Water Cycle
Atmosphere
Soil Characteristics
Soil Texture
Soil Horizons
100

Recycling of water throughout the atmosphere

water cycle

100

most abundant gas in the atmosphere

nitrogen

100
  • refers to the size of the                                    particles that make up the soil and                     depends on the proportion of sand,                       silt, clay-sized particles, and organic matter in the soil.

soil texture

100

The three components of soil texture

clay, sand, silt

100

The substance that makes up Horizon O

Organic Material

200

water changing from a gas to a liquid in clouds and falling to the ground

percipitation

200

the middle layer of the atmosphere

mesosphere

200

the way the sand, silt, and clay particles are clumped together.

soil structure

200

the largest component of soil texture

sand

200

Under the subsoil

parent rock

300

on mt everest this occurs when water goes straight from a solid to a gas

sublimation

300

the layer where weather occurs

troposphere

300

the pores within the soil.

porosity

300

the component that retains the most water

clay

300

Under the parent rock

Bedrock

400

suspended water particles in a cloud very close to ground level

fog

400

where the ionosphere is located

thermosphere

400
  • Soils can be acidic, alkaline, or neutral. 

chemistry

400

you use to determine a soil's texture

soil texture triangle

400

Soil layers that have gained materials from other layers by water movement

eluviated soil

500

the chemical formula for water

H2O

500

the order of the layers of the atmosphere inner to outermost.

troposphere, stratosphere, mesosphere, thermosphere, and exosphere

500

Soil colors range from black to red to white.

color

500

90% sand, 5% silt, and 5%clay

sand

500

The letter classification for the soil horizon layers.

O, A, E, B, C, or R.