973 resultados para Dayananda Sarasvati, Swami, 1824-1883.


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本文简要介绍了光学触觉传感器阵列的用途和特点,并对各种类型的结构、原理和存在问题作了较详细的分析说明。

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The 3-D velocity images of the crest and upper mantle beneath the region of 112° -124°E, 28°-39°N including the Dabie-Sulu orogenic belt are reconstructed by using 36405 P-wave arrivals of 3437 regional and 670 distant earthquakes during the period from 1981 to 1996, and gridding the area of 0.5° * 0.5°. The results of tomography demonstrate that: 1. The results of tomographic imaging show a broad heterogeneity in P wave velocity structure for the lithosphere beneath the Dabie-Sulu orogenic belt. 2. In the Dabie orogenic belt, the velocity patterns in the crust are different among various tectonic units. The Dabie and Qinling orogenic belts are remarkable in the tomographic images, and in mm the Hongan and Dabie blocks in the Dabie orogenic belt are also imaged very distinguishably. 3. A velocity (about 5.9~6.0 km/s) layer exists in the Dabie block at depth between 15~25 km, which is coincident with the low-resistance layer at the depth of 12-23 km, being inferred to be the tectonic detachment zone and suggesting that the extension detachment structure was formed in the middle crust. Beneath the southern and northerm Dabie tectonic units, the north-dipping high-velocity (at level of 6.5 ~ 6.6 km/s) block was developed in the crust, which might be correlated with the UHP rockswith low content of the meta-ultramafic rocks. This result is in agreement with the geological observation on the surface. 4. The velocity image at 40 km depth reveals the features at the top of mantle and the configuration of the Moho discontinuity. The depth of the Moho changes slightly along the trend of the orogenic belt. It in Hongan block is less than 40 km, but it is different in the western and eastern parts of the Dabie block, the former is more than 40 km, and the latter less than or equal to 40 km. The remnant of the mountain root exists between the Shangcheng-Macheng fault and the line of Huoshan-Yuexi-Yingshan in the Dabie orogenic belt, and beneath the southern and northern Dabie tectonic units. However, the thickness of the Moho is about 40 km and there is no obvious changes, which suggest that the Dabie orogenic belt has been experienced quite in the gravity equilibration. The Moho's depth in the Sulu is less than 40 km. 5. There is a dipping slab-like high-velocity body in the uppermost mantle. It is sandwiched by slow velocities and exists beneath the Dabie-Sulu orogenic belt in the range of depths between the Moho discontinuity and 110 km at least. This high-velocity body outlines a picture of the slab interpreted as the remnant of the Triassic subducted YZ. 6. The Sulu orogenic belt displays "crocodilian" velocity structure, the upper crust of the Yangtze thrusted over the Huabei crest, and the Huabei crust indented into the Yangtze crust, where the ancient subduction zone of the Yangtze lithosphere located. Based on the previous geological data, this structure is not related with the collision between the Yangtze and Sino-Korean Blocks, but caused by the sinistral offset of the Tan-Lu Fault. Studied on the velocity structure of the eastern Huabei lithosphere indicates: 1. The 'present-day' lithosphere of the eastern Huabei is between 40-100 km thick with greatly thinned lithosphere around the Bohai Sea. Generally, thickness of the lithosphere in this region decreased eastwards. 2. The attenuation of the lithosphere is attributed to the strongly uplift of the asthenosphere. In the area between the Taihang Mountains and the Tan-Lu Fault, there is a 'lever' with red low velocity belt, it is clearly defined, transverse continuity, depth between 100-150 km, local variations visible, and an upwards trend towards the Bohai Sea. Generally, the velocity structure in the mantle beneath the lithosphere displays irregular column-shape consisting of alternating high and low velocities, and when cold high velocity ancient lithosphere connects with the hot low velocity mantle materials forming precipitous compact structure. More heat pathways from the mantle occur towards the Tan-Lu Fault. 3. The strongly irregular characteristics of the contact between the asthenosphere and the lithosphere is induced by the long-term hot, chemical erosion and alteration on the contact. 4. There are still preserved high velocity lithosphedc root beneath Huabei with 'block-shape' distribution and surrounded by hot materials. Results of our studies indicate that the evolution models of the eastern China mantle are characterized by the direct contact between the uplifted lithosphere and the Huabei Craton accompanying the upwelling of the deep mantle materials. At the contact betwen the lithosphere and the asthenosphere, the upwelled mantle materials replaced and altered the lower lithosphere forming the metasome through the hot and chemical modifications impacted on the Craton lithosphere, and changed it into the lithosphere gradually, resulting in the lithospheric thinning. Thus, the lithospheric thinning is the result of the upwelling of the asthenosphere.

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对河水样品中低含量硼的分离方法及硼同位素组成的测定进行了研究。将约1000mL河水样品分别用硼特效树脂,混合树脂富集和纯化后,紫外灯照射去除有机质,蒸发浓缩至小体积,采用正热离子质谱法进行硼同位素组成的测定。全流程回收率在95%以上,同位素稀释法测得全流程空白为41ng。经该方法处理后的样品能满足同位素质谱测定的需要。不产生同位素分馏,测试精度基本在0.6‰以内。

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A broca da bananeira ou moleque, Cosmopolites sordidus (Germar, 1824) (Coleoptera, Curculionidae), constitui-se na principal praga da bananeira, provocando perdas de até 80% na produção. As larvas são causadoras do dano por produzirem galerias no rizoma, enfraquecendo a planta e reduzindo o peso do cacho, que acaba tombando pela ação do vento. No entanto, por estarem protegidas dentro do rizoma, a verificação de sua presença é mais difícil e também o seu controle. Quando adulto, o besouro de coloração preta mede aproximadamente 1 cm de comprimento e é ativo no período noturno. O moleque se espalha facilmente pelo uso de mudas infestadas ou pelo caminhamento. Durante o dia, o besouro é encontrado entre as bainhas mais externas da bananeira e em restos de pseudocaule que permanecem sobre o solo após a colheita, os quais atuam como verdadeiros esconderijos para a broca.

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O CPAA esta testando um metodo de conservacao fundamentado em aspectos genetico-ecologicos. Em uma area de 0,25ha, procurou-se representar as estrategias utilizadas pelas especies autoctones para manterem-se em equilibrio no ecossistema tropical: diversidade, densidade e variabilidade genetica. A pesquisa, iniciada em janeiro de 1994, estuda a conservacao de recursos geneticos de sete especies frutiferas (Theobroma grandiflorum, T. cacao, Bactris gasipaes, Euterpe spp, Myrciaria dubia, Rollinia mucosa e Couma utilis) e cinco florestais (Hevea spp, Ceiba pentandra, Jacaranda copaia, Buchenavia huber, Trattinickia burserifolia), utilizando-se tres espacamentos. As caracteristicas biometricas das plantas sao anualmente medidas e, apos cinco anos, a viabilidade tecnica sera avaliada quanto a sobrevivencia e capacidade das especies em deixar descendentes. Preliminarmente, as especies que apresentaram valores superiores na avaliacao de estabelecimento foram C. pentandra entre as florestais (medias de 4,76m de altura e 11,46cm de diametro, a 50cm do solo) e R. mucosa entre as fruteiras (media de 3,71m de altura e 6,28cm de diametro, a 50cm do solo).

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Sketch of life

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http://www.archive.org/details/johnludwigkrapfe00kretiala

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http://www.archive.org/details/historyofcatholi00sheaiala

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http://www.archive.org/details/maryandifortyyea00riggrich

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In this report, we extend our study of the intensity of mistreatment in distributed caching groups due to state interaction. In our earlier work (published as BUCS-TR-2006-003), we analytically showed how this type of mistreatment may appear under homogeneous demand distributions. We provided a simple setting where mistreatment due to state interaction may occur. According to this setting, one or more "overactive" nodes generate disproportionately more requests than the other nodes. In this report, we extend our experimental evaluation of the intensity of mistreatment to which non-overactive nodes are subjected, when the demand distributions are not homogeneous.

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This thesis is structured in the format of a three part Portfolio of Exploration to facilitate transformation in my ways of knowing to enhance an experienced business practitioner’s capabilities and effectiveness. A key factor in my ways of knowing, as opposed to what I know, is my exploration of context and assumptions. By interacting with my cultural, intellectual, economic, and social history, I seek to become critically aware of the biographical, historical, and cultural context of my beliefs and feelings about myself. This Portfolio is not exclusively for historians of economics or historians of ideas but also for those interested in becoming more aware of how these culturally assimilated frames of reference and bundles of assumptions that influence the way they perceive, think, decide, feel and interpret their experiences in order to operate more effectively in their professional and organisational lives. In the first part of my Portfolio, I outline and reflect upon my Portfolio’s overarching theory of adult development; the writings of Harvard’s Robert Kegan and Columbia University’s Jack Mezirow. The second part delves further into how meaning-making, the activity of how one organises and makes sense of the world and how meaning-making evolves to different levels of complexity. I explore how past experience and our interpretations of history influences our understandings since all perception is inevitably tinged with bias and entrenched ‘theory-laden’ assumptions. In my third part, I explore the 1933 inaugural University College Dublin Finlay Lecture delivered by economist John Maynard Keynes. My findings provide a new perspective and understanding of Keynes’s 1933 lecture by not solely reading or relying upon the text of the three contextualised essay versions of his lecture. The purpose and context of Keynes’s original longer lecture version was quite different to the three shorter essay versions published for the American, British and German audiences.