Impact of the closure of Indonesian seaway on climate: A numerical modeling study

Using a global OGCM and its relevant coupled ocean-atmosphere GCM with the contemporary, 6 MaBP and 14 MaBP oceanic topography, respectively, a series of numerical experiments are implemented in order to investigate the effect of the north shift of Australian continent on the tropical oceanic circulation, especially the formation of the western Pacific warm pool. The numerical experiments of the individual OGCM forced by the modern atmospheric circulation indicate that the closure of Indonesian passage results in warming in the tropical Pacific Ocean and cooling in the tropical Indian Ocean; furthermore, it also results in change in source of the Indonesian Through Flow (ITF) water, e.g. ITF mainly originates from the south Pacific at 14 MaBP, but it mainly originates from the north Pacific now. The coupled model shows similar results as the individual OGCM qualitatively.     

底水稠油油藏水平井含水规律预测方法

针对底水稠油油藏水平井出水位置难以确定的问题,通过建立底水稠油油藏物理及数学模型,利用Green函数、Newman乘积方法和叠加原理推导底水稠油油藏水平井非均匀产液的压力响应解析解,采用Stehfest数值反演算法得到考虑井筒储集效应和表皮效应的底水稠油油藏水平井分段产液试井井底压力解.通过绘制水平井分段试井典型图版,进行流动阶段划分及分析,进而得到不同生产段长度、生产段数目、生产段位置分布、流量分布等影响因素影响规律,并绘制相关解释图版.矿场应用实例验证了研究结果的有效性及广阔的应用前景.     

铝制沐浴水热回收器的初步设计

对一种新型的铝制沐浴水热回收器进行初步设计。该沐浴水热回收器具有成本低,回收效率高等优点。介绍其工作原理,并以某三口之家为例,计算该热回收器的节能效益。结合沐浴水余热使用情况不合理的现状,讨论其发展前景。     

When and how did plate tectonics begin？ Theoretical and empirical considerations

Plate tectonics is the horizontal motion of Earth’s thermal boundary layer (lithosphere) over the convecting mantle (asthenosphere) and is mostly driven by lithosphere sinking in subduction zones. Plate tectonics is an outstanding example of a self organizing, far from equilibrium complex system (SOFFECS), driven by the negative buoyancy of the thermal boundary layer and controlled by dissipation in the bending lithosphere and viscous mantle. Plate tectonics is an unusual way for a silicate planet to lose heat, as it exists on only one of the large five silicate bodies in the inner solar system. It is not known when this mode of tectonic activity and heat loss began on Earth. All silicate planets probably experienced a short-lived magma ocean stage. After this solidified, stagnant lid behavior is the common mode of planetary heat loss, with interior heat being lost by delamination and “hot spot” volcanism and shallow intrusions. Decompression melting in the hotter early Earth generated a different lithosphere than today, with thicker oceanic crust and thinner mantle lithosphere; such lithosphere would take much longer than at present to become negatively buoyant, suggesting that plate tectonics on the early Earth occurred sporadically if at all. Plate tectonics became sustainable (the modern style) when Earth cooled sufficiently that decompression melting beneath spreading ridges made thin oceanic crust, allowing oceanic lithosphere to become negatively buoyant after a few tens of millions of years. Ultimately the question of when plate tectonics began must be answered by informa- tion retrieved from the geologic record. Criteria for the operation of plate tectonics includes ophiolites, blueschist and ultra-high pressure metamorphic belts, eclogites, passive margins, transform faults, paleomagnetic demonstration of different motions of different cratons, and the presence of diagnostic geochemical and isotopic indicators in igneous rocks. This record must be interpreted individually; I interpret the record to indicate a progression of tectonic styles from active Archean tectonics and magmatism to something similar to plate tectonics at ~1.9 Ga to sustained, modern style plate tectonics with deep subduction——and powerful slab pull——beginning in Neoproterozoic time.     

管壳式换热器与板式换热器选型参考

阐述管壳式换热器与板式换热器各自的特点,并通过对此两种换热器在闭式循环冷却水系统中水水换热器的性能参数的对比和计算,详细论述了管壳式换热器和板式换热器的结构性能的比较,为换热器的选型提供参考。     

数值沉积模拟在澳大利亚W区块沉积储层研究中的应用

利用古环境、古生物年龄、钻井岩性、岩心等资料，应用DinosoS软件对澳欠利亚W区块的Elang—Frigate组进行了数值沉积模拟。研究区重点层位Elang-Frigate组共划分为3个层序，海平面为向上脉动加深变化形式，东南方为主要物源方向．通过各个层序的构造图以及井资料读取的各个层序的残露厚度，利用软件自动·趺复古地貌、古构造的功能，得到了相对真实的沉积背景，利用这些参数进行了三维数值模拟，进一步得到了本地区沉积体系的时空展布特征。结果显示，该区的三角洲－河口湾沉积体系，具有早期浪控、晚期潮控，近源扇三角洲、相对远源三角洲的复合型沉积特点。     

降低海南铁矿烧结固体燃耗的研究

对海南铁矿烧结燃耗高的原因及降低燃耗的途径进行了研究．试验结果表明：用３０％澳矿代替海南粉矿，燃耗从１０１．８ｋｇ／ｔ降到９０．２５ｋｇ／ｔ；添加０．０３％添加剂，随着料层高度增加，节能效果变得明显，但是当料层高度超过４５０ｍｍ时，生产率降低；焦粉分加，可使焦粉配比由７．０％降到６．２％～６．５％，燃耗由９６．６５ｋｇ／ｔ降到８３．２５ｋｇ／ｔ．     

板式蒸发式冷凝器传热传质的数值模拟

基于VOF算法,建立了板式蒸发式冷凝器气-液两相降膜流动传热传质的计算模型,该模型考虑了表面张力动量源项和气-液相间传热传质源项．并利用该模型,定量分析了不同壁面热流密度、液相进口温度和空气速度下竖直板面的温度分布、气-液界面处潜热和显热换热量的相对关系．计算结果显示,液膜和空气内温度随壁面热流密度的增大而增大,在气液界面处,温度梯度存在不连续;气-液相界面处的换热主要形式为水蒸发传质引起的潜热换热为主、空气显热传热为辅,并且传热热阻主要集中于水膜内;并且随风速的增加,相间传质量也随之增大．