địa Soils range in depth form just

địa Soils range in depth form just a few inches to tens of meters and in may instances they have been
transported many kilometers from the site of their initial formation and then deposited over materials
such as bedrock which is much different than the original source of the soil materials. The effects of
five soil forming factors alter the soil material: climate, time, relief, organisms, and parent material.
These factors act together to differentiate individual bodies of soil. This is accomplished through four
basic processes acting on the parent material to alter its properties and differentiate one soil from
another. These are (A) Translocations, (b) Transformations, (c) Additions, and (d) Losses. (Figure 3)

Kết quả (Anh) 1:

the Soils range in depth form just a few inches to tens of meters and in may instances they have been transported many kilometers from the site of their initial formation and then deposited over the materials such as bedrock which is much different than the original source of the soil materials. The effects of five soil habit-forming factors alter the soil material: climate, time, relief, organism, and parent material. These factors act together to differentiate individual bodies of soil. This is accomplished through four basic processes acting on the parent material to alter its properties and differentiate one soil from another. These are (A), (b) Translocations Transformations, (c) Additions, and (d) Losses. (Figure 3)

Kết quả (Anh) 2:

Soils range in depth local Just a few inches to form tens of meters and in sewing instances chúng được
transported many kilometers from the site of initial formation and then ask for their materials deposited over
much như Bedrock mà the original coal khác source of the soil materials. The effects of
five soil forming Factors alter the soil material: climate, time, relief, organisms, and parent material.
These act together to differentiate the individual Factors bodies of soil. This Is Accomplished through four
basic processes acting on the parent material to alter its soil properties and differentiate one from
another. These are (a) translocations, (b) Transformations, (c) Additions, and (d) Losses. (Figure 3)