Because the quantity of water (Q is

Because the quantity of water (Q is directly proportional to
the hydraulic gradient (dhldl), we say that ground-water flow is
laminar-that is, water particles tend to follow discrete
streamlines and not to mix with particles in adjacent streamlines
(1) . (See "Ground-Water Flow Nets .")

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Because the quantity of water (Q is directly proportional tothe hydraulic gradient (dhldl), we say that ground-water flow islaminar-that is, water particles tend to follow discretestreamlines and not to mix with particles in adjacent streamlines(1) . (See "Ground-Water Flow Nets .")

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Karena kuantitas air (Q berbanding lurus dengan
gradien hidrolik (dhldl), kita mengatakan bahwa aliran air tanah adalah
laminar-yaitu, partikel air cenderung mengikuti diskrit
arus dan tidak mencampur dengan partikel di arus yang berdekatan
(1) . (Lihat "Tanah-Air Arus Nets.")

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