strain Ă Time 2.54
Bhattacharya et al., 2016Jorhat, India
Case 6: Isolation of potash mobilizing microorganisms in tea soil and evaluation of
their efficiency in potash nutrition in tea
46
57. ďź The microbes play a vital role in nutrient mobilization, transformation
and fertilizer use efficiency are evident by many case studies, without
them or their activities stated for different natural biological
processes and the crop growth remains low
ďź Microbial inoculantâs actions in rhizosphere directly helps for the
nutrient accessibility viz. N, P, K, S, Fe, Zn etc. in soil by taking part in
nutrient dynamics and ultimately to achieve the important goal of
agriculture to harvest better crop yield and to keep soil healthy and
living for a long run in sustained manner
Conclusion
57
58. ďź Need for search of newer native microbes which have better
mobilization, transformation activity which can save
chemical fertilizer and increase fertilizer use efficiency
ďź Search for novel multifunctional native microbial
community
ďź Molecular approaches for microbial strain improvement for
greatest mobilization and transformation activity
Future prospects
58