「porosity」の共起表現一覧(1語右で並び替え)
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Some types, depending on their grade of | porosity, also remove certain microscopic fungi and pa |
nts 1 and 2, this overpressure helps preserve | porosity and enables the chalk to be an effective rese |
are similar but with differing permeability, | porosity and wetting properties. |
ain water and nutrients while still providing | porosity and free drainage. |
h performance polymer frameworks with regular | porosity and high surface area is based on triazine ma |
This depends on the | porosity and flatness of the surface and the rim of th |
ε is the void fraction of the bed(Bed | porosity at any time). |
gelfiltration resins, with varying degrees of | porosity; bead sizes fall in discrete ranges between 2 |
This calculates to a | porosity between 0.43 and 0.36. |
Specific yield can be close to effective | porosity, but there are several subtle things which ma |
Increases in | porosity can increase light refraction, diffuse reflec |
mineral associations, mineral liberation and | porosity can be characterised. |
The | porosity can be controlled in order to produce high fl |
ized by ultra-low permeability but has a high | porosity compared to other shales. |
These attempts show that the use of a neutron | porosity device which has a DOI similar to that of the |
φ is | porosity, dimensionless |
s empirical quantitative relationship between | porosity, electrical conductivity, and brine saturatio |
A popular method of obtaining a formation | porosity estimate is based on the simultaneous use of |
Under normal logging conditions, the | porosity estimates obtained from these tools agree, wh |
Recent attempts at obtaining better | porosity estimates under these conditions have been re |
neficially, there is little or no cracking or | porosity formation. |
flattened hot, relatively low viscosity, high | porosity fragments of volcanic glass or pumice. |
ult to accurately estimate the true formation | porosity from these two curves. |
Notice how far to the left the | porosity goes where all the sand (in yellow) is. |
Waismann's concept of open texture, or | porosity, has been very influential in legal philosoph |
The | porosity has to consist of at least two or a continuum |
Many relationships between travel time and | porosity have been proposed, the most commonly accepte |
ctional melting (e.g., constant intergranular | porosity in the rock during melting and/or reactive po |
more accurate estimate of the true formation | porosity, in the presence of gas, particularly in form |
Finally, | porosity, in most cases surface area, is measured by a |
titatively, the sonic log is used to evaluate | porosity in liquid filled pores. |
The | porosity in (Figure 1) is represented by the blue line |
The | porosity in powder metal parts becomes a liability whe |
pper is drawn up by capillary action into the | porosity, increasing the conductivity of the component |
Porosity is not a direct or physical measurement of th | |
This | porosity is generally localized to the deepest cross-s |
Porosity is typically 95%, but can be as high as 98%. | |
The liquid monomer within the | porosity is polymerized into a solid to seal the passa |
The high | porosity is attained by a highly interconnected void c |
ause of its low specific gravity and its high | porosity it may float upon water, hence its German nam |
where φ0 is the surface | porosity, k is the compaction coefficient (m−1) and z |
Under these conditions, the true formation | porosity lies between the measured neutron and density |
ad of water or oil in the pore space, the two | porosity logs separate, to form what is referred to as |
Finally, and crucially, their | porosity means that they can be infiltrated by materia |
c gravity varies from 0.988 to 1.279, but the | porosity of the mineral may lead to error. |
e a definitive answer to how permeable or the | porosity of the formation that it is logging. |
The | porosity of the ground in the area severely limited th |
Rosalind Franklin worked on | porosity of coal during WWII. |
Porosity of surface soil typically decreases as partic | |
The initial | porosity of a sediment depends on its lithology. |
Open | porosity: Pores are open to each other within the stru |
measurement is affected by secondary phases, | porosity, preferred orientation, exponential distribut |
he particle-to-particle stresses resulting in | porosity reduction primarily through a more efficient |
Porosity sealing, also known as vacuum impregnating, m | |
They differ in their | porosity, specific gravity, optical properties, presen |
Reticulated foams are used where | porosity, surface area, low density are important. |
ling the primer's physical properties such as | porosity, tackiness, and hygroscopy. |
The flux is divided by | porosity to account for the fact that only a fraction |
Such models incorporate interconnected | porosity to facilitate buoyant flow of liquids from lh |
ete is a special type of concrete with a high | porosity used for concrete flatwork applications that |
large error in the determination of the true | porosity using either the density or neutron measureme |
where e is void ratio, φ is | porosity, VV is the volume of void-space (such as flui |
r, if the part is also machined, the internal | porosity will be exposed and the part will leak if pre |
Angrites are basaltic rocks, often having | porosity, with vesicle diameters of up to 2.5 cm. |
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