- flow. In soil,
macropores are
created by
plant roots, soil cracks, soil fauna, and by
aggregation of soil
particles into peds.
Macropores can also be found...
- capillarity. When
water enters the soil, it
displaces air from
interconnected macropores by buoyancy, and
breaks aggregates into
which air is entrapped, a process...
- litter,
stems and
trunks slow down
surface runoff;
their roots create macropores –
large conduits – in the soil that
increase infiltration of water; they...
-
concrete mixing and
shrink when the
matrix hardens,
leave behind macropores.
These macropores operate as weak
matrix sites,
attracting and
encouraging multiple...
- soil is at
field capacity. Typically, at
field capacity, air is in the
macropores, and
water is in the micropores.
Field capacity is the
optimal condition...
-
express the
quantitative interactions between the
three phases of soil.
Macropores or
fractures play a
major role in
infiltration rates in many
soils as...
- 'macroporosity'
refers to
pores greater than 50 nm in diameter. Flow
through macropores is
described by bulk diffusion.
Mesoporosity In
solids (i.e. excluding...
- "Strong and
Ductile Colossal Carbon Tubes with
Walls of
Rectangular Macropores". Phys. Rev. Lett. 101 (14): 145501. Bibcode:2008PhRvL.101n5501P. doi:10...
-
region with no
visible macropores dubbed the
Initial Zone (IZ).
Directly after the IZ is the
Transition Zone (TZ),
where macropores begin to form and align...
- seal
prevent the
disruption and
detachment of soil
aggregates that
cause macropores to block,
infiltration to decline, and
runoff to increase. This significantly...
