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Soil horizons in tropical areas and in temperate areas

by shiv

what is a soil horizon

types of horizon

Tropical soil horizion

Soil in the tropical rainforests is very nutrient poor. The topsoil is only one to two inches 2.5 to 5 centimeters deep. The only reason plant life is so lush is because the plants store the nutrients in themselves rather than getting them from the soil. When plants decay, other growing plants tap the nutrients from the dead matter and reuse nutrients left over from that plant.

Trees depend on soil for; stability, nutrients, and water. Most nutrient cycling takes place in the top two feet of soil where supplies of air, water and food allow microorganisms to thrive. These include bacteria, fungi and algae.

soil animals, e.g earthworm, carry humus deeper

into the soil

All layers (horizons) are well drained some nutrients are carried away (leached) into the groundwater

Roots from the plants penetrate

all horizons.

Temprate soil horizon

All generalizations about soil systems have significant exceptions, but two generalizations

that differentiate temperate from tropical soils are quite tenable. First, because temperate

soils are seasonally cold, during a significant portion of the year, plant growth and soil

biological activity are low or nil due to suboptimal or freezing soil temperatures.

Seasonality with its temperature fluctuations results in important changes in the chemical

and physical soil environment.

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