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Effects of irrigation and nitrogen fertilization on greenhouse soil organic nitrogen fractions and soil-soluble nitrogen pools

机译:灌溉和氮肥对温室土壤有机氮级分和土壤可溶性氮池的影响

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Soil organic nitrogen fractions and soil-soluble nitrogen pools are important indicators of soil fertility and plant nutrition requirements. However, little is known about soil organic nitrogen fractions and their correlations with soil mineral nitrogen (SMN) and soluble organic nitrogen (SON). A five-year field experiment was conducted to determine the effects of lower irrigation limits (25, 35, and 45 kPa) and nitrogen fertilization (75, 300, and 525 kg ha(-1)) rates on greenhouse soil organic nitrogen fractions and soil-soluble nitrogen pools. The results indicated that the soil organic nitrogen fractions and soil-soluble nitrogen pools were significantly affected by the irrigation and nitrogen fertilization rates and their interactions at various greenhouse soil depths (P 0.01). The soil organic nitrogen occurred mainly in the form of acid-hydrolyzable N (AHN). The soil organic nitrogen fractions other than the amino sugar N (ASN) and the soil-soluble nitrogen pools (SMN and SON) decreased with increasing soil depth. Our findings suggest that ammonium N (AN), amino acid N (AAN), and SMN may predict the soil nitrogen supply potential in greenhouse agroecosystems. Soil total nitrogen (N-total), soil organic carbon (SOC), and nitrate nitrogen (NO3--N) appeared to be the major factors explaining the soil organic nitrogen fractions. Considering water saving, nitrogen reduction, and soil nitrogen supply optimization, it was concluded that the best schedules to use in the greenhouse were I2N1 and I2N2 treatments.
机译:土壤有机氮级分和土壤可溶性氮气池是土壤肥力和植物营养要求的重要指标。然而,关于土壤有机氮级分的知识及其与土壤矿物氮(SMN)和可溶性有机氮(儿子)的相关性。进行了五年的现场实验,以确定温室土壤有机氮级分和氮肥(25,35和45kPa)和氮肥(75,300和525千克HA(-1))率的影响土壤可溶性氮气池。结果表明,土壤有机氮级分和土壤可溶性氮气池受到灌溉和氮肥率的显着影响及其在各种温室土壤深度的相互作用(P <0.01)。土壤有机氮主要是酸 - 水解N(AHN)的形式。除氨基糖N(ASN)和土壤 - 可溶性氮气池(SMN和儿子)之外的土壤有机氮级数随着土壤深度的增加而降低。我们的研究结果表明,N(AN),氨基酸N(AAN)和SMN可以预测温室农业系统中的土壤氮供应潜力。土壤总氮(N-总量),土壤有机碳(SOC)和硝酸盐氮(NO3 - N)似乎是解释土壤有机氮级分的主要因素。考虑到节水,减少和土壤氮供应优化,得出结论是,在温室中使用的最佳时间表是I2N1和I2N2治疗。

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