The effect of mineral fertilizers on the phosphate stock of leached chernozem and the productivity of grain crops

L. P. Galeeva
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Abstract

It was found that the content of readily available phosphorus in the soil of the small-scale experiment after 3 years of fertilizer application remained average in all variants, fertilizers compensated for its removal by grain crops. In the field experiment, the content of this form of phosphorus in the arable soil layer significantly increased only with row fertilization, with other methods of application it decreased to low. Fertilizers in both experiments, with all methods of application, not only compensated for the removal of mobile phosphorus by cereals, but also created a high and increased supply of plants with it. They increased the content of mineral phosphates and did not affect the ratio of their groups in the soil. The active fractions accounted for 22–25 %, Ca – P3 phosphates accounted for 68–72 %, the proportion of Al – P and Fe – P phosphates was the lowest and practically unchanged, indicating the absence of rearrangement and fixation of phosphates into less accessible and inaccessible forms for plants. Phosphorus of fertilizers was absorbed not only by plants, but also by microorganisms. The most microbial phosphorus in a layer of 0-20 cm of leached chernozem in a small–scale experiment was found with local fertilization – 22 kg /ha, and in the chernozem of the field experiment – with row application – 31 kg / ha, which can be used by plants in the aftereffect. In the soil layer of 0–40 cm of the small– scale experiment, the reserves of microbial phosphorus, depending on the method of fertilization, increased in a row: row – scattered – local, and field: scattered – local – row. Only when applied to rows during sowing with seeds, fertilizers significantly increased the yield of spring wheat, the increase from them in small–scale and field experiments averaged 42 and 26 %, respectively. The highest yield of oats in conditions of sufficient moisture supply of the soil was obtained with scattered fertilization in action and with row–in aftereffect, the increase in yield was 12 and 20 %, respectively. The balance of readily available phosphorus in the chernozem of the field experiment is positive for all methods of fertilization, with its deficiency in the control – 26 kg /ha, and mobile – positive in all variants.
矿物肥料对沥滤过的切尔诺泽姆磷酸盐储量和粮食作物产量的影响
研究发现,施肥 3 年后,小规模试验土壤中的易得磷含量在所有变量中都保持平均水平,肥料弥补了粮食作物对磷的消耗。在田间试验中,耕地土壤层中这种形式的磷含量只有在施用行肥时才会显著增加,而在施用其他肥料时则降至较低水平。在这两项实验中,各种施肥方法的肥料不仅弥补了谷物对流动磷的清除,而且还为植物提供了大量和更多的流动磷。这些肥料增加了矿物磷酸盐的含量,但并不影响其在土壤中的比例。活性组分占 22%-25%,Ca - P3 磷酸盐占 68%-72%,Al - P 和 Fe - P 磷酸盐的比例最低,几乎没有变化,这表明磷酸盐没有重新排列和固定为植物较难获得和无法获得的形式。肥料中的磷不仅被植物吸收,也被微生物吸收。在小规模试验中发现,当地施肥时,0-20 厘米沥滤土壤层中的微生物磷最多,为 22 千克/公顷,而在田间试验的沥滤土壤中,行施肥的微生物磷最多,为 31 千克/公顷。在小规模试验的 0-40 厘米土层中,微生物磷的储量根据施肥方法的不同而增加:行施-撒施-局部;田间:撒施-局部-行施。只有在播种时在行间施肥,肥料才能显著提高春小麦的产量,在小规模试验和大田试验中,肥料的平均增产率分别为 42% 和 26%。在土壤水分充足的条件下,燕麦的最高产量是在播种时分散施肥和播种后在行间施肥,增产率分别为 12% 和 20%。在田间试验中,所有施肥方法都能平衡土壤中的易得磷,对照组的缺磷量为 26 千克/公顷,而所有施肥方法都能平衡土壤中的易得磷。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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