The Nitrogen Cycle By: Rachel Brewer Kaci Kelley-Brown Jennifer Moats

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Presentation transcript:

The Nitrogen Cycle By: Rachel Brewer Kaci Kelley-Brown Jennifer Moats Dolleen Wiltgen

What is nitrogen?

Nitrogen is in the Nonmetals/BCNO Group Periodic Table

Where is nitrogen found in the environment?

The largest single source of nitrogen is in the atmosphere. Nitrogen makes up 78% of our air!

What happens to atmospheric nitrogen (N2) in the nitrogen cycle?

Atmospheric nitrogen is converted to ammonia or nitrates. Atmospheric Nitrogen (N2) N N Nitrates (NO3) Nitrogen combines with Oxygen to make Nitrates Ammonia (NH3) Nitrogen combines with Hydrogen to make Ammonia

Why does atmospheric nitrogen need to be converted?

It is one of nature’s great ironies… Nitrogen is an essential component of DNA, RNA, and proteins—the building blocks of life. Although the majority of the air we breathe is nitrogen, most living organisms are unable to use nitrogen as it exists in the atmosphere!

How does atmospheric nitrogen get changed into a form that can be used by most living organisms?

By traveling through one of the four processes in the Nitrogen Cycle! (1) Nitrogen Fixation (4) Denitrification Nitrogen Cycle (3) Nitrification (2) Ammonification

The first process in the nitrogen cycle is… Nitrogen Fixation!

What is “nitrogen fixation” and what does it mean to say nitrogen gets “fixed”?

“Nitrogen Fixation” is the process that causes the strong two-atom nitrogen molecules found in the atmosphere to break apart so they can combine with other atoms. Nitrogen gets “fixed” when it is combined with oxygen or hydrogen. N N Oxygen Hydrogen Hydrogen N N N N Oxygen

There are three ways that nitrogen gets “fixed”! (a) Atmospheric Fixation (b) Industrial Fixation (c) Biological Fixation Bacteria

Lightning “fixes” Nitrogen! Atmospheric Fixation (Only 5 to 8% of the Fixation Process) The enormous energy of lightning breaks nitrogen molecules apart and enables the nitrogen atoms to combine with oxygen forming nitrogen oxides (N2O). Nitrogen oxides dissolve in rain, forming nitrates. Nitrates (NO3) are carried to the ground with the rain. N N O Nitrogen combines with Oxygen Nitrogen oxides forms (N2O) Nitrogen oxides dissolve in rain and change to nitrates (NO3) Plants use nitrates to grow!

N N H Industrial Fixation Under great pressure, at a temperature of 600 degrees Celcius, and with the use of a catalyst, atmospheric nitrogen (N2) and hydrogen are combined to form ammonia (NH3). Ammonia can be used as a fertilizer. N H3 Industrial Plant combines nitrogen and hydrogen Ammonia is formed (NH3) Ammonia is used a fertilizer in soil

Symbiotic Relationship Bacteria Biological Fixation (where MOST nitrogen fixing is completed) There are two types of “Nitrogen Fixing Bacteria” Free Living Bacteria (“fixes” 30% of N2) Symbiotic Relationship Bacteria (“fixes” 70% of N2)

Free Living Bacteria Highly specialized bacteria live in the soil and have the ability to combine atmospheric nitrogen with hydrogen to make ammonia (NH3). N N H N H3 Free-living bacteria live in soil and combine atmospheric nitrogen with hydrogen (NH3) Nitrogen changes into ammonia Bacteria

Symbiotic Relationship Bacteria Bacteria live in the roots of legume family plants and provide the plants with ammonia (NH3) in exchange for the plant’s carbon and a protected home. Legume plants N NH3 N Roots with nodules where bacteria live Nitrogen changes into ammonia.

Most atmospheric nitrogen (N2) is “fixed” and changed to ammonia (NH3) Most atmospheric nitrogen (N2) is “fixed” and changed to ammonia (NH3). Ammonia is highly toxic to many organisms. Can plants use ammonia?

Very few plants can use ammonia (NH3)… …but, fortunately the second process Ammonification can help! (1) Nitrogen Fixation (2) Ammonification

What is ammonification?

Ammonification: Bacteria decomposers break down amino acids from dead animals and wastes into nitrogen ammonium. Bacteria decomposers break down amino acids into ammonium

Why is ammonification necessary?

Because plants cannot use the organic forms of nitrogen that are in the soil as a result of: (1) wastes (manure and sewage) (2) compost and decomposing roots and leaves

How does ammonification occur?

Microorganisms convert the organic nitrogen to ammonium Microorganisms convert the organic nitrogen to ammonium. The ammonium is either taken up by the plants (only in a few types of plants) or is absorbed into the soil particles. Ammonium (NH4) in the soil is stored up to later be changed into inorganic nitrogen, the kind of nitrogen that most plants can use. Bacteria converts organic nitrogen to ammonium (NH4) Ammonium (NH4) is used by some plants Bacteria Ammonium (NH4) is stored in soil.

What happens to ammonium (NH4) stored in the soil?

It travels through the third process of the nitrogen cycle called Nitrification! (1) Nitrogen Fixation (3) Nitrification (2) Ammonification

First we will quickly “run through” a general overview of the Nitrification Process

Nitrifying bacteria in the ground first combine ammonia with oxygen to form nitrites. Then another group of nitrifying bacteria convert nitrites to nitrates which green plants can absorb and use! Nitrifying bacteria in soil combine ammonia with oxygen Ammonia changes to nitrites Nitrifying bacteria in soil convert nitrites to nitrates Ammonia Nitrites Nitrates Plants absorb nitrates and grow! (NH3) (NO2) (NO3)

Now we will take a “closer look” at the Nitrification Process

Nitrification is a biological process during which nitrifying bacteria convert toxic ammonia to less harmful nitrate. Nitrification aids in the decomposition of nitrogenous material and thus in the recycling of nitrogen atoms since the decontamination of organic nitrogen produces ammonia that is subsequently oxidized to nitrate by nitrification. There two bacterial species involved. Nitrosomonas sp. Bacteria oxidize ammonia into nitrite, while Nitrobacter bacteria convert nitrite to nitrate, with both species utilizing the energy released by the reactions. Ammonia can be used by some plants. Most nitrogen taken up by plants is converted by chemoautotrophic bacteria from ammonia, which is highly toxic to many organisms, first into nitrite (NO2-), and then into nitrate (NO3-). This process is called nitrification, and these bacteria are known as nitrifying bacteria.

Nitrifiers such as Arthrobacter (heterotroph), Aspergilli’s (heterotroph), and Nitrosomonas (autotroph) are delicate organisms and extremely susceptible to a variety of inhibitors. They are extremely slow growing, unlike many bacteria that can double their numbers every hour or so. In order to thrive, nitrifying bacteria need a relatively clean environment with a steady supply of ammonia and oxygen.

Nitrification is a Two Step Process 1. First Step: Ammonium Oxidation The microorganisms involved are called the ammonia oxidizers. Nitrosomonas is the most extensively studied and usually the most numerous in soil. Nitrosospira is an aquatic nitrifier. Nitrosomonas Nitrosospira Nitrosococcus Nitrosolobus Ammonia-Oxidizing Bacteria: These organisms are chemoautotrophs, growing with ammonia as the energy and CO2 as the main carbon source. Species are distributed in a great variety of soils, oceans, brackish environments, rivers, lakes, and sewage disposal systems.

2. Second step: Nitrite Oxidation Microorganism involved: Nitrobacter These bacteria comprise a diverse group of rod, ellipsoidal, spherical, and spiral-shaped cells. At least one strain of Nitrobacter has been described that can grow by anaerobic respiration (denitrification). Nitrite-oxidizing bacteria are found in aerobic, but occasionally also in anaerobic, environments where organic matter is mineralized. They are widely distributed in soils, fresh water, brackish water, seawater, mud layers, sewage disposal systems, and inside stones of historical buildings and rocks. They are also found inside corroded bricks and on concrete surfaces such as in cooling towers and highway-automobile tunnels.

How does nitrogen reenter the atmosphere in the nitrogen cycle?

Through the fourth process called denitrification! (1) Nitrogen Fixation (4) Denitrification (2) Nitrification (3) Ammonification

What does denitrification do?

Denitrification converts nitrates (NO3) in the soil to atmospheric nitrogen (N2) replenishing the atmosphere. Nitrogen in atmosphere (N2) Nitrates (NO3) in Soil

How does the denitrification process work? Nitrates in soil

Denitrifying bacteria live deep in soil and in aquatic sediments where conditions make it difficult for them to get oxygen. The denitrifying bacteria use nitrates as an alternative to oxygen, leaving free nitrogen gas as a byproduct. They close the nitrogen cycle! Nitrogen in atmosphere closes the nitrogen cycle! (N2) (NO3) Denitrifying bacteria live deep in soil and use nitrates as an alternative to oxygen making a byproduct of nitrogen gas.

Other ways that nitrogen returns to the atmosphere… Emissions from industrial combustion and gasoline engines create nitrous oxides gas (N2O). Volcano eruptions emit nitrous oxides gas (N2O).

Ammonia is converted to nitrites and nitrates. (b) N2O (4) Denitrification (1) Nitrogen Fixation (c) Nitrogen Cycle (3) Nitrification (2) Ammonification NO3 NH3 Ammonia is converted to nitrites and nitrates. Organic nitrogen is converted to ammonium. Nitrates in Soil

Ammonia is converted to nitrites and nitrates. (b) N2O (4) _____________ (1) _____________ (c) Nitrogen Cycle (3) ____________ (2) _____________ NO3 NH3 Ammonia is converted to nitrites and nitrates. Organic nitrogen is converted to ammonium. Nitrates in Soil

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