952 resultados para Catulo, Cayo Valerio, CA. 87-CA.54 a.C
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The use of hindered amine light stabilizers (HALS) to retard thermo- and photo-degradation of polymers has become increasingly common. Proposed mechanisms of polymer stabilisation involve significant changes to the HALS chemical structure; however, reports of the characterisation of these modified chemical species are limited. To better understand the fate of HALS and determine their in situ modifications, desorption electrospray ionisation mass spectrometry (DESI-MS) was employed to characterise ten commercially available HALS present in polyester-based coil coatings. TINUVIN® 770, 292, 144, 123, 152, and NOR371; HOSTAVIN® 3052, 3055, 3050, and 3058 were separately formulated with a pigmented, thermosetting polyester resin, cured on metal at 262 C and analysed directly by DESI-MS. High-level ab initio molecular orbital theory calculations were also undertaken to aid the mechanistic interpretation of the results. For HALS containing N-substituted piperidines (i.e., N-CH3, N-C(O)CH3, and N-OR) a secondary piperidine (N-H) analogue was detected in all cases. The formation of these intermediates can be explained either through hydrogen abstraction based mechanisms or direct N-OR homolysis with the former dominant under normal service temperatures (ca. 25-80 C), and the latter potentially becoming competitive under the high temperatures associated with curing (ca. 230-260 C). © 2013 Elsevier Ltd. All rights reserved.
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We have studied the carbonate mineral kamphaugite-(Y)(CaY(CO3)2(OH)·H2O), a mineral which contains yttrium and specific rare earth elements. Chemical analysis shows the presence of Ca, Y and C. Back scattering SEM appears to indicate a single pure phase. The vibrational spectroscopy of kamphaugite-(Y) was obtained using a combination of Raman and infrared spectroscopy. Two distinct Raman bands observed at 1078 and 1088cm(-1) provide evidence for the non-equivalence of the carbonate anion in the kamphaugite-(Y) structure. Such a concept is supported by the number of bands assigned to the carbonate antisymmetric stretching mode. Multiple bands in the ν4 region offers further support for the non-equivalence of carbonate anions in the structure. Vibrational spectroscopy enables aspects of the structure of the mineral kamphaugite-(Y) to be assessed.
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Proteiinit ovat elämälle välttämättömiä orgaanisia yhdisteitä, jotka koostuvat yhdestä tai useammasta aminohappoketjusta. Proteiinien toiminnan määrää niiden kolmiulotteinen rakenne, joka taas riippuu pitkälti proteiinien aminohappojärjestyksestä, sekvenssistä. Proteiinien tunnettujen sekvenssien määrä kasvaa DNA-sekvensoinnin tuloksena selvästi nopeammin kuin selvitettyjen kolmiulotteisten rakenteiden, konformaatioiden, määrä. Proteiinien rakenteitakin tunnetaan jo lähes 45 000, joten niiden tilastollisella analyysillä on yhä merkittävämpi osuus uusien proteiinien rakenteen määrittämisessä, ennustamisessa ja suunnittelussa. Työssä etsittiin pentapeptidejä (viiden aminohapon pituisia ketjuja), joilla on sama konformaatio kaikissa tunnetuissa proteiinien rakenteissa. Näitä rakennuspalikoita voisi käyttää suoraviivaisessa proteiinien suunnittelussa halutun kolmiulotteisen rakenteen aikaansaamiseksi. Aineistona käytettiin proteiinitietopankin joulukuussa 2007 sisältämiä rakenteita, joihin kuului lähes 45 000 proteiinin kolmiulotteista rakennetta. Aineiston laajuuden takia rakennuspalikoita etsittiin kahdessa vaiheessa vertailemalla pentapeptidien rakenteen keskeisten atomien (CA, CB, O, C ja N) sijaintia proteiinien aminohappoketjuissa. Työssä löytyi yli 9000 rakennuspalikkaa, pentapeptidiä, joista jokaisella oli sama konformaatio yli 12 eri rakennetiedostossa, niissä ilmoitettujen tarkkuuksien rajoissa. Löydetyistä rakennuspalikoista 48:lla oli täysin sama konformaatio kaikkialla, mistä ne löydettiin. Näistä useimmin esiintyneitä voi käyttää suoraan proteiinien rakenneanalyysissä valmiina kolmiulotteisen rakenteen osina. Eri konformaatioihin laskostuvia identtisiä pentapeptidejä löytyi yli 266 000 kappaletta. Rakennuspalikoiden stabiiliudesta johtuen ne saattavat olla tärkeitä proteiinien fysikaalisen mallinnuksen tutkimus- ja vertailukohteina. Käytännön kannalta työn lupaavin tulos oli se, että rakennuspalikoita löytyi eri vasta-aineiden rakennetiedostoista. Ehkäpä juuri vasta-aineita voitaisiin suunnitella työssä esitetyillä menetelmillä.
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High-temperature reactions (Ca 900-degrees-C) involving albite, K-feldspar or plagioclase and K, Ba-or K, Sr chlorides were experimentally studied. These experiments reveal that the reaction between K-exchanged albite, potash feldspar, or plagioclase and Ba-chloride/Ba-K chloride results in the formation of celsian by the breakdown of the starting feldspar structure above 800-degrees-C. Sr-feldspar does not form under similar conditions. A size-effect of the large M-site cation appears to be responsible for the formation of celsian. The reaction between K-feldspar and barium chloride may be used as a method for synthesizing celsian.
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Garnet-kyanite-staurolite gneiss in the Pangong complex, Ladakh Himalaya, contains porphyroblastic euhedral garnets, blades of kyanite and resorbed staurolite surrounded by a fine-grained muscovite-biotite matrix associated with a leucogranite layer. Sillimanite is absent. The gneiss contains two generations of garnet in cores and rims that represent two stages of metamorphism. Garnet cores are extremely rich in Mn (X(Sps) = 0.35-038) and poor in Fe (X(Alm) = 0.40-0.45), whereas rims are relatively Mn-poor (X(Sps) =0.07-0.08), and rich in Fe (X(Alm), = 0.75-0.77). We suggest that garnet cores formed during prograde metamorphism in a subduction zone followed by abrupt exhumation, during early collision of the Ladakh arc and Karakoram block. The subsequent India-Asia continental collision subducted the metamorphic rocks to a mid-crustal level, where the garnet rims overgrew the Mn-rich cores at ca. 680 degrees C and ca. 8.5 kbar. PT calculations were estimated from phase diagrams calculated using a calculated bulk chemical composition in the Mn-NCKFMASHT system for the garnet-kyanite-staurolite-bearing assemblage. Muscovites from the metamorphic rocks and associated leucogranites have consistent K-Ar ages (ca. 10 Ma), closely related to activation of the Karakoram fault in the Pangong metamorphic complex. These ages indicate the contemporaneity of the exhumation of the metamorphic rocks and the cooling of the leucogranites. (C) 2011 Elsevier B.V. All rights reserved.
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Sapphirine + quartz and orthopyroxene + sillimanite occur in garnet from an Mg-Al granulite from the Central Zone of the Limpopo Complex in South Africa. Textural evidence and a chemical gradient in garnet between the zones preserving the inclusions argue for the formation of sapphirine + quartz after orthopyroxene + sillimanite. Petrological observations, pressure-temperature phase diagrams, and compositional and model proportion results on isopleths indicate the sapphirine + quartz + garnet + orthopyroxene (high-Al) assemblage as the peak metamorphic assemblage (similar to 1050 degrees C at similar to 8.5 kbars), whereas orthopyroxene (low-Al) + sillimanite represents the prograde stage (at ca. 900 degrees C at similar to 8.5 kbars). Our report of these two diagnostic ultrahigh-temperature mineral assemblages in garnet from an Mg-Al granulite is unique, given the rare occurrence of sapphirine + quartz postdating orthopyroxene + sillimanite assemblage in granulites.
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Blends of bromo-terminated polystyrene (PS-Br) and poly(vinyl methylether) (PVME) exhibit lower critical solution temperatures. In this study, PS-Br was designed by atom transfer radical polymerization and was converted to thiol-capped polystyrene (PS-SH) by reacting with thiourea. The silver nanoparticles (nAg) were then decorated with covalently bound PS-SH macromolecules to improve the phase miscibility in the PS-Br-PVME blends. Thermally induced demixing in this model blend was followed in the presence of polystyrene immobilized silver nanoparticles (PS-g-nAg). The graft density of the PS macromolecules was estimated to be ca. 0.78 chains per nm(2). Although the matrix and the grafted molecular weights were similar, PS-g-nAg particles were expelled from the PS phase and were localized in the PVME phase of the blends. This was addressed with respect to intermediate graft density and favourable PS-PVME contacts from microscopic interactions point of view. Interestingly, blends with 0.5 wt% PS-g-nAg delayed the spinodal decomposition temperature in the blends by ca. 18 degrees C with respect to the control blends. The scale of cooperativity, as determined by differential scanning calorimetry, increased only marginally in the case of PS-g-nAg; however, it increased significantly in the presence of bare nAg particles.
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Early afterdepolarizations (EADs), which are abnormal oscillations of the membrane potential at the plateau phase of an action potential, are implicated in the development of cardiac arrhythmias like Torsade de Pointes. We carry out extensive numerical simulations of the TP06 and ORd mathematical models for human ventricular cells with EADs. We investigate the different regimes in both these models, namely, the parameter regimes where they exhibit (1) a normal action potential (AP) with no EADs, (2) an AP with EADs, and (3) an AP with EADs that does not go back to the resting potential. We also study the dependence of EADs on the rate of at which we pace a cell, with the specific goal of elucidating EADs that are induced by slow or fast rate pacing. In our simulations in two-and three-dimensional domains, in the presence of EADs, we find the following wave types: (A) waves driven by the fast sodium current and the L-type calcium current (Na-Ca-mediated waves); (B) waves driven only by the L-type calcium current (Ca-mediated waves); (C) phase waves, which are pseudo-travelling waves. Furthermore, we compare the wave patterns of the various wave-types (Na-Ca-mediated, Ca-mediated, and phase waves) in both these models. We find that the two models produce qualitatively similar results in terms of exhibiting Na-Ca-mediated wave patterns that are more chaotic than those for the Ca-mediated and phase waves. However, there are quantitative differences in the wave patterns of each wave type. The Na-Ca-mediated waves in the ORd model show short-lived spirals but the TP06 model does not. The TP06 model supports more Ca-mediated spirals than those in the ORd model, and the TP06 model exhibits more phase-wave patterns than does the ORd model.
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Sodium-ion batteries have been extensively pursued as economic alternatives to lithium-ion batteries. Investigating the polyanion chemistry, alluaudite structured Na2Fe2II(SO4)(3) has been recently discovered as a 3.8 V positive electrode material (Barpanda et al., Nature Commun., 5: 4358, 2014). Registering the highest ever Fe-III/Fe-II redox potential (vs. Na/Na+) and formidable energy density, it has opened up a new polyanion family for sodium batteries. Exploring the alluaudite family, here we report isotypical Na2+2xMn2-xII(SO4)(3) (x = 0.22) as a novel high-voltage cathode material for the first time. Following low-temperature (ca. 350 degrees C) solid-state synthesis, the structure of this new alluaudite compound has been solved adopting a monoclinic framework (s.g. C2/c) showing antiferromagnetic ordering at 3.4 K. Synergising experimental and ab initio DFT investigation, Na2+2xMn2-xII(SO4)(3) has been found to be a potential high-voltage (ca. 4.4 V) cathode material for sodium batteries.
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Resumen: Nuestro conocimiento de algunos aspectos de las Historias de Polibio se ha incrementado significativamente durante las dos últimas décadas. En ese sentido, ha habido ciertos desarrollos importantes con respecto a aspectos culturales de la obra, cuyo alcance ha ido permitiendo repensar durante estos años algunos presupuestos clásicos sobre la relación entre Polibio, Roma y el mundo helenístico. Proponemos aquí ofrecer un rápido análisis de las tres principales líneas de estudio propuestas por los estudiosos, cuyo alcance es considerado, en efecto, como un total reubicación del historiador aqueo al interior del universo cultural del mundo helenístico.
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Abstract: Focusing on Obadiah and Psalm 137, this article provides biblical evidence for an Edomite treaty betrayal of Judah during the Babylonian crisis ca. 588–586 B.C.E. After setting a context that includes the use of treaties in the ancient Near East to establish expectations for political relationships and the likelihood that Edom could operate as a political entity in the Judahite Negev during the Babylonian assault, this article demonstrates that Obadiah’s poetics include a density of inverted form and content (a reversal motif) pointing to treaty betrayal. Obadiah’s modifications of Jeremiah 49, a text with close thematic and terminological parallels, evidence an Edomite treaty betrayal of Judah. Moreover, the study shows that Obadiah is replete with treaty allusions. A study of Psalm 137 in comparison with Aramaic treaty texts from Sefire reveals that this difficult psalm also evidences a treaty betrayal by Edom and includes elements appropriate for treaty curses. The article closes with a discussion of piecemeal data from a few other biblical texts, a criticism of the view that Edom was innocent during the Babylonian crisis, and a suggestion that this treaty betrayal may have contributed to the production of some anti-Edom biblical material.
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Aristófanes nasceu em Atenas entre 450 e 445 a.C. e morreu por volta de 388 a.C. Considerado o principal representante da comédia antiga, em suas peças predominavam a sátira política e a social. Suas primeiras comédias foram assinadas sob pseudônimo e somente após ‘Os Acarnianos’ (ou ‘Acarnanos’) tornou-se conhecido. Da sua obra apenas onze peças conservaram-se integralmente. Esta coleção, em dois volumes, contém onze peças. O primeiro volume inclui ‘Os Plutos’ (publicada no ano de 388 a.C.), sua ultima comédia; ‘As Nuvens’ (423 a.C.); ‘As Rãs’ (405 a.C.); ‘Os Cavaleiros’ (424 a.C.); ‘Os Acarnianos’ (425 a.C.) e ‘As Vespas’ (422 a.C.). O segundo volume contém ‘Os Pássaros’ (414 a.C.); ‘A Paz’(421a.C.); ‘A Assembleia das mulheres’ (392 a.C.); ‘As Convocadas’ (411 a.C.) e ‘Lisistrata’ (411 a.C.)
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In 2001, representative samples of adult Columbia Basin chinook (Oncorhynchus tshawytscha), sockeye (O. nerka), and coho salmon (O. kisutch) populations at Bonneville Dam were collected. Fish were trapped, anesthetized, sampled for scales and biological data, revived, and then released adult migrating salmonids. Scales were examined to estimate age composition; the results contributed to an ongoing database for age class structure of Columbia Basin salmon populations. Based on scale analysis of chinook salmon, four-year-old fish (from brood year [BY] 1997) comprised 88% of the spring chinook, 67% of the summer chinook, and 42% of the Bright fall chinook salmon population. Five-year-old fish (BY 1996) comprised 9% of the spring chinook, 14% of the summer chinook, and 9% of the fall chinook salmon population. The sockeye salmon population at Bonneville was predominantly four-year-old fish (81%), with 18% returning as five-year-olds in 2001. The coho salmon population was 96% three-year-old fish (Age 1.1). Length analysis of the 2001 returns indicated that chinook salmon with a stream-type life history are larger (mean length) than the chinook salmon with an ocean-type life history. Trends in mean length over the sampling period for returning 2001 chinook salmon were analyzed. Chinook salmon of age classes 0.2 and 1.3 show a significant increase in mean length over time. Age classes 0.1, 0.3, 0.4, 1.1, 1.2, and 1.4 show no significant change over time. A year class regression over the past 12 years of data was used to predict spring, summer, and Bright fall chinook salmon population sizes for 2002. Based on three-year-old returns, the relationship predicts four-year-old returns of 132,600 (± 46,300, 90% predictive interval [PI]) spring chinook and 44,200 (± 11,700, 90% PI) summer chinook salmon for the 2002 runs. Based on four-year-old returns, the relationship predicts five-year-old returns of 87,800 (± 54,500, 90% PI) spring, 33,500 (± 11,500, 90% PI) summer, and 77,100 (± 25,800, 90% PI) Bright fall chinook salmon for the 2002 runs. The 2002 run size predictions should be used with caution; some of these predictions are well beyond the range of previously observed data.
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预计到本世纪末,大气CO2浓度将会增加到540~970ppm,大气CO2浓度升高所引起的全球气候变化已经受到广泛的关注。植物生长依赖CO2,并且对大气CO2浓度升高在结构和生理上产生响应。目前已有大量报道,从生态系统、群落、种群、个体、器官、组织、生理以及生化等水平上研究高浓度CO2所对植物产生的影响。但是有关高浓度CO2对植物有性生殖影响的报道却很少,同时多数实验均建立在短期的生殖响应,忽视了植物在长期高CO2浓度下具有的反馈作用和CO2浓度变化对植物的驯化作用。植物有性生殖与其生态适应性和农作物籽粒产量的关系极为密切;同时,植物有性生殖特性的变化,也可作为预测植物对全球气候变化响应的重要指标之一。为此,利用高浓度CO2对植物进行长期选择实验将很有必要。研究结果将为预测未来大气CO2浓度增加的条件下陆地生态系统的演变趋势、全球变化对植物有性生殖响应的方式和机制提供新的思路和有效方法。 在本研究中,我们以模式植物拟南芥(Arabidopsis thaliana)作为实验材料,利用370和700ppm CO2对其进行连续8个世代处理,首先研究高浓度CO2对每一个世代的拟南芥有性生殖特性的影响,然后比较各个世代中各种生殖特性指标变化的规律,从细胞、组织和个体尺度上揭示拟南芥有性生殖对全球变化的响应模式。此外,在700ppm CO2处理下,我们对拟南芥叶片生理、生化以及结构的变化进行了相关研究。两部分研究结果及主要结论如下: 首先,在每一个世代中,与370ppm CO2相比较,700ppm CO2处理显著促进了拟南芥开花,缩短生长周期,增加花、角果及种子等生殖的产量,降低种子N含量,提高种子C/N比、种子千粒重以及生殖生物量所占总生物量的比例等,而对种子萌发率、角果所含种子数目以及角果长度则无显著影响。但是, 通过对相同CO2浓度处理条件下,不同世代之间的研究结果比较发现,不同世代之间相关的生殖生物学指标并无显著差异。 其次,高浓度CO2显著降低叶片气孔密度、气孔指数、气孔导度以及蒸腾速率。在高浓度CO2处理下,叶肉细胞中叶绿体数目、叶绿体宽度和表观面积、淀粉粒大小和数量、叶片和细胞壁厚度等都显著增加,但是基粒内囊体膜的数量却显著下降。叶片中碳水化合物如可溶性总糖、淀粉以及纤维素含量在高浓度CO2下分别显著增加71.9%、78.7% 和 22.3%。此外,在高浓度CO2处理下,叶片中多数激素如如吲哚乙酸(indole-3-acetic acid, IAA)、赤霉素(gibberellin, GA)、玉米素核苷(zeatin riboside, ZR)、二氢玉米素核苷(dihydrozeatin riboside, DHZR)和异戊烯基腺苷(isopentenyl adenosine, iPA)均都显著地增加,而脱落酸(abscisic acid, ABA)含量却有所下降。最后,叶片中各种矿物质元素含量如N、P、K、CaMg等含量在高浓度CO2处理下也都显著下降,而C/N比增加24.8%。 以上结果表明: (1) 在每一个世代中,700ppm CO2处理对拟南芥各种有性生殖特性具有显著的影响,但是高浓度CO2处理对植物所引起的效应在多个世代以内并不能够传递给后代,所以在多个有性生殖世代内,高浓度CO2处理对植物生长、生殖没有驯化作用。 (2) 在高浓度CO2处理下,拟南芥叶片中叶绿体超微结构的变化,可能主要是由于叶绿体中淀粉粒数量和体积大小显著增加而引起。 (3) 在高浓度CO2处理下,由于拟南芥叶片内与促进细胞分裂与伸长的激素含量显著增加,从而对拟南芥植株生长发育速率的提高起了重要的作用。 (4) 拟南芥生长在高浓度CO2条件下,其叶片中各种矿质元素含量(如N、P、K、CaMg)均显著降低,究其原因可能是,第一由于叶片中碳水化合物含量的显著增加而对矿物质元素具有稀释作用;第二由于蒸腾速率下降,引起矿质元素从根部随着蒸腾流运输到地上部分的含量相应减少。
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Twelve commonly occurring coenocytic and siphonaceous species of marine benthic algae, i.e., Bryopsis pennatta Lamouroux, Caulerpa chemnitzia (Esper) Lamouroux, Ca. faridii Nizamuddin, Ca. manorensis Nizamuddin, Ca. racemosa (Forsskal) J. Agardh, Ca. taxifolia. (Vahl) C. Agardh, Chaetomorpha antennina (Bory de Saint-Vincent) Kutzing, Cladophora uncinella Harvey, Codium decorticatum (Woodward) Howe, Co. flabellatum Nizamuddin, Co. iyengarii Borgesen, and Valoniopsis pachynema (Martens) Borgesen, belonging to four different orders of the class Bryopsidophyceae, division Chlorophyta, were collected from the intertidal region of different coastal areas near Karachi (Pakistan) and investigated taxonomically. Codium decorticatum is a new report from this region and Co. decorticatum, Co. flabellatum and Co. iyengarii are described for the first time from the coast of Pakistan.