新模块化单桩缓冲系泊浮式集成结构系统研究     

于悦凯  宋育新  周道成  任年鑫 《海洋工程》2021,39(5):59-65

为配合我国南海重要岛礁陆域拓展及海洋资源开发,提出了一种基于新型单桩缓冲系泊与波浪能装置(WEC)集成的具有潮汐自适应特性的模块化浮体结构系统。基于三维势流理论,综合考虑浮体模块与单桩缓冲结构的相对运动及相关波浪能装置的机械耦合机理,重点研究了新型单模块浮式结构系统在典型海况下的动力响应特征,获得了单桩缓冲系泊系统的初步优化设计参数,并对极端海况进行安全校核,提出了优化自存策略。数值结果表明,此带有波浪能装置的新型单桩缓冲系泊系统,不仅可以有效地降低浮体模块的运动响应幅值并改善平台舒适度,还可以获得可观的发电量,而且在极端海况下,可以通过调整阻尼装置系统来稳定浮体模块的运动。  相似文献   

内蒙古十大孔兑主河道纵剖面发育动力机制（英文）     

顾畛逵  师长兴  彭杰 《地理学报(英文版)》2019,(3):417-431

The longitudinal profiles of main streams of ten kongdui basins within Inner Mongolian Autonomous Region of China were characterized in this study by analyzing a series of quantitative indexes that are relevant to tectonic activity and river action, and by establishing a series of multiple regression models. The results reveal that all longitudinal profiles are concave in shape, with a range of concavity between 1.1 and 3.1, increasing from west to east. Data also show that the concavity of the profiles is significantly negatively correlated with profile length, altitude difference, average altitude, drainage area and sediment load of the basins. Analysis reveals that kongdui basins have suffered from moderate-to-weak tectonic activity over time, again characterized by a west-to-east weakening trend. Stream power also varies along the main channels of the ten kongdui basins; average values in each case fall between 0.8 W/m and 8.4 W/m, generally higher within the middle reaches. This decreasing trend in stream power within the lower reaches of kongdui basins might provide one key explanation for sedimentation there. Data also show that the average stream power in western and central basins tends to be higher than that in eastern examples, even though both the highest and the lowest values are seen within two middle ones. This analysis shows that the longitudinal profile concavity values are mainly controlled by tectonic activity and that the effect of river action is insignificant.  相似文献   

内蒙古自治区油砂分布特征与资源状况     

张亭荣  师雅洁  杨才 《西部资源》2019,(1)

油砂作为非常规油气资源的一种,通常具有资源量大,分布面积广等特点。本文简要地介绍了我国油砂资源的发展历程,并重点围绕松辽盆地外围(内蒙古境内)、二连盆地和鄂尔多斯盆地油砂矿富集情况进行了论述,对内蒙古自治区油砂的分布特征与资源状况进行了总结,在此基础上预测了自治区内油砂的发展方向及找矿前景。  相似文献   

近7000年巢湖沉积物环境磁学特征及其指示的亚洲季风变化   总被引：12，自引：11，他引：1       下载免费PDF全文

张卫国  戴雪荣  张福瑞  师育新  俞立中  J.A.Dearing 《第四纪研究》2007,27(6):1053-1062

利用巢湖ACN钻孔,通过多参数磁性测量、粒度和AMS 14C测年分析,探讨了近7000年以来巢湖沉积物磁性特征变化及其控制因素,并进而探讨了其对亚洲季风变化的指示意义.研究结果表明,ACN钻孔磁性特征由磁铁矿主导,其变化主要受沉积动力环境控制,间接反映了流域降水的变化.总体上粘土含量高的沉积物中磁性矿物含量较低、颗粒较细,形成于高湖泊水位环境,对应了降水量高的时期;而＞32μm组分含量高的沉积物磁性较强、颗粒较粗,形成于低湖泊水位环境,对应了降水量低的时期.巢湖ACN的磁性记录(尤其是χARM/χ和χARM/SIRM两个参数)揭示了近7000年以来巢湖流域降水具有减少的趋势,导致湖泊收缩和沉积物中磁性矿物颗粒变粗.在这一长期变化的基础上,还存在6000aB.P.,5500aB.P.和3800aB.P.附近的显著干旱事件.这一磁性记录与中国东部地区的石笋、湖泊等记录可以很好地对比,是亚洲季风演变的区域响应结果.  相似文献   

曹娥江沉积物黏土矿物与磁性特征及其指示意义     

何姗姗  师育新  戴雪荣  许锐  刘朝 《海洋地质与第四纪地质》2018,(1)

曹娥江位于钱塘江河口区,建河口大闸前受钱塘江涌潮影响,沉积作用与物质来源较复杂,建闸后则改变了河流原有沉积作用与物质来源。采用XRD和环境磁学分析,对曹娥江流域表层物质中的黏土矿物组合和磁性特征进行了研究,并探讨了曹娥江干流沉积物来源。结果表明:表土与支流沉积物黏土矿物组合和磁性参数特征相似,1.4nm黏土矿物以蛭石和1.4nm过渡矿物为主,χ、SIRM、HIRM和χARM值较高。干流不同河段沉积物黏土矿物组合和磁性参数特征存在差异,上浦闸以上河段1.4nm黏土矿物以蛭石为主,4种磁性参数值较高,与表土、支流沉积物的值相近;新三江闸以下河段1.4nm黏土矿物以绿泥石为主,磁性参数值相对最低;上浦闸至新三江闸段1.4nm黏土矿物则以绿泥石+蛭石为主,磁性参数值介于前两者之间。物源分析结果显示,上浦闸以上河段干流沉积物来自于上游支流和流域表土,新三江闸以下河段干流沉积物主要为江外(长江口、杭州湾和钱塘江)物质,上浦闸至新三江闸段则兼有流域和江外两个区域物质,且江外物质对其影响更大。  相似文献   

内蒙古中北部白垩系下统固阳组（K1g）特征及其区域对比     

师春  师雅洁  郭婧 《西部资源》2012,(4):192-193

固阳组在测区内分布广泛,主要出露在固阳盆地的昔连脑包,西河盆地的兴茂昌,塔林宫盆地的塔林宫、本布黑,园房子盆地的毛忽洞、园圃图,东红胜盆地的流通壕一带,出露面积1,823．4km2,其岩石组合、生物特征、沉积环境等方面都有可比性。  相似文献   

襄城局创新廉政教育形式     

师中雨 《河南地质》2009,(12):48-49

本刊讯 进入11月份以来,襄城县国土资源局依托每周集体学习日机关内举办的“国土大讲堂”这一新的教育载体,紧密结合自身业务,加强廉政警示教育,收到良好效果。  相似文献   

长江上游社会经济因子对侵蚀产沙的影响   总被引：1，自引：0，他引：1  

杜俊  师长兴  范小黎  周园园 《地理学报(英文版)》2011,21(2):359-371

In recent years,the role of human activities in changing sediment yield has become more apparent for the construction of hydraulic engineering and water conservation projec-tions in the Upper Yangtze River,but it has not been evaluated at the macro scale.Taking Sichuan Province and Chongqing City as an example,this paper studies the relationship between socio-economic factors and sediment yield in the Upper Yangtze River based on section data in 1989 and 2007.The results show that sediment yield is significantly correlated with population density and cultivated area,in which the former appears to be more closely related to sediment yield.Moreover,in the relation of sediment yield vs.population density,a critical value of population density exists,below which the sediment yield increases with the increase of population density and over which the sediment yield increases with the decrease of population density.The phenomenon essentially reflects the influence of natural factors,such as topography,precipitation and soil property,and some human activities on sediment yield.The region with a higher population density than critical value is located in the east of the study area and is characterized by plains,hills and low mountains,whereas the opposite is located in the west and characterized by middle and high mountains.In the eastern region,more people live on the lands with a low slope where regional soil erosion is slight;therefore,sediment yield is negatively related with population density.In contrast,in the western region,the population tends to aggregate in the areas with abundant soil and water resources which usually lead to a higher intensity of natural erosion,and in turn,high-intensity agricultural practices in these areas may further strengthen local soil erosion.It is also found that popu-lation tends to move from the areas with bad environment and high sediment yield to the areas with more comfortable environment and less sediment yield.The natural factors have greater influence on sediment yield of western region than that of eastern region.Generally,the natural factors play a dominant role on sediment yield in the Upper Yangtze River.  相似文献   

深部气层和干层测井模拟综合评判   总被引：1，自引：0，他引：1  

胡云昌  师先进 《上海国土资源》1995,(2):19-26

深部气层和干层的区分是常规测井解释的难题，认识始于实践。本文依据东濮凹陷深层试采资料，建立了两个模式各四个以参数的隶属度曲线，进行气层和干层模糊综合评判研究，并用该地区深层试井资料作了检验，效果颇佳。证明模糊综合评判是区分深部气层和干层的一种行之有效的方法。  相似文献   

内蒙古岱海古水温定量恢复及其古气候意义   总被引：13，自引：4，他引：13  

沈吉  王苏民  R.Matsumoto  朱育新 《中国科学D辑》2001,31(12):1017-1023

通过分析岱海岩芯沉积中介形类壳体（Limnocythere of.inopinata）的Sr/Ca比值,结合现代活体介形类生态特征研究,获取了湖水的定量古盐度.另外,在实验室内开展湖水蒸发模拟试验,建立了湖水盐度与氧同位素之间的定量函数关系,获取了古湖水的氧同位素.最后,根据岩芯沉积中自生碳酸盐矿物的氧同位素分析值,结合古湖水的氧同位素组成,定量恢复了岱海古湖水温度,并探讨了其古气候意义.  相似文献