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排序方式: 共有198条查询结果,搜索用时 15 毫秒
51.
为弥补SUBSITE型仪器未提供比值法测深功能的缺陷,特设计了“任意比值测深尺”。其原理表明,埋深是偏距的一元函数,任意选取一个比值参数d,根据实测的偏距即可确定埋深。株洲地质勘察院在江阴市城市管线普查工作中,根据上述原理设计制作了任意比值法测深尺。其制作简单,只需一把普通钢卷尺,以比值0.7为例,偏距为0.058m时埋深为0.1m。对卷尺0.058m处背面用白色油漆画上刻度并标上0.1m 即可,其余依此类推。这把卷尺背面,就成了SUBSTTE型仪器专用的比值法测深尺。实际操作中,与RD型仪器70%比值法比较,除量取偏距的米尺不同外,其余完全相同。生产实践中使用它测深约3000个点,精度很高,经受住了实践的检验。 相似文献
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An Oscillating Water Column (OWC) device can output energy through reciprocating or unidirectional airflow. The unidirectional airflow is helpful to utilize a simple and high-efficiency unidirectional air turbine. The pentagonal BBDB proposed by us based on OWC principle can be regarded as a floating Oscillating Body and its Power Take-Off (PTO) consists of a chamber, a water column, a turbine and a generator. The Capture Width Ratio (CWR) of the pentagonal BBDB model with the reciprocating and unidirectional airflow was studied in this paper. The wave flume test results indicate the mean CWR of the pentagonal BBDB model with reciprocating airflow can reach up to 121.91% and the mean CWR of the model with unidirectional airflow could reach 100.94% during the whole wave cycle in regular waves. For irregular waves, the mean CWR of the model with the unidirectional airflow is as high as 62.83% during the whole wave cycle. Hopefully, the combination of the pentagonal BBDB with the check valve to output power during the air exhalation and conventional high-efficiency unidirectional turbine will improve the total efficiency of the BBDB. 相似文献
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利用新疆伽师震区附近的喀什、乌什、巴楚3个数字台记录到的伽师地震序列波形资料,开展地震波谱研究。首先分析了伽师6.8级地震序列各台的地震波拐角频率及其比值的时序变化特征,然后从中选出对这3个台都有较好记录的66个地震事件,进行拐角频率比时序变化特征的对比研究。结果表明,这3个台的拐角频率及其比值在伽师6.8级地震前后都出现了不同的变化趋势,尤以比值的变化更为明显,而且不同台站间的变化趋势存在较为明显的差异。最后讨论了这些差异可能存在的一些原因。 相似文献
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In the study of the application of MODIS satellite remote sensing data to earthquake prediction, the paper puts forward for the first time a quantitative method to estimate the ratio for the pixels with abnormal brightness temperature (BT) increase and a preliminary scheme for cloud removal. The principle is that, firstly, the cloudless data observed by the same satellite at the same period of time but in different days (usually 1 day to 3 days) are mosaiced to get high ratio of clear sky, and then the BT variation curve and mean square difference (MSD) of each pixel are calculated with the data from the covered area to determine daily whether the BT data of the day is normal or not at a certain pixel by using double the MSD as the criterion. The ratio for the pixels with abnormal BT increase can be calculated by dividing the total number of abnormal pixels with the total pixels of the whole area. Analysis on a series of recent earthquakes in the Taiwan area shows that the ratio for pixels with abnormal BT increase, which normally undulates around zero, has a sudden enhancement 1 day to 20 days before medium-strong earthquakes. It is expected that a new method for identifying earthquake auspice could be found through special studies in regions with frequent seismic activity by analyzing the change of the ratio for the pixels with abnormal BT increase from MODIS satellite remote sensing infrared (IR) information from which the effect of clouds has been removed to a certain extent. 相似文献
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饱和砂土液化判别方法中问题浅析 总被引:19,自引:3,他引:16
国内外各种勘察规范中所判别砂土液化的方法很多,但其效果如何,很维得到难3,笔者利用唐山地震砂土液化资料对几种目前较为常用、有代表性的方法进行了回判分析,指出了这些方法中存在的问题,并阐述了影响液化的主要因素。 相似文献
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This study tests the hypothesis that the in situ void ratio of surficial marine sediments may be predicted from shear wave velocity-depth data with a reliability equal to that of other methods currently available. Shear wave velocity is fundamentally controlled by the number of grain-to-grain contacts per unit volume of material and by the effective stress across those contacts. In this study, three previously established empirical formulae are used to predict void ratio from velocity-depth data. Field data were acquired along a transect off the northern Californian coast across which water depth increased from 35 to 70 m and seafloor sediment type varied from sand to silty-sand, respectively. A towed seafloor sled device was used to collect shear wave refraction data, and a marked, systematic decrease in velocity was observed along the line, ranging from 35-70 m/s for the coarse, near-shore material to 25-40 m/s for the finer, offshore deposits. Void ratios predicted from these velocities were compared with data measured directly from box-core samples. Of the formulae used for prediction, two agree remarkably well with the control data. Both predicted and control values increase from 0.6-0.8 for the sandy material to 1.1-1.5 for the silty-sand. Thus, this study does not disprove the hypothesis set and demonstrates the potential of field shear wave velocity-depth data as a means of delineating spatial variation in void ratio for surficial marine sediments in a remote, nondestructive manner. 相似文献