Soil

Clay soil typically absorbs more water than potting soil due to its high density and fine particles that hold water well. Potting soil is designed to provide a well-draining environment for potted plants, which may contain ingredients like perlite or peat moss to improve drainage and aeration.

Loam soil can typically be rolled into a ball when it is moist, but it should not form very hard clumps. It is a balance of sand, silt, and clay, providing good drainage and moisture retention without becoming too compacted.

Pollutant

Loam soil is a well-balanced soil type that contains a mix of sand, silt, and clay. It provides good drainage, retains moisture well, and has a fertile composition that supports healthy plant growth. Additionally, loam soil is easy to work with and has good aeration, making it ideal for many gardening purposes.

The cost of a truckload of sandy loam will vary depending on the supplier, location, quantity, and quality of the soil. Prices typically range from $200 to $800 per load, with additional fees for delivery and any specialized blending or treatment required. It's best to contact local suppliers for specific pricing information.

Solar, chemical, heat and radiation

Sandy soil cannot be rolled into balls or clumps because it has large particles with low cohesion. This type of soil has poor water and nutrient retention due to its coarse texture.

Clay soil is the stickiest type of soil due to its fine particles that have a high affinity for water molecules and form a cohesive mass when wet.

Topsoil has higher fertility than subsoil because it contains a higher concentration of organic matter, nutrients, and microorganisms that support plant growth. These components break down and enrich the topsoil, making it more conducive to plant root development and nutrient uptake. Subsoil, on the other hand, is typically less fertile and lacks the same level of organic matter and biological activity found in the topsoil.

Mountains typically have rocky, well-drained soil due to the steep terrain and erosion processes. The soil composition can vary depending on the specific location and elevation of the mountain, but it is often shallow and nutrient-poor, making it challenging for plants to thrive.

Pioneer species help develop soil by breaking down rocks and organic matter through their roots and decomposition processes. They also enrich the soil with nutrients through their leaf litter and other organic material, which eventually leads to the creation of a more fertile soil for other plant species to establish and grow.

A granular soil structure is considered most desirable for crop production because it allows for good root penetration, water infiltration, and nutrient absorption. Granular soil structure also provides good aeration and drainage, promoting healthy plant growth.

Testing the soil - will reveal any deficiency in minerals etc. This gives the farmer the chance to add chemicals to counterbalance the shortfall, before seeding the area. This will increase the yield of the crop.

Oats grow well in a well-draining loamy soil with a pH of 6.0-7.0. They prefer soil that is rich in organic matter and nutrients to support their growth and development. Proper soil preparation and regular fertilization can help ensure successful oat cultivation.

Groundnuts grow best in well-drained sandy loam soil that is rich in organic matter. They prefer soil with a pH between 6.0 and 7.0. Good soil structure is important to allow for proper root development and nutrient uptake by the plant.

The two main components of soil are mineral particles and organic matter. Mineral particles, such as sand, silt, and clay, provide the physical structure of soil, while organic matter, derived from decaying plants and animals, contributes to soil fertility and supports microbial activity.

Topsoil refers to the outermost layer of soil, typically the top 2-8 inches, that is rich in organic matter and nutrients. It is crucial for plant growth and provides a habitat for soil organisms. Topsoil is important for agriculture and landscaping purposes.

Amaterasu, the Shinto sun goddess, is often associated with agriculture and fertility in Japanese mythology. She is believed to bring light and warmth to the world, supporting the growth of crops and the natural cycle of life. Worship of Amaterasu is thought to bring blessings for fertility and prosperity.

the top one

Turning over the soil helps to aerate it, improving drainage and allowing roots to grow more easily. It also helps to mix in organic matter, nutrients, and fertilizers, improving soil health and promoting plant growth.

Subsoil is typically found in the B-horizon of the soil profile. It is located below the topsoil layer (A-horizon) and contains less organic matter, more minerals, and is often denser than the surface soil.

Lichens and mosses are pioneer species that help initiate soil formation by breaking down rock surfaces through physical and chemical weathering. Their growth and decay contribute organic matter to the soil, enhancing its structure and fertility over time. Additionally, lichens and mosses help retain moisture and prevent erosion, creating a more hospitable environment for other plant species to establish themselves.

Human activities such as deforestation, urbanization, agriculture, and construction can accelerate soil erosion by removing vegetation that helps protect soil from erosion, disturbing the natural landscape, and increasing surface runoff. These activities can lead to the depletion of topsoil, loss of soil fertility, and increased sedimentation in rivers and streams.

This is not accurate. Relief refers to the differences in elevation within a landscape or terrain. The number of microbes in soil is related to soil health and fertility, which is influenced by various factors including moisture, temperature, and organic matter content.

Rocks break down physically and chemically over time due to weathering processes like freezing and thawing, water erosion, and the growth of plant roots. These processes gradually break rocks into smaller pieces, which then mix with organic matter to form soil. Decomposition of rocks also releases minerals that enrich the soil, providing nutrients for plant growth.