The water-holding capacity of [[1]] is the ability of the soil to hold and retain water for plant use.

The water-holding capacity of soil is the ability of the soil to hold and retain water for plant use.

Water holding capacity refers to the ability of the soil to hold onto water and make it available for plants to use over time. When water is applied to soil, it is held in the pore spaces between soil particles. The amount of water that can be held depends on the texture, structure, and organic matter content of the soil.

For plants to grow and thrive, they need a steady supply of water to uptake through their roots. If the soil has a low water holding capacity, it may dry out too quickly, making it difficult for plants to obtain the water they need. Conversely, if the soil has a high water-holding capacity, it can hold onto too much water, which can lead to waterlogging, reduced oxygen availability, and nutrient leaching.

Maintaining an appropriate water holding capacity in the soil is important for promoting healthy plant growth and maximizing water use efficiency in agricultural systems. This can be achieved through practices such as adding organic matter, reducing soil compaction, and implementing irrigation management strategies that balance water application with plant water use.