沸石和生物沼液对草甸-灰色土壤硝酸盐机制和硝化能力的影响

N. I. Orujova, V. Q. Isakova
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摘要

摘要 在对豆类(绿豆)种植下的草甸灰色土壤进行的固定田间试验中,研究了沸石和生物腐殖质及其联合作用对草甸灰色土壤硝酸盐机制和硝化能力的影响。田间试验证明,有机肥料(生物沼液,每公顷 7.5 吨)和沸石(每公顷 7.5 吨)的综合使用效率最高。从植物生长初期到生物成熟期,豆子的硝态氮含量有所下降。土壤的硝化能力随菜豆生长阶段的不同而动态变化;在菜豆开花期,这一指标更为突出。土壤中的硝酸盐含量与硝化过程强度之间的多项式关系在植物生长初期(春季)和生物成熟期(秋季)较高,而在夏季(开花期)较弱。沸石和生物腐殖质对土壤中硝酸盐氮的含量和硝化能力的积极影响已经得到证实;它们的联合使用也被证明是有效的。
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Influence of Zeolite and Biohumus on the Nitrate Regime and Nitrification Capacity of Meadow-Gray Soils

Abstract

The effect of zeolite and biohumus and their combined effect on the nitrate regime and nitrification capacity of meadow-gray soils have been studied in a stationary field experiment on meadow-gray soils under beans (mung bean). The field experiment has established the highest efficiency of the combined use of organic (biohumus at the rate of 7.5 t/ha) fertilizers and zeolite (7.5 t/ha). The amount of nitrate nitrogen under beans decreased from the initial period of plant growth to the period of biological ripeness. The nitrification capacity of the soil dynamically changed depending on the phase of bean development; this indicator was more intensive in the flowering phase of the plant. The polynomial relationship between the amount of nitrates in the soil and the intensity of the nitrification process was high during the period of the initial development (spring) and period of biological ripeness of the plant (autumn) and weak in summer (during the flowering period). A positive effect of zeolite and biohumus on the content of nitrate nitrogen and the nitrification capacity of the soil has been established; their combined use has also proven to be efficient.

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