黄土高原多年生草本物种根部导水结构及空间分异特征

植物茎干导水系统起着植株水分长距离输导功能,深入了解植物导水解剖结构和功能对于认识植物水分、养分输导和分配策略具有重要意义,然而相关研究还是主要集中在木本乔、灌木物种上,而对于多年生草本物种的相关研究还未引起人们的重视。以黄土高原多年生草本物种为研究对象,在黄土高原沿降雨梯度(250—530 mm)布设12个采样点,采集了30种多年生草本物种的主根解剖材料,并分析了该地区草本物种根部导管解剖结构及空间分异特征。研究结果表明1)多年生草本物种根部导管特征参量具有较大的变异性,在固定测量范围内导管数量、导管直径、导管分数、总水分传导效率的变化范围分别为25—295个、24.46—54.58μm、2.42%—33.16%、0.034—25.357 kg m~(-1) MPa~(-1) s~(-1)。2)多年生草本根部导管直径、导管分数和导水效率均沿降雨量的增加呈不断下降趋势,其中以导水效率下降趋势最为明显(R=-0.3—-0.362,P0.05),这表明水分条件是限制黄土高原草本物种根部导水特征空间变异的主要因素。3)多年生草本根部导管直径和导水效率以半荒漠分布为主的蒺藜科草本物种中数值最高,其次是人工种植为主的豆科草本物种,而以自然分布为主的菊科草本物种的导管参量数值最低,这表明黄土高原不同类群草本物种的导水特征和输水策略存在较大差异性。     

黄土高原北部草地的恢复与重建对土壤有机碳的影响

草地的恢复与重建是黄土高原生态建设的重要内容,探讨草地恢复过程中土壤有机碳密度（SOCD）的变化规律对于合理评价北方水蚀风蚀交错带地区生态恢复的环境效应及其对土壤碳固存潜力的影响具有重要的理论价值。以黄土高原北部水蚀风蚀交错带地区不同生长年限的紫花苜蓿（Medicago sativa）人工草地及其退化后形成的次生草地为主要研究对象,探讨了SOCD的动态变化特征。结果表明,研究区0-100cm土体的SOCD普遍较低,变化范围为1.18-2.81kgCm^-2,略高于地球上荒漠带的水平（1.4kgCm^-2）,显著低于黄土高原中部（4.46-9.95kgCm^-2）与全国（11.52-12.04kgCm^-2）的平均水平。但是当土地利用方式由农田转变为人工草地以后,以及随着人工草地向长芒草（Stipabungeana）次生天然草地的自然演替,SOCD均有不同程度的增加,增加幅度最大可达72%,土壤表现为明显的碳汇。不同土地利用方式0-100cmSOCD的变化顺序为：灌木林地（2.11kgCm^-2）〉次生天然草地（1.95kgCm^-2）〉人工草地（1.91kgCm^-2）〉弃耕地（1.69kgCm^-2）〉农田（1.68kgCm^-2）,但统计差异不显著,意味着植被恢复对土壤碳固存的影响相对较小,该地区土壤固存CO2的潜力并不大,发育较好的次生天然草地0-100cm土体SOCD平均仅为2.20kgCm^-2。对SOCD垂直变化的分析结果表明表层SOC主要固存于表层0-20cm土壤,而且与0-100cm土体的SOCD具有显著的线性相关性,由表层观测值可以有效估计0-100cm土体的SOCD,估计误差为9.9%（0.18kgCm^-2）。     

Dynamics of species richness and composition in a limestone grassland restored after tree cutting

Abstract. After abandonment many limestone grasslands have been overgrown by trees and shrubs; as a result, species-rich communities with many regionally rare and endangered species are vanishing. Some studies suggest that, in cases where grassland is being restored, the species composition and rate of change is strongly dependent on the initial conditions, i.e. the earlier presence of grassland species and the opportunity for colonization of new sites by grassland species. These hypotheses were tested in a five-year restoration experiment after the clearing of a 35-yr-old secondary pine wood developed on abandoned grassland. Tree cutting induced rapid changes in the floristic composition and species cover. The number of grassland species from the class Festuco-Brometea increased significantly in the restored grassland, but their cover was much lower than in the old grassland. Canonical Correspondence Analysis showed significant differences in species composition between the grassland restored in former wood gaps and that developed in former closed wood. In wood gap sites the cover of species from the class Molinio-Arrhenatheretea and tufted perennials was much higher, whereas the cover of Festuco-Brometea species was lower. Significantly more shrubs, woodland species, ruderal and nitrophilous species as well as annual and biennial species occurred in the former closed wood site. It was found that richness and composition of the restored grassland depended strongly on the community composition before tree cutting, as well as on the presence of grassland species in the neighbourhood. Periodical tree cutting enables the maintenance of a temporal-spatial mosaic of scrub-grassland communities in isolated habitats and the preservation of local species diversity.     

松嫩草地66种草本植物叶片性状特征

植物叶片功能性状及其相互关系越来越受到关注.以松嫩草地66种草本植物为研究对象,测量叶片干物质含量、比叶面积、叶片厚度、叶片氮含量、叶片磷含量、叶绿素含量和类胡萝卜素含量,检验性状间的相互关系,比较不同功能群(多年生根茎禾草,多年生丛生禾草,多年生杂类草,1年生或2年生草本)间性状的差异性.结果表明,叶片厚度变异系数最大,比叶面积、叶片氮含量、叶片磷含量、叶绿素含量和类胡萝卜素含量之间存在显著的正相关关系;叶片于物质含量与叶片磷含量没有显著的相关关系,与其它叶片性状呈显著的负相关关系;叶片厚度只与叶片干物质含量和比叶面积呈显著的负相关关系,与其它叶片性状不相关.叶片干物质含量、比叶面积、叶片厚度、叶片氮、磷含量在4个功能群间差异显著,叶绿素含量和类胡萝卜素含量在各个功能群间差异不显著;多年生根茎禾草和多年生丛生禾草叶片的7个性状差异不显著;多年生根茎禾草和多年生丛生禾草的叶片干物质含量高于多年生杂类草和1年生或2年生草本,其它性状小于这两个功能群.     

黄土高原腹地人工林下草本层群落构建机制

群落构建机制是生态学研究的核心论题。生态位理论和中性理论是阐明群落构建的两种主要理论, 但这两种理论分别强调的环境过滤和扩散限制对群落构建的影响尚存争议。该研究以黄土高原人工林下草本层群落为研究对象, 将群落物种组成数据与地理空间、气候、地形以及生物因子相结合, 运用随机森林模型(RF)和基于距离矩阵的多元回归方法(MRM), 探究了各个因子的重要性, 并通过邻体主坐标矩阵(PCNM)和基于距离的冗余分析(db-RDA)分别筛选显著的空间结构和环境因子, 最后结合筛选出的PCNM特征值和环境变量进行变差分解。研究结果显示: 1)林下草本层群落组成相似性随地理距离和生境差异的增加而减小。2)地理距离与生境差异共同解释了群落组成相似性变化的47.8%。其中, 空间因子和环境因子的独立解释率分别为14.1%和9.8%, 两者的联合解释率为23.9%。3)地理距离和年降水量是引起研究区内物种组成变化的关键因子, 且地理距离的重要性大于年降水量。在黄土高原腹地, 扩散限制与环境过滤共同主导了人工林下草本层群落的构建过程。     

黄土高原典型草原地上生物量估测模型

为了寻求有效的草地地上生物量估测方法和精确估测黄土高原典型草原草原地上生物量。于2014年8月中旬,在黄土高原典型草原草原地上生物量达到最大值,分别从单株水平和种群水平进行野外调查。以株高(H)和盖度(C)的复合因子(C×H)为自变量,通过回归分析,建立地上生物量估测模型,采用留一法对其精确性进行评估;并通过校正系数以及群落总生物量估测值和实测值比较单株水平和种群水平所建模型的精确性。结果表明:黄土高原典型草原草地,无论在单株水平还是种群水平,线性和幂函数对该区域生物量的拟合效果更好。估测模型检验结果表明,在单株水平各个物种的生物量估测值与实测值相关性较好,均达到了显著水平(P0.05),其r值均大于0.6,总相对误差RS均小于10%,平均相对误差绝对值RMA(average absolute value of relative error)均小于30%,总生物量的实测值与估测值比较接近,校正系数均接近1;而在种群水平上,虽然各物种的生物量估测值与实测值相关性均达到了显著水平(P0.05),但多数物种平均相对误差绝对值RMA大于30%,总相对误差RS(total relative error)均大于10%,总生物量的估测值均大于实测值,校正系数均偏离了1,说明在黄土高原典型草原通过单株水平建立的物种生物量估测模型的精度优于种群水平建立的物种生物量估测模型的精度。     

Comparing the effect of naturally restored forest and grassland on carbon sequestration and its vertical distribution in the Chinese Loess Plateau

Vegetation restoration has been conducted in the Chinese Loess Plateau (CLP) since the 1950s, and large areas of farmland have been converted to forest and grassland, which largely results in SOC change. However, there has been little comparative research on SOC sequestration and distribution between secondary forest and restored grassland. Therefore, we selected typical secondary forest (SF-1 and SF-2) and restored grassland (RG-1 and RG-2) sites and determined the SOC storage. Moreover, to illustrate the factors resulting in possible variance in SOC sequestration, we measured the soil δ(13)C value. The average SOC content was 6.8, 9.9, 17.9 and 20.4 g kg(-1) at sites SF-1, SF-2, RG-1 and RG-2, respectively. Compared with 0-100 cm depth, the percentage of SOC content in the top 20 cm was 55.1%, 55.3%, 23.1%, and 30.6% at sites SF-1, SF-2, RG-1 and RG-2, suggesting a higher SOC content in shallow layers in secondary forest and in deeper layers in restored grassland. The variation of soil δ(13)C values with depth in this study might be attributed to the mixing of new and old carbon and kinetic fractionation during the decomposition of SOM by microbes, whereas the impact of the Suess effect (the decline of (13)C atmospheric CO(2) values with the burning of fossil fuel since the Industrial Revolution) was minimal. The soil δ(13)C value increased sharply in the top 20 cm, which then increased slightly in deeper layers in secondary forest, indicating a main carbon source of surface litter. However the soil δ(13)C values exhibited slow increases in the whole profile in the restored grasslands, suggesting that the contribution of roots to soil carbon in deeper layers played an important role. We suggest that naturally restored grassland would be a more effective vegetation type for SOC sequestration due to higher carbon input from roots in the CLP.     

Litter standing crop of shrubland ecosystems in southern China

Aims Litter is an important component of terrestrial ecosystems, which plays significant roles in carbon and nutrient cycles. Quantifying regional-scale pattern of litter standing crop would improve our understanding in the mechanism of the terrestrial ecosystem carbon cycle, also with help in predicting the responses of carbon cycle of terrestrial ecosystems to future climate change. Our objective was to examine variation in litter standing crop of shrublands along the environmental gradients in southern China.
Methods During 2011-2014, we investigated the litter standing crop at 453 shrublands sites by the stratified random sampling, reflecting climatic and soil attributes across southern China.
Important findings We found that the mean value of litter standing crop in these shrubland ecosystems across southern China was 0.32 kg·m^-2. It was 68% of forest litter standing crop (0.47 kg·m^-2) and was five times higher than that in grasslands (0.06 kg·m^-2) in China. Litter standing crop increased with latitude. Our results showed that litter standing crop was negatively correlated with mean annual temperature, soil total P and soil pH, but not significantly correlated with other environmental variables, including mean annual precipitation, soil carbon, nitrogen and soil organic matter. The conversion coefficient of carbon in litter standing crop was 0.41, which is significantly lower than that of vegetation in shrublands (0.50), resulting in an overestimate in carbon storage of litter standing crop in shrubland up to 22% by applying wrong conversion coefficient. We concluded that litter standing crop of shrublands is an important component in terrestrial ecosystems. Mean annual temperature was the most important environmental variable, accounting for the variation in litter standing crop of shrublands in southern China. To our best of knowledge, this is the first study to quantify variation in litter standing crop of shrublands at the regional scale. Therefore, our study will have important implications for assessing the carbon budget of terrestrial ecosystems in China.     

黄土高原草地植被碳密度的空间分布特征

草地是世界上分布最广的植被类型之一,作为陆地生态系统的重要组成部分,参与了全球碳源/汇及碳循环过程,在全球气候变化中扮演着重要角色,并对其产生重大影响。以黄土高原草地植被为研究对象,结合国家退耕还林草与封山禁牧工程的实施,对封禁前后的天然草地和退化草地,采用样带多点调查与多年定位测定相结合的方法,分析了黄土高原不同类型草地植物活体、凋落物和根系碳密度分布格局与地带性规律,系统研究了黄土高原不同草地类型退化草地和封禁草地生物量与碳密度沿海拔及降水梯度的时空变异特征,阐述了影响草地碳密度分布的主要驱动因子及其作用机理。结果表明:4种草地类型3种处理的草地生物量和碳密度自西北向东南均与降雨量呈指数增长趋势,并随海拔降低而显著降低,且二者呈显著的线性回归关系;各草地类型地上/地下生物量与碳密度分布规律均为荒漠草原<丘陵典型草原<梁塬典型草原<草甸草原;封禁11a草地活体植物、凋落物和根系碳密度总量:荒漠草原为7.066 t/hm2,丘陵典型草原为8.080 t/hm2,梁塬典型草原为15.319 t/hm2,草甸草原为20.982 t/hm2,分别是退化草地的14.8、8.33、6.5倍和15.88倍。充分表明,封禁不仅能使草地植被恢复和生物量提高,而且也是草地生产力和碳密度增加的一条重要途径。由此可见,气候干旱和草地退化是影响草地生物量和碳密度的关键因素,系统研究黄土高原封禁草地生物量增长与碳密度变化过程,将会对未来全球气候变化分析作出重要贡献。     

黄土高原草地净初级生产力时空动态及其影响因素

利用光能利用效率模型(Carnegie-Ames-Stanford approach,CASA)模拟2000-2015年黄土高原草地净初级生产力(NPP),分析黄土高原草地NPP的时空动态、NPP变化稳定性和持续性特征,从植被类型、地形因素、气候变化和人类活动4个方面探讨黄土高原草地NPP的影响因素.结果表明:黄土高原草地NPP的平均值为202.93 g C·m^-2·a^-1,其年际变化特征呈现显著增加的趋势,平均年增加速率为2.43 g C·m^-2·a^-1;分布具有明显的空间异质性,大体呈南高北低的状态.黄土高原草地NPP呈增加趋势的区域占总草地面积的91.2%,主要分布在陕西省的大部分地区、甘肃陇东及陇中地区和青海等地.草地NPP变化较为稳定的区域主要集中在鄂尔多斯的南部地区、陕北地区和甘肃等地.大部分地区草地NPP未来的变化趋势与过去一致,且陕西省的大部分地区以及甘肃省的陇中及陇东地区的草地NPP将呈现持续显著增加的趋势.坡面草地的平均NPP值最高,为703.37 g C·m^-2·a^-1;而高山亚高山草地NPP平均值最低,为57.28 g C·m^-2·a^-1.高海拔地区的草地NPP较高,而平原及丘陵地带草地NPP相对较低.研究期间黄土高原降水量的增加对草地NPP的增加具有明显的促进作用;人类活动诸如过度放牧状况的改善以及退耕还草等政策的实施对黄土高原草地NPP的增加也具有重要作用.     

Changes in composition and structure of Vitex shrubland in northern China in relation to human disturbance

Vegetation and biomass in six plots, each with five quadrats, in Vitex shrubland in northern China were related to type and degree of human disturbance. Canonical correspondence analysis of the vegetation and environmental data showed two lines of variation, the first one highly correlated with the degree of disturbance, but the second one appearing within the disturbed plots cannot yet be fully explained. Changes in life-form spectrum were small, but the geographical spectrum changed under heavy disturbance towards a higher proportion of tropical, subtropical and cosmopolitan species. The number of shrub species also decreased noticeably. The above-ground biomass of both Vitex and the accompanying species and the total above-ground biomass of the shrubland was negatively correlated with the intensity of disturbance. The root/stem biomass ratio in Vitex reaches values of over 5 in disturbed plots, but only between 1 and 2 in the protected plots.     

青藏高原北部多年冻土区草地植物多样性

研究了青藏高原北部多年冻土区草地群落植物多样性的特征。研究表明 :草地群落间丰富度指数差异不显著 ,均匀度指数和多样性指数差异显著 (P<0 .0 5 )。均匀度指数表现为高山嵩草 (Kobresia pygmaea)草甸 <紫花针茅 (Stipa purpurea)草原 <矮嵩草 (K.humilis)草甸 <青藏苔草 (Carex moorcroftii)草甸 ,多样性指数表现为高山嵩草草甸 <矮嵩草草甸 <紫花针茅草原<青藏苔草草甸。修路时破坏的矮嵩草草甸在次生恢复过程中 ,离公路 10 0 m处群落的丰富度指数 ,均匀度指数和多样性指数大于原生群落 ,而原生群落的多样性又大于 30 m和 5 0 m处群落的多样性。地上草地群落植物多样性伴随地下冻土退化过程表现为 ,以 1m2样方统计时 ,各个演替群落间的丰富度指数差异不显著 ,而以 10 0 m2样条统计时 ,高寒草甸和草原化草甸的丰富度指数显著大于沼泽草甸和稀疏草原 (P<0 .0 5 ) ,但均匀度和多样性指数在两种统计面积时均表现为先增加后下降的变化趋势。     

黄土高原北部紫花苜蓿草地退化过程与植物多样性研究

以陕西省神木县六道沟小流域为研究区域,探讨了黄土高原北部紫花苜蓿人工草地退化过程中植物多样性的变化.结果表明,在黄土高原北部森林草原气候区,紫花苜蓿人工草地的退化演替过程可以划分为3个阶段:紫花苜蓿草地阶段(1～6年)、人工草地向天然草地演替的过渡阶段(6～10年)与长芒草次生天然草地阶段(10年以上).在1～30年的演替过程中,调查样方内共出现高等植物32种,分属于13科28属,其中90%以上出现在前6年.植被演替过程中累积出现的植物科属种数的动态变化可以用对数函数进行较好地描述.在群落演替过程中,物种丰富度指数、多样性指数和Pielou均匀度指数的变化趋势基本一致,在演替前期(第1个阶段)增加较快,在第2个阶段(过渡阶段)达到最高,然后有所降低并渐趋稳定.种植紫花苜蓿可显著地加快植被的自然演替进程,这与人工草地水分消耗强烈加速了土壤的旱化过程密切相关.发展人工草地是黄土高原北部加速天然植被恢复与发展畜牧业、增加农民收入的有机结合点,是西部生态环境建设中生态效益与经济效益兼顾的良好范式.     

Soil surface disturbance alters cyanobacterial biocrusts and soil properties in dry grassland and shrubland ecosystems

Plant and Soil - Biological soil crusts (biocrusts) dominate soil surfaces in drylands, providing services that include soil stabilization and carbon uptake. In this study, we investigated the...     

松嫩草地80种草本植物叶片氮磷化学计量特征

以松嫩草地常见草本植物为研究对象, 分析了各生活型和功能群叶片氮磷化学计量特征。结果显示: 松嫩草地80种草本植物的叶片氮、磷质量浓度分别为(24.2 ± 0.96) mg·g ^-1和(2.0 ± 0.10) mg·g ^-1, 面积浓度分别为(13.0 ± 0.54) mg·cm ^-2和(1.0 ± 0.05) mg·cm ^-2, 氮磷比为13.0 ± 0.39, 氮磷比与叶片磷质量浓度、叶片氮、磷面积浓度有显著相关关系; 松嫩草地植物生长受到氮限制。一年生植物叶片氮、磷质量浓度和变异系数高于其他生活型, 各生活型之间氮面积浓度和氮磷比差异不显著。豆科植物叶片氮的质量浓度、面积浓度和氮磷比高于其他功能群。在不同生活型或功能群之间, 植物叶片磷的面积浓度差异不显著, 都在1.0 mg·cm ^-2左右; 适当地增加群落中豆科植物的比例, 可能有助于提高松嫩草地产量和质量。     

青藏高原高寒灌丛生态系统草本层生物量分配格局

青藏高原高寒灌丛生态系统生物量分配的研究相对较少,尤其是其草本层。为了探究高寒灌丛生态系统草本层生物量分配特征及其影响因素,分析了青藏高原东北部灌丛生态系统的49个高寒灌丛样地的草本层地上与地下生物量特征及其气候因子之间的关系。结果表明1)草本层地上生物量与地下生物量分别为121.1,342.8 g/m2均大于高寒草地的地上生物量与地下生物量。2)草本层的根冠比为3.6低于高寒草地的根冠比。3)地上生物量与地下生物量之间呈现幂函数的关系y=8.0x0.83(R2=0.48,P0.001)。4)根冠比与年均温度、年均降雨量之间没有显著的相关关系。     

Effects of Robinia pseudoacacia on the undergrowth of herbaceous plants and soil properties in the Loess Plateau of China

刺槐对黄土高原林下草本植物及土壤性质的影响 外来物种刺槐(Robinia pseudoacacia)的引入会对林下草本植物、土壤性质及二者之间的相互关系产 生一定影响,且这种影响可能与植被带有关。然而,在黄土高原较大面积范围内,关于刺槐对林下草本植物和土壤影响的研究依然很少。我们以黄土高原草原带、森林草原带和森林带作为研究区,选择了两种冠层植物类型：刺槐林分和相邻的原生植被。我们测定了5个叶片功能性状：叶片碳含量、叶片氮含量、叶片磷含量、比叶面积和叶组织密度,并计算了群落功能多样性、物种多样性和群落加权性状值。研究结果表明,(1)与原生植被相比,3个植被带内林下草本植物群落的叶氮、叶磷和比叶面积的群落加权性状值均显著提高,而叶碳和叶组织密度的群落加权性状值显著降低。(2)物种多样性、功能多样性和群落生物量在草原带内呈下降趋势,在森林带内呈上升趋势,在森林草原带内差异不显著。(3)与原生植被相比,土壤有机碳和土壤全氮仅在森林带内显著减少。(4)林下草本植物群落特性与土壤之间的关系是受刺槐和植被带所依赖的。总的来说,刺槐对林下草本植物和土壤性质的影响与植被带密切相关。该研究结果对黄土高原人工植被恢复与重建的规划具有重要指导意义。     

基于SOFM网络对黄土高原森林生态系统的养分循环分类研究

对森林生态系统进行分类是认识森林生态过程的根本途径,传统的从结构角度对森林生态系统分类只能反映森林的外在特征,而无法从功能角度区别森林的本质差异.通过对黄土高原3个生物气候区18个不同森林生态系统的养分循环特征测算和分析,选取了能全面反映养分的积累和分布(生物量、枯落物积累量、养分积累量)、循环通量(年吸收量、年存留量、年归还量)以及养分循环效率(循环系数、利用系数、养分生产力)等多方面指标作为分类指标体系,利用自组织映射特征网络(SelfOrganizing Feature Maps,SOFM)聚类方法,从养分循环的角度将黄土高原森林生态系统划分为2个一级类型,6个二级类型.该分类结果与实际较符,从而探索了森林生态系统的功能分类方法,也验证了SOFM网络模型应用于森林养分循环分类的可行性.