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The inhibiter of gas hydrates in deep sea drilling fluids[J].

深水海底钻进泥浆中使用的天然气水合物抑制剂[J]。

The conclusions can be drawn through numerical simulation: The hydrate-forming region becomes small with increasing circulation rate and inhibiter concentration, and it is possible to make the hydrate-forming region away from sea floor by increasing circulation rate and inhibiter concentration, thus preventing blowout preventer lines from hydrate plugging; the decrease in gas volume fraction in the annulus due to hydrate formation reduces pit gain, which can delay the detection of well kick; the possibility of hydrate presence at a relatively low gas production rate is much greater than that at a relatively higher production rate; the bottom hole pressure is affected little by hydrate phase transition, and it is allowable not to consider hydrate phase transition when the bottom hole pressure is calculated; shut-in casing pressure cann't truly reflect gas kick due to hydrate formation and the situation is getting worse with time

模拟计算结果表明:溢流期间,天然气水合物的生成区域会随着循环流量的增大或抑制剂浓度的提高而减小,可通过增大流量和抑制剂浓度使水合物的生成区域脱离海底,减小防喷器管线被堵塞的危险;水合物的生成使环空中气体体积分数降低,泥浆池增量减小,给溢流检测带来延迟;当检测到有气侵发生时,水合物藏分解速率比较小时,井筒中生成水合物的可能性要比分解速率大的情况下更为严重;水合物相变对井底压力的影响较小,在工程中计算井底压力时可以忽略;由于天然气水合物的生成使得关井套压值不能真实反应气侵情况,而且随着时间的增加情况会更加严重。

In 1996, the second session of the Authority (see ISBA/C/11), the Council requested the Secretary-General to refer to the International Seabed ...

在1996 年管理局第二届会议上(见ISBA/C/11),理事会请秘书长参考国际海底管理。。。

The different grains of the deposited materials are basically parallel to the isobaths, sand lower than–3m isobath and silty clay deeper than–3m isobath.

2数值模型要定量预测海湾填海工程可能引起的海底冲淤影响,建立数学模型是最有效的方法。

The conception of crustal isostasy produces a great effect to the geo-scientific research; especially take an important role in the studies of Geodesy and Geodynamics.

地壳均衡的概念对地学的研究有着极大的影响,特别是在大地测量学和地球动力学中发挥了重要作用。均衡重力大地水准面异常作为研究海底地形、地壳结构、构造及地震活动的重要手段,已被科学家广泛应用。

" Hong"…… is along with Qingdao for boat for Qingdao for big ringing, beauty resembling the on the water sailing ascending the big storm sink intoing the bottom of sea, satisfiedly through vicissitudes of life of a voice, change intoed the underwater city, a short moment, lightning flashes thunder the ming , storm rise everywhere, shot of dashing and crashing wave row coast, drown a door door house, blew to turn over the tower of a, peopled to painfully sad to want the desperate, thoroughly despair, in these persons, the husband and wife two depend on each other for life, wife yang jeremiad of day

" 哄"……随着一声声巨响,美丽的青岛就像在海上航行的小船遇上了大风暴沉入了海底,饱经沧桑的青岛,变为了水下城市,霎时间,电闪雷鸣,风暴四起,汹涌澎湃的海浪排击着海岸,淹没了一户户家,吹翻了一座座塔,人们悲痛欲绝,彻底绝望了,在这些人中,夫妻俩相依为命,妻子仰天悲叹

What if you're wrong about the Great Juju at the bottom of the sea?

你为什么不问问你自己:对于海底下的伟大祖祖,如果你也错了来?

Kelp grows only on rocky seafloor and only as deep as the sun's rays penetrate.

海带的增长不仅要有对岩石的海底,只有深太阳的射线穿透。

A theoretical analysis shows that the non-zonation of ACC in the region of Kerguelen Plateau is due to the changes in potential vorticity of the water column caused by the curl of the ratio of wind stress to topography. The bifurcation and turning of ACC is related to the curl distribution.

理论分析表明,凯尔盖朗海台区ACC的非纬向性主要是由风应力和海底地形的变化造成的,它通过该海台时的南北路径的分叉和转向与该海区风应力与水深之比的旋度的分布相吻合。

Once the surplus electricity on the island, but also through the 110 kilovolt submarine cable power transmission line and network to the mainland to be out.

岛上电力一旦过剩,又可通过海底电缆110千伏输变电线路,并网向大陆需出。

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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.

最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。

Only person height weeds and the fierce looks stone idles were there.

只有半人深的荒草和龇牙咧嘴的神像。

This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.

这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。