葛洲坝截流24年来中华鲟产卵群体结构的变化

以1981～2004年间捕获的中华鲟(AcipensersinensisGray)亲鲟样本为研究材料,研究葛洲坝截流24年来中华鲟繁殖季节中坝下30km范围内产卵群体结构的变化情况。测定与统计结果显示,中华鲟雌雄性比由1981～1983年的1.10∶1降低到1987～1989年的0.63∶1,而后上升到2003～2004年的5.86∶1。雌鲟平均体长由1990～1992年的263.1cm增加到1999～2001年的276.7cm,升幅为5.2%(差异极显著);平均体重由1990～1992年的202.4kg

臂轮凹口虫新种及其生活史的研究

于1979年7月在武昌中国科学院水生生物研究所湖汊采集水草,经研究发现须根上栖息的轮虫体内有一种专门攻击萼花臂尾轮虫和双棘臂尾轮虫的凹口虫,经鉴定系一新种,其主要特征为,传布子长椭圆形,两端较尖小,中间稍微凹;体前方有锥形的钻孔器,后端有3—5根长尾毛;大核香肠状,小核一个,椭圆形,伸缩泡一个,居中偏后。营养子圆球形,直径78—141μm,大核肾形,小核和伸缩泡各一个,亦具尾毛;裂子数为2—32个。寄生。致死轮虫,并在轮虫躯壳内完成其生活史。能形成次级包囊和抵抗性包囊。

24-二甲基戊二稀土化合物的合成

本文叙述了2.4-二甲基戊二烯基稀土金属有机化合物的合成并通过元素分析，红外光谱、核磁共振谱及质谱的鉴定。测定了Gd(2.4-GH_(11))_3的单晶结构，此外还合成了（2.4-GH_(11)K.TMEDA及K_2C_8H_8·3THF并也测定了它们的晶体结构。在所合成化合物的红外光谱中，没有属于C=C双键的吸收峰，表明分子中配位体以η~5形式的大π键体系与稀土金属离子结合，在Ln(2.4-GH_(11))_2Cl·TMF和Ln(2.4-GH_(11))Cl_2·GH_THF的红外光谱中，于1060波数附近出现一强而宽的吸收峰，即化合物中有四氢呋喃分子络合。化合物的室温NMR谱有四个吸收峰，2.4-二甲基戊二烯配位体可能为η~5平面∪或W构型。化合物的水解'H-NMR谱与质谱都证实水解产物为2.4－二甲基－1.3－戊二烯。它是－2.4二甲基戊二烯阴离子水解所得的唯一产物，它表明化合物中的配位体确为2.4－二甲基戊二烯阴离子。(2.4-GH_(11))_2Cl·TMDA配合物晶体结构是应用低温X－射线衍射技术用Nicolet R_3 M/E型四园衍射仪LT－1低温装置并利用重原子法测定的最小二乘法精修至收敛时的一致性因子R=0.055. Rw=0.057。晶体属单斜晶系P21/n空间群。晶胞参数a=11.322(4)A, b=9.242(3)A, c=15.956(5)A. β=106.70(3)分子中2.4－二甲基戊二烯阴离子呈平面∪构型。钾离子与四甲基乙二胺二啮体结合形成的络合阳离子和2.4-二甲基戊二烯阴离子相间排列形成无限链状结构分子。2.4－二甲基戊二烯阴离子的C－C键长明显分为中间与外端C－C键两组。外端组C－C键双性质较强键长较短。表明C3具有负电荷的共振杂化体贡献较大。分子中K－C键最短的是K-C(1.5)。而不是具有较多负电荷的C3－K键。这可能是由于几何因素造成的。K_2C_8H_8·3THF的晶体结构是采用与前者相同的方法测定的。它属三斜晶系，PT空间群，晶胞参数a=10.263(3)A, b=13.157(4)A, c=9.443A, α=87.51(2)°, β=114.93(2)°, γ=76.81(2)°. V=1111.6A, R=0.051. 晶体中负二价的环辛四烯阴离呈平面构型，具有中心对称性，两侧与两中心对称相关的钾离子连接，相邻的非等效的钾离子间通过两四氢呋喃分子的氧原子相连接，从而形成了无限链状结构的分子。环辛四烯反映了Huckel的4n+2芳香性规则。该结构的特别之处在于四氢呋喃分子的氧原子以桥键形式与两个钾离子同时连接。而这种形式的桥键在其它化合物中似还未发现。Go(2.4-GH_(11))_3的晶体结构亦是采用与前述相同的方法测定的。其晶体为三斜晶系，PT空间群，晶胞参数a=12.541A, b=12.853A, c=8.432A, α=91.44°, β=108.61°, γ=117.97°, V=112.54A~3. 结构测定表明，Gd(2.4-GH_(11))_3分子具有C_3h对称性。三个配位体阴离了的九个带负电荷的碳原子近似以三帽三角棱柱形式与钆离子配位。分子中2.4－二甲基戊二烯阴离子的C－C键长－亦分为而组。外端C－C键较中间C－C键强，键长较短，亦表明C3具有较多的负电荷。2.4－二甲基戊二烯阴离子本身近似呈平面∪构型。C2,C4偏离由C1 C3 C5三碳原子构成的平面0.067A。方向上远离中心钆离子。可能在此以离子性为主的化合物中，钆离子与不带电荷的C2 C4间的相互作用有些排斥性质。与Nd(2.4-GH_(11))_3不同的是，在Gd(2.4-GH_(11))_3分子中，Gd-(C(1,5）键最短，而不是Gd-C(3)键。这可能是由于钆离子的半径较小，化合物的空间位阻效应较大所致。

姚虻成功从宿主获得血餐的分子机制初探

在长期的吸血进化过程中，吸血节肢动物在唾液腺中形成了一系列有助于适应吸 血生存的活性物质，这些物质包括血管舒张分子、血小板聚集抑制分子、抗凝血分子 和其它相互作用的分子。此外，为了得到洁净的血液和防止在吸血过程中被病原微生 物感染，吸血节肢动物在其唾液腺中形成了许多防御物质以保护自身和宿主，这些物 质包括抗菌肽和蛋白酶抑制剂等。因此，研究吸血节肢动物的唾液腺重要活性物质和 转录体组学有助于弄清其吸血机制。 姚虻（Tabancus yao Macquart）是我国特有的牛虻，其雌性在产卵前需要吸食大 型哺乳动物的血液以促使卵的发育。我们希望通过对姚虻唾液腺重要活性物质和转录 体组学的研究揭示姚虻成功从宿主获得血餐的分子机制，找到具有药用前景的活性物 质和为控制该虫及其传播的疾病的提供理论基础。 首先，我们对其唾液腺匀浆物活性进行了系统分析，发现姚虻唾液腺匀浆物具有 如下活性：有抗金黄色葡萄球菌活性，并且对大肠杆菌、白色念球菌和枯草杆菌都有 效；能够抑制ADP 诱导的洗涤和富血浆血小板的聚集；能够凝集兔红细胞、能够抑制 丝氨酸蛋白酶对小肽底物的水解、具有对纤维蛋白原的水解活性（金属蛋白酶）、具 有过敏原活性、能够促进肥大细胞脱粒和组氨释放；反复检测而没有发现的活性如下： 磷脂酶A2(PLA2)活性、溶血活性、血浆凝固活性、体外抗补体、血管生长促进与抑制 活性、对小鼠脾细胞因子分泌的促进和抑制活性、抗肿瘤细胞HepG2 的生长活性。 以来源姚虻唾液腺的mRNA为材料，我们成功构建了丰度为1ｘ106的姚虻唾液腺 cDNA文库。通过对400个随机克隆的测序，我们得到了编码23种保守蛋白，44种分泌 蛋白和5种功能未知的蛋白。44种分泌蛋白中比较重要的分别是：20种抗原5相关蛋白、 2种α淀粉酶、2种麦芽糖酶、2种attactins抗菌蛋白以及血管舒张肽、过氧化物酶、 抗菌肽、透明质酸酶、mucin样蛋白和脯氨酸丰富蛋白。另外，一些不知道功能的分 泌肽也被发现,这其中包括四个与Hybomitra bimaculata的分泌肽相似性达47-82%的 多肽，这些信息有助于我们发现牛虻唾液腺活性物质和加快从知道部分氨基酸序列的 蛋白的鉴定速度，加快对姚虻从宿主获得血餐的分子机制的诠释速度。 通过分子筛、高压液相色谱等程序，我们从姚虻唾液腺中得到了一个由55 个氨 基酸组成，分子量为6 kDa，含有3 对二硫键的Kunitz 型丝氨基酸蛋白酶抑制剂TYTI。 该抑制剂与Anemonia sulcata 的蛋白酶抑制剂AsKC3 和SA5II 的成熟肽部分的同源 性达66%；并且该抑制剂，对热相对稳定；对凝乳酶、弹性蛋白酶、凝血酶、胰酶等 都有抑制作用，对胰酶的抑制常数为2.586ｘ10-4M 。 通过分子筛、高压液相色谱等程序，我们从姚虻唾液腺中得到了一分子量为7 kDa，由65 个氨基酸组成且含有3 对二硫键的防御素Taymin，它与长角血蜱的防御素的相 似性达43%，但它的第二个半胱氨酸比长角血蜱的半胱氨酸靠前一个氨基酸。该抗菌 肽对大肠杆菌、金黄色葡萄球菌、枯草芽孢杆菌和白色念球菌的最小抑菌浓度分别是: 160、80、140 和120μg/mL。 通过与分离丝氨酸蛋白酶抑制剂相同的生化分离手段,从姚虻唾液腺中得到一种 红细胞凝集素样活性物质TYML1，其能凝集原始和经胰酶、链霉蛋白酶和弹性蛋白酶 处理的A、B、O 和AB 血型的人、兔、绵羊、大鼠、小鼠、鹌鹑的红细胞, 对链霉蛋 白酶处理的鹌鹑红细胞的凝集效价比正常下降了8 倍；对热、酸、碱处理和蛋白酶降 解稳定；具有Ca2+依赖性，活性能为半乳糖胺和胎球蛋白所完全抑制。 通过分子筛、阴离子交换、高压液相色谱等程序，我们从姚虻唾液腺中分离得到 了一分子量为26 kDa,由234 个氨基酸组成，含有10 个半胱氨酸的血小板聚集抑制剂 Macquaritin-2,它与报道的所有血小板聚集抑制剂均不具有同源性，但是与双翅目昆 虫唾液腺过敏原却有一定的同源性(25%-33%),对其血小板聚集抑制活性研究发现:其 能抑制胰酶、花生四烯酸、Stejnulxin、TMVA、ADP、U46619 等激动剂诱导的血小板 聚集；血小板膜结合试验表明:其能与血小板细胞膜结合,故该血小板聚集抑制剂可能 通过作用血小板上的受体来阻止激动剂诱导血小板聚集。 通过分子筛、阳离子交换、高压液相色谱等程序，我们从姚虻唾液腺中分离得到 分子量为24-30 kDa 的两个血小板聚集抑制剂Macquaritin-3 和Macquaritin-1，它 们的N 端16 个氨基酸分别是V N Y C R L P C R G C D Y H V 和 V A V D Y L G L P G R G Y H V。通过PCR, Macquaritin-3 的核苷酸序列被得到，其推导蛋白的成熟区 和信号肽分别含有232 和23 个氨基酸。利用根据Macquaritin-1 的N 端氨基酸设计 的简并引物扩到含有V A V D Y L G L P 序列的两组核苷酸序列。它们与报道的所有 血小板聚集抑制剂均不具有同源性，但是其与双翅目昆虫的唾液腺抗原5 相关蛋白却 有一定的同源性。将所有血小板抑制剂及其相关序列和通过cDNA 文库筛选得到的抗 原5 相关序列进行分析,发现它们有很高的相似性,这种相似性介于33.3%-93.0%间, 且大部分高于50%。另外，两个血小板聚集抑制剂和一个可能的血小板抑制剂分别处 于这些抗原5 相关蛋白进化树的三个簇中。因此，我们推测这些过抗原5 相关蛋白可 能都具有血小板抑制剂活性。

氦离子注入形成980nm脊型波导激光器腔面非注入区的研究

报道了氦离子注入技术在提高980nm半导体激光器灾变性光学损伤（catastrophic optical damage，COD）阈值上的应用.p-GaAs材料经氦离子注入后可以获得的电阻率。在距离腔面25μm的区域内进行氦离子注入，由此形成腔面附近的电流非注入区。腔面附近非注入区减少了腔面载流子的注入，因此减少了非辐射复合的发生，提高了激光器的灾变性光学损伤阈值。应用氦离子注入形成腔面非注入区的管芯的平均最大功率达到440.5mW，没有发生COD现象。而应用常规工艺制作的管芯的平均COD阈值功率为407.5mW。同常规工艺相比，应用氦离子注入形成腔面非注入区技术使管芯的最大输出功率提高了8％。

黄龙世界自然遗产地岷江冷杉原始林群落结构与植物多样性：生境差异性研究

黄龙世界自然遗产地岷江冷杉林(Abies faxoniana)生境类型多样，群落结构复杂，群落植物种类组成多样性丰富。揭示不同生境的生物多样性及其差异是认识生物多样性格局、形成及维持机制的前提和进行多样性保育的基础。本文采用样方法对黄龙钙化滩生境、阴坡非钙化生境及半阳坡非钙化生境的岷江冷杉原始林植物群落结构及植物多样性进行了研究。结果表明： 黄龙岷江冷杉林具有明显的复层异龄结构，垂直结构明显，乔木、灌木、草本、苔藓层次分明。共发现高等植物386 种，其中维管植物46 科103 属163 种，苔藓植38 科83 属物223 种。各层片结构及物种组成如下: (1)钙化滩生境、阴坡非钙化生境、半阳坡非钙化生境分别发现乔木18 种、13种、8 种。乔木层均可分为两个亚层，第一亚层优势种均为岷江冷杉，第二亚层主要为岷江冷杉异龄树或其它大高位芽物种。钙化滩生境第一亚层除优势种岷江冷杉外混生有巴山冷杉(Abies fargesii)、粗枝云杉(Picea asperata)以及阔叶树种白桦(Betula platyphylla)等，第二亚层主要为岷江冷杉异龄树；阴坡非钙化生境第一亚层除优势种岷江冷杉外间有巴山冷杉和白桦，第二亚层物种主要为川滇长尾槭(Acer caudatum var. prattii)；半阳坡非钙化生境第一亚层除优势种岷江冷杉外混生有巴山冷杉，第二亚层主要为岷江冷杉异龄树。依乔木层优势种的差异，钙化滩生境及半阳坡非钙化生境为岷江冷杉纯林，阴坡非钙化生境为岷江冷杉－川滇长尾槭混交林。不同生境乔木层郁闭度、乔木密度、树高结构、直径结构均存在差异。 (2)钙化滩生境发现灌木41 种，平均盖度为18.49±1.72(％)，平均高度为52.12±4.45(cm)，优势种为直穗小檗(Berberis dasystachya)；阴坡非钙化生境发现灌木30 种，平均盖度为29.33±2.56 (％)，平均高度为119.55±8.01 (cm)，优势种为箭竹 (Fargesia spathacea) 、唐古特忍冬(Lonicera tangutica) 和袋花忍冬(Lonicera saccata)；半阳坡非钙化生境发现灌木29 种，平均盖度为31.35±1.93 (％)，平均高度为107.55±4.24 (cm)，优势种为箭竹(Fargesia spathacea)。不同生境灌木层结构和物种组成多样性差异显著，钙化滩生境的灌木盖度、高度总体上较非钙化的坡地生境低, 钙化滩生境灌木以小型叶的落叶灌木为主，沟两侧非钙化的坡地生境上则发育了丰富箭竹。 (3)钙化滩生境发现草本46 种，平均盖度为7.18±0.79 (％)，平均高度为5.04±0.26(cm)，以山酢浆草(Oxalis griffithii)为优势种；阴坡非钙化生境发现草本物种71 种，平均盖度达29.04±2.31(％)，平均高度为9.08±0.52(cm)，以钝叶楼梯草(Elatostema obtusum)、山酢浆草为优势种；半阳坡非钙化生境草本物种50 种，平均盖度为以8.79±0.82(％)，平均高度为7.67±0.43 (cm)，以扇叶铁线蕨(Adiantum flabellulatum)、双花堇菜(Viola biflora)、华中蛾眉蕨(Lunathyrium shennongense)、山酢浆草为优势种。阴坡非钙化生境草本层片发育良好，多样性最为丰富，盖度和物种丰富度均显著高于钙化滩生境和半阳坡非钙化生境。 (4)钙化滩生境发现苔藓物种140 种，平均盖度达84.25±1.30 (％)，以仰叶星塔藓(Hylocomiastrum umbratum) 等大型藓类为优势种；阴坡非钙化生境发现苔藓物种115 种，平均盖度为79.29±1.64 (％)，以刺叶提灯藓(Mnium spinosum)、大羽藓(Thuidium cymbifolium)、毛尖燕尾藓(Bryhnia trichomitra)等个体较小的物种为优势种；半阳坡非钙化生境发现苔藓物种91 种，平均盖度为60.64±1.93 (％)，也以刺叶提灯藓为优势种。 (5)钙化滩生境、阴坡非钙化生境、半阳坡非钙化生境的物种数分别为234 种、221 种、175 种。乔木层的Shannon-Wiener 指数分别为0.75 ±0.12、1.87±0.12、1.78±0.07（灌木层，0.44±0.08、1.71± 0.15、2.49±0.06；草本层，0.33±0.13、1.31±0.15 、2.15±0.08； 苔藓层1.30±0.11、2.08±0.04、1.73±0.11，）；Pielou 均匀度指数分别为0.45±0.05、0.29±0.06、0.28±0.08（灌木层，0.75±0.03、0.68±0.05、0.52±0.06；草本层，0.68±0.02、0.77±0.02、0.74±0.02；苔藓层，0.40±0.03、0.63±0.02、0.52±0.03）；Simpson's 优势度指数分别为0.63±0.06、0.78±0.04、0.83±0.07（灌木层，0.21±0.03、0.28±0.05、0.45±0.06；草本层，0.25±0.02、0.12±0.01、0.17±0.01；苔藓层，0.45±0.04、0.18±0.01、0.31±0.04）。三种生境间乔木层、草本层的Sorenson 群落相似性系数较低, 灌木层、苔藓层的的Sorenson 群落相似性系数较高。 综上所述，黄龙岷江冷杉林的群落结构、植物多样性在三种生境间存在差异性，这将意味着我们在进行黄龙世界自然遗产地的森林经营管理时要较多地关注岷江冷山林群落在不同生境中的差异性。 There were multiplex habitat types, complicated community structure and abundant species composition in the Huanglong World Natural Heritage Site. Uncovering the differences of biodiversity among different habitats was a precondition to understand the distribution, formation and sustaining mechanism of the biodiversity, and the foundation of biodiversity conservation. In the present study, using plenty of quadrants, we investigated the community structure and the biodiversity of the primitive Abies faxoniana forest in different habitats (travertine bottomland, semi-sunny-slope non-calcified habitat and shady-slope non-calcified habitat) in the Huanglong World Natural Heritage Site. The main results are as follows: All the primitive Abies faxoniana forests in the three habitats were uneven-aged with obvious vertical structure including tree layer, shrub layer, herb layer and bryophyte layer. A total of 386 higher plants including 163 vascular plant species (103 generic, 46 families) and 223 bryophyte species (83 generic, 38 families) were investigated. The structure and species composition of each layer are as follows: (1) There were 18, 13 and 8 tree species in travertine bottomland, shady-slope non-calcified habitat and semi-sunny-slope non-calcified habitat, respectively. The tree layers in all habitats can be divided into two clear sub-layers. The upper tree layers were dominated by Abies faxoniana, and the lower tree layers were dominated by uneven-aged Abies faxoniana or other phanerophytes species. There were Abies fargesii , Picea asperata and Betula platyphylla besides the dominated species (Abies faxoniana) in the upper tree layer in travertine bottomland, and the lower tree layers were dominated by uneven-aged Abies faxoniana; There were Abies fargesii and Betula platyphylla besides the dominated species (Abies faxoniana) in the upper tree layer in shady-slope non-calcified habitat, and the lower tree layers were dominated by Acer caudatum var. prattii; There was Abies fargesii besides the dominated species (Abies faxoniana) in the upper tree layer semi-sunny-slope non-calcified habitat, and the lower tree layers were dominated by uneven-aged Abies faxoniana. According to composition percentage of dominate species in tree layer, both the forest in travertine bottomland and in semi-sunny-slope non-calcified habitat could be ranked as pure forest, and the forest in shady-slope non-calcified habitat could be ranked as mingled forest. There were significant differences in crown density, plant density, height structure and diameter structure among the three habitats. (2) A total of 41 shrub species (average coverage 18.49±1.72％; average height 52.12±4.45 ㎝)were found in travertine bottomland, and the dominate species was Berberis dasystachya; A total of 30 shrub species (average coverage 29.33±2.56 ％;average height 119.55±8.01 ㎝)were found in shady-slope non-calcified habitat, and the dominate species was Fargesia spathacea, Lonicera tangutica and Lonicera saccata. A total of 29 shrub species (average coverage 31.35±1.93％; average height 107.55±4.24 ㎝) were found in semi-sunny-slope non-calcified habitat, and the dominate species was Fargesia spathacea. There were significant differences in structure and species diversity of the shrub layers among the three habitats. The coverage and height of shrub had lower value in travertine bottomland than in two non-calcified habitats. Moreover, travertine bottomland was dominated by deciduous shrub species with microphyll and non-calcified habitats developed abundant Fargesia spathacea species. (3) A total of 46 herb species (average coverage 7.18±0.79％;average height 5.04±0.26 ㎝)were found in travertine bottomland, and the dominate species was Oxalis griffithii; A total of 71 herb species (average coverage 29.04±2.31％;average height 9.08±0.52 ㎝)were found in shady-slope non-calcified habitat, and the dominate species was Elatostema obtusum and Oxalis griffithii. A total of 50 herb species (average coverage 8.79±0.82％;average height 7.67±0.43 ㎝) were found in semi-sunny-slope non-calcified habitat, and the dominate species was Adiantum flabellulatum, Viola biflora, Lunathyrium shennongense and Oxalis griffithii. Herb layers developed well in shady-slope non-calcified habitat and had the higher species richness and coverage than travertine bottomland and semi-sunny-slope non-calcified habitat. (4) A total of 140 bryophyte species (average coverage 84.25±1.30％)were found in travertine bottomland, and the dominate species was big bryophyte species such as Hylocomiastrum umbratum and so on; A total of 115 bryophyte species (average coverage 79.29±1.64％)were found in shady-slope non-calcified habitat, and the dominate species was small bryophyte species such as Mnium spinosum, Thuidium cymbifolium, Bryhnia trichomitra and so on. A total of 91 bryophyte species (average coverage 60.64±1.93％) were found in semi-sunny-slope non-calcified habitat, and the dominate species was Mnium spinosum. (5) There were 234, 221 and 175 plant species in travertine bottomland, shady-slope non-calcified habitat and semi-sunny-slope non-calcified habitat, respectively. Shannon-Wiener index of the tree layer was 0.75 ±0.12, 1.87±0.12 and 1.78±0.07 (the shrub layer, 0.44±0.08, 1.71± 0.15 and 2.49±0.06; the herb layer, 0.33±0.13, 1.31±0.15 and 2.15±0.08; the bryophyte layer, 1.30±0.11, 2.08±0.04 and 1.73±0.11.) for the three habitats, respectively; Pielou index of the tree layer was 0.45±0.05, 0.29±0.06 and 0.28±0.08 (the shrub layer, 0.75±0.03, 0.68±0.05 and 0.52±0.06; the herb layer, 0.68±0.02, 0.77±0.02 and 0.74±0.02; the bryophyte layer, 0.40±0.03, 0.63±0.02 and 0.52±0.03.) for the three habitats, respectively. Simpson's index of the tree layer was 0.63±0.06, 0.78±0.04 and 0.83±0.07 (the shrub layer, 0.21±0.03、0.28±0.05、0.45±0.06; the herb layer, 0.25±0.02, 0.12±0.01 and 0.17±0.01; the bryophyte layer, 0.45±0.04, 0.18±0.01 and 0.31±0.04.) for the three habitats, respectively. There were low Sorenson index both in the tree layer and in the herb layer among the three habitats, whereas, high Sorenson index occurred both in the shrub layer and in the bryophyte layer. To sum up, there were differences both in community structure and plant diversity among the three different habitats, which means that we should pay more attention to habitats heterogeneities of the primitive Abies faxoniana forest when we take action to manage the forest in the Huanglong World Natural Heritage Site.

高电荷态离子~(207)Pb~(q+)(24≤q≤36)与Si(110)固体表面作用的电子发射研究

报道了利用兰州重离子加速器国家实验室ECR源引出的高电荷态离子207Pbq+(24≤q≤36)入射到Si(110)表面产生的电子发射的实验测量结果.结果表明,高电荷态离子与固体表面相互作用产生的电子发射产额Y与入射离子的电荷态q、入射角度ψ和入射能量E都有很强的关联.首次发现,电子发射产额Y与入射角度ψ间有接近1/tanψ的关系.理论分析认为,这些过程与基于经典过垒模型的势能电子发射过程密切相关.

Electron emission induced by the interaction of highly charged ions Pb-207(q+) (24 <= q <= 36) with solid surface of Si(110)

The electron emission induced by highly charged ions Pb-207(q+) (24 <= q <= 36) interacting with Si(110) surface is reported. The result shows that the electron emission yield Y has a strong dependence on the projectile charge state q, incidence angle psi and impact energy E. In fitting the experimental data we found a nearly 1/tan psi dependence of Y. Theoretical analysis shows that these processes are closely related to the process of potential electron emission based on the classical over-the-barrier model.

The oxidative demethylation of 24-membered hexa-aza macrocyclic bicopper(I) complex - The mimicking for monooxygenase

By [2 + 2] Schiff base condensation of 5 - bromo - 2 - methoxylbenzene - 1,3 - dicarboxaldehyde with diethylenetriamine, a new hexaaza 24 - membered macrocyclic ligand was obtained,which formed a macrocyclic binuclear copper(I) complex in the presence of [Cu . (CH3CN)(4)]ClO4. When the copper(I) complex was oxidized in air or oxygen, a new macrocyclic binuclear copper( II) complex was obtained. The copper( II.) complex was characterized by several methods and its oxidized products was characterized by H-1 NMR. The results show that during oxidation, a methoxyl group in the ligand ring broke; and the phenoxy - and water - bridged Cu(II) complex formed. In oxidation of monooxygenase such as ligninase, oxidative demethylation also happened. Therefore this work mimicked this process for the first time by using macrocyclic complex. The quantity of absorbed oxygen and the absorption rate of oxygen were determined.

Palaeoenvironmental changes from pollen record in deep sea core PC-1 from northern Okinawa Trough, East China Sea during the past 24 ka

A pollen record of core PC-1 from the northern Okinawa Trough, East China Sea (ECS), provides information on vegetation and climate changes since 24 cal. kaBP. A total of 103 samples were palynologically analyzed at 8 cm intervals with a time resolution of 230 a. Four pollen zones are recognized: zone I (812-715 cm, 24.2-21.1 cal. kaBP), zone II (715-451 cm, 21.1-15.2 cal. kaBP), zone III (451-251 cm, 15.2-10.8 cal. kaBP), zone IV (251-0 cm, 10.8-0.3 cal. kaBP), corresponding to Late MIS 3, Last Glacial Maximum (LGM), deglaciation and Holocene, respectively. The LGM is characterized by the dominance of herbs, mainly Artemisia, and high pollen influx, implying an open vegetation on the exposed continental shelf and a cool and dry climate. The deglaciation is a climate warming stage with Pinus percentage increased and Artemisia percentage decreased and a rapid sea-level rise. The Holocene is characterized by predominance of tree pollen with rapid increase in Castanea-Castanopsis indicating the development of mixed evergreen and deciduous broad-leaved forest and a warm, humid climate. Low pollen influx during the Holocene probably implies submergence of the continental shelf and retreat of the pollen source area. The vegetation indicated by pollen assemblage found in this upper zone is consistent with the present vegetation found in Kyushu, Japan. Originating from the humid mountain area of North Luzon of the Philippines, Tasmania and New Zealand, Phyllocladus with sporadic occurrence throughout PC-1 core probably suggests the influence of Palaeo-Kuroshio Current or intense summer monsoon. The observed changes in Pinus and Herbs percentage indicate fluctuations of the sea level, and high Pinus percentage corresponds to high sea level. Spectrum analysis of the pollen percentage record reveals many millennial-scale periodicities, such as periodicities of 6.8, 3.85 2.2, 1.6 ka.

中国南方热带地区田洋玛珥湖24万年以来的气候变化及湖泊演变

A continuous long (224m) and high-resolution core TY2 was recovered from paleo-maar-lake Tianyang, tropical South China. Based on the diatom records of the upper 130-m core, this paper focuses on exploring climate change and the lake evolution history in tropical South China during the past 240ka. The most typical and unique characteristics of the diatom assemblages is that, Aulacoseira granulata was dominant or absolutely dominant species (80-90%) during most parts of the 130-m core, while Cyclotella stelligera var. tenuis and Fragilaria construens var. venter were subdominant species in only limited parts of the lower and upper core, respectively. Time scale is always the biggest problem for the study of TY2 core, so although diatom is seldom used for establishing time scale, here we attempt this by correlating the diatom-reconstructed temperature sequence with the time scale of ODP core 806B from Equatorial Western Pacific. Verified by the few most reliable ages from TY2 core and the parallel core TYl, a rather reasonable and reliable time scale was established. 01S 7/6 falls at the depth of 100m (ca. 194kaBP), OIS 6/5 at 75m (ca. 132kaBP), OIS 5/4 at 46m (ca. 75kaBP), OIS 4-3 at 35m (ca. 60kaBP). Qualitative and quantitative environmental reconstructions are made on the basis of diatom assemblage ecotype and EDDI dataset. Correlation of diatom-reconstructed temperature and moisture changes of Core TY2 with pollen-reconstructed temperature and rainfall sequence of Core TYl proves that the results are quite consistent in most periods. Thus the reconstruction results from diatom are quite reliable, and probably have a much higher resolution than pollen results. Combined with lithological and magnetic susceptibility variations, the diatom analysis reveals that, the general climate in tropical South China during the past 240ka was warm and wet. On the time scale of glacial-interglacial, warm and wet, cool and dry are not always synchronous. It was relatively warm-wet during the penultimate interglacial, cool-dry during the penultimate glacial, warm-dry during the last interglacial, and cooler-drier during the last glacial. In contrast, on the time scale of subglacial-subinterglacial scales, warm and dry, cool and wet corresponds very obviously, showing very clear 21-23 ka precession cycle. Analysis also shows that, the water of Tianyang paleo-maar-lake was generally warm, turbulent, turbid, meso-trophic, slightly alkaline, low conductivity and fresh during the past 240 kaBP, with small variations in some parts. Tianyang paleolake experienced shallow to semi-deep lake in OIS7d, open shallow lake in OIS7c-OIS5b, shallow coastal lake in OIS5a-OIS4c, swamp in OIS4b, and then completely dried up in OIS3c. The lake evolution was mainly controlled by temperature and precipitation changes in tropical China. While temperature and precipitation changes were probably controlled by the migrations of monsoon rainband and the evaporation rate, which was in turn controlled by the evolution of East Asian monsoon. Therefore, when the summer monsoon was strongest the climate was warm-dry, when stronger the climate was warm-wet; when the winter monsoon was strongest the climate was cool-dry, stronger cool-wet. This mechanism caused the warm-dry sub interglacial and cool-wet subglacial climate in the tropical South China.

《陕西铜厂矿田构造成矿动力学》书评

该书以陕西勉(县)-略(阳)-阳(平关)地区铜厂铜金多金属矿田为例，在总结构造成矿动力学的理论和方法基础上，从成矿地质背景、矿床地球化学、矿田地质力学、矿田构造地球化学及矿田构造应力场等方面对研究区进行了系统地构造成矿动力学研究，根据所获研究成果对该区进行了隐伏矿定位预测。全书约35万字，共分7章，其中图¨6幅、表53个、照片62张。陈庆宣院士为该书作了序。