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三峡水库汛末蓄水对长江中游航道条件影响及调度优化探讨 总被引:1,自引:0,他引:1
根据实测资料分析了三峡水库汛末蓄水对长江中游航道条件的影响,在此基础上,对正常运行期的蓄水调度方案进行了优化探讨。研究结果初步认为:目前水库蓄水时间必须提前至9月,宜昌下泄流量应大于10 000~12 000 m3/s,每日流量变幅不宜超过1 500 m3/s。 相似文献
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三峡水库坝下航道有8处重点浅滩和7处一般碍航浅滩。根据主要浅滩的碍航特性,为保证三峡水库初期汛后水库蓄满和减轻对坝下航道的不利影响,对长江委原设计的正常蓄水方式、清华大学的推迟蓄水方式、武汉大学的提前蓄水方式和长江航道局的有控制延长蓄水方式等4种不同汛后蓄水方案进行了对比分析,针对各汛后蓄水方式存在的优缺点,结合日平均最小下泄流量和两坝间水位日变幅的要求,提出了汛后蓄水的较优调度控制对策。 相似文献
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夹岩水利枢纽及黔西北供水工程是贵州省有史以来规模最大的水利枢纽工程,总库容1323亿立方米。水库于2021年12月28日实现.下闸蓄水,由于前期未考虑导流洞封堵蓄水至泄洪洞进口水位阶段的生态流量下放满足121m3/s环境水量问题,不满足现行环保政策下放生态流量的要求,为顺利实现下闸蓄水、同时满足生态流量下放要求,在制定下闸蓄水方案时,导流洞内安装两条生态道及生态流量闸阀,蓄水前期由导流洞内安装的两条生态下放生态流量,蓄水至泄洪洞进口水位后,由泄洪洞下放生态流量,实施导流洞二期永封堵从而确保了水库水利实现下闸;蓄水,同时满足河道生态流量下放的保障措施。 相似文献
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某水电站坝区地层以第四系地层为主,水库蓄水后存在绕坝渗漏问题。在采用渗流模拟程序对坝区渗流场蓄水前后进行计算后,认为库区蓄水后渗漏量较大,需进行相应的防渗工程处理。 相似文献
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介绍了我国港口资源的整合现状,指出港口整合可以提升港口的形象和地位,也为区域经济和城市的发展注入强大的动力。最后指出在港口资源整合中要避免的几个问题。 相似文献
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广州集装箱码头的轮胎式场桥小车制动器使用10多年后,出现了许多问题,故进行了改造.分析了轮胎式集装箱龙门起重机小车制动器的主要故障现象,提出了改造方案,并加以实施. 相似文献
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本文对现有的选定球面轴承的三种工程方法进行了分析比较.引入了“合力系数”,并给出了合力方向上投影面积的精确解. 相似文献
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分析柴油机故障中常见的机体裂纹故障原因,认为由于设计缺陷和管理及操作不当,易造成船舶柴油机缸体上的裂纹多发生在气缸套凸肩处。如不及时处理这些裂纹和故障,就会造成缸套的裂纹直至出现缸套漏水等严重后果,针对NANTAIQUEEN轮柴油机对该类型故障的检修提出具体措施。 相似文献
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The hydrophysical and hydrochemical structure of the Sea of Azov, with developed bottom anoxia, was studied during the RV “Akvanavt” cruise from July 31 to August 03, 2001. The anoxic zone with a thickness from 0.5 to 4 m above the bottom was found in all deep regions of the Sea. Concentrations of hydrochemical parameters were similar to the pronounced anoxic conditions (about 90 mmol m− 3 of hydrogen sulfide, 17 mmol m− 3 of ammonia, 6 mmol m− 3 of phosphate, 7 mmol m− 3 of total manganese). The hydrophysical structure was characterized by the uniform distribution of temperature in the upper 6–7 m mixed layer (UML). Below this a thin (0.4–0.8 m) thermocline layer was observed, just above the anoxic waters. Formation of this phenomenon was connected with that summer weather conditions. Intensive rains led to increased influx of river waters in June. That resulted in large input of allochtonous organic matter (OM) and inorganic nutrients; the latter were consumed on the additional autochthonous organic matter production. In July the weather was characterized by a significant rise in the daily averaged air temperature and large oscillations of temperature during the day. In this period a wind of constant direction was absent, but wind bursts were observed. The completed analyses showed that the formation of such a structure could be connected with the following factors: (i) positive growth trends of the daily averaged temperature and the daily oscillations of temperature, (ii) presence of wind bursts. The joint action of these factors resulted in the formation of the UML. The amplitude of wind bursts determined the depth of UML, and the value of trend determined the value of the temperature change in the thermocline. An initial presence of bottom halocline (caused by the Black Sea water influx to the bottom of the Sea of Azov) prevented the heating of the bottom layer and therefore led to an increase of vertical gradient of temperature in the thermocline. The spatial distribution of the turbulent exchange coefficient confirmed the existence of a “stagnation” area located above the anoxia zone, which is also, apparently, the reason for its occurrence. 相似文献