土壤水分梯度对阔叶红松林结构的影响

2002年8月,在吉林省白河林业局红石林场(12755E,4230N),沿着一个山坡设置了一个长宽为112m8m、包含14个样方的样带。调查了群落结构、0-10cm和10-20cm的土壤含水量、枯落物现存量及其C、N、P含量,主要树种的叶片和枝条的C、N、P含量。沿着山坡的不同位置土壤含水量的不同导致阔叶红松林的群落结构发生变化。蒙古栎的比例随着土壤含水量的下降而逐渐升高,而其他主要阔叶树种则逐渐减少乃至消失。枯落物的水分变化趋势与土壤一致。在不同坡位枯落物的分解状况不同,干重差异显著。坡下枯落物含量较坡上的丰富,部分原因在于群落结构的变化。水分和养分含量的变化影响了枯落物的成分、降解及其养分的释放,进一步影响了林木的生长速度和林分结构并最终影响整个生态系统。图7表2参14。     

Effect of fertilization on the litter fall of pinus sylvestris and betula pubescens on drained peatlands

NPK fertilization on a dwarf shrub pine bog initially increased the amount and nutrient content of the tree litter. Eight years after fertilization, however, the amount of micronutrients decreased compared to the amount of N and P in the litter. Fertilization on a fertile mire also increased the nutrient content of the litter fall, especially in the mature pine and birch stands. The amount of nutrients in the litter fall of the birch stands was considerably greater than that in the pine stand of the same volume.     

秦岭松栎林带生物量及其营养元素分布特征

秦岭脱齿栎林、油松林和华山林（包括０－６０cm土层）营养元素总贮量达２９．２５００－３９０．１７３９t.hm^-2，其大小为锐齿栎林＞华山松＞油松林，土壤中营养现贮量占系统总量的９３．１０％－９９．３９％，植被层和凋落物层仅占０．５７％－３．００％和０．１０％－１．９９％；３林分乔木层生物量、木材蓄积量和营养元素积累量平均值分别为１２０．４８３t.hm^-2,129.384m^3.hm^-2和１２２６．９kg.hm^-2，锐齿栎林＞油松林＞华山松林。３林分林下植被层生物量现存量和营养元素积累量平均值分别为１．５５３t.hm^-2和５３．１kg.hm^-2，锐齿栎林最大，华山松林最小。林下凋落物现存量和营养元素积量平均值分别为１７．４７５t.hm^-2和５０２．５kg.hm^-2，３林分凋落物现存量、营养元素含量及其积累量都存在明显的差异。锐齿栎林、油松林和华山松林营养元素年吸收量、归还量、存留量和平均归还率分别为３３．４、１４７．２和２６４．３，１９５．６、６６．９和８４．１，１３８．８、８０．４和１８０．２kg.hm^-2和０．５８５、０４５４和０．３１８，３林分各营养元素的年吸收量，归还量和存留量也存在一定的差异，锐齿栎林干和皮中Ｃa和Ｍg含量远远高于油松林和华山松林的，锐齿栎林多代连作势必导致营养元素的大量流失，特别是Ｃa和Ｍg，会破坏土壤原有离子动态平衡，引起林地土壤理化性质改变，林地生产潜力逐渐下降。     

Effect of vegetation and land use on soil fertility in Wutai Mountains of Shanxi Province

IntroductionSoilpropertiesdependonclimate,vegetationtypes,parentmaterials,landformandsoilderivedage(Bei-jingForestryCoIlege1982).VegetationpIaysasig-nificantroIeintheformationofsoiIparticuIarIyforthepropertiespfSurfBcesoil.PlantsabsorbselectivelynutrientfromsoilandbuiIdtheirbodies.ThenutrientpartofIitterdecomposedgradualIybymicrobeswouldraturntoground-TheroOtsystemOfplantaIsoplaysasignificantroleinsoiIproperties.EffectofpIantsonsoildependonthevegdstiontype,speciescomposi-tion,age,dens…     

The effects of microhabitat,plant litter,and seed burial on the regeneration of Quercus wutaishanica and Pinus tabulaeformis

The effects of microhabitat (shrubs and herbs), plant litter, and seed burial on the regeneration of Liaodong oak (Quercus wutaishanica Mayr) and Chinese pine (Pinus tabulaeformis Carr.) were studied in three typical stands (Liaodong oak forest, Chinese pine plantation, and grassland) in the Loess Plateau, China. We monitored the establishment and growth of seedlings of these two woody species in sown experimental plots, in which shrubs and herbs, plant litter, and seed burial were manipulated. In the grassland, shrubs and herbs facilitated Liaodong oak establishment, with no effect on the establishment of Chinese pine. In the two forest stands, shrubs and herbs primarily had an inhibition effect on the establishment of these trees. The effects of plant litter were facilitation or inhibition, depending on the target species and the habitat. Seed burial had a positive effect on seedling establishment. In all three habitats, shrubs and herbs had inhibition effects on seedling growth of both tree species. Plant litter and seed burial did not influence seedling growth in either species. Liaodong oak and Chinese pine use different regeneration strategies during early stages of succession and similar strategies during late stages of succession.     

Influences of stand composition and age on forest floor processes and chemistry in pure and mixed stands of Douglas-fir and paper birch in interior British Columbia

The influence of stand composition and age on forest floor chemical properties, nitrogen availability, and microbial activity was examined in mixed and pure stands of Douglas-fir (Pseudotsuga menziesii) and paper birch (Betula papyrifera). Decomposition of Douglas-fir and birch litter over two years as well as annual litter input was also measured. Mixed and pure stands of each species aged 10–25, 50–65 and >85 years old were selected in the Interior Cedar Hemlock (ICH) zone of southern interior British Columbia. Significantly more total N was mineralized in the forest floor of pure birch compare to that of pure Douglas-fir stands while forest floor of mixed species stands had intermediate N mineralization values. When sampling times were pooled forest floor N mineralization was lowest in the young stands compared to the older stands. Stand composition did not significantly affect litter decomposition were found in litter decomposition, microbial respiration and biomass. Stand age, however, did affect these parameters significantly. More birch litter mass was lost in young stands than in their older counterparts while the opposite trend was observed for fir litter. Generally, lower basal respiration, microbial biomass and C_mic/C_org was found in young compared to older stands. Concentrations and contents of forest floor total N and exchangeable K and Mg, and pH under pure birch were consistently higher compared to pure Douglas-fir. While forest floor total C, available P contents, exchangeable K and Mg concentrations were lowest in young stands, no differences were observed for total N and exchangeable Ca. All litter nutrient concentrations and contents were highest in pure birch stands. No clear trends could be discerned in litter nutrient concentration data among stand ages, although when converted to nutrient contents, there was a general increase with stand age. Both stand type and age had significant effects on forest floor properties and processes suggesting that stand age is another factor to evaluate when assessing the influence of forest composition on forest floor processes and chemistry. In terms of the effect of mixture, the data indicated that the maintenance of paper birch in mixed stands in these forest may have some effect on nutrient availability and status.     

间伐后杉木人工林生态系统养分动态的研究

将定位试验地杉木人工林间伐后,对其生态系统不同层次养分积累动态特性进行了研究．结果表明：间伐后林木各器官营养元素含量发生了变化;乔木层由于生物量的减少,养分积累量也相应减少,而灌、草及死地被物层养分积累分别增加２７２．１％,３７．２％和１６０．０％;整个杉木人工林生态系统养分的积累无论是大量元素,还是微量元素均超过对照;林下植被和死地被物层在系统养分循环中具有重要作用．     

Diversity of higher plant in broad leaved Korean pine and secondary birch forests in Liangshui Natural Reserve

INTRoDUCTIoNBroad-lcavedKoreanpincforcstisthczonalclimaxecosystcminnortl1castmountainsofChina.Itisknot"nasdivcrscsPCCicsandsPCcialindicatorinthcnortl1cmtcmPCratcforcstty'PCsofthccarth.Bccauscthiski11dofforcstllashighproductivityandlargcasscss-ment,andiscomPoscdoflnany'\1aluabIccoIl1-mercialtI-eesPCcicssucl1asI,inuskoraicnsi3,Fraxinusman'I3huricactc.IthasbecncutoverinIargcarcasduringtl1clastscveraldcc-adcsandtl1coldforcstI1asbccndamagcdscri-ousIy.Noxt'n1ostoftl1cml1a\'cbcenreplacc…     

NITROGEN NUTRIENT MECHANISM IN SECONDARY SUCCESSION PROCESS OF THE MIXED BROAD-LEAVED/ KOREAN PINE (PINUS KORAIENSIS) FOREST

INTRODUCTlONThemixcdbroad-leaved/Pinuskor`IiensiSforestwhichisoneofthemainforestsofNortheastChina,isintlleCllangbaiMountail1s(JilinProvince)a11dtheXiaoxing'anMotu1-tains(inHeilonroIangProvince).Thisistl1empicalmixcddeciduous/co11iferforestvegcta-tionofthcarca.But,duetocuttingandanunbalancebctWeenharvesti11gandanntlalin-crement,themixedbroad-leaved/PinuSko-raiensIjforestsha1,ebeenreplacedwithsec-ondaryforests(includingthelargearPaofsecondaryforestleftfrol11thepast)sinceltsclearcutti…     

白河林业局云冷杉林的植物种类组成

对白河林业局云冷杉林的植物种类组成进行了初步研究。结果表明,白河林业局云冷杉林的主要建群树种均为臭松、鱼鳞云杉,伴生树种为红松、长白落叶松,白桦,组成白河林业的种子植物和蕨类植物共计109种,分属43科88属,其中草本植物73种,灌木层植物21种,乔木植物15种。     

塞罕坝机械林场地表可燃物类型划分与载量研究

对塞罕坝机械林场8个林分类型108个林班的地表森林可燃物组成、载量、含水率等进行了调查。结果表明落叶松成林和幼林、樟子松成林和幼林、针叶混交林、桦次生林等林分地表可燃物以枯落物为主,栎次生林和灌木林地表可燃物由枯落物与灌木组成,未成林地与草地可燃物以草本植物为主;地表可燃物载量依次为落叶松成林〉落叶松幼林〉针叶混交林〉樟子松成林〉樟子松未成林〉针阔混交林〉桦次生林〉樟子松幼林〉落叶松未成林〉灌木林〉栎次生林〉草地;草地与栎次生林的含水率最低,着火点也最低,火险危险程度最高;将现有林分按燃烧类型划分为5个类型20个亚类,全场地表可燃物总载量约为2．5×10^6t。     

The interaction between organic layer and forest growth and forest development on former heathland

Heathland soils are characterized by high acidity and poor nutrient contents. Nutrient availability could then be an important factor in forest growth and development on these soils. The hypothesis to be verified was 1. The enduring change in vegetation composition and production is of great influence especially on the development of the organic layer and on the nutrient distribution between this compartment and the mineral soil, and 2. As a result, forest nutrition and water supply will change during forest growth with consequences for forest development itself. In NW Germany heathland forest development are dominated by heathlands as the initial stage of the succession, naturally established pioneering pine dominated woodlands, and oak and beech dominated forests as the terminal stages. In a comparative study, within these stages of forest succession the nutrient and water supply in the organic layer were investigated with regards to the nutrient and water supply in the mineral soil and to the morphology of the organic layer itself. The successional development was associated with an increased productivity and a marked enrichment of organic material and nutrients in the organic layer, whereas the nutrient storage in the mineral soil was unchanged. The nutrient storage in the organic layer in the forested sites amounted to up to 80% of the plant-available nutrients within the organic layer–mineral soil system. The water supply increased too due to higher water storage and increasing root penetration within the organic layer. However, the increase in water supply was less marked than the nutrient enrichment. Especially the beech-dominated broad-leaved forests depend on higher nutrient and water supply of the organic layer. They have better growth conditions in the late stages of succession, due to an intense humus accumulation by the pioneering birch–pine woodlands. Consequently, the development of the organic layer facilitates the change of coniferous woodlands to forests and woodlands dominated by broad-leaved trees. Using pine as first planted tree is recommended to support this development.     

Nitrogen nutrient mechanism in secondary succession process of the mixed broad-leaved/Korean pine (Pinus koraiensis) forest

Chemical and biochemical analysis methods were used to monitor the variations of nitrogen nutrient among the dominance trees species in secondary succession process of the mixed broad -leaved/Korean pine forest on Changbai Mountains, Northeast China. Amounts of total nitrogen, ammonium and NRA in soils of virgin broad-leaved/Korean pine forest which is in climax were higher than those ofsecondary birch forests those are in succession stage. The amount of nitrate was in the other hand. In climax, dominance trees species are tolerant mesophytic trees such asPinus Koraiensis, Tilia amurensis, Acer mono and alsoFraxinus mandshurica, they are all ammonium + nitrate adapted species, but they show a preference for the ammonium rather than those of the pioneer trees species in secondary birch forest, such asPopulus davidiava andBetula platyphylla. Because they have more ammonium in their leaves and roots, especiallyPinus koraiensis. Populus davidvana andBetula platyphlla are intolerant trees, amounts of nitrate and total nitrogen is higher in their leaves and roots and also NRA in their leaves, so they preference for the nitrate rather than the others. In secondary birch forest, the regeneration trees species adapt their nitrogen nutrient to the variation of nitrogen nutrient situation in soil, finally they could survival well and the secondary birch forest would succession to climax. In climax, dominance trees species adapt their Nitrogen nutrient to the situation in soil and there are not strong competition in nitrogen nutrient among them, so they can coexist well and keep the climax as stable vegetation.     

Temperate forest development during secondary succession: effects of soil,dominant species and management

With the increase in abandoned agricultural lands in Western Europe, knowledge on the successional pathways of newly developing forests becomes urgent. We evaluated the effect of time, soil type and dominant species type (shade tolerant or intolerant) on the development during succession of three stand attributes: above-ground biomass, stand height (HT) and stem density (SD). Additionally, we compared above-ground biomass (AGB) in natural and planted forests, using ten chronosequences (8 from the literature and 2 from this study). Both AGB and HT increased over time, whereas SD decreased. HT, SD and AGB differed among species types. For example, birch had greater HT than alder, willow and ash at a similar age and had higher SD than pine and oak at a similar age. However, birch showed lower AGB than pine. HT and AGB differed among soil types. They were higher in rich soil than in poor soils. Comparative analysis between chronosequences showed an effect of the regeneration method (natural regeneration vs plantation) on above-ground biomass. Planted sites had higher AGB than natural regeneration. Time, soil type, species and regeneration method influenced the mechanism of stand responses during secondary succession. These characteristics could be used to clarify the heterogeneity and potential productivity of such spontaneously growing temperate forest ecosystems.     

Leaf and twig litter decomposition of main species in different forests along the north slope of Changbai Mountain, northeast China

From 2001 to 2003, the litter decomposition dynamics of dominant tree species were conducted using a litterbag burying method in the broadleaf-Korean pine forest, spruce-fir forest and Ermans birch forest, which represents three altitudinal belts in Changbai Mountain, northeast China. The spatial and temporal dynamics of litter decomposition and the effects of litter properties were examined. Furthermore, the decomposition trend of different species was simulated by the Olson model, and results showed that annual mass loss rates increased over time, but was not significantly correlated. Leaf decomposition rates increased after decomposing for 638 days (1.75 years), and the order of dry weight remaining rates of leaf litter for different species is: Asian white birch (Betula platyphylla) (24.56%) < Amur linden (Tilia amurensis) (24.81%) < Korean pine (Pinus koraiensis) (38.48%) < spruce (Picea jezoensis var. microsperma) (41.15%) < Ermans birch (Betula ermanii) (41.53%) < fir (Abies nephrolepis) (42.62%). The dry weight remaining rates of twig litter was smaller than that of leaf litter, and followed the order of Amur linden (44.98%) < fir (64.62%) < Korean pine (72.07%) < spruce (73.51%) < Asian white birch (77.37%) < Ermans birch (80.35%). The simulation results by the Olson model showed that, in leaf, the 95%-decomposition rates ranged from 4.5 to 8.0 years, and annual decomposition rate (k) followed the order of Amur linden (0.686) > Asian white birch (0.624) > Korean pine (0.441) > spruce (0.406) > fir (0.397) > Ermans birch (0.385); in twig, it ranged from 7.8 to 29.3 years, and k follows the order: Amur linden (0.391) > fir (0.204) > Korean pine (0.176) > spruce (0.157) > Asian white birch (0.148) > Ermans birch (0.102). In general, the differences of decomposition rate are evident between leaf and twig litter and among species, and were higher in broad-leaved species compared with coniferous species at the same elevation, and decreased with the ascending of elevation. __________ Translated from Acta Ecologica Sinica, 2006, 26(4): 1,037–1,046 [译自: 生态学报]     

林分密度对桉树幼龄能源林的影响

对0.5年生3种不同密度配置的幼龄尾巨桉优良无性系DH32-29各器官生物量、热值以及灰分进行了调查和测定,结果表明:所选3种密度间树高差异显著,基径差异达到极显著水平,随着密度的增加,树枝、叶片、树干的生物量分别呈现减少趋势,密度与树枝和树干生物量的相关性达到了0.01极显著水平;单株生物量随密度的增大而减小,林分生物量则相反;单株热值无显著差异,仅单株平均灰分含量高密度与中密度存在显著差异。综合分析,高密度0.25 m×2 m林分生物量最大,其灰分含量比低密度的林分低,适合作为能源林培育密度。     

Influence of fire intensity on structure and composition of jack pine stands in the boreal forest of Quebec: Live trees,understory vegetation and dead wood dynamics

North American jack pine (Pinus banksiana Lamb.) stands are generally characterized by an even-aged structure resulting from high intensity fires (HIF). However, non-lethal fires of moderate intensity (MIF), which leave behind surviving trees, have also been reported. The objectives of this study were two-fold: (1) assess the concurrent dynamics of live trees, understory vegetation and different types of coarse woody debris (CWD) during succession after HIF; and (2) document how MIF affects stand structure component dynamics compared to HIF. Stands affected by both HIF and MIF were selected. Tree characteristics and age structure, understory biomass, and CWD volume were assessed. Our results suggest that the structural succession of jack pine stands following HIF comprises three stages: young stands (<48 years), premature and mature stands (58–100 years) and old stands (>118 years). Canopy openness and jack pine density significantly decreased with time since HIF, while black spruce density and CWD volume significantly increased. The highest structural diversity was measured in the premature and mature stands. Compared to HIF, MIF increased mean jack pine basal area, decreased average stand density, delayed the replacement of jack pine by black spruce replacement in the canopy, decreased CWD volume, and significantly increased bryophytes mass. MIF increased the diversity of live trees and generally decreased CWD structural diversity. The study confirms the diversity of natural disturbance magnitude and successional processes thereby initiated. Thereafter, it appeared to be relevant for adjustment of disturbance emulating forest-management systems.     

Changes in aboveground and belowground properties during secondary natural succession of a cool-temperate forest in Japan

Forest development in temperate regions is considered to be a global carbon sink. Many studies have examined forest development after harvesting or fire from aboveground (e.g., biomass) or belowground (e.g., soil nutrient) perspectives. However, few studies have explored forest development from both perspectives simultaneously in cool-temperate forests in Japan. In this study, we examined changes over 105 years in both aboveground and belowground components during secondary natural succession. The aboveground biomass increased for 50 years and reached a plateau in a 105-year-old stand. The N mineralization rate increased during succession for 50 years, but showed a decline in the 105-year-old stand due to the decrease in the nitrification rate in late succession. The percent nitrification (i.e., relative contribution of nitrification to N mineralization) decreased significantly with increasing forest stand age. The N mineralization rates had significant relationships with N concentrations of the dominant tree foliage and litter fall and with the amount of litter fall N. Meanwhile, other belowground properties (i.e., soil pH, phenol concentration, soil microbial respiration, and litter mass loss) did not show any significant relationship with forest stand age. This may be because the soil at the study sites was heterogeneous and consisted of Cambisols and Andosols, the latter of which originally has high organic matter content, and thus may have buffered the effect of the aboveground development. These results indicate that belowground N dynamics are more closely associated with aboveground development than other belowground properties in these forests.     

The chemical composition of needle and leaf litter from Scots pine, Norway spruce and white birch in Scandinavian forests

Needle litter from 14 stands of Scots pine (Pinus silvestris,L.), 13 stands of Norway spruce (Picea abies (L.) Karst.) andleaf litter from three stands of white birch (Betula pubescensEhrh.) were analysed for chemical composition. The concentrationsof the elements N, P, K, Ca, Mg and Mn as well as solid organiccomponents (lignin, cellulose and hemicelluloses) and solubleswere determined. When the average chemical compositions werecompared the Scots pine needle litter was clearly the most nutrient-poorlitter type. Of the solid organic-chemical components the ligninfraction dominated in the spruce and birch litter whereas thecellulose dominated in the pine needle litter. When Norway spruce and Scots pine were growing in adjacent standson soils with the same bedrock origin the spruce litter hadsignificantly higher concentrations of nutrients (N, P, K, Ca,Mg, Mn) than the pine needle litter. At sites where Norway spruceand white birch were growing in adjacent stands, the birch leaflitter had generally higher concentrations of nutrients. However, significant or nearly significant differences were onlyobtained for Mg (P = 0.002), K (P = 0.056) and N (P = 0.087),probably due to the few replicates of stands compared. Concerningorganic chemical components, the spruce needle litter had significantlyhigher concentrations of lignin and mannan than all the otherlitters and lower levels of ethanol-soluble substances, celluloseand galactan than the pine needle litter. Further, it had lowerconcentrations of water solubles, rhamnan and xylan than thebirch litter. No relationships were established between the nutrient statusof the conifer litters and the site index H100 (the dominantheight of the trees at a reference age of 100 years) of thestands. Concentrations of solid carbohydrates in the litterswere, however, positively correlated with site index (P <0.001). Further, the concentration of nitrogen in the pine needlelitter was negatively correlated with the latitude of the sites(P < 0.01). The influence of litter chemistry on the decompositionof litter and nutrient cycling of forests is discussed.     

FDA‐active fungal mycelium and lignin concentrations in some needle and leaf litter types

The concentration of live fungal biomass (FDA mycelium) was investigated in seven chemically very different litter types, i.e. grey alder leaves, green and brown leaves of white birch, green and brown needles of both Scots pine and lodgepole pine. Concentration of FDA mycelium in the litters changed with the season, being low during the dry late summer and relatively higher during the more rainy, wet autumn. During autumns, when moisture was not limiting, lignin concentration and live fungal biomass were negatively related. It was concluded that the concentration of live fungal biomass in litter decreased linearly as the lignin concentration increased and thus also decreased linearly to decomposition level of the litter.