Lab.8 isolation of nitrogen fixer bacteriaHama Nabaz
ย
Here are the answers to your questions:
1. The enzyme responsible for nitrogen fixation is nitrogenase. The level of O2 is regulated to obtain maximum nitrogenase activity through a process called microaerophily, where O2 concentration is kept low to protect the oxygen-sensitive nitrogenase enzyme.
2. Nitrogen fixation is important because atmospheric nitrogen gas (N2) is inert and unavailable to most organisms. Nitrogen fixation converts atmospheric N2 into bioavailable forms like ammonia (NH3) that can be used by plants and other organisms for growth. It replenishes soil nitrogen.
3. The Rhizobiaceae that form symbiotic relationships with legumes are more important than the Azotobacteraceae in
This document provides an overview of the nitrogen cycle and legumes. It discusses how legumes have a symbiotic relationship with rhizobia bacteria in their roots that fix nitrogen. It also explains the processes of nitrogen fixation, nitrification, denitrification, volatilization, decay, and the carbon-nitrogen ratio in relation to the nitrogen cycle. Key points covered include how rhizobia are specific to different legume species and that naturalized rhizobia can be as effective as commercial inoculants in fixing nitrogen.
The document summarizes the nitrogen cycle. It describes the key steps in the nitrogen cycle as nitrogen fixation, nitrogen assimilation, ammonification, nitrification, and denitrification. Nitrogen fixation involves converting nitrogen gas from the atmosphere into inorganic nitrogen compounds usable by plants and animals. This is done mainly by nitrogen-fixing bacteria. The nitrogen is then assimilated by plants and animals and enters the ecosystem. As organisms die and decay, ammonification occurs which converts nitrogen into ammonia. Nitrification then transforms ammonia into nitrates which can be used by plants. Finally, denitrification returns nitrates to the atmosphere as nitrogen gas by bacteria. The document also discusses how human activities like fertilizer use and fossil fuel burning
The document summarizes the nitrogen cycle. It discusses the main sources of nitrogen including the atmosphere, soil, fertilizers and volcanic activity. It then describes the key processes in the nitrogen cycle including nitrogen fixation, ammonification, nitrification, and denitrification. Nitrogen fixation occurs through symbiotic and non-symbiotic bacteria. Ammonification and nitrification are multi-step biological processes converting organic and ammonia forms of nitrogen into nitrites and nitrates. Denitrification returns nitrogen to the atmosphere through bacteria. The factors that impact these nitrogen transformations such as oxygen, temperature, pH and carbon levels are also outlined.
The nitrogen cycle consists of 5 main stages:
(1) Ammonification is the conversion of organic nitrogen into ammonium by microbes.
(2) Nitrification is the oxidation of ammonium to nitrite and then nitrate by bacteria.
(3) Plants uptake nitrate and convert it into amino acids and other nitrogen compounds.
(4) Nitrogen fixation converts atmospheric nitrogen to ammonium via bacteria and cyanobacteria.
(5) Denitrification reduces nitrates back to nitrogen gas which re-enters the atmosphere. The nitrogen cycle involves the circulation of nitrogen through air, soil, plants and animals via specialized microbes.
The document discusses the different types of microbes based on their oxygen requirements for growth:
- Obligate aerobes require oxygen to live and have enzymes like superoxide dismutase and catalase that allow them to tolerate oxygen. Facultative anaerobes can use oxygen but can switch to fermentation if oxygen is gone. Obligate anaerobes and aerotolerant anaerobes cannot use oxygen for growth and it is toxic. Microaerophiles require oxygen levels lower than atmospheric levels.
Lab.11 methods for estimating denitrification processHama Nabaz
ย
1. Denitrification is the process by which nitrates in soil are converted to atmospheric nitrogen gases like nitrous oxide and dinitrogen through the action of denitrifying bacteria that use nitrates as an electron acceptor during respiration.
2. The denitrification process involves the step-wise reduction of nitrates to nitrites, nitric oxide, nitrous oxide, and ultimately dinitrogen gas, which escapes into the atmosphere. This closes the nitrogen cycle by returning nitrogen to its gaseous form.
3. Experiments were conducted to detect denitrification in soil samples by inoculating nitrate broths containing Durham tubes to detect gas production, identifying isolates that grow on nitrate agar,
Lab.8 isolation of nitrogen fixer bacteriaHama Nabaz
ย
Here are the answers to your questions:
1. The enzyme responsible for nitrogen fixation is nitrogenase. The level of O2 is regulated to obtain maximum nitrogenase activity through a process called microaerophily, where O2 concentration is kept low to protect the oxygen-sensitive nitrogenase enzyme.
2. Nitrogen fixation is important because atmospheric nitrogen gas (N2) is inert and unavailable to most organisms. Nitrogen fixation converts atmospheric N2 into bioavailable forms like ammonia (NH3) that can be used by plants and other organisms for growth. It replenishes soil nitrogen.
3. The Rhizobiaceae that form symbiotic relationships with legumes are more important than the Azotobacteraceae in
This document provides an overview of the nitrogen cycle and legumes. It discusses how legumes have a symbiotic relationship with rhizobia bacteria in their roots that fix nitrogen. It also explains the processes of nitrogen fixation, nitrification, denitrification, volatilization, decay, and the carbon-nitrogen ratio in relation to the nitrogen cycle. Key points covered include how rhizobia are specific to different legume species and that naturalized rhizobia can be as effective as commercial inoculants in fixing nitrogen.
The document summarizes the nitrogen cycle. It describes the key steps in the nitrogen cycle as nitrogen fixation, nitrogen assimilation, ammonification, nitrification, and denitrification. Nitrogen fixation involves converting nitrogen gas from the atmosphere into inorganic nitrogen compounds usable by plants and animals. This is done mainly by nitrogen-fixing bacteria. The nitrogen is then assimilated by plants and animals and enters the ecosystem. As organisms die and decay, ammonification occurs which converts nitrogen into ammonia. Nitrification then transforms ammonia into nitrates which can be used by plants. Finally, denitrification returns nitrates to the atmosphere as nitrogen gas by bacteria. The document also discusses how human activities like fertilizer use and fossil fuel burning
The document summarizes the nitrogen cycle. It discusses the main sources of nitrogen including the atmosphere, soil, fertilizers and volcanic activity. It then describes the key processes in the nitrogen cycle including nitrogen fixation, ammonification, nitrification, and denitrification. Nitrogen fixation occurs through symbiotic and non-symbiotic bacteria. Ammonification and nitrification are multi-step biological processes converting organic and ammonia forms of nitrogen into nitrites and nitrates. Denitrification returns nitrogen to the atmosphere through bacteria. The factors that impact these nitrogen transformations such as oxygen, temperature, pH and carbon levels are also outlined.
The nitrogen cycle consists of 5 main stages:
(1) Ammonification is the conversion of organic nitrogen into ammonium by microbes.
(2) Nitrification is the oxidation of ammonium to nitrite and then nitrate by bacteria.
(3) Plants uptake nitrate and convert it into amino acids and other nitrogen compounds.
(4) Nitrogen fixation converts atmospheric nitrogen to ammonium via bacteria and cyanobacteria.
(5) Denitrification reduces nitrates back to nitrogen gas which re-enters the atmosphere. The nitrogen cycle involves the circulation of nitrogen through air, soil, plants and animals via specialized microbes.
The document discusses the different types of microbes based on their oxygen requirements for growth:
- Obligate aerobes require oxygen to live and have enzymes like superoxide dismutase and catalase that allow them to tolerate oxygen. Facultative anaerobes can use oxygen but can switch to fermentation if oxygen is gone. Obligate anaerobes and aerotolerant anaerobes cannot use oxygen for growth and it is toxic. Microaerophiles require oxygen levels lower than atmospheric levels.
Lab.11 methods for estimating denitrification processHama Nabaz
ย
1. Denitrification is the process by which nitrates in soil are converted to atmospheric nitrogen gases like nitrous oxide and dinitrogen through the action of denitrifying bacteria that use nitrates as an electron acceptor during respiration.
2. The denitrification process involves the step-wise reduction of nitrates to nitrites, nitric oxide, nitrous oxide, and ultimately dinitrogen gas, which escapes into the atmosphere. This closes the nitrogen cycle by returning nitrogen to its gaseous form.
3. Experiments were conducted to detect denitrification in soil samples by inoculating nitrate broths containing Durham tubes to detect gas production, identifying isolates that grow on nitrate agar,
Decomposers such as bacteria and fungi break down dead organic matter and release nutrients back into the soil. Nitrogen is an essential nutrient that is recycled through a nitrogen cycle. This involves nitrogen fixation by bacteria, assimilation by plants, ammonification through decomposition, nitrification by special bacteria, and denitrification which returns nitrogen to the atmosphere. Maintaining this nitrogen cycle is important for supporting new plant growth in ecosystems.
The nitrogen cycle describes the movement of nitrogen through ecosystems. Nitrogen is absorbed by plants from the soil and incorporated into proteins. Animals get nitrogen by eating plant proteins. Bacteria break down nitrogenous waste from dead plants and animals, converting it into ammonium, then nitrites and nitrates, which enrich the soil. Lightning and bacteria also fix atmospheric nitrogen into forms usable by plants.
Lab.10 methods for estimating nitrification processHama Nabaz
ย
Nitrification is the two-step process by which ammonia is oxidized to nitrite and then to nitrate by autotrophic bacteria. In the first step, ammonia is oxidized to nitrite by bacteria like Nitrosomonas. In the second step, nitrite is oxidized to nitrate by bacteria like Nitrobacter. This process occurs in aerobic environments in soil and water and makes nitrogen available to plants. The summary demonstrates the key steps in nitrification and the bacteria involved in converting ammonia to nitrates through nitrites in two steps.
Sewage contains organic waste that provides food for bacteria. The bacteria multiply and consume oxygen in the water, causing other aquatic organisms to suffocate due to lack of oxygen. Sewage treatment uses microbes to convert harmful materials in sewage into harmless products through processes like activated sludge digestion and anaerobic sedimentation, allowing the treated waste to be safely released into rivers.
This document summarizes nitrogen-fixing microorganisms. It discusses how biological nitrogen fixation is carried out by prokaryotes, either symbiotically within plant nodules like Rhizobia bacteria with legumes, or as free-living soil microbes like Azotobacter. A hierarchy of controls on nitrogen fixation is described from the genetic to ecosystem levels. Symbiotic nitrogen fixation provides a source of fixed nitrogen for plants in exchange for carbon from photosynthesis.
The nitrogen cycle describes the natural process by which nitrogen is converted between its various chemical forms and circulated between living organisms and the atmosphere. Nitrogen is essential for building proteins and other organic molecules in living things. It enters ecosystems through nitrogen fixation by bacteria or lightning. Nitrifying bacteria then convert nitrogen into nitrites and nitrates that can be absorbed by plants. Plants and animals incorporate nitrogen into their tissues through consumption or root uptake, and nitrogen returns to the atmosphere through decomposition, denitrification, and other processes. The nitrogen cycle is crucial for supporting life but anthropogenic nitrogen pollution from sources like fossil fuel combustion and fertilizer runoff can disrupt ecosystems.
The document summarizes the nitrogen cycle, which is the process by which nitrogen is converted between various chemical forms through biological and physical processes like fixation, ammonification, nitrification, and denitrification. It discusses how these processes work together in ecosystems and how human activities have significantly impacted the global nitrogen cycle through fossil fuel combustion, fertilizer use, and waste release.
Nitrogen is essential for all life and is required to make proteins, DNA, RNA and other biomolecules. It can be obtained through nitrogen fixation, the process by which atmospheric nitrogen is converted to nitrogen-containing compounds that can be used by plants and other organisms. This process is carried out by bacteria that are able to break the strong triple bond of dinitrogen gas and "fix" it into useable forms like ammonia. Important nitrogen-fixing bacteria include Rhizobium species that form symbiotic root nodules on legumes and blue-green algae. Nitrogen fixation provides the main natural source of nitrogen in ecosystems and is vital for agriculture.
The document discusses the nitrogen cycle, which is the process by which nitrogen is converted between various chemical forms through biological and non-biological processes. It outlines several key microbial nitrogen transformations: nitrogen fixation by bacteria converts atmospheric nitrogen to ammonia; nitrification converts ammonia to nitrites and nitrates; denitrification converts nitrates back to nitrogen gas; and anammox converts nitrites and ammonium directly to nitrogen gas. It also discusses the enzymes, genes and electrons involved in these transformations, as well as deficiency symptoms from a lack of fixed nitrogen.
The document summarizes a study that examined the effect of salt stress on the total lipid composition of two banana varieties: dwarf and tall. The study found that salt stress influenced the lipid composition differently between the two varieties. For the dwarf variety, triglyceride and diglyceride levels were not affected by increasing salt concentration, but monoglycerides and free fatty acids were more influenced. For the tall variety, triglycerides were absent even in control plants not exposed to salt stress, and membrane lipids seemed less affected than in the dwarf variety. The results indicate that the lipid composition of the tall variety is less sensitive to salt stress than the dwarf variety.
The nitrogen cycle describes how nitrogen is converted between its various chemical forms and circulates between the atmosphere, soil, water, and living organisms. It involves five processes: nitrogen fixation, nitrogen assimilation, ammonification, nitrification, and denitrification. Nitrogen fixation converts atmospheric nitrogen to ammonia through bacteria. Assimilation incorporates nitrogen into living tissues. Ammonification and nitrification convert nitrogen waste into plant-usable nitrates. Denitrification returns nitrogen to the atmosphere. Human activities like fertilizer use can disrupt the cycle by adding excess nitrogen.
Nitrogen is an essential element that cycles through various forms in the environment. The nitrogen cycle involves nitrogen fixation, ammonification, nitrification, and denitrification processes carried out by microorganisms. Nitrogen fixation converts atmospheric nitrogen gas into ammonium which can then be used by plants and other organisms. Ammonification and nitrification convert organic nitrogen and ammonium into nitrates. Denitrification returns nitrogen to the atmosphere as nitrogen gas. The nitrogen cycle is crucial for ecosystems as it makes nitrogen available to support primary production.
Nitrogen is essential for plants and animals but cannot be used directly from the atmosphere. Biological nitrogen fixation is the process by which nitrogen-fixing bacteria convert atmospheric nitrogen into ammonia. There are two types of nitrogen-fixing bacteria - symbiotic bacteria that have a mutualistic relationship with plants, and live in root nodules, and asymbiotic bacteria that fix nitrogen independently in soil. The nitrogenase enzyme is key to this process, using iron and molybdenum to catalyze the conversion of nitrogen to ammonia. The fixed nitrogen enters the nitrogen cycle and is eventually assimilated by plants to produce amino acids and proteins.
This document presents an overview of bioremediation and the enzymes used. It discusses how bacteria, fungi, and plant enzymes are involved in biodegrading toxic pollutants. Major enzymes discussed include lignin peroxidase, horseradish peroxidase, and manganese peroxidase. Advantages of bioremediation are that it is relatively inexpensive and doesn't require removing contaminated soil. Limitations include difficulty controlling bacteria and limited effectiveness on non-biodegradable compounds.
The nitrogen cycle involves the transformation of nitrogen between its various chemical forms and exchanges between the atmosphere, soil, plants, and animals. Nitrogen enters the soil through decomposition, is converted to ammonium then nitrates by microbes, taken up by plant roots, and either remains in plant tissue or enters the food chain when consumed by animals. It can return to the atmosphere through denitrification by soil bacteria or industrial fixation through the Haber process. Anthropogenic activities such as agriculture and fossil fuel combustion have significantly impacted the global nitrogen cycle.
This document discusses nitrogen fixation by various organisms. It begins by introducing nitrogen fixation and its importance for plant growth. It then describes different types of nitrogen fixation including industrial, non-biological, and biological fixation. Biological nitrogen fixation is accomplished by nitrogen-fixing bacteria and blue-green algae. These can be free-living or symbiotic, with the latter forming nodules on roots of legumes and some non-legumes to carry out nitrogen fixation. The document concludes by explaining the process of nodule formation in legumes through infection and differentiation of root cells.
The nitrogen cycle describes the movement of nitrogen through the environment. It involves nitrogen fixation by bacteria, ammonification by decomposers, nitrification by soil bacteria, and denitrification by bacteria in waterlogged soils that converts nitrogen back to its gaseous form. Human activities such as fossil fuel combustion, use of nitrogen fertilizers, and livestock ranching have significantly increased the global nitrogen cycle, causing issues like smog, acid rain, eutrophication, and increased greenhouse gas emissions. While some seek solutions, many nations prioritize food production over environmental impacts.
- Harshil Suthar is a student pursuing a F.Y.B.Sc in biotechnology at the government science college.
- The nitrogen cycle is the biogeochemical cycle by which nitrogen is converted between its various chemical forms as it circulates in the ecosystem. Key processes include nitrogen fixation, nitrification, denitrification, and ammonification.
- Nitrogen-fixing bacteria such as Rhizobium and Azotobacter convert atmospheric nitrogen into organic nitrogen compounds that can be used by plants and other organisms.
Nitrogen fixation is the process by which atmospheric nitrogen is converted into nitrogen compounds that can be used by plants and other organisms. There are two main ways this occurs: biologically via certain bacteria, cyanobacteria, and symbiotic relationships with plants; and non-biologically through lightning and cosmic radiation. Biologically, nitrogen-fixing bacteria contain the enzyme nitrogenase, which converts nitrogen gas into ammonia. This process requires significant energy in the form of ATP. Nitrogen fixation is crucial for all life as it makes nitrogen available for use in important compounds like amino acids, proteins, and chlorophyll.
The Deepwater Horizon oil spill in 2010 released 780 million liters of crude oil into the Gulf of Mexico, the largest marine oil spill in history. It impacted wildlife like sea turtles, dolphins, and over 82,000 birds. Bioremediation using indigenous microbes was challenging due to the large scale and deep water conditions. Later efforts using specialized oil-eating microbes and nutrients encapsulated in beeswax balls (PRP) were more effective at degrading the oil while minimizing environmental impacts. Future bioremediation may utilize cotton fibers that can absorb and biodegrade large amounts of oil.
Decomposers such as bacteria and fungi break down dead organic matter and release nutrients back into the soil. Nitrogen is an essential nutrient that is recycled through a nitrogen cycle. This involves nitrogen fixation by bacteria, assimilation by plants, ammonification through decomposition, nitrification by special bacteria, and denitrification which returns nitrogen to the atmosphere. Maintaining this nitrogen cycle is important for supporting new plant growth in ecosystems.
The nitrogen cycle describes the movement of nitrogen through ecosystems. Nitrogen is absorbed by plants from the soil and incorporated into proteins. Animals get nitrogen by eating plant proteins. Bacteria break down nitrogenous waste from dead plants and animals, converting it into ammonium, then nitrites and nitrates, which enrich the soil. Lightning and bacteria also fix atmospheric nitrogen into forms usable by plants.
Lab.10 methods for estimating nitrification processHama Nabaz
ย
Nitrification is the two-step process by which ammonia is oxidized to nitrite and then to nitrate by autotrophic bacteria. In the first step, ammonia is oxidized to nitrite by bacteria like Nitrosomonas. In the second step, nitrite is oxidized to nitrate by bacteria like Nitrobacter. This process occurs in aerobic environments in soil and water and makes nitrogen available to plants. The summary demonstrates the key steps in nitrification and the bacteria involved in converting ammonia to nitrates through nitrites in two steps.
Sewage contains organic waste that provides food for bacteria. The bacteria multiply and consume oxygen in the water, causing other aquatic organisms to suffocate due to lack of oxygen. Sewage treatment uses microbes to convert harmful materials in sewage into harmless products through processes like activated sludge digestion and anaerobic sedimentation, allowing the treated waste to be safely released into rivers.
This document summarizes nitrogen-fixing microorganisms. It discusses how biological nitrogen fixation is carried out by prokaryotes, either symbiotically within plant nodules like Rhizobia bacteria with legumes, or as free-living soil microbes like Azotobacter. A hierarchy of controls on nitrogen fixation is described from the genetic to ecosystem levels. Symbiotic nitrogen fixation provides a source of fixed nitrogen for plants in exchange for carbon from photosynthesis.
The nitrogen cycle describes the natural process by which nitrogen is converted between its various chemical forms and circulated between living organisms and the atmosphere. Nitrogen is essential for building proteins and other organic molecules in living things. It enters ecosystems through nitrogen fixation by bacteria or lightning. Nitrifying bacteria then convert nitrogen into nitrites and nitrates that can be absorbed by plants. Plants and animals incorporate nitrogen into their tissues through consumption or root uptake, and nitrogen returns to the atmosphere through decomposition, denitrification, and other processes. The nitrogen cycle is crucial for supporting life but anthropogenic nitrogen pollution from sources like fossil fuel combustion and fertilizer runoff can disrupt ecosystems.
The document summarizes the nitrogen cycle, which is the process by which nitrogen is converted between various chemical forms through biological and physical processes like fixation, ammonification, nitrification, and denitrification. It discusses how these processes work together in ecosystems and how human activities have significantly impacted the global nitrogen cycle through fossil fuel combustion, fertilizer use, and waste release.
Nitrogen is essential for all life and is required to make proteins, DNA, RNA and other biomolecules. It can be obtained through nitrogen fixation, the process by which atmospheric nitrogen is converted to nitrogen-containing compounds that can be used by plants and other organisms. This process is carried out by bacteria that are able to break the strong triple bond of dinitrogen gas and "fix" it into useable forms like ammonia. Important nitrogen-fixing bacteria include Rhizobium species that form symbiotic root nodules on legumes and blue-green algae. Nitrogen fixation provides the main natural source of nitrogen in ecosystems and is vital for agriculture.
The document discusses the nitrogen cycle, which is the process by which nitrogen is converted between various chemical forms through biological and non-biological processes. It outlines several key microbial nitrogen transformations: nitrogen fixation by bacteria converts atmospheric nitrogen to ammonia; nitrification converts ammonia to nitrites and nitrates; denitrification converts nitrates back to nitrogen gas; and anammox converts nitrites and ammonium directly to nitrogen gas. It also discusses the enzymes, genes and electrons involved in these transformations, as well as deficiency symptoms from a lack of fixed nitrogen.
The document summarizes a study that examined the effect of salt stress on the total lipid composition of two banana varieties: dwarf and tall. The study found that salt stress influenced the lipid composition differently between the two varieties. For the dwarf variety, triglyceride and diglyceride levels were not affected by increasing salt concentration, but monoglycerides and free fatty acids were more influenced. For the tall variety, triglycerides were absent even in control plants not exposed to salt stress, and membrane lipids seemed less affected than in the dwarf variety. The results indicate that the lipid composition of the tall variety is less sensitive to salt stress than the dwarf variety.
The nitrogen cycle describes how nitrogen is converted between its various chemical forms and circulates between the atmosphere, soil, water, and living organisms. It involves five processes: nitrogen fixation, nitrogen assimilation, ammonification, nitrification, and denitrification. Nitrogen fixation converts atmospheric nitrogen to ammonia through bacteria. Assimilation incorporates nitrogen into living tissues. Ammonification and nitrification convert nitrogen waste into plant-usable nitrates. Denitrification returns nitrogen to the atmosphere. Human activities like fertilizer use can disrupt the cycle by adding excess nitrogen.
Nitrogen is an essential element that cycles through various forms in the environment. The nitrogen cycle involves nitrogen fixation, ammonification, nitrification, and denitrification processes carried out by microorganisms. Nitrogen fixation converts atmospheric nitrogen gas into ammonium which can then be used by plants and other organisms. Ammonification and nitrification convert organic nitrogen and ammonium into nitrates. Denitrification returns nitrogen to the atmosphere as nitrogen gas. The nitrogen cycle is crucial for ecosystems as it makes nitrogen available to support primary production.
Nitrogen is essential for plants and animals but cannot be used directly from the atmosphere. Biological nitrogen fixation is the process by which nitrogen-fixing bacteria convert atmospheric nitrogen into ammonia. There are two types of nitrogen-fixing bacteria - symbiotic bacteria that have a mutualistic relationship with plants, and live in root nodules, and asymbiotic bacteria that fix nitrogen independently in soil. The nitrogenase enzyme is key to this process, using iron and molybdenum to catalyze the conversion of nitrogen to ammonia. The fixed nitrogen enters the nitrogen cycle and is eventually assimilated by plants to produce amino acids and proteins.
This document presents an overview of bioremediation and the enzymes used. It discusses how bacteria, fungi, and plant enzymes are involved in biodegrading toxic pollutants. Major enzymes discussed include lignin peroxidase, horseradish peroxidase, and manganese peroxidase. Advantages of bioremediation are that it is relatively inexpensive and doesn't require removing contaminated soil. Limitations include difficulty controlling bacteria and limited effectiveness on non-biodegradable compounds.
The nitrogen cycle involves the transformation of nitrogen between its various chemical forms and exchanges between the atmosphere, soil, plants, and animals. Nitrogen enters the soil through decomposition, is converted to ammonium then nitrates by microbes, taken up by plant roots, and either remains in plant tissue or enters the food chain when consumed by animals. It can return to the atmosphere through denitrification by soil bacteria or industrial fixation through the Haber process. Anthropogenic activities such as agriculture and fossil fuel combustion have significantly impacted the global nitrogen cycle.
This document discusses nitrogen fixation by various organisms. It begins by introducing nitrogen fixation and its importance for plant growth. It then describes different types of nitrogen fixation including industrial, non-biological, and biological fixation. Biological nitrogen fixation is accomplished by nitrogen-fixing bacteria and blue-green algae. These can be free-living or symbiotic, with the latter forming nodules on roots of legumes and some non-legumes to carry out nitrogen fixation. The document concludes by explaining the process of nodule formation in legumes through infection and differentiation of root cells.
The nitrogen cycle describes the movement of nitrogen through the environment. It involves nitrogen fixation by bacteria, ammonification by decomposers, nitrification by soil bacteria, and denitrification by bacteria in waterlogged soils that converts nitrogen back to its gaseous form. Human activities such as fossil fuel combustion, use of nitrogen fertilizers, and livestock ranching have significantly increased the global nitrogen cycle, causing issues like smog, acid rain, eutrophication, and increased greenhouse gas emissions. While some seek solutions, many nations prioritize food production over environmental impacts.
- Harshil Suthar is a student pursuing a F.Y.B.Sc in biotechnology at the government science college.
- The nitrogen cycle is the biogeochemical cycle by which nitrogen is converted between its various chemical forms as it circulates in the ecosystem. Key processes include nitrogen fixation, nitrification, denitrification, and ammonification.
- Nitrogen-fixing bacteria such as Rhizobium and Azotobacter convert atmospheric nitrogen into organic nitrogen compounds that can be used by plants and other organisms.
Nitrogen fixation is the process by which atmospheric nitrogen is converted into nitrogen compounds that can be used by plants and other organisms. There are two main ways this occurs: biologically via certain bacteria, cyanobacteria, and symbiotic relationships with plants; and non-biologically through lightning and cosmic radiation. Biologically, nitrogen-fixing bacteria contain the enzyme nitrogenase, which converts nitrogen gas into ammonia. This process requires significant energy in the form of ATP. Nitrogen fixation is crucial for all life as it makes nitrogen available for use in important compounds like amino acids, proteins, and chlorophyll.
The Deepwater Horizon oil spill in 2010 released 780 million liters of crude oil into the Gulf of Mexico, the largest marine oil spill in history. It impacted wildlife like sea turtles, dolphins, and over 82,000 birds. Bioremediation using indigenous microbes was challenging due to the large scale and deep water conditions. Later efforts using specialized oil-eating microbes and nutrients encapsulated in beeswax balls (PRP) were more effective at degrading the oil while minimizing environmental impacts. Future bioremediation may utilize cotton fibers that can absorb and biodegrade large amounts of oil.
Petroleum Microbiology is a state-of-the-art presentation of the specific microbes that inhabit oil reservoirs, with an emphasis on the ecological significance of anaerobic microorganisms. An intriguing introduction to extremophilic microbes, the book considers the various beneficial and detrimental effects of bacteria and archaea indigenous to the oil field environment. Presenting fundamental and applied biological approaches, the book serves as an invaluable reference source for petroleum engineers, remediation professionals, and field researchers.
This document discusses bioremediation of oil spills. It defines bioremediation as using microbes to clean up contaminated soil and water. There are two main types of bioremediation for oil spills - bioaugmentation, which adds microbes, and biostimulation, which adds nutrients to stimulate existing microbes. While bioremediation is less expensive and more natural than other cleanup methods, it also takes more time to see results. The document examines bioremediation approaches to the infamous Exxon Valdez oil spill.
Improving Oil Recovery through Microbial Enhanced TechniqueModesty Jnr.
ย
Microbial enhanced oil recovery (MEOR) utilizes microorganisms and their byproducts to improve oil extraction from reservoirs. MEOR works by microbes reducing oil viscosity, producing gases like CO2 to displace oil, generating biomass, selectively plugging pores, and secreting biosurfactants. While MEOR offers benefits like being inexpensive and environmentally friendly, challenges include ensuring microbes can survive harsh reservoir conditions and don't damage infrastructure. After nearly a century of research, MEOR has proven effective in some fields but more integrated testing is still needed to fully establish it as a viable recovery method.
Bioremediation uses microorganisms to break down pollutants in the environment. It can be used to clean up oil spills, wastewater, and contaminated soil. Various techniques exist including biostimulation, which adds nutrients to stimulate microbes, and bioaugmentation, which introduces new microbes. Nanoparticles are also being used for nano bioremediation due to their large surface area and ability to penetrate contaminated areas. The document discusses using bacteria, fungi, and genetically engineered organisms to degrade pollutants and discusses turning waste into bioplastics or other materials through bioremediation techniques.
This document discusses bioremediation of BTEX (benzene, toluene, ethylbenzene, and xylenes) compounds. It provides background on what BTEX are, how they enter the environment, their health effects, and what bioremediation is. It then describes different bioremediation techniques for BTEX including in situ bioremediation approaches like intrinsic and engineered bioremediation. Key factors that affect bioremediation success like nutrients, moisture, temperature, and electron acceptors are explained. Advantages and disadvantages of in situ bioremediation are summarized. The role of different microbes and electron acceptors in the biodegradation process is also outlined.
Biosurfactants: An Environmentally Friendly Solution for Oil SpillsZaighamKamal
ย
Can biosurfactants increase microbiological oil degradation in North Sea seawater? An international research team has been exploring this question and the results have revealed the potential for a more effective and environmentally friendly oil spill response.
This paper provides an overview of oil spills, their causes and environmental effects. It discusses how oil spills occur mainly as a result of human activities like oil exploration and transport. The paper outlines several methods used to control oil spills, such as using oil booms, sorbents, and dispersal agents to clean up affected areas. It also discusses the environmental and economic impacts of oil spills, which can be devastating and take a long time to remediate.
BIOREMEDIATION 2 Bio mod how to make bio modAniket789077
ย
Bioremediation uses microorganisms like bacteria and fungi to break down oil spills and other hydrocarbon pollutants in the environment. Oil spills release liquid petroleum into the marine ecosystem and cause harm by coating and poisoning animals. Bioremediation works by harnessing microbes like Alcanivorax borkumensis that produce enzymes to consume and break down crude oil molecules into carbon dioxide and water. While bioremediation can help degrade pollutants, it also has disadvantages like being a slow process and requiring careful monitoring.
Bioremediation of Aquifers and Marine Oil SpillsAsma Hossain
ย
This document discusses bioremediation techniques for cleaning up aquifers and marine oil spills. It defines bioremediation and oil spills, describes causes and impacts of spills. Techniques discussed include using nutrient enrichment or microorganisms like Alcanivorax borkumensis bacteria to break down oil, and developing "superbugs" with multiple degradation gene plasmids. While bioremediation is more natural and cost effective than physical/chemical methods, it works slowly and requires site-specific approaches.
ABSTRACT
INTRODUCTION
METHODOLOGY
BIOREMEDIATION OF OIL SPILLS
CASE STUDY
CONCLUSION
Subtopics
Bio remediation in hot and cold environments
Use of Nitrogen fixing Bacteria
Bio remediation using fungi from soil samples
Bio remediation using bacteria and case studies
Microbial bioremediation uses microorganisms to remove or prevent environmental pollution by degrading organic pollutants. There are different types of bioremediation including biostimulation, bioaugmentation, and intrinsic bioremediation. Bioremediation involves interactions between organisms, pollutants, and environments. Various bacteria and fungi can be used to degrade pollutants through aerobic or anaerobic metabolic pathways. Bioremediation can occur insitu or ex situ and involves degradation, detoxification, or immobilization of pollutants like heavy metals, hydrocarbons, and industrial wastes.
Importance of biosurfactant production in removal of oilP.A Anaharaman
ย
Pollution from oil spills harms the environment and is difficult to clean up. Biosurfactants, which are compounds produced by microbes, can help remediate oil spills by emulsifying oil and increasing the surface area that microbes can use to degrade oil. However, biosurfactants are currently not widely used for oil spill cleanup due to their relatively high production costs compared to synthetic surfactants. Research is ongoing to develop cheaper production methods to make biosurfactant use more economically viable for large-scale oil spill remediation.
This document discusses the potential of algae as a biofuel feedstock. It describes how algae can be grown through open pond systems or photobioreactors, then harvested and processed to extract oil. The oil can then be converted into biodiesel. Algae has advantages over petroleum and other biofuel feedstocks in that it is carbon neutral, does not require arable land, and can be harvested multiple times per year, making it a more efficient producer of oil. While challenges remain in making algae biofuels cost competitive, researchers are working to develop faster growing and higher oil producing algae strains through genetic engineering to improve the viability of algae as a sustainable transportation fuel alternative.
Oil Spill Eater II one step bioremediation cleaning process 2019Angus Macdonald
ย
Oil Spill Eater II (OSE II), is the worldโs most environmentally safe & cost-effective bioremediation product, for the mitigation of hazardous waste, spills & contamination.
OSE II is an environmentally safe clean-up method because it uses natureโs own bioremediation process to effectively eliminate hazardous materials.
OSE II is not a bacteria (bug), fertilizer or dispersant product. It is a biological enzyme that converts the waste into a natural food source for the native bacteria found in the environment. The end result is only CO2 and water.
OSE II will reduce clean-up costs and permanently eliminate the hazardous waste problem with no secondary clean-up required.
This document summarizes a study on microbial enhanced oil recovery using Clostridium tyrobutyricum bacteria. The study investigated how the bacteria survives and functions at different salinities, produces metabolites, modifies chalk porosity, and impacts oil recovery. Key findings include: (1) the bacteria can produce metabolites for oil recovery and survive up to 100 g/L salinity but metabolism decreases with increasing salinity; (2) gas production includes CO2 and H2 decreasing with salinity; (3) chalk porosity increases over time likely due to acid dissolution; (4) over 30% residual oil was recovered from sandstone columns after microbial treatment.
This document discusses various topics in geomicrobiology including extremophiles, exomicrobiology, applications like ore leaching and microbial enhanced oil recovery, and techniques of bioleaching. It also discusses how microbes are being studied in space using facilities like BIOPAN and EXPOSE. Microbial fuel cells and closed loop life support systems like MELiSSA that use microbes are also summarized.
Biotechnology in Industrial Waste water Treatmentshuaibumusa2012
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3. MICROBES
๏ข 3.5 billion years ago, micro organisms have evolved
which can use carbon compounds as food.
๏ข And HC are also essentially, chains of hydrogen and
CARBON.
๏ข Many bacterias can digest crude oil.
5. OIL EATERS
๏ข Oil eater microbes (OEM) are very useful in various
steps of different petroleum activities.
๏ข Eg. Exploration, EOR, well to well correlations ,for oil
spill cleaning , etc.
6. HOW IT WORKS
๏ข Oil eaters bacterias or microbes EAT the oil.
๏ข They converts oil into surfactants.
๏ข And releases the water , carboxylic acids and carbon
dioxide.(not harmful to ocean's plants and animals)
7. USES/APPLICATIONS
๏ข 1. In enhanced oil recoveries
๏ข 2. To clean the oil spills
๏ข 3. In modern oil exploration works.
8. EOR
๏ข Microbes digests the oil and release the surfactants, (and
reduces viscocity of oil and IFT between oil and
brine.(microbial E.O.R.))
9. OIL SPILLS
๏ข Oil eaters Microbes can eat almost all oil spilled.
๏ข Special kind of adsorbers are prepared by immersing
adsorber material in OEM solution before using it for oil
clean ups.
๏ข Adsorber material adsorb all spilled oil and OEM convert
that adsorbed oil into non toxic surfactants and release them.
10. EXAMPLE
Deep water horizon oil spill, mexico.
After spill,They released adsorber substance in spilled oil(
called ,SOT which has oil eaters and oil adsorbers in it.)
So, by putting SOT in spilled oil,oil adsorbers adsorb oil
and get heavier than initial one,and settled down in sea.
Following action were taken by oil eaters.(so,that marine
life is not affected by oil.)
11.
12. BIOREMEDIATION
๏ข Bioremediation is use of naturally occurring or
introduced micro organisms or other forms of life to
consume or break down environment pollution in order
to clean up the polluted area
๏ข (Collins , english dictionary 2015)
13. ๏ข 2 ways of bioremediation
๏ข Add nutrients to already exiting OEM (in their own
environment) for their further growth
๏ข Or
๏ข Introduce OEM from outside and feed nutrients to
them.
14. EXPLORATION
๏ข Oil eaters microbes are generally found nearby oil
places.(nearby petrol pumps also)
๏ข So,presence of oil eaters bacterias in core, or formation
indicates that there might be oil in nearby areas.
16. EXPLORATION
๏ข Oil eaters bacterias and oil quantity inside plants tissues
indicates that, there were oil spill happened in that or
nearby area.
๏ข (eg. Mexico's after oil spill study )
17. ๏ข In soil nearby seabed, certain type of bacteria can
indicate the presence of hydrocarbons.
18. ADVANTAGES
๏ข Low cost
๏ข No need of complex technology.
๏ข Do not involve any type of chemical compounds
injection.
๏ข It is mostly non hazardous process for environment.
22. We interested in three groups of bacteria.
1.Bacteria that eat hydrocarbons and breathe with oxygen.
(where oxygenated water comes into contact with the
hydrocarbons.(aerobic environment))
2.Bacteria that eat hydrocarbons but breathe with alternative
electron acceptors like sulphate.( typically found a little bit
deeper in the sediment where there is no longer any
oxygen.(anaerobic environment))
Thirdly, we are interested in a group of bacteria that can only
grow at specific high temperatures โ โthermophilesโ.
23. ๏ข Can it directly save offshore operators money ?
๏ข If microbiological assays can help companies avoid
drilling a dry hole โ then based on the cost per hole, there
are millions to billions in cost savings.
24. REFERENCE
๏ข Casey Hubert interview ,the University of Calgary,canada.
๏ข Research papers (microbes fact sheets ).
๏ข Taylorscinecegeeks(
http://taylorsciencegeeks.weebly.com/blog/oil-eating-
bacteria-new-technology-using-microorganisms).
๏ข Oil spill and their remedies.
๏ข Microbial application in EOR process.
๏ข Collins , english dictionary (2015).
๏ข Gulf of mexico,oil spill.
๏ข Youtube.
๏ข Google.
๏ข Wikipedia.