By J.W. HOLMES and T. TALSMA (Eds.)
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V) I I - q c ] (17) To s o l v e equation ( 1 7 ) , the v a l u e s o f D ^ ( z , t ) With e ( z , t ) a l r e a d y known from s o l u t i o n v a l u e of D ( z , t ) for one-dimensional For zero v a l u e s of Q and S ^[60(6 h(z,t), soils. equation f o r t r a n s i e n t by equation ( 3 ) . : c o n t e n t , and w a t e r f l u x as a f u n c t i o n are obtained. it These a r e t h e predetermined w a t e r p r e s s u r e p r o f i l e domain, 0 < ζ < Ζ n and q ( z , t ) (15f) to the s u r f a c e and bottom boundary c o n d i t i o n s , specify i n i t i a l h (z) =0 and D ( z , t ) must a l s o be known.
2 concentrDiffuse ( B r e s l e r , 1970) was used t o o b t a i n s a l t e x c l u s i o n data w i t h d i v i d e d by t h e s p e c i f i c s u r f a c e a r e a o f t h e s o i l . findings solution. of ) F i g . 3 . H y d r a u l i c c o n d u c t i v i t y ( K ) as a f u n c t i o n of v o l u m e t r i c w a t e r c o n t e n t ( θ ) and s o l u t i o n c o n c e n t r a t i o n ( C ) f o r seven c a t i o n i c r a t i o s [ R = N a / ( C a ) * ] . 0 has been s h i f t e d f o r s u c c e s s i v e s e t s of c u r v e s , as i n d i c a t e d by t h e arrows along t h e a b s c i s s a .
S . , 1968. On the w a t e r b a l a n c e of g r a s s l a n d and forest. T r a n s . 9th Congr. I n t . S o i l S c i . S o c , A d e l a i d e , 1 : 39-46. Holmes, J . W . and C o l v i l l e , J . S . , 1970a. G r a s s l a n d hydrology i n a k a r s t i c r e g i o n of southern A u s t r a l i a . J . H y d r o l . , 10: 38-58. Holmes, J . W . and C o l v i l l e , J . S . , 1970b. F o r e s t hydrology i n a k a r s t i c region of southern A u s t r a l i a . J . H y d r o l . , 10: 59-74.