首页> 外文期刊>International journal of agricultural research >The Effect of N Fertilizer Placement and Timing on Soil Profile Dynamics of Available Phosphorus and Exchangeable Potassium at Different Growth Stages of Spring Wheat ( Triticum aestivum L. cv. Spectrum) on Leached Chernozem
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The Effect of N Fertilizer Placement and Timing on Soil Profile Dynamics of Available Phosphorus and Exchangeable Potassium at Different Growth Stages of Spring Wheat ( Triticum aestivum L. cv. Spectrum) on Leached Chernozem

机译:氮素淋施黑麦草不同生育期氮,磷,钾素交换对土壤剖面动态的影响

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The maintenance of optimum levels of nitrogen (N), phosphorus (P) and potassium (K) in the soil encourages vigorous growth of spring wheat root systems, which in turn significantly enhances uptake of other nutrients in the soil. A study was carried out to determine the effect of N fertilizer placement and timing on accumulations and distributions of available P and exchangeable K in the soil profile at different phenological stages of the wheat crop at Krasnodar Agricultural Research Institute in Krasnodar County (45°5`N, 38°50`E, >400 m elev.) in Eastern Europe. The experiment was designed as Randomized Complete Block with four replicates, which were subjected to six N fertilizer treatments (T1-T6). Spring wheat was grown under rainfed conditions with treatments varying in N fertilizer placement and timing. N treatments (T2-T6) triggered an available P bulge of 2.7-6.4 mg 100 g-1 soil when compared with accumulations in the control plots during the first season. In the second season, available P build-ups of 2.7-6.3 mg 100 g-1 soil were observed. This was attributed to increased concentration of H+ ions associated with the use of ammoniacal fertilizers, which promoted the solubility of immobile P into relatively available forms. There was a bulge of available P content in the topsoil of about 0.1-2.8 mg 100 g-1 soil and 0.2-3.0 mg 100 g-1 soil compared with its content in the upper subsoil in the first and second seasons, respectively. This was largely due to the rapid fixation of P, which curtailed its mobility to lower layers of the soil. Peak build-ups of available P (11.0-17.3 mg 100 g-1 soil) and exchangeable K (19.1-28.1 mg 100g-1 soil) in the soil profile were observed at tillering stage before rapidly dwindling to as low as 9.0 and 16.6 mg 100 g-1 soil, respectively at anthesis in the first season of the study. In the second season this trend was largely distorted by excessive rainfall. This pattern was attributed to the peak P uptake by wheat plants between stem elongation and anthesis, which caused the P depletion in the soil profile. Comparatively high potassium requirement by wheat plants between seed germination and anthesis accounted for corresponding depletion of exchangeable K in the soil profile at anthesis. However, at milky ripe stage the content of exchangeable K exceeded that at tillering stage by as much as 8.9 mg 100 g-1 soil, which was attributed to the release of K by wheat plant roots into the soil towards the end of the vegetative period. Single basal application of N (T2) had the lowest accumulations of available P (9.4-16.1mg 100 g-1 soil) compared with other treatments in which N was applied. T3 plots in which N45P90K60 was applied as incorporated basal fertilizers before planting and N45 applied at tillering stage by broadcasting method, recorded the highest content of available P (19.9 mg 100 g-1 soil). The single split application of N (N45) as ammonium nitrate may have created a rather acidic environment, which is conducive for the temporary solubility of P coupled with a rather subdued growth of wheat plants and the related low uptake of P under dwindling supply of N in post-tillering period. The same trend was perpetuated in the accumulations of exchangeable K during the growth and development of the wheat crop. T3 plots had the highest content of K (13.0-20.6 mg 100 g-1 soil). This was largely attributed to the reduced plant growth associated with this treatment and the related subdued uptake of this nutrient by N-starved wheat plants in the post-tillering period.
机译:保持土壤中氮(N),磷(P)和钾(K)的最佳水平会促进春小麦根系的旺盛生长,进而显着提高土壤中其他养分的吸收。在克拉斯诺达尔县的克拉斯诺达尔农业研究所(45°5`东欧,北纬38°50`,海拔> 400 m。实验设计为随机完全区组,一式四份,分别进行了六次氮肥处理(T1-T6)。春小麦是在雨养条件下种植的,氮肥的施用方式和时机不同。与第一个季节在对照地块的累积相比,N处理(T2-T6)触发了2.7-6.4 mg 100 g-1土壤的有效P膨胀。在第二季,观测到100 g-1土壤中2.7-6.3 mg的有效磷积累。这归因于与氨水肥料使用相关的H +离子浓度增加,这将固定磷的溶解度提高为相对可用的形式。与第一季和第二季上部土壤的含量相比,表层土壤的有效磷含量分别高出约0.1-2.8 mg 100 g-1和0.2-3.0 mg 100 g-1。这主要是由于P的快速固定,限制了P向土壤下层的迁移。在分till期观察到土壤剖面中有效磷(11.0-17.3 mg 100 g-1土壤)和可交换钾(19.1-28.1 mg 100g-1土壤)的峰值积累,然后迅速降低至9.0和16.6。在研究的第一季花期分别取100 mg-1土壤。在第二个季节,这种趋势在很大程度上因降雨过多而扭曲。这种模式归因于小麦植物在茎伸长和花期之间吸收的峰值磷,这导致土壤剖面中磷的消耗。在种子发芽和开花期之间,小麦植物对钾的需求量相对较高,这解释了在开花期土壤剖面中可交换钾的相应消耗。然而,在乳熟期,可交换钾的含量比分till期高出8.9 mg 100 g-1土壤,这归因于小麦植株根在营养期结束时向土壤中释放的钾。与施用氮肥的其他处理相比,单一基础施用氮肥(T2)的有效磷累积量最低(9.4-16.1mg 100 g-1土壤)。在T3地块上,播种前将N45P90K60用作基础肥料,在分ing期通过广播法施用N45,记录了最高的有效磷含量(19.9 mg 100 g-1土壤)。 N(N45)作为硝酸铵的单次施用可能创造了一个相当酸性的环境,这有利于P的暂时溶解性以及小麦植株的生长较弱,以及在N供给减少的情况下相关的P吸收低在分period期。在小麦作物的生长和发育过程中,可交换钾的积累也保持着相同的趋势。 T3地块的钾含量最高(13.0-20.6 mg 100 g-1土壤)。这主要归因于分treatment后氮饥饿的小麦植物与这种处理相关的植物生长减少以及相关的养分吸收不足。

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