南方岩溶含水系统结构识别方法初探

岩溶含水系统因其含水介质的高度不均匀性和各向异性而难以刻画。文章选取鄂西岩溶槽谷区典型的岩溶含水系统为研究对象,基于野外地面调查、裂隙测量、洞穴探测、多源高精度地下水示踪试验、地下水动态监测等传统手段,结合新技术、新方法来综合查明岩溶含水系统的结构,探讨岩溶含水系统的边界结构、岩溶发育主控方向、介质空间结构的识别方法,最终刻画出岩溶含水系统结构的概念模型。文章的研究成果旨在为岩溶山区1∶5万水文地质调查工作思路与方法应用提供参考,为提高全国新一轮1∶5万水文地质调查成果的精度与质量做贡献。      

川中蓬莱地区须家河组须二段储层成岩相与优质储集层预测

通过岩心观察并综合利用普通薄片、铸体薄片和扫描电镜分析等资料,对须二段储层岩石学特征、物性及孔隙结构特征、成岩作用、成岩矿物、成岩环境、所处成岩阶段和成岩演化序列等进行了研究。结果表明,须二段储层经历压实压溶、胶结、溶蚀和破裂等成岩作用,现今处于中成岩A 期。根据成岩作用类型和强度、成岩矿物及其对储层物性的影响划分出3种成岩相：强压实自生矿物胶结相、强压实不稳定组分溶蚀相和破碎裂缝相。选取了对成岩相较敏感的声波时差、电阻率、自然伽马、密度和中子5条常规测井曲线和成像测井资料,通过岩心资料刻度测井建立了各成岩相的测井识别标准,将成岩相进行剖面展开和平面成图。再根据有利成岩相的平面展布规律,对蓬莱地区须二段优质储层发育带进行了预测,认为平面上的斜坡中部为主要的优质储集层发育区。     

Parameter identification of hysteretic model of rubber-bearing based on sequential nonlinear least-square estimation

In order to evaluate the nonlinear performance and the possible damage to rubber-bearings (RBs) during their normal operation or under strong earthquakes, a simplified Bouc-Wen model is used to describe the nonlinear hysteretic behavior of RBs in this paper, which has the advantages of being smooth-varying and physically motivated. Further, based on the results from experimental tests performed by using a particular type of RB (GZN110) under different excitation scenarios, including white noise and several earthquakes, a new system identification method, referred to as the sequential nonlinear least-square estimation (SNLSE), is introduced to identify the model parameters. It is shown that the proposed simplified Bouc-Wen model is capable of describing the nonlinear hysteretic behavior of RBs, and that the SNLSE approach is very effective in identifying the model parameters of RBs.     

A new identification method for five species of oysters in genus Crassostrea from China based on high-resolution melting analysis

The high phenotypic plasticity in the shell of oysters presents a challenge during taxonomic and phylogenetie studies of these economically important bivalves. However, because DNA can exhibit marked differences among morphologically similar species, DNA barcoding offers a potential means for oyster identification. We analyzed the complete sequences of the cytochrome oxidase subunit I （COI） of five common Crassostrea species in China （including Hong Kong oyster C. hongkongensis, Jinjiang oyster C. ariakensis, Portuguese oyster C. angulata, Kumamoto oyster C. sikamea, and Pacific oyster C. gigas） and screened for distinct fragments. Using these distinct fragments on a high-resolution melting analysis platform, we developed an identification method that does not rely on species-specific PCR or fragment length polymorphism and is efficient, reliable, and easy to visualize. Using a single pair of primers （Oyster- COI-1）, we were able to successfully distinguish among the five oyster species. This new method provides a simple and powerful tool for the identification of oyster species.     

高分辨率遥感影像的田间道路识别方法

田间道路是农田建设和管理的重要工程,其走向、宽度及通达性直接影响着农田耕作的便利程度,精准识别田间道路对农田建设效果评估具有重要意义。借助高分辨率遥感影像,本文首先基于分层分类思想,采用面向对象方法对田间道路进行识别;然后引入张量投票法、八邻域断点检测和形态学算法,对田间道路断点进行连接修复,最终得到田间道路识别结果。在河北省定州市典型案例区开展实证分析,田间道路识别的完整率、正确率、质量分别可达91%、74%、69%。     

近50年中国大范围持续性冰冻天气过程的变化特征

定义了一种大范围持续性冰冻、雨凇和雾凇天气过程的识别方法,并基于该方法识别出了1954-2009年中国60个大范围持续性冰冻天气过程、28个大范围持续性雾凇天气过程和19个大范围持续性雨凇天气过程。雾凇天气过程主要出现在中国北方地区;而雨凇天气过程集中在江南一带。大范围持续性冰冻、雨凇、雾凇天气过程均在20世纪80年代末期以后出现了突变减少,在90年代初至21世纪初几乎没有出现该类过程。气候变暖可能是大范围持续性冰冻天气过程减少的重要原因。受气温升高影响,中国冰冻天气过程的持续性减弱、影响范围缩小,导致大范围持续性冰冻天气过程出现的频次减少,易于出现持续时间更短、影响范围更小的过程。     

斜坡区断层圈闭发育部位及其形成时期识别方法及应用——以冀中坳陷文安斜坡为例

断层圈闭是斜坡区重要的构造圈闭类型,为了识别斜坡区断层圈闭发育部位及其形成时期,基于断层生长机制,分析斜坡区顺向断层圈闭和反向断层圈闭形成演化过程。结果表明：顺向断层圈闭形成于断层"硬连接"阶段,发育在断层下降盘分段生长部位;反向断层圈闭形成于断层开始活动时期,发育在断层上升盘位移最大部位。在此基础上,充分利用详细三维地震资料,结合断距-距离曲线、相干体切片、断层分段生长时期定量表征以及断距回剥等技术,建立了斜坡区断层圈闭发育部位及形成时期的识别方法,并将该方法应用于冀中坳陷文安斜坡典型断层圈闭发育部位及形成时期的识别,研究结果与实际油气分布吻合关系较好。