��̬������С����ģ�͵������㷨   总被引：6，自引：2，他引：4  

袁振超  沈云中  周泽波 《大地测量与地球动力学》2009,29(2):131-135

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��Ӷ��Ѵ������ֽ�������ЧӦ   总被引：1，自引：1，他引：0  

孙少安  申重阳  项爱民 《大地测量与地球动力学》2009,29(3):11-15

????????????????????????β??????????????1985??2006??β?????仯??????????1???????????????????????????????????????????????????????????????????????????2????????????????????????????????1?λ??????????￡??????????ε?????????????????????1?γ????????仯?????3?? ????????????????仯?????????????????仯????????????????????????????  相似文献   

����ԳƷ��ڵ��㶨λ�е�Ӧ��   总被引：1，自引：0，他引：1  

汪平  郝金明  沈国康  王兰 《大地测量与地球动力学》2009,29(5):112-115

???GPSα????λ????????????????????μ?????????????λ??????????????ù????????????????????????????????棨???棩?????????????????????????????????α?????????????????????α???????????????????????λ??????????·??????????????????λ???????????????????????????????ν????????????????????????Ч????????λ?????????????????  相似文献   

不同盐度对克氏螯虾幼虾代谢率的影响     

李庭古  马甡 《海洋湖沼通报》2009,(3)

研究了不同盐度对克氏螯虾(Procambarus clarkii)幼虾耗氧率和排氨率的影响.试验用虾体长(3.13±0.30)cm,体重在(1.82±0.21)g.在25℃条件下,试验设置0、2、4、6、8、10、12共7个盐度梯度.在试验设置的盐度范围内,在盐度为2时,克氏原螯虾幼虾的的耗氧率与排氨率最低,由此可以表明幼虾对盐度调节的等渗点在2左右.随着盐度升高,幼虾的耗氧率和排氨率也随之上升,Turkey HSD test发现,在对照组、2、4和6盐度组的耗氧率、排氨率差异明显(P＜0.05).超过0～6的盐度范围时,盐度对幼虾的耗氧率、排氨率影响与对照组的差异显著(P＜0.05).  相似文献   

太湖蓝藻水华遥感动态监测预警信息系统   总被引：1，自引：0，他引：1  

王甡  江南  胡斌  魏清宇 《地球信息科学学报》2008,10(2):147-150

太湖蓝藻水华暴发对其周边地区的生态、经济和社会造成了严重影响,对蓝藻水华进行监测预警对于改善太湖水环境具有重要意义。本文在分析蓝藻水华遥感监测预警研究动态基础上,从信息系统构建角度,结合太湖蓝藻水华监测情况,对太湖蓝藻水华遥感监测预警流程进行系统性分析,提出建立太湖蓝藻水华遥感监测预警系统的总体框架,利用C#语言和IDL语言实现了该框架的软件架构,并且论述了实现该系统框架所采用的系统集成技术和软件模式技术。  相似文献   

GPS测量技术在海阳市城区控制中的应用研究          下载免费PDF全文

车谦刚  徐万祥  沈婷  王丰科 《山东国土资源》2008,24(6)

通过海阳市城区D级GPS控制网的布设,探讨了GPS控制网的布网方法和要求,阐述了GPS外业观测的质量控制措施,基线处理方法及其精度检验,讨论了已知控制点的选用方法,以及平差中应注意的问题等。  相似文献   

塔里木盆地牙哈-英买力地区寒武系-奥陶系碳酸盐岩储层成因类型、特征及油气勘探潜力   总被引：1，自引：0，他引：1  

沈安江  王招明  郑兴平  贺晓苏  郑多明 《海相油气地质》2007,12(2):23-32

牙哈—英买力地区是塔北隆起上的主要油气富集区,古潜山风化壳型储层的观点一直主导着该地区寒武系—奥陶系碳酸盐岩油气勘探的思路。但储层精细描述揭示了牙哈—英买力地区除古潜山风化壳型储层外,还发育有暴露浅滩型、层间古岩溶型、白云岩型储层。其中位于古潜山面之下经风化作用改造的白云岩型储层是最有勘探价值的,勘探成功率高。其次是暴露浅滩型储层,油藏类型有早成藏残留型和晚成藏型。暴露浅滩型、层间古岩溶型和白云岩型储层也是很有勘探价值的储层类型。早成藏型原生油气藏,位于寒武系—奥陶系与志留系呈假整合接触的地区,与古潜山无关。古潜山风化壳型储层可以形成晚成藏型油气藏,但目前试油结果均为水层,值得进一步探索。  相似文献   

Characteristics and origins of middle Miocene mounds and channels in the northern South China Sea     

Yufeng Li  Gongcheng Zhang  Renhai Pu  Hongjun Qu  Huailei Shen  Xueqin Zhao 《海洋学报(英文版)》2021,40(2):65-80

Numerous elongated mounds and channels were found at the top of the middle Miocene strata using 2D/3D seismic data in the Liwan Sag of Zhujiang River Mouth Basin(ZRMB) and the Beijiao Sag of Qiongdongnan Basin(QDNB). They occur at intervals and are rarely revealed by drilling wells in the deepwater areas. Origins of the mounds and channels are controversial and poorly understood. Based on an integrated analysis of the seismic attribute, palaeotectonics and palaeogeography, and drilling well encountering a mound, research results show that these mounds are dominantly distributed on the depression centres and/or slopes of the Liwan and Beijiao sags and developed in a bathyal sedimentary environment. In the Liwan and Beijiao sags, the mounds between channels(sub) parallel to one another are 1.0–1.5 km and 1.5–2.0 km wide, 150–300 m and 150–200 m high, and extend straightly from west to east for 5–15 km and 8–20 km, respectively. Mounds and channels in the Liwan Sag are parallel with the regional slope. Mounds and channels in the Beijiao Sag, however, are at a small angle to the regional slope. According to internal geometry, texture and external morphology of mounds, the mounds in Beijiao Sag are divided into weak amplitude parallel reflections(mound type I), blank or chaotic reflections(mound type II), and internal mounded reflections(mound type Ⅲ). The mounds in Liwan Sag, however, have the sole type, i.e., mound type I. Mound type I originates from the incision of bottom currents and/or gravity flows. Mound type II results from gravity-driven sediments such as turbidite. Mound type Ⅲ is a result of deposition and incision of bottom currents simultaneously. The channels with high amplitude between mounds in the Beijiao and Liwan sags are a result of gravity-flow sediments and it is suggested they are filled by sandstone.Whereas channels with low-mediate amplitudes are filled by bottom-current sediments only in the Beijiao Sag,where they are dominantly composed of mudstone. This study provides new insights into the origins of the mounds and channels worldwide.  相似文献   

Improving performances of ITO/GaP contact on AlGaInP light-emitting diodes     

李春伟  朱彦旭  沈光地  张勇辉  秦园  高伟  蒋文静  邹德恕 《海洋学报(英文版)》2010,29(9)

In this paper AlGaInP light emitting diodes with different types of electrodes: Au/Zn/Au-ITO Au/Ti-ITO Au/Ge/Ni-ITO and Au-ITO are fabricated. The photoelectricity properties of those LEDs are studied. The results show that the Au/Zn/Au electrode greatly improves the performance of LEDs compared with the other electrodes. Because the Au/Zn/Au electrode not only forms a good Ohmic contact with indium tin oxide (ITO), but also reduces the specific contact resistances between ITO and GaP, which are 1.273×10^-6 Ω · cm² and 1.743×10^-3 Ω ·cm² between Au/Zn/Au-ITO and ITO-GaP respectively. Furthermore, the textured Zn/Au-ITO/Zn electrode is designed to improve the performances of LEDs, reduce the forward-voltage of the LED from 1.93 to 1.88 V, and increase the luminous intensity of the LEDs from 126 to 134 mcd when driven at 20 mA.  相似文献   

Determining the age of water and long-term transport timescale of the Chesapeake Bay   总被引：5，自引：0，他引：5  

Jian Shen  Harry V. Wang 《Estuarine, Coastal and Shelf Science》2007,74(4):585-598

The concept of age of water (AW) is applied to the Chesapeake Bay to investigate the long-term transport properties for dissolved substances. A real-time calibrated hydrodynamic Chesapeake Bay model in 3 Dimensions (CH3D), employing a boundary-fitted curvilinear grid, is used for the study. The long-term transport properties, represented by AW, are investigated under the conditions of low river inflow of 1995 and high river inflow of 1996, as well as for constant mean inflows. The influences of freshwater, density-induced circulation, and wind-induced transport on age distribution have been investigated. Model results show that river inflows, wind stress, and density-induced circulation play important roles in controlling the long-term transport in the Bay. The model results shows that it requires 120–300 days for a marked change in the characteristics of the pollutant source discharged into the Bay from the Susquehanna River to affect significantly the conditions near the mouth under different hydrodynamic conditions. An increase of river discharge results in increases of downstream residual current and gravitational circulation, and thus reduces AW. The density-induced circulation contributes to the transport substantially. The dissolved substances discharged into the Bay are transported out of the Bay more rapidly when the estuary becomes more stratified. Southeasterly and southwesterly winds have strong impacts on the transport compared to the northeasterly and northwesterly winds. The former increases lateral and vertical mixing significantly. Consequently, the gravitational circulation is reduced and the transport time is increased by 50%. The model results provide useful information for understanding the long-term transport processes in the Bay.  相似文献