A note on the root development in dry tropical naturally revegetated coalmine spoils

Root biomass distribution on an age series of naturally revegetated coalmine spoils in a dry tropical environment is described. 65 to 85% of the total root biomass was observed in the upper 0–15 cm of spoil depth. Highest (724 g m^-2) and lowest (186 g m^-2) values of root biomass were found on 12-yr old protected flat surfaces and 5-yr old grazed undulating sites, respectively. There is an increase in root biomass with increase in age of coalmine spoil.     

Microbial degradation of geogenic organic C and N in mine spoils

Many mine spoils present at the surface of reclamation sites in the Lower Lusatian mining district are carboniferous substrates, i.e. contain geogenic organic matter. Depending on its susceptibility to microbial degradation, geogenic organic matter might influence the establishment of a carbon requiring microflora in mine spoils. As geogenic organic matter contains substantial amounts of organic nitrogen it is also a potential source for plant available N. The objective of the present study was to quantify C and N mineralisation and microbial biomass in geogenic organic matter present at reclamation sites in Lower Lusatia. We also studied, whether these properties can be influenced by raising the originally low pH to near neutral conditions. In laboratory incubation studies, the rates of CO₂ evolution and net N mineralisation were determined in geogenic organic matter and carboniferous mine spoil with and without addition of lime. At the same time, microbial biomass carbon was estimated. As a reference, soil organic matter originating from the humus layer of a 60-year-old Pinus sylvestris stand was used. As indicated by the initial rates of C mineralisation, geogenic carbon was microbially available but to a lower extent than soil organic carbon. During incubation, C mineralisation remained constant or tended to increase with time, depending on the origin of the sample, while it decreased in soil organic matter. Unlike in soil organic matter, in geogenic organic matter and carboniferous mine spoil, C mineralisation was not consistently promoted by lime addition. Prior to incubation, microbial biomass in geogenic organic matter and carboniferous mine spoil was about 10-fold lower than in soil organic matter and tended to increase with incubation time while it decreased in soil organic matter. Similar to C mineralisation, microbial biomass in geogenic organic matter increased after liming, while it declined in carboniferous mine spoil immediately after lime addition. Rates of net N mineralisation were very low in geogenic organic matter and carboniferous mine spoil regardless of the length of incubation and could not be enhanced by raising the pH. It was concluded, that in mine spoils where accumulation of soil organic matter has not yet occurred, geogenic organic matter can be favourable for the establishment of a heterotrophic microflora. However, in the short term, geogenic matter is no source for plant available N in mine spoils. This revised version was published online in June 2006 with corrections to the Cover Date. This revised version was published online in June 2006 with corrections to the Cover Date. This revised version was published online in June 2006 with corrections to the Cover Date.     

Seedling Growth and Heavy Metal Accumulation of Candidate Woody Species for Revegetating Korean Mine Spoils

Selecting plant species that can overcome harsh soil and microclimatic conditions and speed the recovery of degraded minelands remains a worldwide restoration challenge. This study evaluated the potential of three woody species and various organic and inorganic fertilization treatments for revegetating abandoned metalliferous mines in Korea. We compared survival, growth, and heavy metal uptake of species common to Korean minelands in two spoil types and a reference forest soil. Substrate type and fertilization both influenced seedling growth and metal concentrations substantially, but they had little effect on seedling survival. Fertilization increased the growth of all three species when grown in mine spoils but influenced the growth of seedlings grown in forest soil only marginally. Initial seedling survival and growth indicate that the study species can tolerate the heavy metal concentrations and other soil constraints of metalliferous spoil types. We estimate that plants can stabilize 2–22% of various heavy metals contained in spoil materials into plant biomass during 20 years of plantation growth. Combined with the erosion control and site amelioration benefits of mineland reforestation, stabilization of heavy metals in forest biomass justifies this treatment on abandoned Korean metalliferous mines.     

Pasture trees in tropical México: the effect of soil nutrients on seedling growth

Environment and seedling community under isolated trees in pastures are different from those in the open pasture. The effect of the pasture trees on the soil nutrients and on the seedling growth were investigated. Seven isolated trees and eight plots were selected in two pastures of 12-yr and 32-yr old derived from a lowland rain forest with nutrient-rich soil at Los Tuxtlas, Mexico. The soil concentrations of total N, P Bray, K+, Na+, Ca2+ and Mg2+, plus others physical and chemical characteristics, were compared between the pasture trees and the open-pasture. An experiment was done to test the hypothesis that soil from under the pasture trees was better for seedling growth than soil from the open pasture. Seedlings of two native tree species and two domesticated species were grown in soil from the two different sites in a shade-house. The dry weight of the shoot and root/shoot ratio were compared. Only total N, P and Na+ differed slightly in concentrations between the sites, but did not promote more seedling biomass. It seems that the soil at this location is sufficiently nutrient-rich even in the open pastures and over-ride any effect of the pasture trees on nutrient availability.     

长白山原始阔叶红松（Pinus koraiensis）林及其次生林细根生物量与垂直分布特征

以我国东北长白山自然保护区内同一海拔梯度的原始阔叶红松林及其次生林——白桦山杨成熟林和白桦山杨幼林为对象,采用土钻取样法对不同演替阶段细根生物量的变化、细根垂直分布规律及其影响因子进行系统地研究。研究结果表明,在原始阔叶红松林的正向演替过程中,林地细根的总生物量逐渐增加,其中主要乔木细根的生物量逐渐增加,而灌木和草本细根的生物量则逐渐降低。在演替过程中,细根的垂直分布逐渐加深。在长白山地区,3块林地中细根生物量的组成分布受林分植被组成的影响;细根的垂直分布与土壤容重、水分含量以及不同土层中C、N含量存在一定的相关性,但与土壤温度则不存在相关关系。     

Influence of a developing tree canopy on the yield of Pennisetum pedicellatum sown on a mine spoil

Abstract. Shoot and root biomass yield of a sown grass, Pennisetum pedicellatum, were measured at below-canopy, canopy edge and open locations in young monoculture stands of eight tree species planted on a coalmine spoil. Incident light as percentage of full sunlight decreased from open to canopy edge to below-canopy locations. The shoot and root weights of Pennisetum in different tree stands for each of the three locations were significantly different and were significantly related to each other, and to percentage sunlight across all tree species plots and locations. The gradient of incident light was the principal factor governing the gradient of grass biomass under developing canopies of tree plantations on the mine spoil.     

粤港澳大湾区不同恢复模式植物群落结构与生态系统健康的动态变化

基于长期定位监测数据,量化揭示了红锥纯林（Castanopsis hystrix）、10种与30种乡土树种混交林等3种乡土人工林植物群落的生物量、物种多样性、生物热力学健康水平（eco-exergy）和土壤理化性状在种植后13年内的发展动态,并与尾叶桉（Eucalyptus urophylla）纯林,以及自然恢复系统（灌草坡）进行了比较。结果表明：（1）研究期间,5种恢复模式的植物群落生物量均呈现波动上升趋势,但在发展节率上有所差异。13龄时的尾叶桉纯林与两种乡土树种混交林生物量显著高于其各自1龄时的水平,且显著高于自然恢复灌草坡;相较于其他人工林,红锥纯林生物量增长缓慢,但快于灌草坡;（2）5种恢复模式植物群落的物种多样性（物种丰富度、Shannon-Wiener指数、Pielou均匀度指数）在6至13龄间均呈下降趋势,且30种乡土树种混交林下降趋势最为显著。13龄时,两种混交林Shannon-Wiener指数略高于两种纯林,显著高于灌草坡;10种乡土树种混交林的Pielou均匀度指数略高于红锥纯林与30种乡土树种混交林,显著高于尾叶桉纯林与灌草坡。（3）4种人工林的植物群落生物热力学健康水平皆在6至13龄间显著增加;13龄时两种乡土混交林群落生态显著高于两种纯林,两种纯林显著高于灌草坡,且该差异主要源自于乔木层生态的差异。（4）不同植被恢复模式中,10种乡土树种混交林土壤养分的累积效果最佳,13龄时其土壤总氮含量显著高于红锥纯林和自然恢复灌草坡,但与30种乡土树种混交林和尾叶桉纯林无显著差异。（5）冗余分析结果显示,研究期间植被与土壤间的相关关系逐步建立,土壤理化性状对地上植被结构变化的解释度由1龄时的73.3%逐步上升至13龄时的82.0%,但只有土壤有机碳含量在13龄时与地上植被结构的相关性达到显著水平。上述结果表明,乡土种人工林与外来种人工纯林群落结构、生物热力学健康水平、及植被与土壤间关系的发展规律相似,且相对而言,混交林优于纯林,纯林优于自然恢复灌草坡。植被恢复的起始物种丰富度并不是越高越好;发展到13龄时,10种乡土树种混交林在植被结构与土壤改良方面均优于30种乡土树种混交林。植被与土壤间相关关系的建立是一个长期的过程,不同植被恢复模式对土壤理化性状的差异性影响难以在短期内有所显现。     

Growth response of native shrubs to acid mine spoil and to proposed soil amendments

Successful reclamation of acid mine sites may be enhanced by revegetating with species that are tolerant to acid mine spoil conditions. This study was conducted to assess the response of four native shrub species, Amelanchier alnifolia Nutt., Symphoricarpos albus (L.) Blake, Berberis repens Lindl., and Ceanothus sanguineus Pursh, to 1) pyritic acid mine spoil amended with various levels of lime and composted sewage sludge with added ammonium nitrate (CSS+N) and 2) acidified granitic spoil, with and without CSS+N. Species responded to soil acidity and nutrient supply similarly in both spoil materials. Berberis and Amelanchier exhibited acid soil tolerance, Symphoricarpos grew poorly in acidic soils but had low mortality, and Ceanothus responded to low pH with very poor growth, high mortality, or both. Amelanchier was conservative in growth and did not respond to either soil pH or nutrient supply with significant differences in biomass accumulation. Symphoricarpos varied in response to CSS+N but was most productive at neutral or higher pH. Berberis responded to nutrient availability with substantial increases in biomass production, including significant growth in strongly acidic spoil. Ceanothus responded to nutrient availability with large increases in biomass and was most productive with added CSS+N at neutral or higher pH. Nitrogen fixing nodules developed on the roots of Ceanothus plants grown in granitic spoil without CSS+N. The results indicated that these species differ significantly in acid soil tolerance and in their potential for growth, stress tolerance, and resource acquisition.     

Topsoil Seed Bank of an Oak–Hickory Forest in Eastern Kentucky as a Restoration Tool on Surface Mines

Typical reclamation practices in the central Appalachian coal region often use compacted spoils as a topsoil replacement, and these soils are revegetated with aggressive grasses and legumes. This restoration approach results in an herbaceous‐dominated landscape with limited natural succession by native flora. An alternative restoration method is to save topsoil prior to mining, stockpile it during mining, and then replace it on uncompacted spoils to “inoculate” the site with native plant species. In an effort to test this approach, vegetation assessments were performed at a relatively undisturbed forested site in Clay County, Kentucky, U.S.A. Eight 15 × 15–m plots were established, and soils from individual plots were used in seed bank studies both in the greenhouse and on loose‐dumped mine spoils. Bulk soil samples were removed from the plots and subjected to cold stratification for 13 weeks, after which seeds were allowed to germinate under greenhouse conditions for 1 year. Additional topsoil (approximately 1.5 m³ from the upper 0–20 cm) was removed from the plots and replaced on fresh spoil in eight 2 × 5–m plots. Controls consisted of uncompacted spoil material substrate only. A total of 105 species emerged in the greenhouse from the seed bank. On the relocated topsoil, 69 species were recorded of which 39 were also observed in pre‐mine vegetation surveys. Ten of the 17 most important pre‐mine forested site species emerged from the relocated topsoil treatments on the mine site. Our results indicate that application of topsoil could enhance plant diversity and native species reestablishment on surface‐mined lands.     

Use of Arbuscular Mycorrhiza and Organic Amendments to Enhance Growth of Macaranga peltata (Roxb.) Müll. Arg. in Iron Ore Mine Wastelands

Macaranga peltata (Roxb.) Mull. Arg. is a disturbance tolerant plant species with potential in mine wasteland reclamation. Our study aims at studying the phyto-extraction potential of M. peltata and determining plant-soil interaction factors effecting plant growth in iron ore mine spoils. Plants were grown in pure mine spoil and spoil amended with Farm Yard Manure (FYM) and Vermicompost (VC) along with arbuscular mycorrhizal (AM) species Rhizophagus irregularis. Pure and amended mine spoils were evaluated for nutrient status. Plant growth parameters and foliar nutrient contents were determined at the end of one year. FYM amendment in spoil significantly increased plant biomass compared to pure mine spoil and VC amended spoil. Foliar Fe accumulation was recorded highest (594.67μg/g) in pure spoil with no mortality but considerably affecting plant growth, thus proving to exhibit phyto-extraction potential. FYM and VC amendments reduced AM colonization (30.4% and 37% resp.) and plants showed a negative mycorrhizal dependency (–30.35 and –39.83 resp.). Soil pH and P levels and, foliar Fe accumulation are major factors determining plant growth in spoil. FYM amendment was found to be superior to VC as a spoil amendment for hastening plant growth and establishment in iron ore mine spoil     

Biomass and production of fine and coarse roots during regrowth of a disturbed subtropical humid forest in north-east India

Seasonal variation and depthwise distribution of dry matter in roots of different diameter classes and their annual production were studied using sequential core sampling. The investigations were carried out in three stands of a subtropical humid forest of north-east India representing different stages of regrowth after tree cutting. The mean annual standing crop of fine (<2 mm in diameter) and coarse (2–15 mm diameter) roots increased gradually from 5.4 Mg ha^-1 and 0.7 Mg ha^-1 in 7-yr old regrowth to 9.4 Mg ha^-1 and 2.8 Mg ha^-1 in 16-yr old regrowth, respectively. The contribution of fine roots to the total root mass declined from 88% in 7-yr old regrowth to 77% in both 13 and 16-yr old regrowths, while that of coarse roots increased from 12 to 23%. A major portion of fine roots (59–62%) was present in 0–10 cm soil layer, but the coarse roots were concentrated in 10–20 cm soil depth (38–48%). In all the three stands, biomass of both fine and coarse roots followed a unimodal growth curve by showing a gradual increase from spring/pre-rainy season to autumn/post-rainy season. Biomass to necromass ratio increased from 2.5 in the 7-yr old to 3.2 in the 16-yr old stand. The annual fine root production increased from 5.9 Mg ha^-1 to 7.7 Mg ha^-1 and total root production from 7.6 Mg ha^-1 to 14.7 Mg ha^-1 from 7-yr to 16-yr old regrowth.     

Carbon and nitrogen cycling during old-field succession: Constraints on plant and microbial biomass

Soil C and N dynamics were studied in a sequence of old fields of increasing age to determine how these biogeochemical cycles change during secondary succession. In addition, three different late-successional forests were studied to represent possible "steady state" conditions. Surface soil samples collected from the fields and forests were analyzed for total C, H₂O-soluble C, total N, potential net N mineralization, potential net nitrification, and microbial biomass. Above-and belowground plant biomass was estimated within each of the old field sites.Temporal changes in soil organic C, total N and total plant biomass were best described by a gamma function [y =at ^b e ^ctd +f] whereas a simple exponential model [y =a(l – e^–bt ) + c] provided the best fit to changes in H₂O-soluble C, C:N ratio, microbial C, and microbial N. Potential N mineralization and nitrification linearly increased with field age; however, rates were variable among the fields. Microbial biomass was highly correlated to soil C and N pools and well correlated to the standing crop of plant biomass. In turn, plant biomass was highly correlated to pools and rates of N cycling.Patterns of C and N cycling within the old field sites were different from those in a northern hardwood forest and a xeric oak forest; however, nutrient dynamics within an oak savanna were similar to those found in a 60-yr old field. Results suggest that patterns in C and N cycling within the old-field chronosequence were predictable and highly correlated to the accrual of plant and microbial biomass.     

模拟N沉降对太岳山油松人工林和天然林草本群落的影响

由于人类活动氮沉降呈逐年增加的趋势,进而增加了陆地生态系统氮的输入,从而影响陆地生态系统多样性、物种组成和功能。为揭示氮沉降增加对油松林草本群落的影响,于2009年7月在太岳山油松人工林和天然林,设计4个施氮水平:对照(CK,0 kg N hm-2a-1),低氮(LN,50 kg N hm-2a-1),中氮(MN,100 kg N hm-2a-1)和高氮(HN,150 kg N hm-2a-1),研究草本群落的生物多样性、生物量以及草本元素含量对模拟N沉降的响应。研究结果表明:模拟N沉降未能显著影响人工林草本群落的生物多样性(P0.05),而中氮、高氮显著降低了天然林草本群落的生物多样性(P0.05);从Jaccard指数和Sorensen指数分析得出人工林不同氮水平之间草本群落差异性较小,而天然林不同氮水平之间草本群落差异性较大。模拟N沉降没有显著改变人工林草本群落生物量(P0.05),而高氮明显促进天然林草本群落生物量的增加(P0.05)。与对照相比,模拟N沉降提高了人工林和天然林羊胡子苔草叶根中的全N含量(P0.05),而降低了全Mg的含量(P0.05),并且根部元素含量变化与土壤养分含量变化较为一致。施氮提高了N/K、N/Ca、N/Mg(P0.05)的比值。说明油松林下草本群落对氮沉降的响应因林分土壤N饱和程度以及林地利用历史的不同而产生差异,其中天然林响应最为敏感。     

青海省森林细根生物量及其影响因子

细根是植物吸收水分和养分的主要器官。全球变暖背景下,研究森林细根生物量及其环境因子的变化对生态系统碳平衡、碳收支及其贡献率具有重要意义。采用土钻法和室内分析法对青海省森林6个海拔梯度上5种林分类型的细根生物量和土壤理化性质进行测定,并分析了与环境因子之间的相互关系。结果表明:(1)青海省森林0—40 cm土层总细根生物量平均为8.50 t/hm~2,随着海拔梯度的增加先降低后升高,不同海拔梯度细根生物量差异显著(P0.05),最大值出现在2100—2400 m处。(2)5种林分0—40 cm土层总细根生物量为:白桦白杨云杉圆柏山杨,不同林分间细根生物量差异不显著。(3)细根垂直分布随土层深度增加而减少,且70%的细根集中在表层(0—20 cm)。(4)土壤容重深层(20—40 cm)显著大于表层(P0.05),并随海拔梯度逐步增加,且林分间差异较大。(5)全碳(Total carbon, TC)、全氮(Total nitrogen, TN)、全磷(Total phosphorus, TP)含量表层显著高于深层。TC、TN随海拔升高先增后降低,TP则随海拔逐步降低。不同林分间土壤养分差异较明显。(6)结构方程模型分析得到海拔、土层、容重直接影响细根生物量,细根生物量直接影响土壤养分。林分类型通过土壤容重间接影响细根生物量。因此,林分和海拔通过影响土壤微环境而影响到细根生物量及其空间分布格局。     

施肥对日本落叶松人工林细根生物量的影响

以辽宁东部山区16年生日本落叶松人工林为研究对象,探讨施肥对落叶松细根总生物量、不同层次生物量及不同根序生物量的影响.结果表明,与对照相比,施氮肥显著降低细根总生物量(P<0.01),而施磷肥及施氮+磷肥处理的细根总生物量差异不显著(P>0.05).落叶松人工林表层土壤(0～10 cm)细根生物量明显高于亚表层(10～20 cm)(P<0.01),各处理样地表层生物量占总生物量的64％～73％.施肥对不同层次、不同级别根序细根生物量的影响不同.与对照相比,施氮肥显著地降低了表层土壤1、3、4、5级根生物量(P<0.05),施磷肥(5级根除外)、施氮+磷肥(2级根除外)表层土壤各级根序细根生物量降低均不显著(P>0.05).在亚表层土壤,施氮肥和磷肥对各级根序生物量均没有显著影响(P>0.05);施氮+磷肥显著增加了1级根生物量(P<0.05),而其余各级根序细根生物量差异不显著(P>0.05).     

Is decline in high altitude eucalypt forests related to rainforest understorey development and altered soil bacteria following the long absence of fire?

Abstract The objective of this study was to identify attributes of the understorey vegetation, soil root biomass, soil chemistry and microbial community that may be associated with tree decline in high altitude eucalypt forests in Tasmania. The sites studied were in healthy eucalypt forest, forest in decline and forest containing dead eucalypts dominated by rainforest, in north‐east (Eucalyptus delegatensis forest) and in north‐west (Eucalyptus coccifera forest) Tasmania. In both regions bare ground, rock and shrubby species were associated with healthy sites whereas decline sites were associated with moss and a tall understorey with a high percentage cover of rainforest species. Healthy sites had low root biomass in the top 10 cm of the soil profile relative to decline and rainforest sites. Seedlings of high altitude species were grown in rainforest soil (0.314% N and 0.060% P) and healthy eucalypt soil (0.253% N and 0.018% P). The four eucalypt species studied had similar root to shoot ratio in the two soils, but the rainforest species, Nothofagus cunninghamii and Leptospermum lanigerum, had higher root to shoot ratio in the healthy eucalypt than in the rainforest soil. We produced three soil filtrates: (i) fungi and bacteria present; (ii) bacteria only present and; and (iii) sterile, from healthy, decline and rainforest sites in north‐east and in north‐west Tasmania and used linseed as a germination bioassay. Filtrates from the north‐east decline and rainforest sites induced a significantly greater dysplastic germination response than healthy sites in (i) and (ii) filtrates, but this was not found in filtrates from sites in the north‐west. We conclude that while the development of a rainforest understorey and elevated soil root biomass in the long absence of fire is generally associated with high altitude eucalypt decline, altered bacterial and/or chemical attributes of soil are not always associated with high altitude eucalypt decline.     

暖温带森林土壤微生物量、群落结构和活性对植物地下碳源的响应

该研究以典型的亚热带—温带过渡区森林为对象,采用野外过程监测和控制试验相结合的方法,利用磷脂脂肪酸和土壤胞外酶活性分别表征土壤微生物群落结构和活性,并结合微环境因子,重点探究土壤微生物生物量、群落结构和活性对植物地下碳输入的响应特征。结果表明：在观测周期内,处理均能显著降低三组年龄段林分的土壤微生物量碳,其变化幅度在－8.72％~－5.72％之间,其中在80年的林分中降幅最大,而在160年的林分中降幅最小;微生物量氮的变化规律与相应的微生物量碳的变化规律相似,但与对照相比其差异性均未达到显著性水平;另外,经壕沟处理2~4个月后,所有林分的土壤微生物量碳和氮与对照相比出现增加的现象。处理均能对三组年龄段林分的土壤微生物群落结构产生不同程度的影响,其中40年林分的土壤微生物群落对处理的响应程度要高于另外两个年龄段的林分;与对照相比,壕沟处理样方的腐生真菌的相对丰富度均下降明显,其中在40年和80年林分中的下降幅度达到显著水平,而细菌、放线菌和丛枝菌根真菌均无明显变化;壕沟处理样方的水解酶(β-葡萄糖苷酶和N-乙酰-葡萄糖苷酶)活性均显著下降,而氧化酶(酚氧化酶和过氧化物酶)活性的变化相对较小,除80年的林分外,其余林分均不显著。此外,处理均不能显著影响土壤的含水量和温度。该研究结果为初步阐明全球气候变化背景下森林土壤微生物结构及其功能的变化特征以及更加精确预测未来森林土壤碳的变化趋势提供了科学依据。     

长白山原始阔叶红松林不同演替阶段地下生物量与碳、氮贮量的比较

以我国东北长白山自然保护区内同一海拔水平的原始阔叶红松林及其次生林--白桦山杨成熟林和幼林为对象,对不同演替阶段林地地下生物量与碳、氮贮量进行了研究.结果表明,随着演替的进行,白桦山杨幼林、成熟林和阔叶红松林根系生物量分别为2.437、2.742和4.114 kg·m^-2,根系碳贮量分别为1.113、1.323和2.023kg·m^-2,土壤碳贮量分别为11.911、11.943和12.87 kg·m^-2,林地地下碳贮量分别为13.024、13.266和14.610kg·m^-2.3块林地中根系氮贮量分别为0.035、0.032和0.039 kg·m^-2,土壤氮贮量分别为1.207、1.222和0.915kg·m^-2,林地地下氮贮量分别为1.243、1.254和0.955 kg·m^-2.在长白山地区次生林演替和恢复过程中林地地下部分是潜在的碳汇,而土壤氮贮量则没有明显的变化规律.     

Invading Monotypic Stands of Phalaris arundinacea: A Test of Fire, Herbicide, and Woody and Herbaceous Native Plant Groups

Phalaris arundinacea L. is an aggressive species that can dominate wetlands by producing monotypic stands that suppress native vegetation. In this study invasion windows were created for native species in monotypic stands of P. arundinacea with either fire or herbicide. Three native species groups, herbaceous plants, herbaceous seeds, and woody shrubs, were planted into plots burned or treated with herbicide in the early spring. Fire did not create an effective invasion window for native species; there was no difference in P. arundinacea root and shoot biomass or cover between burned and control plots (p≥ 0.998). Herbicide treatment created an invasion window for native species by reducing P. arundinacea root and shoot biomass for two growing seasons, but that invasion window was fast closing by the end of the second growing season because P. arundinacea shoot biomass had nearly reached the shoot biomass levels in the control plots (p= 0.053). Transplant mortality, frost, and animal herbivory prevented the herbaceous species and woody seedlings from becoming fully established in the plots treated with herbicide during the first year of the experiment. Transplanted monocots had a greater survival than dicots. By the second growing season the herbaceous group had the greatest mean areal cover (5%), compared to the woody seedlings (3%) and seed group (0%). Long‐term monitoring of the plots will determine whether the herbaceous transplants will compete effectively with P. arundinacea and whether the woody species will survive, shade the P. arundinacea, and accelerate forest succession.     

CO_2倍增对植物生长和土壤微生物生物量碳、氮的影响

关于大气ＣＯ２浓度倍增（即为７００μｍｏｌＣＯ２·ｍｏｌ－１空气）将对植物生长产生诸多影响,已有大量报道［１,２］。但ＣＯ２倍增对植物及所在土壤中微生物影响的研究甚少［３,４］。土壤微生物是陆地生态系统中最活跃的成分,担负着分解动植物残体的重要作用,...