Chapter 9: Food Section 9.2: Agriculture and Soil.

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Presentation transcript:

Chapter 9: Food Section 9.2: Agriculture and Soil

The Earth has a limited amount of arable land – fertile land available to grow crops.

Farmland Destruction Facts Every minute America is losing 2 acres of farmland. 59% of growth and development is occurring on prime soils.

Thanks to modern farming techniques, America's farmers and ranchers are producing more food on fewer acres, leaving more open space for wildlife habitat.

Agricultural land provides habitat for 75 percent of the nation's wildlife.

Some of the basic techniques used in farming – plowing, fertilization, irrigation, and pest control – began with the earliest farmers.

Plowing the soil – cutting through it and turning it over – helps crops grow by mixing up soil nutrients, loosening soil particles, and uprooting weeds.

Fertilization – synthetic or organic – is used to help maintain the fertility of the soil.

STRUCTURE OF FERTILE SOIL

There are six layers of fertile soil.

O Horizon - The top, organic layer of soil, made up mostly of leaf litter and humus (decomposed organic matter).

A Horizon - The layer called topsoil; it is found below the O horizon and above the E horizon.

Seeds germinate and plant roots grow in this dark-colored layer. It is made up of humus (decomposed organic matter) mixed with mineral particles.

E Horizon - This eluviation (leaching) layer is light in color; this layer is beneath the A Horizon and above the B Horizon.

It is made up mostly of sand and silt, having lost most of its minerals and clay as water drips through the soil.

B Horizon - Also called the subsoil - this layer is beneath the E Horizon and above the C Horizon.

It contains clay and mineral deposits (like iron, aluminum oxides, and calcium carbonate) that it receives from layers above it when mineralized water drips from the soil above.

C Horizon - Also called regolith: the layer beneath the B Horizon and above the R Horizon.

It consists of slightly broken-up bedrock. Plant roots do not penetrate into this layer; very little organic material is found in this layer.

R Horizon - The unweathered rock (bedrock) layer that is beneath all the other layers.

Most soil is produced from bedrock due to temperature and moisture changes that break up the rock into smaller particles.