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林业科学 ›› 2001, Vol. 37 ›› Issue (3): 126-138.doi: 10.11707/j.1001-7488.20010321

• 论文及研究报告 • 上一篇    下一篇

森林细根生产和周转研究

张小全 吴可红   

  1. 中国林业科学研究院森林生态环境与保护研究所,北京100091;Institute of Forest Botany, University of Goettingen,Buesgenweg 2, Goettingen, D-37077, Germany
  • 收稿日期:1999-12-02 修回日期:1900-01-01 出版日期:2001-05-25 发布日期:2001-05-25

FINE-ROOT PRODUCTION AND TURNOVER FOR FOREST ECOSYSTEMS

Zhang Xiaoquan,Wu Kehong   

  1. Institute of Forest Ecology and Environment, the Chinese Academy of Forestry Beijing100091;Institute of Forest Botany, University of Goettingen,Buesgenweg 2, Goettingen, D-37077, Germany
  • Received:1999-12-02 Revised:1900-01-01 Online:2001-05-25 Published:2001-05-25

摘要:

随着近20多年来对细根功能的深入认识和研究方法的发展,林分细根生物量、生产和周转及其与环境因子的关系成为森林生态学的研究热点之一,开展了大量研究。本文在收集了大量研究报道基础上,对森林细根研究结果进行综述。结果如下:细根(直径<2~5mm)生物量变化在46~2805g·m-2之间,大部分在100~1000g·m-2;细根生物量分别占地下部分总生物量和林分总生物量的3%~30%和0.5%~10%;北方常绿针叶林平均细根生物量最低(216g·m-2) ,热带常绿阔叶林最高(1087g·m-2)。细根年净生产量20~1317g·m-2·a-1,占林分总净初级生产量的3%~84% ,大部分在10%~60%;从北方森林到温带、亚热带至热带森林,细根生产量呈增加趋势;针叶林细根生产在总净初级生产中的比例小于阔叶林(常绿和落叶)。树木细根生命周期短至数天,长达数年。细根年周转率4.3%~273.2% ,阔叶林细根周转率低于针叶林。细根生产和周转是土壤碳和养分的重要来源,细根生产向林地输入的生物量占总输入(细根生产和地上枯落物输入)的6.2%~88.7%。除气候森林类型外,森林生态系统细根生物量、分布、生产、周转还因季节、土壤类型、立地条件和生长发育阶段而异。同时,还受树木体内碳源-碳汇分配关系的控制,涉及地上净同化量、根系生长和维持所需的碳水化合物量以及根系生长的微环境因子,包括土壤养分、水分、养分有效性及土壤温度、有毒元素、菌根和其它土壤因子等。

关键词: 森林, 细根, 生物量, 生产, 生命周期, 周转

Abstract:

The fine-root biomass and its vertical distribution, production, turnover, lifespan of global major climatic forest types and its role in C and nutrient cycling of forest ecosystems were reviewed and evaluated based on published information and 169 data sets. The fine-root biomass varied from 46 to 2805g·m-2, mostly between 100~1000 g·m-2, accounting for 3%~30% and 0.5%~10% respectively of below-ground biomass and total biomass of ecosystems. Boreal evergreen needleleaf forest had the lowest average fine-root biomass (216 g·m-2) while tropical evergreen broadleaf forest had the highest (1087g·m-2). Annual fine-root net primary production (NPP) was 20~1317 g·m-2·a-1, amounting to 3%~84% of total stand NPP, mostly 10%~60%. The fine-root NPP tended to increase from boreal forest, through cold-temperate, warm-temperate and subtropical forest, to tropical forest ecosystem. The percentage of fine-root NPP in total NPP of needleleaf forest seems lower than that of broadleaf forest within same climatic zone. The fine-root lifespan of tree species varied from several days to years, with annual fine-root turnover between 4.3%~273.2%. The necromass input through fine-root turnover accounted for 6.2%~88.7% of total input from both above- and below-ground, indicating substantial amount of C and nutrients input from the fine-root production and turnover. Apart from the climatic forest type, fine-root biomass, production and turnover varied with seasons, soil type, site conditions, development stage of forest and etc. They are also controlled by carbon source-sink relations, involving above-ground assimilation,carbonhydrate needed for fine-root growth and maintenance and site-specific conditions such as soil nutrients, water, temperature, toxic element, mycorhiza and other soil factors.

Key words: Forest, Fine-root, Biomass, Production, Turnover, Lifespan