植物生态学报 ›› 2004, Vol. 28 ›› Issue (5): 704-710.DOI: 10.17521/cjpe.2004.0094

• 综述 • 上一篇    下一篇

林木细根寿命及其影响因子研究进展

梅莉1, 王政权1*, 程云环1, 郭大立2   

  1. (1东北林业大学林学院,哈尔滨150040)(2 美国J.W.Jones生态学研究中心,Georgia39870)
  • 出版日期:2004-09-30 发布日期:2015-11-03
  • 通讯作者: 梅莉

A REVIEW: FACTORS INFLUENCING FINE ROOT LONGEVITY IN FOREST ECOSYSTEMS

MEI Li1, WANG Zheng-Quan1*, CHENG Yun-Huan1, and Guo Da-Li2   

  1. (1 Forestry College,Northeast Forestry University,Harbin 150040,China)(2 Joseph W.Jones Ecological Research Center,Newton,Georgia 39870,USA
  • Online:2004-09-30 Published:2015-11-03
  • Contact: MEI Li

摘要:

细根周转要消耗大量的C,它影响森林生态系统C分配格局与过程和养分循环,对生态系统生产力具有重要意义。细根的周转取决于细根的寿命,细根寿命越短,周转越快,根系对C的消耗也越多。大量研究表明,细根的寿命与地上部分C向根系供应的多少有密切关系,同时也与细根直径大小、土壤中N和水分的有效性、土壤温度以及根际周围的土壤动物和微生物的活动有关。本文综述了国外近年来在该领域里的研究进展,特别是对控制细根寿命的机理和主要影响因子进行了评述,目的是引起国内研究者的关注,促进我国根系生态学的研究与发展。

关键词: 森林, 细根寿命, 细根周转根系C和N, 根系结构

Abstract:

Fine root is a critical determinant of root turnover and therefore carbon (C) and nutrient flow in terrestrial ecosystems. Despite the ecological importance of fine root longevity and the tremendous research efforts devoted to it,the understanding of fine root longevity and turnover is still rudimentary. This article reviews some of the most important factors that control fine root longevity,including carbon allocation,fine root structure,soil nitrogen (N) and water availability,soil temperature,and soil biota in forest ecosystems,with the purpose of providing a brief summary of recent advances in fine root longevity research and to point out the gaps of understanding and directions for future root longevity research in China.The most important function of fine roots is resource acquisition from the soil. To perform this function,C fixed in leaves must be used to build the fine root biomass and to supply energy needed for root growth,resource uptake,and maintenance of the fine roots. Consequently,C availability to roots may exert strong control over root longevity,and the interactions between C source (leaves) and C sink (roots) has been postulated as a mechanism through which root longevity may be explained. However,due to the lack of experimental evidence,the mechanisms by which C is allocated to roots and how C availability in roots controls root longevity remains poorly understood. Detailed studies on C allocation and utilization in processes such as root growth and root respiration (in growth and maintenance) are needed.In addition to physiological controls of root longevity (e.g.,C availability),structural characteristics of root systems also have a strong influence over root longevity. Recent studies showed that both root diameter and branching order were important regulators having shorter lifespans and turn over more rapidly than larger diameter,higher order roots. These findings are likely to contribute greatly to a more accurate quantification and prediction of C and nutrient flow via root turnover. The efficiency model,which suggests that the mortality of fine roots may occur when the C costs of plant roots exceed the benefits (e.g.,nutrient acquisition) they provide,also has been invoked to explain root mortality and longevity. This model necessitates that root longevity is closely related to resource availability in the soil. Some evidence suggests that roots in resource rich sites live longer,while others suggest the opposite. Much of the controversy may result from different methods used in estimating fine root longevity and turnover,and differences in C sink-source relationships among different species,stand development,as well as the length of the experiments in which the influence of resource levels on root longevity are tested. Climatic factors also influence root longevity. Fine root longevity appears to be the longest in cold environments with marked seasonal variations in seasonal environments. However,most recent evidence suggests that root longevity may be more dependent on root structure than on root environment,with first order roots having similar longevity regardless of differences in species and the root environment.Finally,ecosystem-scale processes,such as environmental stresses and pathogen and herbivory pressure,may also influence root longevity. Drought and high temperatures may shorten root longevity. However,because soil moisture,temperature,leaf C fixation,and soil resource availability are tightly linked,independent tests of moisture and temperature influences on root longevity are difficult to conduct. Evaluating the regulation of herbivores and pathogens on root longevity is also difficult,in part because little quantitative information is available on the populations of root pathogens and herbivores in different ecosystems and the responses of root systems to different levels of pathogen and herbivory pressure. In sum,root longevity is a critical but difficult research subject. There are many opportunities as well as challenges for future root longevity research in China,of which we list only a few: 1) C allocation and C utilization in fine roots may be a primary mechanism controlling root longevity,but,to understand this mechanism fully,the methods for accurately estimating C allocation and utilization in roots of different structural and functional characteristics must be developed first;2) Root longevity is clearly related to soil resource availability (e.g. N and moisture) and environmental factors (e.g.,soil temperature and moisture),and further studies on the impact of these factors on the longevity of individual roots and root systems as a whole may prove fruitful. Studies in this area should be large-scale and long-term to encompass large environmental variability frequently observed in natural ecosystems and to provide relevant information for a better understanding of the belowground

Key words: Forests, Fine root longevity, Fine root turnover, Root carbon and nitrogen, Root structure