Soil fertility
Testing
Fertile soil is a mixture of well-balanced minerals, high organic matter,
humus, humic, fulvic and carbonic acids having good aeration and a rich
microbial population. Soil fertility is the ability of a soil to sustain plant
growth by providing essential plant nutrients and favorable chemical, physical,
and biological characteristics as a habitat for plant growth. Fertilizers are
chemical or natural substance or material that is used to provide nutrients to
plants, usually via soil, but sometimes to foliage or through water. The main
function provided by a fertile soil is the provision of food and thus have an
economic impact and is related to economic growth and the fight against
poverty.
Soil fertility comprises three interrelated components: physical fertility,
chemical fertility and biological fertility.
Physical fertility is the physical properties and processes of soil that
affect soil fertility by altering water movement through soil, root penetration
of soil and waterlogging. Important physical properties that affect fertility
include soil structure and texture.
Chemical fertility means the presence and concentration of plant
nutrients which include the macronutrients such as nitrogen, phosphorus and
potassium, sulfur, calcium and magnesium and Micronutrients like Iron, cobalt,
selenium, boron, chlorine, copper, iron, manganese, molybdenum and zinc.
Biological fertility includes the organisms that live in the soil, the population of which varies greatly depending upon various environmental conditions and it is highly complex and dynamic. It is the least well-understood fertility component. There may be hundreds of millions to billions of microbes in a single gram of soil. The most numerous microbes in soil are the bacteria, fungi, algae, protozoa and virus.
Soil
organisms improve soil fertility by performing a number of functions such as
releasing nutrients from organic matter, Fixing atmospheric nitrogen,
Increasing phosphorus availability, Degrading pesticides, Controlling pathogens
and improving soil structure. In addition to soil fertility, soil
microorganisms play essential roles in the nutrient cycles that are fundamental
to life on the planet.
Releasing nutrients from organic matter - Soil microorganisms are responsible for most of the nutrient release
from organic matter. When microorganisms decompose organic matter, they use nutrients
in the organic matter for their own growth and release excess nutrients into
the soil and these can be taken up by plants. If the organic matter has a low
nutrient content, then microbes will take nutrients from the soil.
Fixing atmospheric nitrogen
- Nitrogen fixation is a significant source of available nitrogen for plants in
soil. Nitrogen fixing bacteria such as Azotobacter,
Azospirillim, Rhizobia, etc fix nitrogen gas from the atmosphere and make
it available to the plants.
Increasing phosphorus availability
- Phosphate solubilizing bacteria, fungi, Mycorrhiza etc are capable of solubilizing
inorganic phosphorus from insoluble compounds and can increase phosphorus
uptake by the plant. Mycorrhizal fungi can provide phosphorus to plants.
Degrading pesticides - Some
microorganisms are capable of producing enzymes that can break down agricultural
pesticides or other toxic substances added to soil.
Controlling pathogens - Some
microorganisms and soil animals infect plants and thereby decrease plant yield.
There are many microbes in in the soil that can control the spread of
pathogens. For example, some pathogenic fungi in soil destroyed by certain
protozoa, they consume the pathogenic fungi.
Improving soil structure
- Some bacteria and fungi produce substances during organic matter
decomposition that chemically and physically bind soil particles into
micro-aggregates. The hyphal strands of fungi can cross-link soil particles and
maintain aggregates. It is observed that a single gram of soil can contain
several kilometres of fungal hyphae. Soil micro fauna increase pores by tunneling
through the soil thereby improving the soil porosity and they also increase
aggregation by ingesting soil.
Soil microbiology is the study of organisms in soil, their functions and
how they affect soil properties. Soil microorganisms can be classified as
bacteria, actinomycetes, fungi, algae, protozoa and viruses. Each of these
groups has different characteristics that define the organisms and different
functions in the soil it lives in.
Soil testing/soil
analysis/ Soil fertility evaluation
This help one to know
the nutrient supplying power of soil to the crop. Soil testing is used to determine both the
amount of different types of nutrients that is immediately available and that
can become available during the growth of a crop. A complete soil test includes: soil pH,
alkalinity, organic matter, macro elements, microelements, cation exchange
capacity (CEC), and cation saturation. A foliar test includes all the major and
micro elements.
Objectives of soil testing
·
To accurately determine the status of
available nutrients in soils (P, K, Mg, pH, Zn, B)
·
To clearly indicate the seriousness of any
deficiency or excess of any nutrient
·
To form the basis on which fertilizer
needs are determined in such a way to permit an economic evaluation of the
fertilizer recommendation
Techniques commonly employed to assess the soil fertility are
1. Soil testing
2. Analysis of
tissues from plants growing on the particular soil to be analysed
3. Biological
tests in which the growth of higher plants or certain micro-organisms is used
as a measure of soil fertility
4. Nutrient
deficiency symptoms of plants
1.
Soil testing:
Soil testing is
the chemical analysis that provides a guideline for addition of fertilizer to soils. The primary
advantage of soil testing is determining the nutrients status of the soil
before the crop is planted as compared to the plant analysis.
Objectives of Soil
testing
·
Soil fertility evaluation for making
fertilizer recommendation
·
Prediction of likely crop response to
applied nutrients
·
Classification of soil into different
fertility groups for preparing soil fertility maps of a given area
·
Assessment of the type and degree of soil
related problems like salinity, sodicity, acidity etc., and suggesting
appropriate reclamation / amelioration measures
Steps
involved in soil fertility analysis
1. Soil
Sampling
2. Preparation
of samples
3. Analytical
procedure
4. Calibration
and interpretation of the results
5. Fertilizer
recommendation
1.
Sampling:
This is the most
vital step for analysis since a very small fraction of the huge soil mass of a
field is used for analysis and used as an index of the whole area in hectare
basis. So it becomes extremely important to get a truly representative soil
sample from the field. This sample
should be a true representative of the farm/plot/field.
A rough map of the
farm is to be made dividing it into sampling units. A minimum of five to six samples in different zones of the
area being tested is to be obtained. Sample
the soil from the surface to about 15 cm (6 inches) depth with a sampling tube. Any surface organic material has to be removed
from the shovel and then the soil samples are mixed together to create a single
sample.
The best tool is the metal tube called “sampling tube”. If this is not available, cutlass, shovel, hand trowel and auger could be used. Do not use brass, bronze, or galvanized tools because they will contaminate samples with copper and/or zinc.
2.
Preparation of sample:
Drying, grinding
and sieving of the soil sample is done according to the need of analytical
procedure.
3.
Analytical procedure:
All analytical instruments used should be properly calibrated either
using different concentration of standards or with a known concentration of
standard. Spectroscopic methods are used
for analyzing inorganic molecules and chromatographic methods are used for
organic compounds.
A suitable method
is one which satisfies the following three criteria.
·
It should be rapid
· It should give accurate and reproducible
results of a given Samples
·
It should have high predictability
Soil test kit is a
compact soil testing equipment with full complement of devices and reagents for
the determination of the pH, electrical conductivity, nitrogen, phosphorus and
potassium concentration, fertilizer and water. Carbon, which is a good index of
organic content in soil, can also be determined. The equipment is robust and
cost saving in terms of laboratory space.
Chemical
methods used for determination of different nutrients
Analysis of
inorganic compounds
Analysis of anions
Colorimetric techniques
are used for the analysis of Chloride, nitrate, nitrite, sulphate, phosphate,
sulphide and ammoniacal nitrogen.
Generally, an automated spectrophotometer which can perform multi
element analyses are used. There will be
an autosampler, and a system for sequentially adding the appropriate chemicals
to develop the colour, and then colour developed will be read and used to
calculate the analyte concentration. These automated analysers are very
efficient and can run up to two hundred samples per hour.
Analysis of Metals
Metals are usually
measured by Inductively Coupled Plasma, or ICP analysis or by atomic absorption
spectroscopy.
Analysis of Sulphur
compounds
·
Total sulphur can be measured using an
induction furnace, but as sulphur can exist in many forms, it will not give
much information regarding soil fertility
·
Elemental (or free) sulphur is analysed
using a solvent extraction, followed by HPLC
·
Total sulphides can be analysed by acid
digestion and ICP
Analysis of Nitrogenous compounds
·
Nitrate and nitrite will be analysed using
water extract of the soil by colourimetric spectroscopy
·
Ammoniacal nitrogen test include both
ammonia (NH3) and ammonium (NH4), and again is either done on a water extract or distilled as exchangeable ammonia
·
Kjeldahl nitrogen gives measure of the
ammoniacal nitrogen and organic nitrogen, and is analysed by a distillation and
titration method
Analysis of Available Micronutrients
·
DTPA extractable test is done which extract
and analyze complexed, chelated and adsorbed form of Fe, Mn, Zn, Cu from soil
Analysis of Organic materials
The amount of
organic matter in soil is relatively high and changes rapidly over a short
period of time. Hence, sampling to monitor changes in soil organic matter
should be done regularly. There should
not be any roots or added organic materials in the sample.
The most common
method used to estimate the amount of organic matter present in a soil sample
is by measuring the weight lost by an oven-dried (105°C) soil sample when it is
heated to 400°C; this is known as 'loss on ignition', essentially the organic
matter is burnt off.
Chromatography
techniques such as HPLC – High performance (or high pressure liquid
chromatography), GCFID – Gas chromatography with flame ionization detection, GCMS
– Gas chromatography with mass spectroscopy detection are also used.
4.
Calibration and interpretation of the results:
For the
calibration of the soil test data, , particular nutrient is selected and the
test crop is grown with varying doses of particular nutrient and basal dose of
other nutrients. By plotting the soil test values against the percentage yield will
allow to calculate the relationship between soil test values and per cent yield
response
2. Plant Testing:
1.
Analysis of tissues from plant growing on the soil
Plant tissue
analysis is the determination of the concentration of an element in a plant
sample taken from a particular portion of a crop at a certain time or stage of
morphological development. The plant
analysis has been used as a diagnostic tool or complementary to soil testing
because
(i) In many
situations, the total or even the available content of an element in soil fails
to correlate with the plant tissue concentration or the growth and yield of
crop due to many reasons including the physico chemical properties of the soils
and the root growth patterns.
(ii) On the other
hand, the concentration of an element in the plant tissue is positively
correlated with the plant health. Therefore, the plant analysis has been used
as a diagnostic tool to determine the nutritional cause of plant
disorders/diseases.
Steps
1. The
collection of the representative plant parts at the specific growth stage,
2. Washing,
drying and grinding of plant tissue
3. Oxidation
of the powdered plant samples to solubilize the elements,
4. Estimation
of different elements,
5. Interpretation
of the status of nutrients with respect to deficiency / Sufficiency /toxicity
3.
Biological tests in which the growth of higher plants or certain
micro-organisms is used as a measure of soil fertility
Neubauer seedling
Method
·
The Neubauer seedling technique is based
on the uptake of nutrient by growing a large number of plants on a small amount
of soil.
·
The seedlings exhaust the available
nutrient supply within short time.
·
The total nutrients removed are quantified
and tables are established to give the minimum values of nutrients available
for satisfactory yield of various crops.
Microbial methods
·
In the absence of nutrients, certain
microorganisms exhibit behavior similar to that of higher plants.
·
For example, growth pattern of Azotobacter or Aspergillus niger reflects nutrient deficiency in the soil.
·
The soil is rated from very deficient to
not deficient in the respective elements, depending on the amount of colony
growth.
·
In comparison with other methods that
utilize higher plants, microbiological methods are rapid, simple and require
little space.
4.
Nutrient deficiency symptoms of plant
·
The plant requires seventeen essential
nutrients for their optimum growth and development.
·
When a plant nutrient is below critical
concentration in plant, it shows deficiency symptoms
·
It is good tool to detect deficiencies of
nutrient in the field
·
These symptoms are nutrient specific and
show different patterns in crop.
Limitations:
·
The visual symptoms may be caused by more
than one nutrient or may be due to an excess quantity of another nutrient.
·
Deficiency symptoms in the field may be
due to disease or insect damage which can produce certain micronutrient
deficiencies.
·
Nutrient deficiency symptoms are observed
only after the crop has already suffered an irreversible loss.
Deficiency
indicator plants
Plant Nutrient
deficiency
Oat Mg,
Mn and Cu deficiencies
Wheat and barley Mg, Cu and some
times Mn deficiencies
Sugar beets B and Mn deficiencies
Maize N,
P, K, Mg, Fe, Mn and Zn deficiencies
Potatoes K,
Mg and Mn deficiencies
Rape N,
P and Mg deficiencies
Brassica species K and Mg
deficiencies
Celery and sunflower
B deficiency
Cauliflower B and Mo
deficiencies
Flax Zn
deficiency
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