— 598 — impermeable layer, Uo is the component of uni<strong>for</strong>m flow towards the sinks, and Q is the combined sink strength, (2): do = D /L , where D is the distance of each sink from the interface, (3): « = l/2rKt/Q, in which Kt is the coefficient of trainsverse dispersion. e1/2 is the characteristic thickness of the mixing layer. It was shown that when the product uodo < 1/2, two distant stagnation points <strong>for</strong>m at the interface, as is sketched in figure 10, and saline water from the upper half of the mixing layer is drawn into the upper sink. The two stagnation points coalesce <strong>for</strong> uodo = 1/2, (figure 10b). If uodo > 1/2, separate stagna-
— 599 — tion points exist above and below the interface, (figure 10c), but each point involves a stagnation stream-line which lies inside the mixing layer. It can be shown that the amount of dissolved salt moving to the upper sink decreases rapidly as uodo is increased beyond the value of 1/2. Thus, it is quite possible to selectively withdraw in the upper sink fresh water only slightly contaminated and of great economical importance. The saline water pumped from the lower sink can of course be discharged somewhere else. January 5, <strong>1973</strong> REFERENCES (1) A n g i n o , E.E.; B i l l i n g s , G .K .: Chem. Geol., 4 ( 1 / 2 ) , 7 -8 ( 1 9 6 9 ) . (2) A r a n o w , R.H.: Phys. Fluids, 9, 172 i-7 (1966). (3a) B e a r , J.; B a c h m a t , Y.: Hydraul. Lab. P.N. 1/65, Technion, Haifa (1965). (3b) B e a r , J.; B a c h m a t , Y.: Hydraul. Lab. P.N. 4/66, Technion, Haifa ( 1 9 6 6 ) . (4) B e a r , J.; D a g a n , G.: J. Geophys. Res., 69, 1563-72 (1964). ( 4 a ) B r e d e h o e f t : BAAPG, 47, 2 5 7 -6 9 ( 1 9 6 3 ) . (5) C v ij a n o v ic h , B.G.: Travaux de l’institut de Rech. Sah., IX, 131-6 (Algiers) (1953). (6) D a g a n , G .; B e a r , J.: J. Hydraul. Res., 6, 15-44 (1968). (7) De J o s s e l in d e J o n g .: Trans. Amer. Geophys. Union, 39, 67-74 (1958). (8) G e l h a r , T.W .; C o l l i n s , M.A.; L i, F.: M.I.T. Hydrodynamics Lab. Rep. (1970). ( 9 ) G o r h a m , E.: Bull. Geol. Soc. Amer., 72, 7 9 5 -8 4 0 ( 1 9 6 1 ) . (10) H a s im o t o , H .: J. Fluid Mech., 5, 317-28 (1959). (11) H o lm e s , J.W.: in Symposium on Salinity and Water Use, Canberra, A.C.T. London MacMillan (1971). (12) I.U.C.N.: Septième Réunion Technique, Athènes (1958). (13) J a c o b s e n , T.; A d a m s , R.M.: Science, 128, 1251-58 (1958). (14) Jain, J.K.: U.N.E.S.C.O. Arid Zone Res. 14, 11-16 (1961). (15) K u N iN , V.N.: in Symposium on Water Resources, Use and Management, Canberra, A.C.T., Melbourne Univ. Press, 212-8 (1964). (16) L is t , E.J.: J. Fluid Mech., 33, 529-43 (1968). (17) L is t , E.J.: ƒ. Fluid Mech., 36, 17-19 (1969). (18) L is t , E.J.; B r o o k s, N.H.: J. Geophys. Res., 72, 2531-41 (1967). (19) L u s c z y n s k i, N.J.: J. Geophys. Res., 66, N° 12, 4247-56 (I960). (20) M il l e r , E.E.; M il l e r , R.D.: ƒ. Appl. Phys., 27, 324-32 (1956). ( 2 1 ) O ’B r i e n , V.: A.P.S. Division of Fluid Dynamic, Annual Meeting ( 1 9 7 1 ) . ( 2 2 ) P o l u b a r i n o v a - K o c h i n a , P.Y.: Theory of Groundwater Movement. Princeton Univ. Press ( 1 9 6 2 ) . ( 2 3 ) P o r c h , M .; E l a t a , C.: Israel ]. Techn., 4, 2 1 4 -7 ( 1 9 6 6 ) . (24) P r a g e r , S .: Phys. Fluids, 4, 1477-82 (1961). (25) R ib l e , J.M.; D a v is, L.E.: Soil Sei., 79, 41-47 (1955). (26a) S a f f m a n . P.G.: J. Fluid Mech., 6, 321 (1959). ( 2 6 b ) Sa f f m a n , P .G .: J. Fluid Mech., 7, 1 9 4 -2 0 8 ( I 9 6 0 ) .
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ACADÉMIE ROYALE DES SCIENCES DOUTR
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CLASSE DES SCIENCES MORALES ET POLI
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Zitting van 15 mei 1973 De zitting
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— 423 — Geheim comité De ere-
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— 431 — dans la correspondance
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— 437 — ANNEXES 1. C o r r e s
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— 439 — être I décidé et je
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— 441 — 13-X-1902: LAURENT M.D.
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Jean Puissant. — Quelques témoig
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— 445 — ge forcent de nombreux
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— 447 — ligne directe postale e
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— 449 — antipodes de la Belgiqu
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— 451 — aller de notre logement
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5. Une lettre d’émigré — 455
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— 461 — (2) D h o n d t , J.:
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— 465 — Sa m e n v a t t in g D
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— 469 — dienste hebben een toev
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— 471 — in sommige N.G.O.-kring
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J.-P. Harroy. — Présentation du
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Séance du 19 juin 1973 Zitting van
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Zitting van 19 juni 1973 De zitting
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— 481 — « L’organisation de
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— 483 — belgo-congolaise à la
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— 485 — les couches plus ancien
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P.C.C. Garnham. — History of the
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J.-B. Jadin *, E. Willaert * et J.
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D iscussion — 524 — N o u s v o
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Séance du 26 juin 1973 M. F. Jurio
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M. Van Himme *. — Le problème du
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— 540 — indigène en Australie,
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