Reid W. Barker, Matthew J. Helmers, Marshall D. McDaniel
{"title":"Cover crops can mitigate no-tillage-induced labile phosphorus stratification","authors":"Reid W. Barker, Matthew J. Helmers, Marshall D. McDaniel","doi":"10.1002/saj2.70064","DOIUrl":null,"url":null,"abstract":"<p>Minimal- and no-tillage systems are effective at reducing soil erosion, increasing soil organic matter, and reducing nutrient losses. However, extended periods of reduced tillage can stratify phosphorus (P) in surface soil layers, which can have negative implications for both water quality and crop nutrition. We measured soil P stratification in a long-term (12-year) experiment under maize (<i>Zea mays</i>)–soybean (<i>Glycine max</i>) rotations that combine two tillage practices (chisel-plow, no-tillage) with/without a winter cover crop (<i>Secale cereale</i> or cereal rye). Our objectives were twofold: (1) to quantify soil P stratification in this 2 × 2 factorial experiment using a common P stratification index (P<sub>strat</sub>) on six soil P measurements—water-extractable (H<sub>2</sub>O-P), microbial biomass (MBP), anion exchange resin extractable phosphorus (AER-P), soil test Mehlich-3 P (STP), bicarbonate extractable phosphorus, and total P. We calculated P<sub>strat</sub> as mean P concentrations at 0–5 cm divided by 5–25 cm depths and (2) to correlate P<sub>strat</sub> to crop P uptake and yield to answer the question—Does P stratification limit crop growth? The P<sub>strat</sub> ranged from 1.3 to 87.5 across all soil P measurements, but H<sub>2</sub>O-P was most stratified (mean H<sub>2</sub>O-P<sub>strat</sub> = 22.8). No-tillage increased P<sub>strat</sub> by 8%–584% compared to chisel plowing, and cover crops (with tillage) increased P<sub>strat</sub> by 8%–269% compared to winter fallow with tillage. In an unexpected antagonistic interaction, however, adding a cover crop to no-tilled soils reduced P<sub>strat</sub> by 23%–72% compared to no-till. Interestingly, soybean P uptake and yield were positively related to a few P<sub>strat</sub> measures (<i>r</i> > 0.48); but maize P uptake was negatively related to stratification of STP (<i>r</i> < −0.46). We confirmed that long-term no-tillage, and even cover crops alone, can stratify soil P. When combined, however, cereal rye as a winter cover crop can alleviate no-till-caused soil P stratification, adding yet another benefit to using this winter-hardy cover crop in US Midwest cropping systems.</p>","PeriodicalId":101043,"journal":{"name":"Proceedings - Soil Science Society of America","volume":"89 3","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2025-05-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/saj2.70064","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Proceedings - Soil Science Society of America","FirstCategoryId":"1085","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/saj2.70064","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Minimal- and no-tillage systems are effective at reducing soil erosion, increasing soil organic matter, and reducing nutrient losses. However, extended periods of reduced tillage can stratify phosphorus (P) in surface soil layers, which can have negative implications for both water quality and crop nutrition. We measured soil P stratification in a long-term (12-year) experiment under maize (Zea mays)–soybean (Glycine max) rotations that combine two tillage practices (chisel-plow, no-tillage) with/without a winter cover crop (Secale cereale or cereal rye). Our objectives were twofold: (1) to quantify soil P stratification in this 2 × 2 factorial experiment using a common P stratification index (Pstrat) on six soil P measurements—water-extractable (H2O-P), microbial biomass (MBP), anion exchange resin extractable phosphorus (AER-P), soil test Mehlich-3 P (STP), bicarbonate extractable phosphorus, and total P. We calculated Pstrat as mean P concentrations at 0–5 cm divided by 5–25 cm depths and (2) to correlate Pstrat to crop P uptake and yield to answer the question—Does P stratification limit crop growth? The Pstrat ranged from 1.3 to 87.5 across all soil P measurements, but H2O-P was most stratified (mean H2O-Pstrat = 22.8). No-tillage increased Pstrat by 8%–584% compared to chisel plowing, and cover crops (with tillage) increased Pstrat by 8%–269% compared to winter fallow with tillage. In an unexpected antagonistic interaction, however, adding a cover crop to no-tilled soils reduced Pstrat by 23%–72% compared to no-till. Interestingly, soybean P uptake and yield were positively related to a few Pstrat measures (r > 0.48); but maize P uptake was negatively related to stratification of STP (r < −0.46). We confirmed that long-term no-tillage, and even cover crops alone, can stratify soil P. When combined, however, cereal rye as a winter cover crop can alleviate no-till-caused soil P stratification, adding yet another benefit to using this winter-hardy cover crop in US Midwest cropping systems.