Estimation of eddy viscosity on the South China Sea shelf with adjoint assimilation method

The eddy viscosity of the ocean is an important parameter indicating the small-scale mixing process in the oceanic interior water column.Ekman wind-driven current model and adjoint assimilation technique are used to calculate the vertical profiles of eddy viscosity by fitting model results to the observation data.The data used in the paper include observed wind data and ADCP data obtained at Wenchang Oil Rig on the SCS (the South China Sea) shelf in August 2002.Different simulations under different wind conditions are analyzed to explore how the eddy viscosity develops with varying wind field.The results show that the eddy viscosity endured gradual variations in the range of 10^-3-10^-2 m²/s during the periods of wind changes.The mean eddy viscosity undergoing strong wind could rise by about 25% as compared to the value under weak wind.     

JZ9-3油田水质对聚合物3640C溶液黏度的影响分析

实验研究了JZ9-3油田的3种水质（水源水、污水、清污混合水）对聚合物溶液剪切前后黏度的影响。结果显示：在相同浓度条件下,清污混合水配制的聚合物溶液黏度最高,其次是污水配制的聚合物溶液,水源水配制的聚合物溶液黏度最低;聚合物溶液经WARING搅拌器（1档3 500 rpm,20 s）剪切后的黏度保留率数据显示,污水配制的聚合物溶液剪切后黏度保留率最高,当浓度大于1 000 mg/L时,保留率在90%左右;最低的是水源水配制的聚合物溶液,保留率在55%左右。分析发现二价阳离子除了对聚合物溶液的黏度存在一定的影响外,对聚合物溶液剪切后的黏度保留率影响更大。     

弱碱三元复合驱过程中黏度和界面张力变化规律实验研究

“碱／表面活性剂／聚合物”三元复合驱油技术以其良好的增油效果而受到石油科技工作者的广泛重视,但驱油剂价格高和在油藏内损失量大一直制约着该项技术的大规模推广应用。为了解三元复合驱过程中驱油剂黏度和界面张力变化特征,以相似理论为指导,利用现代物理模拟技术和仪器检测方法,开展了三元复合驱过程中驱油剂黏度和界面张力变化及其影响因素研究。结果表明,随着注入量或PV数的增加,油藏内各处三元复合体系黏度增大、界面张力值降低。在注入PV数相同条件下,距注入井愈近,三元复合体系黏度愈大、界面张力愈低。因滞留和稀释作用的影响,三元复合体系在油藏内运移过程中黏度和界面张力分别呈现不断降低和升高趋势。     

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??????λ??????μ???У?Kalman?????????????????????????????????????????????????Щ??????????????????????????????????????????????????????Щ????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????У????????????Kalman?????????????????????????????????μ??????е??????     

Geopulsation, Volcanism and Astronomical Periods

Volcanism is mainly controlled by the intermittent release of energy in the earth. As far as the differential rotation of the earth's inner core is concerned, the Galactic Year may change the gravitational constant G, the solar radiative quantity and the moving speed of the solar system and affect the exchange of angular momentum between core and mantle as well as the energy exchange between crust and mantle. As a result, this leads to eruptions of superplumes and magma, and controls the energy flow from core - mantle boundary (CMB) to crust. When the earth' s speed decreases, it will release a huge amount of energy. They are the reason of the correspondence of the volcanic cycles one by one with the astronomical periods one by one. According to the astronomical periods, volcanic eruptions may possibly be predicted in the future.     

陀螺全站仪仪器常数稳定性的影响因素及解决措施

陀螺全站仪是一种全天候、不依赖其他条件能够测定真北方向的物理定向仪器,在军事、航天、矿山、铁道、森林、建筑、海洋和测绘等部门日益得到广泛应用。陀螺全站仪定向中,仪器常数的稳定性直接影响到定向结果的可靠性。介绍了仪器常数的测定方法,总结了影响仪器常数稳定性的因素,提出相应解决措施。     

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栾家河花岗岩体中的矿物包裹体研究

根据熔融包裹体的均一温度和均一过程的时间,利用熔融包裹体的扩散率公式（ＤＨ＝ｒ２／４ｔ）、Ｅｙｒｉｎｇ方程（ＤＮ＝ＫＢ·Ｔ／η·λ）以及不同含水量花岗质熔体的ＬｎＤＨ－１／Ｔ实验图解,计算了胶东金矿区内与金矿形成关系密切的栾家河岩体中包裹体熔体的粘度和含水量。结果表明,熔融包裹体均一温度为９７０℃,粘度为３．８×１０６Ｐａ·ｓ,含水量为２．５％;流体熔融包裹体的均一温度为８５５℃,粘度为６１７．７Ｐａ·ｓ,含水量为５．８％,反映出花岗岩浆在结晶过程中含水量不断增高,粘度不断降低,到结晶作用晚期,流体相接近饱和状态。     

地震波速度约束的大横向黏度变化的地幔对流研究

本文将横向黏度变化提高到3个量级,获得了地震波速度结构约束下的大横向黏度变化的地幔浅部的极型场和环型场对流图像.与小横向黏度变化下的结果相比,本文的结果具有显著的改善.对极型场对流图像,主要体现在本文结果能更清楚地解释太平洋板块、大洋洲和南美洲以及东太平洋洋中脊处的现今运动状态;对环型场对流图像,能更合理地解释北太平洋...     

微波波段大气折射率结构常数的仿真研究

大气折射率结构常数描述了大气湍流起伏的强弱,它表征了大气折射率随机不均匀性的剧烈程度。光波和无线电波在大气中传播时会受到大气湍流的影响而产生各种不良效应,如:光斑漂移、闪烁、相位起伏等。因此,对大气折射率结构常数的研究具有重要的意义。本文利用常规探空资料对微波波段大气折射率结构常数进行了仿真研究,结果表明:在低空,特别是大气边界层之内,大气折射率结构常数主要为湿度所贡献;在高空,大气折射率结构常数主要为温度所贡献。在微波波段,影响大气折射率结构常数最大的气象因子并不是温湿压的大小,而是它们梯度的大小,其中湿度梯度的大小对其影响最大,在实际的低空测量大气折射率结构常数时,主要考虑湿度梯度与温度梯度的影响。