丛枝菌根真菌接种介导石漠化植物-土壤性质变化对氮积累时空分布的影响
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国家自然科学基金项目(32271722,32060281);云南省高原湿地保护修复与生态服务重点实验室


Effects of plant-soil changes on spatiotemporal distribution of nitrogen component accumulation under the arbuscular mycorrhizal fungi inoculation in rocky desertification areas
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    摘要:

    为探明丛枝菌根真菌接种处理下石漠化"植物-土壤环境变化"对氮组分含量时空分布的影响规律,选取云南弥勒白枪杆(Fraxinus malacophylla)为供试寄主植物,分别接种摩西斗管囊霉(Funneliformis mosseae,FM)、幼套近明球囊霉(Claroideoglomus etunicatum,CE)和根内根孢囊霉(Rhizophagus intraradices,RI),并设置对照处理(不添加菌种,CK),揭示不同丛枝菌根(Arbuscular mycorrhiza,AM)真菌接种处理下土壤氮库各组分(全氮、水解氮、铵态氮、硝态氮)含量及占比(水解氮/全氮、铵态氮/全氮、硝态氮/全氮)的时空变化特征,分析植物生长和土壤性质变化对氮组分含量时空分布特征的影响。结果表明:1)AM真菌接种显著促进了土壤氮组分含量及其占比的积累(P < 0.05)。相较于对照,3种菌种处理对4种氮组分含量的提升率达12.09%-156.88%,对水解氮、铵态氮和硝态氮含量占比的提升率变幅达13.25%-60.07%;不同AM菌种对各氮组分含量及占比的提升率均表现为FM > CE > RI。2)不同菌种处理下土壤氮组分含量及占比的时空变化存在差异。除全氮含量在6月最大,其余3种氮组分含量在9月最大,不同菌种处理下各氮组分含量沿土层的减幅大小顺序均表现为:RI > FM > CE;不同菌种处理下水解氮、铵态氮和硝态氮含量占比均在9月最大,其沿土层的减幅均表现为:FM > CE > RI。3)相较于对照,AM真菌处理显著提升树高、地径、根系生物量、土壤含水率及碳组分(总有机碳、易氧化碳、微生物量碳)、磷组分(全磷、有效磷)、钾组分(全钾、有效钾)含量,但降低了土壤pH及容重,FM处理对总有机碳提升率(72.25%)最大,RI处理对有效磷的提升率(1.49%)最小。4)冗余分析表明,土壤总有机碳、易氧化碳、微生物量碳、全磷是氮组分含量积累的主要驱动因子,根系生物量、易氧化碳、微生物量碳是氮组分含量占比增加的主控因子。因此,AM真菌接种通过介导根系生物量及土壤碳磷含量变化,进而调控土壤氮组分含量积累与分配的时空分布。

    Abstract:

    This study aimed to expound the effects of the changes in plant and soil environments on spatiotemporal distribution of nitrogen component accumulation under the arbuscular mycorrhizal fungi inoculation in rocky desertification areas. The Fraxinus malacophylla was selected as the host plant and it was inoculated with Funneliformis mosseae (FM), Claroideoglomus etunicatum (CE), and Rhizophagus intraradices (RI), using no fungal inoculation as the control treatment. The effects of changes in plant growth and soil physicochemical properties on the spatiotemporal variations in soil nitrogen components (i.e., total nitrogen, hydrolyzabl nitrogen, ammonium nitrogen, nitrate nitrogen) and their proportion (i.e., hydrolyzable nitrogen/total nitrogen, ammonium nitrogen/total nitrogen, nitrate nitrogen/total nitrogen) were identified under different AM inoculation. The results were as follows: 1) AM fungal inoculation significantly increased the values of soil nitrogen components and their proportion (P < 0.05). Compared with the control, the concentrations of the four nitrogen fractions increased from 12.09% to 156.88% in three fungal treatments, while the increasing rates of the proportion of hydrolyzabl nitrogen, ammonium nitrogen, and nitrate nitrogen in total nitrogen ranged from 13.25% to 60.07%. The increase in the vales of soil nitrogen components and their proportion ranked as FM > CE > RI. 2) The levels of soil nitrogen components and their proportion had spatiotemporal variations in the three fungal inoculation treatments. The maximum accumulation of the total nitrogen occurred in June, while that of the other nitrogen components occurred in September. They all decreased along the soil layer and the order of reduction magnitude for the four nitrogen components was FM > CE > RI. The maximum proportion rates of the hydrolyzable, ammonium, nitrate components were all in September. The proportion of the three nitrogen components decreased along the soil layer and was ranked as FM > CE > RI. 3) The AM fungal treatments significantly increased ground diameter, tree height, root biomass, soil carbon components (total organic carbon, readily oxidizable carbon, and microbial carbon), phosphorus components (total and available phosphorus), potassium components (total and available potassium), and water content compared with that of the control. In contrast, they significantly decreased soil pH and bulk density. The total organic carbon was at its maximum (72.25%) under FM treatment, while the available phosphorus was at its minimum (1.49%) under RI treatment. 4) Redundancy analysis showed that total organic carbon, readily oxidizable carbon, microbial carbon, and total phosphorus were the main driving factors affecting nitrogen component accumulation, while root biomass, readily oxidizable carbon, and microbial carbon were the main controlling factors of nitrogen component proportion. Therefore, AM fungal inoculation promoted nitrogen component accumulation and proportion through mediating the alterations in root biomass as well as soil carbon and phosphorus concentrations.

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兰梦杰,王邵军,李瑞,罗双,夏佳慧,杨胜秋,郭晓飞,解玲玲,肖博,王郑钧,郭志鹏.丛枝菌根真菌接种介导石漠化植物-土壤性质变化对氮积累时空分布的影响.生态学报,2025,45(1):112~127

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