Soil Acidification: Mitigating Yield Loss with Seed-placed Phosphorus Fertilizer and Aglime
The article outlined below can be accessed at: http://landresources.montana.edu/fertilizerfacts/documents/FF79AcidAlseedP.pdf
SUMMARY OF ARTICLE
- Soil acidification occurs from long-term use of ammonium N fertilizers
- Phosphate deficiencies are common in acidic soils despite high soil P levels
- Phosphate deficiencies lead to stunted growth and reduced yields
- Soil liming as remediation strategy; however costly
- Use of fertilizer-P applied in seed row as alternative solution
- Tissue levels of P and grain yield are improved in the study with both fertilizer-P and lime applications
FERTOZ-PHOS AS AN IMMEDIATE AND LONG-TERM SOLUTION
Rock phosphates are very effective in acidic soils (Black and Kempthorne, 1956) due to their enrichment of orthophosphates and release of calcium to the soil; both providing phosphorus nutrition, improving soil physiochemical properties and pH. Residual phosphate after harvest also provides nutrition to subsequent crops (Dib et al., 2006).
Loganathan et al., 2005 determined that continual use of quality rock phosphate can significantly reduce soil acidification rates through their liming effects. Fertoz-Phos is a high quality source of rock phosphate that provides an immediate and residual source of fall applied phosphorus and calcium for the spring and future cropping years. Compared to other sources of phosphate fertilizer, Fertoz-Phos is less susceptible to leaching and runoff. Rock phosphates are not damaging or phytotoxic to the seed, even when applied at high rates.
Soil Acidification: Mitigating Yield Loss with Seed-placed Phosphorus Fertilizer and Aglime No. 79 June 2020
by Richard Engel1 , Clain Jones1 , and Simon Fordyce2 1 Land Resources and Environmental Sciences, MSU-Bozeman, 2 Central Ag Research Center, Moccasin
Soil acidification is a recent development in Montana that has occurred because of long-term use of ammonium-based nitrogen (N) fertilizers. Acidification has led to cases of aluminum (Al) toxicity of field crops where the surface soil pH has fallen below 5.0. Remediation of acid-affected soils will ultimately require the application of liming materials. However, aglime can be quite expensive, exceeding $100 per acre. Short-term solutions to manage these soils are important where farm budgets are tight and under scenarios where farmland is being leased on a short-term basis. Previous work from Oklahoma (Johnson et al. 1991; Kaitibie et al. 2002) found that seed-placed phosphorus (P) can prevent winter wheat yield losses from aluminum toxicity on acidaffected soils. We conducted this study to determine if high rates of seed-placed fertilizer-P could mitigate Al toxicity and increase yield of cereal grains similar to aglime in an acid-affected Montana soil.
Field experiments with durum wheat (cv. Alzada, WestBred, LLC in Bozeman, MT) were conducted during two field seasons (2018 and 2019) on a dryland farm near the town of Highwood in Chouteau County. The dominant soil series was a Bearpaw clay loam in 2018, and a Bearpaw-Vida clay loam in 2019. Soil pH in the surface layer (0-4 inch depth) was 4.2 in 2018 and 4.4 in 2019. Both fields had a prior history of yield losses from soil acidity and Al toxicity. The soils tested very high in available P at 50 and 83 ppm in the top 4 inches according to the NaHCO3 (i.e., Olsen-P) test, in 2018 and 2019, respectively. Our study included five fertilizer-P rates of 0, 15, 30, 60, and 90 lb P2O5/ acre in combination with two aglime rates (-lime and +lime, or 0 and 5 ton/acre). The ten treatments were replicated three times in a split-block design. Individual plots were 5 x 20 feet. Fertilizer-P was applied in the seed-row as 0-45-0. An agricultural dolomitic limestone product (99.2% passing through a #100 sieve) from Montana Limestone Company (Warren, MT) was applied to the limed treatments on October 30, 2017, using a Stoltzfus (Morgantown, PA) wet-lime applicator. The aglime material was incorporated by chisel plowing (15- inch sweeps) two times to a 6-inch depth on the first pass and to 8-inch depth and at right angles on the second pass. The application of aglime was deemed effective at remediating acidity as soil pH (0-4 inch depth) was 6.1 and 6.8 during the spring of 2018 and 2019 in the lime treated areas.
Early season growth and plant tissue P
We observed large differences in shoot growth as a result of the aglime application and fertilizer-P in 2018 (Figure 1). Plants in areas without lime or fertilizer-P had thick stubby roots, characteristic of Al toxicity, and chlorotic purple lower leaves that reflect P deficiency (Figure 2). The chlorotic purple leaves occurred despite very high P soil test levels (Olsen P = 50 ppm). We analyzed plant tissue samples for P at the early tiller stage to determine the impact of lime and fertilizer-P on plant nutrition (Figure 3). Plants in the plot without lime or fertilizer-P had very low plant P concentrations (0.17%), consistent with our visual observations of P deficiency. Plant tissue P was i) improved with seed-placed fertilizer-P; and, ii) greater with lime than without lime at similar fertilizer-P levels. Overall, our results indicate that under very acidic soil conditions Al toxicity and P deficiency may both cause reduced crop growth and grain yield. The possibility of yield losses from P deficiency will likely not be forecast from a soil test report. As noted above, our trials were conducted on soils that tested very high in available P according to the Olsen test. These results indicate the Olsen test is likely not a good predictor of P availability under very acidic soils conditions, such as occurred in our trials.
Figure 1. Durum growth differences at early tiller were very evident as a result of liming and fertilizer-P (90 lb P2O5 /acre) during the 2018 growing season. Soil pH = 4.2 without aglime and pH 6.1 with aglime. Soil pH did not change notably with fertilizer P.
Figure 2. Chlorotic-purple leaves (lower leaves, note white arrow) were evident in durum plants that did not receive lime or fertilizer-P (-lime, 0 P).
Figure 3. Durum tissue P concentration at early-tiller as affected by seed-placed fertilizer-P (0-45-0) for -lime and +lime areas in 2018.
Figure 4. Durum grain yield on the Highwood Bench was improved with seed-placed fertilizer-P (0-45-0) under acid soil conditions (-lime) but was not affected where soil acidity was mitigated with lime applications. Olsen soil P level = 50 ppm in 2018 and 83 ppm in 2019 (very high).
We found durum grain yield increased with P fertilization in 2018 and 2019, but only where soil pH was not increased with the addition of aglime (Figure 4). The interaction of lime and fertilizer-P was particularly impressive in 2018. In 2018, seedplacing 60 lb P2O5/ac ($23 cost @ $0.38 per lb of P2O5) increased grain yield by 22.2 bu/acre over the 0 P controls where lime was not applied. Conversely, yields did not increase with fertilizer-P when lime was applied to correct soil acidity. In 2019, we found a similar interaction between lime and fertilizer-P, but durum growth and grain yield was greatly reduced by two hailstorm events. The second hailstorm occurred during grain-fill and caused considerable numbers of shattered heads and broken tillers. Still, the results of our study indicate that seed-placed P fertilizer can mitigate Al toxicity and related P deficiency at field sites with very acidic soils (pH < 4.5 in top 4 inches). Most importantly, this response occurred even though the soils tested very high in available-P. Our results were consistent with previous reports from Oklahoma winter wheat trials. How fertilizer-P mitigates Al toxicity in crops is still a bit unclear. Two possible mechanisms suggest that i) fertilizer-P ties up dissolved Al in the soil so it can’t be taken up by the plant; and ii) fertilizer-P uptake by crops results in Al-P minerals to form on root surfaces, in root cell walls or within root cells that decrease Al toxicity. Whatever the response mechanism, use of high rates of fertilizer-P should be viewed as a shortterm approach to manage acidic soils. In Montana, this strategy might best be applicable where a farmer is renting land under a short-term lease agreement, is selling the land soon, or does not want to till after lime application, which is needed to raise pH in the root zone. Although all plots in this study were tilled, we expect the benefit of seed-placed fertilizer-P would be similar under no-till management.
Ongoing MSU research is determining appropriate soil testing procedures and prevention, adaptation, and mitigation options, which will be discussed in a future Fertilizer Fact. More information is available at http://landresources.montana.edu/soilfertility/ acidif/index.html, and in The Soil Scoops Soil Acidification: Problems, Causes & Testing, and Soil Acidification: Management http://landresources. montana.edu/soilfertility/soilscoop/index.html.
Addition of seed-placed fertilizer-P can mitigate Al toxicity and increase growth and grain yield of cereal crops in acid-affected soils. § Responses to seed-placed fertilizer-P in acidaffected soils occur even if the soils test very high in available-P.
We thank the Montana Agricultural Experiment Station, the Montana Fertilizer Advisory Committee, and USDA’s Western Sustainable Agriculture Research and Education program for supporting this study. We also thank collaborating producers for allowing us to conduct research on their farms.
Johnson, G.V., R.L.Westerman, E. Allen, and R. Boman. 1991. Managing acid soils for wheat production. Oklahoma State Univ. Ext. Facts F-2240. Oklahoma State Univ., Stillwater, OK. Kaitibie, S., F.M Epplin, E.G. Krenzer, Jr, and H. Zhang. 2002. Economics of lime and phosphorus application for dual-purpose winter wheat production in low-pH soils. Agron. J. 94:1139-1145.
Loganathan*, M.J. Hedley, N.S. Bolan and L.D. Currie. Field evaluation of the liming value of two phosphate rocks and their partially acidulated products after 16 years of annual application to grazed pasture. Nutrient Cycling in Agroecosystems (2005) 72: 287–297
Dib, A.I. Rezk and Mohamed M. El- Fouly, 2006. Release of P from Natural Syrian Rock Phosphate in Acidic Soils. International Journal of Soil Science, 1: 134-139.