Mix of geological (rock) and organic (living) components: sand, silt, clay, humus (main organic part), nutrients (ammonium, phosphates, nitrates), water, air, and living organisms.
Supports plant roots, provides water, shelter, and nutrients for growth (N, P, K, Mg).
Filters rainwater and runoff, trapping pollutants, allowing clean water to enter groundwater and aquifers.
Habitat for organisms like earthworms, fungi, and bacteria, contributing to nutrient recycling by decomposing organic matter.
Weathering breaks down rocks into smaller pieces through:
Physical: wind, rain, freezing/thawing.
Biological: roots of trees crack rocks.
Chemical: acid rain, acids from moss/lichen.
Erosion transports weathered rock fragments by wind and rain, leading to deposition in new locations.
Influenced by:
Parent Material: affects soil pH and nutrient content.
Topography: steep slopes lead to more erosion; flatter areas promote deposition.
Climate: warmer conditions result in faster breakdown of organic matter and increased weathering.
Organisms: soil organisms like bacteria, fungi, and worms break down organic matter, enriching the soil.
O-Horizon: layer of organic matter (plant roots, dead leaves, animal waste) on top of soil, providing nutrients and limiting water loss.
A-Horizon (Topsoil): composed of humus and minerals, has high biological activity.
B-Horizon (Subsoil): lighter layer mostly of minerals, contains some nutrients, with little organic matter.
C-Horizon: least weathered soil, closest to the parent material, sometimes referred to as bedrock.
Loss of Topsoil: caused by tilling and vegetation loss, which disturb soil, leading to increased erosion, drying out soil, and nutrient loss.
Compaction: from machinery and grazing reduces the ability of soil to hold moisture, leading to erosion.
Nutrient Depletion: repeated cropping removes essential nutrients (N, P, K, Na, Mg), reducing future agricultural productivity.