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Effect of temperature and moisture on the mineralization and humification of leaf litter in a model incubation experiment

机译:温度与水分对模型孵化实验中叶凋落物矿化和腐殖质的影响

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The mineralization and humification of leaf litter collected in a mixed forest of the Prioksko-Terrasny Reserve depending on temperature (2, 12, and 22A degrees C) and moisture (15, 30, 70, 100, and 150% of water holding capacity ( WHC)) has been studied in long-term incubation experiments. Mineralization is the most sensitive to temperature changes at the early stage of decomposition; the Q (10) value at the beginning of the experiment (1.5-2.7) is higher than at the later decomposition stages (0.3-1.3). Carbon losses usually exceed nitrogen losses during decomposition. Intensive nitrogen losses are observed only at the high temperature and moisture of litter (22A degrees C and 100% WHC). Humification determined from the accumulation of humic substances in the end of incubation decreases from 34 to 9% with increasing moisture and temperature. The degree of humification C-HA/C-FA is maximum (1.14) at 12A degrees C and 15% WHC; therefore, these temperature and moisture conditions are considered optimal for humification. Humification calculated from the limit value of litter mineralization is almost independent of temperature, but it significantly decreases from 70 to 3% with increasing moisture. A possible reason for the difference between the humification values measured by two methods is the conservation of a significant part of hemicelluloses, cellulose, and lignin during the transformation of litter and the formation of a complex of humic substances with plant residues, where HSs fulfill a protectoral role and decrease the decomposition rate of plant biopolymers.
机译:在Prioksko-Terrasny储备的混合森林中收集的叶子凋落物的矿化和腐殖质,其根据温度(2,12和22A℃)和水分(15,30,70,100和150%的水持量(已经在长期孵育实验中研究了WHC)。矿化对分解早期的温度变化最敏感;实验开始(1.5-2.7)的Q(10)值高于后来分解阶段(0.3-1.3)。碳损失通常在分解过程中超过氮气损失。仅在垃圾的高温和水分(22A℃和100%WHC)的高温和水分中观察到强化氮损失。随着水分和温度的增加,从孵育结束时腐殖质的积累中的腐殖量降低了34%至9%。静止的C-HA / C-FA在12A C和15%WHC时最大(1.14);因此,这些温度和湿度条件被认为是最佳的腐殖质。从垃圾矿化的极限值计算的腐殖质几乎与温度无关,但随着水分的增加,它从70%到3%显着降低。通过两种方法测量的湿度值之间的差异的可能原因是在凋落物的转化过程中守恒,以及在植物残留物的腐殖质物质的形成中形成植物残留物的综合体,其中HSS实现了保护作用并降低植物生物聚合物的分解率。

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