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Manipulating the N release from 15N labelled celery residues by using straw and vinasses.

机译:通过使用稻草和酒桶处理15N标记的芹菜残渣中的N释放。

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The aim of this laboratory study was to investigate the effect of straw and vinasses on the nitrogen (N) mineralization-immobilization turnover of celery residues during two periods (each simulating a time period from autumn till spring) under laboratory conditions. During the first period (1-198 d), 15N-labelled celery residues (1.1 g dry matter (DM) kg-1 soil) were incubated together with straw (8.1 g DM kg-1 soil), aiming to immobilize the N released from celery residues, followed by an incorporation of vinasses (1.9 g DM kg-1 soil) after 84 d, with a view to remineralizing the immobilized celery-N. During the second period (198-380 d), the experimental set-up was repeated, except that non-labelled celery residues were used. Total N, mineral N and their 15N enrichments as well as microbial biomass N were determined at regular time intervals. During both periods, mixing celery residues with straw significantly increased microbial biomass N (90.5 and 40.5 mg N kg-1 extra compared to celery only treatment) and decreased the amount of mineral N (reduction of 56.1 and 45.9 mg N kg-1 soil compared to celery only treatment) and the celery-derived mineral 15N (0% of mineral celery-derived 15N in straw treatment compared to 35% of mineral celery-derived 15N in celery only treatment). After maximum immobilization, a natural remineralization (without addition of vinasses) of 32.2 (at day 198) and 11.1 mg N kg-1 soil (at day 380) occurred in the straw treatment, but the mineral N content remained significantly lower than in the celery only treatment during the complete experiment, and the amount of remineralized celery-15N was very low (5.4% of celery-derived 15N after 380 d). Vinasses caused no real priming effect, although it did slightly increase the amount of remineralized celery-15N (+6.4% of celery-derived 15N at day 380 compared to the straw treatment), probably due an apparent added N interaction caused by displacement reactions with the soil microbial biomass..
机译:这项实验室研究的目的是研究在实验室条件下的两个时期(每个时期模拟从秋天到春季)芹菜和酒糟对芹菜残渣氮(N)矿化固定化周转的影响。在第一阶段(1-198 d),将15N标记的芹菜残渣(1.1 g干物质(DM)kg-1土壤)与稻草(8.1 g DM kg-1土壤)一起孵育,以固定释放的氮从芹菜渣中提取,然后在84天后掺入酒糟(1.9 g DM kg-1土壤),以使固定化的芹菜N矿化。在第二阶段(198-380 d),重复实验设置,不同的是使用了未标记的芹菜残留物。以固定的时间间隔确定总氮,矿物质氮及其15N富集以及微生物生物量N。在这两个时期中,将芹菜残留物与秸秆混合显着增加了微生物生物量氮(与仅芹菜处理相比增加了90.5和40.5 mg N kg-1)并减少了矿质N的量(与之相比减少了56.1和45.9 mg N kg-1 (仅限于芹菜处理)和源自芹菜的矿物质15N(秸秆处理中占芹菜矿物的15N的0%,而仅限芹菜处理中占矿物芹菜的15N的35%)。最大限度地固定化之后,秸秆处理中发生了32.2(在第198天)和11.1 mg N kg-1的土壤(在第380天)的自然矿化(不添加酒糟),但矿质N含量仍然显着低于土壤中的N。在整个实验期间仅进行芹菜处理,而再矿化的芹菜15N的量非常少(380天后,芹菜来源的15N的5.4%)。酒糟没有引起真正的引发作用,尽管它确实略微增加了再矿化的芹菜15N的量(与秸秆处理相比,在380天时,芹菜来源的15N的含量增加了6.4%),这可能是由于明显的氮交互作用所引起的,土壤微生物量

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