5.1 Introduction to Soil Systems Flashcards
Soil
composed of mineral and organic matter, air, and water, that forms the uppermost layer of the Earth’s surface and is capable of supporting plant life
Soil texture
The relative proportions of sand, silt, and clay particles in soil.
Clay
The smallest soil particles.
High porosity (holds water), but low permeability (slow to drain)
Silt
Medium-sized soil particles (between clay and sand) that feel smooth and powdery.
Often river deposited.
Sand
The largest soil particles, which feel gritty and allow for good drainage.
Porosity
The measure of the void spaces in soil, affecting its ability to hold water and air.
Permeability
Relates to drainage.
The ability of soil to transmit water and air through its pores.
Horizons
The distinct layers of soil that form a soil profile.
Soil profile
A vertical section (cross-section) of soil that shows all its horizons.
“O” horizon
The topmost soil layer, rich in organic matter and decomposed material.
Humus lies above it, not within it.
“A” horizon
The topsoil layer, rich in organic material and minerals, where most plant roots grow.
“B” horizon
The subsoil layer, where minerals leached from above accumulate.
“C” horizon
The layer of partially disintegrated and weathered parent material beneath the B horizon.
Bedrock
The solid rock layer beneath the soil layers.
Sometimes called the “R” layer
Parent material
The underlying geological material from which soil forms.