Soil Pollution
Soil Pollution Introduction:
We can no more manufacture a
soil with a tank of chemicals than we can invent
a rain forest or produce a single bird. We may
enhance the soil by helping its processes along,
but we can never recreate what we destroy. The
soil is a resource for which there is no substitute.
(Environmental historian Donald Worster
reminds us that fertilizers are not a substitute
for fertile soil).
Soil is a thin covering over the land consisting of
a mixture of minerals, organic material, living
organisms, air and water that together support
the growth of plant life. Several factors contribute
to the formation of soil from the parent
material. This includes mechanical weathering
of rocks due to temperature changes and abrasion,
wind, moving water, glaciers, chemical
weathering activities and lichens. Climate and
time are also important in the development of
soils. Extremely dry or cold climates develop soils
very slowly while humid and warm climates develop
them more rapidly. Under ideal climatic
conditions soft parent material may develop into
a centimeter of soil within 15 years. Under poor
climatic conditions a hard parent material may
require hundreds of years to develop into soil.
Mature soils are arranged in a series of zones
called soil horizons. Each horizon has a distinct
texture and composition that varies with different
types of soils. A cross sectional view of the
horizons in a soil is called a soil profile.
The top layer or the surface litter layer called
the O horizon consists mostly of freshly fallen
and partially decomposed leaves, twigs, animal
waste, fungi and other organic materials. Normally
it is brown or black.
The uppermost layer of the soil called the A
horizon consists of partially decomposed organic
matter (humus) and some inorganic mineral
particles. It is usually darker and looser than the
deeper layers. The roots of most plants are found
in these two upper layers. As long as these layers
are anchored by vegetation soil stores water
and releases it in a trickle throughout the
year instead of in a force like a flood. These two
top layers also contain a large amount of bacteria,
fungi, earthworms and other small insects
that form complex food webs in the soil that
help recycle soil nutrients and contribute to soil
fertility.
The B horizon often called the subsoil contains
less organic material and fewer organisms than
the A horizon. The area below the subsoil is
called the C horizon and consists of weathered
parent material. This parent material does not
contain any organic materials. The chemical
composition of the C-horizon helps to determine
the pH of the soil and also influences the soil’s
rate of water absorption and retention.
Soils vary in their content of clay (very fine particles),
silt (fine particles), sand (medium size
particles) and gravel (coarse to very coarse particles).
The relative amounts of the different sizes
and types of mineral particles determine soil
texture. Soils with approximately equal mixtures
of clay, sand, silt and humus are called loams.
Causes of soil degradation
Erosion
Soil erosion can be defined as the movement of
surface litter and topsoil from one place to another.
While erosion is a natural process often
caused by wind and flowing water it is greatly
accelerated by human activities such as farming,
construction, overgrazing by livestock, burning
of grass cover and deforestation.
Loss of the topsoil makes a soil less fertile and
reduces its water holding capacity. The topsoil,
which is washed away, also contributes to water
pollution clogging lakes, increasing turbidity
of the water and also leads to loss of aquatic
life. For one inch of topsoil to be formed it normally
requires 200-1000 years depending upon
the climate and soil type. Thus if the topsoil
erodes faster than it is formed the soil becomes
a non-renewable resource.
Thus it is essential that proper soil conservation
measures are used to minimize the loss of top
soil. There are several techniques that can protect
soil from erosion. Today both water and
soil are conserved through integrated treatment
methods. Some of the most commonly employed
methods include the two types of treatment
that are generally used.
• Area treatment which involves treating the
land
• Drainage line treatment which involves
treating the natural water courses (nalas)
Continuous contour trenches can be used to
enhance infiltration of water reduce the runoff
and check soil erosion.
These are actually
shallow trenches dug across the slope of the
land and along the contour lines basically for
the purpose of soil and water conservation. They
are most effective on gentle slopes and in areas
of low to medium rainfall. These bunds are stabilized
by fast growing tree species and grasses.
In areas of steep slopes where the bunds are
not possible, continuous contour benches (CCBs)
made of stones are used for the same purpose.
Gradonies can also be used to convert wastelands
into agricultural lands. In this narrow
trenches with bunds on the downstream side
are built along contours in the upper reaches of
the catchment to collect run-off and to conserve
moisture from the trees or tree crops. The area
between the two bunds is use for cultivation of
crops after development of fertile soil cover.
Some of the ways in which this can be achieved
are:
Live check dams which barriers created by
planting grass, shrubs and trees across the gullies
can be used for this purpose.
A bund constructed out of stones across the
stream can also be used for conserving soil and
water.
An Earthen checkbund is constructed out of
local soil across the stream to check soil erosion
and flow of water.
A Gabion structure is a bund constructed of
stone and wrapped in galvanized chainlink.
A Gabion structure with ferrocement impervious
barrier has a one inch thick impervious
wall of ferrocement at the center of the structure
which goes below the ground level upto
the hard strata. This ferrocement partition supported
by the gabion portion is able to retain
the water and withstand the force of the runoff
water.
An Underground bandhara is an underground
structure across a nalla bed to function
as a barrier to check the ground water
movement.
Excess use of fertilizers: Approximately 25
percent of the world’s crop yield is estimated to
be directly attributed to the use of chemical fertilizers.
The use of chemical fertilizes has increased
significantly over the last few decades
and is expected to rise even higher. Fertilizers
are very valuable as they replace the soil nutrients
used up by plants. The three primary soil
nutrients often in short supply are potassium,
phosphorus and nitrogen compounds. These are
commonly referred to as macronutrients. Certain
other elements like boron, zinc and manganese
are necessary in extremely small amounts
and are known as micronutrients. When crops
are harvested a large amount of macronutrients
and a small amount of micronutrients are removed
with the crops. If the same crop is grown
again depleted levels of thee nutrients can result
in decreased yields. These necessary nutrients
can be returned to the soil through the
application of fertilizers. In addition to fertilizers
a large amount of pesticides (chemicals used to
kill or control populations of unwanted fungi,
animals or plants often called pests) are also used
to ensure a good yield. Pesticides can be subdivided
into several categories based on the kinds
of organisms they are used to control. Insecticides
are used to control insect populations while
fungicides are used to control unwanted fungal
growth. Mice and rats are killed by rodenticides
while plant pests are controlled by herbicides
Problems with pesticide use
Pesticides not only kill the pests but also a large
variety of living things including humans. They
may be persistent or non-persistent. Persistent
pesticides once applied are effective for a long
time. However as they do not break down easily
they tend to accumulate in the soil and in the
bodies of animals in the food chain.
For example, DDT which was one of the first
synthetic organic insecticide to be used was
thought to be the perfect insecticide.
During the
first ten years of its use (1942-1952) DDT is estimated
to have saved about five million lives
primarily because of its use to control disease
carrying mosquitoes. However after a period of
use many mosquitoes and insects became tolerant
of DDT, thus making it lose its effectiveness.
DDT in temperate regions of the world
has a half life (the amount of time required for
half of the chemical to decompose) of 10 to 15
years. This means that if 100 kilograms of DDT
were to be sprayed over an area, 50 kilograms
would still be present in the area 10 to 15 years
later. The half-life of DDT varies according to
the soil type, temperature, kind of soil organisms
present and other factors. In tropical parts
of the world the half life may be as short as six
months. The use of DDT has been banned in
some countries. India still however permits the
use of DDT though for purposes of mosquito
control only. Persistent pesticides become attached
to small soil particles which are easily
moved by wind and water to different parts thus
affecting soils elsewhere. Persistent pesticides
may also accumulate in the bodies of animals,
and over a period of time increase in concentration
if the animal is unable to flush them out
of its system thus leading to the phenomenon
called bioaccumulation.
When an affected animal
is eaten by another carnivore these pesticides
are further concentrated in the body of
the carnivore. This phenomenon of acquiring
increasing levels of a substance in the bodies of
higher trophic level organisms is known as
biomagnification. This process especially in the
case of insecticides like DDT have been proved
to be disastrous. DDT is a well known case of
biomagnification in ecosystems. DDT interferes
with the production of normal eggshells in birds
making them fragile.
Other problems associated with insecticides is
the ability of insect populations to become resistant
to them thus rendering them useless in a
couple of generations. Most pesticides kill beneficial
as well as pest species. They kill the predator
as well as the parasitic insects that control
the pests. Thus the pest species increase rapidly
following the use of a pesticide as there are no
natural checks to their population growth. The
short term and the long-term health effects to
the persons using the pesticide and the public
that consumes the food grown by using the
pesticides are also major concerns. Exposure to
small quantities of pesticides over several years
can cause mutations, produce cancers, etc.
Thus the question that comes to mind is that if
pesticides have so many drawbacks then why
are they used so extensively and what are the
substitutes for them? There are three main reasons
for the use of pesticides. Firstly the use of
pesticides in the short term has increased the
amount of food that can be grown in many parts
of the world as the damage by pests is decreased.
The second reason for its extensive use
is base on an economic consideration. The increased
yields more than compensates the
farmer for cost of pesticides. Thirdly current
health problems especially in developing countries
due to mosquitoes are impossible to control
without insecticides.
However more and more farmers are increasingly
opting to replace chemical fertilizers and
use different methods of controlling pests without
affecting their yield. Thus several different
approaches that have slightly varying and overlapping
goals have been developed. Alternative
agriculture is the broadest term that is used that
includes all non-traditional agricultural methods
and encompasses sustainable agriculture, organic
agriculture, alternative uses of traditional
crops, alternative methods for raising crops, etc.
Sustainable agriculture advocates the use of
methods to produce adequate safe food in an
economically viable manner while maintaining
the state of the ecosystem. Organic agriculture
advocates avoiding the use of chemical fertilizers
and pesticides. A wide variety of techniques
can be used to reduce this negative impact of
agriculture. Leaving crop residue on the soil and
incorporating it into the soil reduces erosion and
increase soil organic matter. Introduction of organic
matter into the soil also makes compaction
less likely. Crop rotation is an effective way
to enhance soil fertility, reduce erosion and control
pests. There have been arguments both for
and against organic farming. Critics argue that
organic farming cannot produce the amount of
food required for today’s population and it is
economically viable only in certain conditions.
However supporters for organic farming feel
that of the hidden costs of soil erosion and pollution
are taken into account it is a viable approach.
Besides organic farmers do not have to
spend on fertilizers and pesticides and also get
a premium price for their products thus making
it financially viable for them.
Another way to reduce these impacts is through
the use of integrated pest management. This is
a technique that uses a complete understanding
of all ecological aspects of a crop and the
particular pests to which it is susceptible to establish
pest control strategies that uses no or
few pesticides. IPM promotes the use of
biopesticides. Biopesticides are derived from
three sources: microbial, botanical and biochemical.
Microbial pesticides are micro-organisms
such as bacteria, fungus, virus or protozoa
that fight pests through a variety of ways. They
produce toxins specific to the pests and produce
diseases in them. Biochemical pesticides contain
several chemicals that affect the reproductive
and digestive mechanisms of the pests. The most
commonly used biopesticides are Bacillus
thuringiensis (Bt), neem (Azadirachta indica) and
trichogramma. Although they are available in
the market they are yet to become market
favourites.
Excess salts and water
Irrigated lands can produce crop yields much
higher than those that only use rainwater. However
this has its own set of ill effects.
Irrigation
water contains dissolved salts and in dry climates
much of the water in the saline solution evaporates
leaving its salts such as sodium chloride in
the topsoil. The accumulation of these salts is
called salinization, which can stunt plant growth,
lower yields and eventually kill the crop and render
the land useless for agriculture. These salts
can be flushed out of the soil by using more
water. This practice however increases the cost
of crop production and also wastes enormous
amounts of water. Flushing salts can also make
the downstream irrigation water saltier.
Another problem with irrigation is water logging.
This occurs when large amounts of water
is used to leach the salts deeper into the soil.
However if the drainage is poor this water accumulates
underground gradually raising the
water table. The roots of the plants then get
enveloped in this saline water and eventually
die.
Thus in the long run it is better for us to adopt
sustainable farming practices so as to prevent
the degradation of soil.

Leave a Comment