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28 Cards in this Set

  • Front
  • Back

horizons

Horizontal layers in the soil

soil profile

A description of the different naturally formed layers, called horizons, in the soil

o horizon

Consists of dead organic matter

a horizon

the topsoil which is mixed with humus and leached mineral soil

top soil

Is also called the A horizon

e horizon

Zone of leaching where their is less humus and minerals or resistant to leaching

b horizion

Is the subsoil where there is an accumulation of leached minerals like iron and aluminum oxides.

subsoil

frequently known as the B horizon, often high in clay and is reddish or yellow in color

c horizion

Horizon where their are weathered parent material

soil texture

The mineral material of soil

soil fertility

the soils ability to support plant growth (often refers specifically to the presence of proper amounts of nutrients

weathering

gradual physical or chemical breakdown

leaching

Process by which nutrients are washed away from the soil as water moves through it

nutrient-holding or ion-exchange capacity

soils capacity to bind and hold nutrient ions until they are absorbed by roots

fertilizer

materials that contain one or more of the necessary nutrients

organic fertilizer

fertilizer that includes plants or animal wastes or both

inorganic fertilizer

fertilizers that are chemical formulations of required nutrients, without any organic fertilizer included

water holding capacity

the soils ability to hold water after it has been infiltrated

evaporative water loss

kind of evaporation that depletes the soil's water reservoir without serving needs of plants

soil aeration

Process in which soil and porous soil allows oxygen to diffuse into the soil and releases carbon from the soil

compaction

packing of the soil

pH

refers to the acidity or alkalinity of any solution

erosion

the process of soil particles being carried away by wind or water

desertification

the formation and expansion of degraded areas of soil and vegetation cover in arid, semi arid, and seasonally dry areas, caused by climatic variations and human activities.

overcultivation

the practice of repeated cultivation and growing of crops more rapidly than the soil can regenerate, leading to a decline in soil quality and productivity.

overgrazing

the phenomenon of animals grazing in greater number than the land can support in the long term

deforestation

the process of removing trees and other vegetation covering the soil, leading to erosion and loss of soil fertility

salinization

the process whereby soil becomes saltier and saltier until, finally, the salt prevents the growth of plants