998 resultados para 18-179


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合成了杂多化合物K8[P2W(18)Mo2Co2(H_2O)2O(68)]·MoO6·15H2O,依据XRD、IR、UV-Vis及XPS确定了其晶体结构和配位原子价态,考察了该化合物催化H2O2分解的动力学行为。

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Li~-和H~-因较强的亲水性,较难穿越液/液界面进行传输。本文报道了冠醚双环已基18冠6对Li~+,Na~+,Rb~-和H~-在水/硝基苯界面的促进传输行为,求得了相应促进传输过程的一系列参数,并对被传输离子在传输过程中的形态变化进行了初步的探讨。

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本文研究了电子轰击、化学电离条件下四碘合钴酸十八胺、四氯合钴酸十八胺加热分解产生的C_(18)H_(37)NH_3~+(m/z270)离子碰撞诱导解离谱,在低碰撞能量范围(0~10eV)、多次碰撞条件下观察到了远电荷碎裂反应,给出了反应所需内能的估计值,该离子比直接由正十八胺质子化得到的离子具有较高的内能。

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In this paper a carbon fibre (CF) microelectrode modified with the 2:18-molybdodiphosphate anion by simple adsorption is described and its electrochemical behaviour is reported. The 2:18-molybdodiphosphate anion (alpha-P2Mo18O626-), which is a Dawson structure, undergoes five successive multielectron reductions in acidic solution. The first three redox waves correspond to the two-electron process, and the last two waves are four-electron and six-electron processes respectively. On the basis of the experimental results it is shown that the electrode process of alpha-P2Mo18O626- on the CF electrode in acidic solution is simultaneously controlled by the diffusion and adsorption of alpha-P2Mo18O626- anions. When the concentration of the alpha-P2Mo18O626- in the solution is reduced, the electrode process mainly exhibits non-diffusion-controlled behaviour, and the diffusion-limited process takes over as the concentration of alpha-P2Mo18O626- becomes higher. The CF electrode modified with a thin film of alpha-P2Mo18O626- exhibits very good stability and redox behaviour in aqueous acidic solution. The alpha-P2Mo18O626- is reduced to heteropoly blue, with an accompanying protonation process. The addition of more than six electrons to the alpha-P2Mo18O626- anion in an aqueous solution does not result in its decomposition. The result obtained is not the same as that reported previously.

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A piston sediment core E017 from the middle-southern Okinawa Trough was investigated. A preliminary study of the deep-water evolution since 18 cal. ka BP was performed based on the quantitative census data of benthic foraminiferal fauna, together with planktonic foraminiferal oxygen and carbon isotope, AMS(14)C dating, and the previous results achieved in the southern Okinawa Trough. The result shows that the benthic fauna was dominated by Bulimina aculeata (d'Orbigny), Uvigerina peregrina (Cushman), Hispid Uvigerina and Uvigerina dirupta (Todd) during the glaciation-deglaciation before 9.2 cal. ka BP, while Epistominella exigua (Brady), Pullenia bulloides (d'Orbigny), Cibicidoides hyalina (Hofker), Sphaeroidina bulloides (d'Orbigny) and Globocassidulina subglobosa (Brady) predominated the fauna in the post-glacial period after 9.2 cal. ka BP. The benthic foraminifera accumulation rate (BFAR), paleoproductivity estimates and benthic foraminiferal assemblage conformably indicate that surface water paleoproductivity and organic matter flux during the glaciation-deglaciation were higher than those of the post-glacial period in the middle-southern Okinawa Trough, and gradually enhanced from the southern to the central Okinawa Trough during the glaciation-deglaciation, which could be caused by the discrepancy of the terrigenous nutrients supply. High abundances of E exigua, an indicator of pulsed organic matter input, after 9.2 cal. ka. BP may indicate that the intensity of seasonally riverine pulsed flux during the post-glacial period was stronger than that of the glaciation-deglaciation period, and the seasonal influx in the central trough might be stronger than in the south. The temporal distributions of the typical species indicating bottom water oxygen content and ventilation condition show that the ventilation of the bottom water during the post-glacial period is more active than the glaciation-deglaciation, which reflects that the evolution of the intermediate and deep waters of the northwestern Pacific during the last glaciation has no evident influence on the deep-water of the middle-southern Okinawa Trough. Additionally, the variations in agglutinated benthic foraminiferal abundance and other carbonate dissolution proxies indicate that carbonate dissolution gradually increased since the last 18 ka in the Okinawa Trough and rapidly enhanced at 9.2 cal. ka BP. The modern shallow carbonate lysocline could form at 3 cal. ka BP.

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近年来,由于对海区不合理的开发,我国浅海贝类筏式养殖接连遭受重创,这亟需从理论上和实践中确定养殖容量和养殖模式。本文在我国北方典型养殖海湾四十里湾对筏式养殖的贝类开展了现场生理生态学研究,对贝类对浮游植物等悬浮颗粒物的处理过程即贝类对颗粒有机物及营养元素C、N、P的摄食、吸收、排泄、排粪和生长进行了剖析,分析了贝类在沿岸养殖生态系中的物质和营养循环中所扮演的角色,为海区贝类养殖容量和养殖模式的最终确定提供了基础数据。另外,本文还对海水、沉积物及生物体中磷的分析方法进行了大量的实验工作。主要结果如下:① 比较系统地评述了双壳贝类的生物沉积(biodeposition)的原理、测定方法及其生态效应。贝类通过生物沉积在沿岸生态系中的物质和营养循环中扮演着重要的角色。国际上已有不少研究专门报道了贝类在海区现场的生物沉积。而在我国,这方面的研究却罕见。② 综述了双壳贝类各种形态的 N 和 P 排泄及其生态效应。对于我国广泛养殖 的栉孔扇贝、海湾扇贝和牡蛎等双壳贝类的TDN、TP排泄尚未见报道。 ③ 在6~7月,在四十里湾的不同养殖海区(8个站位)对扇贝的生物沉积进行了现场测定。在整个四十里湾海区,一龄栉孔扇贝(壳高 41.1±4.1mm,软体干重 0.48±O.10 g/ind))每个每天所产生生物沉积物干重平均为59.9mg,对颗粒有机质(POM)、颗粒有机碳(POC)、颗粒有机氮(PON)和颗粒有机磷(POP)的生物沉积速率范围及平均值分别为: 6.88、3.09、0.392 和 0.022mg/ind·d。还在一个站位测定了海湾扇贝(壳高 24.6±2.3mm;软体干重 O.14g/ind)的生物沉积速率为 24.3mg/ind·d,或179.2mg/g·d。不同站位一龄栉孔扇贝的生物沉积速率有较大变化,这主要与饵料浓度不同有关。二龄栉孔扇贝(壳高60.9±8.2mm;软体干重1.91±0.32 g/ind)的生物沉积速率平均为 112.7mg/ind·d,对POM、POC、PON和POP的沉积速率分别是一龄扇贝的1.85倍、1.68倍、1.77倍和2.33倍。养殖海区与非养殖海区比较,前者近海底沉积速率是后者的 1.51~3.47 倍。根据以上数据,作者计算了中等规格栉孔扇贝(用壳高 41.1±4.8mm 扇贝估算)在四十里湾在夏季每天的生物沉积量达 162 吨(干重),或18.6tPOM、8.37tPOC、1.06tPON和60kgPP。在四十里湾的贝类筏式养殖海区,可以估计贝类每年因生物沉积的生产而循环427tN和98.OtP(包括20.0t OP的贡献),它们能分别满足浮游藻类生产所需求N和P的17.0%和28.3%(其中OP贡献 6.9%)。可见,贝类在养殖生态系的物质和营养盐循环中扮演着重要的角色。高密度、大面积的贝类养殖使大量的生物沉积物聚集于海底,可能对海区环境产生冲击。作者分析,98年8月份烟台养殖区赤潮的发生很可能与海底生物沉积物营养盐的快速释放以及栉孔扇贝大面积死亡而使浮游藻类失去了摄食控制有关,而风平浪静和养殖笼对水流的阻挡也为赤潮的发生提供了有利条件。④ 采用半现场流水系统法测定了栉孔扇贝在不同养殖密度、不同养殖模式(扇贝单养、贝藻混养、贝藻参混养)中的生物沉积。实验时间尺度大,前后计80天。结果说明扇贝的生物沉积速率与其养殖密度呈反比关系。养殖密度的高低影响饵料浓度的变化(两者呈负相关的对数函数关系),而饵料浓度的高低直接决定着扇贝的生物沉积速率的高低,两者呈正相关关系(生物沉积速率与POC和叶绿 a 分别呈对数和指数函数关系)。不仅生物沉积物的数量与养殖密度(或饵料浓度)有关,生物沉积物的质量同样与养殖密度(或饵料浓度)有关。栉孔扇贝的养殖使沉积物的有机质含量及C、N 和 P 含量降低,且密度越高,它们的含量越低。这反映了扇贝对环境的适应能力。在海带和扇贝的混养模式中,海带对扇贝生物沉积物的数量和质量不构成影响,当然这是在海带不影响浮游植物数量的前提下得出的结果。而实际上在自然海区两者可能是竞争关系。⑤ 对从海区取回到实验室的多种滤食性动物,包括经济双壳贝类(栉孔扇贝、海湾扇贝、长牡蛎、贻贝、菲律宾蛤仔等)和养殖中的污损动物(栖海鞘、玻璃海鞘、藤壶、玟斑稜蛤)的 N 和 P 排泄进行了测定,包括排泄成分和排泄速率。在N排泄中,NH_4-H 占主要部分,如笼式养殖的双壳贝类 NH_4-N 占总N排泄的70%以上,平均值范围为70.8~80.1%。氨基酸是第二大排泄成分,平均占总N排泄的10~25%。其它形态的N,如尿素、亚硝酸盐和硝酸盐也有检出,如双壳贝类尿素氮在总氮排泄中占 2~5%。但在双壳贝类中未检出尿酸氮。比较而言,海鞘、藤壶的尿素氮相对高一些。在P排泄中,OP约占TDP排泄的15~27%。栉孔扇贝TDP排泄速率为0.281μmol/h·ind。作者以实验室测定结果计算,在整个四十里湾的夏季,所养殖的双壳贝类每天将排泄4.54t总溶解氮,其中NH_4-N 3.36t、Amino-N 0.69t、Urea-N 0.2t。 同时每天磷的排泄为0.57t TDP,其中OP O.15t。对面积为1.3 * 10~4hm~2的海区而言,贝类的N、P排泄分别能满足浮游植物生产所需N、P的44%和40%。尽管Urea-N所占比例有限,但也能满足海区浮游植物所需 N 的 2%左右。以上说二月高密度的贝类养殖对海区生态系统营养盐循环的影响是很显著的。附着动物(柄海鞘等)的N、P 排泄也不容忽视,它们分别能满足浮游藻类生产所需 N、P 的 ll%和 12%。它们一方面通过排泄和排粪加速营养盐和物质的循环对浮游植物的生长产生刺激作用;另一方面,对藻类产生摄食控制,如果海区中滤食性动物太多,即使营养盐再丰富也难以使浮游植物大量繁殖,这无疑将影响滤食性动物的生长速率。⑥ 运用近年来发展起来的生物沉积法对四十里湾半现场流水系统中贝类的滤水率、吸收率、生长率、生态效率等生理生态学参数进行了测定。栉孔扇贝(收获时规格0.194~0.412g软体干重/ind)滤水率平均为3.65 1/ind·h。扇贝放养密度和饵料浓度没有显著关系。扇贝的总摄食率平均为3.98mg/ind·h,对POM、POC、PON的 摄食率范围为0.84~1.87、0.335~0.748、0.0515~O.1293mg/ind·h。扇贝的摄食率随放养密度的升高而降低,与POM呈正相关关系。扇贝的吸收速率受密度和饵料浓度的影响不明显。扇贝对N的吸收效率较C、P稍高,对总有机质的吸收效率为75.9±4.1%,如此高的吸收效率与低饵料浓度有关。扇贝氨基酸泄漏所损失的能量高于排氨的能量损失。代谢能与吸收能呈明显的正相关关系。SFG与饵料浓度呈正相关关系。总生长效率K1(* 100)变化较大,范围为20~49;净生长效率K,K_2(* 100)随POM的升高而升高。扇贝对N的总生态效率范围为6.2~12.8%(平均9.9%),这高于对C(平均5.9%)和P(平均4.1%)的总生态效率。扇贝对POC、PON和PP的生长余力(SFG_C、SFG_N、SFG_P)平均分别为197、46.8和6.2μg/ind·h,它们分别与POC、PON和PP呈正比关系。扇贝对N的净生长率高于对C和P的净生长率。在N的预算中,如果仅考虑NH_4-N的排泄而忽视其它形态氮的排泄,将会产生很大偏差(平均约20%)。扇贝贝壳生长所需的能量在整个扇贝生长所需能量的9.0~15.1%(平均 11.2%);贝壳C、N和P在扇贝生长中所占的比例分别为10.5~17.8%、9.4~16.1%和8.7~15.O%。可见,贝壳不管在能量预算还是在元素预算中都不应该被忽视。理论计算而得到的SFG和SFG_C、SFG_N、SFG_P与扇贝的实际生长和扇贝C、N、P的实际增长量之间呈正相关关系,但前者明显过高地估计了扇贝的生长。⑦ 运用生物沉积法在四十里湾养殖海区现场对栉孔扇贝的生理生态学特征进行了研究。不同海区扇贝的滤水率有变化,一龄扇贝(41.1±4.1mm,软体干重 0.48±O.10g/ind)滤水率变化范围为 0.72~2.54(平均 1.27)1/ind·h 或 1.65~5.97(平均 2.61)1/g·h。与半现场研究结果一致,滤水率与TPM没有明显关系,而摄食率却与TPM呈正相关关系。二龄扇贝(软体干重 1.91±0.32g/ind)滤水率为 2.09~3.99(平均 3.10)1/ind·h。吸收速率与POM(或TDM)呈正相关关系,与饵料质量(POM/TPM)无明显的相关关系。吸收效率AE_(POM)与TPM(或POM)没有相关关系,却与饵料质量呈明显 的正相关关系。扇贝对POC、PON和PP的吸收效率平均分别为68.9%、64.0%和63.6%。不同海区SFG差别很大。一龄扇贝SFG范围为-O.174~24.08 J/ind·h,SFG与饵料浓度POM呈正相关关系。SFG负值的出现主要与低饵料浓度有关。SFG_C、SFG_N、SFG_P分别与POC、PON和PP呈正相关关系。在N的生长余力计算中,如果仅考虑NH_4-N排泄,而不考虑其它形态N的排泄,就可能产生相当大的偏差,偏差范围为11~360%,这高于半现场的偏差值,显然SFG_N越低,产生的偏差就越大。这说明在饵料不足、扇贝生长受到限制的环境下进行N生长余力的计算时必须考虑其它形态N的排泄。⑧ 对四十里湾养殖海区一些双壳贝类和藻类的化学组成和有机净生产量进行了讨论。不同双壳贝类的软体有机碳含量差别不大,而N含量差异较大。栉孔扇贝N含量最高(占软体干重的12.36%),而牡蛎、毛蚶软体N含量相对较低,为 8~9%。从双壳贝类贝壳的组成来看,贻贝和菲律宾蛤仔贝壳中N含量最高,分别为 0.55% 和 0.56%;而栉孔扇贝贝壳N含量相对较低,在 O.1%左右。贻贝贝壳有机磷含量 (308ppm) 也明显高于栉孔扇贝贝壳(62.1 ppm)。不同海区海带的 C/N 比值较高,变化明显,范围为17.36~30.23。石莼与此相似。大型藻类高 C/N 比值说明海区营养元素N的不足。海带的不同部位N含量差别很大,中带部和边叶在不同海区有较大变化,即对环境的营养状况比较敏感。紫贻贝贝壳中C、H、N 和 P 的含量在整个贻贝中占有相对大的比例,分别为 30.4%、30.2%、31.8%和 29.6%。

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There have been no detailed studies on reproductive biology of the Great Cormorant (Phalacrocorax carbo sinensis) in Qinghai-Tibet Plateau. We conducted such investigations during the breeding seasons of 1999 and 2000 in Qinghai-Lake Bird Isle, China. Great Cormorants began to migrate to Qinghai-Lake for reproduction from the middle of March and left from early October at the end of reproduction. Nesting periods were from early April to mid June and took 50 days. Egg-laying occurred during the three weeks from the end of April to 20 May. Females typically laid an egg every 1-2 days until clutch completion. Mean clutch size in the study area over two years was 3.3 (SE +/- 0.13, N = 68, range 1-5) and most (66.18%) fell within the range 3-4 eggs. Length of eggs averaged 61.01 mm and breadth averaged 34.13 mm. Fresh egg weight averaged 57.34 g (SE +/- 0.36, range 46.0-73.7 g, N = 179). Hatching success was 48.7% and fledging success was 64.9% over two years. Decline of available fish resources in Qinghai-Lake might be one of main causes of lower reproductive success. The causes of chick loss were possibly high altitude, high winds and prolonged rain.

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目前,ROV(无人遥控潜水器)在水下工程和海洋石油工业上得到了广泛应用。ROV是通过各种水下作业工具来完成相应的作业任务。本文介绍了一种ROV携带海上石油钻井平台需要的新型水下作业工具一钢圈取放器。