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节水减氮调控盐渍土壤细菌氮代谢途径阻控氮素损失

Water-saving and nitrogen-reducing regulation of bacterial nitrogen metabolism pathways in the salt-affected soil to control nitrogen loss

  • 摘要: 为阐明节水减氮如何调控根际土壤细菌氮代谢途径以阻控氮素损失,该研究2023—2024年于内蒙古土默川平原灌区开展田间小区试验,以当地常规水氮管理即现蕾期施氮200 kg/hm2,灌水450 m3/hm2为对照(CK),设计现蕾期轻中度水分亏缺(W1:300 m3/hm2;W2:150 m3/hm2)、现蕾期减氮25%与50%(N1:150 kg/hm2;N2:100 kg/hm2)共5个处理。结果表明,轻度水分亏缺(W1)与减氮25%(N1)处理显著改善根际土壤环境并促进根系生长,W1与N1处理显著促进现蕾期与成熟期根系分泌草酸与柠檬酸,并提高根长密度;W1处理增加现蕾期根际土壤K+与成熟期Ca2+含量,降低开花期根际Na+含量;然而中度水分亏缺(W2)与减氮50%(N2)虽能显著降低现蕾期根际Cl-与SO42−含量,却对根表面积密度值(RSAD)无显著促进作用。氮代谢细菌群落结构方面,W1处理显著提升苗期、现蕾期、开花期与成熟期根际土壤细菌群落Chao1、Observed_species与Ace指数(P<0.05),然而W2处理显著降低现蕾期Chao1指数和Observed_species指数。氮代谢途径方面,N1处理显著减小开花期根际细菌norBnirKnapA相对丰度,提高根际细菌nxrA相对丰度,形成“高硝化-低反硝化”氮代谢模式,增加开花期根际土壤氮素损失风险;节水减氮处理(W1、N1、N2)显著减小现蕾期根际细菌nxrAnorBnirKnapA相对丰度;W1处理还显著提高现蕾期根际细菌nosZ相对丰度(11.16%),不仅在源头上阻控根际土壤氮素损失,还能促进N2还原,减少温室气体N2O的排放潜力。综上,现蕾期轻度水分亏缺有效降低盐渍农田向日葵根际土壤氮素损失风险、改善根际土壤离子环境并促进植株根系生长,兼具农业节水与环境保护的双重效益。

     

    Abstract: To elucidate how water-saving and nitrogen-reducing practices regulate bacterial nitrogen metabolism pathways in the rhizosphere to control nitrogen loss, field plot experiments were conducted in the irrigation district of the Tumuchuan Plain from 2023 to 2024. Using local conventional water-nitrogen management (nitrogen application of 200 kg/hm2 with irrigation of 450 m3/hm2 at the bud stage) as the control, five treatments were established, combining deficit irrigation (300 m3/hm2 mild deficit and 150 m3/hm2 moderate deficit) with reduced nitrogen application by 25% (150 kg/hm2, medium nitrogen) and 50% (100 kg/hm2, low nitrogen) at the bud stage. Results indicated that compared to the CK treatment, both the mild water deficit (W1) and the 25% nitrogen reduction (N1) treatments demonstrated significant advantages in improving the rhizosphere soil environment and promoting root growth. The W1 and N1 treatments significantly increased oxalate and citrate content in the rhizosphere at both the bud stage and maturation, while also increasing root length density (RLD). Furthermore, the W1 treatment increased K+ content during the bud stage and Ca2+ content at the maturation, while reducing Na+ content during the anthesis. However, moderate water deficit (W2) combined with 50% nitrogen reduction (N2) significantly decreased Cl and SO42− content in the rhizosphere during the bud stage but failed to significantly enhance the root surface area density (RSAD). Regarding bacterial community structure, the W1 treatment significantly increased the Chao1, Observed_species, and Ace indices of nitrogen-metabolising bacterial communities in the rhizosphere soil during the seedling stage, bud stage, Anthesis, and Maturation (P<0.05). However, the W2 treatment significantly reduced the Chao1 and Observed_species indices during the bud stage. Regarding nitrogen metabolism pathways, the N1 treatment during the anthesis significantly reduced the relative abundance of rhizosphere bacteria norB, nirK, and napA while increasing the relative abundance of nxrA, establishing a ‘high nitrification-low denitrification’ pattern that increased the risk of nitrogen loss from the rhizosphere soil at this stage. During the bud stage, water-saving and nitrogen-reducing treatments (W1, N1, N2) significantly reduced the relative abundance of rhizosphere bacteria nxrA, norB, nirK, and napA; The W1 treatment also significantly increased the relative abundance of rhizosphere bacterial nosZ (11.16%) during the bud stage. This not only controls nitrogen loss from rhizosphere soil at its source but also promotes N2 reduction, thereby reducing the potential for N2O greenhouse gas emissions. In summary, mild water deficit during the bud stage effectively reduces the risk of nitrogen loss from sunflower rhizosphere soils in saline-affected farmland, improves the rhizosphere ionic environment, and promotes plant root growth, delivering dual benefits of agricultural water conservation and environmental protection.

     

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