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草业学报 ›› 2022, Vol. 31 ›› Issue (5): 115-123.DOI: 10.11686/cyxb2021375

• 研究论文 • 上一篇    

退化沙质草地菌根对细根分解过程中营养元素释放的影响

丁杰萍1(), 罗永清2(), 刘伟春3, 温飞1, 王立龙2, 王旭洋2, 段育龙2, 连杰2   

  1. 1.甘肃省生态环境科学设计研究院,甘肃 兰州 730020
    2.中国科学院西北生态环境资源研究院奈曼沙漠化研究站,甘肃 兰州 730000
    3.内蒙古自治区库伦旗农业技术推广中心,内蒙古 通辽 028200
  • 收稿日期:2021-10-19 修回日期:2021-11-23 出版日期:2022-05-20 发布日期:2022-03-30
  • 通讯作者: 罗永清
  • 作者简介:Corresponding author. E-mail: luoyongqing@nieer.ac.cn
    丁杰萍(1987-),女,副高级工程师,硕士。E-mail: dingjieping1@163.com
  • 基金资助:
    陇原青年创新创业人才(团队)项目(黄河流域甘肃段水污染防治研究),甘肃省自然科学基金项目(20JR10RA442);国家自然基金项目(31500369)

Effects of mycorrhiza on nutrient release during fine root decomposition in degraded sandy grassland

Jie-ping DING1(), Yong-qing LUO2(), Wei-chun LIU3, Fei WEN1, Li-long WANG2, Xu-yang WANG2, Yu-long DUAN2, Jie LIAN2   

  1. 1.Gansu Academy of Eco-environmental Sciences,Lanzhou 730020,China
    2.Naiman Desertification Research Station,Northwest Institute of Eco-environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China
    3.Agricultural Technology Extension Center of Kulun Banner of Inner Mongolia Autonomous Region,Tongliao 028200,China
  • Received:2021-10-19 Revised:2021-11-23 Online:2022-05-20 Published:2022-03-30
  • Contact: Yong-qing LUO

摘要:

细根分解过程中的营养元素释放是低覆盖度植被区土壤物质循环的关键环节,菌根在该过程中的作用目前尚不明确。本研究以退化沙质草地植被恢复过程中的先锋灌木差不嘎蒿为对象,采用内生芯法,分别研究了活细根+菌根、菌根以及无根(对照)处理下其细根分解过程中的营养元素(氮、磷、钾)释放动态。结果表明:菌根对差不嘎蒿细根分解过程中营养元素含量的影响主要发生在分解后期(1 a以后)。当分解超过1 a,菌根的存在显著降低了细根氮含量,这种效应不受活的细根的影响,菌根+活细根以及菌根处理下的氮含量分别较对照低15.3%和9.5%;而对于磷和钾,菌根处理下的含量均显著低于对照(P<0.05),但该效应受活根的影响,活细根+菌根处理下的差不嘎蒿磷含量与钾含量均与对照无显著差异(P>0.05);从营养元素的物质残留动态分析发现,菌根显著促进了分解细根中氮素的释放(P<0.05),这种促进效应主要发生在分解的中期;而对于磷和钾主要发生在分解的后期,且受活细根干扰。研究结果表明,菌根是影响根系分解过程中营养元素释放的关键要素,在植物根系分解及其与土壤物质周转关系的研究中应当重点关注。

关键词: 菌根, 细根分解, 营养元素, 内生芯法, 差不嘎蒿

Abstract:

The release of nutrients during the decomposition of fine roots is the key process in the circulation of materials in soils in low-vegetation areas, but the role of mycorrhiza in this process is unclear. In this study, we explored the dynamics of nutrient (nitrogen, phosphorus, potassium) release during the fine root decomposition of Artemisia halodendron, a pioneer shrub during vegetation restoration in degraded sandy grassland. The in-growth core method was used to collect samples from two treatments (living fine roots+mycorrhiza, and mycorrhiza only) and a root-free control. We found that mycorrhiza affected the nutrient contents of A. halodendron fine root litter during decomposition, with the strongest effect at the later stage of the decomposition period (after 1 year). When the decomposition period was longer than 1 year, mycorrhiza significantly reduced the N content of fine root litter, and this was not affected by presence of living fine roots. The N content of litter in the mycorrhiza+living fine roots and mycorrhiza treatments was 15.3% and 9.5% lower, respectively, than that of litter in the control. The P and K contents in fine root litter were significantly lower in the mycorrhiza treatment than in the control after 1 year of decomposition (P<0.05), but this effect was weakened by the presence of living fine roots. The P and K contents did not differ significantly between the living fine roots+mycorrhiza treatment and the control (P>0.05). Analyses of the dynamics of nutrients remaining in the litter showed that the mycorrhiza significantly promoted N release during decomposition (P<0.05), and this promoting effect mainly occurred in the middle stage of decomposition. For the release of P and K, the promoting effect of mycorrhiza was mainly at the late stage of decomposition, and the effect was weakened by the presence of living fine roots. These results indicate that mycorrhiza affect nutrient release during fine root decomposition, and should be paid more attention in research on root decomposition and its relationship with the turnover of materials in soil.

Key words: mycorrhiza, fine root decomposition, nutrient elements, in-growth core method, Artemisia halodendron