Usually, in some educational setting, soil temperature is listed when someone lists the various factors that affect nutrient uptake. In most instances, however, there is no description of how this soil property impacts early crop growth. Based on recent e-mails and telephone calls, soil temperature had a major impact on crop growth in some parts of Minnesota in May and early June. In general, May and early June of this year can be characterized as cool, if not cool and dry. So, what effect did these cool/dry conditions have on early crop growth? Although the recent days of warm and humid weather have stimulated crop growth, this is a good time to review the impact and importance of soil temperature on nutrient availability, nutrient absorption and crop growth.
From the crop growth perspective, soil temperature has a direct impact on root growth and development. Corn, for example, can germinate at soil temperatures of 50 degrees F. But, roots are slow to develop at this temperature and growth of the secondary root system is slowed. To be absorbed by plants, the immobile nutrients (P,K, micronutrients) must either move to the root via a process called diffusion or the root must grow to and intercept the nutrient. Thus uptake of the immobile nutrients is directly affected by soil temperature primarily because of the impact on root growth. Except for the effect on the process called mineralization, availability is not affected by soil temperature. The following table illustrates the effect of soil temperature on phosphorus uptake.
Phosphorus uptake by corn as affected by soil temperature.
phosphate in a band 59 68 77
lb. P2O5/acre —————–milligrams P/pot——————————
35 3.5 10.4 18.0
The data were collected in a greenhouse experiment where temperature in the soil could be easily controlled. Phosphorus uptake by corn was reported as milligrams per pot. The actual numbers are not importrant. The relative differences are. The uptake measurements were taken 5 weeks after corn emergence.
At each rate of applied phosphate, phosphorus uptake increased as soil temperature increased. With a higher probability of cool temperatures early in the growing season in Minnesota, it’s important to use management practices that maximize uptake of immobile nutrients. Use of banded fertilizer near the seed at planting is the major or most important management practices.
This spring, corn in some fields showed symptoms of phosphorus deficiency even though soil tests for P were medium to high. At these soil test values, corn usually does not exhibit symptoms of phosphorus deficiency. In most cases, the problem could be traced to cool soil temperatures. There were peat soils and other other situations where corn was planted where there was a lot of residue from the preceeding crop. Soil temperature usually remains low in these situations early in the growing season. Therefore P uptake would be reduced and there could be symptoms of P deficiency.
Soil temperature has a major effect on the breakdown or decomposition of soil organic matter. This process is usually referred to as mineralization. This organic component of the soil system is a major reservoir for phosphorus, sulfur, and nitrogen. For example, approximately 90% of the total amount of sulfur in soil is found in the organic matter. So, if decomposition (mineralization) is slowed, the ready availability of some nutrients necessary for crop growth can be restricted early in the growing season.
For example, there was one call this spring reporting that corn growing on soil with a high organic matter content was showing symptoms of sulfur deficiency. These symptoms appeared when corn followed corn; but not when corn followed a soybean crop. With a chisel plow used for the primary tillage more residue remained on the soil surface when corn followed corn this spring, therefore, delaying the decomposition of the organic matter. Because of this, availability of sulfur may have been limited for a short period of time. But, with the warmer temperatures, mineralization should increase, sulfur should become more available,and the sulfur deficiency symptoms should disappear without any subsequent reduction in corn yield.
Organic matter, of course, is a major source of nitrogen needed for crop production. There is no question. The release of nitrogen from organic matter is highly dependent on both soil moisture and soil temperature. Researchers have worked for many years in an attempt to predict nitrogen release to the nitrate form if soil soil temperature and soil moisture content are known. It is possible to predict this release in certain well defined and controlled conditions. When looking at the big picture, however, there is no general agreement as to what this mathmatical relationship should be. So, the research goes on. If it were possible to measure soil moisture and soil temperature and predict the amount of nitrate-nitrogen released into the soil system, current N fertilizer guidelines could be fine tuned and there could be more precision in the use of N fertilizers.
Although it may not be possible to completely overcome the negative impacts of a cool season on crop growth and development, there are some management practices that can be used to keep the negative impacts of soil temperature to a minimum.
Removal of residue above the row and the use of a banded fertilizer at planting are two practices that can have positive effects when soil temperatures are low. A residue free zone that is 10″ to 14″ wide over the row can stimulate germination and early growth. This is easy to achieve when corn follows a soybean crop or sugarbeet crop and some primary tillage has been used. Good residue removers on the planter are essential to maintain this zone if corn follows corn.
Use of a banded fertilizer placed near the seed at planting is the second practice that helps young plants to overcome low soil temperatures early in the growing season. This fertilizer placement stimulates eartly root development as well as placing essential nutrients very near the seed. Use of these two practices does not guarantee that low soil temperatures will not have a negative effect on crop production. These practices, however, improve the odds for improved production.