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帯水層

6 件の記事

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天水（メテオリックウォーター）とは？地下水の起源と種類を解説

天水メテオリックウォーター地下水水文サイクル
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Schematic of an aquifer showing confined zones, groundwater travel times, a spring and a well

帯水層の仕組みと地下水の重要性地球を支える見えない水資源

帯水層地下水水文地質学不透水層
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The preservation and cementation of aeolian dune stratigraphy in Burns Cliff in Endurance Crater are thought to have been controlled by the flow of shallow groundwater.[1]

火星の地下水システム古代の湖から現代の液体水まで

火星地下水インサイト液体水
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Topographic map – volcanic peaks in white due to great height. Near the equator, three volcanoes point south to Phaethontis quadrangle and three large craters – an area containing many gullies.

火星のガリー液状水の痕跡と形成メカニズムの謎

火星ガリー液状水帯水層
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An illustration showing groundwater in aquifers (in blue) (1, 5 and 6) below the water table (4), and three different wells (7, 8 and 9) dug to reach it.

地下水地球を支える不可視の水資源とその危機

地下水帯水層水資源地下水位
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On an average day, nearly 303 million US gallons (1,150,000 m3) of water flow from Big Spring in Missouri at a rate of 469 cubic feet per second (13.3 m3/s).

湧水（泉）の仕組みと多様な種類地球が育む天然の水源

湧水泉地下水帯水層
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