Ultrasonic measurement of suspended sediment concentrations: an experimental validation of the approach using kaolin suspensions and reservoir sediments under variable thermal conditions     

C. C. Sung  Y. J. Huang  J. S. Lai  G. W. Hwang 《水文研究》2008,22(16):3149-3154

Multiphase suspension systems are used extensively in hydrology, biochemistry, and the food industry. Ultrasonic spectroscopy is a rapid, on‐line, non‐invasive measurement technique for suspension characterization over different particle sizes and a wide range of concentration. Although the properties of kaolin suspensions have been investigated extensively, kaolin ultrasonic attenuation properties at different temperatures and concentrations have not yet been reported. Through experimental validation in the laboratory, this study provides results from a series of measurements of kaolin ultrasonic attenuation over a wide range of concentrations (0–300 000 ppm) and practical temperatures (5–25 °C). The ultrasonic measurement of attenuation of sediment sampled from the Shihmen reservoir in Taiwan is also investigated. Results show that variations in ultrasonic attenuation are driven by concentration and temperature. Two regression functions are established to quantitatively relate attenuation to kaolin concentration and the Shihmen reservoir sample at a given temperature. An ultrasonic system is designed and manufactured for real‐time sediment concentration monitoring in the Shihmen reservoir based on these experimental ultrasonic attenuation measurements. Copyright © 2007 John Wiley & Sons, Ltd.  相似文献   

2004年上海天文台卫星激光测距观测报告     

杨福民张忠萍  陈菊平陈婉珍 《中国科学院上海天文台年刊》2005,(1):48-51

介绍了2004年上海天文台卫星激光测距观测概况。  相似文献   

A COMPARISON OF EASTERN AND WESTERN HONG KONG PHYTOPLANKTON FROM WEEKLY SAMPLES （1997-1999）   总被引：3，自引：0，他引：3  

Mike Dickman  Tang Sen-ming  Jessie Lai 《中国海洋湖沼学报》2002,20(1):52-61

Weekly phytoplankton samples were taken from western Hong Kong (Lamma) from Jan. 1997 to Dec. 1999 and from Port Shelter in Eastern Hong Kong from January 1998 to December 1999. During that time diatom blooms occurred repeatedly at both sites but never in synchrony. One species would bloom at one site and then weeks later it or another species would bloom at the other site; while the 1998 red tide of the mucus producing dinoflagellateGymnodinium mikimotoi occurred at both sites. It first occurred at the Port Shelter site in March and did not appear at the Lamma site until April. With the single exception of this species, no other dinoflagellate reached bloom concentrations at the Lamma site. In addition, dinoflagellate abundance at the Lamma site was significantly lower (P<0.05) than that at the Port Shelter site. This was correlated with a significantly higher turbidity (i. e. low Secchi transparency) and higher turbulence (stronger currents) at the Lamma site. Annual variation in surface temperature correlated with total surface phytoplankton abundance at both our sample sites. Phytoplankton abundance increased in spring as water temperatures warmed. In fall, as surface water temperatures began to decline and the monsoon rains became less frequent there was a reduction in phytoplankton abundance associated with the reduction in temperature and light. Because so many variables co-occur with temperature (e. g. the amount of rainfall light intensity and light duration etc.) it is not possible to cite temperature as the causal factor associated weth controlling phytoplankton abundance at our two sample sites. Our data support the rather controversial notion that percentage-wise, there are relatively more harmful bloom forming species in nutrient-rich coastal waters than there are in the world's oceans. 16% of the dinoflagellate species and 10.3% of the diatom species observed at our two sample sites were classed as harmful. These percentages were higher than those cited by Sournia (1995) for the worlds oceans (9.6% and 6.8% respectively). This raises the possibility that there are relatively more toxic species in the nutrient-rich coastal waters of the world than there are in the mid ocean nutrient-poor areas of the world. Some reasons for this are briefly discussed.  相似文献   

2003年上海天文台激光测距观测报告     

杨福民  张忠萍  陈婉珍  陈菊平 《中国科学院上海天文台年刊》2004,(1)

介绍了 2 0 0 3年度上海天文台卫星激光测距观测概况 ,同时介绍了我国第一颗带激光反射器的航天器—神舟四号轨道舱的激光观测和双波长卫星激光测距实验。  相似文献   

Atmospheres and spectra of strongly magnetized neutron stars   总被引：1，自引：0，他引：1  

Wynn C. G. Ho  Dong Lai 《Monthly notices of the Royal Astronomical Society》2001,327(4):1081-1096

We construct atmosphere models for strongly magnetized neutron stars with surface fields     and effective temperatures     . The atmospheres directly determine the characteristics of thermal emission from isolated neutron stars, including radio pulsars, soft gamma-ray repeaters, and anomalous X-ray pulsars. In our models, the atmosphere is composed of pure hydrogen or helium and is assumed to be fully ionized. The radiative opacities include free–free absorption and scattering by both electrons and ions computed for the two photon polarization modes in the magnetized electron–ion plasma. Since the radiation emerges from deep layers in the atmosphere with     , plasma effects can significantly modify the photon opacities by changing the properties of the polarization modes. In the case where the magnetic field and the surface normal are parallel, we solve the full, angle-dependent, coupled radiative transfer equations for both polarization modes. We also construct atmosphere models for general field orientations based on the diffusion approximation of the transport equations and compare the results with models based on full radiative transport. In general, the emergent thermal radiation exhibits significant deviation from blackbody, with harder spectra at high energies. The spectra also show a broad feature     around the ion cyclotron resonance     , where Z and A are the atomic charge and atomic mass of the ion, respectively; this feature is particularly pronounced when     . Detection of the resonance feature would provide a direct measurement of the surface magnetic fields on magnetars.  相似文献   

Genesis of the Madang Cenozoic sodic alkaline basalt in the eastern margin of the Tibetan Plateau and its continental dynamic implications     

Lai  ShaoCong  Zhang  GuoWei  Li  YongFei  Qin  JiangFeng 《中国科学:地球科学(英文版)》2007,50(2):314-321

The Madang Cenozoic sodic alkaline basalt occurred in the eastern margin of the Tibetan Plateau, where is a key tectonic transform region of Tibet, North China, and Yangtze blocks. The basalts are characterized by the variation in SiO₂=42%–51%, Na₂O/K₂O>4, belonging to the sodic alkaline basalt series. The rocks are enriched in Ba, Th, Nb, Ta, relative to a slight depletion in K, Rb in the trace and rare earth element (REE) spider diagrams that are similar to the typical oceanic island alkaline basalt. The Sr-Nd-Pb isotopic compositions suggest that they are derived from a mixed mantle reservoir. The western Qinling-Songpan tectonic region was controlled by Tibet, North China and Yangtze blocks since Cenozoic, therefore, the region was in the stage of the substance converge from the mantle to upper crust, producing a mixed mantle reservoir in the studied area. The Madang basalts occurred in the specific tectonic background, they result from partial melting of a mixed asthenospheric mantle reservoir in the western Qinling-Songpan tectonic node.

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一种新的可信平台模块   总被引：1，自引：0，他引：1  

张焕国  覃中平  刘毅  韩永桥 《武汉大学学报(信息科学版)》2008,33(10):991-994

介绍了可信平台模块(TPM)的结构和技术,指出了TCG的可信平台模块存在的一些不足.在此基础上,详细介绍了研制的一种新型可信平台模块.它在资源上是丰富的,在功能和性能上是先进的,符合TCG的技术规范.经过实际测试,其密码运算速度是高速的,完全可以满足可信平台模块的各种应用需求.  相似文献   

“苏拉”台风引发福建西部大暴雨成因分析     

冯晋勤  蔡菁  赖巧珍 《气象科技》2017,45(1):149-157

利用常规天气资料、NCEP 1°×1°再分析资料、地面降水资料以及福建新一代天气雷达资料对2012年"苏拉"台风登陆后引发福建西部大暴雨天气成因进行分析,结果表明:"苏拉"登陆后高空涡旋受大陆高压东侧偏北气流引导向偏南方向移动,同时,台风登陆后进入大的环境风垂直切变区并向切变左侧倾斜,使得台风南倾结构进一步加大。台风结构南倾为福建西部大暴雨区提供了良好的动力条件,"苏拉"自身带来的水汽及台风南侧西南气流为暴雨区提供了充足的水汽来源,高空冷空气入侵与低层的高温高湿区形成上冷下暖结构呈现出条件不稳定层结,有利于深厚湿对流产生,结合充分的水汽供应,出现大暴雨天气。大范围暖平流配合风速辐合,中高层冷空气入侵与低层西南暖湿空气结合以及低层的西南急流建立是三个强降水阶段对应的中尺度天气特征。  相似文献   

Trends and uncertainties in surface air temperature over the Tibetan Plateau, 1951–2013          下载免费PDF全文

Wei Hua  Guangzhou Fan  Yiwei Zhang  Lihua Zhu  Xiaohang Wen  Yongli Zhang  Xin Lai  Binyun Wang  Mingjun Zhang  Yao Hu  Qiuyue Wu 《Acta Meteorologica Sinica》2017,31(2):420-430

Trends and uncertainties of surface air temperature over the Tibetan Plateau (TP) are evaluated by using observations at 100 meteorological stations during the period 1951–2013. The sampling error variances of gridded monthly data are estimated for every month and every grid box of data. The gridded data and their sampling error variances are used to calculate TP averages, their trends, and associated uncertainties. It is shown that large sampling error variances dominate northern and western TP, while small variances appear over southern and eastern TP. Every month from January to December has a positive linear trend during the study period. February has the largest trend of 0.34 ± 0.18°C (10 yr)^–1, and April the smallest at 0.15 ± 0.11°C (10 yr)^–1. The uncertainties decrease steadily with time, implying that they are not large enough to alter the TP warming trend.  相似文献   

赣北黄茅潭湖泊沉积记录的240年以来古洪水事件   总被引：1，自引：1，他引：0  

吴霜  刘倩  曹向明  赖忠平  陈远辉  贾玉连 《地理科学进展》2017,36(11):1413-1422

古洪水研究是近几十年来全球变化研究的一个热点,同时也是难点。本文利用赣北黄茅潭的湖泊沉积,建立了小冰期以来全球变暖背景下的区域洪水记录。采用²¹⁰Pb和¹³⁷Cs方法厘定了地层年代,基于粒度与元素地球化学指标的对比分析,揭示了器测记录(1950年)以来指标记录的特点与区域日降水超过50 mm天数的关系,认为黄茅潭HMT-01孔粒度(包括粗粉砂+砂/粘土比值、平均粒径)和Zr/Rb、Ti/Rb、Zr/Fe比值可作为洪水指标记录,共识别出1950-2010年期间记载的13次洪水事件中的11次。基于这些指标记录及指标特点,共识别1769-1950年间由历史文献记录的31次洪水事件中的23次,识别率达74.2%。研究表明：①湖泊沉积中Zr/Rb、Ti/Rb、Zr/Fe比值和粒度参数(平均粒径、粗粉砂+砂/粘土)作为洪水指标,对洪水事件沉积有较好的指示作用,且Zr/Rb比值对洪水事件的检出率较高;②黄茅潭流域洪水发生频率暖期高于冷期;③年代际尺度上,1820s-1840s,1860s-1870s为19世纪冷期黄茅潭洪水高频期,这两个阶段对应东亚夏季风偏强,长江中下游地区降雨较多;20世纪赣北黄茅潭洪水基本随1920s-1940s,1980s-1990s两个变暖阶段而高频出现,与长江中下游大洪水演变特点基本一致。研究结果为利用湖泊沉积记录反演过去的洪水变化,延长洪水序列、认识洪水规律提供了一定的科学依据。  相似文献