丛枝菌根真菌接种对喀斯特石漠化人工林土壤特性的影响
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1.中南林业科技大学;2.邵阳县林业局

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Effects of the Arbuscular Mycorrhizal Fungi Inoculation on Soil Properties of Plantations in Karst Rocky Desertification Areas
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Central South University of Forestry and Technology

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    摘要:

    【目的】阐明丛枝菌根真菌(AMF)接种对土壤养分水分供给不足的削减机制,支撑喀斯特脆弱生态系统的可持续恢复。【方法】基于湖南省邵阳县典型喀斯特石漠化区人工林样地的原位接种试验,分别采集上、中、下坡0~15、15~30 cm土层细根和0~15、15~30、30~50 cm土层土壤样品测定AMF侵染状况、群落组成和土壤理化性质,明确关键微生物添加对土壤养分水分等特性的影响。【结果】结果表明:接种提升根系AMF侵染强度和侵染率;属水平上,类球囊霉属、球囊霉属和双型囊霉属是AMF群落的优势属,其相对丰度在接种后变化较大,且在不同坡位和土层间存在差异。接种后,Simpson多样性指数在0~15 cm土层各坡位、15~30 cm土层中坡、30~50 cm土层中下坡皆有所增加,但差异不显著;Chao1丰富度指数皆呈增加变化,但仅在0~15 cm土层上坡差异显著;Pielou均匀度指数在0~15 cm土层上中坡、15~30 cm土层中坡、30~50 cm土层各坡位皆呈增加变化,差异皆不显著。各土层碱解氮质量分数皆呈减少变化,速效磷质量分数仅在15~30 cm土层有所下降,土壤有机碳质量分数在0~15、15~30 cm土层呈减少变化,但差异皆不显著;水分体积分数在各土层皆极显著增加,毛管孔隙在0~15、30~50 cm土层有所增加,pH和交换性Ca2+在各土层皆有所降低,但差异皆不显著。速效养分氮磷比在0~15、15~30 cm土层呈降低趋势,表明接种AMF可在一定程度缓解土壤养分磷的限制。土壤特性间相关性和冗余分析表明,接种后微生物群落组成的变化会直接或间接影响养分水分等理化性状。【结论】研究结果厘清石漠化人工林土壤特性对AMF接种的响应特征,明确养分水分变化及其驱动因素,有助于突破土壤生态功能恢复滞后瓶颈,提升脆弱生态系统服务功能。

    Abstract:

    [Objective] Clarifying the reduction mechanism of arbuscular mycorrhizal fungi (AMF) inoculation in insufficiency of soil nutrient and water supply, can realize the sustainable restoration of fragile karst ecosystems. [Methods] Based on the in-situ inoculation experiment in plantations in typical karst rocky desertification areas of Shaoyang County, Hunan Province, this study collected 0-15 and 15-30 cm fine roots and 0-15, 15-30, and 30-50 cm soil samples in different slopes (upper, middle, and lower slopes), to determine the infestation and community composition of AMF and physicochemical properties. Effects of key microorganism addition on soil properties such as nutrient and water were studied. [Results] The results showed that, inoculation increased the intensity and rate of AMF infestation in roots. At the generic level, Paraglomus, Glomus, and Ambispora were the dominant genera in AMF community composition. After inoculation, changes in their relative abundances were obviously and varied in different slopes and soil layers. Simpson diversity index in 0-15 cm increased at all slopes, while that in 15-30 cm increased only at middle slope and in 30-50 cm increased at middle and lower slopes, with no significant changes; all Chao1 richness indexes increased, but differed significantly only in 0-15 cm at upper slope; Pielou evenness index increased in 0-15 cm at upper and middle slopes, in 15-30 cm at middle slope, and in 30-50 cm at all slopes, with no significant changes. Alkali-hydrolyzed nitrogen (AN) concentration decreased in different soil layers, while available phosphorus (AP) concentration decreased only in 15-30 cm. Soil organic carbon concentration decreased in 0-15 and 15-30 cm, with no significant changes. Volumetric water content increased significantly in different soil layers. Capillary pores increased in 0-15 and 30-50 cm, with no significant changes. Values of pH and exchangeable Ca2+ decreased in all soil layers, with no significant changes. The ratios of AN∶AP decreased at 0-15 and 15-30 cm, indicating that the inoculation of AMF could alleviate the restriction of soil P to some extent. Correlation and redundancy analysis among soil properties showed that the changes in microbial community composition after inoculation could directly or indirectly affect soil physical and chemical conditions such as nutrient and water. [Conclusion] The results clarify the response characteristics of soil properties to AMF inoculation in plantations of rocky desertification areas, and clear the changes in nutrient and water with showing the drivers, which is helpful to break the bottleneck of soil ecological function restoration lag and improve the service function of fragile ecosystems.

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  • 收稿日期:2025-02-27
  • 最后修改日期:2025-04-21
  • 录用日期:2025-05-20
  • 在线发布日期: 2025-07-07
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