A gronomy J our n al • Volume 10 9, I ssue 3 • 2 017 M icronutrients are essential for plant growth because these trace elements perform important biological functions. Defi ciencies of micronutrients in soils can signifi cantly reduce crop yield, quality, and economic return (Marschner, 2002). Soybean is an important cash crop in Minnesota being grown on 3.05 million ha in 2015 (USDA, 2016). Th ere has been increased pressure for farmers in Minnesota in the recent years to apply micronutrients to soybean due to a perception that defi ciencies have increased. Soybean response to fertilizer B has been reported in many areas in the United States. In Arkansas, Ross et al. (2006) found that soil-applied B increased soybean grain yield by 4 to 130% and increased trifoliate and grain B concentration. Application of 0.28 to 1.12 kg B ha-1 was suffi cient to produce maximum grain yield. Research in Georgia found that soil, leaf, and grain B concentration were signifi cantly increased with increasing rates of soil-applied B (Touchton et al., 1980). In 3 of the 9 yr, soybean yield increased when fertilizer B was applied. In a separate study, foliar application of 0.56 kg B ha-1 was found to be the optimal rate for increasing the number of pods per branch but application of 1.12 kg B ha-1 promoted the highest seed yield per plant due to increase in seed size (Schon and Blevins, 1990). In the Midwest, Oplinger et al. (1993) summarized 29 trials across Illinois, Ohio, Missouri, and Wisconsin and reported yield increase only in four sites on B-suffi cient soils. Chlorine plays an important role in gas exchange, photosynthesis, and disease resistance in crops. Defi ciency of Cl can negatively impact a crop's normal growth and reduce grain yield if aff ected by disease. In Minnesota, Cl defi ciency has not been reported for major fi eld crops. Chlorine defi ciency is unlikely because most agricultural fi elds in Minnesota routinely receive KCl fertilizer to prevent K defi ciency, which is 50% Cl by mass. Chlorine toxicity is a serious yield-limiting factor for soybean in the southern states of the United States. Toxicity of Cl is caused by accumulation of Cl in the upper soil profi le (Rupe et al., 2000). Chlorine accumulation occurs in poorly drained soils and with limited precipitation because these two factors promote soil Cl retention (Yang and Blanchar, 1993). Soybean grown in the poorly drained Flatwoods soils (fi ne, mixed, semiactive, mesic Aquic Hapludults) of Georgia which received Cl-containing fertilizer exhibited leaf scorching consistent with