Soil

Dead leaves that fall to the ground undergo the process of decomposition. They are broken down by decomposers such as fungi, bacteria, and other organisms, which recycle the nutrients back into the soil. This helps enrich the soil and provides nutrients for new plant growth.

The range of soil bearing capacity in Quezon can vary depending on the specific location and soil composition. However, typical values range from 2,000 to 4,000 pounds per square foot for residential construction. It is recommended to conduct a site-specific soil investigation to determine the exact bearing capacity for a particular project.

Loam soil is a combination of sand, silt, and clay, with relatively balanced proportions of each component. This type of soil is known for its ability to retain moisture while still allowing for good drainage, making it ideal for plant growth.

Roots grow in soil due to a combination of factors such as geotropism (response to gravity), thigmotropism (response to touch), and chemotropism (response to chemicals). These forces help roots navigate through the soil, find nutrients, water, and anchorage, and ultimately support plant growth.

Soil is not formed to rocks.

Soil is formed from rocks. As the parent material is chemically and physically weathered, transported, deposited and precipitated, it is transformed into a soil.

Microorganisms in soil play a crucial role in nutrient cycling, decomposition of organic matter, and soil structure formation. They can also help control harmful pathogens and support plant growth by fixing nitrogen. Overall, microorganisms contribute to maintaining soil health and fertility.

the soil make more agriculture , and human have more food .

If soil loses its fertility, it would not be able to support plant growth effectively. This could lead to decreased crop yields, poor plant health, and ultimately impact the entire ecosystem as it disrupts the food chain and biodiversity. Restoring soil fertility usually involves adding organic matter, nutrients, and proper management practices to improve the soil's health.

The layer of soil below the topsoil that is less suited for crops is called subsoil. It typically has lower organic matter content, fewer nutrients, and poorer soil structure, making it less suitable for plant growth without proper management.

A dead plant decomposes in soil because it contains organic matter that can be broken down by microorganisms. Rocks, however, do not decompose in soil because they are not organic and are composed of minerals that do not break down easily.

Soil supports plant growth by providing nutrients, water, and anchorage for roots. It also acts as a habitat for a variety of organisms such as bacteria, fungi, insects, and earthworms that contribute to soil health and nutrient cycling. Additionally, soil plays a role in filtering and purifying water as it moves through the ground.

When organic matter in soil decomposes, it creates a layer called humus. Humus is a dark, organic material that is rich in nutrients and contributes to soil fertility. It helps to improve soil structure, moisture retention, and microbial activity.

Dirt can turn into mud when it gets wet from water or rain, but when the water evaporates, the mud can dry back into dirt. This cycle can happen depending on the presence of water or other wet conditions.

it is formed by weathering

Plants take up water and nutrients from the soil through their root systems. The roots absorb water and nutrients using specialized structures like root hairs and mycorrhizal fungi, which help facilitate the uptake process. This absorbed water and nutrients are then transported throughout the plant to support growth and other essential functions.

Yes, the UK has a variety of soil types, ranging from fertile soils in areas like East Anglia to peaty soils in Scotland. Overall, the soil quality in the UK is considered to be good for agriculture, with proper management practices. However, urbanization and industrial activities have also led to soil degradation in some areas.

Lighting can affect soil by influencing the rate of photosynthesis in plants, which in turn affects nutrient uptake and organic matter decomposition. Excessive light can dry out soil, while a lack of light can hinder plant growth and weaken the soil ecosystem by reducing microbial activity. Overall, proper lighting is essential for healthy soil and plant growth.

All the organic stuff, from worm poo to fallen leaves.

Soil can turn into sediment through the process of erosion, where weathering and transportation break down and carry soil particles to new locations. Over time, these soil particles can accumulate in layers, compact, and become sediment through processes such as lithification and cementation.

Coarse textured soils have larger particle sizes, which create larger pore spaces and promote better drainage. This allows organic matter to decompose more quickly due to increased aeration and microbial activity. In fine textured soils, smaller particle sizes lead to tighter pore spaces, which can create waterlogging conditions that slow down the decomposition of organic matter.

rivers flourishes with soil erosion and then it through of in the banks of river and make land fertile,

Clay soil has very fine particles that pack together tightly, creating small spaces that can trap air and water. This compacted structure limits the movement of air and water through the soil, leading to poor drainage and aeration.

The price of dirt can vary depending on the quality and quantity needed. In general, prices can range from a few dollars per cubic yard for basic topsoil to hundreds of dollars per cubic yard for specialized or enriched soil blends. It's best to check with local suppliers for specific pricing.

Sandy soils are more prone to wind erosion because they have larger particle sizes with low cohesion, making them easier for wind to pick up and transport. Additionally, sandy soils often lack organic matter and vegetation cover, which further reduces their ability to resist wind erosion.