Title: Biodegradation Microbiology
1Biodegradation Microbiology
Biodegradation Microbiology
- Introduction
- Naturally occurring compounds
- Hydrocarbons
- Pesticides
- Insecticides
- Herbicides
- Fungicides
- Use patterns, transport and circulation in
the environment
2Molecular Models
1,4-dichlorobenzene
DNA molecule
P-cresol
Molecular Models
Molecular models of many of the compounds
mentioned in this section are available on the
course website To view these models, you need
to use a plug-in called Chime that can be
downloaded from the MDL Information Systems
website at http//www.mdl.com/d
ownloads/downloadable/index.jsp After
downloading and installing the Chime plug-in, you
can look at three-dimensional representations of
molecules, rotate them freely using the mouse,
change the colour scheme, zoom in and out,
change the view from basic stick
representations to stick and ball, etc. Note
that some of the molecule files are very large
and may cause errors in display on slower
computer systems or slow internet
connections. Also note that when you first
click on the name of molecule from the list, it
may appear as a small window. Click on the
molecule name again and it should appear
full-size.
WebLink
3General Introduction
- Introduction
- Microbial degradation of chemicals in the
environment is an important route for removal. - The types of compounds range from plastics
through organic chemicals (both industrial
chemicals used in large quantities and trace
chemicals such as pesticides) to organometallics
such as methylmercury. - The biodegradation of these compounds is often a
complex series of biochemical reactions and is
often different when different microorganisms are
involved. The particular details of each
biodegradation scheme are not particularly
important, but the general series of reactions
and enzyme types involved are relatively
straightforward. - The biodegradation schemes and pathways for
biodegradation of many chemicals can best be
understood by considering the same pathways for
natural chemicals such as hydrocarbons, lignins,
cellulose and hemicellulose. Many of the
pathways, particularly the later stages of
metabolism, are similar.
4Biodegradation - Definitions
Biodegradation   -   Definitions Overview  Â
Biodegradation is the partial or complete
conversion of the compound of interest to its
elements. It usually mediated by microorganisms
but many macro-organisms can also carry out
biodegradative processes. The term
"biodegradation" is usually applied to compounds
that are xenobiotic - compounds manufactured or
used by humans in the course of their activities
and thereby introduced as a "foreign"Â substance
(xeno foreign) into an environment. It is also
often applied to the study of the
"biodegradation" of naturally occurring compounds
such as lignin or cellulose - typically, in that
case the compounds studied are those that are
more resistant to decomposition. You will see
the terms "biotransformation", "partial
biodegradation" and "complete biodegradation"Â
used in some literature. These terms are used
to distinguish between the complete decomposition
of a compound to its elemental form (complete
biodegradation) and an intermediate stage of
"partial biodegradation" to less complex
molecules. This is somewhat of an artificial
distinction. To restrict the use of the term
"biodegradation" to mean "complete
biodegradation" is too limiting.
"Biotransformation" has also come to mean the
changing of a compound to another reasonably
stable molecule (often one that is useful or one
that is less or more toxic than the original)
5Biodegradation - Interactions
Biodegradation of a given compound is a complex
result of the interacting factors listed in this
diagram. It is a function of the chemical
structure of the compound, the environmental
conditions, the organisms present and their
quantities, the adsorption, release and
solubility of the compound, the general
bioavailability of the compound, interactions
with other compounds present in the environment,
kinetics of growth and metabolism, threshold
effects, co-metabolic processes, acclimation
effects, and others.
6Biodegradation Interactions 2
Biodegradation of a given compound is a complex
result of the interacting factors listed in this
diagram. It is a function of the chemical
structure of the compound, the environmental
conditions, the organisms present and their
quantities, the adsorption, release and
solubility of the compound, the general
bioavailability of the compound, interactions
with other compounds present in the environment,
kinetics of growth and metabolism, threshold
effects, co-metabolic processes, acclimation
effects, and others. Some factors appear in
more than one of these columns since they involve
more than one of the columns (Biological,
Chemical and Environmental) Remember that all of
these features are inter-related and that it is
often impossible to separate them neatly as we
have done here Some of the interacting factors
are summarised in the diagram. Note that these
same features and factors will be used in the
module on Applications/Bioremediation
7Biodegradation - Concepts
- Some of the concepts in the diagram that are
important in looking a biodegradation activities
(and which may not be as familiar to you as the
others) are - Bioavailability
- Toxicity
- Thresholds
- Sorption (see Module on Groundwater)
- Acclimation (see 2,4-D herbicides)
- Recalcitrance (dealt with in this module)
8Lack of Biodegradation
- There can be many reasons why a particular
compound, although biodegradable in testing, is
not biodegraded - Required nutrients are missing
- Environmental conditions are unsuitable
- Toxic substance concentration is too high
- Compound may be at too low a concentration
- Compound may not be bioavailable
9Biodegradation 2
- There can be many reasons why a particular
compound, although biodegradable in testing, is
not biodegraded - Required nutrients are missing
- Environmental conditions are unsuitable
- Toxic substance concentration is too high
- Compound may be at too low a concentration
- Compound may not be bioavailable
- Required nutrients are missing - One or more
nutrients required for growth are missing. The
"limiting" nutrient is the one that is exhausted
first in the growth cycle. This assumes that
growth is required for biodegradation this may
not be true if sufficient biomass is already
present, or if the compound is degraded by
enzymes already present.
10Biodegradation 3
- There can be many reasons why a particular
compound, although biodegradable in testing, is
not biodegraded - Required nutrients are missing
- Environmental conditions are unsuitable
- Toxic substance concentration is too high
- Compound may be at too low a concentration
- Compound may not be bioavailable
- Required nutrients are missing - One or more
nutrients required for growth are missing. The
"limiting" nutrient is the one that is exhausted
first in the growth cycle. This assumes that
growth is required for biodegradation this may
not be true if sufficient biomass is already
present, or if the compound is degraded by
enzymes already present. - Environmental conditions are unsuitable - There
are many environmental conditions that can
inhibit growth or metabolism high or low pH
levels, high or low Eh (redox potentials), high
or low temperatures, etc. A good example is in
some peat bogs where organic materials may be
over 20,000 years old. Â
11Biodegradation 4
- There can be many reasons why a particular
compound, although biodegradable in testing, is
not biodegraded - Required nutrients are missing
- Environmental conditions are unsuitable
- Toxic substance concentration is too high
- Compound may be at too low a concentration
- Compound may not be bioavailable
- Required nutrients are missing - One or more
nutrients required for growth are missing. The
"limiting" nutrient is the one that is exhausted
first in the growth cycle. This assumes that
growth is required for biodegradation this may
not be true if sufficient biomass is already
present, or if the compound is degraded by
enzymes already present. - Environmental conditions are unsuitable - There
are many environmental conditions that can
inhibit growth or metabolism high or low pH
levels, high or low Eh (redox potentials), high
or low temperatures, etc. A good example is in
some peat bogs where organic materials may be
over 20,000 years old. Â - Toxic substance concentration is too high - Some
conditions (high hydrogen sulfide levels, high
acid concentrations, etc. may inhibit growth or
metabolism. - Compound may be at too low a concentration If a
compound is degraded through the growth of
microorganisms on that compound, there will be a
minimum concentration below which growth will not
occur. There will be an even lower concentration
that will not even provide maintenance energy
levels sufficient for the organism.
12Bioavailability
- Bioavailability can be affected by
- Sorption to some solid materials in the
environment (see Groundwater Module) - Presence in a NonAqueous Phase Liquid (NAPL)
- Confinement or entrapment in physical soil or
aquifer matrix - Complexation
- Solubility (often translated to Octanol/Water
Partition Coefficient)
13Octanol-water partition coefficient
Octanol Water Partition Coefficient This measure
is the partition coefficient derived when a
compound is mixed with water and octanol and
allowed to equilibrate. It is supposed to
represent the degree of bioconcentration that
compound would undergo in animal tissues because
octanol is a surrogate for the lipids in animal
tissues. A compound that is very slightly
soluble in water (hydrophobic) is usually soluble
in lipids (or octanol). Compounds soluble in
water (hydrophilic) are not soluble to the same
extent in octanol or lipids.
14Toxicity - Overview
- Toxicity is too large a field to cover adequately
in this course. Briefly, toxicological analyses
attempt to measure the effects of chemicals on
different types of organisms. - The dose-response of chemicals applied to these
organisms is used to calculate a toxicity
concentration that is then applied to regulate
the allowable concentration of that chemical in
the field. - Toxicology tends to be divided into four main
areas - Hazard identification
- Exposure assessment
- Dose-response measurements - Quantitative risk
characterization by estimation. - Risk Assessment is the process of calculating,
by integrating all of the available data from
different sources, the risk that an individual
will develop symptoms by a given time for a
specified set of exposure conditions. The risk is
the probability (from 0 to 1) of this happening
to an individual.
15Toxocity 2
- Some other points
- Toxicologists generally believe there is a
threshold dose below which there are no toxic
effects in any individual in a population. - This is thought to be be true for most biological
effects except carcinogenicity where a single
molecule could in theory cause a deleterious
mutation. The basis for this belief is that are
doses of toxic chemicals where it is impossible
to find differences between treated and untreated
organisms. - Unfortunately, every test has a statistical
"resolving power" or limit of detection based on
the number in the sample population exposed and
the statistical analysis of the results. It also
ignores the effect of a very small dose on
pre-existing toxicity from other chemicals. Even
that small addition may then cause a small
increase in effects.Â
16Thresholds - Overview
- Since many organic pollutants are present only in
very low concentrations in the environments, the
concept that there might be a minimum
concentration below which they would not be
biodegraded is and important and interesting one.
The concept of a threshold concentration that is
below that needed for microorganisms to take in,
assimilate and biodegrade is therefore very
important. - Â Â
17Thresholds 2
- Since many organic pollutants are present only in
very low concentrations in the environments, the
concept that there might be a minimum
concentration below which they would not be
biodegraded is and important and interesting one.
The concept of a threshold concentration that is
below that needed for microorganisms to take in,
assimilate and biodegrade is therefore very
important. - Note Even though the concentrations of compounds
in the field can be low (at the threshold
concentration for biodegradation), they still can
have important effects. Such as - Very low levels of a compound, when applied to
an entire population, may cause significant risk
to some of that population. - Compounds can be bio-concentrated to higher
levels in target organisms and cause effects (see
DDT) - Even at these low concentrations, some compounds
are toxic, especially to aquatic organisms - Some standards for human and ecosystem health
are set very low because the risk analysis
procedures tell us that the risk is only
acceptable at these low acceptable
concentrations. - Â Â
18Naturally occurring materials
Naturally Occurring Compounds
There are some compounds which are
naturally-occurring and are also recalcitrant
they are resistant to biodegradation in the sense
that they are not rapidly degraded in nature.
One of the most important of this group is
lignin. Lignin is a complex polymeric compound in
plants that is degraded only very slowly when it
enters the soil.
19Biodegradation
- Microorganisms respond to the presence of
organic materials by growing rapidly and using
the easily available parts of the organic
material. - Different populations of microorganisms then use
more resistant parts until a recalcitrant or
resistant fraction remains. The order of use is
often - carbohydrates
- proteins
- cellulose and hemicellulose
- lignins and associated compounds.
- There are distinct populations of microorganisms
able to degrade each of these categories of
organic materials. - The environmental conditions play a large role
in determining the speed at which the materials
are used. - The physical form of the materials (finely
divided versus granular, crystalline cellulose
versus amorphous cellulose, etc.) also plays a
large part in determining the rate of reaction.
20Factors
- The most important environmental factors are
- Temperature
- pH
- water content
- oxygen content
- There are therefore three main determinants of
the fate of organic materials added to a soil or
water system - Microbial activities
- Environmental conditions
- Chemical structure of the compound.
- Each of these factors works by affecting the
microbial colonization and breakdown of the
materials. Two examples will be used cellulose
breakdown and lignin breakdown
21Cellulose
- Cellulose breakdown
- Cellulose is a carbohydrate consisting of b 1-4
linked glucose units in a linear chain. It is
degraded by a very wide range of bacteria and
fungi and is degraded under a variety of
different environmental conditions. - Typically bacteria of the genera Streptomyces,
Cytophaga, Cellulomonas, Nocardia, and Vibrio are
involved in cellulose breakdown while Clostridium
is an important anaerobic cellulose degrading
organism. - Some bacteria can degrade it at very high
temperatures (C. thermocellum). - Anaerobic metabolism results in low molecular
weight fatty acids and carbon dioxide while
carbon dioxide is the main metabolite under
aerobic conditions. - Aerobic decomposition is thus more efficient
than anaerobic more cellulose-carbon is
transformed to CO2 and biomass. - Many fungi are also extremely active in
cellulose decomposition Trichoderma, Chaetomium,
Aspergillus, Fusarium, and Phoma are particularly
active in soils.
22Cellulose
- The enzymatic processes are similar in most
microorganisms - extracellular cellulase enzymes are produced.
- There are several different compounds in the
cellulase enzyme system. - The normal cellulase enzyme complex contains
three types of enzymes - a Cl enzyme which acts primarily on native
cellulose and not on partially degraded
cellulose, - a Cx enzyme which acts upon partially degraded
cellulose molecules in two ways the endo 1-4
glucanases break the cellulose internally at
random while the exo 1-4 glucanases attack the
end of the chains resulting in cellobiose
molecules. - The degradation of the cellobiose and other
small fragments is by the enzyme b-glucosidase
that forms glucose from these fragments.
23Lignin
Lignin
- Lignin is a complex polymer found in plants,
especially in woody plants. - It is an amorphous, three-dimensional aromatic
polymer composed of oxyphenylpropane units. - It is formed by polymerization in the plant of
cinnamyl alcohols p-coumaryl alcohoI, coniferyl
alcohol and sinapyl alcohol
24Lignin
There are three main types of lignin, depending
on the type of plant  1. guaiacyl lignin from
conifers, lycopods, horsetails and ferns. Mainly
coniferyl alcohol units with small amounts of
coumaryl and sinapyl alcohol units. Â 2.
guaiacyl-syringyl lignin from dicotyledonous
angiosperms and some gymnosperms. Equal amounts
of coniferyl and sinapyl units with minor amounts
of coumaryl units. Â 3. guaiacyl-syringyl-p-hydr
oxyphenyl lignin in the highly evolved plants and
woody tissues of conifers. Equal amounts of all
three types of units.
25Lignin
- O - (ether links) are very common
- Phenyl-C-C-C structure is common
- Highly aromatic nature of material
- Large number of methoxy groups
- Large number of - O - cross links between
subunits
26Lignin Biodegradation
- Lignin biodegradation
- The lignin molecules are degraded by the
"white-rot fungi" and some bacteria. - There are several hundred species of white rot
fungi including members of the Agaricaceae,
Hydnaceae, Polyporaceae, and the Thelephoraceae. - The white rot basidiomycetes are probably the
most efficient microorganisms at degrading
lignin. The soft rot fungi include Chaetomium
spp., Paecilomyces andAllescheria spp. - Bacteria such as Pseudomonas, Xanthomonas,
Acinetobacter, Bacillus, Arthrobacter,
Micrococcus, Aeromonas, Chromobacterium, and
Flavobacterium, have all been implicated in
lignin breakdown. - Good evidence has been given for Streptomyces,
Bacillus, Nocardia, and Pseudomonas spp. in that
they have released 14CO2 from radiolabelled
lignin molecules.
27Hydrocarbons
Biodegradation
Hydrocarbons
- Importance of hydrocarbon microbiology
- Â
- Oil spill problems (marine and freshwater)
- Degradation of stored oil supplies
- Use of hydrocarbons as carbon source for
microbial food production (?) - Oil prospecting using microbial distributions in
soils and air - Use of bacteria to release oil from oil sands
- Waste disposal - methane production, etc.
- Soil gases and groundwater evolution
28Hydrocarbon Biodegradation 1
Hydrocarbon biodegradation The main types of
hydrocarbons are Alkane C-C single
bond Alkene CC double bond Alkine CC
triple bond Alicyclic Aromatic Complex
Aromatic
29Gas Chromatography
Natural sources of hydrocarbons tend to be
complex mixtures of the different types above.
The particular composition varies so greatly that
it is often possible to analyze a particular
hydrocarbon mixture with such discrimination that
the oil well and certainly the oil field, where
it originated can be identified. This is usually
done by gas chromatographic techniques, yielding
"fingerprints" of the particular oil
Analysis by gas chromatographic techniques are
essentially fractional distillation methods
higher boiling point hydrocarbons are delayed in
the GC column and so elute later in the process.
In other words, different fractions of the oil
"boil off" at different temperatures. This is
the basis of oil refining, where the crude
hydrocarbon is heated and the different
components are collected at different
temperatures. After refining, the gasoline,
diesel fuel, kerosene, etc., have a much less
complex series of different chain lengths of
hydrocarbons. Octane is a component of gasoline
and it is the standard by which the gasoline is
rated - the "octane rating". Diesel fuel is less
volatile (higher chain lengths). The crude
hydrocarbon also contains other components such
as metals (vanadium, nickel) and sulfur as well
as many different aromatic compounds.
30Mechanisms General 1
- Hydrocarbons
- Mechanisms of degradation
- General
- Hydrocarbons are only degraded in water.
- Bacteria and fungi do not grow in hydrocarbons,
they grow on water in or surrounding the
hydrocarbons. - All hydrocarbons are soluble to some extent.
- This is why the process of degradation is able
to start and then continue. Without the presence
of water, oil is not degraded. - Emulsion formation is an important part of
hydrocarbon degradation. There are two kinds of
emulsion - Oil-in-water emulsion are common and occur when
small quantities of oil are present in large
quantities of water. Droplets of oil are
suspended in water.
31Mechanisms General 2
- Water-in-oil emulsion are less common and occur
when large quantities of oil are present in
water. - These are droplets of water suspended in a matrix
of oil. - The damage caused by oil spills in marine or
freshwater systems is usually caused by the
water-in-oil emulsion. - A thick layer of crude oil on the surface of
water will take up about 50 water by weight and
remain a free-flowing, oily liquid. - It can spread over the water surface to form an
oily film and will eventually disperse and be
degraded. - When the water content reaches about 80 by
weight, the consistency of the emulsion changes -
it becomes a thick semi-solid mass with a
grease-like consistency. It is often called
"chocolate mousse" at this stage because of both
its consistency and its brown colour. This
process does not readily occur with fuel oils
such as diesel oil and kerosene, but occurs
easily with light and heavy crude oils - the
usual cargoes of oil tankers.
32Microorganisms
Many types of microorganisms can degrade
hydrocarbons. Bacteria, yeasts, and filamentous
fungi all have taxa that degrade some types of
hydrocarbon molecules. Bacteria - The
heterotrophic bacteria utilize carbon from the
hydrocarbons as a source of carbon and energy for
biomass production. There are many genera of
bacteria which carry out these reactions on
different hydrocarbons. They include Bacillus,
Pseudomonas, Mycobacteria, and actinomycetes
(especially Nocardia spp.) The autotrophic
bacteria Thiobacillus and Desulfovibrio can both
metabolize the sulfur component of crude oil.
Thiobacillus can metabolize S to H2SO4 (sulfuric
acid) and Desulfovibrio metabolizes this under
anaerobic conditions to sulfide. Both sulfide and
sulfuric acid can damage metal containers and
fuel systems. This is not true utilization of
hydrocarbons as carbon sources, but is important
in practical terms any water present in oil
storage tanks may lead to the growth of these
organisms and subsequent damage. Fungi - Many
yeasts are active in soils and water systems in
hydrocarbon degradation, as are some very common
genera of mycelial fungi such as Trichoderma,
Aspergillus and Cladosponum.
33Rates of Biodegradation
None of these microorganisms degrade all of the
possible hydrocarbon molecules at the same rate
if at all. There is a definite preferential use
of certain chain lengths of aliphatic
hydrocarbons and each organism may have a
different spectrum of activity. In general
terms, the utilization of n-alkanes (non-branched
alkane hydrocarbons) is reasonably well
established
Gases
Liquids
Solids
C1 C2 C3 C4 C5 C6 C7 C8 C9 C10 C11 C12 C13 ------
C19 C20 C21C22 C23 C24..
Not susceptible tomicrobial attack
Attacked by manymicroorganisms
Solid at room temperaturenot susceptible to
attack
Methane is attacked only by very specific groups
of bacteria
This means that a crude oil subjected to
microbial action will lose some of the
hydrocarbon chain lengths and retain others it
will be "enriched" in those hydrocarbons not
susceptible to microbial decompositlon.
34Oil releases
The graph below shows how many millions of
gallons of oil each source puts into the oceans
worldwide each year                         Â
                                   Â
Routine Maintenance 137 Million
Gallons Every year, bilge cleaning and other
ship operations release millions of gallons of
oil into navigable waters, in thousands of
discharges of just a few gallons each. 137
million gallons Down the Drain 363 Million
Gallons Used engine oil can end up in waterways.
An average oil change uses five quarts one
change can contaminate a million gallons of fresh
water. Much oil in runoff from land and municipal
and industrial wastes ends up in the oceans. 363
million gallons. Road runoff adds up Every year
oily road runoff from a city of 5 million could
contain as much oil as one large tanker spill
http//www.ddluk.com/oilspillteachers/weblinkInfo.
html
35Oil Releases 2
Up in Smoke 92 Million Gallons Air pollution,
mainly from cars and industry, places hundreds of
tons of hydrocarbons into the oceans each year.
Particles settle, and rain washes hydrocarbons
from the air into the oceans . Offshore
Drilling 15 Million Gallons Offshore oil
production can cause ocean oil pollution, from
spills and operational discharges . Natural
Seeps 62 Million Gallons Some ocean oil
"pollution" is natural. Seepage from the ocean
bottom and eroding sedimentary rocks releases
oil. Big Spills 37 Million Gallons
Only about 5 percent of oil pollution in oceans
is due to major tanker accidents, but one big
spill can disrupt sea and shore life for miles
36Oil Spills
A large recent spill was the deliberate emptying
of 250 million gallons into the Persian Gulf by
the Iraq government. This was in addition to 80
million gallons spilled into the Gulf during the
Iran-Iraq war in 1983
In Module 5- Background Materials -
http//wvlc.uwaterloo.ca/biology447/modules/module
5/5_back1.htm
37Marine Oil Spills
Marine Oil Spills and Remediation of the Exxon
Valdez Oil spillÂ
WebLink
Go to the Exxon Valdez Spill WWW site
to get updates on Cleanup The Exxon Valdez
accident spilled 11,000,000 gallons of crude oil
in Prince William Sound, Alaska on March 24,
1989. About 2.5 billion has been spent by Exxon
plus about 160 million by state and the federal
governments in clean up efforts. Exxon's efforts
were concentrated on beach cleanup and oil
recovery. The Exxon Valdez was only one of
numerous oil spills occurring around the world.Â
Â
38Marine Oil Spills and Remediation of the Exxon
Valdez Oil spillÂ
WebLink
Go to the Exxon Valdez Spill WWW site
to get updates on Cleanup The Exxon Valdez
accident spilled 11,000,000 gallons of crude oil
in Prince William Sound, Alaska on March 24,
1989. About 2.5 billion has been spent by Exxon
plus about 160 million by state and the federal
governments in clean up efforts. Exxon's efforts
were concentrated on beach cleanup and oil
recovery. The Exxon Valdez was only one of
numerous oil spills occurring around the world.Â
Â
- Tanker accidents contribute only about 5 percent
of the total oil entering the seas each year. In
1985 it was 12.5 percent. - The total entering the seas may be as large as
2.5 million gallons per year (U.S. Coast Guard
estimates). - There were 16,000 accidents in 1988 - spilling
four times the amount of the Exxon Valdez oil
spill into US waters. - About 35 of the oil entering the seas each year
comes from normal ballasting and washing
operations of tankers and 36 comes from urban
and industrial run-off.Â
39Fate
What happened to the oil released into the
environment? A 1992 National Oceanic and
Atmospheric Administration (NOAA) study provided
some insight, estimating that the great majority
of the oil either evaporated, dispersed into the
water column or degraded naturally. Cleanup
crews recovered about 14 percent of the oil and
approximately 13 percent sunk to the sea floor.
About 2 percent (some 216,000 gallons) remained
on the beaches
40Exxon Valdez 1997
In 1997, eight years after the oil spill,
villagers from Chenega Bay returned to nearby
beaches to clean some of the most heavily-oiled
sites. The crew of mostly-local residents
applied a chemical agent to the weathered oil at
five sites, along about one-half mile of beach on
LaTouche and Evans islands. They used PES-51, a
citrus-based product from the oil of oranges and
lemons. PES-51 binds to the oil and floats,
allowing both the chemical agent and the oil to
be collected through the use of oil-absorbent
pads. Â
41Exxon Valdez 2001
- The most recent survey of lingering oil was
conducted in the intertidal zone of Prince
William Sound in Summer 2001 by NOAA. The survey
covered roughly 8,000 meters of shoreline.
Ninety-six sites were randomly selected from the
total number of oiled beaches assessed during
previous surveys he survey results indicate a
total area of approximately 20 acres of shoreline
in Prince William Sound are still contaminated
with oil. - Oil was found at 58 percent of the 91 sites
assessed and is estimated to have the linear
equivalent of 5.8 km of contaminated shoreline. - Buried or subsurface oil is of greater concern
than surface oil. - Subsurface oil can remain dormant for many years
before being dispersed and is more liquid, still
toxic, and may become biologically available. - A disturbance event such as burrowing animals or
a severe storm reworks the beach and can
reintroduce unweathered oil into the water. - Results of the 2001 survey showed that the oil
remaining on the surface of beaches in Prince
William Sound is weathered and mostly hardened
into an asphalt-like layer. - The toxic components of this type of surface oil
are not as readily available to biota, although
some softer forms do cause sheens in tide pools.
42Exxon Valdez 1
Whatever else the Exxon Valdez spill did, it led
to a massive cleanup operation and the first
large scale testing of some bioremediation
technologies in a reasonably controlled
experimental environment. Some problems were
that the initial cleanup was by high-pressure hot
water sprays onto the beaches. Very little oil
was actually recovered by the "skimmers" and boom
flotation devices that were used to try to
contain and recover the raw oil. Estimates range
up to a recovery of 5 to 7 of the spilled oil.
Many different treatment systems were tried
ranging from some new low toxicity dispersants to
steam cleaning to addition of fertilizers to
promote bioremediation. The dispersants have to
be applied within the first 36 hours to be
effective at all and they were not used after
that time. The addition of nutrients was tested
to see if they stimulated or promoted
biodegradation of oil on beaches contaminated
with oil. The types of nutrients ranged from
water soluble mixtures (232 NP garden
fertilizer formulation) through slow release
fertilizers (isobutylenediurea) and oleophilic
(oil soluble - Inipol EAP 22 oleic acid, urea,
lauryl phosphate). Each was tested in the
laboratory and in small scale field experiments.
Application rates were adjusted to minimize
eutrophication effects and fish toxicity. The
most effective in the tests was the oleophilic
group. Two (Inipol and Customblen) were
eventually approved for use in the field.
Initial claims were that the beaches were
"significantly cleaner" after application of the
oleophilic fertilizers.Â
Exxon Valdez
 Â
43Exxon Valdez 2
Exxon Valdez Some researchers thought that using
dispersants could transport the oil into deeper
waters and cause more damage to marine organisms.
Another method that was NOT tried at Prince
William Sound, but that is often effective if
used within the first few hours, is burning the
floating oil slick About 90 can be removed by
this method but it causes air pollution. The oil
layer must be more than 3 mm thick and should not
have formed the oil-in-water emulsion that
prevents burning. High wave action promotes
emulsion formation. One of the major problems
with the science at Prince William Sound was that
it was driven by urgency and controlled
experiments were very infrequent. Much of the
data is also sealed - to be used in any upcoming
law suits. Because of this, data of recovery
percentages and sub-lethal toxic effects are
essentially unavailable . The secrecy
surrounding the data even on the extent,
frequency and temperature of water during the hot
water washing sessions makes meaningful
comparisons with other methods very difficult to
carry out. This is coupled with a very low
baseline data level about Prince William Sound in
the first place almost no data on the situation
existing before the spill is available. Only 10
or 12 very short stretches of beach were set
aside to act as control sections. The
scientists from NOAA (National Oceanic and
Atmospheric Administration) had to fight the oil
company and their consultants and operating
cleanup companies as well as the local people to
get even that much.
Biodegradation Scientists from Exxon and the EPA
tried to speed up the natural rates of
biodegradation by hydrocarbon-utilizing bacteria
and yeasts by adding nutrients to the system. The
best that can be said about the results is that
they are still in doubt some scientists say they
achieved an increase (Exxon says 5 to 10 fold,
Ron Atlas and the EPA say about 2 fold) of the
rate of biodegradation and others say the natural
process would have been just as fast.
44Biochemistry 1
There are many different reactions involved with
the degradation of hydrocarbons by
microorganisms. We will deal only with the more
common reaction types. A) Hydroxylation at
C1. B) Hydro-peroxidation C) Dehydrogenation
reactions D) Subterminal reactions
45Biochemistry 2
Note molecular oxygen
46Biochemistry 3
Note No molecular oxygen is required
47Biochemistry 4
Note that the first three processes deal with a
terminal -CH3 group while subterminal oxidation
process "splits" the alkane at a subterminal
site.
Note molecular oxygen is required
48Generalizations
- There are some generalizations that can be made
concerning the biodegradation of aliphatic
hydrocarbons (alkanes, alkenes and alkines
alkynes ). - The chain length has a significant effect on
biodegradability it is almost the same for
alkanes, alkenes and alkines alkynes. Not a
simple relationship to number of carbon atoms. - Aliphatic compounds are more easily degraded with
decreasing saturation and increasing reactivity
Thus - Degradation rates
- Alkines alkenes
alkanes -
- The degree and type of branching in a structure
has a marked effect on the biodegradability of
aliphatic compounds. In general terms, branching
decreases biodegradability. - In aliphatic compounds with very large numbers of
carbons, the presence of branching may bring the
branch chain length down to the number of carbon
atoms which can be degraded this would promote
biodegradability compared to the compound with
the same number of carbon atoms but in a
non-branched linear chain.
Faster than
Faster than
49Aromatic HC
Aromatic hydrocarbons The aromatic ring
structure and the convention for naming various
substituent groups is given below.
If a phenol is considered, then
other compounds with groups at the different
carbon position can be named either by the ortho,
meta, para convention, or by the 1,2- 1,3- and
1,4-, etc. convention. For instance, a
chlorophenol with a chlorine atom at position
number 3 would be 3-chlorophenol or
meta-chlorophenol Benzene itself is quite
susceptible to decomposition in some ecosystems.
50Aromatic - Groups
Adding another substituent group has a
significant effect on the rate of degradation of
the new compound. For example, adding different
substituent groups to benzene (producing mono
substituted benzenes) produces the following
result
Group added to benzene
Persistence in soil.(half-life) - Days
51Phenol Substitution
OH
-Cl -Br Substituent groups
52Summary of Substitution
- Â
- The effects of these substituent groups may be
summarized - Single substituent groups on benzene affect the
degradation in the order (COOH or OH) -gt NH2
-gt OCH3 -gt SO3H -gt NO2 (increasing
persistence). - Meta substitution for halogens on phenol causes
the greatest persistence. - Ortho- and para-substitution of halogens has
less effect. - Increasing amounts of chlorination or
bromination in a molecule increase persistence.
Metabolic pathways for aromatic hydrocarbon
decomposition There are many pathways of
breakdown for aromatic compounds. Many of them
have catechol as a central intermediate.
The next stage is ring fission of catechol,
followed by incorporation into the normal
biochemical pathways of the cell. This can be
by two distinct mechanisms ORTHO or META
cleavage
OH
OH
catechol
53Generalized aromatic metabolism
Generalized aromatic metabolism
54Ortho and Meta pathways
55Dehalogenation
Dehalogenation
- One irnportant mechanism in the breakdown of
many compounds is the removal of the halogen
atoms, which confer much of the resistance to
decomposition of such diverse compounds as the
insecticide DDT, polychlorinated biphenyl (PCB),
pentachlorophenol (PCP), halogenated benzenes
(e.g. hexachlorobenzene), etc. - This is often a process of dehalogenation
involving several mechanisms, by which halogen
atoms are removed from the molecules. - These processes can occur under both anaerobic
(reductive dehalogenation) and aerobic conditions - Some compounds (such as the chlorinated
benzenes) appear to be only dehalogenated under
aerobic conditions, whereas other compounds can
be dehalogenated under either anaerobic or
aerobic conditions. - Yet other compounds (some pesticides and
halogenated 1 and 2 carbon compounds) undergo
only reductive dehalogenation.
56Benzene utilization
Utilization of benzene Surprisingly little
information was available before 1968. Early
observations showed that bacteria grown on
benzene were able to metabolize catechol (see
above). Experiments with Pseudomonas putida by
Gibson and his colleagues showed two routes to
catechol from benzene. Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â
 Â
57Routes from benzene to catechol
Generalized metabolic routes from benzene to
catechol. The enzymes involved have been
extracted from a number of bacteria including
Pseudomonas, Moraxella and Arthrobacter. A three
component enzyme system was found to be
operativeÂ
The conversion from cis-benzenediol to catechol
was by a dehydrogenase enzyme - cisbenzenediol
dehydrogenase - coupled with NAD.
58PAHs
Polyaromatic hydrocarbons
- These compounds are fused ring aromatic
hydrocarbons - common in coal products and coal
byproducts. - They are ubiquitous pollutants in the atmosphere
and are relatively resistant to biodegradation
they can therefore accumulate to substantial
levels in the environment. - Since some of the larger species are
carcinogenic, they can pose a significant health
hazard. - There are more than 70 compounds classed as PAHs
(or Polynuclear Hydrocarbons PNAs) and they have
from 2 to 7 rings. - They have been detected in a wide range of soils
and sediments, including some ancient sediments.
Significant quantities are present in both
industrial and domestic effluents and sometimes
cause problems in waste water treatment. - Another source is from hydrocarbon spills, the
more biodegradable aliphatic and aromatic
fractions are removed leaving the more resistant
fractions these often include PNA's which can
sink to the bottom of water bodies and become
permanent pollutants of oceans, lakes and rivers.
59PAHs (contd)
Polyaromatic hydrocarbons (contd)
- They are produced in large quantities from
coking operations and gasification processes
using coal and from other sources of incomplete
combustion such as automobile exhausts, power
generation plants, refuse burning and industrial
emissions. - They can also have a natural origin in coal
deposits, from natural aromatics such as
terpenes, sterols and quinones from plants which
volatilize and can become condensed to PAHs
(PNAs). - Plant lignins also may become progressively
decomposed to humic substances which can become
larger during maturation of the pest or coal
deposits and can eventually produce PAHs (PNA's) - Several species of bacteria have produced PAHs
in agar devoid of hydrocarbons but containing
glycerol. - Algae can also synthesize PHAs.
-
- In summary, PHAs are mainly of anthropogenic
origin, but also have geological and natural
biological origins.
60Examples of PAHs
Examples of common polyaromatic hydrocarbons
A listing of more than 650 PAHs and their
chemical names, properties and CHIME molecular
diagrams from NIST (Special Publication 922)
61PAH Biodegradation
- Biodegradation of PAH's
- Factors affecting biodegradability include
- The number of fused rings
- Number and position of substituents of the
rings. - Degree of ring saturation.
- In a typical experiment
- There was no significant oxidation of compounds
with more than three rings. Four-membered ring
systems are oxidized at negligible rates.
Five-membered ring systems underwent no
significant oxidation - Naphthalene nuclei with a small alkyl group
(methyl, vinyl or ethyl) were oxidized rapidly
while those with phenyl were extremely resistant.
- A substituent at position 2 allowed faster
oxidation than at position 1 (less steric
hindrance) - Other methyl-substituted ring systems were
oxidized slowly. - Substituted naphthalene with more than 1 methyl
group on one ring had at least a small amount of
oxidation. - Methyl substitution of methyl groups on both
rings led to decreased rates of oxidation. - Increased ring saturation) led to decreased
oxidation. - As long as one aromatic ring was available, some
measurable oxidation rate was achieved. - The perhydro compounds (cis- and trans-decaline,
perhydrophenanthrene, hexahydroindane and
perhydrofluorene) were resistant to
decomposition.
End of Section Continued in Next Module
62Pesticide Biodegradation
Biodegradation - Pesticides
- Pesticides including
- Insecticides
- Herbicides
- Fungicides
- Use patterns, transport and circulation in the
environment
63Overview
The factors that influence biodegradation are the
same for pesticides as for other compounds We
will concentrate on the biochemistry, the
chemical and environmental factors and
recalcitrance in this Module 5 and deal with the
kinetics and other aspects in Module 7.
64Insecticides Chlorinated hydrocarbons
Insecticides Chlorinated hydrocarbons
- DDT and analogues Â
- The outline below gives a general picture of the
many interconversions that DDT can undergo in the
environment. - Many of the analogues of DDT are breakdown
products of the DDT itself. - The main reaction route in microorganisms is
through TDE (DDD) and TDEE. - It is a direct reductive dechlorination process
and is carried out by bacteria in the soil and
water. - Studies on the metabolic fate of the other
products of DDT metabolism are limited. - The importance of DDT is emphasized when
examining the distribution of the material in the
environment.
65DDT Biodegradation
Biodegradation of DDT
dechlorination
dechlorination
66DDT - details
From the University of Minnesota
Biocatalysis/Biodegradation Database -- LINK
67DDT and analogues
Note increasing levels at higher levels in the
food chain - Bioaccumulation
68Cyclodienes
- BHC (lindane) Â
- The gamma isomer of BHC was extensively used as
an insecticide studies on its biodegradation are
limited. It does not accumulate to the same
extent as DDT in animal tissues. - Chlorinated cyclodiene insecticides Â
- These compounds represent one of the more
persistent groups of pesticides. Examples are
aldrin, dieldrin, heptachlor, isodrin and endrin.
Aldrin and dieldrin have been banned in many
jurisdictions and are only used for particular
purposes in many other jurisdictions. - In soil and water, degradation is probably
microbial but very often leads to the formation
of an epoxide ring structure in the molecules. - Â
Aldrin
Dieldrin
Heptachlor
69Cyclodienes
- This is formed from the CHCH group of the least
chlorinated ring. This process of epoxidation
converts aldrin to dieldrin, isodrin to endrin,
and heptachlor to heptachlor epoxide. All the
epoxide forms are more stable than the parent
form. - Â
- Oxidation processes of cyclodiene compounds
yield more stable toxic intermediates - The rates of disappearance of the various
cyclodiene insecticides are as follows on the
next slide
Stable toxic intermediates
70Stable Toxic Intermediates
The so called "stable toxic intermediates" are
not completely inert (as can be seen by their
eventual breakdown by microorganisms).
Heptachlor
Heptachlor epoxide
71Organophosphates
Organophosphorous compounds
The group contains many well known insecticides
such as malathion, parathion, methyl parathion,
mevinphos, sevin, and diazinon. Their persistence
is of a lower order of magnitude than the
organochlorine insecticides above. They are not
particularly persistent pesticides, with half
lives in soils measured in weeks or months.
They are metabolised by many different
microorganisms, particularly members of the
Pseudomonas, Arthrobacter, Streptomyces, and
Thiobacillus genera and by the fungi in the
Trichoderma genus. The formula of the
organophosphorus insecticides is relatively
simple Malathion
Parathion
72Organophosphates
There are many sites of attack for microorganisms
in these molecules. There are therefore many
different possible breakdown patterns. For
example, in malathion, the sites of attack are
marked A,B,C, and D and can be attacked by
phosphatase, mixed function oxidase, and carboxyl
esterase enzymes A phosphatase and
mixed function oxidases B mixed function
oxidase C phosphatase D carboxyl
esterase Many different products can be formed.
It has been shown that autoclaving soil destroys
about 90 of its ability to degrade malathion.
However, a treatment with sterilizing levels of
gamma irradiation does not affect the soils
ability to degrade malathion. It was possible to
extract a fraction of the soil with 0.2N NaOH
that activity degraded malathion. It is therefore
possible that some organic compound in soils is
able to chemically degrade some organophosphorus
insecticides.
methyl parathion
Diazinon
73Carbamates
CarbamatesÂ
- Carbaryl is an example of the carbamate
insecticides. Its formula is - Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â
               - Other examples are 3-keto carbofuran,
carbanolate, propoxur, carbofuran and landrin.
They are moderately persistent insecticides.
Typical mechanisms of biodegradation are by - Ring hydroxylation
- 2) N-methyl hydroxylation
74Insecticides - Summary
Insecticides - Summary
- Insecticides range in persistence from
organophosphates (1 week to 16 months), through
carbamates (2 months to 14 months), to
organochlorines (18 months to 25 years). - In most cases, the persistence can be explained
by the chemical structure and by the degree of
water solubility. - "Stable toxic intermediates" can be produced,
but these are eventually degraded in most cases. - Bioaccumulation can occur with the more lipid
soluble and persistent insecticides such as DDT. - In certain cases, chemical breakdown of the
organophosphorus insecticides is possible
75Herbicides - Phenoxyacetic
Herbicides - Phenoxyalkanoic acids and
derivatives
The three main groups are the phenoxyacetic,
phenoxypropionic, and 4-phenoxybutyric
derivatives. Many of them are the acids of these
groups, but more recently, forms such as esters
and amines are becoming more common. The basic
structure is
Phenoxyacetic group
1 CI 2 CI 2,4-dichlorophenoxyacetic (2,4-D)
3 H Â 1 CI 2 CI 2,4,5-trichlorophenoxyaceti
c acid (92,4,5-T) 3 CI Â 1 CH 2 CI MCPA 3
H
76Herbicides - Phenoxypropionic
Phenoxypropionic group
1 CH3 2 CI mecoprop 3 H Â 1 CI 2 CI
2(2,4,5-trichlorphenoxy) propionic acid -
silvex 3 CI
77Herbicides - Phenoxybutyric
Phenoxybutyric group
1 CH3 2 CI MCPB (4-(2-methyl-4-chloro-phenoxy)
butyric acid 3 H Â 1 CI 2 CI
2,4-DB4-(2,4-dichlorophenoxy)butyric acid Â
1 CI 2 CI 2,4,5-DB4-(2,4,5,trichlorophenoxy)
butyric acid 3 CI
78Herbicides - Sesone
A closely related compound to the phenoxy group
Is Sodium 2,4-dichlorophenoxy
ethyl sulfate (Sesone herbicide)
79Herbicides - Degradation of phenoxy-alkanoics
Degradation of Phenoxyalkanoic Herbicides
Plants are able to degrade these herbicides in
their tissues, but the rates of degradation are
very low. The rates of degradation vary
considerably in soils. Most of the available
results are from the phenoxyacetic - particularly
2,4-D itself. The patterns of microbial breakdown
may be summarised as follows 1). 2,4-D is
rapidly degraded in soil. MCPA is more persistent
and 2,4,5-T is even more resistant to
decomposition. 2). Microorganisms in soils can
become "adapted" in two separate ways a). by
enzyme induction b). by selection for
2,4-D-degrading organisms 3). Such adaptation
often leads to the rapid degradation of other
members of the group of phenoxy herbicides. 4).
Many microorganisms can degrade more than one of
the groups. 5). There appear to be two main
pathways of biodegradation a). Via
hydroxyphenoxyacetic acid b). Via phenol
80Herbicides - 2,4-D Biodegradation
2,4-D and MCPA Biodegradation
812,4D Biodegradation
A more complete version of 2,4-D biodegradation
From The University of Minnesota
Biocatalysis/Biodegradation Database
82Herbicides - S-triazine group
- s-triazine group
- The most commonly used a-triazines are the
herbicides atrazine, prometryne, simazine, and
ametryne. They are used in very large quantities
(especially atrazine and simazine) in weed
control in field crops. - Atrazine
2. Simazine - The triazines are moderately persistent in soils
(atrazine about 12 months, simazine about 12-14
months).
83Herbicides - Triazine biodegradation
- General formula for triazine herbicides Â
- Biodegradation of Triazine Herbicides
- Attack can occur at C2 by hydroxylation
- Attack can occur at C4 or C6 by oxidative
removal - Attack by cleavage of triazine ring to produce
straight chain compound. Reaction is slow in
soil.
84Herbicides - Substituted ureas
Substituted ureas
There are many different substituted urea
herbicides being used. Typical examples include
monuron, linuron, diuron, neburon, chlorbromuron,
etc. Most are phenyl substituted ureas
                                        Â
Monuron The phenyl
substituted urea herbicides resist chemical
breakdown in soils and are degraded by
microorganisms. Typical persistence is of the
order of 4-18 months in most soils. Typical
schemes of biodegradation include dealkylation
85Herbicides - Bipyridilium group
Bipyridylium group
- Diquat and paraquat are the most commonly used
bipyridylium herbicides. Â - Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â
     - Diquat dibromide (Reglone)                      Â
                                     Â
86Herbicides - Others
Thiolcarbamates
Typical examples are CDEC, pebulate and
diallate. Vapourisation and biodegradation are
the most significant factors in the losses from
soils. Very little information is available on
the metabolic pathways involved, or on the
products formed.
Chlorinated aliphatic acids
The most important are TCA (trichloracetic acid)
and dalapon (2,2-dichloropropionic acid). The
persistence is of the order of 3 - 6 months.
Microbial decomposition is the most important
factor. Hydrolytic processes are the most common
biodegradative pathways.
Miscellaneous
The other chemicals used as herbicides include
the trifluaralin group, the chloracetamides,
amitrole, phenyl, carbamates, and
pentachlorophenol.
87Fungicides - Aliphatics
Fungicides - Aliphatic compounds
These compounds (carbon disulfide, ethylene,
dibromide, chloropicrin, formaldehyde, allyl
alcohol, etc.) are often used as soil fumigants
to kill fungi and nematodes. They are degraded
at various rates by the microorganisms in soil.
Chloropicrin and allyl alcohol are probably the
most persistent. They are often degraded by soil
fungi, even though they are fungicidal!
Quinones - dichlone
Chloranil and dichlone are effective fungicides.
They are SH enzyme inhibitors and are usually
degraded by hydrolysis.
88Fungicides - Thiocarbamates
ThiolcarbamatesÂ
These compounds are very common fungicides
(thiram, zineb, ferbam and vapam) and are broken
down in most soils within 2 days to 2 weeks. A
typical formula is that of thiram tetramethyl
thiuram
tetramethyl thiuram
89Fungicides - Phenols
Phenols (dinitrophenol)
The phenols used as fungicides are usually
halogen and nitro derivatives of an aromatic
hydrocarbon. Pentachloronitrobenzene (PCNB) is
an example and is used as a stable soil
fungicide. It is active against a narrow range of
soil fungal plant pathogens. It is not readily
degraded and probably has a half life of 2 to 3
years in soils. Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â Â
                                                 Â
                                         Â