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生态学杂志 ›› 2020, Vol. 39 ›› Issue (8): 2528-2537.

• 研究报告 • 上一篇    下一篇

中亚热带杉木人工幼林林下植被生物量对短期增温和隔离降雨交互作用的响应

李超1,2,林伟盛1,2*,杨智杰1,2,刘小飞1,2,陈仕东1,2,郑蔚1,2,纪宇皝1,2     

  1. 1福建师范大学地理科学学院, 福州 350007; 2湿润亚热带山地生态国家重点实验室培育基地, 福州 350007)
  • 出版日期:2020-08-10 发布日期:2021-02-10

Interactive effects of shortterm warming and precipitation exclusion on undergrowth vegetation biomass in a Chinese fir (Cunninghamia lanceolata) plantation in midsubtropical China.

LI Chao1,2, LIN Wei-sheng1,2*, YANG Zhi-jie1,2, LIU Xiao-fei1,2, CHEN Shi-dong1,2, ZHENG Wei1,2, JI Yu-huang1,2   

  1. (1School of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China; 2Cultivation Base of State Key Laboratory of Humid Subtropical Mountain Ecology, Fuzhou 350007, China).
  • Online:2020-08-10 Published:2021-02-10

摘要: 通过在野外条件下设置对照(CT)、土壤增温(W,+5 ℃)、隔离降雨(P,隔离50%降雨量)以及增温与隔离降雨协同作用(WP)4种处理,研究增温与隔离降雨及其交互作用对中亚热带杉木人工林林下植被生物量的影响,结果表明:增温和隔离降雨及其交互作用显著影响杉木人工林林下植被生物量。W和WP处理显著提高地上、地下和总生物量,其中W处理地上、地下和总生物量增加比例均高于WP处理;隔离降雨导致地下部分生物量显著减少;增温、隔离降雨及其交互作用均导致林下植被根冠比值下降。土壤温度升高是导致植被地上、地下和总生物量以及根冠比值变化的根本原因,而土壤溶液中可溶性碳氮及矿质元素浓度的变化可能是导致植被地上、地下和总生物量变化的直接原因。其中,Al3+、Fe3+、Ca2+浓度的降低可能是导致增温后杉木林林下植被地上、地下和总生物量显著增加的原因;Al3+、Na+浓度的增加可能是导致隔离降雨后林下植被地下部分生物量下降的原因。本研究从土壤溶液养分组成变化的角度,探讨增温、隔离降雨及其交互作用对中亚热带杉木幼林林下植被生物量的影响,研究结果可为全球气候变化背景下森林生态系统碳循环研究与森林经营提供重要理论依据。

关键词: 增温, 隔离降雨, 林下植被生物量, 土壤溶液, 矿质元素浓度

Abstract: We examined the interactive effects of soil warming and precipitation exclusion on understory vegetation biomass in Chinese fir (Cunninghamia lanceolata) plantation in subtropical China, with factorial treatments of soil warming (W, +5 ℃ above the ambient temperature) and 50% of precipitation exclusion (P) in a mesocosm experiment. The results showed that soil warming, precipitation exclusion and their interaction had significant effects on understory vegetation biomass. The above and belowground biomass increased significantly in the treatments of W and WP, with the increasing proportion being higher in W treatment. The P treatment significantly decreased belowground biomass. Root/shoot ratio decreased in the treatments of W, P and WP. The responses of above and belowground biomass and root/shoot ratio were primarily caused by the increase of soil temperature. However, the changes of dissolved carbon and nitrogen and mineral element concentrations of soil solution might directly affect undergrowth biomass. The increase in undergrowth biomass of different parts in the W treatment was significantly related to the decreases of the concentrations of Al3+, Fe3+ and Ca2+, while the increases of Al3+ and Na+ concentrations in P treatment might reduce belowground biomass. This study focuses on the main and interactive effects of increasing temperature and precipitation exclusion on the undergrowth biomass of Chinese fir plantation from the perspective of soil nutrient composition changes. The results can provide important theoretical basis for study of carbon cycling and forest management under the background of climate change.

Key words: warming, precipitation exclusion, undergrowth biomass, soil solution, mineral element concentration.