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polar mud systems.
Osmotic Pressure. When the energy level or activity in shale pore fluid,
a
s
, is different from the
activity
in drilling mud,
a
m
, water movement can occur in either direction across a
semipermeable membrane as a result of the development of osmotic pressure,
p
os
, or chemical
potential,
μ
c
. To prevent or reduce water movement across this semipermeable membrane that
has certain efficiency,
E
m
, the activities need to be equalized or, at least,
their differentials
minimized. If
a
m
is lower than
a
s
, it is suggested to increase
E
m
and vice versa. The mud activity
can be reduced by adding electrolytes that can be brought about through the use of mud systems
such as seawater, saturated-salt/polymer, KCl/NaCl/polymer, and lime/gypsum.
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