ASBTRACT
The aims of this research work is to isolate and identify phosphate solubilizing Bacillus from soil. Soil samples were collected and evaluated for phosphate solubilizing Bacillus in piskovskaya agar plates. A total of eight (8) phosphate solubilizing Bacillus colonies were isolated from the rhizosphere soils on pikovskaya agar (PVK) medium containing tricalcium phosphate. Out of the 8 bacterial isolates three showed clear halo zones around the colony. Phosphate solubilizing index (PSI) of each isolate was calculated. The three isolates include Bacillus species, streptomyces species and Lysini bacillus. From the results it was revealed that isolate Lysini bacillus had the highest phosphate solubilizing ability with a PSI value of 4.00 followed by Lysini bacillus (3.60) while the lowest was found in Streptomyces with 3.42. The halo zone of inhibition was found in Bacillus species with 13.0mm while the lowest was found in Lysini bacillus. from the result also it was shown that Streptomyces spp has phosphate solubilizing efficiency (μg/ml) in Pikovskaya broth. Eight phosphate solubilizing actinomycete isolates were identified on the basis of colony characteristics, microscopic observation and biochemical test. It is clear from the present study that the rhizosphere actionomycete are efficient in solubilization of phosphate in soil by producing organic acids. The strain M6 belongings to genera Bacillus spp showed significant potential in solubilizing the phosphate may be due to its capability to produce high amount of organic acids which release phosphate to soil solution from phosphate bearing minerals. The release of phosphate from the muscovite mica increased with the inoculation period of specific strain of streptomycete and Bacillus. As the strains of M2 and M6 gave very good results, they can be now tested on the field to rate its performance as biofertilizer for the particular location.
TABLE OF CONTENT
TITLE PAGES
Title page i
Certification ii
Dedication iii
Acknowledgements iv
Table of contents v
Lists of tables ix
CHAPTER ONE 1
1.1 Introduction 1
1.2
Objectives the Study 2
CHAPTER TWO
3
2.0 Literature Review 3
2.1 Soil 4
2.2 Function of soil 5
2.3 Soil
organic matter 6
2.4 Microbial diversity of the soil 6
2.5
Phosphate solubilizing microorganism 8
2.5.1 Mechanism of phosphate solubilization 8
2.5.2 Inorganic phosphate solubilization 8
2.5.3 Organic phosphate solubilization 9
2.5.4 Phosphate solubilizing bacteria as plant
growth promoters 11
2.4.1 Genetic engineering of phosphate
solubilizing microorganisms 12
CHAPTER THREE 13
3.0 Materials and
Methods 13
3.1 Materials 13
3.2 Method 13
3.2.1
Sample Collection and preparation 13
3.2.2 Microbiology analysis serial dilution 13
3.2.3
Identification of phosphate solubilizing bacteria 14
3.2.3.1 Gram Staining 14
3.2.4 Biochemical Reaction Test 27
3.2.4.1 Catalase Test 27
3.2.4.2 Methyl Red Test 27
3.2.4.3 Voges- Proskauer (Vp) Test 28
3.2.4.4 Indole Test 28
3.2.4.5 Citrate Utilization Test 28
3.2.4.6
Sugar Utilization Tests 28
3.2.5
Identification of Isolate 29
3.2.6
Optimal Growth Condition of the Isolates 29
CHAPTER
FOUR 30
4.0 Results 30
CHAPTER
FIVE
38
5.0 Discussion
and Conclusion 38
5.1 Discussion 38
5.2 Conclusion 39
References 40
4.1: Phosphate solubilization efficiency
of the isolates 19
4.2: Colonial characteristic and
Biochemical features of the Bacterial isolates 20
CHAPTER ONE
1.0.
INTRODUCTION
Phosphorous
is a one of the most abundant metallic elements found in the earth’s crust and
is present in the soils in both inorganic and organic forms (Gyaneshwar et
al., 2002). It is utilized or absorbed by the plants in inorganic form i.e.
in orthophosphate (H2PO4-and HPO42-) (Hinsinger, 2001). It has a key role in
metabolic processes such as photosynthesis, energy transfer, signal
transduction, nitrogen fixation in legumes, crop quality and resistance to
plant diseases are the main features associated with phosphorous nutrition (
Khan et al, 2014).
The solubilization of
phosphate-bearing inorganic materials by microorganisms would seem to be an
attractive solution that has been actively studied during the last decade.
Several mechanisms, such as lowering the pH by acid production, ion chelation
and exchange reaction in the growth environment, have been reported to play a
role in solubilization by phosphate solubilizing microorganisms (PSM) (Rajankar
et al., 2007). Among these PSM, Actinomycetes are of special interest
since these filamentous sporulating bacteria are able to develop in extremely
different soils (Jiang et al., 2005; Pathom-Aree et al., 2006)
and produce various substances (anti-fungi, insecticides, anthelminthics,
phytohormone-like compounds etc.) that could benefit plant growth (Jain and
Jain, 2007) showed that the abundance of actinomycetes solublizing Moroccan
rock phosphate, from a Togolese phosphate mine, was approximately 19%. Reports
in the literature suggested that microbial solubilization of mineral phosphate
might be either due to the excretion of organic acids causing acidification of
the external medium (Whitelaw, 2000), or to the excretion of chelating
substances (such as sidero-phores) that form stable complexes with phosphorus adsorbents
(aluminium, iron and calcium) (Welch et al.,2002), and thus increase
phosphate solubilization.
A
number of heterotrophic microorganisms excreting organic acids which
solubalized P that chelate cationic partners of P ions and release the P
directly into solution (He et al., 2002). These phosphate solubilizing
bacteria (PSB) are being used as biofertilizer since 1950s. Microbial
inoculants assimilate soluble P, and prevents it from adsorption or fixation
(Khan and Joergesen, 2009). These microorganisms influences soil fertility
through various processes viz. decomposition, mineralization and release of
nutrients. Microorganisms enhance the P availability to plants through
solubilization of inorganic form of P to in available form (Chen et al.,
2006). Hence, microbial inoculants are used as an alternate source, which are
both economic as well as eco-friendly. A continued exploration of the natural
biodiversity of soil microorganisms and the optimization of microbial
interactions in the rhizosphere represents a prerequisite step to develop the
more efficient microbial inoculants with phosphorus-solubilizing ability.
Microorganisms
constitute an inexhaustible reservoir of compounds with pharmacological,
physiological, medical or agricultural applications (Nanjwade et al., 2010). Soil is not only
important for agriculture but also very useful for living organism (Jain and
Singh, 2013). The diversity of physical characteristics of soil associate with
aggregation at small scales means that soil can contain a large diversity of
microorganisms in close proximity, and the chemical composition of soil is
highly heterogeneous in both vertical and horizontal dimensions (Kang and
Mills, 2006). Jain and Singh (2013) suggested that different variety of soil
contains different properties, which support many organisms of the soil. Soil
in particular is an extensively exploited ecological niche, the inhabitants of
which produce many biologically active natural products including clinically
important antibiotics (Kumar, Durapanduyan and Ignacimuthu, 2014).
1.2. AIM AND OBJECTIVES
This research aims is to isolate and identify
phosphate solubilizing bacteria from soil
1.2.1 OBJECTIVES
The
specific objectives of this study are, namely;
· To
isolate bacteria from soil
· To
characterize and identify bacteria from soil.
· To
determine phosphate solubilizing bacteria isolates from soil.
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