Title: EUTROPHICATION, etc.
1EUTROPHICATION, etc.
- READINGS FREEMAN,
2005 - Chapter 54 Pages
1261-1262
2EUTROPHICATION
- Eutrophication is the accumulation of nutrients
in aquatic ecosystems. - It alters the dynamics of a number of plant,
animal and bacterial populations thus, bringing
about changes in community structure. - It is a form of water pollution and like all
other forms of pollution is the result of human
activities influencing ecological cycles.
3POLLUTION
- Pollution is the contamination of the environment
by humans adding any substance or energy. - Heavy metals, gases, oil, sewage, noise, heat,
radiation and pesticides are common pollutants
that can affect the environment adversely. - A pollutant is any matter or energy introduced by
human activities that produces harmful effects on
resident populations thus altering community
structure.
4Pollutants, Population Dynamics and Community
Structure
- Pollutants may be toxic (effect survival and/or
reproduction of individuals) thus directly affect
population dynamics. - 1. Radioactive Atoms (Radioisotopes)
- .. I131, St90, etc.
- 2. Heavy Metals
- .. Cu, Hg, Pb, etc.
- 3. Man-made Organic Molecules
- .. DDT, PCBs, Dioxin, 2-4-5 T, etc.
5Pollutants, Population Dynamics and Community
Structure
- Pollutants may alter the abiotic environment thus
indirectly affect population dynamics - 1. Increases in Atmospheric Gases
- ozone (smog, uv radiation)
- sulfur dioxide (acid rain)
- CO2 (greenhouse effect)
- ammonia/nitrates (nitrogen
deposition) - 2. Waste Heat (thermal pollution)
- 3. Nutrient Enrichment (eutrophication)
6Trophic Transfer, Biological Magnification and
Toxic Substances I
- The movement on compounds (molecules) through
trophic levels is called trophic transfer. - Toxic substances, like nutrients, can be
transferred through trophic levels. - Substances that can not be metabolized are
particularly suitable for trophic transfer, as
are radioactive atoms.
7Trophic Transfer, Biological Magnification and
Toxic Substances II
- Biological magnification is the increase in
concentration of a substance in successive
members of a food chain. - Toxic substances may accumulate in members of
higher trophic levels as a result of
biomagnification. - Two classic examples of substance that are
biomagnified are 1) Strontium90 and 2) DDT.
8Trophic Transfer and Biological Magnification of
Strontium90 I
- St90 is a radioactive material with a 1/2 life of
28.1 years. - Half life is a measure of how long it will take
for the mass of the substance to decrease over
time. For example, a kilogram of a radioactive
compound with a 1/2 life of 10 years will weigh
one half of a kilogram is left to sit from 1996
to 2006. By 2016, it will weigh one quarter of a
kilogram.
9Trophic Transfer and Biological Magnification of
Strontium90 I
- St90 is a radioactive material with a 1/2 life of
28.1 years. - Half life is a measure of how long it will take
for the mass of the substance to decrease by half.
10Trophic Transfer of Strontium90 in a Canadian
Lake II
The concentration of St90 tends to increase at
successive trophic levels. The lake was thousands
of miles from the South Pacific location of the
nuclear test. The radioactive materials had been
carried by atmospheric circulation.
11Trophic Transfer and Biological Magnification of
Strontium90 III
- The Canadian lake example shows how a radioactive
material is concentrated as it enters a food web.
This is known as biomagnification. - Biomagnification of St90 is due to
- 1) physiological similarity with calcium a
mineral - nutrient retained by plants and
animals - 2) biomass transfer through food chains.
12Trophic Transfer and Biological Magnification of
DDT (I)
- DDT is one of a class of compounds known as
chlorinated hydrocarbons. - Widely used to kill mosquitoes after WWII.
- Widespread use banned in US in 1972.
13Trophic Transfer and Biological Magnification of
DDT (II)
- DDT, like radioactive elements, once released
into the environment may enter meteorological and
ecological cycles that distribute it and
concentrate it to dangerous levels. - Studies show that it can persist in the
environment for 15 to 25 years.
14Trophic Transfer and Biological Magnification of
DDT (III)
- The concentration of DDT tends to increase in
food chain from one trophic level to the next. - Those at the top of the food chain receive the
largest doses. - Biomagnification of DDT is due to
- 1) high solubility in tissue fats low in
water - 2) very low rate of metabolism low loss from
body - 3) biomass transfer from one trophic level to
next.
15Trophic Transfer, Biological Magnification and
Toxic Substances
- Pesticides, PCBs, dioxins, radioisotopes, heavy
metals and similar substances are biomagnified. - As a rule of thumb, their concentration increases
10 fold as biomass is transferred from one
trophic level to the next. - See illustration.
16Pollutants that Act Through the Abiotic
Environment
- There are groups of pollutants that are not
directly toxic as they are emitted into the
abiotic environment but accumulate to such an
extent that they effect community structure. - Examples are
- 1. Increases in Atmospheric Gases
- nitrogen oxides (smog, uv
radiation) - sulfur dioxide (acid rain)
- CO2 (greenhouse effect)
- ammonia/nitrates (nitrogen
deposition) - 2. Waste Heat (thermal pollution)
- 3. Nutrient Enrichment
(eutrophication)
17Nitrogen Oxides and Ozone (I)
- Nitrogen oxides (N2O, NO and NO2) form a major
component of photochemical smog. - When they combine with hydrocarbons in the
presence of sunlight, the result is ozone (O3),
the major component of smog.
18Pollution Sources of Nitrogen Oxides
- Photochemical smog in urban areas is common due
to the fact that vehicles emit both nitrogen
oxides and hydrocarbons. - It is responsible for respiratory problems.
- It is also known to result in damage to crops.
19Global Effects of Nitrous Oxide (N2O)
- The concentration of nitrous oxide has been
increasing in the atmosphere for the last 30-40
years at a rate of 0.2-0.3 per year. - It absorbs infrared radiation (heat) thus,
contributes to global warming. - In the stratosphere, it reacts with ozone in the
stratosphere and thus contributes to ozone
depletion. Thus, allowing increased ultraviolet
radiation to reach the earth.
20Sulfur Dioxide and Acid Rain
- Sulfur dioxide (SO2) is a colorless gas produced
by combustion of fossil fuels at power plants and
certain industrial sources. - It along with nitrogen oxides results in acid
rain. - The impact of acid rain in Europe has been sever
and is most noticed in forests of the
northeastern US.
21Other Pollutants that Act Through the Atmosphere
- The increased use of fossil fuels has resulted in
an increase in CO2, a greenhouse gas. Its effects
will be discussed in the lecture on climate
change. - Increases in atmospheric ammonia and nitrate find
their way into the rain that hits the earth. The
potential effects of nitrogen deposition on
natural ecosystems will be discussed in lecture
in two weeks.
22Acid Rain
- Sulfuric and nitric acids formed in cloud
droplets can give extremely low pH. - Water collected at the base of clouds in eastern
US have been as low as 2.6 - In L.A, values as low as 2 have been recorded-the
acidity of lemon juice.
23Thermal Pollution
- Many industries take water from a lake, stream or
inlet and use it to cool equipment or products. - Often this increases the temperature of the water
so that it kills fish or stimulates algal growth.
The result is eutrophication. - Sometimes this increase in productivity is
beneficial.
24EUTROPHICATION
- The nutrient enrichment of an aquatic ecosystem.
- Natural Eutrophication -- a process that occurs
as a lake or river ages over a period of hundreds
or thousands of years. - Cultural Eutrophication -- a process that occurs
when humans release excessive amounts of
nutrients it shortens the rate of aging to
decades.
25Natural Eutrophication
- Lake classification based on
- nutrient content and production
- of organic matter. Oligo- nutrient
- poor meso- middle nutrient
- eu- nutrient rich.
26Cultural Eutrophication
- The addition of excess nutrients from a variety
of sources results in the rapid aging of aquatic
ecosystems. - During this process the species composition of
the aquatic community changes.
27Water Chemistry and Eutrophication (I)
- Eutrophication brings about changes in water
chemistry. - These include
- pH
- Dissolved O2
- CO2
- Ammonia
- Nitrates/Nitrites
- Phosphates
28Water Chemistry and Eutrophication (II)
- pH -- The pH of water reflects the CO2 contents
as well as the presence of organic and inorganic
acids. Values below 5 and above 9 are definitely
harmful to fish and limit growth of algal and
invertebrate populations. - Dissolved O2 -- The amount of dissolved oxygen in
water varies with temperature and pressure high
temperature or pressure, low oxygen. Most
invertebrates die if oxygen levels fall below 4-5
mg/l for extended periods of time. Game fish
(bass, perch, trout, etc) require oxygen to be in
the range of 8-15 mg/l.
29Water Chemistry and Eutrophication (III)
- CO2 -- Carbon dioxide is largely a product of
aerobic and anaerobic decomposition of organic
matter. It reacts with water to form carbonic
acid. Normal concentrations are usually less than
1 mg/l. Fish are affected at higher levels and
continued exposure to 10mg/l or more is fatal to
many species. - Phosphates -- Present in low quantities in
natural waters less than 0.01 mg/l. Released
during decomposition. High levels stimulate algal
blooms.
30Water Chemistry and Eutrophication (IV)
- Ammonia (NH3 or NH4) -- Ammonia is a product of
decomposition of animal and plant protein. It is
an important plant nutrient. Natural bodies of
water contain gt 1 mg/l. Levels higher than this
stimulate algal growth and are toxic to fish. - Nitrates/Nitrites -- These N containing compounds
are formed during decomposition and are
inter-converted by certain species of bacteria.
Natural concentrations rarely exceed 10 mg/l and
are often gt 1mg/l.
31Major Sources of Excess Nutrients
- Major sources of excess nutrients are
agricultural fertilizers, domestic sewage and
livestock wastes. - Agricultural fertilizers provide inorganic
nutrients. - Sewage and wastes provide both inorganic and
organic nutrients.
32Overview of Cultural Eutrophication
- Start with clear water stream or blue water lake.
- Introduction of organic and/or inorganic
nutrients. - The pathways of these two nutrient sources
differ. - Follow organic pathway first inorganic nutrient
pathway second.
33Oligotrophic Aquatic Ecosystems
- A clear water stream or deep blue lake contains
enough bacteria to decompose organic material
from organisms that die. - Water is neither acidic or basic.
- Inorganic nutrients are present in low
concentrations. - Ammonia produced by animals and bacteria is taken
up and used for plant growth.
34Excess Organic Matter
- Untreated sewage, manure, paper pulp, packing
plant wastes are sources of excess organic matter
added to aquatic ecosystems. - Results in exponential growth of bacterial
populations. - Bacteria deplete dissolved oxygen in the water.
35Low Oxygen Levels Cause Die-off
- Rapidly growing bacterial populations need
exponentially increasing amounts of oxygen. - Once dissolved oxygen levels become too low, fish
and many freshwater invertebrates die, thus
adding more organic matter.
36Oxygen Depleted Waters
- As oxygen disappears, anaerobic bacteria produce
methane, hydrogen sulfide and ammonia. - Bacterial respiration increases carbonic acid.
- In all but the most oxygen depleted waters,
tubificid worms, midge larvae and mosquito larvae
replace oxygen-loving invertebrates.
37Oxygen Replenishment
- If organic material is not continually added or
the water moves downstream, bacteria eventually
use up their food and populations decline. - The concentration of dissolved oxygen increases,
either through atmospheric replenishment or
increased photosynthesis.
38Recovering Aquatic Ecosystem
- If stocks are available then fish can recolonize
and the stream or lake will recover. - Carp, which tolerate low oxygen levels, do well.
- Oxygen-loving species such as trout, bass and
other game fish may return.
39Recovering Aquatic Ecosystem
- If available freshwater invertebrates recolonize,
then the stream or lake can recover. - Oxygen-loving species such dragonfly, mayfly,
caddis fly, stone fly larvae may return.
40Oligotrophic Aquatic Ecosystems
- A clear water stream or deep blue lake contains
enough bacteria to decompose organic material
from organisms that die. - Water is neither acidic or basic.
- Inorganic nutrients are present in low
concentrations. - Ammonia produced by animals and bacteria is taken
up and used for plant growth.
41Excess Inorganic Nutrients
- Agricultural runoff from fertilizers and effluent
from secondary sewage treatment plants are the
primary sources of inorganic nutrient addition to
aquatic ecosystems. - These sources are rich in nitrogen and phosphorus.
42Nutrients Stimulate Algal Blooms
- Nitrogen and phosphorus from runoff and effluents
or decay of organic matter stimulates aquatic
plant growth. - In particular, algal blooms give the water a
green or blue-green color.
43Plants Die, Bacteria Grow, Deplete Oxygen, Fish
Die
- Plants exhaust nutrients and die.
- Bacteria thrive on organic decay of plants and
lower dissolved oxygen. - Fish and invertebrates die when oxygen gets too
low.
44Oxygen Replenishment and Ecosystem Recovery
- In temperature regions, the growing season ends.
- Bacteria eventually use up their food and
populations decline. - The concentration of dissolved oxygen increases,
either primarily through atmospheric
replenishment. - If stocks are available then fish and
invertebrates can recolonize and the stream or
lake will recover.
45The Good News
- Since the 1970s, many of the worst conditions
that lead to air and water pollution have been
abated. - The last above ground nuclear tests occurred in
China. - The catalytic converters lowered hydrocarbon
emissions, but increased nitrogen oxide
emissions thus requiring new technology. - Some of the worst cases of water pollution have
been addresses and in some cases reversed.
46EUTROPHICATION, etc.
- READINGS FREEMAN,
2005 - Chapter 54 Pages
1261-1262