外来植物入侵对土壤氮有效性的影响

外来植物入侵对土壤氮循环和氮有效性的影响是入侵成功或进一步加剧的重要原因。通过对比相同研究地点入侵区域和无入侵区域的土壤原位氮状态差异, 探讨了外来植物入侵对土壤氮有效性的影响程度和生理生态学机制。基于107篇相关研究文献数据的整合, 发现植物入侵区域相对于无入侵区域土壤总氮、铵态氮、硝态氮、无机氮、微生物生物量氮含量显著增加, 增幅分别为(50 ± 14)%、(60 ± 24)%、(470 ± 115)%、(69 ± 25)%、(54 ± 20)%。土壤硝态氮含量增幅较大反映硝化作用增强, 这可能增加入侵植物硝态氮利用以及喜硝植物的共存。温带地区植物入侵后土壤的硝态氮含量增幅显著高于亚热带地区。固氮植物入侵后土壤的总氮和无机氮含量增幅均显著高于非固氮植物入侵。木本和常绿植物入侵后土壤的总氮含量增幅分别高于草本和落叶植物入侵; 而土壤铵态氮含量的增幅没有显著差异且与固氮入侵植物占比无明显关系; 然而硝态氮含量的增幅普遍较高且与固氮入侵植物占比显著正相关。外来入侵植物固氮功能以及凋落物质量和数量是影响土壤氮矿化和硝化过程的关键因素。该研究为理解外来植物入侵成功和加剧的机制以及入侵植物功能性状与土壤氮动态之间的关系提供了新的见解。     

氮硅添加对青藏高原高寒草甸土壤氮矿化的影响

为了解全球气候变化背景下氮沉降对土壤氮矿化的影响及硅添加对土壤氮矿化的促进作用, 该试验设置不同浓度的氮肥单独添加(0、20、40、60 g·m ^-2, 分别为对照CK、N20、N40、N60)以及与硅肥配施(硅酸4 g·m ^-2, Si4), 测定不同处理下0-20、20-40、40-60 cm土层土壤硝态氮含量、铵态氮含量、净硝化速率、净氨化速率以及净矿化速率。结果显示: (1)单独添加氮肥, 各土层土壤硝态氮和铵态氮含量均随处理浓度的增加而增加, 0-20 cm土层N20、N40、N60处理下土壤硝态氮和铵态氮分别较CK增加63.48%、126.04%、247.03%和80.66%、152.52%、244.56%; 随着土层深度增加, 土壤硝态氮、铵态氮含量均有下降, 20-40、40-60 cm土层较0-20 cm土层硝态氮含量分别平均减少53.90%、76.05%, 铵态氮含量分别平均减少48.62%、68.23%。(2)土壤净硝化速率、净氨化速率及净矿化速率随着氮肥浓度增加均呈上升趋势。相同氮肥添加浓度下, 土壤净硝化速率、净氨化速率和净矿化速率随着土层深度增加逐渐下降(除CK外)。(3)与单独添加氮肥比较, 氮硅肥配施, 土壤氮含量有显著提高, 在0-20 cm土层硝态氮和铵态氮较CK分别增加98.78%、192.62%、330.16%和99.96%、195.82%、306.32%, 20-40、40-60 cm土层也有类似趋势。同时, 氮硅配施促进了土壤氮矿化行为, 在0-20 cm土层, N60Si4处理下的土壤净硝化速率、净氨化速率较单独施氮时分别增加35.88%、27.41%。以上结果表明, 与单独氮肥添加相比, 氮硅配施不但能提高土壤氮含量, 而且能促进土壤氮的矿化作用, 对大气氮沉降有一定的缓解作用。     

Effects of enhanced UV-B radiation and nitrogen deposition on the growth of invasive plant Triadica sebifera

Aims Exotic plant invasions are important components of global change, threatening both the stability and function of invaded ecosystems. Shifts in competitive ability of invasive plants versus their native congeners have been documented. Enhanced UV-B radiation and nitrogen (N) deposition might interact with soil biota communities impacting the invasion process of exotic plant species. To understand the potential effects by UV-B and N with soil biota on plant growth would enhance our understanding of the mechanisms in plant invasions in the context of global change.
Methods We conducted a full-factorial pot experiment in the native range (China) of Triadica sebifera invading US to investigate how UV-B radiation, N and soil biota together determined their seedling growth.
Important findings The results showed that UV-B radiation, N and soil sterilization together impacted the growth of T. sebifera seedlings. UV-B radiation induced changes in biomass allocation with larger leaf biomass observed in response to UV-B radiation. In addition, N increased aboveground biomass and decreased root biomass simultaneously. Soil biota imposed positive effects on growth of T. sebifera, and the addition of N amplified these positive effects. The negative effects by UV-B radiation on growth of T. sebifera showed no response to N addition. Plant height, leaf biomass and total biomass of the invasive T. sebifera populations out- performed those of the native ones. In addition, invasive T. sebifera populations weakened the dependence of root/shoot ratio and root biomass on local soil microorganisms than native populations, but enhanced that of leaf area ratio.     

Responses of soil inorganic nitrogen to increased temperature and plant removal during the growing season in a Sibiraea angustata scrub ecosystem of eastern Qinghai-Xizang Plateau

为了揭示气候变暖背景下高寒灌丛土壤氮转化过程, 该文研究了青藏高原东缘窄叶鲜卑花(Sibiraea angustata)灌丛生长季节土壤硝态氮和铵态氮含量对增温和去除植物的响应。结果表明: 窄叶鲜卑花灌丛土壤硝态氮和铵态氮含量具有明显的季节动态。整个生长季节, 土壤硝态氮含量呈先增加后降低的趋势, 而铵态氮含量均表现为一直增加的趋势。在生长季初期和中期, 各处理土壤硝态氮含量均显著高于铵态氮含量, 而在生长季末期土壤硝态氮含量均显著低于铵态氮含量, 说明该区域土壤氮转化过程在生长季初期和中期以硝化作用为主, 而在生长季末期以氨化作用为主。不同时期土壤硝态氮和铵态氮含量对增温和去除植物的响应不同: 增温对硝态氮的影响主要发生在生长季中期和末期, 且因植物处理的不同而有显著差异, 增温仅在生长季中期使不去除植物样方铵态氮含量显著升高。去除植物对土壤硝态氮的影响仅表现在对照样方(不增温), 去除植物显著提高了生长季初期和中期土壤硝态氮含量, 显著降低了生长季末期土壤硝态氮含量; 同时去除植物显著降低了增温样方生长季中期土壤铵态氮含量。灌丛植被在生长季初期和中期可能主要吸收土壤硝态氮, 其吸收过程不受土壤增温的影响。     

Effects of plant invasion on soil nitrogen transformation processes and its associated microbes

外来入侵植物不仅影响植物群落组成、生物多样性以及生态系统的结构和功能, 而且显著影响土壤氮(N)的转化过程。外来入侵植物对N循环影响的研究已成为入侵生态学的研究热点。N循环与凋落物的分解和养分释放有关, 外来入侵植物能够改变凋落物的组成与结构, 进而影响土壤的N转化过程。另外, 外来入侵植物的化感作用也会影响土壤N转化过程, 这些作用与土壤微生物的结构与功能变化密不可分。该文主要从凋落物分解与养分释放及外来入侵植物化感作用两个方面综述了外来入侵植物对土壤N转化的影响, 总结了外来入侵植物对土壤N转化相关土壤微生物(尤其是氨氧化细菌与氨氧化古菌)的影响, 探讨了土壤N转化对外来植物入侵的反馈, 并探讨了丛植菌根真菌与外来入侵植物的互相影响。     

Allelopathy and exotic plant invasion

The primary hypothesis for the astonishing success of many exotics as community invaders relative to their importance in their native communities is that they have escaped the natural enemies that control their population growth – the `natural enemies hypothesis'. However, the frequent failure of introduced biocontrols, weak consumer effects on the growth and reproduction of some invaders, and the lack of consistent strong top-down regulation in many natural ecological systems indicate that other mechanisms must be involved in the success of some exotic plants. One mechanism may be the release by the invader of chemical compounds that have harmful effects on the members of the recipient plant community (i.e., allelopathy). Here, we provide an abbreviated compilation of evidence for allelopathy in general, present a detailed case study for Centaurea diffusa, an invasive Eurasian forb in western North America, and review general evidence for allelopathic effects of invasive plants in native communities. The primary rationale for considering allelopathy as a mechanism for the success of invaders is based on two premises. First, invaders often establish virtual monocultures where diverse communities once flourished, a phenomenon unusual in natural communities. Second, allelopathy may be more important in recipient than in origin communities because the former are more likely to be naïve to the chemicals possessed by newly arrived species. Indeed, results from experiments on C. diffusa suggest that this invader produces chemicals that long-term and familiar Eurasian neighbors have adapted to, but that C. diffusa's new North American neighbors have not. A large number of early studies demonstrated strong potential allelopathic effects of exotic invasive plants; however, most of this work rests on controversial methodology. Nevertheless, during the last 15 years, methodological approaches have improved. Allelopathic effects have been tested on native species, allelochemicals have been tested in varying resource conditions, models have been used to estimate comparisons of resource and allelopathic effects, and experimental techniques have been used to ameliorate chemical effects. We do not recommend allelopathy as a `unifying theory' for plant interactions, nor do we espouse the view that allelopathy is the dominant way that plants interact, but we argue that non-resource mechanisms should be returned to the discussion table as a potential mechanism for explaining the remarkable success of some invasive species. Ecologists should consider the possibility that resource and non-resource mechanisms may work simultaneously, but vary in their relative importance depending on the ecological context in which they are studied. One such context might be exotic plant invasion.     

Effects of exotic-native species relationship on naturalization and invasion of exotic plant species

达尔文归化难题描述了外来种-本地种亲缘关系促进(预适应假说)或阻止(达尔文归化假说)外来种成功入侵的悖论。目前, 在中国仍缺少针对达尔文归化难题的研究。为系统研究外来种-本地种亲缘关系对中国外来植物入侵的影响, 该文利用线性混合效应模型从省级、市级和群落3个空间尺度以及归化、扩散和入侵3个阶段探究了外来种-本地种谱系距离和外来植物表现的关系。结果表明: 在省级和市级(区域)尺度上, 与本地种亲缘关系较近的外来植物更有可能在当地归化和扩散, 符合预适应假说的预期; 而在群落(局域)尺度上, 外来种-本地种亲缘距离与外来种是否在群落中成功定居及其入侵程度无关。该研究结果表明与本地区系亲缘较近的外来种和本地种的竞争并不强烈, 却能较好地适应本地气候环境而具有更强的归化和入侵潜力。因此, 在今后的外来植物管理和治理中需要尤其重视与本地区系亲缘关系较近的外来植物。     

Altered ecosystem carbon and nitrogen cycles by plant invasion: a meta-analysis

Plant invasion potentially alters ecosystem carbon (C) and nitrogen (N) cycles. However, the overall direction and magnitude of such alterations are poorly quantified. Here, 94 experimental studies were synthesized, using a meta-analysis approach, to quantify the changes of 20 variables associated with C and N cycles, including their pools, fluxes, and other related parameters in response to plant invasion. Pool variables showed significant changes in invaded ecosystems relative to native ecosystems, ranging from a 5% increase in root carbon stock to a 133% increase in shoot C stock. Flux variables, such as above-ground net primary production and litter decomposition, increased by 50-120% in invaded ecosystems, compared with native ones. Plant N concentration, soil NH+4 and NO-3 concentrations were 40, 30 and 17% higher in invaded than in native ecosystems, respectively. Increases in plant production and soil N availability indicate that there was positive feedback between plant invasion and C and N cycles in invaded ecosystems. Invasions by woody and N-fixing plants tended to have greater impacts on C and N cycles than those by herbaceous and nonN-fixing plants, respectively. The responses to plant invasion are not different among forests, grasslands, and wetlands. All of these changes suggest that plant invasion profoundly influences ecosystem processes.     

凋落物与单宁酸对森林土壤无机氮的影响

采用室内培养试验,研究了不同凋落物和单宁酸对森林土壤硝态氮和铵态氮的影响.结果表明：凋落物和单宁酸加入均降低了土壤硝态氮和铵态氮含量.杉木凋落物使红壤硝态氮和铵态氮含量分别降低6.1%～25.9%和19.7%～68.6%.杉木凋落物中黄红壤无机氮含量的降幅大于毛竹,对铵态氮的影响极显著.与对照相比,单宁酸处理能显著降低黄红壤中铵态氮含量,单宁酸浓度越高,其降幅越大,至高浓度(HG)时,其降幅达31.9%～57.8%.随着培养时间的延长,低浓度单宁酸处理(HL)中硝态氮含量降幅逐渐增大,第84天达到4.5%;在HG处理下,第7～28天的硝态氮含量增加了10.3%～18.5%,而第56和85天分别降低 23.9%和42.3%.     

植物氮形态利用策略及对外来植物入侵性的影响

氮是影响外来植物入侵性的重要因素之一, 但相关研究多关注土壤氮水平的效应, 较少考虑氮形态的作用。为从土壤氮形态利用的角度阐释外来植物的入侵机制, 本文在植物氮形态利用策略分析的基础上, 综述了外来植物氮形态利用的偏好性及其对入侵性的影响。植物的氮形态利用策略有偏好性和可塑性两种, 这可能与植物对土壤氮形态特性的长期适应有关; 植物不仅可以对土壤氮形态做出响应, 而且还能改造土壤氮形态, 并对改变后的土壤氮形态做出反馈响应。很多外来植物入侵硝态氮占优势的干扰生境, 偏好硝态氮的外来植物与本地植物竞争硝态氮; 而偏好铵态氮的外来植物通过抑制土壤硝化作用, 营造铵态氮环境, 促进自身生长, 同时抑制偏好硝态氮的本地植物生长。然而, 植物氮形态利用策略不是一成不变的, 而是受多种生物和非生物因素共同作用影响的复杂过程, 今后应加强多因素交互作用对外来入侵植物氮形态利用策略的影响及机制研究, 更好地揭示氮形态利用策略, 尤其是氮形态利用的可塑性与外来植物入侵性的关系。     

外来植物入侵对土壤生物多样性和生态系统过程的影响

随着科学家对生态系统地下部分的重视,评价外来植物入侵对土壤生态系统的影响成为当前入侵生态学领域的研究热点之一。本文综述了外来植物入侵对土壤微生物、土壤动物以及土壤碳、氮循环动态影响的研究,并探讨了其影响机制。已有的研究表明,植物入侵对土壤生物多样性及相关生态系统过程的影响均存在不一致的格局,影响机制也是复杂多样的。外来植物与土著植物凋落物的质与量、根系特征、物候等多种生理生态特性的差异可能是形成格局多样性和影响机制复杂性的最主要原因。今后,加强多尺度和多生态系统的比较研究、机制性研究、生物多样性和生态系统过程的整合性研究及土壤生态系统对植物入侵的反馈研究是评价外来植物入侵对土壤生态系统影响的发展趋势。     

Effects of nitrogen addition on soil respiration in shrublands in Mt. Dongling,Beijing, China

Aims Soil respiration from terrestrial ecosystems is an important component of terrestrial carbon budgets. Compared to forests, natural or semi-natural shrublands are mostly distributed in nutrient-poor sites, and usually considered to be relatively vulnerable to environmental changes. Increased nitrogen (N) input to ecosystems may remarkably influence soil respiration in shrublands. So far the effects of N deposition on shrubland soil respiration are poorly understood. The aim of this study is to investigate the soil respiration of Vitex negundo var. heterophylla and Spiraea salicifolia shrublands and their response to N deposition. Methods We carried out a N enrichment experiment in V. negundo var. heterophylla and S. salicifolia shrublands in Mt. Dongling, Beijing, with four N addition levels (N₀, control, 0; N₁, low N, 20 kg N·hm^-2·a^-1; N₂, medium N, 50 kg N·hm^-2·a^-1 and N₃, high N, 100 kg N·hm^-2·a^-1). Respiration was measured from 2012-2013 within all treatments.Important findings Under natural conditions, annual total and heterotrophic respiration were 5.91 and 4.23, 5.76 and 3.53 t C·hm^-2·a^-1 for the V. negundo var. heterophylla and S. salicifolia shrublands, respectively and both were not affected by short-term N addition. In both shrubland types, soil respiration rate exhibited significant exponential relationships with soil temperature. Temperature sensitivity (Q₁₀) of total soil respiration in V. negundo var. heterophylla and S. salicifolia shrublands ranged from 1.44 to 1.58 and 1.43 to 1.98, and Q₁₀ of heterotrophic soil respiration ranged from 1.38 to 2.11 and 1.49 to 1.88, respectively. Short-term N addition decreased only autotrophic respiration rate during the growing season, but had no significant effects on total and heterotrophic soil respiration in V. negundo var. heterophylla shrubland. In contrast, N addition enhanced the heterotrophic soil respiration rate and did not influence autotrophic and total soil respiration in S. salicifolia shrubland.     

植物外来种对土壤理化特性的影响

植物外来种对土壤特性可产生深刻的影响。植物外来种可影响土壤的温度、湿度、土壤侵蚀等土壤物理特性 ;同样会影响土壤的含氮量、有机质、金属元素等化学特性。植物外来种对土壤特性的影响是十分复杂的 ,在不同的环境里同一植物外来种可产生不同的影响。总的来说 ,植物外来种对土壤特性的影响有正面、中性和负面 3种效应     

外来植物对陆地生态系统氮循环的影响途径

外来植物的引种和入侵已成为一个全球性的重要问题.许多外来植物不仅可以改变陆地生态系统的氮输入、输出,而且还可以通过改变氮素吸收、再利用,凋落物质量,土壤环境,土壤生物等因子影响陆地生态系统内都氮循环.在概述陆地生态系统氮循环基础上,系统综述了外来植物对陆地生态系统氮循环的影响方式和途径以及可能造成的生态后果,并对将来研究方向进行了展望:应更多考虑外来植物影响机制的复杂性、不同养分元素循环的相互作用和新技术手段的应用.     

生物炭对黄壤中氮淋溶影响:室内土柱模拟

土壤氮素的淋失作用不仅造成土壤营养元素的损失,而且对河流和湖泊等环境水体的富营养化具有重要贡献.采用土柱室内模拟方法,通过模拟降雨淋滤,研究了生物炭对土壤淋溶液体积、pH和电导率以及NH4+-N和NO3--N淋溶的影响.试验中所用的生物炭是以桉树木屑为原料制成,分别按照炭土质量比1％、2％、4％、10％施用于土壤中.结果显示,与对照相比,向土壤添加10％、4％、2％、1％生物炭分别减少土壤水分损失14％、0.03％、0.02％和0.01％;随生物炭添加量增加,淋溶液的pH和电导率也逐渐增加;土壤生物炭添加量为10％、4％、2％时,NH4+-N淋溶量分别增加235％、28.1％、31.6％,NO3--N淋溶量分别增加4.2％、14.5％、25.6％;但生物炭添加量为1％的土柱NH4+-N淋溶量减少15.8％,NO3--N淋溶量减少19.2％.本研究表明,桉树生物炭对土壤氮淋溶与其施用量有关,1％施用量能减少氮淋溶,过量施用将增加氮淋溶,这种作用是否与生物炭种类有关有待进一步研究.     

半干旱地区不同地膜覆盖时期对土壤氮素有效性的影响

在年降水量415mm的半干旱地区黄绵土上,以春小麦为供试作物进行大田试验,研究地膜覆盖(包括不覆膜、播种后覆膜30d、覆膜60d和全程覆膜)对土壤水分、温度和氮素有效性的影响.结果表明,覆膜对2m土层贮水量基本没有影响,能显著提高0～20cm土层的含水量;覆膜对5cm处土壤温度的影响呈"U”型变化,即在作物生长前期和后期影响显著,中期影响较小;覆膜能增加土壤呼吸和有机氮的矿化,因而显著影响土壤剖面中NO-3-N的累积表现为在收获时覆膜30d和60d处理剖面中NO-3-N的累积明显下降,而全程覆膜处理剖面中NO-3-N的累积显著增加,在覆膜的基础上施用氮肥,这种作用会更加突出.显然全程覆膜易造成有机质的大量矿化和NO-3-N的淋溶损失.     

Effects of dissolved organic matter from different plant sources on soil enzyme activities in subtropical forests

探究不同植物来源可溶性有机质(DOM)进入土壤后对酶活性的影响, 可以为降水淋溶下亚热带地区不同森林生态系统土壤碳循环提供科学依据。该研究提取杉木(Cunninghamia lanceolata)、木荷(Schima superba)和楠木(Phoebe zherman) 3种植物鲜叶中的DOM分别输入杉木人工林土壤中, 以等量的去离子水添加为对照, 进行25天的室内培养。培养结束后测定土壤理化性质、微生物生物量和酶活性等指标。结果表明: 与对照处理(CT)相比, 添加3种叶片DOM后, 土壤总有机碳(SOC)、总氮(TN)含量和碳氮比均无显著变化。杉木叶片DOM添加处理(CL)的TN含量显著低于木荷叶片DOM添加处理(SL)和楠木叶片DOM添加处理(PL), 碳氮比显著高于SL和PL。3种叶片DOM输入整体上提高了土壤溶解有机碳(DOC)和溶解有机氮(DON)的含量。叶片DOM输入后土壤微生物生物量碳(MBC)含量无显著变化, 然而CL和SL的土壤微生物生物量氮(MBN)含量分别比CT降低了50.9%和51.1%, PL的MBN含量比CT提高了54.0%。与CT相比, 不同植物来源DOM输入后, β-葡萄糖苷酶(βG)、纤维素水解酶(CBH)和过氧化物酶(PEO) 3种酶活性均显著上升, 而多酚氧化酶(PPO)活性则显著下降; 此外, βG和CBH活性均表现出CL > SL > PL的特征。相关性分析的结果表明, 添加叶片DOM 3种处理的SOC、TN、MBN含量和βG、CBH活性都与所输入DOM的DOC含量和腐殖化指数(HIX)显著相关, 此外, 土壤MBN含量和PPO活性与输入叶片DOM的pH呈正相关关系。冗余分析(RDA)结果表明, 叶片DOM输入后引起土壤酶活性变化的关键因子是DON和DOC含量。总体来说, 不同植物来源DOM性质的差异会影响土壤碳循环水解酶的活性, 而叶片DOM输入后增加了土壤碳和氮的有效性, 引起4种碳循环酶的不同响应。     

氮沉降对草地土壤及团聚体元素有效性的影响

深入理解土壤及团聚体元素有效性对氮沉降的响应机制,是研究全球变化背景下土壤养分供应及生态系统结构和功能的关键.本研究综合评述了草地生态系统土壤表土及团聚体内元素分布及其对氮沉降的响应机制.总体而言,草地表土内碳、氮、磷、硫有效性研究较多,且研究结果因氮添加形态、添加时间及生态系统类型而异.氮沉降通过改变碳、氮、磷、硫等生源要素的转化过程及其在土壤团聚体内的再分配,而影响这些元素的生物有效性.然而,氮沉降影响草地土壤交换性盐基及有效态微量元素的研究较少.氮沉降促进土壤酸化,导致各团聚体内钙、镁差异性流失,其中大粒径团聚体内盐基元素更易流失;酸化还有助于提高团聚体内铁、锰、铜、锌有效性.土壤小粒径团聚体内的养分对外界环境变化响应不敏感.当前研究的不足之处在于,较少关注氮沉降对土壤团聚作用及团聚体元素有效性的影响.今后应加强团聚体元素有效性与土壤酶活性耦合变化关系的研究,并分析氮沉降背景下土壤物理结构和化学组成的变化对植物群落的反馈作用.     

植物外来种入侵及其对生态系统的影响

对植物外来种的入侵及生态系统的影响进行综述与分析,植物入侵多种因子的影响,可分为外因和内因两类,植物外来种对生态系统的影响主要体现在生产力,土壤营养,水分,干扰体制,群落的结构和动态等方面,在管理外来种时,需对外来种的特性和影响因子进行系统的观察研究,采用机械法,化学方法和生物控制法等综合办法控制植物的入侵,引进植物引来种时,要对引进种的行为特性进行了调查研究,注意其安全性。     

Current plant diversity but not its soil legacy influences exotic plant invasion

植物多样性而非其土壤遗留效应影响外来植物入侵 植物多样性可以影响外来植物入侵,然而植物多样性的土壤遗留效应是否能够影响外来植物入侵目前仍不清楚。植物多样性能够改变土壤微生物群落和土壤理化性质,这种遗留效应可能会对该土壤中外来植物的生长产生影响。因此,我们假设植物多样性的土壤遗留效应会影响外来植物的入侵。为了检验该假说,我们开展了一个两阶段的植物-土壤反馈实验。在土壤驯化阶段,我们将12个植物物种(4种禾草植物、3种豆科植物和5种杂类草植物)分别单独种植,或者随机选择8个物种(包含3个功能型)混合种植在土壤中。在反馈阶段,我们将入侵植物三叶鬼针草(Bidens pilosa)分别与本地禾草荩草(Arthraxon hispidus)、本地杂类草翅果菊(Pterocypsela indica)或者同时与荩草和翅果菊种植在被驯化过的土壤中。研 究结果显示,三叶鬼针草相对于其本地竞争植物的生长取决于驯化植物和竞争植物物种的功能型。驯化植物的多样性对三叶鬼针草与其本地竞争植物之间的生长差异没有显著影响。然而,随着本地竞争植物物种多样性的增加,三叶鬼针草相对于其本地竞争植物的生长显著降低。这些结果表明,当前的植物多样性可以通过增加入侵植物和本地植物之间的生长不平衡性来减少外来植物的入侵。但是,植物多样性的土壤遗留效应对外来植物入侵的影响可能很小。