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1 ed and finally stabilized by an intracameral gas bubble.
2 between the anterior inferior retina and the gas bubble.
3 of systemic intravascular and extravascular gas bubbles.
4 he study of the pathophysiological aspect of gas bubbles.
5 terfaces and form protective coatings around gas bubbles.
6 face is less prone to blockage by any formed gas bubbles.
7 ts that are suspended together with numerous gas bubbles.
8 spreading of the minority liquid around the gas bubbles.
9 not higher than 2.5 V to avoid generation of gas bubbles.
11 that the relationship between an intraocular gas bubble and contact with the retina has been evaluate
15 positioning gives better contact between the gas bubble and the inferior and anterior retina than pro
16 urvey what is known about the interaction of gas bubbles and electrode surfaces and the influence of
17 ine monomers across the interface and retain gas bubbles and heat of the reaction in the interfacial
20 efforts to model the behavior of individual gas bubbles and multiphase flows produced at gas-evolvin
22 ion of various thickness of zones denuded in gas bubbles and precipitates, and their relation to the
23 , confirming that the optical method detects gas bubbles and provides insights into the air-seeding h
24 veal contrasting interaction between growing gas bubbles and the crystal framework in crystal-rich ma
26 blocking of the catalyst surface by evolved gas bubbles, and (iii) detachment of the catalyst from t
27 lar disorder superimposed and exacerbated by gas bubbles, and clearly differ from acute systemic gas
28 The effects of undissolved quartz particles, gas bubbles, and compositional inhomogeneity on the melt
29 he buoyant jet of petroleum liquid droplets, gas bubbles, and entrained seawater, using 279 simulated
30 que bubble layer, epithelial breakthrough of gas bubbles, and gas bubbles within the anterior chamber
31 ack between decompression rate, retention of gas bubbles, and integrity of the crystal framework lead
32 gen gas formation, entrapment and release of gas bubbles, and secondary mineral precipitation have be
33 ge transport capability, easy release oxygen gas bubbles, and strong structural stability, which are
36 g liquids (aqueous assay solution, oil), the gas bubbles are clearly visible from the top, when the a
40 lipid and polymer-stabilized perfluorocarbon gas bubbles before and after their destruction with high
41 locities are consistent with the presence of gas bubbles beneath the water table under valley and rid
42 s of simulated petroleum liquid droplets and gas bubbles by 3.2-fold and 3.4-fold, respectively, whic
43 demonstrate that these interactions enhance gas bubble detachment and displacement through magnetic
44 yancy in microgravity, resulting in hindered gas bubble detachment from electrodes and diminished ele
47 d can only be attributed to the existence of gas bubbles due to the strong compressibility dependence
48 ificantly advantageous in producing a single gas bubble during shallow as well as during deep injecti
51 e negative impacts such as Joule heating and gas bubble evolution from common nanosecond pulse treatm
52 R may reach a critical point at which oxygen gas bubbles fill the pores of the ACL and PTL, completel
55 to physiological changes that contribute to gas bubble formation and growth that could lead to anima
58 was seen to modify the plasma properties and gas bubble formation dynamics, significantly influencing
59 ar followed by rapid decompression may cause gas bubble formation within the blood stream (embolism)
60 live oil droplets within 14.5 min, prior to gas bubble formation, during the experiments of Pesch et
64 , to efficiently detect and classify fission gas bubbles from scanning electron microscopic images.
67 vel adaptation of cryo-EM based on detecting gas bubbles generated by radiation damage was used to lo
70 ide liquid droplets by surface attachment to gas bubbles has been suggested as a mechanism to overcom
71 cept for the lowest irradiation temperature, gas bubbles have the shape of thin hexagonal prisms with
72 ose to a liquid-vapor interface of a captive gas bubble in a microchannel, interphase mass-transfer t
76 ique parameters on the formation of multiple gas bubbles in a porcine eye model for pneumatic retinop
78 achieve a supersaturated state and can form gas bubbles in blood and tissues, with resulting tissue
79 servation of the nucleation and migration of gas bubbles in iron (hydr)oxide using transmission elect
84 ortant in reducing the formation of multiple gas bubbles in the eye were shallow depth of injection a
85 crofluidic generation of highly monodisperse gas bubbles in the liquid reaction medium and subsequent
89 ater interface, stabilizing micrometer-sized gas bubbles in water, and disassemble by tuning of the a
94 of the overall evolution behavior of fission gas bubbles is well known, lacking the quantitative data
95 fragmentation of magma, containing abundant gas bubbles, is thought to be the defining characteristi
96 ulness of this first fish model to study the gas-bubbles lesions associated to DCS from a pathologica
97 as-filled cysts, tentatively interpreted as "gas-bubble" lesions in various other cetacean species.
98 cal reactions, the formation and collapse of gas bubbles, merger of fluid droplets, and release of hy
99 an association between swelling due to inert gas bubble nucleation and growth and radiation-induced s
100 Our results suggest that the size of stable gas bubble nuclei depends only on the local concentratio
101 clear fission reactions tend to form fission gas bubbles of various shapes and sizes inside nuclear f
102 1.6%) were located outside the limits of the gas bubble on the first or third day postoperatively.
103 ible reasoning for the abundant formation of gas bubbles on intermetallic precipitates, observation o
105 investigate the mechanisms of nucleation of gas bubbles on nanoelectrodes, and characterize their st
106 onic thickening and several focal intramural gas bubbles (pneumatosis intestinalis) surrounding the p
107 h/kg COD, reduced foam formation due to less gas bubble production, minimum scale formation, and lowe
108 e model scenarios suggest that 5 mm diameter gas bubbles released at a <470 m water depth can transpo
109 from the sediment into the water column via gas bubbles released from the seabed was documented.
111 draulic pathways in some plants, as residual gas bubbles should expand when vessels are reconnected t
112 ed system was distinctly more robust against gas bubbles, showed a higher signal gain, and allowed us
114 uires a combination of fast gas release from gas bubbles (slugs) at the top of the magma conduit and
116 ful in determining size and structure of the gas bubble superlattice as a function of irradiation con
117 with our recent theoretical predictions for gas bubble superlattice formation and highlight that sup
118 pacings similar to those observable when the gas bubble superlattice has formed with very large order
120 ers on the formation and structure of helium gas bubble superlattices within a tungsten host matrix t
122 ve quantities of macroscopic and microscopic gas bubbles, systemically distributed, circulating throu
124 egative pressure without constantly creating gas bubbles that would disable their hydraulic systems.
128 nced ultrasound (CEUS) uses shell-stabilized gas bubbles to provide acoustic backscatter in vasculatu
129 cts during metamorphosis, including impaired gas bubble translocation, head eversion, leg elongation,
132 etermination of the size and symmetry of the gas bubbles was performed using a combination of small a
133 due to the formation of frequent embolisms (gas bubbles), which could be removed by the occurrence o
134 s such as misoriented subdomains and trapped gas bubbles, which are stabilized by molecular-scale str
135 ostructural modification is the formation of gas bubbles, which is revealed at all studied irradiatio
137 ing summer to -68.5 per mil during winter in gas bubbles with an average methane content of 95%.
138 model has the capability to identify fission gas bubbles with and without lanthanides to better under