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1.
Virtanen  R.  Johnston  A.E.  Crawley  M.J.  Edwards  G.R. 《Plant Ecology》2000,151(2):129-141
The relationships between bryophyte biomass and species richness and soil pH, nutrient applications and vascular plant biomass and species richness were analyzed for the Park Grass Experiment (Rothamsted, UK). The study examined the abundance of bryophytes in relation to long-term fertilizer and lime application and to fertilizer treatments recently being ceased on some plots. The probability of bryophytes being present on a plot increased with increasing soil pH, and on plots at soil pH 3.3–4.5, the lowest values in this experiment, there were virtually no mosses present. Total bryophyte biomass decreased with increasing vascular plant biomass and vascular plant richness. Both bryophyte biomass and species richness showed a curvilinear response to soil pH. Bryophyte biomass was markedly increased on plots where nitrogen (N) fertilization had recently been ceased. The abundance of the common bryophyte species showed individualistic responses to treatments. N had a negative effect on the abundance of Brachythecium rutabulum. Increasing soil pH, and the application of phosphorus (P) and potassium (K) fertilizer together, had a positive effect on Eurhynchium praelongum. This species was also negatively affected by N, but tolerated larger amounts of it (100–150 kg ha–1 N) than B. rutabulum. An ephemeral moss, Bryum subapiculatum, had a unimodal response to soil pH but showed no response to N, P, K or other explanatory variables.  相似文献   

2.
滇西北高原纳帕海湖滨湿地退化特征、规律与过程   总被引:1,自引:0,他引:1  
尚文  杨永兴 《应用生态学报》2012,23(12):3257-3265
采用双向指示种分析(TWINSPAN)和典范对应分析(CCA)方法,研究了滇西北高原纳帕海湖滨湿地退化特征、规律与过程.结果表明: 纳帕海湖滨湿地植物群落可以划分为4个群丛,群落演替规律为水生植物群落→沼泽植物群落→沼泽化草甸植物群落→草甸植物群落.随植物群落演替,群落盖度、密度、多样性指数、物种丰富度和地上生物量均增大,群落高度减小;植物水分生态型演替规律为水生植物→沼生植物→湿生植物→中生植物.随群落演替,湿地水体矿化度、硬度和碱度均降低,氨氮和总磷含量升高,总氮和硝态氮含量变化不明显;土壤pH、有机质和全氮含量逐渐降低,全磷和全钾含量逐渐升高,速效氮和速效磷含量先增大后减小.CCA分析表明,群落结构和物种组成主要受水分梯度影响,土壤pH、全磷和湿地水的总氮、氨氮对湿地植物物种分布和群落演替影响显著.  相似文献   

3.
土壤微生物多样性的形成、维持和变化机理是生态学研究的核心内容, 已有大量研究表明土壤微生物群落构建不仅受到土壤环境的深刻影响, 也与植物群落物种多样性密切相关。由于自然群落中土壤环境和植物多样性协同影响土壤微生物, 难以区分和厘清植物多样性和土壤环境对土壤微生物多样性构建的各自影响。该研究基于在青藏高原高寒草地构建的人工草地群落, 比较分析了3种优势禾本科牧草单播和混播及施肥处理13年后, 土壤细菌和真菌物种多样性及其与植物群落和土壤理化因子的关系。主要结果: 1)与各单播处理相比, 3种牧草两两混播一致显著降低了土壤细菌群落的丰富度和多样性, 其中变形菌门和放线菌门相对丰度显著增加, 而酸杆菌门、拟杆菌门和浮霉菌门相对丰度显著减小; 牧草混播对土壤真菌多样性没有显著影响。2)牧草混播显著降低了土壤pH和土壤全氮含量, 增加了土壤全磷含量; 施肥显著降低土壤pH, 增加了土壤速效磷含量; 但这些土壤理化因子的变化不足以解释土壤细菌和真菌多样性在处理间的差异。3)施肥显著提高了植物群落地上生物量, 降低了植物物种丰富度, 土壤细菌多样性随植物物种丰富度增加而减小, 而与植物生物量变化无关。该研究在野外条件下, 通过长期控制实验揭示了高寒草地禾草混播并不增加土壤微生物多样性, 为高寒地区牧草混播人工草地实践提供了科学依据。  相似文献   

4.
杜志勇  丛楠 《生态学报》2024,44(6):2504-2516
高寒草地作为青藏高原高寒生态系统的重要组分之一,其退化已严重影响到高原的可持续发展和草地恢复重建。搜集了2004—2022年间关于青藏高原高寒草地退化的64篇研究结果,包含土壤有机碳、生物量和多样性指数等16个指标的1403组数据,运用meta分析解析了草地退化对土壤理化性质、植被生产力和物种多样性的影响,并对重度退化草地的土壤理化性质和植物生物量进行线性回归分析。结果表明:随着草地退化的加剧,土壤有机碳、全氮、全磷、有效氮、有效磷、有效钾、土壤含水量、地上生物量、地下生物量和植被高度显著下降;土壤容重显著上升;土壤pH、全钾在各个退化阶段没有明显差异;Shannon多样性指数、Pielou均匀度指数和Margalef丰富度指数整体呈下降趋势。土壤有机碳、全氮、全磷、有效氮、有效磷、有效钾和土壤含水量与地上生物量、地下生物量存在显著的正相关;土壤容重与地上生物量、地下生物量呈显著的负相关;土壤pH与地上生物量、地下生物量呈负相关。因此,青藏高原高寒草地退化通过改变土壤理化性质而改变地上群落多样性和生物量,为阐明植被与土壤特征对草地退化的响应机制以及高寒退化草地的恢复提供了科学依据。  相似文献   

5.
杨军  刘秋蓉  王向涛 《应用生态学报》2020,31(12):4067-4072
选取西藏自治区拉萨市当雄县4块不同退化程度的高山嵩草高寒草甸,采用空间序列代替时间演替的方法,研究不同退化阶段高寒草甸的土壤理化性质和植物群落特征以及二者之间的相关关系。结果表明: 不同退化阶段高寒草甸的土壤有机碳、全氮、速效磷、速效钾、铵态氮、硝态氮和含水量均随土壤退化程度加剧呈降低的趋势,而pH值呈现升高的趋势。中度退化草甸的植物群落高度、丰富度指数、多样性指数、均匀度指数最大。群落盖度、总生物量均为未退化草甸最大、重度退化草甸最小。随着草甸退化程度加剧,莎草科生物量及比例下降,豆科和杂类草生物量及比例增加,禾本科生物量及比例先增加后减小;草甸植物群落地上生物量与土壤有机碳、全氮、全磷含量和土壤含水量呈显著正相关,与土壤pH值呈显著负相关。随着草甸植被的退化,土壤退化加重,最终表现为草地生产力显著下降。  相似文献   

6.
研究生物多样性对季节的响应对于维持生态系统稳定、保护生物多样性、解析群落构建机制具有重要意义。本文以博斯腾湖湖滨湿地为研究对象,探究不同季节植物群落的物种多样性与功能多样性的变化规律。结果显示:(1)物种多样性指数随季节变化没有显著改变;功能多样性指数中,功能丰富度由春季到夏季逐渐减小,功能离散度逐渐增大;不同季节的功能均匀度差异性不显著;(2)植物功能性状在不同季节间差异显著;春季叶绿素含量显著低于夏季;夏季比叶面积和叶干物质含量显著高于秋季;叶片含水量和厚度由春季到秋季呈递增趋势;(3)影响Pielou指数和功能丰富度的主要环境因子分别为土壤铵态氮和速效磷;影响Shannon-Wiener指数、Simpson指数和功能均匀度的主要环境因子为土壤有机质;影响功能离散度的主要环境因子为土壤含水量;(4)影响最大株高的主要环境因子为土壤pH值;影响叶干物质含量的主要环境因子为土壤速效钾;影响叶片厚度和比叶面积的主要环境因子为土壤总磷;而影响叶片含水量的主要环境因子为土壤硝态氮;叶绿素含量与土壤因子无显著相关关系。  相似文献   

7.
Several different hypotheses account for the success of introduced species in new environments. Experimental studies show a negative native-exotic richness relationship (NERR), while observational studies suggest that this relationship is usually positive. Increased resource availability and environmental variation can also enable introduced species to establish in new environments. We conducted an observational study in a semi-arid grassland in the Thompson-Nicola District of British Columbia to examine the biotic and abiotic factors that account for variation in introduced and native species richness.In each of 12 sites, an 8 × 8 m area was set up, containing 64, 1-m2 plots. We identified and categorized plant species in each site into introduced and native species. We tested the relationship between introduced species richness and native species richness at the 1-m2 sampling grain and at sampling grains up to 64 m2. We also analysed the relationship between native and introduced species, and within-plot biomass, and between native and introduced species and variation in biomass. For a representative subset of four sites, we tested the relationship between introduced and native species richness and nitrogen, phosphorus and potassium.We found no NERR at the 1 m2 sampling grain, nor for the other sampling grains up to 64 m2. Introduced species richness increased with phosphorus and nitrogen availability, and was also positively related to biomass heterogeneity.Our results indicate that introduced species richness in these grasslands is likely influenced by phosphorus and nitrogen, and by variation in vegetation biomass, but not by native species. More non-native plants are likely to occupy nutrient-rich plots compared to nutrient-poor plots in these grasslands. Variation in biomass can leave gaps for the establishment of introduced species. These results should inform management considerations for the control of invasive species to optimize preservation of grasslands.  相似文献   

8.
A microcosm-based approach was used to study impacts of plant and chemical factors on the fungal community structure of an upland acidic grassland soil. Seven plant species typical of both unimproved and fertilized grasslands were either left unamended or treated with lime, nitrogen or lime plus nitrogen. Fungal community structure was assessed by a molecular approach, fungal automated ribosomal intergenic spacer analysis (FARISA), while fungal biomass was estimated by measuring soil ergosterol content. Addition of nitrogen (with or without lime) had the largest effect, decreasing soil pH, fungal biomass and fungal ribotype number, but there was little corresponding change in fungal community structure. Although different plant species were associated with some changes in fungal biomass, this did not result in significant differences in fungal community structure between plant species. Addition of lime alone caused no changes in fungal biomass, ribotype number or community structure. Overall, fungal community structure appeared to be more significantly affected through interactions between plant species and chemical treatments, as opposed to being directly affected by changes in individual improvement factors. These results were in contrast to those found for the bacterial communities of the same soils, which changed substantially in response to chemical (lime and nitrogen) additions.  相似文献   

9.
五大连池火山熔岩台地草本层物种多样性及环境解释   总被引:2,自引:0,他引:2  
五大连池火山熔岩台地是一种火山地貌, 研究熔岩台地草本物种分布及其环境解释, 对认识火山原生演替过程中植物群落空间格局形成及适应机制具有重要意义。本文以五大连池熔岩台地的草本物种为研究对象, 调查了苔藓、草本、灌丛、阔叶林和针阔混交林等不同植被类型中的草本层样方, 并测定样方中的土壤养分和水分等状况, 采用多样性指数、优势度指数、均匀度指数、物种丰富度评价草本层物种多样性, 通过典范对应分析方法研究了群落组成与土壤因子的关系。结果表明: (1)熔岩台地草本层物种丰富, 共56种, 占本研究调查区总物种数的82.35%, 草本样地的草本层物种多样性、优势度和均匀性高于其他植被类型。(2)熔岩台地土壤pH值对群落草本层物种丰富度和物种个体的空间分布均有较大影响。(3)土壤因子解释了群落分布的79.39%, 其中土壤pH值、速效磷、硝态氮、铵态氮所占的解释量比较大。(4)岩败酱(Patrinia rupestris)、万年蒿(Artemisia sacrorum)、硬质早熟禾(Poa sphondylodes)和中华苦荬菜(Ixeris chinensis)对环境要求较低, 能够适应熔岩台地土壤贫瘠恶劣的环境。熔岩台地不同植被类型表现出对环境资源的特定需求, 熔岩地貌导致了土壤pH值、养分、水分的差异, 并影响植物群落的分布。  相似文献   

10.
A microcosm-based approach was used to study impacts of plant and chemical factors on the bacterial community structure of an upland acidic grassland soil. Seven perennial plant species typical of both natural, unimproved (Nardus stricta, Agrostis capillaris, Festuca ovina and F. rubra) and fertilized, improved (Holcus lanatus, Lolium perenne and Trifolium repens) grasslands were either left unamended or treated with lime, nitrogen, or lime plus nitrogen in a 75-day glasshouse experiment. Lime and nitrogen amendment were shown to have a greater effect on microbial activity, biomass and bacterial ribotype number than plant species. Liming increased soil pH, microbial activity and biomass, while decreasing ribotype number. Nitrogen addition decreased soil pH, microbial activity and ribotype number. Addition of lime plus nitrogen had intermediate effects, which appeared to be driven more by lime than nitrogen. Terminal restriction fragment length polymorphism (TRFLP) analysis revealed that lime and nitrogen addition altered soil bacterial community structure, while plant species had little effect. These results were further confirmed by multivariate redundancy analysis, and suggest that soil lime and nitrogen status are more important controllers of bacterial community structure than plant rhizosphere effects.  相似文献   

11.
Understanding changes in biodiversity in agricultural landscapes in relation to land-use type and intensity is a major issue in current ecological research. In this context nutrient enrichment has been identified as a key mechanism inducing species loss in Central European grassland ecosystems. At the same time, insights into the linkage between agricultural land use and plant nutrient status are largely missing. So far, studies on the relationship between chemical composition of plant community biomass and biodiversity have mainly been restricted to wetlands and all these studies neglected the effects of land use. Therefore, we analyzed aboveground biomass of 145 grassland plots covering a gradient of land-use intensities in three regions across Germany. In particular, we explored relationships between vascular plant species richness and nutrient concentrations as well as fibre contents (neutral and acid detergent fibre and lignin) in the aboveground community biomass.We found the concentrations of several nutrients in the biomass to be closely linked to plant species richness and land use. Whereas phosphorus concentrations increased with land-use intensity and decreased with plant species richness, nitrogen and potassium concentrations showed less clear patterns. Fibre fractions were negatively related to nutrient concentrations in biomass, but hardly to land-use measures and species richness. Only high lignin contents were positively associated with species richness of grasslands. The N:P ratio was strongly positively related to species richness and even more so to the number of endangered plant species, indicating a higher persistence of endangered species under P (co-)limited conditions. Therefore, we stress the importance of low P supply for species-rich grasslands and suggest the N:P ratio in community biomass to be a useful proxy of the conservation value of agriculturally used grasslands.  相似文献   

12.
We measured aboveground plant biomass and soil inorganic nitrogen pools in a biodiversity experiment in northern Sweden, with plant species richness ranging from 1 to 12 species. In general, biomass increased and nitrate pools decreased with increasing species richness. Transgressive overyielding of mixed plant communities compared to the most productive of the corresponding monocultures occurred in communities with and without legumes. N2-fixing legumes had a fertilizing function, while non-legumes had a N retaining function. Plant communities with only legumes had a positive correlation between biomass and soil nitrate content, whereas in plant communities without legumes they were negatively correlated. Both nitrate and ammonium soil pools in mixed non-legume communities were approximately equal to the lowest observed in the corresponding monocultures. In mixed legume/non-legume communities, no correlation was found for soil nitrate with either biomass or legume biomass as percentage of total biomass. The idea of complementarity among species in nitrogen acquisition was supported in both pure non-legume and mixed non-legume/legume communities. In the latter, however, facilitation through increased nitrogen availability and retention, was probably dominating. Our results suggest that diversity effects on biomass and soil N pools through resource use complementarity depend on the functional traits of species, especially N2 fixation or high productivity.  相似文献   

13.
陕北黄土丘陵区撂荒草地群落生物量及植被土壤养分效应   总被引:29,自引:2,他引:27  
杜峰  梁宗锁  徐学选  山仑  张兴昌 《生态学报》2007,27(5):1673-1683
为了明确植被演替过程中植被与土壤的互动效应,为植被恢复提供依据。根据陕北黄土丘陵区36块不同年限(时间尺度为2—45a)的撂荒样地地上生物量、土壤养分和水分的测定结果,及4块典型撂荒群落样地地上/地下生物量,7种撂荒群落主要植物生长特性的测定,分析了撂荒演替过程中群落生物量与土壤养分的变化过程、趋势及其相互关系,进而探讨了撂荒演替过程中群落生物量对土壤养分的作用效应,并利用多元回归和通径分析法分析了土壤养分对群落生物量的作用。结果表明:(1)除速效磷外,撂荒演替过程中群落地上生物量和土壤有机质、全氮、全磷、全钾、NO3-N、NH4-N和速效钾都呈先减少后增加的趋势,步调基本一致。(2)从撂荒年限与土壤养分的相关性来看,0—20cm土壤有机质含量、速效磷含量和0—20、20—40cm土壤层NO3-N含量与撂荒年限相关显著,说明演替过程中有机质、速效磷和NO3-N有较为明显的植被土壤效应,而其它土壤养分与撂荒年限相关不显著,不能排除演替初始条件和植物暂时固定的影响;从群落生物量与土壤养分的相关性来看,群落生物量对土壤有机质、全氮、磷、钾、NO3-N、速效钾和速效磷含量具有正效应,而对NH4-N具有负效应,但都不显著。(3)通径分析说明撂荒年限、土壤全氮、全钾、速效钾和土壤水分变异量对生物量表现为正的直接作用,其中以撂荒年限和土壤水分波动量作用较大,土壤养分对群落地上生物量的作用以土壤全氮最大,全钾和速效钾影响较小;演替过程中群落地上生物量的变化主要是由于植被盖度和群落组成种的生态学特性造成的(撂荒年限较大的直接作用),其次是由于撂荒演替过程中土壤水分的波动造成的(撂荒年限通过土壤水分的间接负作用)。(4)随着土层深度的加深植物根系生物量呈幂函数递减过程,演替后期群落根冠比有增加的趋势,演替后期序列种根冠比和根长也有增加的趋势,这些在一定程度上会影响到生物量积累和有机质分解等,进而会影响到植被土壤效应。  相似文献   

14.
赵敏  赵锐锋  张丽华  赵海莉  周远刚 《生态学报》2019,39(11):4116-4126
湿地植物多样性的研究对维持湿地生态系统完整性和稳定性有着重要意义。以黑河中游湿地为研究对象,基于野外采样数据和不同盐分梯度植物群落多样性指数,重点分析不同盐分梯度植物多样性变化及其与土壤因子关系。结果表明:黑河中游湿地植物组成比较丰富,共出现植物30科71属102种;随土壤盐分梯度增加,植物群落组成发生显著变化,Margalef丰富度指数(R)和Shannon-Weiner多样性指数(H)均减小,说明研究区植物多样性随盐分增加而减少;不同盐分梯度影响植物多样性的土壤因子存在差异,低盐梯度是pH、速效钾和全氮,中盐梯度是pH、速效磷和速效钾,高盐梯度是有机质、全磷、速效钾和速效氮。该研究结果对于认识不同盐分梯度下影响植物多样性的主要土壤因子具有重要意义,同时对黑河中游湿地植物多样性的有效管理和维持具有一定的参考价值。  相似文献   

15.
Anthropogenic nutrient enrichment of mountain grasslands has boosted grasses and fast‐growing unpalatable plants at the expense of slow‐growing species, resulting in a significant loss in biodiversity. A potential tool to reduce nutrient availability and aboveground productivity without destroying the perennial vegetation is carbon (C) addition. However, little is known about its suitability under severe climatic conditions. Here, we report the results of a 3‐year field study assessing the effects of sawdust addition on soil nutrients, aboveground productivity, and vegetational composition of 10 grazed and ungrazed mountain grasslands. Of particular interest was the effect of C addition on grasses and on the tall unpalatable weed Veratrum album. After 3 years, soil pH, ammonium, and plant‐available phosphorus were not altered by sawdust application, and nitrate concentrations were marginally higher in treatment plots. However, the biomass of grasses and forbs (without V. album) was 20–25% lower in sawdust‐amended plots, whereas the biomass of V. album was marginally higher. Sawdust addition reduced the cover of grasses but did not affect evenness, vegetation diversity, or plant species richness, although species richness generally increased with decreasing biomass at our sites. Our results suggest that sawdust addition is a potent tool to reduce within a relatively short time the aboveground productivity and grass cover in both grazed and ungrazed mountain grasslands as long as they are not dominated by tall unpalatable weeds. The technique has the advantage that it preserves the topsoil and the perennial soil seed bank.  相似文献   

16.
Du F  Liang Z S  Xu X X  Shan L  Zhang X C 《农业工程》2007,27(5):1673-1683
In order to have a basic knowledge of revegetation, one needs to deepen his understanding of the interactive effects of vegetation and soil. In this article, aboveground biomass, soil nutrients and moisture of 36 old-fields with different abandonment ages (from 2 to 45 years after abandonment), aboveground biomass of 4 typical old-fields, and growth characteristics of 7 predominant old-field species were measured. Changing pace, trend and relationship of community aboveground biomass and soil nutrition during the secondary succession were evaluated; effects of soil nutrition on community aboveground biomass were analyzed using multivariable analysis and pathway analysis, and effects of aboveground biomass on soil nutrition were further discussed. The results show that: (1) Soil nutrients, including organic matter, total nitrogen, total phosphorus, total potassium, nitrate nitrogen, ammonium nitrogen, active phosphorus and active potassium, have the same changing pace and trends as the aboveground biomass. In the process of secondary succession, both the soil nutrition and the community aboveground biomass decreased in the earlier abandonment stage of succession and then increased subsequently. (2) On the basis of the correlation of soil nutrients and abandonment ages, effects of vegetation on 0–20 cm organic matter, active phosphorus, 0–20 cm and 20–40 cm nitrate nitrogen nutrition are significant, while on the basis of the correlation of soil nutrition and aboveground biomass, no significant effects were observed. Hereinbefore, aboveground biomass accounts for only a part of vegetation-soil nutrition effects. The effects of biomass on organic matter, total nitrogen, total phosphorous, total potassium, nitrate nitrogen, active potassium and phosphorous are positive, whereas for ammonium nitrogen it is negative. (3) Abandonment ages, total nitrogen, total potassium, active potassium and soil moisture fluctuation have direct positive effects on the aboveground biomass of old-field communities; abandonment and soil moisture fluctuation have lager effects. Each ingredient of soil nutrition has relatively small effect, among which total nitrogen has larger effects than total and active potassium. The changes in aboveground biomass of old-field communities during succession are caused mainly by the changes in coverage and ecological characteristics of community species (the relatively larger direct effects of abandonment ages), and secondly by the soil moisture fluctuation (the relative smaller indirect effect of abandonment ages through soil moisture). (4) As a dependent variable, belowground biomass approaches power function of soil depth and declines in deeper layer. The root/shoot ratio of communities tends to increase in later succession stages, which also has an increasing tendency. These may influence the accumulation of biomass and decomposition of organic matter, and the vegetation-soil effects may be different.  相似文献   

17.
在甘南高寒草甸单户经营草场与联户经营草场进行野外群落学调查,分析其物种多样性和功能多样性的变化,以揭示不同经营方式下土壤理化性质对植物多样性的影响机制。结果显示:(1)联户草场内植物群落的Margalef指数、Simpson指数、Shannon-Winener指数较大,而Pielou指数在不同放牧经营方式下的差异并不显著。(2)不同经营方式下,土壤含水量、土壤全氮、土壤全磷和土壤有机碳质量分数表现为联户大于单户的趋势且差异显著(P<0.05);单户草场土壤电导率与土壤pH大于联户草场;随着土层的加深土壤含水量、土壤全氮质量分数、土壤全磷质量分数、土壤有机碳质量分数和土壤电导率增加,而土壤pH在土层之间的差异并不显著。(3)联户经营方式下的功能丰富度、功能均匀度与功能离散度显著大于单户草场(P<0.05)。(4)相关性分析表明,植物群落物种多样性和功能多样性与土壤含水量、土壤全氮质量分数和土壤全磷质量分数存在正相关关系,土壤电导率和土壤pH与植物群落物种多样性和功能多样性存在负相关关系。冗余分析表明,联户经营方式下土壤理化性质对植物多样性的影响更显著,且0相似文献   

18.
除草剂在桉树人工林中的应用越来越普遍,但关于除草剂对桉树人工林林下植物和土壤微生物群落的影响知之甚少。通过桉树人工林低剂量高频率(LHF)、中剂量中频率(MMF)、高剂量低频率(HLF)除草剂喷施试验,并与人工除草(MT)为对照,比较分析不同剂量、不同频率除草剂施用对林下植物和土壤微生物群落的影响。结果表明,施用除草剂导致桉树人工林林下植物种类和功能群组成发生显著变化,但并未显著降低林下植物群落物种丰富度和多样性,随除草剂施用频率的降低及恢复时间的增加,物种丰富度及多样性指数呈恢复趋势。除草剂施用也导致土壤养分含量降低。除草剂通过对林下植物群落和土壤养分的负面影响间接影响土壤微生物群落。LHF显著降低藤本植物而显著提高蕨类植物功能群的重要值,从而显著降低了微生物群落、真菌和放线菌的磷脂脂肪酸(PLFA)含量。MMF显著降低木本和藤本植物而显著提高禾草植物功能群的重要值,导致土壤微生物群落和放线菌的PLFA含量显著降低。HLF未显著影响林下植物及土壤微生物群落,但土壤全磷含量显著降低,速效磷含量也大幅下降。施用除草剂显著降低了土壤微生物生物量碳、氮的含量。因此,生产上应减少除草剂的施用,...  相似文献   

19.
为探讨不同入侵压力下入侵植物对本地植物功能性状土壤碳、氮、磷化学计量特征的影响,以入侵植物曼陀罗(Datura stramonium)及共存本地植物为研究对象,调查了无入侵区、轻度入侵区和重度入侵区(按入侵种盖度比例划分)的植物种类、株数、株高及本地植物群落的物种多样性,分析了各区入侵植物和本地植物叶片的比叶面积、碳含量、氮含量、碳氮比、叶片建成成本以及不同土层的碳、氮、磷化学计量特征。结果显示:随曼陀罗入侵压力的增加,本地植物种类及株数逐渐减少;曼陀罗株高和叶片氮含量在不同入侵压力下均显著高于本地植物,且随入侵压力的增加具有升高趋势;叶片碳氮比显著低于无入侵区本地植物;比叶面积、叶片碳含量和叶片建成成本等与入侵区本地植物相比不具有显著差异。随曼陀罗入侵压力的增加,土壤全氮含量、全碳含量、氮磷比与碳磷比显著增加,而全磷含量与碳氮比显著下降;土壤碳氮化学计量特征呈现出一定的表聚效应。这些研究结果表明,曼陀罗具有较高的资源捕获能力,并且改变了入侵地土壤特性,进而增强自身竞争能力以提高入侵力,这些可能是曼陀罗成功入侵的原因之一。  相似文献   

20.
Summary We studied the effect of liming on the rates of mineralization and nitrification in a coarse-textured kaolinitic Ultisol. Soil samples were taken from field plots which received lime rates from 0 to 4mt/ha three years prior to the study. The pH of the soil samples varied from 4.2 to 6.1. Ammonification of soil organic N and added urea source proceeded readily and was not affected by lime rate. Nitrification occurred in both limed and unlimed soils but the rate of nitrification depended upon the rate of lime application. Soil pH, exchangeable Ca and exchangeable A1 were significantly correlated with the amount of NO3-N accumulated at the end of the 65 days incubation period. Nitrification of NH4-N from ammonium sulfate was absent in soils receiving lower rates of lime which gave pH values ranging from 4.2 to 4.8. Added ammonium source was nitrified readily after a 3-week delay period in the soil (pH 6.1) which received a higher rate of lime (4 mt/ha).  相似文献   

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