Nitrogen
is probably the nutrient that most often
limits plant growth. The bulk of soil N
is found within 2 feet of the surface. Soil
N is present in three major forms.
Elemental N,
found in a gaseous form in the soil atmosphere,
is of direct significance to plants only
as it may be involved in bacterial fixation.
(e.g., symbiotic N fixation associated with
a legume plant or small amounts of N fixation
by free-living bacteria).
Organic N
makes up about 5 percent of the soil organic
matter (humus) by weight and about 98 percent
of the total soil N. Although organic N
is not available to plants, soil organisms
convert a portion of it each year to inorganic
forms (ammonium and nitrate) that are readily
used by plants. Organic N fertilizers (e.g.,
manures and biosolids) are popular for lawns
and gardens because of their "slow
release" and long-lasting properties.
The relatively low concentration of N in
organic materials means several tons per
acre are required to supply sufficient N
for commercial field crop production. The
economics of transporting these bulky materials
are a major factor when considering their
use as an N source.
Nitrogen in fertilizers
for agricultural crops is largely inorganic
N consisting of three types: ammonium (NH
4 + ), nitrate (NO 3 - ), and urea (CO(NH
2 ) 2 ). Although urea is an organic N fertilizer,
it is rapidly converted to the ammonium
form within a short time after exposure
to moist, aerated soil. Therefore, under
most conditions urea acts more like inorganic
ammonium fertilizers than like natural organic
fertilizers.
In warm, moist soils with
a pH above 5.0, the majority of ammonium
N is converted to nitrate N by soil organisms
rather quickly (within days). Therefore,
most N taken up by plants is in the NO 3
- form, although NH 4 + is taken up when
present in the soil solution. Thenitrate
ion (NO 3 - ) carries a negative charge
which prevents its retention by the negatively-
charged soil colloids. Since it is soluble
and mobile, the nitrate ion is readily and
easily available to plants.
Nitrate moves in the soil
solution and can be leached below the plant
root zone when soil moisture is excessive.
The loss of nitrate by leaching is a common
problem on coarse-textured, sandy soils.
Leaching losses of fertilizer N are minimal
when rates of application conform to recommendations
consistent with the yield potential for
the crop and soil in question. Nitrate N
is also subject to denitrification, a process
in which the nitrate ion (NO 3 - ) is reduced
through several intermediate steps to a
gaseous N oxide or to elemental N.
Potassium (K)
Potassium is one of the
sixteen nutrient elements which is needed
by plants for healthy growth. It is second
only to nitrogen in the quantities required
by plants.
Potassium is very mobile
within plants, and performs a wide range
of vital roles in plant systems, including
photosynthesis, enzyme activation, stomatal
control and transporting plant sugars.
Although potassium occurs
naturally as up to 3.5% of the earth's crust,
only a small proportion of it is available
to plants.
After many years of agricultural
production, and removal of potassium in
produce harvested from the field, even soils
which were naturally well supplied will
become depleted.
If soil potassium supplies
are insufficient to meet plant requirements,
supplementation by potash fertilisers -
fertilisers containing potassium - is necessary
to maintain healthy plant growth and a sustainable
agricultural environment.
Potassium (K)
is absorbed by plants in larger amounts
than any other mineral element except N
and, in some cases, Ca. Potassium is supplied
to plants by soil minerals, organic materials,
and inorganic fertilizer. Due to the highly
weathered status of soils, their K supplying
power is quite low in most cases. Potassium
occurs in the soil solution as a monovalent
cation (K + ). The cation exchange capacity
(CEC) of the soil controls the retention
of K + and in very sandy soils (low cation
exchange capacity) under high rainfall,
K is subject to leaching losses.
Potassium, unlike N and
P, is not found in organic combination with
plant tissues. Potassium plays an essential
role in the metabolic processes of plants
and is required in adequate amounts in several
enzymatic reactions, particularly those
involving the adenosine phosphates (ATP
and ADP), which are the energy carriers
in the metabolic processes of both plants
and animals. Potassium also is essential
in carbohydrate metabolism, a process by
which energy is obtained from sugar. There
is evidence that K also plays a role in
photosynthesis and protein synthesis.
Potassium Nitrate
Potassium nitrate, sometimes
also known as saltpetre, is often used in
foliar sprays or fertigation because it
is highly and quickly water soluble. Its
nutrient composition is approximately:
Duet has the following
composition
Potassium: 37%
Nitrogen: 12%
Potassium nitrate has
application as a potassium source for crops
which are highly sensitive to chloride,
such as tobacco. Potassium nitrate is an
oxidising agent and should be handled and
stored with care.
Dosage and method
of application
| Name of crop
|
Dose |
| Plantation crops like tea, coffee,sugarcane
|
@5gms/lit of water every 35
days,
start 1st spray after 40 days after
planting in the main field |
| Fruit crops and ,Cereal crops like
paddy, wheat, maize etc |
@3 gms/lit of water every 20 days
start 1st spray after 40 days after
planting in the main field |
| Vegetable crops |
@2.5 gms/lit of water every 15 days
start 1st spray after 40 days after
planting in the main field |
| Pulses |
@3 gms/lit of water every 20 days
start 1st spray after 40 days after
planting in the main field |
| Oilseeds |
@3 gms/lit of water every 20 days
start 1st spray after 40 days after
planting in the main field |
| Flowers |
@ 1gm/lit of water every 20 days
start 1st spray after 40 days after
planting in the main field |
| Tobacco |
@3 gms/lit of water every 20 days
start 1st spray after 40 days after
planting in the main field |
| PACKING |
| 1 kg Pouch x 20 =
20 kg CFB Carton |
|