Central Valley Aquifer, Chapters A and B - MAE Class Websites

2
displayed in
is found.
2
(full 2
1
and the pressure head at the bottom of
2 1
is not found
1
but by the pressure
1
the uptake from saturated conditions is formulated as
Tgw−act−sat ( h)= Tc−pot i( ASRZ1( h) + ASRZ 2( h) i
( h)) / TRZ (3)
( )= ( ( ) + ( )+
ASRZ 2( h) i
( h)) / TRZ
T h T i AURZ h ASRZ1 h
gw−act c− pot
and
1 2 1
2
depend on the simulated
ASRZ 2( h) i ( h)
-
k k
gw−act ( )= c− pot ( ( )+ ( )+
k
T h T i AURZ h ASRZ1 h
( ) ( ))
k k−1
ASRZ 2 h i
h / TRZ
can
be split into non-head-dependent and head-dependent terms.
, is separated into terms either dependent
or not dependent on the head of the current iteration. While
(4)
(5)
The Farm Process (FMP1) 219
made here.
possible transpiration.
transpiration components. These components are fed either by
-
,
-
possible transpiration may be supplemented by precipitation
,
-
stress response,
1 2
1 2 ) may
response,
2 is found
2
1 2