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The soil N-turnover after application of easily degradable organic fertilizers does not follow the classical pattern

机译:施用易于降解的有机肥后的土壤N-周转不会遵循古典图案

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In spite of other influencing factors, the turnover of recalcitrant or moderately degradable organic fertilizers in soil is usually described as a function of the soil temperature. In our investigations, we focussed on those materials containing considerable fractions of easily degradable water soluble or structural organic matter, each of which was characterised by a relatively low C/N-ratio. Typical materials were fresh or dried green manure plants, especially legumes, and other plant derived fertilizers such as different leguminous seed meals and castor cake meal. Laboratory incubation studies as well as field experiments were carried out. It could be shown that the turnover of these materials differed considerably from the classical concept of temperature dependency mentioned above. Net N-mineralisation after soil incorporation of these materials was not or only very little temperature sensitive. Strong N-priming effects could be detected for some of the materials even at low temperatures, especially if considering soil microbial biomass N in addition to soil mineral N. It was concluded that low temperatures induce a decrease of the bioavailability of C-rich polymers (e.g. cellulose) and a preferential microbial utilisation of N-rich low molecular substances.
机译:尽管其它影响因素,顽固或适度降解的有机肥料的土壤中的营业额通常被描述为土壤温度的函数。在我们的研究中,我们侧重于含有的易降解水溶性或结构有机物相当级分的那些材料,其中的每一个的特征为相对低的C / N比。典型材料为新鲜或干燥的绿肥植物,尤其是豆科植物,和其他植物来源的肥料,如不同豆科种子餐和蓖麻饼餐。实验室培养的研究以及实地进行了试验。它可以表明,这些材料的营业额从上述温度依赖性的经典概念有很大不同。这些材料中的掺入土壤后净n矿化没有或仅非常小的温度敏感。强n吸作用可用于某些甚至在低温下的材料的被检测到,特别是如果考虑土壤微生物量氮除了土壤矿物N.得出的结论是低温诱导C-富聚合物的生物利用度的降低(例如,纤维素)和N个富含低分子物质的优先微生物利用。

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