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Study of the Potentially Mineralized Nitrogen Content and Nitrogen Supply by Soil Incubation Method in a Long-Term Field Experiment in East Hungary

机译:匈牙利东部长期田间试验通过土壤培养法研究潜在矿化氮含量和氮供应的研究

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The formation and fate of soluble nitrogen (N) forms and their response to organic-matter mineralization is not obvious yet, and results are often inconsistent despite intensive research. The available N supply of the soil is very important for plant nutrition and environmentally sound N fertilization. The determination of actual N supply is very important for sustainable agriculture in Hungary, especially in acidic sandy soils, which are very sensitive to environmental effects and inefficient human treatment. Therefore, the aim of this article is to provide further information about N mineralization processes and organic-mineral interactions of soil. To establish the potentially mineralized N content and available N supply of soil, a biological (incubation) method was carried out an acidic brown forest soil of the Nyirlugos long-term field experiment in Hungary. The incubation was carried out in the laboratory with differently treated soils of the long-term field experiment to investigate the effect of treatments on N mineralization processes of soil. The incubation period was 16 weeks long. The pH and the easily soluble mineralized and organic N fractions of soil were measured periodically from leached solution (0.01 M calcium chloride; CaCl2). The leaching process was repeated after 2, 3, 5, 7, 9, 12, and 16 weeks. The potentially mineralized N content of soil and the actual rate of N mineralization were calculated from periodically collected data. The results of the incubation method can be summarized as follows: the kinetics of incubation of 0.01 M CaCl2 soluble organic N is similar to mineral N; 0.01 M CaCl2-soluble N fractions were mainly in inorganic forms in the incubation period but the content of the organic form was significant too; and the mineralization rate is greater where the microbiological activity of the soil is expressed and the soil properties are more favored as a result of applied treatments.
机译:可溶性氮(N)的形成和结局以及它们对有机物矿化的反应尚不明显,尽管进行了深入研究,结果常常不一致。土壤的有效氮供应对植物营养和无害环境的氮肥非常重要。氮的实际供应量的确定对于匈牙利的可持续农业非常重要,尤其是对环境影响和无效人类处理非常敏感的酸性沙质土壤。因此,本文的目的是提供有关N矿化过程和土壤有机矿物相互作用的更多信息。为了确定潜在矿化的氮含量和土壤的可用氮供应,在匈牙利的尼鲁戈斯长期野外实验中,采用了一种生物(孵化)方法对酸性棕色森林土壤进行了研究。在实验室进行了长期田间试验的不同处理土壤的孵育,以研究处理对土壤氮矿化过程的影响。潜伏期为16周。定期从沥滤溶液(0.01 M氯化钙; CaCl2)中测量土壤的pH值以及易溶的矿化和有机氮含量。在2、3、5、7、9、12和16周后重复浸出过程。土壤的潜在矿化氮含量和实际氮矿化率是根据定期收集的数据计算得出的。孵育方法的结果总结如下:0.01 M CaCl2可溶性有机氮的孵育动力学与矿质N相似;在孵化期中,0.01 M CaCl2可溶性氮组分主要以无机形式存在,而有机形式的含量也很大;表现出土壤的微生物活性的矿化率更高,并且由于进行了处理而使土壤特性更加有利。

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