月地岩矿光谱特征对比及月表信息提取方法简介

分析了月、地同类岩石矿物的光谱特征差异,对比了遥感地质信息提取方法和模型的适用性。利用Clemen-tine UV-VIS（紫外—可见光）数据,以月表典型撞击坑Aristillus（阿里斯基尔）和典型月海Humorum（湿海）为研究区,对月球表面岩矿信息提取方法进行了初步实践。     

全极化SAR数据反演桥面高度

根据高分辨率SAR图像上建筑区的影像特征, 提出了基于灰度共生矩阵(gray-level cooccurrence Matrix, GLCM)纹理分析的建筑区提取方法, 该方法由初步定位和边界调整2个步骤组成, 均遵循特征计算、基于Bhattacharyya距离的特征选择和KNN分类流程, 所不同的是2个步骤中分别采用了逐块和逐点计算纹理特征的方式以兼顾纹理分析的效率和准确性。文中对不同SAR传感器获取的图像进行了实验。实验结果表明, 选用具有最大Bhattacharyya距离值的3或4个特征可以获得较好的初步定位结果, 建筑区的检测率超过80%, 虚警率低于10%;随着边界调整的进行, 检测到的建筑区边界逐渐接近于真实边界。实验结果验证了该算法的有效性。     

Submarine canyons on the north of Chiwei Island:influenced by recent extension of the southern Okinawa Trough

Based on new multibeam bathymetric data and about 300 km long single seismic profiles, three topographic units were identified： the canyons, fractural valley and submarine terrace on the north of Chiwei Island where is a structural transition zone between the southern trough and the middle trough. The Chiwei Canyon and the North Chiwei Canyon are two of the largest canyons in the East China Sea （ECS） slope. Topographic features and architectures of them are described. The study shows that both of them are originated along faults. The evolution and spatial distribution of topographic units in the study area are controlled mainly by three groups of faults which were formed and reactive in the recent extensional phase of Okinawa Trough. The Chiwei Canyon was initia- ted during the middle Pleistocene and guided by F4 that is a N--S trending fault on the slope and F1, a large NW--SE trending fault on the trough. The pathway migration from the remnant channel to the present one of Chiwei Canyon is the result of uplift of tilted fault block that is coupled to the recent extension movements of the southern trough. The submarine terrace is detached from the ECS slope by the NEE -trending fault. The North Chiwei Canyon, developing during the late Pleistocene, is guided by FS, a N-S trending fault, diverted and blocked by the submarine terrace.     

基于时空特征分析技术的烤烟GIS系统

本文分析了烤烟信息系统对烤烟种植、生产和销售的重要作用,构建系统的必要性和应用需求,并在.NET框架下,利用ArcEngine和ArcSDE,以C/S结构实现该系统。介绍了系统的结构和功能:包括地图服务、烤烟信息查询统计和烤烟地理信息时空分析和决策支持。同时,讨论了实现该系统的关键技术,包括时空数据库、时空序列的烤烟时空事件分析模型、Web服务等。时空数据包括业务数据和行政区数据两类,对于行政区,除了需要记录行政区的生命周期外,还需记录行政区变更事件,通过行政区变更事件表查询行政区撤消、合并等事件后的业务数据,进而实现时空分析。系统的实现对促进烤烟生产信息化有重积极意义。     

基于Gabor变换和支持向量机的手写体字符识别算法

针对在手写字符识别中由于书写习惯和风格的不同造成字符模式不稳定的问题,将支持向量机SVM方法用于手写字符的识别.算法首先采用Gabor变换提取手写字符图像的特征参数,然后采用提取的特征训练SVM分类器.再应用SVM分类器分类和判别手写字符.实验表明这种方法具有良好的车牌识别效果,较强的鲁棒性,较大的应用价值.     

基于特征提取的目标变化检测方法研究

针对不同时相遥感影像中特定目标的变化,研究了基于特征提取的目标变化检测方法。该方法首先根据目标的几何特征进行检测与提取,然后对提取出的两目标影像进行比较,得到特定目标的变化。实验结果表明该方法对特定目标的变化检测有较好的效果。     

东海三疣梭子蟹雌体不同生理阶段肝胰腺的生化组成与其组织学结构的关系

通过生化分析和组织切片技术,系统研究了东海三疣梭子蟹第一次卵巢发育过程中肝胰腺指数(HSI)、主要生化成分和组织学结构的变化。结果表明:(1)三疣梭子蟹第一次卵巢发育过程中HSI呈先上升后下降趋势,最大值在Ⅳ期[(7.46±1.23)%],最低值在Ⅵ期[(4.62±0.63)%];(2)三疣梭子蟹第一次卵巢发育过程中,肝胰腺中的生化组成存在显著变化,Ⅰ期肝胰腺中水分含量高达67.91%,其他各期间无显著差异(P>0.05),肝胰腺中脂肪/湿重含量呈先上升后下降趋势,Ⅰ期最低(13.48%),Ⅳ期最高(24.24%);肝胰腺中蛋白/湿重并无显著变化(P>0.05),而总糖/湿重呈显著下降趋势(P<0.05);(3)不同生理阶段雌体肝胰腺组织学存在两个较明显的变化—生殖蜕壳及产卵前后,Ⅰ期肝小管中B细胞占优势(约50%左右),R细胞较细长,肝小管内腔中存在大量食物残渣和脱落的B细胞顶泡等,生殖蜕壳后(Ⅱ期后)的雌体肝胰腺中R细胞数量较多,随着时间的推移R细胞逐渐饱满。产卵后雌体肝胰腺中的细胞间界限变得模糊,部分肝小管的管腔开始自溶,但是此时B,F细胞数量开始增多,这说明随着春季东海海区水温的升高,雌体开始恢复摄食,以保证第二次卵巢发育的顺利进行。     

Submarine canyons on the north of Chiwei Island: influenced by recent extension of the southern Okinawa Trough

Based on new multibeam bathymetric data and about 300 km long single seismic profiles, three topographic units were identified:the canyons, fractural valley and submarine terrace on the north of Chiwei Island where is a structural transition zone between the southern trough and the middle trough. The Chiwei Canyon and the North Chiwei Canyon are two of the largest canyons in the East China Sea (ECS) slope. Topographic features and architectures of them are described. The study shows that both of them are originated along faults. The evolution and spatial distribution of topographic units in the study area are controlled mainly by three groups of faults which were formed and reactive in the recent extensional phase of Okinawa Trough. The Chiwei Canyon was initiated during the middle Pleistocene and guided by F4 that is a N-S trending fault on the slope and F1, a large NW-SE trending fault on the trough. The pathway migration from the remnant channel to the present one of Chiwei Canyon is the result of uplift of tilted fault block that is coupled to the recent extension movements of the southern trough. The submarine terrace is detached from the ECS slope by the NEE-trending fault. The North Chiwei Canyon, developing during the late Pleistocene, is guided by F5, a N-S trending fault, diverted and blocked by the submarine terrace.     

北黄海大鹿岛海域营养盐分布特征

根据１９９０年７月辽宁省海岛调查资料，本文讨论了北黄海大鹿岛海水营养盐（ＰＯ４－Ｐ，ＳｉＯ３－Ｓｉ，ＮＯ３－Ｎ，ＮＨ４－Ｎ，ＮＯ２－Ｎ）分布特征，并对海域环境质量作了初步评价。     

莱州湾地区郯庐断裂带的构造特征及其新生代演化

郯庐断裂带中段分东西两支从莱州湾进入渤海,在莱州湾地区的构造特征与演化历史一直鲜为人知。通过对横穿研究区的两条地震测线的解释和分析,揭示了该区郯庐断裂带中段在研究区的构造差异,研究表明郯庐断裂带东西两支在该研究区表现出不同的断裂性质,西支断裂表现为正断层,东支断裂表现为走滑断层。郯庐断裂是本研究区的主控断裂,通过对本地区地层形态及其组合、断层的剖面形态和空间展布规律的深入研究,揭示了郯庐断裂带在莱州湾地区新生代以来的构造演化历史:古新世—始新世的伸展阶段、渐新世—中新世早期的挤压和右行走滑阶段、中新世中晚期至今的稳定发展阶段,这几个不同时期的演化阶段主要受太平洋板块运动的方向和速度变化的控制。