ABSTRACT
Soil enzymes play essential roles in catalyzing reactions necessary for nutrient cycling in the biosphere. The purpose of this study is to estimate soil microbial enzymes activities of collected soil samples using fluorimetric assays. The general concept of the fluorescence enzyme assay is that synthetic Carbon, Nitrogen or Phosphorus rich substrates bound with a fluorescent dye are cleaved from their substrates, which allows them to Florence. Potential Carbon, Nitrogen and Phosphorus enzyme acquisition activities assayed at 0-5cm soil depths did not differ by experimental treatment. Calculating and plotting the sum of all Carbon, Nitrogen and Phosphorus cycling enzyme activities was a useful approach to observe broader patterns regarding their potential cycle. Enzymes activities for total Carbon, Nitrogen and Phosphorus cycling trended lower in the plot exposed to Elevated Heating Condition and CO2 (EHC) compared to the plots exposed to Ambient Climatic Conditions (ACC) at the 5-15cm soil depths. This trend was on significant for total N and P cycling activities (p< 0.046). Potential enzyme C: P and N : P ratios were higher in the plots exposed to Elevated Heating Condition and CO2 (EHC) compared to the plots exposed to Ambient Climatic Condition (ACC) at 5-15cm soil depths (p= 0.05). This observation suggests that there is a relatively higher P mineralization enzyme activity at lower soil depth (5-15cm). For the estimation of soil enzymes activities, Fluorescence-based assays are a useful tool that is widely used to examine potential Enzyme activities among treatment plots.
TABLE OF CONTENTS
Title
page i
Certification ii
Dedication iii
Acknowledgement iv
Table
of contents v
List
of tables vi
List
of figures vii
Abstract viii
CHAPTER ONE
1.0
Introduction 1
1.1
Objective of the Study 3
CHAPTER TWO
2.0
Literature Review 4
2.1
Soil Enzymes 4
2.2
Microorganism as Indicators of Soil
Health 5
2.3
Types of Soil Enzymes 6
2.4
Origin and State of Soil Enzymes 9
2.5
Importance of Enzymes to Soil
Management 9
2.6
Soil Enzyme Activities; A Component
of Soil Biodiversity 11
2.7
Environmental Factors Affecting the
Distribution of Soil Enzymes 12
2.8
Sources of Soil Enzymes Activities 15
2.9
Methodological Consideration for
Estimating/Measuring Enzyme
Activities in Soils 16
CHAPTER THREE
3.0
Materials and Methods 20
3.1
Materials/Equipment 20
3.2
Enzyme Assay Set-up 20
3.3 Incubation of Assay Plates 22
3.4
Florescent Measurements on a
Microplate Fluorometer 23
3.5
Data Analysis 23
CHAPTER FOUR
4.0
Results 26
CHAPTER FIVE
5.0
Discussion, Conclusion and
Recommendation 37
5.1
Discussion 37
5.2
Conclusion 38
5.3
Recommendation 39
REFERENCES 40
LIST OF TABLES
Table
1: Important Classes of Soil Enzymes 8
Table
2: Roles of Soil Enzymes 10
Table
3: Deep well plate design for fluorescence standard concentrations
with soil
samples 28
Table
4: Deep well palate design for soil samples with substrate 29
Table
5: Incubator temperatures required for corresponding incubation time periods 29
Table
6: MUB and MUC standard curve calculations 30
Table
7: Enzyme activity calculations 31
LIST OF FIGURES
Figure
1: MUB standard curve plot 32
Figure
2: C, N and P cycling enzyme activities 33
Figure
3: Total C, N and P cycling enzyme stiochiometric ratios 34
Figure
4: Enzyme stoichiometry for total C, N and P cycling enzyme activities 35
CHAPTER ONE
1.0 INTRODUCTION
Enzymes are defined as biological catalysts for
specific reactions, which depend on several biotic and abiotic factors such as:
pH, temperature, presence or absence of inhibitors, soil organic matter
composition, cultivation technique, and other factors, which can directly
influence the chemical reactions of these molecules in the soil (Shukla et al., 2006). Enzymes are released in soils by microbes and
plant roots. They can degrade complex substrates into low molecular weight
compounds in soils (Schimel and Bennett, 2004). The
chemical and physical processes related to organic matter decomposition may be
better understood when accompanied by the activity of several enzymes, not only
one, because organic substrates contain a great diversity of organic compounds
and ions with active participation in the soil biogeochemical cycles (Caldwell et al., 2005).
The
origin of soil enzymes is mainly microbial. They can be found within microbial
cells as well as extracellularly in the soil, bound to clay minerals and humic
substances. Extracellular enzymes are
important for the breakdown of macromolecules such as celluloses,
hemicelluloses, and lignin, while intracellular enzymes are the disrupting
agents of smaller molecules, e.g., sugars or amino acids (Dick and Kandeler,
2004). Microbial enzymes can participate
in adsorption, oxidation, reduction, hydrolysis, and complexation reactions,
converting organic substances into other products to maintain the balance in
the soil environment (Dinesh et al.,
2004; Caldwell et al., 2005).
Enzymes can be affected by many factors, biological
(microbial populations, fauna, etc.), chemical (pH, organic matter
contents, etc.) and, human activities (fire treatment, pesticides, heavy
metals, etc.) (Sannino and Gianfreda, 2001; Shen et al., 2005; kicker, 2007), all of which change the biogeochemical
cycles in an ecosystem. Therefore, the evaluation of enzyme activity in the
soil is very important in order to assess the biochemical function, organic matter
fraction, nutrient cycle, and decomposition of xenobiotics.
Enzyme activities are involved in
processes important to soil function such as organic matter decomposition and
synthesis, nutrient cycling, and decomposition. Enzyme activity stoichiometry
has been more recently adopted as an index to assess soil biochemical nutrient
cycling by intersecting ecological stoichiometric theory and metabolic theory
of ecology to assess potential microbial nutrient imbalances corresponding to
environmental conditions (Sinsabaugh et al., 2009).
Numerous studies have suggested that wide stoichiometric ratios are indicative
of nutrient growth limitations (Fujita et al., 2010)
and as soil nutrients become limited, microbes respond by allocating metabolic
resources to produce specific enzymes to acquire deficient nutrients (Allison et al., 2007).
The aim of this study is
to estimate the activities of soil microbial enzymes in collected soil samples
using fluorometric assays. The general concept of the fluorescence enzyme assay
is that synthetic Carbon, Nitrogen, or Phosphorus rich substrates bound with a fluorogenic
moiety (fluorescent dye) are added to soil samples. When intact, the labeled
substrates do not fluoresce. During enzyme-catalyzed substrate degradation, the
bond breaks between the fluorescent dye and the substrate. The fluorescent dye
liberated from the substrate is consequently used as an indirect estimation of
enzyme activity, and can be quantified using a microplate reader to detect the
fluorescence intensity of the dye. In brief, fluorescence quantification is
accomplished as the liberated dye emits light of one wavelength after absorbing
light of a different wavelength.
Enzyme
activity can be subsequently quantified based on the known fluorescent-dye
concentrations of the substrate (i.e. known quantities of synthetic
substrate added to soil samples) along with referencing a standard dilution
curve of fluorescence intensities for the specific fluorogenic moiety of the
substrate used in the assay (i.e. 4-methylumbelliferone (MUB) or
7-amino-4-methylcoumarin (MUC)).
The two most commonly used synthetic fluorescent
indicators are 4-methylumbelliferone (MUB) and 7-amino-4-methylcoumarin (MUC)
(Jasinski and Woudenberg, 1994). MUC-linked substrates are commonly associated
with N-rich synthetic substrates such as proteins and/or amino acids.
1.1 OBJECTIVES OF THE STUDY
The broad objective of this study is to estimate
soil enzyme activities in collected soil samples of different depth, using
fluorometric enzyme assays.
The specific objectives of the study are to;
i.
determine the overall soil enzyme activity in the collected soil sample
ii.
determine the Carbon, Nitrogen, and Phosphorous enzyme acquisition
activities
iii.
determine the soil Enzyme activities
stoichiometry for total Carbon, Nitrogen, and Phosphorus cycling
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