Tables of Physical and Chemical Constants

Kaye, G. W. C.; Laby, T. H.

doi:10.1259/jrs.1921.0043

Cited by 120 publications

(154 citation statements)

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“…2A,B) (Czabany et al 2008;Cheng et al 2009). A similar segregation may also occur among TGs because they have vastly different melting temperatures depending on fattyacid composition (Kaye et al 1995). Concentric lines observed by cryoelectron microscopy ( Fig.…”

Section: Structure Of Lipid Dropletsmentioning

confidence: 70%

Not Just Fat: The Structure and Function of the Lipid Droplet

Fujimoto

Parton²

2011

Cold Spring Harbor Perspectives in Biology

408

336

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Lipid droplets (LDs) are independent organelles that are composed of a lipid ester core and a surface phospholipid monolayer. Recent studies have revealed many new proteins, functions, and phenomena associated with LDs. In addition, a number of diseases related to LDs are beginning to be understood at the molecular level. It is now clear that LDs are not an inert store of excess lipids but are dynamically engaged in various cellular functions, some of which are not directly related to lipid metabolism. Compared to conventional membrane organelles, there are still many uncertainties concerning the molecular architecture of LDs and how each function is placed in a structural context. Recent findings and remaining questions are discussed.

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Section: Structure Of Lipid Dropletsmentioning

confidence: 70%

Not Just Fat: The Structure and Function of the Lipid Droplet

Fujimoto

Parton²

2011

Cold Spring Harbor Perspectives in Biology

408

336

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“…Medically pure oxygen was obtained from the same sources, and oxygensaturated solutions were prepared by bubbling the gas through the appropriate buffer solution at room temperature (20'C) and atmospheric pressure for 10-1Smin. The concentrations of oxygen-saturated solutions were found by reference to the appropriate published Tables (Kaye & Laby, 1966). Solutions of oxygen, less than saturated, were prepared by serial dilution of the saturated stock by using buffer equilibrated with O2-free N2.…”

Section: Methodsmentioning

confidence: 99%

The reaction of Pseudomonas aeruginosa cytochrome c-551 oxidase with oxygen

Greenwood¹,

Barber²,

Parr³

et al. 1978

Biochemical Journal

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The reaction of ascorbate-reduced Pseudomonas cytochrome oxidase with oxygen was studied by using stopped-flow techniques at pH 7.0 and 25°C. The observed time courses were complex, the reaction consisting of three phases. Of these, only the fastest process, with a second-order rate constant of 3.3 x 104 M-1 S-s, was dependent on oxygen concentration. The two slower processes were first-order reactions with rates of 1.0 ± 0.4s-' and 0.1 ±0.03s-'. A kinetic titration experiment revealed that the enzyme had a relatively low affinity constant for oxygen, approx. 1 0 M-1. Kinetic difference spectra were determined for all three reaction phases, showing each to have different characteristics. The fast-phase difference spectrum showed that changes occurred at both the haem c and haem di components of the enzyme during this process. These changes were consistent with the haem c becoming oxidized, but with the haem d1 assuming a form that did not correspond to the normal oxidized state, a situation that was not restored even after the second kinetic phase, which reflected further changes in the haem d1 component. The results are discussed in terms of a kinetic scheme.

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“…12.5 m below the seafloor of the sediment core at Station MD179-3296, indicating the existence of gas hydrate that dissociated during the recovery (Kakuwa et al 2013a). No indication of the existence of gas hydrate Johnson and Olhoeft (1984) b Horai (1971) c Drury et al (1984) d Brigaud and Vasseur (1989) e Skauge et al (1983) f Drury (1987) g Robie and Hemingway (1995) h Kaye and Laby (1995) i Calculated from other properties was observed in the sediment core recovered at Station MD179-3304. Sediment cores with no indication of gas hydrate were recovered at Stations MD179-3299 and MD179-3301 on the eastern flank of the Umitaka Spur.…”

Section: Measurements Sediment Core Samples Recovered In the Joetsu Bmentioning

confidence: 98%

Physical and thermal properties of mud-dominant sediment from the Joetsu Basin in the eastern margin of the Japan Sea

et al. 2017

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on the sediment mineral composition. Conversely, the grain heat capacity and grain specific heat showed hardly any dependency on the mineral composition. We propose empirical formulae for the relationships between: thermal diffusivity and thermal conductivity, and heat capacity and thermal conductivity for the sediment in the Joetsu Basin. These relationships are different from those for mud-dominant sediment in the eastern flank of the Juan de Fuca Ridge presented in previous work, suggesting a difference in mineral composition, probably mainly in the amount of quartz, between the sediments in that area and the Joetsu Basin. Similar studies in several areas of sediments with various mineral compositions would enhance knowledge of the influence of mineral composition.

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Tables of Physical and Chemical Constants

Cited by 120 publications

References 0 publications

Not Just Fat: The Structure and Function of the Lipid Droplet

Not Just Fat: The Structure and Function of the Lipid Droplet

The reaction of Pseudomonas aeruginosa cytochrome c-551 oxidase with oxygen

Physical and thermal properties of mud-dominant sediment from the Joetsu Basin in the eastern margin of the Japan Sea

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