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Soil Solid & Solution

In the soil, there are different kinds of constitunets. These properties are divided into two major types- solid and solution.

This composition of soil solids and soil solution is discussed in this article.  


Chemical Composition of Soil Solids

Soil Solid consists of soil mineral matter and soil organic matter. The composition of soil varies from place to place so do its mineral and organic matter composition.

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Soil Mineral Matter

All soils do not have the same mineral matter composition. It varies depending upon the parent material. Still, some common chemical elements in soil are found responsible for the mineral matter composition. These are as follows:

Chemical Elements % (by weight)

Non-metals:

Oxygen 46.60
Silicon 27.72
Total= 74.32%

Metals:

Aluminium 8.13
Iron 5.00
Calcium 3.63
Sodium 2.83
Potassium 2.59
Magnesium 2.09
Others 1.41
Total= 25.68%

 

Soil Organic Matter

Organic matter generally comes in soil from plant and animal residues. Among them, plant tissues mainly through decomposition forms the organic matter. So, the composition of organic matter is similar to the composition of a fresh plant tissue. This composition can mainly be divided into two parts:

a) Water = 75% (60-90%)

b) Dry Matter =25% (10-40%)

This dry matter generally have the following constituent elements:

Total  100% 25%
Element In 100% Dry matter  In 25% Dry matter of organic matter
Carbon 42%  10.5%
Oxyzen 42% 10.5%
Hydrogen 8% 2%
Ash/others 8% 2%


(These composition may vary depending upon plant type.)

Moreover, the organic compounds which are chiefly found in detectable form in the soil organic matter are:

i) Carbohydrates (60%)

a) Sugars and starches = 1-5%
b) Hemicelluloses = 10-30%
c) Cellulose = 20-50%

ii) Lignins = 10-30%
iii) Protein = 1-15% (Water soluble and crude protein)
iv) Fats, waxes, and tanins = 1-8%
v) Polyphenols = 2%
Besides, humic acid, fulvic acid, cholorophyll etc. may also be present.


Soil Solution

Soil solution refers to the liquid phase of soil which consists of dissolved substances both organic and inorganic, in ionic or in molecular form.

Composition of soil solution

Soil solution is composed of both organic and inorganic constituents. These are mentioned below:

i) Organic constituents

a) Organic acids:
Formic acid, Acetic acid, Oxalic acid, Malonic acid, Malic acid, Citric acid, Tartaric acid, Gluconic acid, 2-ketogluconic acid, Gallic acid, Salicylic acid, Lactic acid.

b) Amino acids:
Alanine, Lysine, Arginine, Aspartic acid, Glycine, Glutamic acid.

ii) Inorganic constiuents

a) Essential elements (17):

The elements which are required for the normal growth and reproduction of plants in order to completing its life cycle are called essential elements. There are 17 essential elements found in different forms in the soil.

Element Form in the soil
1. Carbon  C
2. Hydrogen  H
3. Oxygen  O
4. Pottasium  k+
5. Calcium  Ca2+
6. Magnesium  Mg2+
7. Nitrogen  NH4+, NO3
8. Phosphorus  H2PO4, HPO42-
9. Sulpur  SO42-
10. Molybdenum  MoO42-
11. Iron  Fe2+, Fe3+
12. Cobalt  Co2+
13. Copper  Cu2+
14. Chlorine  Cl
15. Manganese  Mn2+
16. Zinc  Zn2+
17.Boric Acid mooecule  H3BO3

b) Beneficial elements (6):

An element is considered to be beneficial when-

  1. It is able to substitute an essential element, for example, sodium can substitute for some of the potassium in sugar beets.
  2. That are sometimes needed by plants.
  3. That benefits plants.

There are 6 beneficial element as following:

  1. Sodium (Na)
  2. Fluorine (F)
  3. Iodine (I)
  4. Silicon(Si)
  5. Strontium(Sr)
  6. Barium (Ba)

Concentration of soil solution

The ideal concentration of soil solution is 0.05- 0.2% which is the range of tolerance of salt proportion in soil solution by plants.

  • 0.05-0.2% = favorable proportion of salt for plants.
  • 0.2-0.5% = plants can tolerate but feels uncomfortable.
  • Greater than 0.5% = plants cannot tolerate.
  • Less than 0.05% = unfavorable condition, element deficiencies are found to occur.

Source:

  1. Inorganic constituents nutrients
  2. Class lecture of Farah Monowara Jahangiri, Department of Soil, Water and Environment, University of Dhaka.
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