共查询到17条相似文献，搜索用时 250 毫秒
1.
光学测量方法是高频振动检测领域新的研究方向。该论文研发了由光纤振动检测传感器、光纤振动信号检测单元等系统组成的一个振动检测系统,使用端面反射的基本原理。振动信号经过光纤振动传感器转化为光信号,再经过检测单元转化为电信号,最终得到测量频率。实验测得该系统的频率响应范围是2～33 kHz,测量误差小于0.21%。该系统的光纤振动传感器是强度调制型光纤传感器,避免了波长解调,相对于其他光学测量系统具有测量带宽广、测量频率高、振动传感器设计简洁等优点。 相似文献
2.
为克服温度对溶解氧传感器的影响，对极谱型溶解氧检测系统的溶解氧电极激励源、高精度信号采样、软件标定和温度补偿等方面进行研究。通过对极谱型溶解氧传感器工作原理进行分析，设计了极谱型溶解氧传感器检测电路；根据溶解氧电极的温度特性，设计了基于NTC（负温度系数）热敏电阻的硬件温度补偿电路，并利用最小二乘法及RBF神经网络构建了软件温度补偿模型。利用饱和蒸馏水进行温度补偿实验，结果表明：经温度补偿后，该溶解氧检测系统的相对误差及采样波动均在1%以内，大大减小了传感器的非线性误差，测量精度和稳定性均可满足应用要求。 相似文献
3.
锁相检波技术采用模拟乘法器,对与本地载频信号频率一致的输入信号有强的检测能力.在分析典型的CW和FSK水声遥测信号特点的基础上,根据音频锁相检波器NE567的设计公式和应用要点,设计了锁相检波模块,用于多通道遥控测距装置,湖上和海上实验证明了应用的有效性. 相似文献
4.
本文提出的跟踪滤波锁相方法是从大气回波信号中有效地检测Ｄｏｐｐｌｅｒ频偏信号的新方法，在信号持续时间受限或数据记录长度受限的条件下，能获得满意的频率分辨力和空间分辨力。 相似文献
5.
本文提出一种以对连续波进行锁相来实现声速测量的方法。它利用压控振荡器的正弦信号在介质中产生连续超声波,然后将来自相隔一定距离的超声波发射点和接收点的两个信号输入鉴相器,鉴相器的输出经低通滤波后即成为压控振荡器的控制电压。这样的锁相环路所锁定信号频率能保证发、收两点间的距离与超声波波长之比为固定值,该频率反映了声速的大小。文章介绍了使用本方法,以斜探头产生的表面波对钢带和钢筋进行的声弹性测量试验;和用收发一体化换能器对特殊形状螺栓所作的轴向力测量试验。试验情况表明,锁相法使超声波频率能灵敏地跟踪介质中声速的变化,而且还能对四端网络传递函数极点位置进行锁定和跟踪。 相似文献
6.
7.
一种新的用于极化SAR图像船只检测的散射相似性测度 总被引：1，自引：0，他引：1
本文提出了一种新的用于极化合成孔径雷达（SAR）海上船只目标检测的测度。首先利用散射相似性参数研究船只与海杂波散射机制的差异。基于这些差异，提出了一种新的船只检测测度，该测度能够有效区分船只目标和海杂波。然后提出了利用核密度估计（KDE）方法对该测度进行建模的方法。基于统计模型，实现了自适应恒虚警率（CFAR）的检测方案。本文利用多景C波段RADARSAT-2极化SAR（Pol-SAR）数据上进行实验，系统分析了所提出测度的海杂波拟合性能与船只检测性能，并与两个经典的极化测度进行了比较，实验和比较结果证明了所提的测度的可行性。 相似文献
8.
溶解氧是海洋水质监测的常规关键参数,基于荧光猝灭原理研制的溶解氧传感器具有准确度高、稳定性好和可长期在线测量等优点,已经被广泛用于海水溶解氧浓度监测。针对传感器可能发生的数据漂移和显著偏差可能造成的准确度问题,本文设计了一套专门的校准装置和校准方法。通过严格控制校准水体的温度和溶解氧浓度,测量待校准传感器和参比传感器的相移、温度和溶解氧浓度数据,拟合获取传感器校准系数,实现对光学溶解氧传感器的单个多点校准。传感器校准值与参比值偏差在±8μmol·L–1以内。实验室和海水现场比测结果显示,校准结果达到传感器性能指标要求。此校准装置及方法并不局限于光学溶解氧传感器,具有良好的推广价值。 相似文献
9.
基于DDS技术的噪声分析及抑噪实现 总被引：2，自引：0，他引：2
直接数字合成(DDS)是一种重要的频率合成技术,具有分辨率高、频率变换快等优点,在雷达、海洋ADCP及通信等领域有着广泛的应用前景。文中对DDS技术所含有的噪声进行了剖析,并得出结论,在量化字长一定的情况下,产生波形的频率误差与参考频率有很大的关系,参考频率越高,波形质量越好,并且当信号的当参考时钟频率与所发射波形频率之比小于10：1时,波形会产生明显的失真;针对DDs技术的噪声,结合具体的数字合成芯片AD9854,提出了一种设计Butterworth滤波器去噪的方法,该方法简单,易行,具有良好的通用性。 相似文献
10.
研制出一种对溶解氧敏感的传感膜,其荧光材料主要是邻菲咯啉钌。由光源发出的中心波长为465 nm的强光照射到铺有该络合物的膜片上,激发出中心波长为620 nm的荧光,水体中的溶解氧会对激发出的荧光产生猝灭效应,猝灭程度与溶解氧的质量浓度之间存在线性关系。该膜片在无氧水中的荧光强度是空气饱和水中的20倍,变化较为明显。对比检测荧光信号在待测水体中猝灭前后的强度,即可测出水体中溶解氧的质量浓度。基于这一原理和荧光测量技术研制了光学溶解氧分析仪,利用该仪器对6处不同水域的天然水体进行测试,所得测试结果与国标碘量法的测试结果之间不存在显著性差异,误差≤2%,响应时间<1 min。在海水中30 m深处进行36h稳定性考察,所得溶解氧质量浓度数值平均偏差小于0.2 mg.L-1,证实仪器可适应较为恶劣的环境,且稳定性较好。 相似文献
11.
介绍一种SWQ-1型多功能水质测定仪,以数字显示温度,盐度,溶解氧,pH和氧化还原电势。仪器用干电池供电,其结构是以一个带有多路模数转换器和液晶显示器的低功耗单片微计算机为基础而构成。通过微计算机按照存贮器中的物理化学公式和定标常数进行数据处理,并把结果送给显示器。温度和pH传感器用的是定型的商品—热敏电阻和玻璃电极。盐度和溶解氧分别采用由作者自行设计的铂电极电导池和薄膜原电池型传感器进行现场测量。溶解氧的测量采用了自动定标程序,减少了电位漂移对测量的影响,提高了测量的可靠性,并且便于操作。这种水质测定仪是一种尺寸小,重量轻,效率高的便携式仪器。 相似文献
12.
RESEARCH ON DETERMINATION OF DISSOLVED OXYGEN IN SEAWATER 总被引：1，自引：0，他引：1
Based on the principle of laminar flow-constant potential-chronocoulometry, this article presents a new method of determining the dissolved oxygen in seawater with considerable success. A new model of electrochemical sensor has been designed for this purpose.The sensor has the advantage of overcoming hysteresis and "outskirts effect", thus increasing its stability and prolonging its use to 1-2 years.In connection with this new method a new model SY-1 integrating microcoulorneter with digital display is designed.It is a fast (a sample/2 min) and accurate (±1 - 1.5%) method, suitable for use in the laboratory on board a ship. 相似文献
13.
Turner RE Rabalais NN Swenson EM Kasprzak M Romaire T 《Marine environmental research》2005,59(1):65-77
An 18-year monitoring record (1978-1995) of dissolved oxygen within a region having hypoxia (dissolved oxygen less than 2 mgl(-1)) in the bottom layer was examined to describe seasonal and annual trends. The monitoring location was near or within a well-described summer hypoxic zone whose size has been up to 20,000 km(2). The monitoring data were used to hindcast the size of the hypoxic zone for before consistent shelfwide surveys started, and to predict it for 1989, when a complete shelfwide survey was not made. The concentration of total Kjeldahl nitrogen (TKN) in surface waters and concentration of bottom water oxygen were directly related, as anticipated if organic loading from surface to bottom was from in situ processes. The TKN data were used to develop a predictive relationship that suggested there was no substantial hypoxia before the 1970s, which was before nitrate flux from the Mississippi River to the Gulf of Mexico began to rise. The peak frequency in monthly hypoxic events is two to three months after both the spring maximum in discharge and nitrate loading of the Mississippi River. These results support the conclusion that persistent, large-sized summer hypoxia is a recently-developed phenomenon that began in the 1970s or early 1980s. 相似文献
14.
南沙群岛海区有机碳沉积作用与古生产力估算 总被引：1，自引：0，他引：1
根据南沙群岛海区５个沉积柱样和大量表层样的分析资料讨论了有机碳的沉积作用。深海有机碳含量一般为０．２％－１．３％。水柱深度对其分布的控制作用不明显。分析结果发现冰期、间冰期，尤其是本次冰期有机碳含量变化明显，４个柱样晚第四纪的质量堆积速率在末次冰期时最大。有机碳保存的主要控制因素是溶解氧浓度、粘土矿物含量、水柱深度和底栖混合强度，其中溶解氧浓度是最重要因素。底栖有孔虫的相对丰度，如Ｕｖｉｇｅｒｉｎａ和Ｂｕｌｉｍｉ－ｎａ，可用来指示溶解氧和有机碳含量。有机碳含量与海洋生产力关系极为密切，它可用来重建海洋古生产力的长期变化。采用Ｍｌｌｅｒ和Ｓｕｅｓｓ方程以及Ｓａｒｎｔｈｅｉｎ方程的计算结果与目前生产力值结果比较表明，后一种方法因充分考虑了溶解氧浓度和水柱深度而更接近现代值。 相似文献
15.
16.
A modified procedure has been proposed for the colorimetric determination of dissolved oxygen in seawater to improve its precision and accuracy. When a pickled sample is acidified, iodine liberated in the iodometric reaction is measured by direct spectrophotometry at 456 nm. Loss of molecular iodine by volatilization is eliminated by transferring the sample to a flow cuvette without contact with air. The method was calibrated for oxygen by spiking known amounts of potassium iodate. Precision was found at better than 0.2% r.s.d. (full scale). Evaluation of accuracy was made by comparison with calculated oxygen solubilities, which shows a relative bias of no more than 0.5% for oxic waters. The analytical throughput was much faster than that of the standard titration procedure. 相似文献
17.
高压密闭消解-电感耦合等离子体光谱和质谱联合测定海洋地质样品中52种元素 总被引：4，自引：0，他引：4
An improved analytical method to determine the content of 52 major, minor and trace elements in marine geological samples, using a HF-HCl-HNO_3 acid system with a high-pressure closed digestion method(HPCD), is studied by an inductively coupled plasma optical emission spectrometry(ICP-OES) and an inductively coupled plasma mass spectrometry(ICP-MS). The operating parameters of the instruments are optimized, and the optimal analytical parameters are determined. The influences of optical spectrum and mass spectrum interferences, digestion methods and acid systems on the analytical results are investigated. The optimal spectral lines and isotopes are chosen, and internal standard element of rhodium is selected to compensate for matrix effects and analytical signals drifting. Compared with the methods of an electric heating plate digestion and a microwave digestion, a high-pressure closed digestion method is optimized with less acid, complete digestion,less damage for digestion process. The marine geological samples are dissolved completely by a HF-HCl-HNO_3 system, the relative error(RE) for the analytical results are all less than 6.0%. The method detection limits are 2–40μg/g by the ICP-OES, and 6–80 ng/g by ICP-MS. The methods are used to determine the marine sediment reference materials(GBW07309, GBW07311, GBW07313), rock reference materials(GBW07103, GBW07104,GBW07105), and cobalt-rich crust reference materials(GBW07337, GBW07338, GBW07339), the obtained analytical results are in agreement with the certified values, and both of the relative standard deviation(RSD) and the relative error(RE) are less than 6.0%. The analytical method meets the requirements for determining 52 elements contents of bulk marine geological samples. 相似文献