90 resultados para 12E-
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Biographical essays of each author in French; selections in Spanish
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Mode of access: Internet.
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Mode of access: Internet.
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Tetrahedrite compounds Cu12-xMnxSb4S13 (0 <= x <= 1.8) were prepared by solid state synthesis. A detailed crystal structure analysis of Cu10.6Mn1.4Sb4S13 was performed by single crystal X-ray diffraction (XRD) at 100, 200 and 300 K confirming the noncentrosymmetric structure (space group I (4) over bar 3m) of a tetrahedrite. The large atomic displacement parameter of the Cu2 atoms was described by splitting the 12e site into a partially and randomly occupied 24g site (Cu22) in addition to the regular 12e site (Cu21), suggesting a mix of dynamic and static off-plane Cu2 atom disorder. Rietveld powder XRD pattern and electron probe microanalysis revealed that all the Mn substituted samples showed a single tetrahedrite phase. The electrical resistivity increased with increasing Mn due to substitution of Mn2+ at the Cu1+ site. The positive Seebeck coefficient for all samples indicates that the dominant carriers are holes. Even though the thermal conductivity decreased as a function of increasing Mn, the thermoelectric figure of merit ZT decreased, because the decrease of the power factor is stronger than the decrease of the thermal conductivity. The maximum ZT = 0.76 at 623 K is obtained for Cu12Sb4S13. The coefficient of thermal expansion 13.5 +/- 0.1 x 10(-6) K-1 is obtained in the temperature range from 460 K to 670 K for Cu10.2Mn1.8Sb4S13. The Debye temperature, Theta(D) = 244 K for Cu10.2Mn1.8Sb4S13, was estimated from an evaluation of the elastic properties. The effective paramagnetic moment 7.45 mu(B)/f.u. for Cu10.2Mn1.8Sb4S13 is fairly consistent with a high spin 3d(5) ground state of Mn.
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[EN]A comprehensive evaluation of the fatty acid composition of subcutaneous adipose tissue from beef cattle produced in western Canada was undertaken to determine if the current Canadian grading system is able to distinguish classes of animals with value added potential due to their fatty acid composition. Grades included youthful Canadian Yield Grade 1 A/AA beef, under (YUTM) and over (YOTM) 30 mo of age and the four mature grades (D1, D2, D2 and D4). Subcutaneous fat between the 12th and 13th ribs over the longissimus muscle was obtained from 18_21 animals per grade. Fatty acids were analyzed using a combination of silver-ion HPLC and GC with a highly polar 100 m column. There were no differences in total trans-18:1 content amongst grades, but adipose tissue from grade D1, D2 and D4 had more 11t-18:1 than YUTM (PB0.05), whereas adipose tissue from YUTM carcasses had more 10t-18:1 than all other grades (PB0.05). Adipose tissue from YUTM carcasses also had less total CLA (PB0.05) than the D grades, mainly due to a lower level of 9c,11t-CLA, but they had slightly more 7t,9c-CLA and 10t,12c-CLA (PB0.05). Adipose tissue from YOTM and D grades contained more n-3 fatty acids relative to YUTM (0.56% vs. 0.29%; PB0.05) and lower n-6:n-3 ratios (PB0.05). Overall, older animals (YOTM and D grades) had adipose tissue compositions with higher levels of fatty acids with reported health benefits. Taken together, these higher levels may provide opportunities for value added marketing if regulatory authorities allow claims for their enrichment based on demonstrated health benefits. Higher concentrations of beneficial fatty acids, however, need to be considered within the context of the complete fatty acid profile and it would be important to demonstrate their advantages in the presence of relatively high levels of saturated fatty acids.
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Based on the analyses of foraminifer and accelerator mass spectrometer radiocarbon dating in DGKS9603 core from mid-Okinawa Trough close to bottom, oscillation curve, which expressed the relation between the surface water temperature and the depth, has been obtained by using foraminifer analysis and calculation of FP-12E transfer function. The whole core indicated seven cold phases and eight warm phases. Obvious expression of low temperature event during Middle and Late Holocene, YD,H1,H2,H3 and H4 events, as well as the short cold phase during the middle last glacial period, implied that short shifts since 50 kaBP would have been global significance. Sedimentation rate during cold phases is usually faster than that in warm stages, with the lowest rate in Holocene, which may be connected with rising sea level and principal axial of Kuroshio Current moving to west. Volcanic activities highly developed in Okinawa Trough during the Quaternary period, thus abundant volcanic glass and pumice were well preserved.
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2005年6月,中法国际合作在西太平洋海域执行IMAGES XII-MD147 Micro Polo1航次科学考察时,由法国极地研究所R/V Marine Dufresne极地考察船利用Calypso重力取样器于冲绳海槽南部钻取了34.2米长MD05-2908柱状样。本文利用AMS14C测年数据建立了该孔的年代模型,对该孔的浮游有孔虫动物群落进行了分析,并利用FP-12E浮游有孔虫转换函数和Q型因子分析方法对该孔浮游有孔虫数据进行了研究,对全新世以来的黑潮流系演化和古环境记录进行了讨论。 结果表明,中晚全新世存在着5次洪水爆发期,洪水爆发期与当时温暖气候相对应,而高海平面对洪水的爆发也产生了影响。进入全新世以来的6790~4000a B.P.期间,黑潮流一直有稳步增强的趋势,黑潮流始终位于冲绳海槽内;4000~3000a B.P.期间,黑潮强度减弱或者发生明显东偏,冲淡水影响增强;3000a B.P.以后黑潮强度逐渐增强,1650~0a B.P.为中晚全新世以来黑潮活动最强的时期,在600a B.P.和140a B.P.左右存在低值,黑潮强度短暂减弱。普林虫低值事件在MD05-2908孔中有很好的体现,对该事件进行了进一步定年,其发生时间为3900~2800a B.P.,持续时间为1100a,该事件的发生可能与东亚冬季风加强有关。 冲绳海槽中晚全新世气候变化可以分为四个阶段: 6790~4800a B.P.低温阶段,4800~4100a B.P.高温阶段,4100~2400a B.P.低温阶段,2400~0a B.P.波动高温阶段。通过与中国及世界其它地方对比可以识别出6.3~5.9、5.5、4.6~4.2、3.6~3.0、2.9~2.4、1.3~1.0、0.5~0.1ka B.P.六个降温事件,为全新世气候波动在深海高分辨率沉积记录中的响应提供了有力支持。该孔SST频谱分析结果显示,存在着3008a、1061a这种千年尺度的周期,以及215a、123a、103~107a、81~78a以及73~71a等周期,表明该孔SST变化与太阳活动强度是密切相关的。 中晚全新世以来,黑潮流在冲绳海槽逐步加强,到4000aB.P.左右达到最大,然后4000~3000a B.P.期间,黑潮强度明显减弱或者发生东偏,3000aB.P.以后,黑潮强度持续增强,在近1000aB.P.波动较大。 对冲绳海槽地区14个柱状样氧同位素以及P.obliquiloculata丰度进行研究,发现LGM以来,黑潮流可能仍然在冲绳海槽地区活动,并没有移出海槽外,但是由于其强度减弱,其流径发生了很大变化。
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Two new lathyrane diterpenes, 3 beta,5 alpha-dihydroxy-15 beta-cinnamonyloxy-14-oxoladiyra-6Z, 12E- diene (1) and 3 beta,5 alpha,20-trihydroxy-15 beta-cinnamoyloxy-14-oxolathyra-6Z, 12E-diene (2), were isolated from the roots of Euphorbia kansuensis. Their structures were determined by spectroscopic methods. (C) 2008 Elsevier B.V. All rights reserved.
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Variante(s) de titre : La Vie et les arts liturgiques : notes d'art et d'archéologie
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Collection : Théâtre contemporain illustré ; 11e et 12e livraisons
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F. 1 Temporal (incompl. du début ; commence à la 12e leçon de l'office de l'Ascension) : — Fête-Dieu (addit.) (9). F. 116-194v Sanctoral (incompl.) : s. Étienne (116) ; — s. Benoît (189). 12 leçons.
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Référence bibliographique : Rol, 60018