Effects of cage fish culture on water quality and selected biological communities in northern Lake Victoria, Uganda

Growing of fish in cages is currently practiced in Uganda and was first introduced in northern Lake Victoria in 2010. An environment monitoring study was undertaken at Source of the Nile, a private cage fish farm, in Napoleon gulf, northern Lake Victoria. In-situ measurements of key environmental (temperature, dissolved oxygen, pH and conductivity) and biological (algae, zooplankton, macro-benthos) variables were made at three transects: Transect 1- the site with fish cages (WC); transect 2- upstream of the fish cages (USC-control) and Transect 3- downstream of the cages (DSC). Upstream and Downstream sites were located approximately 1.0 km from the fish cages. Environment parameters varied spatially and temporally but were generally within safe ranges for freshwater habitats. Higher concentrations of SRP (0.015-0.112 Mg/L) occurred at USC during February, September and at DSC in November; NO2-N (0.217- 0.042 mg/L) at USC and DSC in February and November; NH4-N (0.0054- 0.065 Mg/L) at WC and DSC in February, May and November. Algal bio-volumes were significantly higher at WC (F (2,780)=4.619; P=0.010). Zooplankton species numbers were consistently lower at WC with a significant difference compared to the control site (P=0.032). Macro-benthos abundance was consistently higher at the site with cages where mollusks and low-oxygen and pollution-tolerant chironomids were the dominant group. Higher algal biomass, concentration of low-oxygen/pollution-tolerant macro-benthos and depressed zooplankton diversity at WC suggested impacts from the fish cages on aquatic biota.

6种常用渔药对厚颌鲂鱼苗的急性毒性试验

在水温29~30℃条件下,用硫酸铜与硫酸亚铁合剂(比例5:2)、高锰酸钾、晶体敌百虫、强氯精、溴氯菊脂、甲醛共6种药物对厚颌鲂(Megalobrama pellegrini)鱼苗进行急性毒性试验。试验结果显示,6种药物48h的半致死浓度分别为5.78、6.50、4.90、2.55、0.042、120mg/L,安全浓度分别为0.445、0.528、0.268、0.190、0.003、7.500mg/L,厚颌鲂鱼苗对药物敏感性比一般鱼类高,实际用药时应根据具体情况确定用药时间和用药量,溴氯菊脂不宜作为治疗药物

极高CO_2胁迫对被甲栅藻(Scenedesmus armatus)生理活性和细胞结构影响

以被甲栅藻(Scenedesmusarmatus)为材料研究极高浓度CO2对其生理活性和细胞结构的影响。研究表明,被甲栅藻能在60%的CO2浓度下快速生长,在5%、20%、40%、60%、80%、100%CO2浓度下的平均增长率分别是1.228、0.925、0.741、0.305、0.042、0.001g·L-1·d-1DW。通入极高浓度CO2(20%、40%)后,被甲栅藻细胞的光系统II(PSII)最大光化学效率(Fv/Fm)在24h内明显下降,对PSII抑制作用较明显;其后,随培养时间的增长而逐渐恢复

Nanostructure in the p-layer and its impacts on amorphous silicon solar cells

The open circuit voltage (V-oc) of n-i-p type hydrogenated amorphous silicon (a-Si:H) solar cells has been examined by means of experimental and numerical modeling. The i- and p-layer limitations on V-oc are separated and the emphasis is to identify the impact of different kinds of p-layers. Hydrogenated protocrystalline, nanocrystalline and microcrystalline silicon p-layers were prepared and characterized using Raman spectroscopy, high resolution transmission electron microscopy (HRTEM), optical transmittance and activation energy of dark-conductivity. The n-i-p a-Si:H solar cells incorporated with these p-layers were comparatively investigated, which demonstrated a wide variation of V-oc from 1.042 V to 0.369 V, under identical i- and n-layer conditions. It is found that the nanocrystalline silicon (nc-Si:H) p-layer with a certain nanocrystalline volume fraction leads to a higher V-oc. The optimum p-layer material for n-i-p type a-Si:H solar cells is not found at the onset of the transition between the amorphous to mixed phases, nor is it associated with a microcrystalline material with a large grain size and a high volume fraction of crystalline phase. (c) 2006 Elsevier B.V. All rights reserved.

Nanostructure in the p-layer and its impacts on amorphous silicon solar cells

The open circuit voltage (V-oc) of n-i-p type hydrogenated amorphous silicon (a-Si:H) solar cells has been examined by means of experimental and numerical modeling. The i- and p-layer limitations on V-oc are separated and the emphasis is to identify the impact of different kinds of p-layers. Hydrogenated protocrystalline, nanocrystalline and microcrystalline silicon p-layers were prepared and characterized using Raman spectroscopy, high resolution transmission electron microscopy (HRTEM), optical transmittance and activation energy of dark-conductivity. The n-i-p a-Si:H solar cells incorporated with these p-layers were comparatively investigated, which demonstrated a wide variation of V-oc from 1.042 V to 0.369 V, under identical i- and n-layer conditions. It is found that the nanocrystalline silicon (nc-Si:H) p-layer with a certain nanocrystalline volume fraction leads to a higher V-oc. The optimum p-layer material for n-i-p type a-Si:H solar cells is not found at the onset of the transition between the amorphous to mixed phases, nor is it associated with a microcrystalline material with a large grain size and a high volume fraction of crystalline phase. (c) 2006 Elsevier B.V. All rights reserved.

聚合物载体缩硫醛大环螯合剂的合成和选择络合汞的性能以及做为高分子汞解毒促排药物的动物实验

在我国某些地区，汞的污染已达到十分严重的程度。如，第二松花江吉林市下游江段，江水总汞含量和鱼体含汞量已能和日本严重汞污染的水俣湾相比。在化学工业，仪表工业中，汞中毒列为严重性占第二位的职业病。因此，汞的污染防治已是急待解决的问题。各种含硫螯合剂可应用于含汞污水处理及汞中毒的治疗。Nyssen等1976年合成了一种缩聚型的缩硫醛大环螯合树脂，作者希望它能成为汞中毒的口服解毒药物。这种产物对Hg~(++)和CH_3Hg~+表现了极强的选择络合性能。但是由于其交联结构不利于Hg~(++)深入树脂内部，因此络合容量太低，仅为2毫克Hg~(++)/克。为了提高其络合能力并进而得到一种水溶性产物，我们合成了二种新的高分子缩硫醛大环螯合剂；其一，以聚苯乙烯为载体的缩硫醛大环螯合剂（简写为PS-S）。其二，以右旋糖苷为载体的缩硫醛大环螯合剂（简写为D-S）。前者做为螯合树脂表现了对Hg~(++)极强的选择络合能力，并且络合容量比缩聚型产物高十倍以上（达30-60毫克Hg~(++)/克）。后者经动物实验证明是一种无毒而有效的高分子汞解毒药。（一）PS-S的合成和络合性能1）醛基的引入采用了不同交联度的凝胶型聚苯乙烯（PS）树脂及不同孔径和表面的大孔型PS树脂做为骨架材料，并采用了二种不同的方法在PS上联结醛基。2）PS-S的合成采用了一系列巯基化合物与PS-CHO反应合成PS-S。例如，用乙二醇二巯基乙酸酯与PS-CHO反应，其它采用的巯基化合物还有：丁二醇二巯基乙酸酯、季戊四醇四巯基乙酸酯、乙硫醇、巯基乙酸、巯基乙酸乙酯等。同一骨架材料的上述各产物的静态Hg~(++)络合容量基本相同，可是含硫环的大小对络合容量影响不大。3）缩硫醛化产物模型化合物的研究合成了几种小分子缩硫醛化产物，对它们进行了MS、NMR谱分析，从以上三种不同类型的缩硫醛化产物本身及其对Hg~(++)作用物的稳定性比较，以第二类大环型产物稳定性最好。4）不同骨架结构的PS-S络合性能比较对不同交联度的凝胶型PS树脂为骨架的PS-S树脂，及不同孔经和比表面积的大孔型PS树脂为骨架的PS-S树脂，分别测定了对Hg~(++)的络合容量，结果表明：大孔型PS-S树脂络合容量最高。当其孔径在100-1000埃，比表面积100米~2/克时，静态络合容量可达65毫克Hg~(++)/克。5）大孔PS-S树脂络合性能的研究①研究了不同测定方法下（静态法、动态法、饱和法），不同测定条件（如树脂用量、Hg~(++)溶液浓度等）对产物络合容量测定的影响。在PS-S装柱反复络合洗脱十次后，树脂络合容量不下降。②不同PH测定PS-S络合容量表明：中性条件下对Hg~(++)络合容量较高。某些有机溶剂（如乙醇、二氧六环）加入Hg~(++)水溶液有利于络合容量的提高。而某些有机溶剂（如丙酮、乙酸）的添加却降低了树脂络合容量。③大孔PS-S树脂对不同金属离子(Pb~(++)、Co~(++)、Cd~(++)、Ca~(++)、Zn~(++))络合容量的测定表明：大孔PS-S树脂对Hg~(++)的络合容量比上述其它金属离子高几十倍到近千倍。（二）D-S的合成与性能研究了介质、温度、时间、反应物用量等条件对反应结果的影响，反应所用Dextran分子量31600，生成的D-CHO含醛基量0.66毫克当量/克。生成的D-S含硫量3.5～6%，分子量约3600。（三）PS-S和D-S对汞中毒巯基酶的解毒实验生物体汞中毒的一个重要毒理是汞使巯基酶中毒，我们采用了PS-S和D-S来对汞中毒的巯基酶-脲酶解毒，使失活的脲酶重新恢复活力，模拟药物在生物体内的解毒过程。实验表明：PS-S和D-S的解毒能力比相同重量的离子交换树脂、巯基树脂、巯基棉等都要强。而且很少量的PS-S和D-S就能使脲酶100%的恢复活力。不同用量的PS-S和D-S使汞中毒脉酶恢复活力的试验显示了良好的线性关系，尤其是D-S，它几乎等当量地（每二个硫原子络合一个汞原子）使汞中毒脲酶恢复活力。（四）D-S的汞解毒及代谢促排过程的同位素示踪试验1）当给小白鼠静脉注射极限注射量（达1毫升/只鼠）的6%D-S水溶液时未发生受试动物的死亡，即LD_(50) > 4000毫克/公斤体重，说明D-S是无毒的。同时病理镜检表明动物肝肾此时无异常。2）分别对10只小白鼠静注致死量的Hg~(++)，对其中一组注射D-S（0.2毫升/只）一次，结果3小时后对照组动物全部死亡时，给药组尚存活6只。D-S表面了对受试动物良好的保护作用。病理镜检表明D-S使肾脏的汞中毒病变有所缓解。3）用同位素~(125)I标记D-S，研究了口服，静注D-S在小白鼠体内的代谢情况。试验得到了D-S经静注，口服二种途径在小白鼠体内血、肝、肾、脾等主要脏器中的经时代谢曲线。六小时后D-S大部分代谢出体外，12天后全部代谢出体外。并进而得到了二种不同给药方式的药物代谢动力学方程。D-S口服为：C_血=0.1 (e~(-0.00183t)-e~(-0.01t))符合于一级吸收过程的单室模型 D-S静注为：C_血=0.384 e~(-0.645t) + 0.074 e~(-0.08t) + 0.042~(-0.00464t)符合于快速静注下的三室模型。4）采用~(203)Hg做了D-S口服、静注给药时对Hg~(++)的促排作用的实验，得到了二种给药方式下Hg~(++) 在小白鼠血、肝、肾、脑及全身的促排代谢经时曲线。实验表明D-S对汞有明显促排作用，其中口报组效果更好。D-S促排与代谢同位素示踪试验数据之间表现了有趣的相关性，有助于我们解释D-S对汞促排的机制。动物实验表明：D-S可能成为一种临床使用的副作用小的汞中毒解毒促排新药。

苄基环戊二烯基和茚基稀土二氯化物的合成与结构

本文通过元素分析，红外光谱、水解产物质谱、核磁共振、热失重分析及x-光单晶衍射分析，确认合成了下述两种新型稀土金属有机配合物。并对它们结构特点进行了研究和讨论。(1) ErCl_3 + C_6H_5CH_2C_5H_4Na → (THF) C_6H_5CH_2C_5H_4ErCl_2·3THF + NaCl; (2)GuCl_3·nTHF + C_9H_7K → (THF) C_9H_7GuCl_2·3THF + Kcl; 在第一种配合物的合成中，讨论了苄基环戊二烯与无水氯化稀土反应的条件。并首次成功的合成了苄基环戊二烯基稀土配合物。对于第二种化合物的合成，采取了与文献不同的反应条件及合成方式。提高了产物收率并第一次得到了茚基稀土二氯化物的单晶结构表征。上述两类配合物均对空气、水汽敏感，均可溶于四氢呋喃溶剂中，难以溶解在汽油等烷烃溶剂中。其中C_6H_5CH_2C_5H_4ErCl_2·3THF在DME·Et_2O甲苯等溶剂中也有较为良好的溶解性。在C_6H_5CH_2C_5H_4ErCl_2·3THF的红外光谱中，1600cm~(-1)、1490cm~(-1)和1450cm~(-1)为苯环骨架振动吸收峰，700cm~(-1)为取代苯环的面外弯曲振动吸收峰，2980cm~(-1)，2880cm~(-1)为CH_2的振动吸收峰，1600cm~(-1)、1040cm~(-1)和860cm~(-1)为环戊二烯基的特征吸收峰，1060cm~(-1)、910cm~(-1)为四氢呋喃分子的特征吸收峰，460cm~(-1)为Ln-Cl键的特征吸收峰。其分子结构见图I，晶体为单斜晶系，空间群为P21/n、晶胞参数a = 11.622A. b = 10.281A, c = 26.040A. β = 86.65°、V = 3106.09A、E = 4L。最终端离因子R = 0.050。中心离子Er~(3+)处于八面体中心，配位数为8。化合物C_9H_(17)GdCl_2·3THF的红外光谱中，出现的四氢呋喃分子特征峰为1050cm~(-1), 900cm~(-1)。茚基特征峰为845cm~(-1)和1020cm~(-1)；GuCl键吸收峰为460cm~(-1)，热失重分析表明，配合物分子中含有三个四氢呋喃分子。单晶结构见图II，单晶属单斜晶系，P21空间群，晶胞参数a = 10.468A, b = 11.888A, c = 11.854A, β = 108.46°, D = 1399.3A~3。最后一改性因子R = 0.042。平均键长Gd-C（环）为2.739，Gd-O为2.444A，两个Gd-Cl键长分别为2.583A和2.721A，夹角Cl(1)-Gd-Cl(2)为158.0°。比较所得两个配合物，它们具有相同的化学组成形式，单晶结构也非常相似。在苄基环戊二烯基化合物结构中Cl(1)-Er-Cl(2)夹角为156.3°，而C_9H_7GdCl_2·3THF中相应角度为158.0°，前者较后者小的不到两度，这可能与取代环戊二烯基的空间位阻小大有关。

取代环戊二烯基稀土有机氯化物的合成及其反应

本文通过无水LnCl_3(Ln = Pr.Nd.Gd)与两倍摩尔的叔丁基环戊二烯基碱金属盐在THF中60－80℃反应，分离到一类新的二（叔丁基环戊二烯基）稀土氯化物（T-DuCp）_2 2net.nTHF (Ln = Pr,Nd,n = 2 Ln = Gd,n = 1)，对它们进行了元素分析。红外光谱及水鲜色质谱的表征。对于配合物（t-BuCp）_2PrCl·2THF的单晶，测定了它的晶体结构，晶体层单斜晶系P21/C空间群，晶胞参数为：a = 15.080 b = 8.855 c = 21.196A, β = 110.34°V = 2653.9A~3 δ = 4，结构分析表明此配合物是一中性的单分子配合物。最后的R = Rw = 0.058平均Pr-C.2.81 Pr-Cent 2.53A, Pr-Cl及Rr-O键长分别为2.72与2.62A。本文通过Lnel_3(Ln = Nd.Pr.Ga)与等摩尔的叔丁基环戊二烯基碱金属盐在THF中60－80℃反应，分离到一类中性的单(叔丁基环戊二烯基)稀土二氯化物，并对它们进行了元素分析，红外光谱及水鲜色质谱的表征。本文通过轻稀土元素La,Pr的三氯化物与带基钠以1:2摩尔比在THF中70－80℃反应，分离到了二带基轻稀土氯化物（CaH_7）_2LaCl.2THF及[(CqH_7)_2PrCl.THF]_2。并且对此二配合物进行了元素分析。红外光谱及水鲜色质谱的表征。对于[(CuH_7)_2PrCl.TH]_2配合物，测定了它的晶体结构，这是第一个得到结构表征的茚基稀土氯化物，晶体层于单斜晶系，P_(21)/C空间群，晶胞参数为a = 7.808 b = 17.796 c = 14.070A β = 93.97°v = 1950.31A. E = 2最后的R = 0.045. Rw = 0.039结构分析表明此配合物以中性的二聚体形式存在。平均的Pr-C.2.81 Pr-Cent 2.53. Pr-Cl.2.84H Pr-O钻长2.54A。为了进一步研究不同配体对配合物结构的影响，我们还研究了Gael_3与Nae_5Mes以1:1摩尔比在THF中的反应，分离到了两种配合物[(NaTHF)(C_5MesGd.THF)_2Cl_5]_2.6THF(I)及L_5Me_5GdCl2.3THF(II)并且对配合物（I），测定了它的晶体结构，晶体层于三斜晶系。Pi空间群。晶胞参数a = 12.183 b = 13.638 c = 17.883A, α = 110.38 β = 94.04 γ = 99.44°, V = 2721.20A, E = 1。结构分析表明，此配合物是一种以两个Na原子通过THF中的O原子而桥联的金层有机配合物，在结构上有十分新颖的特点。在此配合物分子中含有四个Gd原子及二个Na原子，Na及Gd间以Cl桥键相联结，Gd-Gd_2 = 4.033 Gdll-Na = 2.818A。最后的R = 0.04M Rw = 0.042。本文还对（t-BuCp）_2P_2Cl.2THF与NaH及LiAlH4的反应进行了初步的研究，分离到（t-Bucp）_2PrH.2THF及(t-Bucp)_2P_2RIH_4.3THF两种新的氢化物，并且对它们进行了元素分析，红外光谱的表征，对于它们水鲜产物的气相分中的H_2，用气相色谱法进行了定性表征。

土壤优先水流及溶质先迁移的研究

本文以探讨土壤优先水流的特征和非吸附性离子优先先移为主要目的，通过对土壤优先水流穿透曲线的分析，定量的论证了优先水流的特征。在分析方法上进行了一系列尝试。得出了土壤优先水流的几个典型特征，即土壤优先水流的优先穿透、穿透曲线的不对称性、穿透曲线的拖尾和出流速率的不稳定性。在土壤优先水流特征分析的基础上，提出了判断土壤优先水流的定量方法。围绕非吸附性离子的优先迁移的实验结果，分析了阶跃输入和脉冲输入的非吸附性离子在不同水力负荷下的运移特点、优先水流的侧向入渗对土体中溶质分布的影响和耕作对土壤优先水流及溶质运移的影响。研究表明原状黑土、棕壤、暗棕壤和红壤中优先水流穿透时的孔隙容积分别为 0.05、0.051、0.048 和 0.042，穿透浓度为 0.759mg/l、0.087mg/l、0.115mg/l 和 0.117mg/l，在穿透时间上分别较对应的填充土柱提前 144、104、168 和 120 小时。原状土柱出流速率波动较大，其变异系数分别较对应的填充土柱高出 5～10 倍。在不同水力负荷下，原状土柱 Br 和 NO_3~- 的累积迁移量均明显高于填充土柱。不同水力负荷条件下，Br 和 NO_3~- 累积迁移量的差异不是来源于土壤优先水流，而是来源于土壤基质流。耕作可以影响土壤优先水流的穿透规律，并对土壤溶质运移构成影响。但耕作对土壤优先水流的穿透时间、穿透时的孔隙容积、穿透峰的出现和累积迁移量的影响并不遵从同一规律，这个过程不能通过孔隙的增减来简单描述的。优先水流存在下, Br 和 NO_3~- 在土壤中的分布表现为以大孔隙为中心向外径向递减，即 I 区溶质含量 ＞ II 区 ＞ III 区。土柱中溶质的径向分布以大孔隙为中心呈辐射状，表现距大孔隙越近溶质浓度越高。土壤优先水流可以引起非吸附性离子的快速大量迁移。这种迁移为深层次土壤和地下水中溶质浓度的大幅度提高提供了条件，一方面可能增加了深层次土壤污染修复的难度，一方面可以导致水体的富营养化，造成在下水污染的危险。

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.

内蒙古陈巴尔虎旗饮茶型氟铝联合中毒调查

目的查明内蒙古陈巴尔虎旗饮茶型氟、铝联合中毒原因。方法在陈巴尔虎旗3个牧区嘎查随机抽取93名20~50岁牧民进行发、血清、尿含氟、铝水平测定,并拍摄前臂、小腿、骨盆正位及腰椎正侧位X线片,同时检测饮水、牛奶、砖茶等氟和铝水平,以扎兰屯市地方病防治研究所的34名23~50岁职工为对照组。结果陈巴尔虎旗牧民发、血清、尿及饮用的奶茶含铝量分别是(22.34±8.06)mg/kg、(1.13±0.48)mg/L、(3.78±1.62)mg/L、(6.02±1.77)mg/L,含氟量分别是(1.21±0.63)mg/kg、(0.092±0.042)mg/L、(2.08±1.16)mg/L、(3.00±1.11)mg/L,饮水、牛奶含铝量分别是(39±16)μg/L、(0.553±0.179)mg/L,含氟量分别是(0.50±0.39)、(0.063±0.032)mg/L;对照组发、血清、尿铝分别是(5.80±2.14)mg/kg,(0.203±0.101)mg/L、(2.19±1.34)mg/L,含氟量分别是(1.17±0.68)mg/kg、(0.033±0.008)mg/L、(0.57±0.32)mg/L,牧民发、血清、尿铝及血清、尿氟均高于对照组(P<0.001)。牧民X线改变硬化型22.2%(20/88),疏松型37.5%(33/88),退行性变86.4%(79/88),对照组退行性变13.3%(4/30),其余改变未检出。结论陈巴尔虎旗牧区饮茶型氟中毒实际为饮茶型氟、铝联合中毒。

New high-dimensional networks based on polyoxometalate and crown ether building blocks

Three novel supramolecular assemblies constructed from polyoxometalate and crown ether building blocks, [(DB18C6)Na(H2O)(1.5)](2)Mo6O19.CH3CN, 1, and [{Na(DB18C6)(H2O)(2)}(3)(H2O)(2)]XMo12O40.6DMF.CH3CN (X = P, 2, and As, 3; DB18C6 = dibenzo-18-crown-6; DMF = N,N-dimethylfomamide), have been synthesized and characterized by elemental analyses, IR, UV-vis, EPR, TG, and single crystal X-ray diffraction. Compound 1 crystallizes in the tetragonal space group P4/mbm with a = 16.9701(6) Angstrom, c = 14.2676(4) Angstrom, and Z = 2. Compound 2 crystallizes in the hexagonal space group P6(3)/m with a = 15,7435(17) Angstrom, c = 30.042(7) Angstrom, gamma = 120degrees, and Z = 2. Compound 3 crystallizes in the hexagonal space group P6(3)/m with a = 15.6882(5) Angstrom, c = 29.9778(18) Angstrom, gamma = 120degrees, and Z = 2. Compound 1 exhibits an unusual three-dimensional network with one-dimensional sandglasslike channels based on the extensive weak forces between the oxygen atoms on the [Mo6O19](2-) polyoxoanions and the CH2 groups of crown ether molecules, Compounds 2 and 3 are isostructural, and both contain a novel semiopen cagelike trimeric cation [{Na(DB18C6)(H2O)(2)}(3)(H2O)(2)](3+). In their packing arrangement, an interesting 2-D "honeycomblike" "host" network is formed, in which the [XMo12O40](3-) (X = As and P) polyoxoanion "guests" resided.

Synthesis and crystal structure of bis(tetrahydrofurfurylindenyl) lanthanide chlorides

Lanthanocene chlorides (C4H7OCH2C9H6)(2)LnCl[Ln=Y(1); Ln=Gd(2)] were synthesized by the reaction of tetrahydrofurfurylindenyl lithium(in situ) with corresponding anhydrous lanthanide chorides in THF. The crystal structures of these two complexes were determined by X-ray diffraction and they were unsolvated monomeric complexes. They were stable in the air for several hours. Complexes 1 and 2 belong to the same crystal system (orthorhombic) and space group(P2(1)2(1)2(1)). The unit cell dimensions of complex 1 were a=1.042 52(9) nm, b=1.47455(12) nm, c=1.497 99(13) nm, Z=4, D-c=1.508 g/cm(3); The unit cell dimensions of complex 2 were a=1.037 01(10) nm, b=1.472 33(12) nm, c=1.513 54(14) nm, Z=4, D-c=1.699 g/cm(3). They have the same structure and different space configurations. The central metal atom is coordinated by two indenyl, two oxygen of the tetrahydrofurfuryl and one chlorine atom to form a distorted trigonal bipyramid.

Hydrothermal synthesis and structure of [Ni(en)(2)V6O14](n)

A new complex [Ni (en)(2)V6O14](n) was hydrothermally synthesized and characterized by 2-dimensional vanadium oxide framework pillared by Ni(en)(2)group. Single crystal X-ray analysis indicates that this compound crystallizes in monoclinic system, space group P2(1)/c with a=0. 892 17(18) nm, b = 1. 711 1(3) nm, c=0. 662 73(13) nm, beta=111. 58(3)degrees, V=0.940 8(3) nm(3), Z=2, D-c=2.501 g/cm(3), R=0. 042 3, omegaR=0. 060 9, S=1. 006.

THE CLEAVAGE REACTION OF THE MO-MO TRIPLE BOND - THE CRYSTAL-STRUCTURES OF MOLYBDENUM COMPLEXES [CPMO(CO)(2)(C(5)H(4)NS)], [CPMO(CO)(2)(C(9)H(6)NS)]O=PPH(3) AND [CPMO(CO)(2)(S(2)CNME(2)]

The reactions of [Cp2Mo2(CO)4] (1) with 2,2'-dipyridyl disulphide (C5H4NS-)2, 8,8'-diquinolyl disulphide (C9H6NS-)2 and tetramethyl thiuram disulphide (Me2NC(S)S-)2 in toluene solution resulted in the cleavage of the Mo-Mo triple bond to yield molybdenum complexes [CpMo(CO)2(C5H4NS)] (2), [CpMo(CO)2(C9H6NS)] (3) and [CpMo(CO)2(S2CNMe2)] (4), respectively. The molecular structures of 2, 3 . O=PPh3 and 4 were determined by X-ray diffraction studies. Crystals of 2 are monoclinic, space group P2(1)/n, with Z = 4, in a unit cell of dimensions a = 6.448(1), b = 12.616(2), c = 14.772(2) angstrom, beta = 92.85(1)-degrees. The structure was refined to R = 0.028 and R(w) = 0.039 for 1357 observed reflections. Crystals of 3 . O=PPh3 are triclinic, space group P1BAR, with Z = 2, in a unit cell of dimensions a = 11.351(3), b = 13.409(3), c = 9.895(2) angstrom, alpha = 94.59(2), beta = 90.35(2), gamma = 78.07(2)-degrees. The structure was refined to R = 0.033 and R(w) = 0.037 for 3260 observed reflections. Crystals of 4 are monoclinic, space group P2(1)/a and Z = 4 with a = 12.468(5), b = 7.637(2), c = 13.135(4) angstrom, beta = 96.62(3). The structure was refined to R = 0.032 and R(w) = 0.042 for 1698 observed reflections. Each of complexes 2-4 contains a cyclopentadienyl ligand, a cis pair of carbonyls and a chelate ligand (S,N donor or S,S donor). All the compounds have distorted square-pyramid structures.