Influence of forest growth on former heathland on nutrient input and its consequences for nutrition and management of heath and forest

The low nutrient supply of heathland soils is often insufficient for the nutrient demand of growing forests and woodlands, and additional atmospheric input of nutrients is beneficial for the tree growth. On old heathland soils tree species influencing nutrient input with regard to higher amounts have competitive benefits on the early stages of succession and/or as first planted trees with consequences for both the successional development and the nutrition and management of heathland and forests. In three stages of heathland forest succession on highly acidified and nutrient poor soil, the influence of the canopies of a Calluna heathland, a pioneering birch-pine woodland, and a terminal oak-beech forest on nutrient input was investigated. Of all investigated species Scots pine has the highest interception of water and nutrients (N, K, Ca, Mg). As a consequence, the nutrient input into the pioneering birch-pine forest is the highest of the three types of ecosystems. This ability to meliorate the nutrient supply by increasing the nutrient input favours pine in the early stages of the succession. The enhanced nutrient input and accumulation within the young successional forest ecosystems involves two different succession and/or management considerations depending upon the further ecosystem development.

• 1.The increasing nutrient availability mitigates the negative influence of the highly acidified nutrient poor soil on the growth of oak and beech and facilitates the conversion of pine dominated woodlands and forests into forests dominated by broadleaved species.
• 2.For regeneration of heathland from naturally established pine woodlands and forests, deforestation have to be combined with techniques of nutrient impoverishment of the soil.

     

基于灰色关联分析的思茅松林下枯落物与土壤有机质含量的关系研究

设计6个大样区,27个样地,7个因子(有机质、朽木、松针、松枝、松果、阔叶、腐殖质)进行调查采样,采用灰色系统理论的灰色关联分析法对景谷县思茅松林下枯落物与土壤有机质含量的关系进行分析研究.结果表明,景谷县思茅松林下松针、松果、朽木对林下土壤中有机质的含量影响最大,其次是松枝、腐殖质层、阔叶.     

Soil phosphorus fractions and their availability over natural succession from clear-cut of a mixed broadleaved and Korean pine forest in northeast ChinaOA

To assess phosphorus(P) status of forest soil under naturally restored vegetation, P fractions in the 10-cm soil layer were quantified at different successional stages on the clear-cut site of mixed broadleaved and Korean pine forest. Four communities of shrub, softwood broad-leaved forest, softwood and hardwood broad-leaved forest, and hardwood broad-leaved forest represented different successional stages. A soil sample from a primary broad-leaved and Korean pine stand was the control. A sequen...     

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。     

Looking deeper: An investigation of soil carbon losses following harvesting from a managed northeastern red spruce (Picea rubens Sarg.) forest chronosequence

Forest harvesting in eastern North America has been occurring for centuries but its effect on soil carbon storage and dynamics below 20 cm is not well known. This paper investigates age-related variations in carbon storage and dynamics in the organic layer and 6 depth strata in the top 50 cm of the mineral soil during ecologically important stages of post-harvest succession in a first rotation red spruce forest chronosequence that includes one of the largest old growth reference stands in northeastern North America. Storage of carbon reached a minimum 32 years post-harvest, at which time stores were approximately 50% of the intact forest. However, storage approached the range of the intact forest approximately 100 years post-harvest. Examination of age-related variations with depth revealed that concentrations of carbon below 20 cm may be driving the temporal trends in whole soil storage in these forests. Corresponding carbon isotope data were consistent with increased isotopic fractionation attributable to increased rates of mineralization post-harvest. Based on these results, we suggest that a greater emphasis should be placed upon examining storage of carbon below 20 cm in the mineral soil when evaluating the sequestration potential of intensive forest management, specifically rotation length.     

Recovery of species diversity after disturbance of broad-leaved Korean pine mixed forest in Changbai Mountain

IntroductionMorerecently,Thehumanl1asshowedagreatinterestli1studiesonpatternsofchangesinspeciesdiversityduriI1gprocessofsuccession,ThedistuIbal1ceofI1umanactivitiesornaturedisastershasagreatbopactonspeciesdiversity.PlantsPeciescomprisingapost-disturbancecommunityderhefromavarietyofsources-winddispersedseed,buriedpropagulesandresproutingsurvivorsl1'l.TheirulthatecontributiontotheserialflorarenectSacomplexinteractionofinitialabundance,includingdistuthanceintCnsity,proPagatCavailability,andc…     

土壤温度和水分对长白山3种温带森林土壤呼吸的影响

为了研究土壤温度和土壤含水量对阔叶红松林(山地暗棕壤)、云冷杉暗针叶林(山地棕针叶林土壤)和岳桦林(生草森林土)的土壤呼吸的影响,于2001年9月在长白山进行了土壤实验。利用增加土壤样柱的含水量,将土壤含水量分为9%,、21%、30%、37%和43%5个等级,土壤样品分别在0、5、15、25和35的温度下保持24小时。阔叶红松林土壤在0~35范围内,土壤呼吸速率与温度呈正相关。在一定的含水量范围内(21%~37%),土壤呼吸随含水量的增加而升高,当含水量超出该范围,土壤呼吸速率则随含水量的变化而降低。土壤温度和水分对土壤呼吸作用存在明显的交互作用。不同森林类型土壤呼吸作用强弱存在显著差异,大小顺序为阔叶红松林>岳桦林>云冷杉暗针叶林.红松阔叶林土壤呼吸作用的最佳条件是土壤温度35,含水量37%;云冷杉暗针叶林下的山地棕色针叶土壤呼吸作用的最佳条件是25,21%;岳桦林土壤呼吸作用的最佳条件是35,含水量37%。但是,由于长白山阔叶红松林,云冷杉林和岳桦林处在不同的海拔带上,同期不同森林类型土壤温度各不相同,相差4~5,所以野外所测的同期的山地棕色针叶林土呼吸速率应低于暗棕色森林土呼吸速率,山地生草森林土呼吸速率应高于山地棕色针叶林土的呼吸速率。图2表1参25。     

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.     

湖南省阔叶林生态系统碳储量及其分布

根据2017年湖南省森林资源清查资料和野外实地调查实测数据,对湖南省阔叶林生态系统碳储量、碳密度的动态特征进行了研究。结果表明:湖南省阔叶林森林生态系统总碳贮量为505.17 TgC,其中乔木层、灌草层、枯落物和土壤层层分别为113.75 TgC、9.92 TgC、9.64 TgC和377.86 TgC,分别占阔叶林生态系统碳贮量的22.52%、1.96%、1.91%和73.61%;湖南省阔叶林森林生态系统碳密度为154.51 t·hm^2,各层碳密度的大小顺序为土壤层(113.74 t·hm^-2)>乔木层(34.79 t·hm^-2)>灌草层(3.03 t·hm^-2)>枯落物层(2.95 t·hm^-2)。在3种类型阔叶林中,乡土阔叶林生态系统碳贮量为485.56 TgC,所占全省阔叶林生态系统碳贮量的96.12%;乡土阔叶林生态系统碳密度最大,为154.72 t·hm^-2,杨树林生态系统碳密度最小,为149.59 t·hm^-2。在阔叶林各龄组中,中、幼龄林约占湖南省阔叶林生态系统碳贮量的67.13%,是阔叶林的主要碳库且固碳潜力巨大;湖南省阔叶林碳密度幼龄林、中龄林、近熟林和成过熟林的碳密度分别介于24.60～55.51 t·hm^-2之间,具体表现为成过熟林(55.51 t·hm^-2)>近熟林(47.51 t·hm^-2)>中龄林(44.68 t·hm^-2)>幼龄林(24.60 t·hm^-2)。全省阔叶林生态系统空间分布表现为碳贮量呈现明显的湘西、湘南,湘中较低特征,而碳密度整体表现出洞庭湖流域地区大于其他地区的趋势。     

不同森林植被下土壤微生物量碳和易氧化态碳的比较

土壤碳库平衡是土壤肥力保持的重要内容[1].不同森林类型,由于其凋落物数量、类组及分解行为不同,因而形成的土壤碳库大小与特征将存在较大差别.常绿阔叶林、马尾松(Pinus massoniana Lamp.)林、杉木(Cunninghamia lanceolata (Lamb.)Hook.)林和毛竹(Phyllostachys edulis(Carr.)H.de Lehaie)林是我国亚热带最主要的4种森林类型.     

辽东山区原始红松混交林土壤有机碳及其影响因素研究

以辽东山区原始红松混交林为研究对象,对比分析了不同树种组成下原始红松混交林土壤有机碳含量的差异,研究了土壤有机碳与土壤属性因子和植被覆盖因子的相关关系,并研究了土壤碳密度的分布规律。结果显示,3种原始红松混交林土壤有机碳含量均随着剖面深度的增加而降低;0~10 cm土层深度土壤有机碳含量为红松阔叶林阔叶红松林针阔混交林,表层土壤有机碳主要来源于枯落物层的分解,表层土壤有机碳的特征表明原始红松混交林树种构成不同,潜在地影响着生态系统内的碳循环。对土壤属性因子而言,碳氮比与有机碳含量呈极显著的正相关关系,而容重、pH值呈显著的负相关关系;对植被覆盖因子而言,枯落物有机碳、全氮、碳氮比与土壤有机碳含量则无相关关系;0~100 cm深度内红松阔叶林的土壤碳密度最大,为181.4 t/hm2,针阔混交林次之,为180.56 t/hm2,阔叶红松林最小,为150.78 t/hm2,且接近70%的土壤碳储存集中在40 cm以上的土层内。旨在为揭示原始红松混交林对土壤有机碳的影响因素和探索我国原始红松混交林土壤碳分布格局提供科学依据。     

江西金盆山林区天然常绿阔叶林生态系统碳储量研究

【目的】探讨亚热带典型天然常绿阔叶林碳储量及其碳分布格局,以期为常绿阔叶林生态系统碳汇功能评价提供基础数据和理论依据。【方法】以江西省金盆山林区优势树种生态系统生物量研究为基础,结合主要优势树种碳含量实测数据,对金盆山典型常绿阔叶林丝栗栲林、南岭栲林、米槠林的碳储量及碳空间分布格局进行研究,并以这3种林分的碳密度均值计算整个金盆山林区天然常绿阔叶林总碳储量。【结果】金盆山林区丝栗栲林、南岭栲林、米槠林生态系统碳密度分别为294.82、307.63、318.97 t/hm^2,林区生态系统总碳密度为307.14 t/hm^2,林区现存碳总量为2.25×10^6 t;生态系统碳密度分布规律为植被层>土壤层>凋落物层,植被层碳密度分布规律为乔木层>灌木层>草本层,其中乔木层主干的碳密度占56.54%;土壤层碳密度随着土壤层的加深呈下降趋势,40 cm以下土层间的碳密度变化不明显。【结论】金盆山林区常绿阔叶林不同林分间生态系统碳密度差异不显著,生态系统内碳密度有较强的空间分布规律,生态系统碳密度高于我国森林生态系统平均碳密度和多种典型森林类型碳密度,具有较强的碳汇功能。     

林口林区次生林植苗改培技术初探

针对黑龙江省林口林区天然次生林较差的林分状况,该地区选择红松和红皮云杉作为主要树种进行改造、更新.文中通过对改培样地的调查,介绍了在不同光照、坡度、坡位条件下,改培树种的生长状况,从而提出较好的改造方案和措施.     

热带次生林经营研究文献分析

热带次生林面积巨大且在热带森林资源中的作用越来越重要,因而拥有巨大的经营潜力和生态功能。次生林演替过程中的主要研究成果如下：土壤贮存的种子对次生林的再生非常重要,光投射的强度增加和温度提高将刺激种子萌芽,而残余植被群落强烈影响次生林种子的散布,食种子动物影响次生林的成林;次生林群落植物种类数量一般随演替的进程而增加;随着演替的进程,次生林内阳生树种趋于衰亡,耐荫树种不断增加;次生林的树种数量能接近原生林水平的时间过程更随着林分种类、过去土地的利用强度和利用种类,以及环境条件的不同而异;在一定环境中,人工林树种通过人工林树种改变光、温度和土壤表层的湿度,能够促进发芽和种子生长,改善林地和林下植被的状况,从而加速次生林演替。大多数食草动物喜欢在次生林中取食,因为次生林中先锋树种很少或没有机械和化学保护,且林内许多树种产生大量可食用的果实;环境和火对次生林演替有一定影响;在早期的演替过程中,更多的生物量分配到资源需求旺盛的组织（如叶和细根）,在演替晚期阶段,更多的生物量则分配到结构组织中（如木质部和根端）。次生林在15至20年内能迅速积累生物量,然后积累逐渐减慢;次生林被砍伐或火烧后,森林土壤的结构被破坏,导致土壤有机质和氮减少。     

Active organic carbon pool of coniferous and broad-leaved forest soils in the mountainous areas of Beijing

In order to explore the effects of different forest types on active soil carbon pool, the amounts and density of soil organic carbon (SOC) were studied at different soil horizons under typical coniferous and broad-leaved forests in the mountainous area of Beijing. The results showed that the amount of total SOC, readily oxidizable carbon and particulate organic carbon decreased with increasing depths of soil horizons and the amounts at depths of 0–10 cm and 10–20 cm in broad-leaved forest was clearly higher than that in coniferous forests. The trend of a decrease in SOC density with increasing depth of the soil horizon was similar to that of the amount of SOC. However, no regular trend was found for SOC density at different depths between coniferous forest and broad-leaved forests. The ratio of readily oxidizable carbon to total amount of SOC ranged from 0.36–0.45 and the ratio of particulate organic carbon to total amount of SOC from 0.28–0.73; the ratios decreased with increasing depths of soil horizons. Active SOC was significantly correlated with total SOC; the relationship between readily oxidizable carbon and particulate organic carbon was significant. A broad-leaved forest may produce more SOC than a coniferous forest.     

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…     

Improved recruitment and early growth of Scots pine (Pinus sylvestris L.) seedlings after fire and soil scarification

The success of seedling recruitment of Scots pine (Pinus sylvestris L.) is strongly dependent on soil surface properties, such as humus depth and moisture content. In an undisturbed forest floor, seedlings are seldom able to become established due to the high incidence of desiccation in the organic soil layer. Methods that remove the organic soil layer are often necessary to improve the availability for radicles to reach the more stable moisture regime in the mineral soil. In this study we investigated pine-seedling establishment after mechanical soil scarification, burning of litter (O_L) and burning of litter and humus (O_L and O_FH) in two mature pine stands in Germany. The herbaceous layer of the first stand was dominated by grasses (Molinia caerulea L. and Deschampsia flexuosa L.), whereas the herbaceous layer of the second stand was dominated by blueberry (Vaccinium myrtillus L.). Pine seeds were placed in experimental plots, and seedling numbers and heights were recorded at regular intervals. All treatments that removed organic soil resulted in higher seedling counts than did the undisturbed forest floor. The highest seedling counts were found on scarified and severely burnt plots, whereas seedling counts were lower on lightly burnt plots. Seedlings were significantly taller on burnt plots. This study shows that pine regeneration is stimulated by fire, not only in boreal forests, but also under central European conditions. With the expectation of higher fire frequency in the near future due to climatic changes, natural regeneration and succession on burnt sites should receive more focus in forest management and research.     

The ecology of tree regeneration in mature and old forests: combined knowledge for sustainable forest management

We focused our attention on quantifying the factor complex of forest regeneration in 423 mature and old stands with contrasting environmental conditions. We recorded the microhabitat selection of tree recruits, the frequency of tree seedlings, and evaluated the drivers of sapling abundance and diversity. The majority of forest regeneration was established on undisturbed forest floor. Dead wood was a frequent substrate in spruce-(co)dominated forests. Seedling frequency within a stand was related to the site-type specific productivity gradient of stands—pine seedlings were common in low-productivity and spruce in high-productivity boreal forests. Seedlings of temperate broad-leaved trees dominated in productive boreonemoral forests, except for oak, which showed a uniform distribution of abundance in all forest site-types. Sapling abundance was dictated by forest site-type, and facilitated by stand diversity, variability in stand closure, lying dead wood, abundant moss, and a thick organic layer. Only in boreal forests was sapling abundance suppressed by the abundant spruce and younger trees. Upon considering the relationship between sapling abundance and species richness, sapling diversity was dependent on forest site-type, suppressed by stand density and dead wood (old gap) abundance, and facilitated by stand diversity. In addition, boreonemoral stands, competition from herbs, and facilitation by mosses occurred. The observed pattern of tree recruitment points to the importance of top-down effects of the overstory, competing or facilitating interactions with forest floor vegetation, and availability of regeneration microhabitats, which in complex make their ecology comparable with forest herbs. Natural forest regeneration can be enhanced if silvicultural methods support mixed stands and enhance field layer diversity. Oak can provide the universal tree species to improve stand structure over a wide range of habitats.     

A succession and silviculture model for the broad-leaved Korean pine forests of Changbai Mountain Area

IntroductionGaPSinforestSwereoftenfomledduetobigtreesfalldown.Regenerationandgrowtl1inthegapsincreasebe-causeofIheAnprovementoflightcondition-Thegapwillbefilledwithnewregeneratedtrees.Wattnamedtl1isforesIdynamicsastheforestgrowtllcycle.SinceD.Bot-kindevelopedthefirstGapmo`Iel(JANOWAnlodel)basedontheforestgrowthcycletheory,dleresearchongapmodelbecameoneofthemostactivedirectio11slilecologybecauseofJANoWAnlodeI'ssuccess.H.Sl1ug-artandhisstUdentSmadegreatc()ntributio11stogapmodeI'sdeve…     

Root biomass and underground C and N storage of the primitive Korean pine and broad-leaved forest and its different succession stages in Changbai Mountain, northeast China

This paper studied root biomass and underground carbon (C) and nitrogen (N) storage of a more than 200-year-old primitive Korean pine and broad-leaved forest and its two 20-and 80-year-old secondary Populus davidiana and Betula platyphylla forests in Changbai Mountain, northeast China. The results showed that with forest succession, the root biomass of 20-year-old, 80-year-old, and primitive forests was 2.437, 2.742, and 4.114 kg/m², respectively. The root C storage was 1.113, 1.323, and 2.023 kg/m², soil C storage was 11.911, 11.943, and 12.587 kg/m², and underground C storage was 13.024, 13.266, and 14.610 kg/m², respectively, while the root N storage was 0.035, 0.032, and 0.038 kg/m², soil N storage was 1.208, 1.222, and 0.915 kg/m², and underground N storage was 1.243, 1.254, and 0.955 kg/m², respectively, which indicated that along with forest succession, the forest underground became a potential “carbon sink,” whereas underground N storage did not change obviously. __________ Translated from Chinese Journal of Applied Ecology, 2005, 16(7): 1,195–1,199 [译自: 应用生态学报, 2005, 16(7): 1,195–1,199]