Pretty simple, plants, just like animals need to eat to survive.
While most of these dietary needs are filled by photosynthesis (process of converting sunlight to use-able energy for the plant), not all of what the plant needs is gathered this way.
Plants tend to leech nutrients from the soil (hence the practice of crop rotation).
Also, soil absorbs water so that plants have more time to soak it up.
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Organisms such as earthworms, bacteria, fungi, and plants contribute to soil formation. They break down organic matter, add nutrients, and improve soil structure. Their activities help create a healthy and fertile soil environment for plant growth.
The role of plants and animals in soil formation is very significant. Human activities help in breaking down the particles that form the soil while the animals waste is used as nutrients for the soil.
Washington gets its soil from a variety of sources such as weathered rock, glacial deposits, volcanic ash, and organic matter from decaying plants and animals. The diverse geology and climate of the state contribute to the formation of different soil types across the region.
When earthworms add their wastes to the soil and die, they contribute to the formation of nutrient-rich organic matter. This organic matter improves soil structure, aeration, and fertility, making it more conducive for plant growth. It also enhances microbial activity in the soil, creating a healthy ecosystem for plants.
Look on another page bi**h
Organisms such as earthworms, bacteria, fungi, and plants contribute to soil formation. They break down organic matter, add nutrients, and improve soil structure. Their activities help create a healthy and fertile soil environment for plant growth.
The role of plants and animals in soil formation is very significant. Human activities help in breaking down the particles that form the soil while the animals waste is used as nutrients for the soil.
Washington gets its soil from a variety of sources such as weathered rock, glacial deposits, volcanic ash, and organic matter from decaying plants and animals. The diverse geology and climate of the state contribute to the formation of different soil types across the region.
by eating the soil
Carbon from plants and animals moves into the soil through processes like decomposition, where organic matter breaks down and releases carbon into the soil. Additionally, root exudates and plant litter contribute to soil carbon as they are broken down by soil organisms. Animal waste and remains also add carbon to the soil through decomposition.
they are called soil animals because they like the natural coolness that the soil provides for them
When earthworms add their wastes to the soil and die, they contribute to the formation of nutrient-rich organic matter. This organic matter improves soil structure, aeration, and fertility, making it more conducive for plant growth. It also enhances microbial activity in the soil, creating a healthy ecosystem for plants.
They move the soil around which gives plants just the right amount of room to spread out and grow.
Tiny pieces of decaying plants and animals make up organic matter that contributes to the formation of soil. This organic matter provides essential nutrients for plants and helps improve the soil's structure and fertility.
Plants need soil to grow. Animals either eat plants, or eat animals that ate plants. No soil, no food.
When the animals die they are decomposed and that make the soil more fertile.