We hope that we’ve seen the last of the snow by now, but both air and soil temperatures remain below average in Illinois heading into the second half of March. According to the Illinois State Water Survey (http://www.isws.illinois.edu/warm/soiltemp.asp) minimum temperatures 4 inches deep under bare soil ranged from the low 30s in northern Illinois to the mid-30s in southern Illinois the morning of March 17, and with some sunshine on that day, reached the upper 40s to low 50w in southern Illinois but did not get above the low 30s in the northern part of the state.
Soils froze deeper than normal this past winter, and stayed cold into March; frost is only now disappearing in the northern parts of Illinois, which accounts for their staying cold during a sunny day. Hopes that such deep freezing will relieve soil compaction from last year may not be realized; while repeated freezing and thawing result in repeated formation of ice crystals that force soil particles apart, soils that stay frozen don’t repeat this cycle often enough to do much good. The freezing and thawing of the surface soils that we’re seeing now will help loosen them some, but we can’t expect that effect to extend more than a few inches deep.
Though having soil temperatures only in the 30s this late in March is somewhat unusual, March soil temperatures are variable over years. At Champaign, March soil temperatures at 4 inches deep have ranged over the past five years from an average of 36/39 (minimum/maximum) in 2013 to 60/66 in 2011. Rainfall totals ranged from 1.47 inches in 2013 to 5.38 inches in 2011. The start and progress of planting were delayed in both 2011 and 2013, but that was based more on April rainfall than on conditions in March.
When it comes to getting soils to dry out, is warm and wet better or worse than cold and dry? Because water has a higher heat capacity than soil mineral matter, cold soils do not dry out very fast, and wet soils do not warm up very fast. We have seen some of the standing water in fields drain out this past week as soils thaw, but the drying process will be very slow until soil temperatures start to increase. Water loss rates are affected by soil texture and water content, but we would expect wet soil to lose 0.1 inch or so of water in a day if average soil temperature is 40, and at least twice that amount if the average soil temperature is 60 degrees. So having soils warm up is the key to enabling them dry out, though of course it has to stop raining for soils to dry.
Though having low soil temperatures at this point in March does not produce a lot of optimism that planting will start early, it is also not a very good predictor about how the spring will go, or of what kind of season we’ll have. If we’ve learned anything in recent years, it’s that what happens during the summer matters much more than what happens in March and April. We simply need to be ready to do fieldwork and plant as soon as conditions permit.