最新刊期
      期 50 ， 2010
      • PANG Chongguang,WEI Yanji,ZHAO Enbao
        Vol. 17, Issue 50, (2010) DOI: 201005001
        摘要：A one-phase model is established by using CFD(Computational Fluid Dynamics) software,which includes a hydrodynamic sub-model,an erosion-deposition and a moving boundary method.in the model,the velocity field surrounding obstacles on the seabed is computed by a three dimensional k-εturbulence closure sub-model.Erosion and deposition caused by the transportation of suspended load and bed load are also calculated.The evolution of bedform is simulated in a mobile grid technipue.The three-dimensional flow pattems and evolution of bedform around three different obstacles are simulated using the one-phase model.The hydrodynamic process and sediment transportation process surrounding the obstacles are reproduced in detail. The simuated results of bedform evolution are in good agreement with laboratory measurement results in 2005.  
          
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        发布时间：2024-01-30
      • BAI Hong,WANG Fan
        Vol. 17, Issue 50, (2010)
        摘要：Based on six=cruise data gathered along 32°N and PN sections fron 1987 to 1998,we examined variations of water mass distribution and associated circulation in the westem part of the East China Sea with the emphasis on the behaviors of the Taiwan Warm Current Water and Changjiang(Yangtze)Diluted Water.It is found that the Diluted Water is Limited in the west of 122.5°E～123°E along 32°N and PN sections in autumn,winter and spring,but extends to 122.5°E～126°E in summer,especially in summer of 1998. Along the PN section, the Taiwan Warm Current (TWC)Water is found all year round,especially in deeper layer.It has significant seasonal and interannual variations which is the strongest in winter and relatively weaker in winter and relatively weaker in spring,summer and fall.The deep water carried by the TWC along 123°E～123.5°E tends to reach the north of 28°N even 30°N not only in warm seasons but also in cold seasons in even greater strength.It is noteworthy that the TWCwater was also strong in the flood summer of 1998.In general,the TWC water acts weakly in the north of 32°Nsection.However in spring of 1994.the body of the TWC water in salinity at 33.5 was found along 32°N section.It seems the extreme of the TWC water's northward intrusion with the depth in summer,but does not in winter.  
          
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        发布时间：2024-01-30
      • FENG Junqiao,BAI Xuezhi,CHEN Yongli,HU Dunxin
        Vol. 17, Issue 50, (2010)
        摘要：Long wavelength baroclinic oceanic Rossby waves are of interest because they are the main mechanism of energy transfer among the oceanic basins as the rotating fluid adjusts under the forcing of gravity and buoyancy,They play an important role in dynamics and thermodynamics in the ocean.The signature of them is evident from the altimeter measurements.Sea surface beight derived from the multiple ocean satellite altimeter missions over 1993～2008 is analyzed to systematically investigate the characteristics of the Rossby waves in the tropical Indian Ocean,by jointly adopting 2D-FFT,2D-Radon Transform,Complex Empirical Orthogonal Function and the classic linear theory methods.Results are as follows.The energy of Rossby wave is mainly concentrated between 5°S～18°S.Annual Rossby wave can be observed all over the whole badin,whereas semi-annual Rossby wave can bw only detected in the equatorial area, and inter-annual Rossby wave in the off-equatorial region.The phase speeds of Rossby waves detected from altimeter satellites are basically in agreement with the calculation based on the classic linear theory, but the former are some slower(faster) north(south)of 15°S than the later,Furthemore,it is indicated from the CEOF analysis that the annual Rossby waves is apparent in the Bay of Bengal,Arabian Sea ,and the open south Indian Ocean,whereas inter-annual Rossby wave mainly presents in the south Indian Ocean ,and eastward Kelvin wave is dominant along equator.  
          
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        发布时间：2024-01-30
      • LIU Guiwen,HUANG Haijun,LIU Yanxia,YAN Liwen,DU Tingqin
        Vol. 17, Issue 50, (2010)
        摘要：Multiple surveys were conducted before and after storm surge at four beach sections,Sediment samples were analyzed and numerically simulated for understanding the characteristicsof becach reaction to storm surge and morphological evolution ,The results show that the sediment sources in this area do not increase in amount;the beach is basically stable in normal weather.While in gale weather,sediment from Yellow River and the eroded matters from the bank becomes a part of the sediment sources.The northem beach of Xiaoqing estuary is eroded seriously, while the southern beach is overall stable,Thw tidal creeks changed from the northern beach are transported greatly sea-ward and the inshore sediment becomes sandy,while that of the southem beach becomes silty,The sand transporting capability is almost 100 times of that in nomal weather. Human activities and big storm surges are the main reasons for the beach evolution.  
          
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        发布时间：2024-01-30
      • Caili,WU Shiguo,YUAN Shengqiang
        Vol. 17, Issue 50, (2010)
        摘要：A deepwater channel complex sedimentary system developed on or beneath slope,and on badin floor. Deepwater channels act as important conduits for transporting terrigenous detrital materials to deepwater basin,and control the formation and evolution lf deepwater sedimentary systems.Generally,a deepwater channel complexforms during the periodt of a relative low stand of sea level,when large volumes of coarse-grained sediment erode the slope and deposit on badin floor.The internal fill is lften quite complex,and the nature of channel-fill deposits varies greatly.Deepwater chanels tend to develop a smooth longitudinal upconcavity that is balanced between erosion and deposition.Based on 2D seismic data and stratigraph,we recognized a central deepwater channel complex sedimentary system,which probably formed during the early Oliocene at 5.0 Ma in Qiongdongnan Basin northern South China Sea. On seismic reflection profiles, the studied channels present an overall“U”or “V”shape and middle-high-amplitude continual seismic phase.Combining the lithologic layering from drilling well and the published channel filling model, we constructed a model of the studied channel complex and found tha most of them were sandstone-rich aggradational channel-fill patterns.the deepwater channel complex can act as good hydrocarbon reservoirs.  
          
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        发布时间：2024-01-30
      • LI Zheng,HUANG Haijun
        Vol. 17, Issue 50, (2010)
        摘要：The Bowtie effect occurs in MODIS Level 1B data,and is stored in Hierarchical Data Format (HDF)in formal.The Bowtie effect can not be removed before geometry calibration,so that Bowtie effect should be removed before geometry calibration.Modistools,amodule incorporated the ENVI environment in order to process the first level MODIS data,was developed by R&D Scanex,for removing the Bowtie effect.However,the module has two defects:it can be used only to manipulate integer data; and more than 50%data value would b e changed if the Modistools is used to manipolate integer typed MODIS data.We use a non-Ephemeris method to remove the effect,by using the Matlab numerical computing environment. The method has less pixels shifting and value changing problems  
          
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        发布时间：2024-01-30
      • MA Qingtao,ZHANG Weidong,LIU Yuming
        Vol. 17, Issue 50, (2010)
        摘要：As a clean and rich energy source,natural gas hydrate has become a focus of study in the world.In this paper,the geologic condition of hydrate reservoir is analyzed. Combining with the natural gas hydrate drilling characteristics and drilling accidents,prevention and response methods are discussed.It is proposed that to restrain and control natural gas hydrate decomposition is the key to safety drilling,in which a reasonable choice of drilling fluid system is important.Some performance parameters should be taken into account in the selection of drilling fluid.The basic parameters requirements of natural gas hydrate drilling are also analyzed.  
          
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        发布时间：2024-01-30
      • GAO Lihua,HAN Zuozhen,FAN Aiping,YANG Renchao
        Vol. 17, Issue 50, (2010)
        摘要：Detailed studies on a number of core sections,well logs and seismic date of the paleogene systems of the southern part of eastem sag in Liaohe Depression revealed theat six sedimentary systems,i,e.delta,lake,fan delta,braided river,delta,river and alluvial fan,were distinguished,The sedimentation in the studied area remarkably controlled reservoir and the variability of sedimentary facied caused the diversity of reservior sand bldies and the inhomogeneity of reservoir properties plane distribution;The best reservoir properties are the sand bodies of deltaic front and braided-river deltaic front;the better are the sand bodies of braided-river deltaic plain,deltaic front,braided river and meandering river;the medium reservoir properties are the sand bodies of delta plain,the fan-delta front,the alluvial-middle fan,beach-bar and turbidite fan;the wores are the sand bodies of upper fan and lower fan of alluvial fan,alluvial plain.The favorable sedimentary facies belt controlled the distribution of favorable reservoir and it was an important evidence for prediction favorable stratigraphiv reservoir.  
          
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        发布时间：2024-01-30
      • LIU Wei
        Vol. 17, Issue 50, (2010)
        摘要：A red tide as an sananomalous ecological phenomenon is characterized with abruptness and nonlinearness,and red tide prediction has been a hot spot in ocean ographic studies.In this paper,by using the principle of fuzzy mathematics,we developed a computer progran to simulate the BP model on the basis of Visual C++ language.Engineering analysis shows the same result between the simulation and the observation of red tide which is practical. The calculation procedures are simple and easy.  
          
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        发布时间：2024-01-30
      • WANG Haibo,WU Zhouhu
        Vol. 17, Issue 50, (2010)
        摘要：Eutrophication of a lake is one of environmental problems in the world.Mathematic modeling of eutrophication plays an im portant role in managing and controlling the Phenomenon.Among different types of eutrophication modeling,the related modeling of phytoplankton and nutrients has good applicability because the relationship between nutrients and eutriphication can be easily monitored. This paper discusses the appocation of the modeling,and analyzes the relationship between chlorophyll a and the TP,TN and CODCr according to the observation data of the Nasi Lake ,and strong relations were found by regression analysis.  
          
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        发布时间：2024-01-30
      • WANG Lijuan,YANG Shujie
        Vol. 17, Issue 50, (2010)
        摘要：Marine carbonate rocks are widespread and their sedimentary layers are huge and thick.Many oil seepages outcrops are found in the Middle-Upper Proterozoic of North China. Combined with previous data, the paper discusses the evaluation criteria of marine carbonate source rocks.Many factors,such as organic matter types of source rocks,thermal maturity,mineral and chemical composition,paleotemperature and source-reservioir relationship etc. Should be considered. Therefore,the abundance cutoff criteria of organic matters in North China especially in the Southern area,needs further.In this paper,North China is divided into the north area dn the south area,and the organic matter type,organic matter abundance and degree of thermal evolution of organic matter in the two areas in overall and both of them are high thermal evaluation level.Furthermore,the majority of the organic matters of the source rock have been in highly over matured phase.Source rock mature period of Liulaobei Formation and Xuhuai Group in the southern area ids equal to that of the lower Xiamalin Formation in the northern area,the hydrocarbon generation capacity of Chuanlinggou Formation,and different organic matter types obtained with different methods on source rock research in the south area of North China are also put forward.  
          
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        发布时间：2024-01-30
      • CAO Hong,DIAO Yujie
        Vol. 17, Issue 50, (2010)
        摘要：The Tutuan River wetland is one of the important wetlands in Rizhao City,Shandong.Comprehensive evaluation of its function was studied for essking a comprehensive remedy to current geological and environmental problems.Ecological function, ecosystem characteristics,environmental problems and function loss of the wetland were assessed,and the effect of climate change on the wetland was analyzed in monthly weather change in 2000-2005.Meanwhile the surface water and groundwater in key sites were sampled and analyze for water quality assessment and sea water invasion to the study area was also evaluated.  
          
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        发布时间：2024-01-30
      • DIAO Yujie,WEI Jiuchuan,CAO Hong
        Vol. 17, Issue 50, (2010)
        摘要：Four major sedimentary systems of the Carboniferous and Permian in the Southern North China (SNC) Basin were identified in sedimentological and depositional features,such as trace fossil,silt body shape,vertical sequence and logging curve. In addition,the sedimentary facied and typical sequences of sedimentary systems were analyzed in principles of sedimentology and coalfield geology,Furthermore,geological patterns of the coal accumulation,paleogeography and tectonic setting in each geological stage were reconstructed. Corresponding to sedimentary system and facies,there was no coal accumulation in the late carboniferous,while Shihezi Formation of the Middle Permian is the best coal accumulation period. And the delta front and sea-water swamp (the gulf) facies were the best environment for coal accumulation,which are meaningful for coalfield prediction and exploration in the Southern North China (SNC) Basin.  
          
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        发布时间：2024-01-30
      • LIU Feng,WU Shiguo,DONG Dongdong
        Vol. 17, Issue 50, (2010)
        摘要：The experimental apparatus for gas hydrate in porous sediments is introduced.Under different constant temperature(1.0℃,2.0℃,4.0℃,7.0℃,10.℃),the formation and dissociation of methane hydrate with three kinde of sediments granule(average diameters 0.15mm,0.06mm,0.03mm respectively) are studied. The saturation of methane hydrate in porous sediments is got by measuring the consumption of methane in vesssel. The results find that the saturation increases as formation pressure and porosity of sediments increase. It is also showed that the P-T curve in distilled water,which is accordant with the results from other papets sediments departure to left comparing to the P-T curve in distilled water, which is accordant with the results from other papers involved .  
          
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        发布时间：2024-01-30
      • FANG Chen,ZHANG Weidong
        Vol. 17, Issue 50, (2010)
        摘要：Gas bydrate is a form of natural gas and water,similar to ice-like solids,mainly in low-temperature occurrence in the context of high voltage submarine and terrestrial and terrestrial sediments permafrost zone.Since 1970s marine lil and gas exploration in the course of a certain depth of the seabed found that the stability of gas hydrate layer and collected samples in kind,its social concem will be on the increase. Landslide Harbor is a major cause of the destructive consequences of the marine geological disaters.In recent years,researchers continue to find that as the undersea gas hydrate decomposition led to the seabed to reduce the stability of rocks,the seabed is a major reason for the decline. The research on submarine landslide,related with natural gas Hydrate is the study of a new direction. This paper analyzes the gas hydrate formation and decomposition fo the seabed sediment. Fron the mechanical aspects of the mechanism,it analyzes of the decomposition of gas hydrate deposits related to property caused by the impact of changes in the landslide,and look to the future hydrate research.  
          
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        发布时间：2024-01-30
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