field capacity is the quantity of water that is retained by a soil after drainage by cohesion and adhesion.
Chat with our AI personalities
Field capacity is the maximum amount of water that soil can hold against the force of gravity after excess water has drained away. It represents the water content in soil that is available to plants for uptake. At field capacity, the soil is typically at its optimal moisture level for plant growth.
Field capacity is the maximum amount of water soil can hold after excess water drains away. It is the point at which gravity overcomes the forces of water absorption and retention in the soil. Field capacity helps determine when plants need watering and ensures proper soil moisture for crop growth.
The water holding capacity of soil refers to the amount of water that soil can retain and store for plants to use. It is influenced by factors such as soil texture, structure, and organic matter content. Soil with high water holding capacity can retain more water for plants, while soil with low water holding capacity may require more frequent watering.
The soil bearing capacity of Pasay City can vary depending on the specific location and type of soil present. However, in general, Pasay City is located on relatively stable ground with a moderate to high soil bearing capacity suitable for construction and development projects. It is advisable to conduct a site-specific soil test to determine the exact soil bearing capacity for a particular area in Pasay City.
Air capacity in soil refers to the volume of pores within soil that are filled with air. It is important for proper soil aeration, allowing for the exchange of gases necessary for plant growth, root respiration, and microbial activity. Soil with high air capacity enables the movement of oxygen and carbon dioxide, supporting healthy soil ecosystems.
Nutrient holding capacity of soil refers to the soil's ability to retain and supply essential nutrients to plants for their growth and development. It depends on the soil's physical and chemical properties, such as texture, organic matter content, and cation exchange capacity, which influence the soil's capacity to retain and release nutrients for plant uptake.