By J.W. HOLMES and T. TALSMA (Eds.)
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2 factors affecting in finite saturated-unsat- paper. 1 Combined C o n v e c t i v e - D i f f u s i o n Transport I n d e a l i n g w i t h the simultaneous t r a n s f e r of s o l u t e and w a t e r , one u s u a l l y assumes t h a t t h e t r a n s p o r t of the s o i l The solution) of s o l u t e i s governed by c o n v e c t i o n ( v i s c o u s movement and d i f f u s i o n (thermal motion w i t h i n the s o i l d i f f u s i o n process i s d e s c r i b e d by F i c k ' s l a w .
Not much i n f o r m a t i o n of t h i s kind about e u c a l y p t u s f o r e s t s in A u s t r a l i a . W i l l i a m s and Coventry (1979) r e p o r t e d t h a t they had observed SWD to be in the range 220 to 110 mm in the r o o t zones of an open woodland community in northern Queensland, which was made up of y e l l o w j a c k {Eucalyptus similis), bloodwood ( E . dichromophloia), i r o n bark s p e c i e s (E. whitei and E. orebra) t o g e t h e r w i t h a c a c i a s and o t h e r n o n - e u c a l y p t s .
Comparison of recharge to groundwater under p a s t u r e and f o r e s t using environmental t r i t i u m . J . H y d r o l . , 1 7 : 81-96. A s t o n , A . R . , 1979. R a i n f a l l i n t e r c e p t i o n by e i g h t small t r e e s . J . H y d r o l . , 4 2 : 383-96. Bethlahmy, N . , 1974. More streamflow a f t e r a bark b e e t l e e p i d e m i c . J . , 23: 185-89. Bowen, I . S . , 1926. The r a t i o of heat l o s s e s by conduction and by e v a p o r a t i o n from any w a t e r s u r f a c e .
