亏缺肥制度对草灰壤壤土磷钾动态及其平衡的影响

E. G. Mezentseva, O. G. Kulesh, A. A. Gracheva
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引用次数: 0

摘要

本文介绍了多年来对施肥制度的影响以及前一阶段引入的矿物肥和有机肥的磷、钾残留量对中等栽培灰化土壤土养分平衡和肥力的影响的研究结果。结果表明,在高产栽培作物(59,6 cfu/ha)施用N80P37K95不足以维持已达到的土壤肥力水平,且磷(-14 kg/ha)和钾(-50 kg/ha)的流动形态呈负平衡。长期从施肥系统中排除特定的营养元素会加剧土壤的退化过程,在本研究的20年期间,导致腐殖质损失0.19 - 0.53%,流动磷和钾的年损失为1,0 - 3,6和2,6 - 8,3 mg/kg土壤。
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 DEFICIT FERTILIZER SYSTEMS ON THE DYNAMICS OF PHOSPHATE AND POTASSIUM CONTENT AND THEIR BALANCE IN LONG-TERM EXPERIMENTS ON SOD-PODSOLIC LOAMY SAND SOIL
The results of multi-year research to assess the impact of fertilizer systems and the effect of residual amounts of phosphorus and potassium introduced with mineral and organic fertilizers in the preceding period on the balance of nutrients and fertility of medium-cultivated sod-podzolic loamy sand soil in article are presents. It was established that application of N80P37K95 at high productivity of cultivated crops (59,6 cfu/ha) was insufficient for maintaining the achieved level of soil fertility with negative balances of mobile forms of phosphorus (–14 kg/ha) and potassium (–50 kg/ha). The exclusion of a particular nutrient element from the fertilization system for a long period contributes to the intensification of degradation processes in the soil, causing the loss of humus by 0,19–0,53 % for the 20-year period of the study, with annual losses of mobile phosphorus and potassium of 1,0–3,6 and 2,6–8,3 mg/kg of soil.
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