Chad Lee and John Grove, Extension Agronomist and Agronomic Soil Scientist, University of Kentucky
When does soil get too dry for young corn? Or, when will you know that the young corn seedlings will not make it? Variations of these questions have been coming in as the lack of rain continues and the temperatures rise on young corn plants. The quickest, and perhaps most practical answer, is to scout fields regularly and identify areas where plants are not recovering from drought stress. In other words, the best indicator of when the plants will not make it is when they have died.
A more technical answer is that a soil gets too dry when the ‘permanent wilting point’ is reached - the level of soil moisture at which plants will fail to recover(Taylor and Ashcroft, 1972, Physical Edaphology: Physics of Irrigated and Non-Irrigated Soils, Freeman and Co., San Francisco).
Most plants will display drought symptoms long before the permanent wilting point is reached. Most silt loam soils will reach the permanent wilting point around 8% moisture content (weight/weight), while a clay loam will reach the permanent wilting point around 10% moisture content (weight/weight).The permanent wilting point varies with temperature, compaction/structure/pore arrangement, and the resulting ability of the soil to conduct water.
| Young corn seedlings require very little water. |
A more technical answer is that a soil gets too dry when the ‘permanent wilting point’ is reached - the level of soil moisture at which plants will fail to recover(Taylor and Ashcroft, 1972, Physical Edaphology: Physics of Irrigated and Non-Irrigated Soils, Freeman and Co., San Francisco).
Most plants will display drought symptoms long before the permanent wilting point is reached. Most silt loam soils will reach the permanent wilting point around 8% moisture content (weight/weight), while a clay loam will reach the permanent wilting point around 10% moisture content (weight/weight).The permanent wilting point varies with temperature, compaction/structure/pore arrangement, and the resulting ability of the soil to conduct water.