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冻融循环期高寒草原典型物种紫花针茅氮吸收策略
引用本文:庞博,洪江涛,马星星,秦小静,王小丹.冻融循环期高寒草原典型物种紫花针茅氮吸收策略[J].生态学报,2023,43(3):1147-1155.
作者姓名:庞博  洪江涛  马星星  秦小静  王小丹
作者单位:中国科学院、水利部成都山地灾害与环境研究所, 成都 610041;申扎高寒草原与湿地生态系统观测试验站, 申扎 853100;中国科学院大学, 北京 100049;山西师范大学, 太原 030006;河南理工大学, 焦作 454000
基金项目:国家重点研发计划项目(2019YFD1100504);第二次青藏高原科学考察研究(2019QZKK0404);国家自然科学基金(41701343)
摘    要:氮(N)是高山和极地生态系统重要的限制性生长因子。目前对冻土区植物N利用机制的研究主要集中于完全融化期,而冻融循环期植物N吸收策略仍存在不确定性。以高寒紫花针茅为研究对象,分别在冻结期(晚秋)和融化期(早春)采用同位素示踪技术,分析植物对(15NH4)2SO4和Na15NO3的吸收量与偏好动态变化。研究结果显示冻结期紫花针茅冠层生长已停滞,融化期冠层尚未返青,但根系和立枯均可以吸收同化15N,具备吸收养分的需求。融化期紫花针茅15N在标记21天后15N-NH+415N-NO-3的总回收率分别为4.44%和6.91%,而冻结期紫花针茅在15N标记21天后15N-NH+415...

关 键 词:氮偏好  硝态氮  铵态氮  冻土  冻结期  融化期
收稿时间:2021/10/8 0:00:00
修稿时间:2022/7/3 0:00:00

Nitrogen absorption strategy of Stipa purpurea, a typical species in alpine grassland during freeze-thaw cycle
PANG Bo,HONG Jiangtao,MA Xingxing,QIN Xiaojing,WANG Xiaodan.Nitrogen absorption strategy of Stipa purpurea, a typical species in alpine grassland during freeze-thaw cycle[J].Acta Ecologica Sinica,2023,43(3):1147-1155.
Authors:PANG Bo  HONG Jiangtao  MA Xingxing  QIN Xiaojing  WANG Xiaodan
Institution:Institute of Mountain Hazards and Environment (IMHE), Chinese Academy of Sciences, Chengdu 610041, China;Xainza Alpine Steppe and Wetland Ecosystem Observation Station, Xainza 853100, China;University of Chinese Academy of Sciences, Beijing 100049, China;Shanxi Normal University, Taiyuan 030006, China;Henan Polytechnic University, Jiaozuo 454000, China
Abstract:Nitrogen is an important limiting growth factor in alpine and polar ecosystems. At present, the research on the mechanism of plant N utilization in permafrost area mainly focuses on the complete thawing period, while the strategy of plant N absorption in the freeze-thaw cycle is still uncertain. In this study, the absorption and preference of plants for (15NH4)2SO4 and Na15NO3 were analyzed by isotope tracer technology in freezing period (late autumn) and thawing period (early spring). The results showed that the growth of Stipa purpurea canopy had stagnated in the freezing period, and its canopy had not turned green in the thawing period, but the root system and standing dry could absorb and assimilate 15N, which had the need to absorb nutrients. The total recoveries of 15N-NH4+ and 15N-NO3- in thawing stage were 4.44% and 6.91% respectively after 21 days of 15N labeling, while the total recoveries of 15N-NH4+ and 15N-NO3- in freezing stage were 8.65% and 3.55%, respectively. In the early stage of thawing, the overall recovery of 15N-NH4+ was higher than 15N-NO3-, but in the later thawing stage of thawing, the recovery of 15N-NH4+ and 15N-NO3- was not significant or 15N-NO3- was slightly higher. The recovery rate of 15N-NH4+ was higher than that of 15N-NO3- in the whole freezing period. This study supplements the nutrient absorption data of plants in the non-growing season in the alpine permafrost region, and provides a scientific basis for a comprehensive understanding of plant N nutrition strategy in the permafrost region and its response to future climate change.
Keywords:nitrogen preference  nitrate nitrogen  ammonium nitrogen  permafrost  freezing period  thawing period
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