978 resultados para 448


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本文对不同立构的聚甲基丙烯酸(PMAA)进行了热表征。实验结果表明,在30℃~200℃内未出现玻璃化转变。间同PMAA分别在-245℃和-280℃发生脱水反应和脱羧,而全同PMAA只在-185℃观察到脱水反应。这种热稳定性的明显差别与不同立构PMAA链上相邻羧酸距离有关。实验数据证实PMAA脱水反应为无规反应,服从一级动力学反应方程。脱水温度和间同立构含量成正比,脱水反应活化能间同PMAA比全同PMAA高~7Kcal/mol。

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CORROSION; WATER; SPECTROSCOPY; CHLORIDE; ZINC; NUCLEATION; INTERFACE; ELECTRODE; SURFACES; GROWTH

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A statistical model of random wave is developed using Stokes wave theory of water wave dynamics. A new nonlinear probability distribution function of wave height is presented. The results indicate that wave steepness not only could be a parameter of the distribution function of wave height but also could reflect the degree of wave height distribution deviation from the Rayleigh distribution. The new wave height distribution overcomes the problem of Rayleigh distribution that the prediction of big wave is overestimated and the general wave is underestimated. The prediction of small probability wave height value of new distribution is also smaller than that of Rayleigh distribution. Wave height data taken from East China Normal University are used to verify the new distribution. The results indicate that the new distribution fits the measurements much better than the Rayleigh distribution.

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本文通过对渤海泥质区不同位置岩芯的粒度、矿物、化学元素等方面的分析,结合浅地层地震剖面、AMS 14C测年、微体古生物分析、稳定同位素测量、古地磁数据等,对全新世渤海泥质区中沉积物物质组成特征、物质来源、形成历史其环境响应进行了探讨。 结果显示,在早全新世期间黄河曾流经渤海南部,其携带泥沙对渤海沉积作用造成一定影响,但不同位置沉积环境及所受黄河影响的大小存在差异。 渤海泥质区的主体部分从约6000 aBP开始形成。当时沉积记录存在突变现象,不仅显示了沉积环境氧化还原条件的改变,而且温度与盐度值的变化以及沉积速率的明显偏高以及浮游有孔虫的出现说明本区开始受到黄海暖流余脉的影响。4500 aBP以来,沉积物中重矿物组合、化学成分等与黄河沉积物已较为接近,说明此时黄河物质对渤海泥质沉积的影响已经占据主导地位。渤海泥质区虽然有着离黄河口较近的特点,但并未出现明显高于陆架其它泥质沉积区的沉积速率,说明受输运机制控制,黄河物质向泥质区的输送量不大,远不如向黄海的输出量。 北部记录着全新世期间发生的两次地磁极漂移,分别发生于2800~3100 aBP(对应Starno事件)和7500~8200 aBP。漂移发生前后,气候、物质来源与海平面均有较大变化,说明地磁极漂移对气候有着重要影响。

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In this paper, we viewed the diel vertical migration (DVM) of copepod in the context of the animal's immediate behaviors of everyday concerns and constructed an instantaneous behavioral criterion effective for DVM and non-DVM behaviors. This criterion employed the function of 'venturous revenue' (VR), which is the product of the food intake and probability of the survival, to evaluate the gains and losses of the behaviors that the copepod could trade-off. The optimal behaviors are to find the optimal habitats to maximize VR. Two types of VRs are formulated and tested by the theoretical analysis and simulations. The sensed VR, monitoring the real-time changes of trade-offs and thereby determining the optimum habitat, is validated to be the effective objective function for the optimization of the behavior; whereas, the realized VR, quantifying the actual profit obtained by an optimal copepod in the sensed-VR-determined habitat, defines the life history of a specific age cohort. The achievement of a robust copepod overwintering stock through integrating the dynamics of the constituent age cohorts subjected to the instantaneous behavioral criterion for DVM clearly exemplified a possible way bridging the immediate pursuit of an individual and the end success of the population. (c) 2005 Published by Elsevier Ltd.

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以高原448小麦品种为材料,分别测定了4个处理(Hoagland营养液、Hoagland营养液+150 mmol/LNaCl、Hoagland营养液+150 mmol/L NaCl+10μmol/L H_2O_2和Hoagland营养液+10μmol/L H_2O_2)的小麦幼苗在第2、4、6、8天叶片叶绿素、丙二醛、可溶性糖和还原性谷胱甘肽含量.结果显示:外源H2O2提高了NaCl胁迫下4个时段小麦幼苗的叶绿素含量(8.27%、32.57%、10.19%、4.86%)及还原性谷胱甘肽含量(3.09%、23.97%、5.85%、2.11%),显著提高了可溶性糖含量(14.58%、8.43%、16.68%、5.8%,P〈0.05),而显著降低了其丙二醛含量(17.53%、14.04%、4.75%、8.47%,P〈0.05).外源H_2O_2(10μmol/L)使NaCl胁迫下叶绿素含量和还原性谷胱甘肽含量峰值提前,同时推迟了丙二醛峰值出现的时间.研究表明,外源H2O2通过提高叶片叶绿素、可溶性糖和还原性谷胱甘肽含量以有效地增强小麦幼苗的耐盐性.

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以海北高寒草甸生态系统定位站的涡度相关系统连续观测的CO_2通量数据为基础,分析了青藏高原的高寒矮嵩草(Kobresia humilis)草甸、高寒金露梅(Potentilla fruticosa)灌丛草甸和高寒藏嵩草(Kobresia tibetica)沼泽化草甸等3种主要植被类型在2005年植物生长季(6-9月)的表观量子产额(a)、最大光合速率(Pmax)和呼吸速率(Reco)的变化特征.结果表明:3种植被类型白天的净生态系统CO_2交换量(NEE)和光量子通量密度(PPFD)存在明显的直角双曲线关系(P<0.05),其a、Pmax和Reco呈现出相似的季节变化趋势,在生长季初期(6月)最小,在7月或8月份达到最大;高寒矮嵩草草甸的a、Pmax和Reco大于灌丛草甸和沼泽化草甸,而后两者差别不大.

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对高寒小嵩草草甸不同放牧强度下20种植物种群的优势度、生态位宽度及生态位重叠规律进行了研究.结果表明,经过2年的放牧实验,对照、轻度和中度放牧组的主要优势种均为小嵩草和垂穗披碱草,重度放牧组的主要优势种为鹅绒委陵菜和阿拉善马先蒿;由于小嵩草、矮嵩草和线叶嵩草具有耐牧和耐践踏等生物学特点,它们的生态位宽度很大(0.938,0.824,0.815);垂穗披碱草由于其耐牧和耐旱性较差,生态位宽度相对较小(0.805),且青海野青茅、异针茅、针茅、紫羊茅和双叉细柄茅等禾本科牧草的生态位宽度在放牧强度梯度上均较小(0.226,0.448,0.445,0.608,0.605),说明放牧抑制了高大禾草层片的发育,为植株矮小的莎草科牧草的生长创造了条件;异针茅和针茅之间、甘肃马先蒿和阿拉善马先蒿之间生态位重叠较小(0.500,0.572),这是种间对资源利用上分化的结果.分布于放牧演替系列2个极端的种群间生态位重叠较小,表明物种的分布是既间断又连续的.

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为了解青海省春小麦收割后田间堆放期间产量和品质的变化,选择近年育成的春小麦品种“高原205”(白粒,易穗发芽)、“高原115”(紫黑色小麦)、“高原448”(红粒)和“高原314”(白粒)以及曾为青海省主栽品种的“青春533”(红粒)为材料,收割后以农民常用的田间堆放方式进行堆放,每隔9d对其进行采样,测定产量、SDS沉淀值和降落数值的变化。结果表明,随着堆放时间的延长,收获产量逐步下降,平均产量从第1次采样(Od)时的504g/m^2减少到63d后的384g/m^2,收获产量平均值与取样时间直线回归F值为20.91,大于F0.01(6.90);SDS沉淀值变化较小,F值为0.90,小于F0.05(2.13);降落数值在取样时间点上差异极显著.F值等于46,72,大于F0.01(2.87)。高原205的降落数值一直呈现下降趋势,而高原448、高原115、高原314和青春533的变化是在O~18d间上升,然后下降。总体而言,田间堆放对收获产量和品质不利。

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经过两年牦牛放牧试验表明,夏季草场不同土壤层有机质、有机碳、全磷、全氮和速效磷的含量及0~20cm土壤层营养因子的平均含量与放牧率呈线性回归关系,速效氮含量与放牧率呈二次回归关系;冬季草场不同土壤层有机质、有机碳和全氮与放牧率呈线性回归关系,全磷、速效磷和速效氮的含量及0~20cm土壤层营养因子的平均含量与放牧率呈二次回归关系。随着放牧率的逐渐增加,夏季草场不同土壤深度速效氮含量也逐渐减小,当放牧率达到1.07、1.08和1.22头·hm-2时,0~5、5~10、10~20cm土壤速效氮含量依此达到最小;冬季草场不同土壤层全磷、速效磷和速效氮含量逐渐增加,当放牧率达到0.81、0.78和1.00头·hm-2,1.03、1.09和1.03头·hm-2,1.36、1.35和1.30头·hm-2时,0~5、5~10、10~20cm土壤层全磷、速效磷和速效氮含量分别依此达到最大。在夏季草场,0~20cm土壤层速效氮平均含量达到最小放牧率是1.07头·hm-2;冬季草场0~20cm土壤层全磷、速效磷和速效氮含量达到最大放牧率分别是0.90、0.83和1.21头·hm-2。

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通过国产画眉草亚族叶片表皮的解剖观察,结合外部形态,对该亚族内6个属的属间关系进行了分析.结果表明:羽穗草属应是国产画眉草亚族中最原始的类群,最高级的类群仍数细画眉草属,而其余4属即画眉草属、弯穗草属、尖稃草属和镰稃草属的演化水平居于两者之间;画眉草属和弯穗草属可能直接起源于原始的羽穗草属,而较高级的尖稃草属和镰稃草属又可能直接起源于较原始的画眉草属,并在镰稃草属的基础上进而派生了最进化的细画眉草属.整个研究结果既弥补了前人演化理论的不足,又为今后族进化的全面探讨提供了参考.

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广袤的草地、特有的高寒湿地以及丰富而有又独特的生物多样性是江河源区重要的自然生物资源.草地占江河源区总土地面积的84.53%,是源区畜牧业经济发展的基础,同时也是长江、黄河和澜沧江三大江河的源头区域,为江河中、下游地区生态环境稳定和经济持续发展提供无可替代的服务.江河源区是世界上海拔最高的高寒湿地主要分布区,湿地总面积达8 000 km2.江河源区独特的生态环境孕育了种类繁多的特有动、植物种类,源区约有哺乳动物、鸟类和鱼类133、249和219种,牧草植物、药用植物、食用植物和观赏植物约800、808、80和400种,是世界海拔最高的生物多样性集中分布区.然而,由于超载放牧、盲目采挖、盗猎等不合理的开发和利用以及气候变化等诸多因素的综合影响,江河源区草地生态系统退化、高寒湿地萎缩、生物多样性锐减等生态环境危机不断加剧.正确权衡江河源区自然生物资源的短期经济价值及其所拥有的巨大生态公益和潜在开发价值,科学决策,保护江河源区自然生物资源迫在眉睫.

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目的对比分析国家一类动物药塞隆骨和禁用传统中药材虎骨中的19种矿物质元素的含量.方法骨骼样品经灰化或消解处理后,采用原子吸收光谱法、氢化物原子荧光光谱法、催化极谱法等分析方法测定矿物质元素.结果两种动物骨骼中元素含量差异显著,塞隆骨11种元素高于虎骨,特别是Cu、Zn、Fe、Mn、Se等生命活动必需微量元素塞隆骨极为显著地高于虎骨,而组成骨骼的主要成分Ca、P则为虎骨高于塞隆骨.矿物质元素在头骨、脊梁骨和腿骨中分布非常不平衡,多数元素以头骨中分布最为丰富,而5种常量元素Ca,P,Na,Mg,K的含量为腿骨>头骨>脊梁骨.骨骼中主要成分Ca和P的存在形式主要为羟磷灰石Ca10(PO4)6(OH)2.结论塞隆骨骨骼中的矿物质元素与虎骨有可比性,必需微量元素塞隆骨明显优于虎骨.

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研究选用耐旱性强的“定西24”和“高原671”与耐旱性弱的“高原448”和“青春533”春小麦品种,在盆栽条件下比较了不同耐旱性品种在拔节后经不同程度水分胁迫后叶片的多种生理参数;叶片相对含水量、净光合速率、叶绿素a、叶绿素b、叶绿素总量和类胡萝卜素含量。结果表明:在土壤相对含水量75%、55%、40%和30%这4个等级上,这些生理指标均随土壤相对含水量的降低而下降,耐旱性强的品种降低慢,且降低幅度小。在水分胁迫下,4个品种叶片的叶绿素a、叶绿素b和叶绿素总量下降,证明此时光合器生理功能遭到破坏;在轻度水分胁迫下,耐旱性强的品种定西24和高原671叶片的类胡萝卜素含量上升;在严重水分胁迫下,4个品种的叶片类胡萝卜素含量明显下降,可能此时自由基积累超过了抗氧化剂的清除能力,从而使细胞受到损伤。根据本研究结果,可以将轻度水分胁迫下叶片类胡萝卜素含量升高作为春小麦品种耐旱性的选择指标之一。

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Stable carbon and nitrogen isotope ratios were measured in plant populations and plateau pikas to determine enrichment in stable isotopes of three alpine meadow ecosystems at different elevations in the Qinghai-Tibet Plateau. The results indicated that stable carbon isotope signatures of plant populations at the three locations showed significant variations, delta C-13 of plant populations showed an enrichment of 0.86 parts per thousand per 1000 in over the linear proportion of the altitudinal response, while stable nitrogen isotopes showed no apparent difference. The stable nitrogen isotopes of plateau pikas became significantly isotopically heavier along altitudinal gradients and showed an enrichment of 3.17 parts per thousand/km. Stable carbon isotopes showed no significance, however, and the enrichment of 0.448 parts per thousand/km. delta C-13 and delta N-15 in plateau pikas were not significantly correlated. There appeared to be segregation between the metabolism of stable carbon and nitrogen isotopes of plateau pikas. Variances in metabolic rate at lower water availability and temperatures are presumed to be the main cause of enrichment of stable nitrogen isotopes along altitudinal gradients. Attention should be paid to construct trophic positions and to trace food chain information based oil an isotopic enrichment model.