Peat soil is composed of partially decayed plant material and has a high water-holding capacity, making it suitable for wetland environments.

Adaptation is the process by which plants develop specific traits or characteristics that allow them to survive and thrive in their particular soil conditions.

Loam soil is a mixture of sand, silt, and clay, and its well-drained structure makes it ideal for agricultural purposes.

Soil plays a crucial role in providing nutrients, anchoring roots, and storing water, all of which are essential for plant growth.

Clay soil has a high proportion of clay particles, which can lead to poor drainage and compaction, making it challenging for plant roots to penetrate.

Soil formation is the process by which soil is created through the physical and chemical weathering of rocks and minerals.

Sandy soil has a high proportion of sand particles, which allow water to drain quickly and result in low water-holding capacity.

The A horizon is the topsoil layer and is typically the most fertile due to its high organic matter content and abundance of nutrients.

Transpiration is the process by which plants release water vapor into the atmosphere through their leaves.

Silt soil has a high proportion of silt particles, which provide good water-holding capacity and nutrient retention.

Absorption is the process by which plants take in water and nutrients from the soil through their roots.

The B horizon is the subsoil layer and is typically the most compact due to the accumulation of clay minerals and other weathered materials.

Photosynthesis is the process by which plants use sunlight to convert carbon dioxide and water into glucose and oxygen.

Peat soil has a high organic matter content, which contributes to good soil structure and fertility.

Germination is the process by which seeds absorb water and nutrients from the soil, leading to the growth of a new plant.