地下的水流
网络释义
... a. 地下的,秘密的 a subterranean stream 地下的水流 territory n.领土，版图；领域 ...
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地下水流动的数值模拟 numerical simulation of groundwater flow
双语例句原声例句
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第三天，土地形成，地下的水流上形成干燥地带。
On day three, land is formed to make dry spots from the waters below.
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并且，由于它们是在地下形成的，而不是由地表水流形成，所以并不是所有的通道都有通向外部世界的开口。
And, since they were created underground and not from flowing surface water, not all these passageways have an opening to the outside world.
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在气候特别湿润的年月里，平常干涸的河床下游可能会有水流动，因为地下水在那里位抬升到了地表以上。
In particularly wet years, short stretches of an otherwise dry stream-bed may have flowing water because the water table rises to intersect the land surface.
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On day three, land is formed to make dry spots from the waters below.
第三天，土地形成，地下的水流上形成干燥地带。
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