What is Soil?

Questions and Answers

Horizontal compacted layering

Loose and porous structure

High water drainage

Vertical dimensions (correct)

To maintain proper soil conditions for future generations (correct)

To understand its natural ecosystem

To use it as a building material

To explore its micro-ecosystems only

Pharmaceuticals

Fiber production (correct)

Cosmetics

Production of fuel

To ensure the structure's integrity Signup and view all the answers

Clay Signup and view all the answers

Because it can hold shape well Signup and view all the answers

Horizontal compacted layering Signup and view all the answers

Because it is the most basic and fundamental piece Signup and view all the answers

To maintain good soil conditions for crops Signup and view all the answers

As a component of concrete Signup and view all the answers

Study Notes

Soil is a medium that consists of a mixture of sediment, minerals, organic matter, air, gases, liquids, and organisms that provide the fundamental ecosystem and essentials for plant life and all life.

Soil provides space and medium for plants to grow, with their roots needing soil to live and thrive.
Soil provides water storage and purification, with water soaking into the soil and being filtered as it flows through.
Soil provides a home for many organisms, especially microorganisms.
Soil takes part in all major biogeochemical cycles, such as the phosphorous cycle, nitrogen cycle, and carbon cycle.

Soil composition varies depending on the region and can have different gas content, including carbon dioxide or methane.
Microorganisms perform cellular respiration and release carbon dioxide into the soil and atmosphere.
Decomposing organic matter in soil produces carbon dioxide and methane.
Plants have different biological processes that take nitrogen out of the soil or release it back into the soil.

Soil develops and accumulates from its basic components of organic matter, sediments or minerals, water, and gases through multiple processes.
Sediment weathering is the first step in soil development, with rocks being broken down into smaller pieces through physical or chemical processes.
Sediment erosion or transport allows the sediment to be deposited and accumulated in a new location.
Organic matter introduction through pioneer species such as lichens and moss helps to further break down bare rock into looser sediments.
Organic matter decomposition introduces gases to the sediments, making it more nutritious for plant growth.

There are four major types of soil: sand, silt, clay, and loam.
Each type of soil provides different circumstances and microclimates, regarding water content and permeability, and aeration.
Sand is the coarsest and loosest of soil classifications, with particles visible to the naked eye, providing easy drainage but being nutrient-poor.
Silt is finer than sand, holding onto water more and longer, making it more nutritious for plants, but less common than sand.
Clay is very fine-grained silt, holding onto water well, but lacking drainage, making it unsuitable for plant growth.
Loam is a combination of sand, silt, and clay, providing the best of both worlds for plant life.

A soil profile consists of many layers of sediments beneath a top layer of soil, each layer being a different soil horizon.
Top layers of soil might have a different sediment matrix than the soil horizon beneath it.
Soil horizons can be compacted layers of sands, silts, or clays before reaching bedrock.

Soil is essential for agriculture and food production, with farmers trying to maintain good soil conditions for their crops.
Soil is also used in fiber production, building construction, and as an ingredient in concrete.
Understanding soil, its micro-ecosystems, and life cycles is important for maintaining proper soil conditions for future generations.