间伐对川西亚高山粗枝云杉人工林细根生物量及碳储量的影响

以川西亚高山50年生粗枝云杉(Picea asperata)人工林为研究对象, 探讨了间伐对粗枝云杉人工林1-5级细根生物量及碳储量的影响。结果表明: 粗枝云杉人工林细根生物量和碳储量随根序等级的增加而显著增加(p < 0.05), 5级根序中1级根生物量及碳储量最小, 5级根生物量及碳储量最大。与对照(间伐0%)相比, 间伐对粗枝云杉人工林林分细根生物量及碳储量有显著影响(p < 0.05); 而对单株细根生物量影响不一, 间伐10%和20%与对照没有显著性差异(p > 0.05)。间伐显著影响生物量在各根序中的分配, 随着间伐强度的增加, 1、2级细根中生物量分配比例增加, 1级细根的生物量增加幅度最大; 3-5级细根的生物量分配比例减小, 5级细根减少幅度最大。其中, 间伐50%显著减少了细根在下层(20-40 cm)土壤中的生物量比例(p < 0.05), 但与间伐20%和30%无显著差异(p > 0.05)。     

不同分类系统下油松幼苗根系特征的差异与联系

植物根序和径级不仅反映细根的形态结构, 而且能反映根系的一些生理特征, 如细根寿命和周转等。该文以二年生油松(Pinus tabulaeformis)幼苗根系为研究对象, 系统比较了根序分类方法和径级分类方法在描述根系特征上的优缺点, 探索了两者之间的内在联系。结果表明: 二年生油松幼苗最多可包括6级根序, 直径的变化范围为0.169-3.877 mm。按根序划分, I-VI级根序的总根长和总根表面积主要集中在前3级根序, 这3级根序的根占总根长的78.77%和总根表面积的62.72%。前3级根序的比根长是后3级根序比根长的1.3-3.0倍, 比根面积是后3级比根面积的1.0-1.5倍。按常用的径级(以0.5、1.0、1.5和2.0 mm为阈值)划分方法, 油松幼苗大部分根系直径≤1.5 mm, 此区间细根的根长和根表面积占总根长的93.76%和总根表面积的84.35%。直径≤1.5 mm的细根平均比根长是>1.5 mm细根比根长的3-7倍, 比根面积的1.5-3.0倍。由于油松根序和径级之间有显著的指数关系, 依据径级最大程度反映根序的原则, 提出了新的径级划分方法, 即以0.4、0.8、1.3和2.0 mm为阈值对油松幼苗根系径级重新进行划分。此时, 上述区间可分别包括I级、II级、III级、IV级、V级根序中根尖数的93.22%、86.37%、75.96%、70.47%和76.67%。同时也可分别涵盖各径级根长的89.34%-70.83%、根面积的86.01%-76.12%以及体积的87.73%-76.12%。此时, 根系不同径级与根序之间可以建立起良好的对应关系。这些结果表明, 通过合理划分径级区间可以较好地反映根序 特征。     

Fine root architecture, morphology, and biomass of different branch orders of two Chinese temperate tree species

We have limited understanding of architecture and morphology of fine root systems in large woody trees. This study investigated architecture, morphology, and biomass of different fine root branch orders of two temperate tree species from Northeastern China—Larix gmelinii Rupr and Fraxinus mandshurica Rupr —by sampling up to five fine root branch orders three times during the 2003 growing season from two soil depths (i.e., 0–10 and.10–20 cm). Branching ratio (R _b) differed with the level of branching: R _b values from the fifth to the second order of branching were approximately three in both species, but markedly higher for the first two orders of branching, reaching a value of 10.4 for L. gmelinii and 18.6 for F. mandshurica. Fine root diameter, length, SRL and root length density not only had systematic changes with root order, but also varied significantly with season and soil depth. Total biomass per order did not change systematically with branch order. Compared to the second, third and/or fourth order, the first order roots exhibited higher biomass throughout the growing season and soil depths, a pattern related to consistently higher R _b values for the first two orders of branching than the other levels of branching. Moreover, the differences in architecture and morphology across order, season, and soil depth between the two species were consistent with the morphological disparity between gymnosperms and angiosperms reported previously. The results of this study suggest that root architecture and morphology, especially those of the first order roots, should be important for understanding the complexity and multi-functionality of tree fine roots with respect to root nutrient and water uptake, and fine root dynamics in forest ecosystems.     

落叶松和水曲柳不同根序细根形态结构、组织氮浓度与根呼吸的关系

根系具有高度的形态和生理功能异质性,在森林生态系统碳和养分循环中起重要作用。根系分枝的顺序构成根序,是根系最基本的构型特征,根序代表根系不同的发育阶段。然而,目前直接测定不同根序细根生理功能的研究很少。以落叶松（Larix gmelinii）和水曲柳（Fraxinus mandshurica）的细根为研究对象,使用气相氧电极测定不同根序细根的呼吸速率,探讨根系呼吸速率与其形态、结构和组织氮浓度的关系。结果表明：落叶松和水曲柳细根的直径、根长和维管束直径均随着根序的增加（1–5级）而增加,而比根长、组织氮浓度和呼吸速率随着根序的增加而降低,各根序之间差异显著（P〈0.05）;1级根比根长最大、皮层组织发达、组织氮浓度最高且呼吸速率也最高,其呼吸速率分别为17.57nmolO2·g^–1·s^–1（落叶松）和18.80 nmolO2·g^–1·s^–1（水曲柳）,比5级根分别高148%（落叶松）和124%（水曲柳）;并且,落叶松根的呼吸速率几乎有96%与根系组织氮浓度相关,而水曲柳根的呼吸速率则有89%与根系组织氮浓度相关。上述结果说明,细根的形态和生理功能异质性是紧密相连的,低级根的形态、结构决定其功能是吸收养分和水,而高级根的形态、结构决定其功能是运输和贮存养分。     

林木细根寿命及其影响因子研究进展

 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。     

海南岛4个热带阔叶树种前5级细根的形态、解剖结构和组织碳氮含量

细根具有复杂的分支系统, 以根序(root order)为取样单元的细根生理生态学研究正在成为根系生态学研究领域的重要内容。该研究以海南岛尖峰岭4个热带阔叶树种海南蕈树(Altingia obovata)、厚壳桂(Cryptocarya chinensis)、山杜英(Elaeocarpus sylvestris)和黄桐(Endospermum chinense)为研究对象, 测定了1-5级细根的形态、解剖结构和组织碳(C)、氮(N)含量, 旨在探讨这些根系特征之间的联系。研究表明: 4个树种的细根形态差异较大, 但在树种水平上直径、根长和组织密度均随着根序的升高而增加, 比根长则随着根序的升高而降低; 低级根(前2级根或前3级根)具有皮层组织, 是典型的吸收根, 而高级根皮层组织消失, 是典型的运输和储藏根; 影响直径大小最重要的因子是皮层厚度, 它可以解释细根直径变异的97%, 而维管束直径仅能解释细根直径变异的70%; 根组织N和C浓度受维管束-根直径比(维根比)的影响, 随着维根比增加, 组织N浓度显著降低, 组织C浓度显著升高。4个树种细根的C/N比的变异受组织N浓度的影响程度为76%, 而受C浓度的影响程度不足10%。上述结果表明, 细根的形态特征、解剖结构和组织化学含量之间存在着紧密联系, 这为我们理解根系结构与功能变异提供了重要依据。     

亚热带6种树种细根序级结构和形态特征

以福建省建瓯市万木林自然保护区内占优势的6种天然林树种(沉水樟Cinnamomum micranthum,CIM;观光木Tsoongiodendron odorum Chun,TOC;浙江桂Cinnamomum chekiangense,CIC;罗浮栲Castanopsis fabri,CAF;细柄阿丁枫Altingiagracilipes,ALG;米槠Castanopsis carlesii,CAC)为研究对象,对其1—5级细根的结构,形态特征及生物量进行了分析。结果表明:沉水樟,细柄阿丁枫和米槠细根分支比表现出在1,2级(4倍以上)明显大于其它序级(3倍左右);其余3种树种则是在3,4级的细根分支比最大,其中浙江桂达到8.65倍,其它序级则大致为3倍左右。6种树种1,2级细根数量占到总数的70%—90%。6种树种细根直径,根长,组织密度随序级升高逐渐增大,比根长减小,生物量未表现出一致的变化规律,6种树种生物量主要集中在高级根部分。方差分析表明,树种对细根分支比例有显著影响(P<0.05),浙江桂和米槠细根分支水平对分支比例有极显著影响(P<0.01),其余4种树种分支水平对分支比例有显著影响(P<0.05),树种和分支水平的交互作用对6种树种细根分支比均有极显著的影响(P<0.01);树种对细根根长,直径以及生物量均有极显著影响(P<0.01),对比根长有显著影响(P<0.05),而对组织密度的影响则不显著(P>0.05);树种和序级的交互作用对细根根长,直径以及生物量均有极显著影响(P<0.01),对组织密度有显著影响(P<0.05),对比根长影响不显著(P>0.05)。序级对6种树种细根根长,直径,比根长以及生物量的影响并未达到一致,对6种树种细根组织密度有极显著影响(P<0.01)。树种间1—4级根的比根长变异主要由组织密度引起,而5级根的比根长变异则由直径引起,同时在1级根中组织密度与直径呈现出权衡的关系。6种树种细根数量,直径,根长,比根长,组织密度以及生物量与序级之间回归分析发现它们与序级之间具有指数函数,线性函数,二次函数,三次函数或者幂函数关系。     

杨树细根碳、氮含量的季节动态及代际差异

研究杨树人工林1～5级根序细根内碳、氮及非结构性碳水化合物含量的季节动态,对比了杨树细根碳氮分配格局的代际差异,以期建立细根生长和功能变化与连作人工林生产力衰退的联系.结果表明： 杨树细根非结构性碳水化合物(NSC)随根序显著增加,而氮含量显著减少.细根中全C和NSC含量与全N存在显著相关性.细根碳氮含量的变化在根序间的解释量占98.2%,而在代际间仅为1.7%.杨树不同根序细根均在生长季具有较高的碳含量和较低的氮含量,且碳、氮及NSC含量在代际间随季节差异显著,但C∶N差异不显著,根序与季节对细根碳氮含量存在显著交互效应.杨树低级细根C∶N约为20∶1,高级根则大于30∶1.细根C∶N在生长季(7和9月)显著低于其他季节,NSC含量在11月最高.连作人工林杨树细根的碳氮分配格局与细根根序具有较强的耦合性,NSC和C∶N在指示细根周转和调控细根季节性生长中具有重要生态学意义.     

Measuring Fine Root Turnover in Forest Ecosystems

Development of direct and indirect methods for measuring root turnover and the status of knowledge on fine root turnover in forest ecosystems are discussed. While soil and ingrowth cores give estimates of standing root biomass and relative growth, respectively, minirhizotrons provide estimates of median root longevity (turnover time) i.e., the time by which 50% of the roots are dead. Advanced minirhizotron and carbon tracer studies combined with demographic statistical methods and new models hold the promise of improving our fundamental understanding of the factors controlling root turnover. Using minirhizotron data, fine root turnover (y⁻¹) can be estimated in two ways: as the ratio of annual root length production to average live root length observed and as the inverse of median root longevity. Fine root production and mortality can be estimated by combining data from minirhizotrons and soil cores, provided that these data are based on roots of the same diameter class (e.g., < 1 mm in diameter) and changes in the same time steps. Fluxes of carbon and nutrients via fine root mortality can then be estimated by multiplying the amount of carbon and nutrients in fine root biomass by fine root turnover. It is suggested that the minirhizotron method is suitable for estimating median fine root longevity. In comparison to the minirhizotron method, the radio carbon technique favor larger fine roots that are less dynamics. We need to reconcile and improve both methods to develop a more complete understanding of root turnover.     

中国温带、亚热带和热带森林45个常见树种细根直径变异

 细根在发挥植物功能以及生态系统碳和养分循环过程中起着重要作用。为了解我国不同森林生态系统细根直径变化规律, 提供建立根系模型的基础, 该文研究了我国温带、亚热带和热带45个常见树种1～5级根直径的变异以及直径与根序的关系。结果表明: 1)在所有树种中, 1级根直径最细, 5级根直径最粗, 直径随根序的增加而增加。此外, 同一根序的直径在不同树种间变异较大, 在不同生态系统中, 各树种1级根的总体平均直径呈现温带<亚热带<热带的格局。2)不同生态系统树种同一根序平均直径变异程度不同, 各个根序都是温带最小, 亚热带次之, 热带最大。3)细根内部各个根序的平均直径变异的52%由根序解释, 33%由树种解释, 生态系统类型和生活型分别解释7%和2%。不同系统不同树种直径的变异说明无法用统一的直径级来研究根的功能, 也无法用统一的根序和直径间的关系来建立根系形态模型。今后的研究需要进一步认识根序和直径在不同树种中如何与根的功能相联系。     

柠条人工林细根不同分枝根序寿命估计

植物细根在发育结构上表现的形态特征和生理功能异质性影响细根寿命的准确估计,因此了解分枝根序细根寿命差异对于深入认识细根的周转过程和陆地生态系统碳分配具有重要意义。采用微根管(Minirhizotron)技术对晋西北黄土区的五年生柠条(Caragana Korshinskii Kom.)人工林细根的生长过程进行了为期3a(2007—2009年)的追踪观测,分析了不同因素(土层深度、季节变化、空间位置)对一级根和高级根寿命的影响。结果表明:(1)在各土层深度处,一级根的中值寿命均低于高级根中值寿命,其中一级根中值寿命表现随土层深度增加而增加趋势,而高级根除表层0—20 cm中值寿命较短外,各土层间变化趋势不明显,40—60 cm、80—100 cm土层高级根在观测期结束时其累积存活率仍在50%以上;(2)不同季节出生一级根和高级根的中值寿命季节性表现为:秋季夏季春季,并且在各个季节均表现,高级根寿命显著大于一级根寿命(P0.01);一级根仅夏季与秋季差异性不显著(P0.05),而高级根仅春季与秋季存在极显著差异(P0.01);(3)一级根和高级根距树干基部0 cm处细根中值寿命均大于50 cm处一级根和高级根细根的中值寿命。同一位置处高级根寿命要大于一级根寿命。在距树干基部0 cm处和50 cm处,一级根和高级根的寿命均存在极显著差异(P0.01),但高级根却在距树干基部0 cm和50 cm处差异不明显,而一级根却表现极显著差异(P0.01)。     

Temperature-induced alteration to root longevity in Lolium perenne

The production and mortality of roots is an important factor determining nutrient and carbon fluxes in terrestrial ecosystems. However, the effect of temperature on the longevity of roots is not understood. In this study the impact of changes in temperature on the longevity of Lolium perenne roots was determined.Plants were grown at 15 °C, 21 °C and 27 °C and their roots observed using a minirhizotron system. Major effects of temperature were measured with large reductions in root longevity occurring at higher temperatures. The implications of these data are discussed.     

Fine root branch orders respond differentially to carbon source-sink manipulations in a longleaf pine forest

Fine roots are a key component of carbon (C) flow and nitrogen (N) cycling in forest ecosystems. However, the complexity and heterogeneity of the fine root branching system have hampered the assessment and prediction of C and N dynamics at ecosystem scales. We examined how root morphology, biomass, and chemistry differed with root branch orders (1–5 with root tips classified as first order roots) and how different root orders responded to increased C sink strength (via N fertilization) and reduced carbon source strength (via canopy scorching) in a longleaf pine (Pinus palustris L.) ecosystem. With increasing root order, the diameter and length of individual roots increased, whereas the specific root length decreased. Total root biomass on an areal basis was similar among the first four orders but increased for the fifth order roots. Consequently, total root length and total root surface area decreased systematically with increasing root order. Fine root N and lignin concentrations decreased, while total non-structural carbohydrate (TNC) and cellulose concentrations increased with increasing root order. N addition and canopy disturbance did not alter root morphology, but they did influence root chemistry. N fertilization increased fine root N concentration and content per unit area in all five orders, while canopy scorching decreased root N concentration. Moreover, TNC concentration and content in fifth order roots were also reduced by canopy scorching. Our results indicate that the small, fragile, and more easily overlooked first and second order roots may be disproportionately important in ecosystem scale C and N fluxes due to their large proportions of fine root biomass, high N concentrations, relatively short lifespans, and potentially high decomposition rates.Electronic Supplementary Material Supplementary material is available for this article at     

Evaluating minirhizotron estimates of fine root longevity and production in the forest floor of a temperate broadleaf forest

The minirhizotron technique (MR) for in situ measurement of fine root dynamics offers the opportunity to obtain accurate and unbiased estimates of root production in perennial vegetation only if MR tubes do not affect the longevity of fine roots. Assuming fine root biomass is near steady-state, fine root production (g m^–2 yr^–1) can be estimated as the ratio of fine root biomass (g m^–2) to median fine root longevity (yr). This study evaluates the critical question of whether MR access tubes affect the longevity of fine roots, by comparing fine root survivorship obtained using MR with those from a non-intrusive in situ screen method in the forest floor horizons of a northern hardwood forest in New Hampshire, USA. Fine root survivorship was measured in 380 root screens during 1993–1997 and in six horizontal minirhizotron tubes during 1996–1997. No statistically significant difference was found between estimates of survivorship of fine roots (<1 mm dia.) at this site from MR versus from in situ screens, suggesting that MR tubes do not substantially affect fine root longevity in the forest floor of this northern hardwood forest and providing greater confidence in measurements of fine root production using the MR technique. Furthermore, the methodology for estimating fine root production from MR longevity data was evaluated by comparison of fine root longevity and production estimates made using single vs. multiple root cohorts, and using root-number, root-length, and root-mass weighted methods. Our results indicate that fine root-length longevity estimates based on multiple root cohorts throughout the year can be used to approximate fine root biomass production. Using this method, we estimated fine root longevity and production in the forest floor at this site to be 314 days (or 0.86 yr) and 303 g m^–2 yr^–1, respectively. Fine root production in this northern hardwood forest is approximately equivalent to standing biomass and was previously underestimated by root in-growth cores. We conclude that the use of MR to estimate fine root longevity and production as outlined here may result in improved estimates of fine root production in perennial vegetation.     

Effects of root diameter,branch order,root depth,season and warming on root longevity in an alpine meadow

Fine root is of importance in biogeochemical cycles especially in terrestrial ecosystems. The lack of understanding of the factors controlling root lifespan has made accurate prediction of carbon flow and nutrient cycling difficult. A controlled warming experiment was performed in an alpine meadow on the northern Tibetan Plateau (near Nagchu Town). We used a minirhizotron technique to measure root dynamics in situ during the growing season of 2013 and 2014 and survival analyses to assess root lifespan and the effects of root diameter, branch order, birth season, root depth and warming on root lifespan. Root diameter, branch order and root depth were all positively correlated with root lifespan. With an increase in diameter of 0.1 mm, mortality hazard ratio of roots declined by 19.3 %. An increase in one level in branch order was associated with a decrease of 43.8 % in root death ratio. Compared with roots born in May–mid-July, the mortality hazard ratio of roots born in late July–August and September–October reduced by 26.8 and 56.5 %, respectively. In warming treatments, roots tended to be thinner, less branched and deeper, and there was a higher proportion of roots born in spring compared to ambient conditions. Warming shortened the median root lifespan 44 days. However, in single warming condition, root diameter had no significant influence on root lifespan. Root diameter, branch order, root depth and season of birth were all factors affecting root lifespan in the alpine meadow; however, root branch order was dominant.     

樟子松人工林细根寿命估计及影响因子研究

细根寿命的估计是了解细根生产和死亡的关键, 对了解陆地生态系统碳分配格局和养分循环具有重要意义。该研究采用微根管(minirhizotron)技术, 以23年生樟子松(Pinus sylvestris var. mongolica)人工林为研究对象, 对细根生长和死亡过程进行了连续两年的观测。细根寿命的估计采用Kaplan-Meier方法, 计算细根的平均寿命(mean longevity)、中值寿命(median longevity)和累积存活率(cumulative survival rate), 用对数秩检验(log-rank test)比较单一因素, 包括细根直径、根序、出生季节和土层以及菌根侵染对细根寿命的影响。采用Cox比例风险回归分析方法, 同时分析上述因素对细根存活的影响程度。结果表明, 樟子松细根的生产和死亡具有明显的季节性, 春末和夏季(6月和7月)为生产高峰; 而死亡高峰出现在夏末至秋末, 以及冬季。樟子松细根的平均和中值寿命分别为(322 ± 10)天和(310 ± 15)天, 对数秩检验表明, 仅考虑单一因子时, 细根直径、根序、出生季节和土层以及菌根侵染均对细根寿命有显著影响。Cox回归分析表明, 菌根侵染、细根直径和土层是影响樟子松细根寿命的重要因子。细根直径每增加1 mm, 细根死亡危险率就降低99%, 即相当于寿命延长99%; 细根出生土层每增加1 cm, 其寿命延长5%; 而菌根侵染后, 会导致细根死亡危险率增加175%; 但根序和出生季节的影响不显著。这些发现证实: 林木细根寿命受到内在与外在因素的共同控制, 而多变量回归分析的方法有助于我们全面揭示细根寿命变异的潜在机制。     

施肥对日本落叶松人工林细根直径、根长和比根长的影响

以辽宁东部山区16年生日本落叶松人工林为研究对象,探讨施肥对日本落叶松1～5级根序中细根直径、根长和比根长的影响.结果表明：随着根序等级的增加,日本落叶松细根平均直径和根长显著增加（P<0。05,P<0。01）、比根长则显著下降（P<0。01）.在日本落叶松的5级根序中,1级根的平均直径最细、根长最短、比根长最高,而5级根则相反;随着根序等级的增加,日本落叶松细根平均直径、根长和比根长的变异系数逐渐增大.除1级根外,土层对细根的平均直径、根长和比根长没有显著影响(P>0。05).与对照样地相比,施肥对各级细根平均直径、根长和比根长的影响主要表现在1～2级根上,对3级根序以上的细根影响不显著（P>0.05）.其中,施氮肥显著降低了1～2级根的平均直径（P<0.05）,施氮肥以及氮磷肥显著降低了表层土壤（0～10 cm）中1级根的平均根长（P<0.05）,表层土壤中细根的比根长在施氮肥的条件下显著增加（P<0.05）.     

Arbuscular mycorrhizal fungi induced alteration to root longevity of poplar

Root longevity is an important element determining the fluxes of nutrients and carbon within terrestrial ecosystems. The effect of colonisation by an arbuscular mycorrhizal (AM) fungus on root longevity of poplar was determined using a minirhizotron camera to make direct observation of roots in situ in conjunction with image analysis. significant influences of colonisation on the longevity of roots were observed with most colonised roots surviving for a shorter period than non-colonised roots: only 16% of colonised roots survived for longer than 49 days compared to 49% of non-colonised roots. After 21 days approximately 5 times as many colonised as non-colonised roots had died. Possible mechanisms are discussed.     

Uncertainties in interpretation of isotope signals for estimation of fine root longevity: theoretical considerations

This paper examines uncertainties in the interpretation of isotope signals when estimating fine root longevity, particularly in forests. The isotope signals are depleted δ¹³C values from elevated CO₂ experiments and enriched Δ¹⁴C values from bomb ¹⁴C in atmospheric CO₂. For the CO₂ experiments, I explored the effects of six root mortality patterns (on–off, proportional, constant, normal, left skew, and right skew distributions), five levels of nonstructural carbohydrate (NSC) reserves, and increased root growth on root δ¹³C values after CO₂ fumigation. My analysis indicates that fitting a linear equation to δ¹³C data provides unbiased estimates of longevity only if root mortality follows an on–off model, without dilution of isotope signals by pretreatment NSC reserves, and under a steady state between growth and death. If root mortality follows the other patterns, the linear extrapolation considerably overestimates root longevity. In contrast, fitting an exponential equation to δ¹³C data underestimates longevity with all the mortality patterns except the proportional one. With either linear or exponential extrapolation, dilution of isotope signals by pretreatment NSC reserves could result in overestimation of root longevity by several‐fold. Root longevity is underestimated if elevated CO₂ stimulates fine root growth. For the bomb ¹⁴C approach, I examined the effects of four mortality patterns (on–off, proportional, constant, and normal distribution) on root Δ¹⁴C values. For a given Δ¹⁴C value, the proportional pattern usually provides a shorter estimate of root longevity than the other patterns. Overall, we have to improve our understanding of root growth and mortality patterns and to measure NSC reserves in order to reduce uncertainties in estimated fine root longevity from isotope data.     

Seasonal dynamics of fine root biomass,root length density,specific root length,and soil resource availability in a Larix gmelinii plantation

Fine root tumover is a major pathway for carbon and nutrient cycling in terrestrial ecosystems and is most likely sensitive to many global change factors.Despite the importance of fine root turnover in plant C allocation and nutrient cycling dynamics and the tremendous research efforts in the past,our understanding of it remains limited.This is because the dynamics processes associated with soil resources availability are still poorly understood.Soil moisture,temperature,and available nitrogen are the most important soil characteristics that impact fine root growth and mortality at both the individual root branch and at the ecosystem level.In temperate forest ecosystems,seasonal changes of soil resource availability will alter the pattern of carbon allocation to belowground.Therefore,fine root biomass,root length density(RLD)and specific root length(SRL)vary during the growing season.Studying seasonal changes of fine root biomass,RLD,and SRL associated with soil resource availability will help us understand the mechanistic controls of carbon to fine root longevity and turnover.The objective of this study was to understand whether seasonal variations of fine root biomass,RLD and SRL were associated with soil resource availability,such as moisture,temperature,and nitrogen,and to understand how these soil components impact fine root dynamics in Larix gmelinii plantation.We used a soil coring method to obtain fine root samples(≤2 mm in diameter)every month from Mav to October in 2002 from a 17-year-old L.gmelinii plantation in Maoershan Experiment Station,Northeast Forestry University,China.Seventy-two soil cores(inside diameter 60 mm;depth intervals:0-10 cm,10-20 cm,20-30 cm)were sampled randomly from three replicates 25 m×30 m plots to estimate fine root biomass(live and dead),and calculate RLD and SRL.Soil moisture,temperature,and nitrogen(ammonia and nitrates)at three depth intervals were also analyzed in these plots.Results showed that the average standing fine root biomass(live (32.2 g.m-2.a-1)in the middle(10-20 cm)and deep layer (20-30cm),respectively.Live and dead fine root biomass was the highest from May to July and in September,but lower in August and October.The live fine root biomass decreased and dead biomass increased during the growing soil layer.RLD and SRL in May were the highestthe other months,and RLD was the lowest in Septemberdynamics of fine root biomass,RLD,and SRL showed a close relationship with changes in soil moisture,temperature,and nitrogen availability.To a lesser extent,the temperature could be determined by regression analysis.Fine roots in the upper soil layer have a function of absorbing moisture and nutrients,while the main function of deeper soil may be moisture uptake rather than nutrient acquisition.Therefore,carbon allocation to roots in the upper soil layer and deeper soil layer was different.Multiple regression analysis showed that variation in soil resource availability could explain 71-73% of the seasonal variation of RLD and SRL and 58% of the variation in fine root biomass.These results suggested a greater metabolic activity of fine roots living in soil with higher resource availability,which resulted in an increased allocation of carbohydrate to these roots,but a lower allocation of carbohydrate to those in soil with lower resource availability.