994 resultados para 208-1263C
Resumo:
Compositions and abundances of calcareous nannofossil taxa have been determined in a ca 170 kyrs long time interval across the Paleocene/Eocene boundary at 1-cm to 10-cm resolution from two ODP Sites (1262, 1263) drilled along the flank of the Walvis Ridge in the South Atlantic. The results are compared to published data from ODP Site 690 in the Weddell Sea. The assemblages underwent rapid evolution over a 74 kyrs period, indicating stressed, unstable and/or extreme photic zone environments during the PETM hyperthermal. This rapid evolution, which created 5 distinct stratigraphic horizons, is consistent with the restricted brief occurrences of malformed and/or weakly calcified morphotypes. The production of these aberrant morphotypes is possibly caused by major global scale changes in carbon cycling in the ocean-atmosphere system, affecting also photic zone environments. No marked paleoecologically induced changes are observed in abundances of the genera Discoaster, Fasciculithus and Sphenolithus at the Walvis Ridge sites. Surprisingly, there is no significant correlation in abundance between these three genera, presumed to have had a similar paleoecological preference for warm and oligotrophic conditions.
Resumo:
The Paleocene-Eocene Thermal Maximum (PETM), ca. 55 Ma, was a period of extreme global warming caused by rapid emission of greenhouse gases. It is unknown what ended this episode of greenhouse warming, but high oceanic export productivity over thousands of years (as indicated by high accumulation rates of barium, Ba) may have been a factor in ending this warm period by carbon sequestration. However, Ba has a short oceanic residence time (~10 k.y.), so a prolonged global increase in Ba accumulation rates requires an increase in input of Ba to the ocean, increasing barite saturation. We use a novel proxy for barite saturation (Sr/Ba in marine barite) to demonstrate that the seawater saturation state with respect to barite did not change across the PETM. The observations of increased barite burial, no change in saturation, and the short residence time can be reconciled if Ba burial decreased at continental margin and shelf sites due to widespread occurrence of suboxic conditions, leading to Ba release into the water column, combined with increased biological export production at some pelagic sites, resulting in Ba sink reorganization.
Resumo:
Barite accumulation rates (BAR) have been measured from 12 DSDP/ODP site globally (DSDP site 525, 549 and ODP site 690, 738, 1051, 1209, 1215, 1220, 1221, 1263,1265 and 1266A) to reconstruct the export production across Paleocene Eocene Thermal Maximum (PETM) around 55.9 million year ago. Our results suggesting a general increase in export productivity. We propose that changes in marine ecosystems, resulting from high atmospheric partial pressure of CO2 and ocean acidification, led to enhanced carbon export from the photic zone to depth, thereby increasing the efficiency of the biological pump. We estimate that an annual carbon export flux out of the euphotic zone and into the deep ocean waters could have amounted to about 15 Gt during the PETM. About 0.4% of this carbon is expected to have entered the refractory dissolved organic pool, where it could be sequestered from the atmosphere for tens of thousands of years. Our estimates are consistent with the amount of carbon redistribution expected for the recovery from the PETM.
Resumo:
Contenido: Estructuras mentales y principios racionales / Lorenzo Vicente Burgoa – Autonomía moral y deliberación en Santo Tomás de Aquino / Ciro E. Schmidt Andrade – Thomas Aquinas and the reality of time / Steven C. Snyder – Fe y razón en Ramón Llull / Marc Egea I Ger – Idealismo y personalismo en Husserl / Francisco Leocata – El discurso no consensuado de Jürgen Habermas / Marisa Villalba de Tablón – Hacia el tercer milenio : el clima posmoderno y la recuperación de la naturaleza humana del hombre (observaciones tomistas) / William R. Darós – Razón, voluntad y praxis / María Celestina Donadío Maggi de Gandolfi – Meditación sobre la felicidad / Alberto Caturelli – “Y llegarán a ser virtuosos” : ley jurídica positiva penal y educación / Héctor H. Hernández – Todos los hombres desean la felicidad / Ignacio E. M. Andereggen – Justicia y derecho en Ley Natural y Derechos Naturales de John Finnis / Carlos I. Massini Correas – El itinerario antiguo y medieval de la negación nominalista de la metafísica / Mario Enrique Sacchi – Notas y comentarios -- Bibliografía
Resumo:
利用高能离子研究了110keV的He+注入Al2O3单晶及随后230MeV的208Pb27+辐照并在不同温度条件下退火样品的光致发光的特性.从测试结果可以清楚地看到在375nm,390nm,413nm和450nm出现了强烈的发光峰.经过600K退火2h后测试结果显示,390nm发光峰增强剧烈,而别的发光峰显示不明显.在900K退火条件下,390nm的发光峰开始减弱相反在510nm出现了较强的发光峰,到1100K退火完毕后390nm的发光峰完全消失,而510nm的发光峰相对增强.从辐照样品的FTIR谱中看到,波数在460—510cm-1间的吸收是振动模式,经过离子辐照后,吸收带展宽,随着辐照量的增大,Al2O3振动吸收峰消失,说明Al2O3振动模式被完全破坏.1000—1300cm-1之间为Al-O-Al桥氧的伸缩振动模式,辐照后吸收带向高波数方向移动.退火后的FTIR谱变化不大.
Resumo:
主要研究了110keV的He~+高温注入Al_2O_3单晶及1.1MeV/u的~(208)Pb~(27+)辐照注氦Al_2O_3样品的光致发光的特性。从测试结果可以清楚地看到在375nm,413nm和450nm处出现了强烈的发光峰。并且在600K,5×10~(16) ions/cm~2剂量点,样品的发光峰是最强的。这表明He~+注入Al_2O_3后使带隙中深的辐射中心复合的效率大幅度提高,极大的增强了其发光强度,而且发光伴随着蓝移现象。而经过高能~(208)Pb~(27+)辐照后的样品,在390nm出现了新的发光峰,从FTIR谱中我们能够看到,可能是~(208)Pb~(27+)辐照相对沉积膜出现一定的晶化,其中含有许多纳米尺寸的Al_2O_3晶粒所致。
Resumo:
介绍了一种弧形靶框夹芯208Pb靶的制备工艺,包括核靶的制备装置和制备方法、核靶厚度和均匀性的控制和测量方法,并对结果进行了讨论。制备采用旋转蒸镀法,该法可以大大提高材料的利用率。所制靶的结构为30μg/cm2C+361μg/cm2208Pb+15μg/cm2C,同一次所制的靶平均厚度为361μg/cm2,不均匀性小于9.8%。其性能能够很好地满足超重核实验研究的要求。
Resumo:
以18 O重离子束轰击厚天然铅靶 ,通过多核子转移反应生成2 0 8Hg核 .辐照铅片放入离线熔化铅靶气相热色谱装置中处理 ,分离并收集汞元素产物 .完成了 4πΔEβγ γ ,γ X(γ)关联事件谱及γ射线时序单谱测量 .建议了 2 1条γ射线 ,以及能量为 1 3 65,1 72 7keV的两条2 0 8Tl新能级的2 0 8Hgβ- 衰变部分γ纲图 .
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用半经典模型考虑20Na+208Pb→p+19Ne+208Pb的Coulomb解离过程。用MonteCarlo方法计算前角放置的望远镜阵列对Coulomb解离碎片的探测效率。讨论了天体环境下p+19Ne→20Na俘获反应道的低能级共振截面测量的可行性。