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1.
如何使QDQ2—1型电解水制氢机安全高效工作   总被引:1,自引:0,他引:1  
QDQ2-1型电解水制氢设备较QJQ-2型设备在结构和性能方面都有了很大的改进和提高。它的优势在今年彩球庆典服务部氢气供给中得到了很大发挥。首先它能连续几天甚至1个月不停机,而且开机时间越长,机器越不易坏,单位时间的产量也越高。它的电解槽采用了水冷却,较过去的QJQ-2型电解槽风冷式有了很大的优越性。QDQ2-1型电解水制氢设备要求电解槽工作温度在75~85℃之间。如果温度太低,产量反而很低,耗电量增大,而且机器频繁开关也会缩短其使用寿命。1 QDQ2-1型电解水安全高效工作方法1.1 开机时低电压、低电流在冷机器开机时,千万不能将…  相似文献   

2.
QDQ2—1型水电解制氢设备自投入业务使用以来,让广大涉氢人员从繁重的化学制氢工作中解脱出来。该设备操作方便、安全系数高,劳动强度低,深受广大涉氢人员喜爱。本文介绍了QDQ2—1型水电解制氢设备的基本组成和基本工作原理以及一些设计上的缺陷,通过对QDQ2—1型水电解制氢设备在台站实际低温工作环境中出现的问题的分析,列举了该设备在低温环境运行时存在的硬件问题,对于该设备在低温环境下自身设计上的一些缺陷提出了后期的弥补改造方法,以达到充分发挥该设备在业务中的积极作用,更好地维护该设备,延长其用寿命的目的。  相似文献   

3.
QDQ2-1型电解水制氢机,系中国船舶工业总公司718所研制的军工产品。该设备的主要优点是:结构紧凑,整体性强。制氢和贮气同步进行,操作方便,产量可调,没有污染,且体积小占地面积少便于安装。工作状态一目了然,各种数据由面板的仪表直接显示。具有完整的安全保障系统。电解槽压力报警,温度报警,贮气罐压力报警。这三项均可设预定值。一旦由于某项失控,超过预定值便发出报警信号,同时自动切断主机电  相似文献   

4.
过去制氢是个繁重的体力劳动,因其操作繁琐而且及其危险,到了冬季制氢尤其困难。QDQ2-1型水电解制氢设备已在各探空站安装使用,为了减少电能消耗,电解液不是用纯净的水,而是用一定浓度的NaOH或KOH溶液,这类新型制氢设备是通过专门装置消耗水及电解得到氢气和氧气。此设备操作简便、安全系数高,大大减轻了劳动强度,使青海省探空质量有了长足的进步。  相似文献   

5.
库尔勒探空站水电解制氢设备2002年10月投入业务运行。笔者从安全生产和设备维护的几个实例中,探讨如何做好Q DQ2-1型水电解制氢设备安全生产使用及故障排除工作。1水电解制氢系统安全生产与使用要做好设备安全使用工作,在建立健全各项规章制度同时,应注重提高工作人员的操作技能。操作人员应严格按照《水电解制氢装置操作规程》进行。开机运行前进行全面巡检,各项技术指标必须达到运行要求后,设备方可正式启动运行。操作人员应保持室内清洁,防止地面积水,特别是电解槽体和PVC电缆管要保持干燥,严禁用金属器件敲击储氢罐,制氢室、充球室…  相似文献   

6.
气象用GX-2型电解水制氢设备是由广西气象技术装备中心研制,经中国气象局列装的气象装备,广泛应用于长江以南各省探空站中.为增加安全使用效果,在大修时,对相关部位应足够重视,还可对相关部分进行改进.  相似文献   

7.
通过对桂林高空站电解水制氢设备常见故障进行分析,总结和阐述维修经验,为提高设备使用效率、保障设备正常运行提供参考.  相似文献   

8.
压滤式电解水制氢使用经验交流会,于五月廿日至二十四日在第一台压滤式电解水制氢设备诞生地——梧州召开。此次会议  相似文献   

9.
对广西型电解水制氢设备的优化改造谢键(宜宾地区气象局)我局有广西气象局设计的压滤式双板型电解制氢设备两台,其槽体由尼龙隔板、微孔隔膜、不锈钢电极组成,用六根螺杆贯穿固定。在使用过程中,由于部件工作条件恶劣,在强碱、高温、电化和较大的压力条件下持续工作...  相似文献   

10.
李峰 《气象》1985,11(3):29-30
一、概述 随着气象事业的发展,我国采用电解水制氢的高空气象台站越来越多。预计今年内,全国将有四十多个高空气象台站采用电解水法制氢。 在电解水制氢过程中,氢气纯度的分析是十分重要的。电解水制氢的氢气纯度应在99.5%以上,当氢气中的含氧量达到5%或以上时便形成爆鸣气体。这种爆鸣气体极易发生爆炸。因此,严格掌握不形成爆鸣气体,是安全制氢和安全用氢的前提条件。掌握好氢气纯度的化验分析,不仅有利于提高氢气的质量与探测的高度,而且还可以保证操作人员的安全。可见氢气纯度的化验分析工作,是采用电解水制氢法时必不可少的一道工序。应该严格规定,不定期进行氢气纯度的化验分析,就不允许开机制氢和使用氢气。  相似文献   

11.
Using the International Comprehensive Ocean-Atmosphere Data Set(ICOADS) and ERA-Interim data, spatial distributions of air-sea temperature difference(ASTD) in the South China Sea(SCS) for the past 35 years are compared,and variations of spatial and temporal distributions of ASTD in this region are addressed using empirical orthogonal function decomposition and wavelet analysis methods. The results indicate that both ICOADS and ERA-Interim data can reflect actual distribution characteristics of ASTD in the SCS, but values of ASTD from the ERA-Interim data are smaller than those of the ICOADS data in the same region. In addition, the ASTD characteristics from the ERA-Interim data are not obvious inshore. A seesaw-type, north-south distribution of ASTD is dominant in the SCS; i.e., a positive peak in the south is associated with a negative peak in the north in November, and a negative peak in the south is accompanied by a positive peak in the north during April and May. Interannual ASTD variations in summer or autumn are decreasing. There is a seesaw-type distribution of ASTD between Beibu Bay and most of the SCS in summer, and the center of large values is in the Nansha Islands area in autumn. The ASTD in the SCS has a strong quasi-3a oscillation period in all seasons, and a quasi-11 a period in winter and spring. The ASTD is positively correlated with the Nio3.4 index in summer and autumn but negatively correlated in spring and winter.  相似文献   

12.
The spatial and temporal variations of daily maximum temperature(Tmax), daily minimum temperature(Tmin), daily maximum precipitation(Pmax) and daily maximum wind speed(WSmax) were examined in China using Mann-Kendall test and linear regression method. The results indicated that for China as a whole, Tmax, Tmin and Pmax had significant increasing trends at rates of 0.15℃ per decade, 0.45℃ per decade and 0.58 mm per decade,respectively, while WSmax had decreased significantly at 1.18 m·s~(-1) per decade during 1959—2014. In all regions of China, Tmin increased and WSmax decreased significantly. Spatially, Tmax increased significantly at most of the stations in South China(SC), northwestern North China(NC), northeastern Northeast China(NEC), eastern Northwest China(NWC) and eastern Southwest China(SWC), and the increasing trends were significant in NC, SC, NWC and SWC on the regional average. Tmin increased significantly at most of the stations in China, with notable increase in NEC, northern and southeastern NC and northwestern and eastern NWC. Pmax showed no significant trend at most of the stations in China, and on the regional average it decreased significantly in NC but increased in SC, NWC and the mid-lower Yangtze River valley(YR). WSmax decreased significantly at the vast majority of stations in China, with remarkable decrease in northern NC, northern and central YR, central and southern SC and in parts of central NEC and western NWC. With global climate change and rapidly economic development, China has become more vulnerable to climatic extremes and meteorological disasters, so more strategies of mitigation and/or adaptation of climatic extremes,such as environmentally-friendly and low-cost energy production systems and the enhancement of engineering defense measures are necessary for government and social publics.  相似文献   

13.
Various features of the atmospheric environment affect the number of migratory insects, besides their initial population. However, little is known about the impact of atmospheric low-frequency oscillation(10 to 90 days) on insect migration. A case study was conducted to ascertain the influence of low-frequency atmospheric oscillation on the immigration of brown planthopper, Nilaparvata lugens(Stl), in Hunan and Jiangxi provinces. The results showed the following:(1) The number of immigrating N. lugens from April to June of 2007 through 2016 mainly exhibited a periodic oscillation of 10 to 20 days.(2) The 10-20 d low-frequency number of immigrating N. lugens was significantly correlated with a low-frequency wind field and a geopotential height field at 850 h Pa.(3) During the peak phase of immigration, southwest or south winds served as a driving force and carried N. lugens populations northward, and when in the back of the trough and the front of the ridge, the downward airflow created a favorable condition for N. lugens to land in the study area. In conclusion, the northward migration of N. lugens was influenced by a low-frequency atmospheric circulation based on the analysis of dynamics. This study was the first research connecting atmospheric low-frequency oscillation to insect migration.  相似文献   

14.
The atmospheric and oceanic conditions before the onset of EP El Ni?o and CP El Ni?o in nearly 30 years are compared and analyzed by using 850 hPa wind, 20℃ isotherm depth, sea surface temperature and the Wheeler and Hendon index. The results are as follows: In the western equatorial Pacific, the occurrence of the anomalously strong westerly winds of the EP El Ni?o is earlier than that of the CP El Ni?o. Its intensity is far stronger than that of the CP El Ni?o. Two months before the El Ni?o, the anomaly westerly winds of the EP El Ni?o have extended to the eastern Pacific region, while the westerly wind anomaly of the CP El Ni?o can only extend to the west of the dateline three months before the El Ni?o and later stay there. Unlike the EP El Ni?o, the CP El Ni?o is always associated with easterly wind anomaly in the eastern equatorial Pacific before its onset. The thermocline depth anomaly of the EP El Ni?o can significantly move eastward and deepen. In addition, we also find that the evolution of thermocline is ahead of the development of the sea surface temperature for the EP El Ni?o. The strong MJO activity of the EP El Ni?o in the western and central Pacific is earlier than that of the CP El Ni?o. Measured by the standard deviation of the zonal wind square, the intensity of MJO activity of the EP El Ni?o is significantly greater than that of the CP El Ni?o before the onset of El Ni?o.  相似文献   

15.
Storms that occur at the Bay of Bengal (BoB) are of a bimodal pattern, which is different from that of the other sea areas. By using the NCEP, SST and JTWC data, the causes of the bimodal pattern storm activity of the BoB are diagnosed and analyzed in this paper. The result shows that the seasonal variation of general atmosphere circulation in East Asia has a regulating and controlling impact on the BoB storm activity, and the “bimodal period” of the storm activity corresponds exactly to the seasonal conversion period of atmospheric circulation. The minor wind speed of shear spring and autumn contributed to the storm, which was a crucial factor for the generation and occurrence of the “bimodal pattern” storm activity in the BoB. The analysis on sea surface temperature (SST) shows that the SSTs of all the year around in the BoB area meet the conditions required for the generation of tropical cyclones (TCs). However, the SSTs in the central area of the bay are higher than that of the surrounding areas in spring and autumn, which facilitates the occurrence of a “two-peak” storm activity pattern. The genesis potential index (GPI) quantifies and reflects the environmental conditions for the generation of the BoB storms. For GPI, the intense low-level vortex disturbance in the troposphere and high-humidity atmosphere are the sufficient conditions for storms, while large maximum wind velocity of the ground vortex radius and small vertical wind shear are the necessary conditions of storms.  相似文献   

16.
Observed daily precipitation data from the National Meteorological Observatory in Hainan province and daily data from the National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis-2 dataset from 1981 to 2014 are used to analyze the relationship between Hainan extreme heavy rainfall processes in autumn (referred to as EHRPs) and 10–30 d low-frequency circulation. Based on the key low-frequency signals and the NCEP Climate Forecast System Version 2 (CFSv2) model forecasting products, a dynamical-statistical method is established for the extended-range forecast of EHRPs. The results suggest that EHRPs have a close relationship with the 10–30 d low-frequency oscillation of 850 hPa zonal wind over Hainan Island and to its north, and that they basically occur during the trough phase of the low-frequency oscillation of zonal wind. The latitudinal propagation of the low-frequency wave train in the middle-high latitudes and the meridional propagation of the low-frequency wave train along the coast of East Asia contribute to the ‘north high (cold), south low (warm)’ pattern near Hainan Island, which results in the zonal wind over Hainan Island and to its north reaching its trough, consequently leading to EHRPs. Considering the link between low-frequency circulation and EHRPs, a low-frequency wave train index (LWTI) is defined and adopted to forecast EHRPs by using NCEP CFSv2 forecasting products. EHRPs are predicted to occur during peak phases of LWTI with value larger than 1 for three or more consecutive forecast days. Hindcast experiments for EHRPs in 2015–2016 indicate that EHRPs can be predicted 8–24 d in advance, with an average period of validity of 16.7 d.  相似文献   

17.
Based on the measurements obtained at 64 national meteorological stations in the Beijing–Tianjin–Hebei (BTH) region between 1970 and 2013, the potential evapotranspiration (ET0) in this region was estimated using the Penman–Monteith equation and its sensitivity to maximum temperature (Tmax), minimum temperature (Tmin), wind speed (Vw), net radiation (Rn) and water vapor pressure (Pwv) was analyzed, respectively. The results are shown as follows. (1) The climatic elements in the BTH region underwent significant changes in the study period. Vw and Rn decreased significantly, whereas Tmin, Tmax and Pwv increased considerably. (2) In the BTH region, ET0 also exhibited a significant decreasing trend, and the sensitivity of ET0 to the climatic elements exhibited seasonal characteristics. Of all the climatic elements, ET0 was most sensitive to Pwv in the fall and winter and Rn in the spring and summer. On the annual scale, ET0 was most sensitive to Pwv, followed by Rn, Vw, Tmax and Tmin. In addition, the sensitivity coefficient of ET0 with respect to Pwv had a negative value for all the areas, indicating that increases in Pwv can prevent ET0 from increasing. (3) The sensitivity of ET0 to Tmin and Tmax was significantly lower than its sensitivity to other climatic elements. However, increases in temperature can lead to changes in Pwv and Rn. The temperature should be considered the key intrinsic climatic element that has caused the "evaporation paradox" phenomenon in the BTH region.  相似文献   

18.
正The Taal Volcano in Luzon is one of the most active and dangerous volcanoes of the Philippines. A recent eruption occurred on 12 January 2020(Fig. 1a), and this volcano is still active with the occurrence of volcanic earthquakes. The eruption has become a deep concern worldwide, not only for its damage on local society, but also for potential hazardous consequences on the Earth's climate and environment.  相似文献   

19.
The moving-window correlation analysis was applied to investigate the relationship between autumn Indian Ocean Dipole (IOD) events and the synchronous autumn precipitation in Huaxi region, based on the daily precipitation, sea surface temperature (SST) and atmospheric circulation data from 1960 to 2012. The correlation curves of IOD and the early modulation of Huaxi region’s autumn precipitation indicated a mutational site appeared in the 1970s. During 1960 to 1979, when the IOD was in positive phase in autumn, the circulations changed from a “W” shape to an ”M” shape at 500 hPa in Asia middle-high latitude region. Cold flux got into the Sichuan province with Northwest flow, the positive anomaly of the water vapor flux transported from Western Pacific to Huaxi region strengthened, caused precipitation increase in east Huaxi region. During 1980 to 1999, when the IOD in autumn was positive phase, the atmospheric circulation presented a “W” shape at 500 hPa, the positive anomaly of the water vapor flux transported from Bay of Bengal to Huaxi region strengthened, caused precipitation ascend in west Huaxi region. In summary, the Indian Ocean changed from cold phase to warm phase since the 1970s, caused the instability of the inter-annual relationship between the IOD and the autumn rainfall in Huaxi region.  相似文献   

20.
正While China’s Air Pollution Prevention and Control Action Plan on particulate matter since 2013 has reduced sulfate significantly, aerosol ammonium nitrate remains high in East China. As the high nitrate abundances are strongly linked with ammonia, reducing ammonia emissions is becoming increasingly important to improve the air quality of China. Although satellite data provide evidence of substantial increases in atmospheric ammonia concentrations over major agricultural regions, long-term surface observation of ammonia concentrations are sparse. In addition, there is still no consensus on  相似文献   

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