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Alternate partial root-zone irrigation induced dry/wet cycles of soils stimulate N mineralization and improve N nutrition in tomatoes

机译:交替进行的局部根区灌溉可引起土壤的干/湿循环,从而刺激番茄中的氮矿化并改善氮素营养

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Given the same amount of irrigation volume, applying alternate partial root-zone irrigation (PRI) has improved crop N nutrition as compared to deficit irrigation (DI), yet the mechanisms underlying this effect remain unknown. Therefore, the objective of this study was to investigate whether PRI induced soil dry/wet cycles facilitate soil organic N mineralization hereby contributing to the improvement of N nutrition in tomatoes. The plants were grown in split-root pots in a climate-controlled glasshouse and were subjected to PRI and DI treatments during early fruiting stage. 15N-labeled maize residues were incorporated into the soils. Results showed that PRI resulted in 25% higher net 15N mineralization than did DI, indicating that the enhanced mineralization of soil organic N alone could account for the 16% increase of N accumulation in the PRI than in the DI plants. The higher net N mineralization under PRI was coincided with an intensified soil microbial activity. In addition, even though soil chloroform fumigation labile carbon (CFL-C, as an index of microbial biomass) was similar for the two irrigation treatments, a significant increase of chloroform fumigation labile nitrogen (CFL-N) was found in the PRI wetting soil. Consequently, the C:N ratio of the chloroform fumigation labile pool was remarkably modified by the PRI treatment, which might indicate physiological changes of soil microbes or changes in labiality of soil organic C and N due to the dry/wet cycles of soils, altering conditions for net N mineralization. Moreover, in both soil compartments PRI caused significantly less extractable organic carbon (EOC) as compared with DI; whilst in the PRI wetting soil significantly higher extractable organic nitrogen (EON) was observed. A low EOC:EON ratio in the PRI wetting soil may indicate an increasing net mineralization of the organic N as a result of microbial metabolism. Conclusively, PRI induced greater microbial activity and higher microbial substrates availability are seemingly responsible for the enhanced net N mineralization and improved N nutrition in tomato plants.
机译:在灌溉量相同的情况下,与亏缺灌溉(DI)相比,进行局部根区交替灌溉(PRI)改善了作物的氮素营养,但仍不清楚这种作用的机理。因此,本研究的目的是调查PRI诱导的土壤干/湿循环是否有助于土壤有机氮矿化,从而有助于改善番茄中的氮营养。将这些植物种植在气候受控的温室中的开根花盆中,并在结实初期进行PRI和DI处理。将 15 N标记的玉米残留物掺入土壤中。结果表明,PRI导致的净 15 N矿化度比DI高25%,这表明,仅土壤有机氮矿化作用的增强可导致PRI中氮积累的增加16%。 DI植物。 PRI下较高的净氮矿化与土壤微生物活性增强同时发生。此外,尽管两种灌溉处理的土壤氯仿熏蒸不稳定碳(CFL-C,作为微生物生物量的指标)相似,但在PRI湿润土壤中发现氯仿熏蒸不稳定氮(CFL-N)显着增加。 。因此,PRI处理显着改变了氯仿熏蒸不稳定池的C:N比值​​,这可能表明由于土壤的干/湿循环,土壤微生物的生理变化或土壤有机碳和氮的硬度变化,改变了净氮矿化的条件。此外,与DI相比,在两个土壤隔室中PRI引起的可提取有机碳(EOC)明显减少。而在PRI湿润土壤中,观察到较高的可萃取有机氮(EON)。 PRI湿润土壤中的EOC:EON比率低可能表明由于微生物代谢,有机氮的净矿化增加。结论是,PRI诱导的更大的微生物活性和更高的微生物底物利用率似乎是导致番茄植物净氮矿化增加和氮营养改善的原因。

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