FACTS soil moisture benchmarking tool
Sandy to clay soils have different hydrological properties such as wilting point, field capacity, and saturation level (Fig 1a). Wilting point means no water is available to plants, field capacity means near optimum moisture for plant growth, and saturation means the soil pores are full of water. Root growth, plant transpiration, and soil nitrogen mineralization are inhibited by too little or too much soil moisture. Nitrogen losses (denitrification and leaching) and soil water evaporation are favored by excess moisture. Thus, knowing the soil moisture level is critically important.