Field Capacity
Field capacity refers to the amount of water soil can hold after excess water has drained away and the gravitational forces no longer pull additional water down. This state occurs when the soil is saturated and then allowed to drain, leaving behind moisture that is available for plants. It's an important concept in agriculture and ecology as it affects plant health and growth. Understanding field capacity helps farmers determine irrigation needs and ensures efficient water management for crops, promoting sustainable practices in farming and enhancing overall soil health.
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Field capacity refers to the amount of water soil can hold after excess water has drained away and the soil has settled. It represents the maximum moisture level at which plants can access water. This state occurs when gravitational water has moved through the soil, leaving behind water that is retained in the soil's pores, making it available for plant roots. Understanding field capacity helps in agriculture and gardening, as it guides irrigation practices and ensures plants receive sufficient moisture without overwatering.