Good soil is soft and bouncy.
It helps plants grow big.
Tiny holes let air and water in.
This helps roots stay healthy.
We can help the soil stay good.
Do you like to dig in dirt?
Good soil feels soft and bouncy. This is called tilth.
Tiny holes in the dirt are very important. They let air and water move. These holes help plant roots grow deep.
Small bugs and worms help too. They turn old plants into food. This makes the soil a strong sponge.
Farmers can help the soil. They use plants to fix it. This keeps the soil healthy for a long time.
Tilth is how soil feels and works for plants. Good tilth means the soil is soft and bouncy. It has many tiny holes called pores. These pores are very important. Large pores let air move through the soil. This keeps plants from drowning in too much water. Small pores hold onto water for dry times. This helps plants stay strong when it does not rain.
Soil is made of small pieces called aggregates. These pieces stick together to form a soil carbon sponge. This sponge holds water and nutrients. Tiny living things like worms and bacteria help make it. They turn old plants into food for the soil.
Farmers can help improve tilth. They can add organic matter to the dirt. They can also use crop rotation. This means planting different things in a set order. For example, planting alfalfa helps. Its deep roots can push through hard ground. Using cover crops can also rebuild the soil sponge. This keeps the soil healthy for a long time.
Tilth is a special word for the physical condition of soil. It describes how well the soil is ready for planting crops. Good tilth means the soil feels spongy and soft. This is because it has many tiny holes called pores. Large pores allow air to move through the soil easily. This helps prevent plants from drowning during wet times. Small pores are also vital because they hold onto water. These small spaces help crops survive during dry periods.
Soil is made of small pieces called aggregates. These aggregates stick together to form a soil carbon sponge. This sponge is very important for holding water and nutrients. In the top layer, small aggregates create many pores. In the subsoil, which is the layer below, aggregates are larger. These subsoil blocks can be 2 to 6 inches big. Deep roots use these paths to find moisture during droughts. However, heavy machines can squash these layers and cause compaction.
People have used many ways to change the soil for a long time. One way is tillage, which is moving the soil with machines. Farmers use tools like mold-board plows or heavy discs. This can break up the ground and add air. In 2021, it was estimated that people till 1,840 cubic kilometers of soil every year. This is much more than the amount of earth moved by engineering projects. While tillage helps at first, it can sometimes hurt the soil sponge over time.
Nature has its own way of building great tilth. Plant roots, earthworms, and tiny microbes work together. Roots release materials that feed helpful bacteria. These bacteria and fungi then help bind soil particles together. This creates a stable structure that resists breaking down in water. Using different crops in a rotation can also help. For example, a corn and soybean rotation has active growth 32% of the time. A rotation with beans, wheat, and corn stays active 72% of the time.
Different types of soil need different kinds of care. Sandy soils are coarse and do not hold water well. Adding organic matter can increase their water capacity by 10 times or more. Clay soils are the opposite and can lack large pores. This can make it hard for air to move through them. Even gravelly soils can be improved by adding organic matter. You might add two inches of organic material for every eight inches of soil you till. This helps all kinds of soil stay healthy for growing food.
Tilth is a term used to describe the physical condition of soil. It specifically refers to how suitable the soil is for planting or growing crops. High-quality tilth is characterized by a spongy texture. This texture is created by many tiny spaces called pores. These pores allow for the movement of air and water throughout the soil. Good tilth is vital because plant roots can only grow where there is enough oxygen. It also ensures that a steady supply of water and nutrients is available to the plants.
To understand how tilth works, we must look at soil aggregation. Aggregation is the process where soil particles stick together into clumps. These clumps must find a balance between tensile strength and friability. Tensile strength is how much force is needed to break a clump. Friability is how easily the soil breaks apart under shallow, non-abrasive tools. If the strength is too high, the soil forms large, cemented clods that are difficult to work. In finer-textured soils, these aggregates may be made of even smaller aggregates.
Different types of pores serve different functions within the soil structure. Large pores are essential for rapid drainage and air exchange. During wet periods, these large pores prevent oxygen deficiency. If soil lacks large pores, plants can drown, and nitrogen can be lost through denitrification. This is the conversion of nitrogen into gaseous forms. Conversely, small pores are critical for water retention. They allow a crop to endure dry periods by holding onto moisture. In degraded soils, large pores are often compressed into small ones, which disrupts this balance.
Soil structure exists in different layers with different characteristics. The top layer is heavily influenced by biological activity and tillage. Below this is the subsoil, which is the layer beneath the tillage zone. Subsoil aggregates are often larger, measuring between 2 and 6 inches. These blocks are more angular and less affected by biology than the topsoil. Deep subsoil aggregates are important because they allow roots to grow deep into the soil profile. This deep growth provides better access to moisture during periods of drought. However, heavy equipment can compact this layer, especially when the soil is wet.
Humans manage tilth through mechanical and biological methods. Tillage involves the mechanical manipulation of soil to break it up and aerate it. Primary tillage uses tools like mold-board or chisel plows. Secondary tillage includes methods like disking and harrowing. In 2021, the global volume of tilled soil was estimated at 1,840 cubic kilometers per year. This amount is two orders of magnitude larger than all global engineering earthworks. While tillage can improve tilth temporarily, it can also be unstable. Over time, intensive plowing can cause the soil carbon sponge to oxidize and break down.
Nature provides a more stable way to build tilth through biological processes. This involves the interaction of plant roots, earthworms, and microorganisms. This process creates a "soil carbon sponge" that binds particles together. For example, plant roots release exudates that feed bacteria. These bacteria emit extracellular polysaccharides, also known as EPS. Fungal hyphae, which are tiny thread-like structures, also grow into the soil. These fungi and bacteria work together to stabilize the soil structure. This biological network helps the soil resist breaking down even when it is saturated with water.
Farmers can use crop rotation to restore and maintain tilth. Rotating crops can help rebuild the soil carbon sponge. For instance, grass and legume sods develop very extensive root systems. As these roots grow and die, they provide organic matter that feeds soil organisms. This feeding process helps create more stable aggregation. Different rotations also change how much time the soil is active. A corn-soybean rotation has active growth only 32% of the time. In contrast, a dry bean-winter wheat-corn rotation stays active 72% of the time.
Finally, the management of tilth depends heavily on the specific soil type. Sandy and gravelly soils are naturally low in small pores and can suffer from drought. Adding organic matter can increase the water capacity of sandy soil by 10 times or more. Clay soils are the opposite, as they often lack large pores for air and water movement. Clay is also more prone to compaction. In gravelly or decomposed granite soils, adding organic matter can help significantly. A common practice is adding two inches of organic material for every eight inches of soil being tilled.
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