在同一温度下，单组分体系T—S图上各等压线随熵值的增大，压力将（）A.增大 B.减小

一列简谐横渡沿x轴正方向传播，在t=0的时刻，波恰好传到x=2m处，波形如图所示波速v=5m/s，质点P平衡位置的坐标为（9，o），则（　　）

A．形成该波的波源起振方向沿y轴正方向

B．该波频率为0.4Hz

C．t=1.8s时，质点P开始振动

D．t=1.7s时，质点P第一次到达波峰

下列属于商业银行固定资产贷前调查报告内容要求的是（）。

A．借款人资信情况

B．投资估算与资金筹措安排情况

C．项目可研报告批复及其主要内容

D．银行从项目获得的受益预测

E．项目效益情况

创作素材

继19世纪的报刊和20世纪的广播、电视之后，1993年因特网开始向公众开放，1998年5月联合国新闻委员会正式提出“第四媒体”的概念。在我国，去年年底网民达210万，除传统媒体如《人民日报》等纷纷上网办电子版外，新浪网、CHINABYTE等网站的新闻味越来越足，第四媒体正在崛起。专家预言，10年到20年内第四媒体的影响力将可能超过传统媒体。理由是，广播问世38年拥有5000万听众，电视则用了13年，因特网只用了4年。
因特网作为一种媒体，优势十分明显：跨越时空，全球一网，信息无限，时效更快；文、图、动画、声音等多种媒体合为一体；每个人可选择自己所需要的内容，发表意见，每一个新闻机构甚至个人都可以随时向全世界发布新闻。对于下个世纪的第四媒体，有的专家这样描述——这是一张个性化的报纸，它是一个带超薄型大平面显示版的移动式网络计算机，不仅有图文声情，甚至扩展到三维空间，它以我为中心，按照受众的需要进行信息项目自主选择、组织。有的专家称之为“我的报纸”。
现在，第四媒体还只是一个小弟弟。即使在美国它也还不能提供比印刷版更多、更快的东西。多数公司只因为这是一个潮流才不得不坚持，一些小报已经停办了电子版。调查表明，关于克林顿绯闻的“司塔尔报告”，只有22%的人是在网上了解到的。这说明因特网在现在的传播中并不占较大比例。有的专家认为，网络媒体现在所能做到的是为传统媒体争取远距离受众，提供交互式服务，满足共性前提下的个性要求。有的专家则认为第四媒体首先要做的，是为争取到生存所需关键数目的受众而努力。

提出的“第四媒体”的概念，指的是：

A．多媒体
B．网络计算机
C．“我的报纸”
D．网上报纸

The Theory of Continental Drift has had a long and turbulent history since it was first proposed by Alfred Wegener in 1910. (46) Vigorously challenged yet widely ignored, the theory had languished for half a century, primarily due to its lack of a plausible mechanism to support the proposed drift. With the discovery of sea-floor spreading in the late 1950’s and early 60’s, the idea was reinvigorated. Plate tectonics is now almost universally accepted. Many details of the mechanism are to be worked out.

The surface of the Earth is divided into approximately six large plates, plus a number of smaller ones. The plates are’ bounded by an interconnected network of ridges, transform faults, and trenches. Ridges, also called spreading centers, occur where two plates are moving away from each Other. As the plates separate, hot molten mantle material flows up to fill the void. (47) The increased heat resulting from this flow reduces the density of the plates, causing them to float higher, thus elevating the boundaries by many thousands of feet above the colder surrounding sea floor. (48) Ridges on the ocean floor form the longest continuous ranges of mountains on the planet, but. only in a very few places on the Earth do these mountains rise above the ocean surface.

New sea floor is constantly being created along spreading centers. Obviously somewhere else old sea floor must be going away. This occurs in trenches, also called subduction zones. Trenches occur along the boundary between two plates that are moving towards each other. (49) Where this occurs, one plate is bent downwards at about a 400 angle and plunges under the other plate’s leading edge, eventually to melt back into the liquid mantle below. As the subducting plate is heated back up to mantle temperatures, certain minerals in the plate melt sooner than others. (50) Minerals that melt at lower temperatures and are lighter than the surrounding material tend to rise, melting their way up through the overriding plate to erupt as volcanoes on the ocean floor. As these volcanoes grow, they rise above the ocean surface to form lines of islands along the leading edge of the overriding plate. Numerous islands of Micronesia and Melanesia in the western Pacific were created in this way.

(50) Minerals that melt at lower temperatures and are lighter than the surrounding material tend to rise, melting their way up through the overriding plate to erupt as volcanoes on the ocean floor.