热带季节雨林和人工橡胶林林冠截留雾水的比较研究

利用 4a( 1 999～ 2 0 0 2 )的雾水截留观测资料 ,对西双版纳热带季节雨林和人工橡胶林林冠截留雾水进行了研究。热带季节雨林和人工橡胶林全年由林冠截留的雾水分别达 89.4± 1 3.5 mm和 1 8.6± 2 .5 mm(平均值±标准差 ) (雾季各占 62 .9%± 4.8%和 91 .9%± 6.3% ) ,分别占全年降水量的 4.9%± 1 .7%和1 .1 %± 0 .2 %。年雾水截留量与年降雨量呈负相关关系。月雾水截留量与月均最低气温呈显著的负相关 ,与月均相对湿度、月均 0∶ 0 0～ 1 0∶ 0 0风速呈显著的正相关。热带季节雨林全年 68%± 5 %、人工橡胶林40 %± 4%的有雾天气里可以收集到雾水 (分别为 0 .38± 0 .2 7mm/ d和 0 .2 4± 0 .1 2 mm/ d) ,且日雾水截留量与气温和风速呈显著的相关 ,即 :气温越低、风速越大 ,日雾水截留量越多。对本地区热带季节雨林生态系统的健康生长和维持而言 ,雾及雾水极大的弥补了降雨量的不足 ,雾的这种作用在降雨量少的年份似乎更为重要     

西双版纳热带季节雨林林冠截留雾水和土壤水的关系

利用2002年1月-2003年12月在西双版纳热带季节雨林观测样地收集的林冠截留滴落雾水、雨水、浅层土壤水和地下水水样,对其氢、氧稳定性同位素比率δD和δ^18O的测定结果进行了分析,研究了林冠截留雾水对土壤水和地下水的影响。干季（11-翌年4月份）,热带雨林林冠截留雾水的稳定性同位素比率、过量氘（d-excess）值明显高于雨水的相应值,表明雾水水汽中包含了区域森林植被蒸发、蒸腾的再循环水汽。林下地表浅层土壤水的稳定性同位素比率介于雾水和雨水的同位索比率之间,表明浅层土壤水来源于雾水和雨水的补给,但是干季浅层土壤水包含更多的雾水。在降雨稀少的干季,浅层土壤水主要来自雾水的补给,表明了林冠滴落的雾水是林下幼树和耐阴树种生长和生存的重要环境因子。干季和雨季（5-10月份）地下水的稳定性同位素比率与雨水的均没有显著差别,表明雾水对地下水的补给没有贡献,其水分补给仅仅来自雨水。     

西双版纳热带季节雨林林下土壤蒸发的稳定性同位素分析

利用2002年1月～2003年12月在西双版纳热带季节雨林样地测定的大气降雨、林冠穿透雨、林冠滴落雾水、溪流水水量及其氢、氧稳定性同位素比率δD和δ18O的测定结果,分析了热带季节雨林林下土壤的蒸发率.结果表明,热带雨林在雨水偏多的2002年和雨水偏少的2003年的蒸发散分别为1186 mm和987 mm,明显低于世界其它湿润热带雨林的蒸发散值;雾水的稳定性同位素比值明显重于雨水,表明雾水中包含区域再循环的蒸发水汽;由于森林林冠和林下土壤的蒸发作用,穿透雨水和溪水的稳定性同位素值又明显重于雨水的相应值.根据溪流水和穿透水（穿透雨水＋滴落雾水）的同位素差值,利用平衡状态下的瑞利蒸馏方程计算的森林土壤蒸发率表明,这两年的森林总蒸发散中分别有5.1%和3.1%来自林下土壤的蒸发.分析认为,持久、浓重的辐射雾是导致西双版纳地区热带雨林蒸发散和土壤蒸发率较低的重要因子.     

中国森林生态系统林冠层降雨截留特征

森林生态系统作为陆地生态系统的主体,其发达的林冠层通过调节降水量、改变降水强度等深刻影响着流域全过程水文通量及水分输出。以中国广泛开展的典型森林降雨再分配过程的年尺度监测数据为基础,揭示中国不同类型森林生态系统的降雨再分配及林冠层降雨截留特征,阐明森林生态系统林冠层截留特征与降雨、植被要素的关系。结果表明:我国不同森林生态系统年穿透雨量处于141.4-2450.0 mm之间,年穿透雨率为36.3%-92.3%。5种典型森林生态系统多年平均穿透雨量((445.3±252.9)-(1230.6±479.6) mm)占同期多年平均降雨量的(72.6±9.2)%-(77.4±8.9)%。不同森林生态系统年树干茎流量介于0-508.2 mm之间,占同期年降雨量的0-25.8%。5种典型森林生态系统树干茎流量多年平均值((9.8±17.3)-(87.8±81.6) mm)占同期多年平均降雨量的(1.4±1.9)%-(5.4±4.6)%。不同森林生态系统林冠层年降雨截留范围在25.7-812.9 mm之间,占年降雨量的4.2%-55.6%。5种典型森林生态系统多年平均林冠截留量((154.2±81.6)-(392.2±203.5) mm)占同期年平均降雨量的(18.7±7.4)%-(25.9±8.3)%。进一步分析表明,我国森林生态系统穿透雨量、树干茎流量和林冠层截留量随观测区年降雨量的增加而呈显著增大(P<0.05),年穿透雨率、年树干茎流率随年降雨量的增加呈显著线性上升趋势(P<0.05),而年林冠截留率与年降雨量呈显著的负相关关系(P<0.01),降雨量、叶面积指数是深刻影响森林生态系统林冠层降雨截留率等特征的重要因素。整体上,不同类型森林生态系统林冠截留降雨能力存在明显差异,林冠层截留率突出表现为:落叶林大于常绿林、针叶林大于阔叶林。     

中亚热带红壤区油桐(Vernicia fordii)林冠水文效应特征

于从2004年7月到2005年9月,对南方红壤区油桐人工林的穿透雨、树干流和林冠截留的水文特征进行了监测,并对其影响因素进行初步分析,结果表明：在整个测定期间,油桐林穿透雨占总降雨量75.6%±8.6%,树干流占3.6%±1.1%,而截留量占20.8%±9.1%。油桐林冠对降雨的再分配受到降雨量和降雨强度的影响,随着雨量的增加,穿透雨、树干流和截留量相应地提高,并且树干流和截留量在高的雨量下逐渐趋于稳定;随着降雨强度的增加,穿透雨率逐渐升高,而树干流率和截留率降低。在不同雨量级间,油桐穿透雨具有显著性的差异,但树干流的差异不显著。油桐林下水分输入存在明显的空间异质性,穿透雨在不同观测点间具有显著性差异,靠近树干的林冠内部穿透雨低于林冠边缘,而且随着降雨量或降雨强度的增加,穿透雨的空间异质性(穿透雨率的变异系数CV)降低;树干流对降雨也具有明显的汇集作用,在树干周围输入的雨量是林外降雨量20~70倍,并且随着降雨量的增加,这种汇集效应（漏斗比率）先提高后降低。同时油桐单株树干流(cm³•mm^-1)与胸径、树高和冠层面积均呈显著正相关(p<0.05),但是与枝下高的相关性不显著(p>0.05)。     

热带人工橡胶林林冠截留雾水的边缘效应研究

利用 2 0 0 1年 1 1月～ 2 0 0 2年 1 0月的林缘和林内雾水截留及相关环境因子观测资料 ,对西双版纳热带人工橡胶林林冠截留雾水的边缘效应进行了研究。西双版纳热带人工橡胶林内的雾日数及雾日频率呈现明显的季节变化 ,全年雾日数可达 1 72 d,其中雾季 (1 1～翌年 2月份 )的雾日数及雾日频率最多 (高 ) ,月均雾日数可达 2 3d(76 .7% )。由林缘至林内 ,年雾水截留量在迎风面和背风面均呈现指数形式急剧减小 ,二者均是在林缘最边行外测的林冠下 (0 m处 )达到最大 ,分别为 4 1 .1 mm和 2 4 .3mm。迎风面和背风面林缘 0 m处的雾水截留量分别是林内雾水截留量 (1 6 .2 mm )的 2 .5倍和 1 .5倍。迎风面雾水截留在林内约 2 5 m处趋于稳定 ,而背风面在林内约 1 5 m处趋于稳定。林缘处的雾水截留量与日 0 :0 0～ 1 0 :0 0平均风速呈显著的正相关(P<0 .0 1 )。风速大 ,则雾水截留的边缘效应向林内越深入 ,且空间变异性减小。相对于迎风面林缘 0 m处的雾水截留而言 ,大的风速将削弱林内和林缘雾水截留量的差别 ,从而导致更多的雾水进入森林     

中亚热带红壤区油桐(Vernicia fordii)林冠水文效应特征

于从2004年7月到2005年9月,对南方红壤区油桐人工林的穿透雨、树干流和林冠截留的水文特征进行了监测,并对其影响因素进行初步分析,结果表明：在整个测定期间,油桐林穿透雨占总降雨量75．6％±8．6％,树干流占3．6％±1．1％,而截留量占20．8％±9．1％。油桐林冠对降雨的再分配受到降雨量和降雨强度的影响,随着雨量的增加,穿透雨、树干流和截留量相应地提高,并且树干流和截留量在高的雨量下逐渐趋于稳定;随着降雨强度的增加,穿透雨率逐渐升高,而树干流率和截留率降低。在不同雨量级间,油桐穿透雨具有显著性的差异,但树干流的差异不显著。油桐林下水分输入存在明显的空间异质性,穿透雨在不同观测点间具有显著性差异,靠近树干的林冠内部穿透雨低于林冠边缘,而且随着降雨量或降雨强度的增加,穿透雨的空间异质性（穿透雨率的变异系数CV）降低;树干流对降雨也具有明显的汇集作用,在树干周围输入的雨量是林外降雨量20-70倍,并且随着降雨量的增加,这种汇集效应（漏斗比率）先提高后降低。同时油桐单株树干流（cm^3·mm^-1）与胸径、树高和冠层面积均呈显著正相关（P〈0．05）,但是与枝下高的相关性不显著（p〉0．05）。     

樟树叶油地理变异的研究

对分布在福建省不同地区的樟树〔C innam omum camphora(L.)Presl〕叶油含量和主要化学成分进行分析,结果表明,J3(118°16′~119°29′)和W 1(28°18′~27°30′)交叉区域芳樟叶油含量(1.90%±0.30%)和芳樟醇含量(95.34%±1.10%)较高,可作为优良芳樟选育的重点区域;J2(117°03′~118°16′)和W 3(26°42′~25°54′)交叉区域桉樟叶油含量(1.36%±0.48%)和1,8-桉叶油素含量(10.44%±17.28%)较高,可以作为优良桉樟选育的重点区域。J2和W 2(27°30′~26°42′)交叉区域樟脑叶油含量(1.13%±0.65%)和樟脑含量(4.80%±13.97%)较高,可以作为优良脑樟选育的重点区域;J4(119°29′~120°43′)和W 6(24°18′~23°31′)交叉区域黄樟叶油含量(1.05%±0.34%)和黄樟油素含量(9.01%±16.73%)较高,可以作为优良黄樟选育的重点区域。樟树叶油含量和主成分类型及含量呈明显的地理分布。     

6种人工针叶幼林下地表苔藓植物层片的物种多样性与结构特征

 为了评估人工林苔藓植物发育状况,同时为人工林生态功能评价提供依据,采用样地取样方法,调查分析了岷江上游大沟流域6种人工幼龄针叶林（川西云杉(Picea balfouriana)林、日本落叶松(Larix kaempferi)林、油松(Pinus tabulaeformis)林、华山松(Pinus armandii)林、油松-华山松混交林和川西云杉-华山松混交林）林下地表苔藓植物层片物种组成、多样性以及结构特征及其异同。6种人工林下共发现了19种苔藓,各林下组成数量在7～13种。除云杉林外,纯林下苔藓种数均小于或者等于混交林下;6种人工林下地表苔藓植物平均盖度、平均密度、平均厚度分别在0.41%±1.49%～17.79%±1.67%、(27.99±367.95)～(3 807.11±412.90)株•m-2和(1.80±1.51)～(19.89±1.69) mm之间。无论是多样性指数,还是结构参数,均以川西云杉林最高,而华山松林最低。总体说来,岷江上游人工针叶幼林下地表苔藓组成物种较少、物种多样性指数（物种丰富度指数、Shannon-Wiener指数）低、Simpson指数高、结构参数（密度、盖度、厚度）较小,说明林下地表苔藓植物组成单一、结构相当简单,发育不良。综合分析表明,具有相对较低林冠郁闭度与林木密度的云杉林是6类人工林中恢复状况相对最好的类型,暗示出疏伐、修枝等管理措施可促进人工密林下地表苔藓植物生物多样性以及地表苔藓植物层片结构的改善。     

连翘的二型花柱

报道了连翘中的二型花柱(长花柱和短花柱)。长花柱的柱头和雄蕊高度分别为6.12±0.05 mm和2.35±0.04mm,短花柱则为2.23±0.04mm和6.02±0.06mm。短花柱花的花冠大小明显超过长花柱。开放授粉条件下,长短花柱花的座果率分别为9.11 %±0.04%和8.93 %±0.07%。人工异交的座果率在长-短(36.8%±0.04%)与短-长(36.2%±0.07%)组合间无明显差异(F(1,39)=1 .38,P=0.14)。人工异交实验表明,传粉者限制可能发生在生长于中国东北部的人工连翘种群中,这可能是因为该地区早春的低温和多风气候条件影响传粉者的种类和活动。     

西双版纳热带季节雨林内雾特征研究

 利用4年（1999～2002）的雾观测资料,对西双版纳热带季节雨林内雾特征进行了观测研究。结果表明,雾首先形成于最上林冠层,林下雾是由上层雾变浓、下沉而来。夜间,雾形成前,气温高于叶表温;雾形成后,气温则低于叶表温。热带雨林内各季节雾日数和雾日频率均高于无林地。热带雨林内平均全年雾日数可达258 d,其中雾季和干热季共占154 d（59.6%）,而雾季的雾日频率高达90%。雾日数的季节变化与各季节雨量呈明显的负相关。雾季,雾在23∶00左右生成,比干热季、雨季分别提前0.7、2.3 h,而消散时间则分别推迟0.8、2.2 h。雾生成和消散时间呈现出较明显的负相关。雾季雾的持续时间达12.2 h·d-1,比干热季、雨季分别长1.5、4.6 h·d-1。全年雾总持续时间占全年时间的39.7%,而雾季的相应值为50.8%。雾的形成不仅凝结了水汽进入森林（全年89.4 mm）,同时也对森林起到了一定的保温作用,这对热带雨林的生存和发展具有至关重要的作用。     

Fog in the California redwood forest: ecosystem inputs and use by plants

Fog has been viewed as an important source of moisture in many coastal ecosystems, yet its importance for the plants which inhabit these ecosystems is virtually unknown. Here, I report the results of a 3-year investigation of fog inputs and the use of fog water by plants inhabiting the heavily fog inundated coastal redwood (Sequoia sempervirens) forests of northern California. During the study period, 34%, on average, of the annual hydrologic input was from fog drip off the redwood trees themselves (interception input). When trees were absent, the average annual input from fog was only 17%, demonstrating that the trees significantly influence the magnitude of fog water input to the ecosystem. Stable hydrogen and oxygen isotope analyses of water from fog, rain, soil water, and xylem water extracted from the dominant plant species were used to characterize the water sources used by the plants. An isotopic mixing model was employed to then quantify how much fog water each plant used each month during the 3-year study. In summer, when fog was most frequent, ～19% of the water within S.sempervirens, and ～66% of the water within the understory plants came from fog after it had dripped from tree foliage into the soil; for S.sempervirens, this fog water input comprised 13–45% of its annual transpiration. For all plants, there was a significant reliance on fog as a water source, especially in summer when rainfall was absent. Dependence on fog as a moisture source was highest in the year when rainfall was lowest but fog inputs normal. Interestingly, during the mild El Niño year of 1993, when the ratio of rainfall to fog water input was significantly higher and fog inputs were lower, both the proportion and coefficient of variation in how much fog water was used by plants increased. An explanation for this is that while fog inputs were lower than normal in this El Niño year, they came at a time when plant demand for water was highest (summer). Therefore, proportional use of fog water by plants increased. The results presented suggest that fog, as a meteorological factor, plays an important role in the water relations of the plants and in the hydrology of the forest. These results demonstrate the importance of understanding the impacts of climatic factors and their oscillations on the biota. The results have important implications for ecologists, hydrologists, and forest managers interested in fog-inundated ecosystems and the plants which inhabit them.     

The dendroecological potential of shrubs in north Iranian semi-deserts

In deserts and semi-deserts such as in the Irano-Turanian region in northern Iran, forest vegetation is scarce but shrubs are dominant. For this floristic province, placed in a biodiversity hotspot with a cold and dry climate, we provide the first climate-growth study on shrubs. From stems of three wide-spread shrubs (Astragalus, Rhamnus and Ephedra species) annual rings were identified and their widths measured.On average, around 40-year long annual-ring series per stem were obtained, cross-dated and related to meteorological variables. Astragalus and Rhamnus reflected a clear regional climate signal in their ring widths whereas Ephedra showed an only weak association with climate variables. While above-average air humidity in combination with low temperatures in spring and summer favored shrub growth, precipitation had surprisingly only a weak effect on growth. From the abundance of fog events in this area, we concluded that the extreme moisture dependency of the shrubs before and throughout the growing season may have been relieved by the uptake of fog drip through the foliage.As projected by climate models, the deficit in humidity will intensify and temperature will continue to rise in this region. So, the ability of the Irano-Turanian endemic shrubs to infiltrate into neighboring regions could become limited and their current distribution range may be confined to higher elevations which provide a moister and cooler environment.     

A resource-sharing model based on a repeated game in fog computing

With the rapid development of cloud computing techniques, the number of users is undergoing exponential growth. It is difficult for traditional data centers to perform many tasks in real time because of the limited bandwidth of resources. The concept of fog computing is proposed to support traditional cloud computing and to provide cloud services. In fog computing, the resource pool is composed of sporadic distributed resources that are more flexible and movable than a traditional data center. In this paper, we propose a fog computing structure and present a crowd-funding algorithm to integrate spare resources in the network. Furthermore, to encourage more resource owners to share their resources with the resource pool and to supervise the resource supporters as they actively perform their tasks, we propose an incentive mechanism in our algorithm. Simulation results show that our proposed incentive mechanism can effectively reduce the SLA violation rate and accelerate the completion of tasks.     

Horizontal and vertical distribution of saproxylic beetles (Col., Buprestidae, Cerambycidae, Scolytinae) across sections of forest edges

Abstract:  We evaluated the preferred home ranges of three saproxylic beetle taxa along transects from the open field into the forest interior, and from the forest floor up to the canopy. By means of trap sets on metal scaffolds, vertical and horizontal strata were sampled across two types of forest edges: soft-edge ecotones with a gradual transition from the field into the forest and hard edges with an abrupt transition. The forest edges consisted of different strata such as herbaceous fringe, shrub belt, unmanaged forest and managed forest. The thermophilic buprestids were mainly caught in the open land (herbaceous fringe and agricultural land) and in the upper forest mantle. In general, the cerambycids were most abundant in the open land and the lower forest mantle, but a few species favoured the forest interior. The bark beetles (Scolytinae) were equally distributed in all habitats. These distribution patterns of the taxa were observed in terms of both species numbers and abundances. Each species with at least five collected specimens was assigned to one of the three habitat types: open land, forest mantle and forest interior. Of 74 ranked species, only 16% were prevalent in the forest interior and are thus considered to be true forest species. The other 84% of the species were attributed to open land or the forest mantle and are, therefore, forest edge species. Soft forest edges generally supported a higher species richness than hard edges, particularly as regards Cerambycidae and Scolytinae. In terms of Shannon diversity, soft edges tended to be more diverse in buprestids and cerambycids. Overall, the forest interior showed the least species richness and diversity. Therefore, for the conservation of saproxylic beetles, not only the amount and quality of dead wood is important, but also the presence and design of forest boundary structures.     

Seasonal and Spatial Patterns in Ground Foraging Ants in a Rain Forest in the Western Ghats,India1

Seasonal variation and spatial distribution in ground foraging rain forest ants were studied in South Kannada–Kodagu District in Karnataka (India) between 1990 and 1991 by pit-fall trap sampling. All ant species showed marked seasonality. A total of 31 species were recorded from the primary forest over a period of two years. More species were recorded from the closed canopy forest than from tree fall gaps in primary forest. All ant species showed marked seasonality with fewer species and individuals sampled/plot during the wetter seasons. The numerically dominant species, Pheidole sp., was markedly lower in abundance during the wet seasons. Spatial patterns were also studied during a dry season both in the primary forest and an adjacent logged forest. More species were recorded from the logged forest than the primary forest. Community composition in primary forest was different from that in logged forest. Common species were more ubiquitous than rarer species. Species were distributed bimodally across sampling plots. Probable underlying processes behind these seasonal and spatial patterns have been discussed.     

喀斯特峰丛洼地不同类型森林养分循环特征

以中国西南喀斯特峰丛洼地为研究区域用标准木法和收获法对人工林、次生林、原生林3个不同类型森林的6个代表性群落的生物量、营养元素生物循环量及循环特征进行了研究。结果表明:(1)不同类型森林群落乔木各器官的养分含量大小顺序为:叶枝根干,林下植被层和凋落物层的养分含量比较高,其含量普遍高于乔木层各组分,仅次于乔木叶片;各组分中营养元素以K、Ca最高,P、Mg最低;(2)3种类型森林间乔木层的养分积累量总规律表现为原生林(4540.30 kg/hm~2)次生林(2107.09 kg/hm~2)人工林(719.51 kg/hm~2),分别占林分养分积累量的88.30%、79.57%和62.60%;(3)3种类型森林生态系统养分总贮量相差不大,均主要集中在土壤层在各层分配格局有所差异;营养元素的年吸收量和年归还量均为次生林原生林人工林,年吸收量分别为:418.80、271.17和148.79 kg hm~(-2)a~(-1);年归还量分别为:182.98、111.43和43.37 kg hm_(-2)a~(-1);(4)不同类型森林养分利用系数总规律为人工林(0.35)次生林(0.20)原生林(0.10);循环系数则相反,为原生林(0.48)次生林(0.46)人工林(0.30);而周转时间为原生林(37.32)人工林(18.63)次生林(13.93)。喀斯特峰丛洼地土层薄,养分贮存能力差,森林养分循环能力相对较弱,沿着强、中、弱干扰递减梯度,3种类型森林养分利用效率和循环能力呈增长趋势。     

Biodiversity and spatial distribution of vascular epiphytes in two biotopes of the Cameroonian semi-deciduous rain forest

The diversity and spatial distribution of vascular epiphytes were surveyed in two biotopes (dryland forest and swamp-inundated forest) of the semi-deciduous rain forest area in Cameroon. Eight sites in each biotope were selected, which included 530 individuals of phorophytes in dryland forest and 460 in swamp-inundated forest. A total of 148 epiphyte species were recorded, which showed that semi-deciduous rain forests represent a major source of African-epiphyte diversity. Dryland forest hosted 110 epiphyte species, while the swamp-inundated forest harboured 108. A total of 56 species were found only in the dryland forest and 60 were restricted to the swamp-inundated forest. At family level, Orchidaceae exhibited the highest-species richness within both biotopes. Pteridophytes were more abundant in the swamp-inundated forest. A TWINSPAN analysis of the floristic similarities separated the two investigated forest types very clearly. No significant difference existed between the two biotopes regarding vertical distribution of epiphytes within single trees. The swamp-inundated forests may serve as a refuge for many epiphytes that occur in the outer canopy of the dryland forests, both because they are inherently less vulnerable to timber extraction, and enjoy better protection by legislation.     

冻融交替对长白山不同林型土壤两种温室气体排放的影响

以长白山5种林型土壤(硬阔叶林、红松阔叶林、次生白桦林、长白松林和蒙古栎林)为对象,利用原位培养连续取样法研究了冻融过程中5种林型土壤CO2和N2O排放特征及相关机理.结果 表明:冻融期5种林型土壤是CO2和N2O的源.次生白桦林和红松阔叶林土壤CO2和N2O的平均通量显著高于其他3种林型.除硬阔叶林外,各林型土壤CO...     

宝天曼地区栓皮栎林恢复过程中高等植物物种多样性变化

对宝天曼地区不同恢复阶段栓皮栎林的高等植物物种多样性特征进行了初步分析。结果表明,各层物种丰富度和多样性指数在不同恢复阶段栓皮栎林表现出草本层＞灌木层＞乔木层的趋势。乔木层物种丰富度和多样性指数基本上随恢复时间的增加而增加;灌木层在未破坏的栓皮栎林内较低,而在其他恢复阶段的栓皮栎林内基本相同;草本层在恢复５年、１５年和２５年的栓皮栎林中较高,而在恢复４５年和未破坏的栓皮栎林内较低。乔木层物种均匀度指数在未破坏的栓皮栎林中较高,在恢复２５年的栓皮栎林中较低;灌木层在恢复４５年的栓皮栎林中较高,在恢复１５年的栓皮栎林较低;草本层在恢复５年的栓皮栎林中较高,在恢复１５年的栓皮栎林中较低。不同恢复阶段栓皮栎林各层次间的物种多样性差异大多不显著,只有乔木层和草本层及灌木层和草本层之间的物种丰富度指数有显著差异。不同恢复阶段栓皮栎林在乔木层物种多样性特征上的差异最大,在灌木层物种多样性特征上有一定差异,在草本层物种多样性特征上没有明显的差异。