「Pore」の共起表現(1語右で並び替え) - Weblio英語共起表現検索

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共起表現

「Pore」の共起表現一覧(1語右で並び替え)

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uble, and the oviducts open by a median ventral	pore about the middle of the body; in this region th
s are identifiably pseudophyllid as the genital	pore and uterine pore are located on the mid-ventral
The α subunit forms the ion conduction	pore and the β subunit contributes to channel gating
Its interior is close-packed with no central	pore and contains both hydrophobic residues and char
ppermost permafrost layers and mainly comprises	pore and segregated ice in Earth material.
e Soccer in 2011, along with Steve Cronin, Ryan	Pore and Eddie Johnson.
ervated, and sensory endings around the genital	pore are more plentiful than other areas.
Richard Le	Pore as Staff Sergeant Kemler, boom operator on KC-1
s well as magnesium ions, that plug the channel	pore at positive potentials, resulting in a decrease
lin D is thought to regulate the opening of the	pore because cyclosporin A (CsA), which binds to CyP
decreases over subsequent cycles as a result of	pore blockages and damage to adsorption sites by the
Most likely, apamin acts as a	pore blocker, although residues both inside and outs
ng nucleoporins and is localized to the nuclear	pore central plug.
Main article: Nuclear	pore complex
eoporins are the main components of the nuclear	pore complex in eukaryotic cells.
PIC1/SUMO-1, which are associated with nuclear	pore complex also associate with nuclear dots.
eads to its trafficking from cytosol to nuclear	pore complex .
The nuclear	pore complex is a massive structure that extends acr
Aladin is a component of the nuclear	pore complex.
ocation of RNA and proteins through the nuclear	pore complex.
er eukaryotic proteins that make up the nuclear	pore complex.
portin heterodimer-bound protein to the nuclear	pore complex.
The nuclear	pore complexes are embedded in the nuclear lamina.
The presence of several million	pore complexes in the oocyte nuclear membrane and th
is depleted p62 fails to assemble with nuclear	pore complexes.
he cytosol into the nucleus through the nuclear	pore complexes.
hibit different functional properties including	pore conductance, size selectivity, charge selectivi
S is introduced, in cement mixtures control air	pore content and prevent agglomeration of powders du
The somatal	pore controls the diffusion of CO2 into the leaves t
d is the average, or effective	pore diameter [length].
brane can also be classified according to their	pore diameter.
The resultant size of the	pore directly affects what molecules are able to pas
A K+ channel	pore domain (S5, selectivity filter, and S6).
Inward rectifiers also differ from tandem	pore domain potassium channels, which are largely re
and c) that form part of the proton-conducting	pore, each containing a buried glutamic acid residue
Basins with different	pore fluid chemistry will have differing hydrostatic
rals at grain-to-grain contacts into an aqueous	pore fluid in areas of relatively high stress and ei
urce rock are first expelled , along with other	pore fluids, due to the effects of internal source r
nds to gp41 preventing the creation of an entry	pore for the capsid of the virus, keeping it out of
ently, however, researchers found evidence that	pore formation is not necessarily linked to cell dea
(IPR005639) involved in membrane insertion and	pore formation; a beta-sheet central domain involved
s aureus and the first identified member of the	pore forming beta-barrel toxin family.
nting the mitochondrial permeability transition	pore from opening, thus inhibiting cytochrome c rele
aland Gasteromycetes (puffballs), Polyporaceae (	pore fungi), Thelephoraceae (crust fungi), and Uredi
They are dehiscent through the large basal	pore, green to brownish purple [to magenta], spheric
transmembrane alpha helices, numbered S1-S6, a	pore helix situated between S5 and S6, and cytoplasm
e longest piece is entitled ‘A complaint of the	pore husbandmen in meter.'
al assembly into cyclical hexamers with a small	pore in the center.
tide sequence, which allows for the size of the	pore in the protein to differ between aquaporins.
large and kidney-shaped, reaching form the male	pore in segment X into segment XI.
he conformational change that opens the channel	pore in response to a displacement in membrane poten
first general description of the K+ ion channel	pore, including the fundamental ideas of a selectivi
es are micro-organisms that can live within the	pore interstices of sedimentary and even igneous (if
ne-spanning alpha helixes (M1, M2, M3, M4), the	pore is primarily formed by M2 of the two alpha subu
ding site) compared to where the ion conduction	pore is located.
Inflated in the middle of each	pore, it is quite crispy yet spongy.
he Australian C. nicolli, which has the genital	pore located further to the front.
acellular loop (known as 'the turret') and 'the	pore loop', which begins and ends extracellularly bu
intermediate region of the receptor, within the	pore lumen, valine and leucine residues (Val 255 and
hat activated Bax and/or Bak form an oligomeric	pore, MAC in the outer membrane.
innamon brown, smooth and ellipsoid with a germ	pore, measuring 8 x 5 micrometers.
Aerating water by means of fine	pore membrane diffuser
a protein which is only slightly smaller than a	pore might enter the pore but does not easily leave
The	pore of sodium channels contains a selectivity filte
It induces mitochondrial permeability	pore opening and inhibits respiration by interfering
The	pore opening raises the permeability of the mitochon
These conformational changes could also lead to	pore opening.
to a functional disorder, so the opening of the	pore plays an important role in cell death.
As with all matters relating to	pore pressure analysis, the method cannot be applied
nge in applied stress (effective stress - σe or	pore pressure - p) per unit volume.
y dc-exponent plots by examining multiple other	pore pressure indicators.
y suddenly) becomes less than the formation, or	pore, pressure in a permeable section downhole, and
he dam site, and the possibility that the added	pore pressure of the deeper water could reactivate t
t-range interaction with the negatively charged	pore region of potassium-channels leading to channel
C287Y and G293R are both located in the	pore region of domain 1 and are present in a single
ning segments and a predicted calcium-selective	pore region.
However, research has shown that the MPT	pore remains closed during ischemia, but opens once
Aplysina fulva, a scattered	pore rope sponge
For the mitochondrial	pore, see mitochondrial permeability transition.
by	pore Shakerlaye.
Correctly used, wheel filters with at least	pore size 0.5 µm (e.g.
The nominal	pore size of the membrane is typically about 1 nanom
A typical microfiltration membrane	pore size range is 0.1 to 10 micrometres (µm).
nd only a few inches above the water table when	pore size is large.
	Pore size is controlled by controlling the concentra
pores provide greater surface area while larger	pore size has better kinetics, especially for larger
If	pore size is small and relatively uniform, it is pos
e from 5 to 2,000 kiloDalton due to the uniform	pore size provided by the polyacrylamide gel.
The bag has a characteristic	pore size that allows small particles, like water or
the material which is smaller than the membrane	pore size passes through the membrane as permeate or
ng to IUPAC, there are three different types of	pore size classifications: microporous (dp < 2 nm),
But the variable	pore size of the agarose causes a potential upper si
ple is drawn through a membrane filter (0.45 µm	pore size) through the use of a vacuum pump.
ious factors including membrane sizes, membrane	pore size, temperature, operating pressure and membr
In soils with a wide range in	pore size, the unsaturated zone can be several times
They do not have a uniform	pore size, but are optimal for electrophoresis of pr
illary rise because of the presence of a mix in	pore size.
It indicates the	pore space within the rock structure.
etimes, under the right conditions, some of the	pore space in the rock is occupied by other liquids
is not a direct or physical measurement of the	pore space but rather an extrapolation from other dr
ontains an open framework of particles with the	pore space being usually filled with water.
njected into a bituminous coal bed would occupy	pore space and also adsorb onto the carbon in the co
3.6 trillion cubic feet of gas filled a lot of	pore space in the source rocks - the field was part
ere there is gas instead of water or oil in the	pore space, the two porosity logs separate, to form
The oil and gas resides within this	pore space.
t coloured areas new mineral growth has reduced	pore space.
Above a capillary fringe,	pore spaces have air in them too.
Blue epoxy fills	pore spaces.
lying horizons, forming tiny quartz crystals in	pore spaces.
8 x 7-10 µm, elliptical, smooth, with an apical	pore, spore print black.
either by macromolecular adsorption to internal	pore structure of membrane, or aggregation of protei
As these fruiting bodies age, the	pore surface turns from yellow to greenish yellow, t
r more across with a characteristic pale yellow	pore surface.
ations flow into a more constricted part of the	pore that is 0.3 by 0.5 nm wide, which is just large
osed of five subunits arranged around a central	pore that opens to allow ions to pass through.
ts depends on the chemistry of the water in the	pore, the surrounding mineralogy, and the temperatur
opening, the electrical conductance of the ion	pore, the activation voltage, and the activation dur
e visible and a truncate apex with a broad germ	pore, thick walled, and dingy yellow brown.
in a geologic model incorporate an estimate of	pore throat size, the densities of the fluids, and t
It is a doughnut shaped	pore through the membrane with 3 major subunits (het
nit has 24 transmembrane segments and forms the	pore through which ions pass into the cell.
others of this class, the α1 subunit forms the	pore through which calcium enters the cell and deter
arranged in such a way that there is a central	pore through which ions can travel down their electr
ge-dependent and has four subunits which form a	pore through which ions flow, carrying type-A potass
ntical alpha subunits, which form the channel's	pore through the plasma membrane.
its fit together and form a ring with a central	pore through which cell contents leak and which acts
The dimer was thought to be a gated	pore through which ADP and ATP were exchanged betwee
nit that acts as the channel gate, blocking the	pore until the channel is bound by ligand.
The	pore velocity (v) is related to the Darcy flux (q) b
The	pore velocity would be the velocity a conservative t
channel pore-forming α-subunit by blocking the	pore via a bimolecular reaction.
f its highly porous structure, large accessible	pore volume with fully exposed edges and faces of th
The location of the ionic	pore was identified, made up of the second transmemb
ive theory is that basal till, weakened by high	pore water pressure, deformed upwards into parallel
e top of the salt when the halite is removed by	pore waters.
l the nucleocapsids make their way to a nuclear	pore where the virus genome is released and transloc
ptate and have a pronounced sigmoid germination	pore, which enables their use in paleoecology as a p
altered but simply shift position, opening up a	pore which acts as the conductive pathway through th
	Pore wing ochreous white irrorated with red-brown, t
	Pore wing: narrow subbasal and outer cellular transv

共起表現