西北农业大学,陕西杨陵,712100
纸质出版:1996
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李世清, 李生秀. 作物生长期间土壤可矿化氮的变化[J]. 水土保持学报, 1996,10(3):73-77.
Li Shiqing, Li Shengxiu. Changes of Soil Mineralisable N during Crops Growth Periods[J]. 1996, 10(3): 73-77.
在陕西杨陵中等肥力的红油土上进行大田试验,定期分层采取土样,测定土壤可矿化氮和生物体氮,研究作物生长期间土壤可矿化氮的变化及其与生物体氮的关系。结果表明,土壤可矿化氮的分布具有明显的层次性,耕层高,下层少;变化具有明显的阶段性,作物生长前期,含量低而稳定,后期显著增加,是前期的2.0倍。施用氮肥对土壤可矿化氮含量无明显影响;施有机肥可使其后期显著增加.作物种类与种植与否对可矿化氮的影响远比采样时期小。培养期间释放的可矿化氮仅是起始时生物体氮的12.0%,两者之间也无密切相关。起始生物体氮似乎难以反映土壤的供氮能力。
Field trials were conducted in a manural loessial soil with medium fertility
located in Yangling
Shaanxi
to study the changes of the mineralisable N and the relationship between its contents and biomass N in soil
the soil in different layers being sampled and the mineralisable and biomass N determined at regular interval times. The results show that the distribution of the mineralisable N varied with layer as well as with plant growth stage: being higher in cultivated layer than in deep layer
and lower and stable in early stage while 1 time higher in late stage. Application of N fertilizer had no obvious influence on the mineralisable N whereas application of organic fertilizer increased its contents in late stage of the plant growth. The effects of kinds of plants and plantation systems(i.e.
with plantation or with no plantation) on mineralisable N were much less than sampling times. The mineralisable N released during plant growth period was only 12% of the biomass N
and there was no correlation between them. It seemed that the biomass N could hardly reflect the N-supplying capacities of a soil.
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