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小兴安岭落叶松沼泽林土壤CO2,N2O和CH4的排放规律 总被引:1,自引:0,他引:1
采用静态箱-气相色谱法,研究小兴安岭兴安落叶松-油桦-修氏苔草沼泽林、兴安落叶松-油桦-笃斯越橘-藓类沼泽林和兴安落叶松-狭叶杜香-中位泥炭藓沼泽林生长季节土壤温室气体(CO2,N2O和CH4)排放通量的季节变化规律、季节排放量及其主控因素.结果表明:1)3种落叶松沼泽林土壤CO:排放通量均呈现夏季高(651.4~823.6 mg·m-2h-1)春秋季低(233.3~310.0 mg·m-2h-1)的单峰型季节变化,N2O排放通量(0.010~0.049,0.012~0.020和0.010~0.080 mg·m-2h-1)分别呈现夏季>春季>秋季,春季>夏季>秋季和秋季>春季>夏季的变化规律,CH4排放通量(-0.083~0.037,-0.122~0.078和-0.05~0.026 mg·m-2h-1)分别呈现春秋季排放、夏季吸收,春季排放、夏秋季吸收和春夏季排放、秋季吸收的交替式季节变化;2)表层土壤(0~30cm)温度是土壤CO2排放的主要影响因素,低水位与较高表层土壤温度是N2O排放的主要影响因素,水位是CH.排放的主要影响因素,高水位时土壤排放CH4,低水位时土壤吸收CH4;3)3种落叶松沼泽林土壤在生长季节均为CO2排放源(20.8~25.2 t·hm-2),且夏季为强排放源、春秋季为弱排放源,3者均为N2O排放源(0.192~1.128kg·hm-2),兴安落叶松-油桦-修氏苔草沼泽林为强排放源,另2者为弱排放源,兴安落叶松-油桦-修氏苔草沼泽林和兴安落叶松-油桦-笃斯越橘-藓类沼泽林土壤为CH4强吸收汇(1.152~1.200 kg·hm-2),兴安落叶松-狭叶杜香-中位泥炭藓沼泽林土壤为CH4弱排放源(0.168 kg·hm-2);4)兴安落叶松-油桦-修氏苔草沼泽林土壤温室气体CO2排放强度最高(25.4 t·hm-2),另2者相对较低(20.8~21.2 t·hm-2),但均以CO2排放占绝对优势地位(99.63%~99.93%),N2O和CH4排放占次要地位(0.19%~0.92%和0.02%~0.10%). 相似文献
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冀北山地3种次生林枯落物和土壤水文效应研究 总被引:1,自引:0,他引:1
对冀北山地3种天然次生林枯落物持水量和土壤水分特征进行了研究。结果表明:枯落物总储量为11.750~15.59t/hm2,最大持水量为44.55~49.18t/hm2之间。枯落物有效拦蓄量为白桦山杨混交林>山杨白桦五角枫混交林>白桦棘皮桦混交林。土壤容重均值的变化范围为0.72~0.95g/cm3,总孔隙度的变动范围为55.16%~60.21%。随着土层深度的增加,土壤容重呈现增加的趋势,总孔隙度减少的趋势,从土壤容重平均值来看,白桦棘皮桦混交林>白桦山杨混交林>山杨白桦五角枫混交林,总孔隙度的均值为山杨白桦五角枫混交林>白桦山杨混交林>白桦棘皮桦混交林。3种林分林地总蓄水量山杨白桦五角枫混交林为1 239.36t/hm2,白桦山杨混交林为1 194.02t/hm2,白桦棘皮桦混交林是1 135.75t/hm2,表明山杨白桦五角枫混交林林地储水能力最强。 相似文献
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以辽东半岛地区的红松、落叶松、红松针阔混交林和灌草4种主要林地为研究对象,利用方差分析、Pearson相关性等方法进行计算与分析。结果显示:(1)土层深度与土壤容重呈正相关,与总孔隙度、毛管孔隙度呈负相关;容重、总孔隙度和毛管孔隙度范围分别在0.50~1.30 g/cm3、40%~88%、30%~80%。(2)林分土壤最大持水量、毛管持水量和田间持水量,随着土层深度增加逐渐降低,波动幅度先逐渐降低最后有所增加。不同林分持水能力不同,有林地>灌草地;落叶松林>红松林和红松针阔混交林>灌草地。(3)林分土壤最大持水量、毛管持水量、田间持水量,与土壤厚度和土壤容重呈极显著负相关,与毛管孔隙度和总孔隙度呈极显著正相关,与非毛管孔隙度差异性不显著。林分主要土壤物理性及其持水性受到林分类型和土壤深度的影响,表现出浅层和中层土壤保水持水能力强;落叶松林土壤结构质地更优,保水持水性更强。 相似文献
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以4种不同桦木组成比例的林分类型为研究对象,比较其土壤水分-物理性质,结果表明:土层深度与容重呈正相关,落桦混交林土壤容重最大(1.14g/cm~3),桦木混交林最小(1.00g/cm~3);土壤孔隙度整体规律基本一致,随土层深度增加而减小,土壤毛管孔隙度、非毛管孔隙度、土壤总孔隙度均是黑桦纯林最大,分别为45.0%、9.6%、53.6%;土壤持水量(除桦木混交林规律不明显外)整体规律基本一致,随土层深度的增加而减小,土壤毛管持水量均值桦木混交林最大(43.2%),土壤最大持水量均值黑桦纯林最大(49.3%);土壤入渗速率与时间呈幂函数关系,初渗速率和稳渗速率规律一致,均是桦木混交林最大、桦杨混交林最小。 相似文献
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为评价速生人工林的土壤环境效应,文章对比分析了海南昌江县次生林、桉树人工林和相思树人工林的土壤水分物理性质。结果表明:(1)在0~60 cm次生林土壤容重最小,其次是桉树林,相思林最大,总孔隙度、毛管孔隙度、毛管/非毛管孔隙度比值、饱和持水量、毛管持水量、田间持水量以及毛管/饱和含水量大小顺序均表现为次生林>桉树林>相思林;(2)桉树林、相思林与次生林0~60 cm土壤贮水能力相差较大;(3)3种林分间同一层土壤容重、土壤总孔隙度、毛管孔隙度、非毛管孔隙度、土壤毛管/非毛管孔隙度比值、饱和持水量、毛管持水量、田间持水量、贮水能力的方差分析结果显示,除底层达到显著差异(p<0.05)或极显著差异(p<0.01)外,其余3层均不显著,各层土壤毛管含水量/饱和含水量比值差异不显著(p>0.05);(4)3种林分土壤容重随土壤深度增大而增大,总孔隙度、毛管孔隙度、饱和持水量、毛管次生林以及田间持水量均随土层厚度增加而减少;(5)次生林的土壤容重、孔隙特征、持水性以及贮水能力随土壤深度变化,但差异均不显著(p>0.05);而桉树林和相思林的所有观测土壤物理变量... 相似文献
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火干扰对马尾松人工林土壤物理性质的影响 总被引:2,自引:0,他引:2
研究了马尾松人工林在强度、中度、轻度和无火干扰情况下林地土壤的物理性质.结果表明:轻度火干扰林地土壤中大团聚体数量增加,小团聚体和原生土粒减少,表层土壤总孔隙度、毛管孔隙度和非毛管孔隙度上升,土壤最大持水量和有效水含量增加,其保水能力增强;随着火干扰强度(中度、强度火干扰)的增大,土壤中细土减少,质地变粗,土壤中大团聚体数量减少,小团聚体和原生土粒增加,表层土壤总孔隙度、毛管孔隙度和非毛管孔隙度下降,大孔隙对火干扰更为敏感,土壤最大持水量、毛管持水量、自然含水量和有效水含量减少,其中,中度、强度火干扰林地表层土壤有效水含量较无火干扰林地土壤分别低32.4%和36.3%,其保水能力下降. 相似文献
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《中南林业科技大学学报(自然科学版)》2017,(8)
为了探明林型差异对土壤理化特征及其持水能力的影响,采集老虎岭水源涵养林区域4种最典型的林型(马尾松林、马尾松-红锥林、马尾松-红锥-椆木林、红锥-大叶栎林)土壤进行理化特征及其持水能力测定分析。结果表明:土壤毛管孔隙度、持水能力和化学性质在4种林型中存在明显的差异,其中马尾松-红锥林土壤容重最小,总孔隙度和毛管孔隙度最大,最大持水量、毛管持水量、有机质、速效氮和速效磷最多;马尾松-红锥-椆木林非毛管孔隙度最大,全氮、全磷、速效钾和代换性镁最多;红锥-大叶栎林全钾最多;马尾松林土壤容重、非毛管持水量和代换性钙最大,总孔隙度、毛管孔隙度、自然含水率、最大持水量、毛管持水量、全量和速效养分均最低。总体表现,混交林型的土壤理化特征及持蓄能力均优于马尾松纯林,尤以马尾松-红锥林型为最佳。 相似文献
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大兴安岭林区的河谷洼地、山麓缓坡地带,乃至宽缓的分水岭岭背上,都有面积不等、程度不同的沼泽地,并堆积了厚约0.5—1米的泥炭层,成为我国一个重要的泥炭沼泽区,这里的沼泽类型多样,既有富营养型的苔草、苔草——小叶樟草本沼泽,也有贫营养型的泥炭藓沼泽,还有在国内难以见到的中——贫营养型木本沼泽,即兴安落叶松——杜香——泥炭藓沼泽和丛桦——苔草沼泽。沼泽分布受地形条件严格限制,依山傍水,多呈不连续的斑块 相似文献
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8种桦树种间亲缘关系的研究 总被引:3,自引:0,他引:3
采用ISSR标记技术,对8种桦树(Betula)进行了亲缘关系的分析,17个ISSR引物共检测到236个位点,多态条带比率(PPB)在5.93%~19.92%之间,遗传分化最高的是油桦,最低的是棘皮桦。8种桦树的基因多样性(Ht)为24.38%,桦树种间变异占总变异(Gst)的79.36%。遗传距离聚类将8种桦树分为3个群,黑桦、油桦、白桦和欧洲白桦为一群;赛黑桦、枫桦和岳桦为另一群;棘皮桦单独为一群。聚类结果与传统的形态分类一致。图2表4参10。 相似文献
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IntroductionUnderstanding the distribution patterns of biomassalong environmental gradients change from swampsthrough ecotones to forests is vital not only for revealing the law of ecotoneal community structure,function and succession, but also for conserving andmanaging ecotoneal communities. Research resultsshowed that conditions stressful in other environments might increase primary production in plantsadapted to wetland ecotones. For example, Sharmaand Gopal (1977) studied biomass structu… 相似文献
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Ma KepingBeijing Forest Ecosystem Location Research Station Acadcmia SinicaZhang Yue Zhou RuichangNatural Resources Institute of Heilongjiang Province 《林业研究》1992,(1)
In this paper,the seasonal rhythms of the above grassland biomass of the two maintypes of the Calamagrostis anguslifolia graaslands,the Calamagrostis angustifolia meadow and theCalamagrostis angustifolia + carex schmiudilii swamp meadow,were reported.The simulation tech-niquc was employed to described the dynamic process.In the end,the absolute growth rate and therelative growth rate of aboveground biomass of the two communities were approached in the lightof the growth analysis method. 相似文献
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In this paper, the seasonal rhythms of the above grassland biomass of the two main types of theCalamagrostis angustifolia grasslands, theCalamagrostis angustifolia meadow and theCalamagrostis angustifolia +Carex schmiditii swamp meadow, were reported. The simulation technique was employed to described the dynamic process. In the end, the absolute
growth rate and the relative growth rate of aboveground biomass of the two communities were approached in the light of the
growth analysis method. 相似文献
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冀北山地华北落叶松、桦木林土壤水分物理性质研究 总被引:2,自引:0,他引:2
华北落叶松和桦木是冀北山区最主要的造林树种。为探讨二者的纯林或混交林对土壤水分物理性质的影响,以冀北山地华北落叶松林、落叶松白桦混交林、桦木林、黑桦林为研究对象,对其土壤水分物理性质进行比较,结果表明:土层越深,土壤容重越大,由大到小依次为华北落叶松林(1.14g/cm~3)、黑桦林(1.03g/cm~3)、落叶松白桦混交林(1.01g/cm~3)、桦木林(0.98g/cm~3),土壤总孔隙度由大到小排序为落叶松白桦混交林(53.04%)、华北落叶松林(51.84%)、桦木林(51.40%)、黑桦林(51.14%);土壤最大持水量由大到小排序为落叶松白桦混交林(55.53%)、桦木林(52.81%)、黑桦林(51.33%)、华北落叶松林(48.22%);土壤稳渗速率由大到小排序为落叶松白桦混交林、桦木林、黑桦林、华北落叶松林。营造华北落叶松和桦木混交林有利于土壤涵养水源和保持水土。 相似文献
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The structure and dynamic succession law of natural secondary forest after severe fire interference in recent 20 years were studied by adopting the method of deducing time series from the spatial sequence of vegetation in Heihe region, Heilongjiang, China. Two typical and widely distributed forest types in the study area, namely forest type A and forest type B, were selected as study subjects. Forest type A is pure broadleaf forest or broadleaf mixed forest mainly composing of superior Betula platyphylla and Populus davidiana in the area with gradient <25°, while forest type B is pure forest or mixed forest composing of superior Quercus mongolica and Betula davurica in the area with gradient >25°. Species richness, vegetation coverage, important value, and similarity index of community in different layers (Herb, shrub, small tree, and arbor layers) were investigated and analyzed for the two typical forests. The results show that after fire interference, the species richness and coverage in each layer in forest type A were higher than that in forest type B. Both for forest type A and B, with elapse of post-fire years, the species richness and coverage of herbs and shrubs showed a decline tendency, while those of arbor layer present a rising tendency. Through comparison of the important values of species in each layer and analysis of community structure changes, the dynamic process of post-fire vegetation succession for forest type A and B was separately determined. Post-fire 80 years' succession tendency of forest type A is B. platyphylla and Larix gmelinii mixed forest. Its shrub layer is mainly composed of Corylus heterophylla and Vaccinium uliginosum, and herb layer is dominated by Carex tristachya, Athyrium multidentatum, and Pyrola incarnate; whereas, the post-fire 80 years' succession of forest type B is Q. mongolica and B. davurica mixed forest. Its shrub layer is mainly composed of lespedeza bicolar and corylus heterophylla and herb layer is dominated by Carex tristachya, Asparagus densiflorus, and Hemerocallis minor. 相似文献