地质雷达探测工程的几个问题   总被引：1，自引：0，他引：1  

余中明  丁强 《地质找矿论丛》2006,21(Z1):182-184

地质雷达(GPR)探测技术在浅层地质勘探领域广泛应用,并取得较好的应用效果.文章针对消除干扰的方法、关于防空洞探测、关于公路路面检测和隧道衬砌质量检测、地下岩溶探测等内容进行了探讨.  相似文献   

广西"十五"数字测震台网信道建设与系统集成   总被引：3，自引：2，他引：3  

姚宏  孙学军 《地震地磁观测与研究》2007,28(5):57-62

通过实施广西"十五"数字测震台网建设项目,在保证地震速报能力的前提下,根据广西区域数字测震台的布局,合理选择台站不同数据传输模式和台网集成方案,以取得系统的优良性价比.  相似文献   

Seismic identification of channel sandbodies in the Fuyang oil layer in North Songliao Basin, China     

刘金平王允清  杨懋新谢春来赵秀红  陈淑梅 《应用地球物理》2007,4(2):127-132

The Fuyang oil-layer in North Songliao Basin is characterized by thin interbedded sands and shales, strong lateral variation, strong reservoir heterogeniety, and so on. The thickness of individual sand layers is generally 3 - 5 m. Identifying the channel sand-bodies of the Fuyang oil layer using seismic techniques is very difficult due to the low seismic resolution. Taking the GTZ area as an example, we discuss the genetic characteristics of the channel sand-bodies and point out the real difficulty in using seismic techniques to predict the channel sand-bodies. Two methods for the identification of channels are presented： frequency spectrum imaging and pre-stack azimuthal anisotropy. Identifying the channel sand-bodies in Fuyu oil-layer using the two seismic methods results in a success rate up to 80% compared with well data.  相似文献   

冰塞水位分析   总被引：2，自引：0，他引：2       下载免费PDF全文

王军  付辉  伊明昆  尹运基  高月霞 《水科学进展》2007,18(1):102-107

高纬度地区河流冬季常形成冰塞,冰塞堵塞过流断面,使湿周增加,致上游水位升高,常因此产生凌洪灾害,冰塞的解体、溃决又常使下游产生灾害。冰期水位是冰塞演变和发展的重要结果之一,对于防灾减灾具有重要的参考价值。依据实验室资料和黄河河曲段的实测资料,针对直道和弯槽,对比分析了不同冰流量、不同初始水深和流速时模拟冰塞和天然河道冰期水位的变化规律。  相似文献   

松辽盆地中央坳陷南部下白垩统泉头组四段沉积相   总被引：7，自引：0，他引：7  

张庆国  鲍志东  那未红  周新茂  孙继武 《古地理学报》2007,9(3):267-276

松辽盆地中央坳陷南部下白垩统泉头组四段沉积时期，松辽盆地地形平缓，基底沉降缓慢，在湖平面整体扩张及浅水背景下河流入湖成三角洲沉积。通过岩心观察、相标志与测井相研究，该区储层主要为岩屑长石砂岩和长石岩屑砂岩，识别出三角洲平原、三角洲前缘、前角洲3种亚相，以及分支河道、天然堤、决口扇、分支河道间湾、水下分支河道、水下决口扇、河口坝、远沙坝、水下分支河道间湾9种微相三角洲平原、三角洲前缘广泛发育，前三角洲不发育。三角洲平原分支河道通过填积和频繁的分叉改道，向湖盆中心方向长距离推进，在三角前缘的浅水区域发育了大量水下分支河道，分支河道与水下分支河道砂体相互切割、叠加，形成了平均宽度200~600 m、平均厚度3~8 m的道单砂体，（水下）分支河道砂体构成了油气富集的主要储集体。该区沉积相的精细研究，为进一步调整开发井网奠定了基础。  相似文献   

南海夏季风爆发早晚的越赤道气流特征   总被引：1，自引：0，他引：1  

覃志年  金龙何慧 《广西气象》2007,28(3):8-11

根据国家气候中心提供的南海夏季风爆发期典型偏早（1966、1972、1996、2000、2001年）和偏晚年份（1970、1973、1987、1989、1991年）,利用ECMW F再分析1-5月逐日经向风资料,计算5个通道越赤道气流和越赤道乞流总量的距平值;探讨越赤道气流与南海夏季风爆发早晚的关系与特征。为预测南海夏季风爆发早晚提供判据。  相似文献   

任意色阶区间精细选区创建方法初探     

江王记 《现代测绘》2007,30(6):37-38

在通道中利用“阂值”命令创建选择X-255。在通道混合中创建任意色阶区间选择X1～X2。利用通道混合“减去”模式中“缩放”“补偿值”实现深度自由选择。  相似文献   

Influence of diversion angle on water and sediment flow into diversion channel     

《国际泥沙研究》2020,35(6):600-608

Accumulation of the sediment in the stream of the diversion channels adversely affects its operational systems. Diversion channels are often constructed perpendicular to the main river. In this study, the water flow and sediment transport in the diversion channel with different angles were investigated in an attempt to maximize water discharge and minimize sediment discharge. A physical model with movable bed was used to simulate water and sediment flow with five diversion angles (θ) between (30°–90°). Moreover, three bed width ratios (B_r) (the relation between diversion to main channel bed width) between 30% and 50% and five total discharges between (7.25 L/s to 12.25 L/s) were considered for each case of (θ). The results showed, up to 10%, increasing in proportion discharge ratios for 30 and 45 diversion angles compared with 90° diversion angle. The results also showed that the lowest diversion sediment concentration was provided by the (θ) of 30°. Across all scenarios, the average proportion concentration reduction was 64%, compared with 90° diversion angle. Closer observation of the diversion system mechanism confirmed that decreased (θ) result in decreased sediment concentrations in the diversion channels. In conclusion, the diversion channel water and sediment discharge could be effectively managed by changing the (θ) to 30° or 45° instead of 90°.  相似文献   

湖平面升降对浅水三角洲前缘砂体形态的影响   总被引：7，自引：4，他引：3  

楼章华  蔡希源 《沉积学报》1998,16(4):27-31

三角洲平原上的分流河道通过填积和湖面的频繁波动向湖泊中心方向长距离推进,在浅水三角洲前缘的浅水区发育很有特色的水下分流河道,且在湖面频繁波动过程中,河流、波浪和沿岸流的冲刷作用对沉积物分布起到再改造作用,导致了以水下分流河道砂体为主的三角洲前缘砂体不同程度的席状化。随着气候变得潮湿,湖面相对稳定,季节性、周期性湖面波动的频率、幅度减小,水动力对三角洲前缘砂体的改造和席状化强度减弱。  相似文献   

Further assessment of flood‐ and drought‐dominated regimes in south‐eastern Australia     

Wayne D. Erskine  R.F. Warner 《The Australian geographer》1998,29(2):257-261

Kirkup et al. (1998) [Australian Geographer 29, pp. 241–55] criticise our theory of alternating flood regimes and question its application to river management. A brief but critical appraisal of their work shows many errors and misrepresentations. When these are corrected, their challenge is found deficient.  相似文献