Calcium, from calcite dissolution, contributes to the modification of the cation exchanger population in the clay and to the cation composition of the pore water
The effect and reasonable description of rapid increasing pore water
pressure of saturated rock fill materials on the dynamic deformation and strength properties should be taken into full consideration.
Instruments to measure ground movement and pore water
pressure thread a site in the area of a prehistoric stream channel near the Alamo River.
The conventional view that plant wilting always occurs at a pore water
suction of h = 1.
6A2), referring to early diagenetic origin of cementation, in some cases the dolomite-cemented rocks of the Vadja and Leivu Fms revealed a somewhat increased content of Mn in dolomite, indicating that in these levels cementation of siliciclastic layers presumably progressed during burial diagenesis under the impact of evolved pore waters
It is difficult to estimate the residual effective stresses or negative pore water
pressure which remains within the specimen, since is not easy to specify completely the stress history of the specimen until the specimen is placed into oedometer.
In most practical cases, the horizontal permeability of sand/gravel drains will be several times greater than its vertical permeability and spacing between vertical drains is closer than the distance required for pore water
to drain vertically towards the free surface.
Sediment obtained from deposits probably accounts for the bulk of the gut's content, but food filtered from pore water
may be most important nutritionally (Barrington, 1940).
consideration of crack and pore water
pressure according to the current flow situation.
The decline of pore water
content is most significant at 200-300 [degrees]C.
The similarity between the global climate records and the pore water
records from the Dead Sea core emphasizes a strong relationship between rainfall and humidity in the region and global climate changes, findings that are important for understanding and predicting climate change in Israel and the central Levant, the researchers wrote.
A longer retention time, due to a lower pore-water velocity, leads to a longer contact time, while shorter retention times might occur at higher superficial velocities (velocities of pore water
on the particle surface).