蒙古栎、白桦根系分解及养分动态

采用埋袋法对蒙古栎(Quercus mongolica)、白桦(Betula platyphylla)两个树种粗根(>10 mm)、中粗根(5—10 mm)、中根(2—5 mm)和细根(<2 mm)的分解速率和养分动态进行研究。结果表明,根系的重量保持率随时间增加呈下降趋势,这种趋势可用Olson指数衰减模型来拟合,即:Xt/X0=e-kt(t为分解时间,X0为根系初始干重,Xt为分解t时间的残留干重,k为年分解系数),通过拟合计算出年分解系数k。在本研究中,蒙古栎粗根、中粗根、中根、细根的年分解系数分别为:0.2928、0.2562、0.2928、0.3660;白桦依次分别为:0.2196、0.3294、0.3660、0.4392,基本呈现随直径增加分解速率减小的趋势。根系分解过程中,两树种各径级均是N浓度增加,可溶性糖浓度减小。在根系分解的不同时期两树种各径级N表现出不同程度的释放或富集,没有明显的规律性;可溶性糖却一直处于释放状态。分解1a时间,蒙古栎各径级根系表现为释放N元素;白桦表现为细根和中根释放N元素,中粗根和粗根富集N元素。蒙古栎、白桦细根和中根可溶性糖的释放率达90%以上,中粗根和粗根的释放率达80%以上。     

水曲柳和落叶松人工林根系分解与养分释放

采用埋袋法对水曲柳和落叶松粗根(5～10 mm)、中根(2～5 mm)、细根(＜2 mm)的分解速率及其养分释放进行了为期2年的研究.结果表明,水曲柳粗根、中根和细根年分解系数分别为0.3649、0.4381和0.2720,落叶松依次分别为0.1967、0.1955和0.2464.通过养分分析发现,根系分解过程释放大量C和养分.分解150 d后,两树种所有级别根系的可溶性糖释放均超过90%.水曲柳粗根和中根K的释放均在40%左右,细根K的释放为71%,落叶松所有级别的根系K的释放均在95%以上.在根系分解第2年,两树种粗根和中根N的释放在50%左右波动,P在40%左右波动,两树种细根N和P的释放均达到60%.因此,根系分解在C和养分循环中起重要作用,如果将其忽略,土壤有机质和养分元素的循环将会被严重低估.     

四个典型温带树种不同根序细根分解速率及其主要影响因素

细根分解是森林生态系统土壤碳和养分的主要输入途径, 但目前人们对于影响细根分解的主要因素和细根分解模式的了解仍然很少。该研究采用根序划分等级方法, 将红松(Pinus koraiensis)、落叶松(Larix gmelinii)、水曲柳(Fraxinus mandschurica)和白桦(Betula platyphylla)细根组分前四级根划分为两个等级: 一级和二级根混合为低级根, 三级和四级根混合为高级根。利用埋袋法对东北地区4个树种不同根序细根进行连续4年的分解实验, 并对其分解速率以及影响因素进行研究。结果显示, 红松低级根和高级根分解系数分别为0.342和0.461, 落叶松依次分别为0.304和0.436, 水曲柳分别为0.450和0.555, 白桦为0.441和0.579。4个树种均显示低级根分解速率较慢, 而高级根分解速率较快。实验表明, 根系分解系数与酸不溶性物质(AUF)和非结构性碳水化合物(TNC)均具有显著相关性。出现上述结果的主要原因是低级根含有较多的AUF, 很难被分解, 以及含有较少的TNC, 为分解者提供能量较少。     

氮添加对温带森林细根长期分解的影响

细根分解是森林生态系统碳循环的重要过程之一,其分解速率受到大气氮沉降增加的潜在影响。利用长期模拟氮沉降样地（2009年至今）,采用凋落物分解袋方法,研究了氮添加对温带常见的5个森林树种长期细根分解的影响。结果表明：细根分解呈现先快后慢的趋势,在分解第516天质量损失达30%~50%,之后质量残留率变化较为平缓。总体上,渐近线分解模型可以更准确的反应各处理细根分解速率。氮添加对细根分解具有阶段性影响,分解前期促进细根分解,分解后期抑制分解。在细根分解后期氮添加减缓分解速率,一方面是因为木质素等较难分解的物质所占比例升高所带来的直接影响,另一方面,是因为氮添加改变了微生物活动所带来的间接影响。     

水曲柳和兴安落叶松人工林细根分解研究

  细根分解是陆地生态系统C和养分循环的重要环节。以往的细根分解研究以埋袋法的应用为主。然而, 由于埋袋法对分解材料的干扰以及对分解环境的改变使其很难揭示原位环境下根系的自然分解过程。该研究应用微根管(Minirhizotron)技术连续3年对水曲柳(Fraxinus mandshurica)和兴安落叶松(Larix gmelinii)细根的分解过程进行原位监测, 运用Kaplan–Meier方法估算细根分解的保存率及分解期中位值(即50%细根完全分解的时间, Median root decomposition time), 做分解曲线, 用对数秩检验(Log-rank test)方法分析不同树种、直径、根序及土层对细根保存率的影响。结果表明, 伴随时间延长, 细根的保存率逐渐下降, 兴安落叶松细根保存率的下降显著快于水曲柳(p<0.001), 两树种分解期中位值分别为(82±7) d 和(317±28) d; 不同直径等级(≤0.3、0.3～0.6、＞0.6 mm)细根的分解速率不同, 两树种最长分解期中位值均出现在最细直径(≤0.3 mm)根中; 高级根分解速率显著低于一级根(p<0.05); 土壤上层分解速度快, 随着土壤深度增加细根分解速率减小。微根管技术为了解细根自然分解过程提供了有效途径。     

喀斯特地区不同石漠化程度草地根系分解与周转特征

为探明喀斯特地区不同草地根系动态及其对石漠化的响应,本文以3种不同石漠化程度（潜在、中度和强度）的草地为研究对象,采用连续根钻法和分解袋法,于2017年3月-2018年1月,分析了不同石漠化草地的根系垂直分布、季节动态、分解、周转及其与土壤因子的关系。结果表明,3种石漠化草地的根系生物量随着土层的深度增加呈逐渐降低的趋势,潜在和中度石漠化草地的根系生物量均呈现明显的单峰型季节变化,强度石漠化草地的根系生物量变化不显著。3种石漠化草地的根系分解速率受土壤有机碳、全钾、全氮、含水量、电导率、温度等的影响显著,随分解时间均表现为"快-慢-快"的变化趋势,根系的年分解率分别为64%、56%和58%。3种草地根系完全分解（分解率为95%）时,分别需要1174天、1351天和1878天。随石漠化程度的加剧,3种草地的根系周转速率呈逐渐降低的趋势,分别为1.70次/a、1.36次/a和0.87次/a。     

中国温带和亚热带8个树种叶和吸收根协同分解

叶和细根(2mm)是森林生态系统的分解主体,二者是否协同分解,将极大影响所属植物在生态系统碳(C)循环中的物种效应。已有研究显示,叶和细根的分解关系具有极大的不确定性,认为很大程度上归因于细根内部具有高度的异质性,导致叶和细根在功能上不相似。为此,使用末梢1级根和细根根枝作为研究对象,它们在功能上同叶类似,称为吸收根。通过分解包法,分别在黑龙江帽儿山和广东鹤山,研究了2个阔叶树种和2个针叶树种(共8个树种)的叶和吸收根持续2a多的分解。结果发现,分解速率k(a~(-1),负指数模型)在8个树种整体分析时具有正相关关系(P0.05),在相同气候带或植物生活型水平上是否相关,受叶的分解环境及吸收根类型的影响;N剩余量整体上并不相关,亚热带树种的叶和细根根枝的N剩余量在分解1a后高度显著正相关,温带树种的叶和1级根的N剩余量在分解2a后显著高度正相关。本研究中,根-叶分解过程是否受控于相同或相关的凋落物性质是决定根-叶分解是否相关的重要原因,其中分解速率与酸溶组分正相关、与酸不溶组分负相关。比较已有研究,总结发现,根-叶分解关系受物种影响较大,暗示气候变化导致物种组成的改变将极大影响地上-地下关系,也因此影响生态系统C循环。     

几种树木枯叶分解速率的试验研究

 本文对几种树木的枯叶分解速率进行了研究,结果表明枯叶的分解速率因树种不同而异。一年的失重率刺槐、山杏、侧柏、元宝槭、黄栌分别为54%、64%、78%、73%、65%。应用指数衰减模型计算枯叶的年腐解率,刺槐、山杏、侧柏、元宝械、黄栌分别为0.490g／(g·a)、0.597g／(g·a),0.990g／(g·a)、0.800g／(g·a)、0.662g／(g·a)。根据枯叶的化学成分分析表明,枯叶的失重,首先是由粗脂肪,可溶性糖、丹宁,有机碳等的丧失所引起。枯叶在一年的分解过程中,碳、氮含量比值随时间的推移而下降。     

探索根系:发现新前沿——第十一届国际根系研究大会暨Rooting2021联席会议

2021年5月24日—28日第十一届国际根系研究大会和第九届根系发育研讨会(Rooting2021)联席会议由美国密苏里州州立大学和英国汉诺丁大学共同组织并在线举办。本次大会主题为“探索根系：发现新前沿”,参加会议的有来自世界51个国家,主要包括：美国、英国,澳大利亚、中国以及来自南美、欧洲和非洲的部分国家,共计693人参会。本届根系大会研讨领域广泛,涉及根的宏观到微观不同尺度的研究。预计未来根系领域研究热点主要集中在：根系表型研究技术的研究、根系的生态系统服务功能、根系的逆境生理学研究、根系与土壤交互作用、根系与微生物互作的研究以及根和根系发育等。     

水曲柳幼苗根系在不同浓度NH4NO3溶液中水流导度的变化

水分吸收过程是根系重要的生理过程。水孔蛋白在根系水分径向运输中起着重要的作用,根系水流导度(L_p)的测定是研究水孔蛋白的重要途径。该研究采用压力流的方法,对相同生长条件下的水曲柳(Fraxinus mandshurica)幼苗根系进行研究,测定了根系在去离子水和不同浓度NH₄NO₃溶液中的L_p。结果表明:未经处理的水曲柳幼苗根系,L_p随NH₄NO₃浓度的增加而上升,而且NH₄NO₃溶液中的L_p比去离子水中的L_p平均高77%;经HgCl₂处理后,水曲柳幼苗根系的L_p仍然随NH₄NO₃浓度的增加而增大,但是根系L_p在去离子水下降了22%,而在NH₄NO₃溶液中下降了68%,与以前的研究相比发现,经HgCl₂处理后,以营养液为吸水基质的根系L_p的降低值普遍高于以去离子水为基质的试验。因此,基质中养分离子的存在对根系中水孔蛋白活性产生了重要的影响,进而影响根系水分的吸收过程。     

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.     

Hydraulic conductivity of branch junctions in three temperate tree species

Summary Hydraulic conductivities were measured in branch junctions and in the proximal segments of Quercus velutina Lam., Acer saccharum Marsh., and Tsuga canadensis (L.) Carr. In all three species, the basal proximal segment was more conductive than the junction by a factor of 1.1–1.5. There was no consistent pattern for the distal proximal segments, where the conductivities were higher, lower, or the same as the junction. These data are discussed in terms of Martin H. Zimmermann's concept of plant segmentation. It is concluded that junction constrictions to water flow contribute less to plant segmentation than the variation in leaf specific conductivity in the crown of these species.     

Effects of isolates of ectomycorrhizal fungi and endophytic Mycelium radicis atrovirens that were dominant in soil from disturbed sites on growth of Betula platyphylla var. japonica seedlings

Effects of ectomycorrhizal fungi and endophytic Mycelium radicis atrovirens Melin (MRA) on growth of Betula platyphylla var. japonica seedlings were investigated under aseptic culture conditions. Three isolates of ectomycorrhizal fungi and two isolates of MRA were used. One MRA isolate was Phialocephala fortinii. Previous field work revealed that these isolates were dominant on the roots of B. platyphylla var. japonica seedlings grown in a mineral subsoil that had been exposed by the removal of surface soil. After a 100-day incubation, the growth of the seedlings was significantly enhanced by the colonization of these ectomycorrhizal fungal isolates as compared with uninoculated seedlings. In contrast, the growth of seedlings was retarded by the colonization of the MRA isolates. The growth of seedlings that were co-inoculated with ectomycorrhizal fungi and MRA was similar to that of uninoculated seedlings in most cases. These results suggest that ectomycorrhizal fungi have a beneficial effect on the growth of B. platyphylla var. japonica seedlings and that they suppress the deleterious effect of MRA. Thus, these ectomycorrhizal fungi probably have an important role in establishing B. platyphylla var. japonica seedlings during the initial stage of re-vegetation following site disturbance by the removal of surface soil.     

Callus proliferation from leaf protoplasts using phenylurea type cytokinin, 4-PU,inBetula platyphylla VAR.Japonica

Summary Protoplasts were isolated from leaves ofBetula platyphylla var.japonica using a 0.6M mannitol solution containing 1% Cellulase Onozuka R-10 and 1% Driselase. The cell division and colony formation were largely enhanced using Murashige and Skoog (1962) liquid medium at half strength (1/2 MS), containing 0.6M mannitol, 0.09M sucrose, and factorial combinations of 0.1–30 μM N-(2-chloro-4-pyridyl)-N′-phenylurea (4-pu) and 0.1–10 μM 1-naphthaleneacetic acid (NAA) or 0.1–30 μM 2,4-dichlorophenoxyacetic acid (2,4-D). The optimal protoplast density was 5–7 × 10⁴/ml. Continuous callus proliferation from protoplasts was achieved by transferring colonies to fresh 1/2 MS agar medium containing 1 μM NAA and 1 μM 4-pu with no mannitol. It appeared that supplementation of the medium with phenylurea type cytokinin, 4-pu gave the successful callus proliferation from the protoplasts ofB. platyphylla.     

Drought acclimation of two deciduous tree species of different layers in a temperate forest canopy

Water-use strategies of Populus tremula and Tilia cordata, and the role of abscisic acid in these strategies, were analysed. P. tremula dominated in the overstorey and T. cordata in the lower layer of the tree canopy of the temperate deciduous forest canopy. Shoot water potential (), bulk-leaf abscisic acid concentration ([ABA]_leaf), abscisic acid concentration in xylem sap ([ABA]_xyl), and rate of stomatal closure following the supply of exogenous ABA (v) decreased acropetally through the whole tree canopy, and foliar water content per area (w), concentration of the leaf osmoticum (c), maximum leaf-specific hydraulic conductance of shoot (L), stomatal conductance (g_s), and the threshold dose per leaf area of the exogenous ABA (d_a) required to reduce stomatal conductance increased acropetally through the tree canopy (from the base of the foliage of T. cordata to the top of the foliage of P. tremula) in non-stressed trees. The threshold dose per leaf dry mass of the exogenous ABA (d_w) required to reduce stomatal conductance, was similar through the tree canopy. After a drought period (3 weeks), the , w, L, g_s, d_a and d_w had decreased, and c and v had increased in both species. Yet, the effect of the drought period was more pronounced on L, g_s, d_a, d_w and v in T. cordata, and on , w and c in P. tremula. It was concluded that the water use of the species of the lower canopy layer—T. cordata, is more conservative than that of the species of the overstorey, P. tremula. [ABA]_leaf had not been significantly changed in these trees, and [ABA]_xyl had increased during the drought period only in P. tremula. The relations between [ABA]_leaf, [ABA]_xyl and the stomatal conductance, the osmotic adjustment and the shoot hydraulic conductance are also discussed.     

硬化地表对不同树种土壤微生物群落结构和功能的影响

城市硬化地表可减少土壤有机物输入,并改变土壤理化性质,由此可能影响土壤微生物群落结构和功能,但目前国内外相关研究较少。为研究不同树种下土壤微生物群落对硬化地表的响应,设置透水硬化地表(Pervious pavement, P)、不透水硬化地表(Impervious pavement, IP)和自然地表(Control, C)3个处理水平的地表类型,并栽种北方常见的常绿针叶树油松(pine,Pinus tabulaeformis)和落叶阔叶树白蜡(ash,Fraxinus chinensis)。采用氯仿熏蒸浸提法、磷脂脂肪酸法(PLFA)及BIOLOG培养法分别测定了土壤微生物量、群落结构和功能多样性。结果表明:(1)与自然地表(C)相比,硬化地表下土壤微生物生物量碳、氮含量显著降低(P0.05),土壤微生物群落组成和群落功能多样性发生了改变。透水和不透水硬化地表下土壤微生物细菌、真菌数量降低,真菌/细菌(fungi/bacteria, F/B)、cy/pre(环丙基脂肪酸/前体结构cyclopropyl fatty acid/monoenoic precursors)和sat/mono(一般饱和脂肪酸/单不饱和脂肪酸normal saturated fatty acid/monounsaturated fatty acid)等环境压力指标均显著升高(P0.05),且土壤微生物cy/pre值在不透水硬化地表下显著高于透水硬化地表下,表明不透水硬化地表下土壤环境压力更大;不透水硬化地表下土壤微生物对糖类、氨基酸类、羧酸类、胺类和聚合物的利用显著降低(P0.05),微生物群落功能丰富度及多样性指数显著降低(P0.05)。(2)土壤微生物群落结构和功能多样性在不同树种间存在一定差异。油松树下土壤微生物真菌、丛枝菌根真菌(arbuscular mycorrhizal fungi, AMF)和F/B值在透水和不透水硬化地表下均显著降低(P0.05),而白蜡树下只在透水硬化地表下显著降低(P0.05);硬化地表使土壤微生物对糖类、氨基酸类和聚合物的利用强度在油松和白蜡树下表现出显著差异。硬化地表对土壤微生物的影响将进一步影响城市绿地的养分循环、树木生境和生态系统服务功能。     

Leaf litter quality and decomposition rates of yellow birch and sugar maple seedlings grown in mono-culture and mixed-culture pots at three soil fertility levels

Seedlings of yellow birch (Betula alleghaniensis Britton) and sugar maple (Acer saccharum Marsh.) were grown for 2 years in mono-culture and mixed-culture and at three fertility levels. Following the second growing season, senescent leaves were analysed for N concentration, acid hydrolysable substances (AHS), and nonhydrolysable remains (NHR). A litter sub-sample was then inoculated with indigenous soil microflora, incubated 14 weeks, and mass loss was measured. Litter-N was significantly higher at medium than at poor fertility, as well as in yellow birch than in sugar maple litter. The species effect on litter-N increased with increasing fertility. At medium fertility, litter-N of sugar maple litter was lower in mixed-culture than in mono-culture. AHS, NHR as well the NHR/N ratio were significantly higher in yellow birch than in sugar maple litter. At medium fertility, the NHR/N ratio of sugar maple litter was significantly lower in mono-culture than in mixed-culture. Mass loss was significantly greater at medium and rich fertility than at poor fertility, and in yellow birch than in sugar maple litter. At poor fertility, mixed-litter decomposed at a rate comparable to yellow birch, whereas at medium and rich fertility, mixed-litter decomposed at a rate comparable to sugar maple. There was a significant positive relationship between litter-N and mass loss. A similar positive relationship between NHR and mass loss was presumed to be a species effect on decomposition. Results support the hypothesis that species × fertility and species × mixture interactions can be important determinants of litter quality and, by implication, of site nutrient cycling.     

Effect of flooding and temperature regime on growth and stomatal resistance ofBetula platyphylla var.japonica seedlings

Summary Both flooding and low temperature reduced height and stem diameter growth; leaf initiation; growth of leaves, stems, and roots; and lowered root-shoot ratios of 112-dayoldBetula platyphylla var.japonica seedlings. Flooding also induced leaf scorching and abscission. Growth was reduced much more by flooding than by low temperature. Interactive effects of flooding and temperature were shown on height growth, leaf initiation and expansion, and dry weight increment of leaves, stems and roots. The amount of growth reduction by flooding and low temperature was greater when based on analysis of dry weight increment of leaves, stems, and roots, than on their relative growth rates. The greater reduction of growth by flooding than by low temperature was associated with fewer and smaller leaves, more leaf injury, more stomatal closure, and greater decay of roots in flooded plants. Flooding and low temperature appeared to reduce growth by somewhat different physiological mechanisms. Research supported by the College of Agricultural and Life Sciences, University of Wisconsin, Madison, WI, USA and by Yamagata University, Tsuruoka, Japan. McIntyre-Stennis Project 2599.     

CO2-induced growth enhancements of co-occurring tree species decline at different rates

To elucidate how enriched CO₂ atmospheres, soil fertility, and light availability interact to influence the long-term growth of tree seedlings, six co-occurring members of temperate forest communities including ash (Fraxinus americana L.), gray birch (Betula populifolia), red maple (Acer rubrum), yellow birch (Betula alleghaniensis), striped maple (Acer pensylvanicum), and red oak (Quercus rubra L.) were raised in a glasshouse for three years in a complete factorial design. After three years of growth, plants growing in elevated CO₂ atmospheres were generally larger than those in ambient CO₂ atmospheres, however, magnitudes of CO₂-induced growth enhancements were contingent on the availability of nitrogen and light, as well as species identity. For all species, magnitudes of CO₂-induced growth enhancements after one year of growth were greater than after three years of growth, though species' growth enhancements over the three years declined at different rates. These results suggest that CO₂-induced enhancements in forest productivity may not be sustained for long periods of time. Additionally, species' differential growth responses to elevated CO₂ may indirectly influence forest productivity via long-term species compositional changes in forests.