Cover crops can mitigate no-tillage-induced labile phosphorus stratification

Reid W. Barker, Matthew J. Helmers, Marshall D. McDaniel
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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.

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覆盖作物可以缓解免耕引起的不稳定磷分层
少耕和免耕系统在减少土壤侵蚀、增加土壤有机质和减少养分损失方面是有效的。然而,长时间的减少耕作会使表层土壤中的磷(P)分层,这可能对水质和作物营养产生负面影响。在玉米(Zea mays) -大豆(Glycine max)轮作的长期(12年)试验中,我们测量了土壤磷的分层,该轮作结合了两种耕作方式(犁耕,免耕),有/没有冬季覆盖作物(黑麦或黑麦)。我们的目标是双重的:(1)在2 × 2析因试验中,采用普通磷分层指数(Pstrat)对6个土壤磷测量指标——水可提取(H2O-P)、微生物生物量(MBP)、阴离子交换树脂可提取磷(AER-P)、土壤试验mehlich - 3p (STP)、碳酸氢盐可提取磷、和总磷。我们计算了Pstrat为0-5厘米深度的平均磷浓度除以5-25厘米深度。(2)将Pstrat与作物磷素吸收和产量联系起来,以回答“磷分层是否限制作物生长?”所有土壤磷测量值的Pstrat范围为1.3 ~ 87.5,但H2O-P分层程度最高(平均H2O-Pstrat = 22.8)。与凿子耕作相比,免耕增加了8%-584%的Pstrat,覆盖作物(耕作)与冬季休耕相比增加了8%-269%的Pstrat。然而,在一个意想不到的拮抗相互作用中,与免耕相比,在免耕土壤上添加覆盖作物可使Pstrat减少23%-72%。有趣的是,大豆磷素吸收和产量与一些Pstrat措施正相关(r >;0.48);但玉米磷素吸收与STP分层呈负相关(r <;−0.46)。我们证实,长期免耕,甚至单独覆盖作物,可以使土壤磷分层。然而,当组合使用时,谷物黑麦作为冬季覆盖作物可以缓解免耕引起的土壤磷分层,这为在美国中西部种植系统中使用这种耐寒覆盖作物增加了另一个好处。
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