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首页> 外文期刊>Communications in Soil Science and Plant Analysis >Interrelations in phosphorus and potassium accumulation characteristics of plants grown in different soil types.
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Interrelations in phosphorus and potassium accumulation characteristics of plants grown in different soil types.

机译:在不同土壤类型中生长的植物磷,钾积累特性之间的相互关系。

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Nutrient accumulation characteristics and mineral content of plants depend on several factors such as crop and site characteristics, environmental conditions, and soil nutrient levels. Nutrient interactions are rather complex and may have an important role in this context. It is evident that phosphorus (P)-potassium (K) interaction is a part of cation-anion balance in plants. Although several authors demostrated the positive P-K interaction in plants, results are still inadequate. Studies on P-K interaction and adequate P/K ratios are needed to improve nutrient efficiency. Pot experiments were carried out under greenhouse conditions with perennial ryegrass (Lolium perenne L.) grown in three soils different in texture, soil organic matter (OM), pH, and available nutrient levels: an Eutric cambisol, a Calcaric fluvisol, and a Haplic phaeosem. Soil samples were taken from selected plots of National Long-Term Fertilization Trials (NLFT) after 30 years of fertilization. Besides the unfertilized control, increasing rates of P were applied in four replicates at four levels of P supply resulting from long-term P fertilization. Dry-matter (DM) production, P and K accumulation characteristics, nutrient concentrations, and K/P ratios of perennial ryegrass were studied for 4 months by taking four cuts. From the results, it was evident that both P and K accumulation of plants were closely related to DM accumulation. Phosphorus accumulation characteristics and amounts of P taken up by plants responded both to the level of long-term P supply and to rates of freshly applied P. Better levels of P supply had a beneficial influence on K uptake and K concentrations in plants. Phosphorus concentrations ranged between 0.20% and 0.53% P, whereas concentrations of K were between 1.63% and 5.64%. As the interaction between P and K may influence that of other nutrients, further research is needed to identify these relationships.
机译:植物的养分积累特征和矿物质含量取决于多种因素,例如作物和场所特征,环境条件和土壤养分水平。营养相互作用非常复杂,在这种情况下可能发挥重要作用。显然,磷(P)-钾(K)的相互作用是植物中阳离子-阴离子平衡的一部分。尽管有几位作者说明了植物中P-K的正相互作用,但结果仍然不足。需要研究磷钾交互作用和足够的磷钾比,以提高养分效率。盆栽实验是在温室条件下进行的,其中多年生黑麦草( Lolium perenne L.)生长在三种质地,土壤有机质(OM),pH和可利用的营养水平不同的土壤中:Eutric cambisol, Calcaric fluvisol和Haplic phaeosem。施肥30年后,从国家长期施肥试验(NLFT)的选定地块中抽取土壤样品。除未施肥的对照外,由于长期施用磷肥,在四个水平的磷供应水平下,一式四份重复施用了增加的磷肥比例。通过四个切分研究了四个月的多年生黑麦草的干物质(DM)产量,磷和钾积累特征,养分浓度以及钾/磷比。从结果可以看出,植物的磷和钾积累都与DM积累密切相关。磷的累积特征和植物吸收的磷的量对长期磷的供应水平和新施磷的速率都有反应。磷供应量的提高对植物对钾的吸收和钾的浓度有有益的影响。磷的浓度介于P的0.20%至0.53%之间,而K的浓度介于1.63%至5.64%之间。由于磷和钾之间的相互作用可能会影响其他养分的相互作用,因此需要进一步研究来确定这些关系。

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