"Grab Your Seat and And Enjoy My Journey" Hello guys and welcome to my blog...First of all, this blog was created to portray my journey in Bachelor Of Science (Hons) In Plantation Technology And Management that consists of Field Work subject. I currently further my study at UITM Jasin, Melaka. So hopefully you guys can join my journey together and stay tuned till the end !!

January 03, 2022

Soil Management

Soil Management

 

So today I'd want to tell you how the soil is formed. Soil is a natural body that covers parts of the earth's surface and provides nutrients for plant growth. The soil is formed continuously, but slowly and occur when rocks break down due to weathering. Weathering is a process that might be physical, chemical, or biological in nature. Soil has the variety properties because of the combined action of climate and creatures working on the parent material through time. There are three layers of soil which are topsoil, subsoil, and parent material. 

 

1) Topsoil

The organically enriched A horizon at the soil surface with a height of 12-25 cm is known as topsoil. It's also known as the plow layer because contain most plant roots, organic matter, nutrients, and water are found.

2)Subsoil

The term "subsoil" refers to the layers beneath the topsoil and below the tillage depth. Because of the low organic matter level in this stratum, plants require a lot of water.

 

3) Parent Material

The parent material is The primary material from which soils are formed


In the a layer of soil, there is a vertical section through soil that show the profile of soil that called horizon.There are five master horizons that are recognized using the capital letters O, A, E, B and C

 

1) O horizon

Organic layer made of fully and partially decayed plant and animal debris


2) A horizon

The surface mineral layer where organic matter accumulates which called topsoil. It is Darker than the horizons below and best environment for the growth of plant roots, microorganisms, and other soil biota

 

3) E horizon

The horizon where clay, chemicals and organic matter are greatly leached. This layer is very light and most soil does not have it.

 

4) B horizon

This is the horizon where clay, chemicals and organic matter leached from A and E horizons and accumulate to become illuviation. This layer is lower in organic matter content than A horizon, but has more clay


5) C horizon

It has little effect of soil-forming processes that usually contain the parent material of the soil. It may also include very soft weathered bedrock that roots can penetrate.