106 resultados para 4-oxo-3-aza-bicyclo[3.1.0]hexane
Resumo:
以 GPS为辅助 ,在保安湖主体湖和桥墩湖进行沉水植物调查。将野外调查数据构建 GIS数据库 ,基于 GIS软件平台 ,运用 Kringing插值法对保安湖沉水植物分布进行模拟。模拟结果清楚地显示出调查时保安湖沉水植物及 4优势种 (金鱼藻 Ceratophyllum demersum L.、穗状狐尾藻 Myriophyllum spicatum L .、微齿眼子菜 Potamogeton maackianus A.Benn.及苦草 Vallisneria spiralis L.)分别在湖中的分布情况。统
Resumo:
萼花臂尾轮虫的交配行为大致可分为 5个阶段。除雌雄性比为 1∶ 2和 1∶ 3时混交雌体的受精率为 1 0 0 %外 ,其余性比下混交雌体的受精率皆无显著的差异。可受精的混交雌体百分率和具受精能力的雄体百分率皆随年龄的增大而下降。所有的混交雌体在出生后的 4 h内均易于受精 ;以后随着龄长 ( X,h)的增加 ,可受精的混交雌体百分率 ( Y,% )呈非线性下降 :Y=1 66.6386-1 7.81 3X+0 .4 837X2。当龄长达 1 8h时 ,所有的混交雌体皆不易受精。雄体在出生后的 8h内 ,
Resumo:
The photoluminescence of four epitaxial ZnS: Te samples with Te concentration from 0.5% to 3.1% was investigated at different temperature and ambient pressure. Two well-known emission bands related to the isolated Te-1 and Te-2 pair isoelectronic centers were observed for the samples with Te concentrations of 0.5% and 0.65%. For the samples with Te concentrations of 1.4% and 3.1%, only was the Te-2-related peak observed. The pressure behaviors of these emission bands, were studied at 15 K. The Te-1 -related band has faster pressure shift to higher energy than ZnS band gap. On the other hand, the pressure coefficient of Te-2 -related bands is smaller than that of the ZnS band gap. According to a Koster-Slater model, we found that the increase of the density bandwidth of the valence band with pressure is the main reason for the faster shift of the Te-1 centers, while the relatively large difference in the pressure behavior of the Te-1 and Te-2 centers is mainly due to the difference in the pressure-induced enhancement of the impurity potential on Te-1 and Te-2 centers.
Resumo:
ZnS:Te epilayers with Te concentration from 0.5% to 3.1% were studied by photoluminescence under hydrostatic pressure at 15 K. Two emission bands related to the isolated Te-1 and Te-2 pair isoelectronic centers were observed in the samples with Te concentrations of 0.5% and 0.65%. For the samples with Te concentrations of 1.4% and 3.1%, only the Te-2-related peak was observed. The pressure coefficients of all the Te-1-related bands were found to be unexpectedly much larger than that of the ZnS band gap. The pressure coefficients for all the Te-2-related bands are, however, rather smaller than that of ZnS band gap as usually observed. Analysis based on a Koster-Slater model indicates that an increase of the valence bandwidth with pressure is the main reason for the faster pressure shift of the Te-1 centers, and the huge difference in the pressure behavior of the Te-1 and Te-2 centers is due mainly to the difference in the pressure-induced enhancement of the impurity potential on the Te-1 and Te-2 centers. (C) 2002 American Institute of Physics.
Resumo:
本文提出了一个三段热化学循环分解水制氢和氧的方法以及将此三段热化学法改为二段热化学循环分解水制氢和氧的新方法。本三段热化学法由下列三个反应组成:{Cr_2O_3+6KoH=2K_3CrO_4+H_2O+2H_2 6K_3CrO_4+5H_2O=Cr_2O_3+4K_2CrO_4+10KOH 4K_2CrO_4+4KOH=4K_3CrO_4+2H_2O+O_2本二段热化学法由下列二个反应组成:{Cr_2O_3+6KOH=2K_3CrO_4+H_2O+2H_2 2K_3CrO_4+3H_2O=Cr_2O_3+6KOH+O_2上面的三步法和二步法分别通过正交试验,讨论了影响各个反应产率的主要因素,利用最小二乘法在计算机上对试验结果进行了回归分析和方差分析,得到了下面几个数学模型。利用x-光射线粉末衍射对反应产物进行了测定,提出了有关反应机理,并对这两种方法的特点给予了评价。三段法的数学模型:(1)y=-0.8295+1.7681*10~(-6)T~2+7.4750*10~(-2)t+0.2753n (2)y=0.2730+0.5301t+3.2600*10~(-4)V (3)y=-0.1785+2.6999*10~(-4)T+3.5259*10~(-3)t~2+0.3370n二段法的数学模型:(1)y=-0.8295+1.7681*10~(-6)T~2+7.4750*10~(-2)t+0.2753n (2)y=-0.1670+4.3999*10~(-4)T+7.2500*10~(-3)t+1.5599*10~(-3)V式中,T:反应温度(℃)V:水的通水量(ml)n:氢氧化钾的实际加入量与其理论量的比y:转化率t:反应时间(hr)
Resumo:
林窗是森林中经常发生的重要中小尺度干扰,在森林天然更新中起着重要作用。灌木和草本植物通过与乔木幼苗竞争林窗资源(尤其是光)而影响林窗树种更新,因此,研究林窗光环境时空特征及其与下层植被关系对揭示林窗树种更新机制具有重要意义。然而,林窗光环境的时空异质性及有效测量方法的缺乏导致这方面研究很少。本研究提出了林窗立体结构的相片测量法;基于林窗立体结构、坡度和坡向改进了目前广泛用于估测林窗光环境的林窗光指数(gap light index, GLI)模型,并提出了林窗内任意位置最大光照时长(potential sunshine duration, PSD)的计算方法;采用改进的GLI和PSD分析了东北次生林3个不同大小林窗(110,270,510 m2)及其对应的9个模拟林窗中2007年光环境的时空特征;通过在12个人工林窗中连续3年的植被调查,研究了林窗形成后前3年下层木本和草本植物对4个光强梯度的响应,主要结论如下: 1. 林窗立体结构和光环境的测量方法:1) 等角椭圆扇形法计算的林窗面积比目前使用较多的等角多边形法具有更高的精度;2) 半球面影像法可以测量林窗面积和形状,且精度较高;3) 双半球面影像法不仅可以测量林窗面积、形状,还可以测量任意方位林窗边缘木高度;4) 改进的GLI可以快速、精确计算林窗任意位置的直射光和散射光;5) PSD可用于分析林窗光照强度时空特征。 2. 东北次生林林窗光环境时空特征:1) 水平空间结构(地面层):光环境空间异质性高,最大值位于林窗北部,坡向对光分布格局影响大而对光强影响小,光强随林窗面积的增大和边缘木高度的降低而增加;2) 垂直空间结构(林窗南北轴):不同高度层光强最大值均位于林窗南北轴中心偏北,南北轴距地面越高光强最大值则越靠近轴中心;光强随距地面高度下降而衰减,最大衰退速率点位于轴中心偏南,靠近该点光强衰退线呈指数形,远离该点则趋于直线形;3) 光成分特征(地面层南北轴):南坡林窗整个南北轴上直射光大于散射光,北坡模拟林窗南半轴散射光大于直射光,而北半轴相反;南坡林窗中直射光的均值及其变化范围都比其对应的北坡模拟林窗大,然而,坡向对散射光影响不大;南坡林窗和北坡模拟林窗北半轴的全光和直射光均比南半轴大,但散射光没有这种显著的规律;4) 时间特征:不同月份PSD在相同大小林窗中分布格局十分相似,6月份林窗中被光照射面积和PSD均值最大,而10月份最小;各月PSD在南北轴上从南到北逐渐增加,在东西轴上自西向东缓慢增加。 3. 林窗早期下层植被对光强梯度的响应:1) 木本植物物种丰富度随光照强度的增加而增高,且在林窗形成后的第2和3年均存在显著相关性;2) DCA排序第一轴表明,木本植物物种组成仅第1年在4个光强梯度间存在显著差异,而在各年间存在显著差异;草本植物物种组成在4个光强梯度上存在显著差异,但在各年间不存在显著差异;3) 木本植物生物体积(biovolume)随光强梯度升高而增加,而植株密度不存在显著变化;生物体积逐年增加,平均年增长率为20.3%,植株密度逐年下降,平均年减少率为30.0%;4) 草本层盖度和高度在4个光强梯度间均不存在显著差异,但在林窗形成后的第2、3年均显著比第1年大。
Resumo:
土壤可溶性有机物质(Dissolved organic matter,DOM)作为土壤有机质的活性组分,在陆地生态系统物质循环中扮演非常重要的角色。土壤DOM的主要成分可溶性有机碳(Dissolved organic carbon,DOC)和氮(Dissolved organic nitrogen,DON)参与C、N循环过程。为深入揭示全球C、N循环过程机制,在未开展DOC和DON的地区进行相关研究是有必要的。森林土壤(包括枯枝落叶层)DOC、DON动态及调控机理的研究是目前国际上森林生态系统C、N循环研究热点之一。本研究立足于暖温带岷江上游茂县地区人工林植被,对土壤DOC和DON的库容量,季节动态及其与其它养分之间的关系进行了系统研究,旨在了解DOC和DON在该区生态系统中的重要作用,并探讨作为DOM主要来源的叶凋落物对DOC和DON的动态影响,研究有助于更加详细地了解该区生态系统C和N循环过程。本论文主要研究结论如下: 1研究了岷江上游地区两大主要土壤类型(棕壤和褐土)不同植物群落下土壤的DOC和DON含量及特征,结果表明:DOC和DON在两种土壤类型中均有库容量存在,DOC在0-10cm和10-20cm土层的含量幅度分别111.96~159.95 mg kg-1和69.02~100.84 mg kg-1。DON在0-10cm和10-20cm土层的含量幅度分别11.88~23.08 mg kg-1和4.70~10.77 mg kg-1。游离氨基酸在0-10cm和10-20cm土层的含量幅度分别0.84~1.66 mg kg-1和0.39~0.73 mg kg-1。DOC、DON与土壤中的一些养分因子表现出了显著的相关关系,共同反映了土壤的状况和质量,在该区开展DOC和DON的系统研究是有必要的。 2 对油松与连香树林地土壤DOC、DON以及其它化学指标的季节动态进行了研究,结果表明:油松与连香树林地土壤DOC和DON的季节动态变化表现了类似的规律,DOC和DON的含量均以秋季最高。DOC和DON的季节动态变化主要受凋落物生物因素的影响,但其微生物活力的生物因素以及降雨、温度等非生物因素也是控制土壤DOC和DON含量的重要因素。土壤DON在土壤中的行为不同于矿质氮,其季节动态不同于NO3--N和NH4+-N的季节动态,在研究N循环过程中,应考虑DON的变化情况。 3 对油松与连香树林地分解层和表层土壤(0-10cm)氨基酸周转动态进行了研究,结果表明:油松林地和连香树林地均以分解层的氨基酸含量高于矿质表层土壤的含量。每个取样时期,油松林地内各层次的氨基酸含量高于连香树林地内相应层次的含量。两林地各层次无机氮含量均超过了氨基酸的含量,并且室内培养30天后无机N的含量仍然高于氨基酸的含量,所以可以认为该区立地条件下无论是在有机分解层还是矿质土层植物吸收利用的氮素仍是以无机N为主。 4 松林下松针凋落物易于累积,这与松针凋落物分解缓慢有关,从而导致松林内养分周转缓慢。通过用不同性质凋落物和灌丛地土壤构建微生态系统,比较油松、辐射松、连香树、灌丛虎榛子凋落物分解对C、N循环过程的影响,结果显示油松和辐射松针叶凋落物比连香树、虎榛子凋落物分解更慢,减缓了养分循环过程。然而将针叶凋落物与阔叶凋落物混合后,油松和辐射松针叶凋落物的分解加快,C、N元素的循环过程也加速。此结果表明在松林内维持具有高质量凋落物的灌丛植被或在松林内栽植一些阔叶树种如连香树对维持和增进松树人工林的土壤肥力有重大的作用。室内培养的结果还显示添加凋落物后土壤DOC和DON的含量显著增加,表明凋落物是土壤DOM的直接来源。然而不同物种凋落物处理下土壤DOC和DON的含量有所不同,并随时间发生改变。混合凋落物处理下土壤DOC和DON的含量均高于松针凋落物单独处理下土壤DOC和DON的含量。DON是一个主要的水溶性N库,随时间的变化趋势与无机N的变化趋势不同,在土壤N循环过程中起到了中间N库的作用。 As a labile fraction of soil organic matter, dissolved organic matter (DOM) plays a very important role in material cycling of terrestrial ecosystem. The turnover of DOM is now being considered as main components in nutrient cycling. DOM mainly includes dissolved organic carbon (DOC), -nitrogen (DON), -phosphorous (DOP) and –sulfur (DOS). Among these constituents, DOC and DON directly participate in C and N cycling. It is essential to study DOC and DON dynamics and their controlling factors in the areas where no related study has ever been carried out. Study about them can provide data supports on understanding the mechanism of the global C and N cycling. DOC and DON dynamics and their controlling factors have been focused on in the research of C and N cycling of forest ecosystems. Based on forest plantations of Maoxian, Minjiang River in warm temperate zone, soil DOC and DON pool size, their seasonal dynamics, and the correlation between DOC, DON and other nutrients were studied in order to understand the importance of DOC and DON in the study area. Soil DOC and DON dynamics induced by leaf litter decomposition were also studied. The study contributed to comprehensively understanding C and N cycling processes and providing baseline data for including DOC and DON into the indices system of evaluating nutrient conditions. The results were as follows: 1 Several different plant communities under brown soil and Cinnamon soil were chosen as sampling plots. The contents and features of soil DOC and DON were evaluated. The results showed that DOC and DON were present under the two soil types. DOC contents in the top soil (0-10 cm) and the subsoil (10-20 cm) respectively varied from 111.96 mg kg-1to 159.95 mg kg-1, and 69.02 mg kg-1 to 100.84 mg kg-1. DON contents in the top soil (0-10 cm) and the subsoil (10-20 cm) respectively varied from 11.88 mg kg-1to 23.08 mg kg-1, and 4.70 mg kg-1 to 10.77 mg kg-1. Free amino acid contents in the top soil (0-10 cm) and the subsoil (10-20 cm) respectively varied from 0.84 mg kg-1to 1.66 mg kg-1, and 0.39 mg kg-1 to 0.73 mg kg-1. Significant correlations were found between DOC, DON and some nutrient indices, which together reflected soil condition and quality. It was hence essential to study DOC and DON in the study area. 2 Seasonal dynamics of DOC, DON, inorganic N, microbial biomass C and N were studied under Pinus tabulaeformis and Cercidiphyllum japonicum plantation. The results indicated that seasonal dynamics of soil DOC and DON under the two plantations performed similar change pattern, with the highest values in autumn. The seasonal dynamics of soil DOC and DON were mainly influenced by the litterfall. However, biotic factors such as soil microbial activities and abiotic factors such as precipitation and temperature also controlled the dynamics of soil DOC and DON. The seasonal dynamic of DON was different from that of NO3--N and NH4+-N, which showed that the behavioral differences between DON and inorganic nitrogen. And hence, it was proposed to include DON into soil N cycling in the study area. 3 Amino acid dynamics in Oa and topsoil (0-10 cm) under P. tabulaeformis and C. japonicum plantation were studied. The results showed that amino acid content in Oa was significantly higher than that in mineral soil. At each sampling time, significantly higher amino acid contents were found in P. tabulaeformis plantation than in C. japonicum plantation. The content of inorganic nitrogen was much higher than the content of amino acid in each sampling layer at each sampling time. After a 30-days laboratory incubation the content of amino acid was still lower than the content of inorganic nitrogen. The results implicated that the form of N absorbed by plants in these study sites were mainly inorganic nitrogen. 4 Usually needle litter is more resistant to decomposition, which leads to needle litter accumulation in pure coniferous stands and slows down the rate of nutrient circulation. By constructing microcosms with local shrubland soil and containing the four single-species (P. tabulaeformis, P. radiata, C. japonicum, Ostryopsis davidiana) litters, the decomposition rates and related C and N dynamics of needle litters and broadleaved litters during the early stage were compared. The results showed that the decomposition rates of pine needles were lower than those of broadleaved litters, which descended C and N cycling processes. However, the presence of C. japonicum or O. davidiana litter into pine needles increased the decomposition rates of pine needles and also dramatically promoted C and N cycling processes. It should be appropriate for plantation managers to consider C. japonicum as an ameliorative species or remain O. davidiana in pine plantations to improve soil conditions and help maintain soil fertility. The laboratory incubation still showed that DOC and DON contents in all litter-amended treatments were significantly higher than no litter-amended treatment, which proved that litter could be a direct source of DOM in soils. Different species litters induced different soil DOC and DON contents, which correspondingly changed over time. DOC and DON contents in mixed litter treatments were higher than those in pine needle litter treatments. As a major soluble N pool, DON developed a different changing pattern over time compared with inorganic N and played a role of interim N pool in soil N cycling.
Resumo:
植物功能生态学研究不仅提供了植物生理生态学与生态系统生态学的连接,还为植物种群生活史对策研究提供了材料。Westoby 等 (2002) 提出了利用植物功能性状变量的主导维度来确定和量化植物生活史的生态适应策略。在他们所提出四个主导维度中,叶大小-小枝大小是研究相对较少的一维;其内部各组分的关系、对环境的响应,以及与其它重要维度的关系,目前的理解非常有限。 本研究以贡嘎山不同海拔不同功能群物种为研究对象,采用种间比较和系统发生独立性比较等研究方法,系统研究了植物的功能特征及其相关性在不同生境及不同功能群间的差异,旨在分析不同功能群物种的叶大小-小枝大小的成本和收益。其研究结果将有助于我们理解植物生活史对策的进化,进而理解物种共存和维持物种多样性的机制。主要研究结果如下: 1. 叶大小-小枝大小关系 小枝茎横截面积与单叶面积和总叶面积均呈异速生长关系,即总叶面积和单叶面积的增加比茎横截面积的增加速度快。但是,总叶面积和叶片干重的增加却基本上与小枝茎干重的增加等速。系统发生独立性比较研究的结果与此相一致。表明,在某一给定的茎投入时,至少大叶大枝物种不比小叶小枝物种在支撑叶面积和叶片干重方面具有优势。同时,在某一给定的小枝茎投入时,常绿阔叶物种比落叶阔叶物种支撑更少的叶面积。在茎干重与总叶面积的关系中,落叶复叶物种比落叶单叶物种具有更高的y轴截距,表明复叶物种比单叶物种在展叶面积方面更有效。复叶物种与单叶物种相比,通常具有较大的叶大小和小枝大小。 2. 叶大小-叶数量关系 叶大小与数量间在不同的叶片习性、不同的叶片形态以及不同的生境类型的物种间均存在稳定的负的等速生长关系,且这种关系在系统发生独立性比较时依然成立。然而,在某一给定的出叶强度 (单位小枝的叶数量) 时,常绿阔叶物种比落叶物种具有更小的叶面积。而在给定体积基础上的出叶强度时,落叶复叶物种的叶面积显著大于落叶单叶物种,且复叶物种比单叶物种具有更大的叶大小和更小的出叶强度。但是,叶大小与数量间的关系在不同的海拔间并没有显著的差异。 3. 小枝大小-总叶面积关系 在不同的生活型或不同的生境下,小枝上总叶面积与茎干重和小枝干重均呈正的异速生长关系,且斜率显著小于1.0,表明小枝上总叶面积的增加都不能赶上小枝及茎大小的增加。这种“收益递减”表明随着小枝干重的增加,光截取的收益递减。此外,叶面积比 (总叶面积与小枝干重的比值) 与单叶干重呈显著负相关关系,系统发生独立性比较的结果与此相一致。根据以上结果,可以推测,大叶的物种在质量较好的生境中出现,而群落内部小枝茎的寿命较长的物种可以拥有较大的叶片。 4. 叶片色素浓度-LMA关系 随着海拔的升高,阔叶木本植物和草本植物的叶片色素浓度减少,叶绿素a/b和类胡萝卜素/叶绿素比值以及比叶重 (LMA) 增加。然而,在草本植物中的色素浓度、色素比值和LMA的变化比阔叶木本植物的更明显。同时,LMA与叶片色素浓度呈负相关关系,但是在落叶物种中的LMA对色素浓度的影响比常绿阔叶物种更强烈。总之,草本植物的叶片特征对海拔梯度的变化似乎比木本植物更敏感,LMA对叶片色素的保护作用在落叶物种中比在常绿阔叶物种显得更重要。这些结果表明不同生活型物种可能采取不同的保护机制来降低叶绿体器官的损伤和增加他们的碳获取能力。 Studies on plant functional ecology not only bridge plant eco-physiology and ecosystem functioning, but also enrich plant population biology. As pointed out by Westoby et al (2002), plant life history strategies can be identified and quantified by four leading dimensions of variations in plant functional traits, i.e., seed size/output, leaf mass per area and leaf life span, plant height, and leaf size-twig size. Compared to the other dimensions, the cost/benefit of the leaf size-twig size spectrum has scarcely been analyzed in relation to environmental gradients and life form types, and the adaptive significance of this spectrum is not fully understood. In the present study, the relationships between functional traits of plant twigs are determined for the species with different life forms along an altitudinal gradient of Gongga Mountain with both cross-species analysis and evolutionary divergence analysis. The primary objective of this study is to examine the cost/benefit of leaf size-twig size in plants. The study results are supposed to provide insights into the understanding of the mechanism of species coexistences. The results are shown in the following. 1. The relationship between leaf size and twig size Twig cross-sectional area allometrically scaled with both individual leaf area and total leaf area supported by the twigs. However, the increase in total lamina mass/area was generally proportional to the increase in stem mass. These correlations between trait variations were significant in both interspecies analysis and phylogenetically independent comparison (PIC) analysis, which indicated that thick-twigged/large-leaved species, at least, do not have an advantage in supporting leaf/lamina area and lamina mass for the same twig stem investment than thin-twigged/ small-leaved species. Meanwhile, the evergreen broad-leaved species supported a smaller leaf area for the same twig stem investment in terms of both cross-sectional area and stem mass than the deciduous species. The deciduous compound-leaved species have a higher y-intercept in the scaling relationship of twig stem mass versus total leaf area than the deciduous simple-leaved species, indicating that compound-leaved species were more efficient in displaying leaf area. The compound-leaved species were larger in both leaf size and twig size than their counterpart in the present study. 2. The relationship between leaf size and leaf number Significantly negative and isometric scaling relationships between leaf size and leafing intensity (leaf number per twig mass or volume) were found to be consistently conserved across species independent of leaf habit, leaf form and habitat type. The negative correlations between leaf size and leafing intensity were also observed across correlated evolutionary divergences. However, leaf area was smaller in the evergreen broad-leaved species at a given leafing intensity than in the deciduous species. The deciduous compound-leaved deciduous species were higher in leaf area than deciduous simple-laved species at a given volume-based leafing intensity. Moreover, the compound-leaved deciduous species were larger in leaf size but smaller in leafing intensity than their simple counterparts. No significant difference was found in the scaling relationships between altitudes. 3. The relationship between twig size and total leaf area Leaf area was found to scale positively and allometrically with both stem and twig mass (stem mass plus leaf mass) with slopes significantly smaller than 1.0, independent of life form and habitat type, indicating that the increase in total leaf area fails to keep pace with increasing twig size and stem size. This ‘diminishing returns’ suggests that the benefit of light intercept decreased with increasing twig mass. Moreover, the leaf area ratio (the ratio of total leaf area to stem or twig mass) correlated negatively with individual leaf mass. The results of PIC were consistent with the correlations. According to the results, it is speculated that large-leaved species may be favored when habitat is good and when stem longevity are long within community. 4. The relationship between leaf pigment concentrations and leaf mass per area With increasing altitude, the concentrations of pigments decreased, but the ratios of chlorophyll a/b and carotenoid/chlorophyll, and LMA increased, in both the broad-leaved woody species and herbaceous species groups. However, the changes in the pigment concentrations, ratios and LMA were more profound in the herbaceous species than in the woody species. In addition, pigment concentrations were negatively correlated with LMA in each life form type and in the pooled dataset. However, the LMA effect on leaf pigment concentrations was more profound in the deciduous species than in the evergreen braode-leaved species. In general, herbaceous species seemed more sensitive to the increasing altitude compared to woody species, and LMA seemed to be a more important mechanism for protecting leaf pigments in deciduous species than in evergreen broad-leaved species. These results suggested that the species with different life forms may employ different protective mechanisms to decrease the chloroplast apparatus damage and increase their carbon gain.
Resumo:
通过对牛蒡(A rctium lapp a L.)不同外植体、不同激素配比的比较研究,建立了牛蒡离体培养高效植株再生体系.牛蒡子叶与下胚轴切段在含2.0 m g/L 2,4-D和0.5~2.0 m g/L BA的M S培养基中愈伤组织诱导率可以达到87%~100%;在1.0~3.0 m g/L NAA和0.5~2.0 m g/L BA的M S培养基上通过愈伤组织间接分化或外植体直接分化形成不定芽,其中愈伤组织分化率可达100%;下胚轴的分化率明显高于子叶,在1.0 m g/L NAA和1.0 m g/L BA的M S培养基上下胚轴直接分化率达77.3%.组织学观察发现牛蒡再生有器官发生和体细胞胚发生两种途径.将生长状态良好的不定芽转至含1.0 m g/L IBA和1.0 m g/L NAA的1/2 M S培养基上生根,移栽,成活率达到93.3%.从诱导愈伤组织到组培苗在珍珠岩中过渡成活,大约需要13周.组培苗次年开花并结实,生长形态特征正常.
Resumo:
在 3 3 .4MeV/u17N束轰击197Au靶产生的反应中 ,利用放置于不同角度组合的 1 7个中子探测器 ( 4°— 83°)和 1 4个半导体望远镜 ( 2 .3°— 9.0°)对反应产物碎片与中子进行了符合测量 .经对所得实验角分布积分得到Z =3— 6元素的同位素产额分布 .在参加者 -旁观者模型框架下 ,采用17N原子核内部的不同密度分布计算了同位素产额分布并与实验数据做比较
Resumo:
We investigate the S-1(0) neutron and proton superfluidity in isospin-asymmetric nuclear matter. We have concentrated on the isospin dependence of the pairing gaps and the effect of a microscopic three-body force. It is found that as the isospin asymmetry goes higher, the neutron S-1(0) superfluid phase shrinks gradually to a smaller density domain, whereas the proton one extends rapidly to a much wider density domain. The three-body force turns out to weaken the neutron S-1(0) superfluidity slightly, but it suppresses strongly the proton S-1(0) superfluidity at high densities in nuclear matter with large isospin asymmetry.
Resumo:
不同氮营养水平对高油玉米吉油一号籽粒产量、蛋白质、氨基酸和油脂的影响的研究表明,不同氮营养水平对高油玉米籽粒产量影响较大,施氮增产10.5%~22.9%。在本试验条件下的经济最佳施氮(N)量为180.3 kg·ha-1。不同施氮水平较不施氮均能明显增加高油玉米籽粒蛋白质及其组分中醇溶蛋白和谷蛋白含量,分别增加7.1%~13.3%(平均10.6%)、22.1%~39.1%(平均29.9%)和25.0%~40.7%(平均35.0%),其中施氮175 kg·ha-1时蛋白质含量最高(10.75%),施氮125 kg·ha-1时蛋白质品质相对较好(谷醇比相对较高,醇溶蛋白占蛋白质比例相对较低)。不同施氮水平较不施氮均能明显增加高油玉米籽粒氨基酸总量和必需氨基酸总量,分别增加11.9%~20.3%(平均17.3%)和12.4%~20.4%(平均17.1%),其中施氮175 kg·ha-1时氨基酸总量(11.50%)和必需氨基酸总量(4.19%)均相对较高。适量施氮能增加高油玉米籽粒油脂含量及不饱和脂肪酸、亚油酸和油酸含量,其中施氮175~225 kg·ha-1时籽粒油分、不饱和脂肪酸、亚油酸和油酸含量均较高,较不施氮分别增加7.0%~7.5%,7.4%~8.3%、7.0%~8.5%和8.1%~8.4%,而过量施氮会明显降低籽粒油分、不饱和脂肪酸、亚油酸和油酸含量。
Resumo:
对青藏高原黄河源区不同退化程度高寒草地的土壤种子库土样用土壤分析筛进行浓缩,并以萌发法分析土壤种子库萌发种子数量和动态.结果表明,孔径0.25~2 mm的土壤分析筛分离土样中萌发种子可达萌发种子总量的85%~97%,而小于0.25 mm的土样中未发现种子.因此,用0.25 mm孔径大小的土壤筛对高寒草地土壤种子库土样进行大规模浓缩是一种方便、可靠的方法.4种不同退化程度高寒草地(A:未退化草甸;B:轻度退化草甸;C:中度退化草甸;D:重度退化草甸)的土壤种子库在实验室条件下萌发的种子数量分别为:A 1 194~3 744粒/m2,平均2 421.3粒/m2;B 5 376~1 0912粒/m2,平均7 786.7粒/m2;C 2 304~1 3216粒/m2,平均8 695.5粒/m2;D 4 768~12 352粒/m2,平均8 125.9粒/m2.除样地A外,其它3个样地的可萌发种子数量差异不大.单子叶植物种子在培养到d 10左右开始萌发,双子叶植物在5~7 d内开始萌发,前者3 wk后基本不再萌发,后者5 wk左右停止萌发.4个样地土壤种子库种子萌发主要集中在第2~3周,并表现出近似单峰型格局.图1表3参39
Resumo:
研究了科尔沁沙地 78种植物的繁殖体 (2 3种为种子 ,5 5种为果实 )重量和形状 ,其重量差别很大 ,最小的单粒重不足 0 .1mg,最大的超过 130 mg;形状差异也很大 ,最小的方差不足 0 .0 3,最大的超过 0 .18。综合本研究和以前研究的全部 14 0种植物的研究结果 ,进行了分析。结果表明 :1计有 2 4种植物繁殖体单粒重小于 1mg并接近圆球形 (方差小于 0 .0 9) ,它们可能具有持久种子库 ;2 1年生植物 (平均方差为 0 .0 70 )与 2年生植物 (平均方差为 0 .12 9)间的形状差异显著 (P<0 .0 5 ) ,2年生植物的繁殖体更加扁、长 ;1年生植物也与多年生草本植物 (平均方差为 0 .10 9)之间形状差异显著 (P<0 .0 5 ) ,多年生草本植物的繁殖体更加扁、长 ;3有 5 5 %的豆科植物、70 %的藜科植物繁殖体接近圆球形 (方差 <0 .0 6 ) ,所有的菊科、萝摩科植物繁殖体都很扁、长 (方差 >0 .0 6 )。豆科植物显著比菊科、禾本科、藜科植物繁殖体的重量大 (P<0 .0 5 ) ;4繁殖体附属物在植物的传播和定居方面具有重要的作用 :6种萝摩科植物和 3种杨柳科植物具有绢毛 ,6 0 %的菊科植物具有冠毛 ,6种植物有翅 ,8种植物有宿存花柱或宿存花萼 ,这些植物可能易于被风传播 ;5 4 %的禾本科植物具芒 ,减小了传播可能 ;苍耳、雾冰藜、鹤虱、蒺藜、
Resumo:
长白落叶松是东北地区主要的用材树种,其种子雨和种子库研究鲜见报道。在辽东山区用收集器收集的种子分析了长白落叶松种子雨组成、质量和扩散距离,每隔2个月调查1次种子库数量,并结合靛蓝染色法测定每次种子的活力来分析土壤种子库动态。结果表明,辽东山区的长白落叶松种子雨从8月中旬开始,9月末到10月初达到高峰期,11月初结束。在起始期,种子雨以干瘪的不完整种子为主,而从高峰期开始,种子雨以完整种子为主。整个长白落叶松种子雨中不完整种子约占种子雨总量的45%,这些不完整种子由被动物取食、空粒和病虫害危害种子组成。完整种子的平均生活力为56.4%,即有活力的种子仅占整个种子雨的30%。种子雨集中在母树周围,在林缘1次扩散距离一般不超过1.5倍树高。种子雨到达地面之后,主要分布在枯枝落叶层,土壤0~5cm层有少量分布,土壤5 cm以下没有种子分布;土壤种子库的种子主要在翌年雪融化后开始萌发、被取食、搬运以及腐烂,其中腐烂种子数占45.4%,动物取食为30.0%。种子库的种子数量和活力在冬季没有明显变化,而在翌年,种子数量和活力明显减少,4、6月和8月份种子数量分别为(506.3±35.56)粒m-2,(267.1±17.47)粒m-2和(143.6±9.83)粒m-2,对应的活力分别为47.8%±4.68%,19.4%±3.39%和0%,这表明长白落叶松种子不能在地面形成连续的种子库。