Chapter 12: Weathering, Erosion, and Soil Resources Flashcards
What is soil?
all unconsolidated material that overlies bedrock, material capable of supporting plant growth
How is soil produced?
produced by weathering: the chemical, physical, and biological processes that break down rocks and minerals
Mechanical Weathering
(physical weathering) anything that breaks up a rock without altering its composition; (ice, wind, water). Breaks larger chunks of rock into smaller ones, increasing the exposed surface area.
Chemical Weathering
Break down of minerals by chemical reactions with water, other chemicals dissolved in the water, and gases in the air.
What conditions make weathering more rapid?
Higher amounts of water (wetter climate), higher temperatures (warmer climate): chemical reactions proceed more rapidly at higher temperatures than at low ones
How does soil form?
- chemical and physical weathering of rocks produce debris.
- mildly acidic rain percolates through the debris and dissolves parts of it, carrying those ions deeper into the ground
Zone of Leaching
the layer of soil from which ions have been extracted or removed, this is an upper soil layer
Zone of Accumulation
the ions that have been leached out precipitate deeper in the soil column forming new minerals and clays in a region, this is a deeper soil layer
Microbes interaction with soil
microbes further weathering and soil breakup, when they die they accumulate in the soil to form an organic-rich soil material (humus) found in the “O” horizon
Soil Profile
a cross-section of soil reveals layers consisting of horizons
A Horizon
- The “O” in O horizon stands for “organic layer” and consists of organic matter, or humus.
- The O and A horizons together make up topsoil, the fertile portion of soil that farmers till for planting crops.
- Below the A horizon is the E horizon.
What zone do O, A, and E horizons form?
form the zone of leaching because rainwater percolates through this initial layer, dissolves soluble minerals, and carries them away
B Horizon
Lies in the zone of accumulation, B horizon is called the subsoil, where ions, clay minerals, and iron oxides accumulate. Organic matter from the surface is largely absent from this layer.
C Horizon
Consists of material from the underlying bedrock that has undergone some weathering, and consists of mostly broken-up bedrock.
What is soil composition influenced by?
- Climate: large amounts of rainfall and warm temperatures accelerate chemical
weathering and lead to heavily leached soils. Cooler temperatures and lower rainfalls may inhibit soil formation by slowing down the weathering process. - Substrate composition (i.e., what is the bedrock that underlies the composed of): soils can form on basalt, granite, volcanic ash, and quartz sand; leading to soils of different compositions.
- Time: in temperate regions, it takes approximately 15,000 years to form 1 meter of soil. This estimate is based on glacial evidence.
- Vegetation: plant roots help prevent soil from washing away