不同施肥和化学补充制度对灰色森林土壤磷动态的影响

A. Pavlichenko
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引用次数: 2

摘要

磷在农业中极为重要。这是因为没有它的参与,植物体内不会发生任何生化反应,因为它是提供能量的ATP分子的一部分。它是核酸、磷脂等的必需元素,积极参与酶促反应的调节。它是人类、动物、植物和细菌细胞的一部分。本研究在1992年灰色森林粗粒轻壤土固定试验的基础上,研究了长期化学复垦和不同施肥制度(无机、有机、有机-无机)对土壤磷素转化的影响。最佳磷营养促进根系发育,改善植株水分和养分供应,提高有机作物的市场产品份额。增加马铃薯中的淀粉含量,根茎、蔬菜、水果、油籽中的糖含量,油籽产出长纤维,其强度增加。因此,植物磷营养的管理是关键问题之一。分析了磷的各种形态(总磷、流动磷、水溶性磷)在上述因素影响下的变化。为了更客观地评估这些因素对土壤磷酸盐状况的影响,分析的不同结果不仅与绝对对照进行了比较,而且与位于试验田旁边的基线(休耕28年的年龄)进行了比较。研究发现,作为土壤遗传特征特征的总磷含量几乎完全取决于总腐殖质储量,并且考虑到腐殖质层的深度和厚度,它明显重复了剖面碳积累的参数。在总磷积累过程中,粒径分布具有重要意义,因为缺陷很容易吸附在土壤结构表面。对分析结果的评价表明,磷的总形态与低浓度的流动形态差距较大,其含量仅占总量的4.7%。根据我们的数据,灰色森林土壤中磷酸水溶性盐的含量通常很低(水平为0.62 mg / kg,且沿剖面逐渐下降),这往往成为作物磷营养的限制因素。石灰通过降低一种半氧化物的活性,削弱了磷的吸附键,增加了磷酸钙的相对数量。施用矿物肥料补充了总磷池(增加了对照码头的0.08%),但磷的流动形式(根据基尔萨诺夫)仅增加了23毫克/公斤,仅次于石灰。一般来说,石灰化的效果显著增加了土壤磷酸盐和肥料的使用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Influence of different fertilization and chemical recruitment systems on the phosphorus regime of gray forest soil
Phosphorus is extremely important in agriculture. This is due to the fact that without its participation in the plant body does not undergo any biochemical reaction, because it is part of the ATP molecule, which provides energy. It is an essential element of nucleic acids, phospholipids and the others is actively involved in the regulation of enzymatic reactions. It is part of human, animal, plant and bacterial cells. The research was conducted on the basis of a stationary experiment conducted in 1992 on gray forest coarsegrained light loam soil, studied the effect of long-term chemical reclamation and various fertilization systems (mineral, organic, organic-mineral) on the transformation of Optimal phosphorus nutrition promotes the development of the root system, which improves the supply of plants with moisture and nutrients, increases the share of marketable products in the organic crop, increases the starch content in potatoes, sugar in roots, vegetables and fruits, oilseeds, oilseeds the output of a long fiber, its strength increases. That is why the management of phosphorus nutrition of plants is one of the key issues. Changes in various forms of phosphorus (gross, mobile, water-soluble) under the influence of the above factors are analyzed. For a more objective assessment of these factors on the phosphate regime of the soil on the variant results of the analysis were compared not only with absolute control, but also tied to baseline (age of fallow 28 years), located next to the experimental field. It was found that the content of gross phosphorus, which characterizes the genetic characteristics of the soil, depends almost entirely on the total humus reserves and clearly repeats the parameters of the profile accumulation of carbon, taking into account the depth and thickness of humus horizons. The particle size distribution is of great importance in the processes of gross phosphorus accumulation, as defects are quite easily adsorbed on the surface of soil structures. Evaluation of the results of the analysis shows a large gap in the gross forms of phosphorus and low concentration of its mobile forms, the content of which is 4.7% of the total. According to our data, water-soluble salts of phosphoric acid in gray forest soil are generally found in very small quantities (0.62 mg / kg in the horizon NOT with a gradual decline down the profile), which often becomes a limiting factor in phosphorus nutrition of crops. Lime, by reducing the activity of one and a half oxides, weakens the adsorption bonds of phosphorus and increases the relative amounts of calcium phosphates. The application of mineral fertilizers replenished the pool of gross phosphorus (by 0.08% of the control dock), but mobile forms of phosphorus (according to Kirsanov) increased by only 23 mg/kg, which was second only to liming. In general, the effect of liming significantly increases the use of soil phosphates and fertilizers.
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