Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Environment Formation

NRCC (1983) Polycyclic aromatic hydrocarbons in the aquatic environment Formation, sources, fate and effects on aquatic biota. NRCC/CNRC, Ottawa, Canada. [Pg.912]

Weiss PS (2008) Functional molecules and assemblies in controlled environments formation and measurements. Acc Chem Res 41(12) 1772-1781... [Pg.36]

Transport of iron in carbonate waters, mainly in the form of Fe " bicarbonate, is more common. The decrease in COj due to the overall reduction in pressure when ground waters come to the surface, when carbon dioxide is consumed as a result of photosynthetic activity of plants or even, as Mokiyevskaya (1959) mentions, when the temperature rises, leads to deposition of FeCOj. In Strakhov s opinion such a process could lead to the formation of oolitic hydrogoethite-chamosite-siderite ores. The iron migrated in mobile form as Fe, which accumulated in solution in a reducing environment. Formation of the ores was related to the draining of high-iron waters formed in swampy regions. The near-shore parts of the sea with... [Pg.142]

Metals are modified by a second element due to the change of either electronic or geometric environment. Formation of stable bimetallic particles or alloys is prerequisite for improved catalytic properties. It seems even more important when metal particles are entrapped inside zeolite cages, like faujasite-type zeolite which is remarkably different from oxide supports. [Pg.171]

While the p-tosylate undoubtedly increases the hydrophobicity of the W micro-environment, formation of heteronuclear S-W peroxodusters might also contribute to the improved epoxide selectivities in Table 3. In order to check this hypothesis, S04 - and Cb exchanged LDHs were compared. Even if these materials have a similar polarity, selectivities are systematically better for the... [Pg.1058]

In an apolar medium, the fluorophore at the excited state will induce the formation of a dipole within the environment. Formation of a new dipole needs less energy than reorientation of an already existing dipole. Thus emission from an apolar environment yields an emission spectrum with a maximum located in the blue compared to the emission occurring from a polar environment. [Pg.134]

A wide variety of bacteria and fungi utilize hydroxamates (Figure 2) to sequester iron from their environment. Formation of the ferric complex from these chelating groups requires the... [Pg.143]

Lower corrosion rate on WS at P2 and P3 appears primarily due to availability of SO2 in the environment. Formation of continuous rust product causes a reduction in oxygen supply to diffuse through rust deposits and reduces the corrosion rate. [Pg.112]

While the thermodynamic properties of nonsolvated forms depend only on temperature and pressure, the free energy of hydrates (and solvates) is influenced by the activity of the water (or solvent) in the environment Formation ofa stoichiometric hydrate with n molecules of water per compound molecule can be described by Equation 5.7 ... [Pg.92]

Society of Petroleum Engineers http //www.spe.org/ (accessed March 24,2011). The Society of Petroleum Engineers publishes titles in four series monograph, textbook, reprint, and conference proceedings. Topics include completions, drilling, economics, enhanced oil recovery, health, safety and environment, formation evaluation, management, production and facilities, reservoir, as well as a set of reference titles. [Pg.485]

In a polluted or urban atmosphere, O formation by the CH oxidation mechanism is overshadowed by the oxidation of other VOCs. Seed OH can be produced from reactions 4 and 5, but the photodisassociation of carbonyls and nitrous acid [7782-77-6] HNO2, (formed from the reaction of OH + NO and other reactions) are also important sources of OH ia polluted environments. An imperfect, but useful, measure of the rate of O formation by VOC oxidation is the rate of the initial OH-VOC reaction, shown ia Table 4 relative to the OH-CH rate for some commonly occurring VOCs. Also given are the median VOC concentrations. Shown for comparison are the relative reaction rates for two VOC species that are emitted by vegetation isoprene and a-piuene. In general, internally bonded olefins are the most reactive, followed ia decreasiag order by terminally bonded olefins, multi alkyl aromatics, monoalkyl aromatics, C and higher paraffins, C2—C paraffins, benzene, acetylene, and ethane. [Pg.370]

Corrosion by Various Chemicals and Environments. In general, the rate of corrosion of magnesium ia aqueous solutions is strongly iafluenced by the hydrogen ion [12408-02-5] concentration or pH. In this respect, magnesium is considered to be opposite ia character to aluminum. Aluminum is resistant to weak acids but attacked by strong alkaUes, while magnesium is resistant to alkaUes but is attacked by acids that do not promote the formation of iasoluble films. [Pg.332]


See other pages where Environment Formation is mentioned: [Pg.248]    [Pg.111]    [Pg.75]    [Pg.313]    [Pg.129]    [Pg.204]    [Pg.78]    [Pg.187]    [Pg.318]    [Pg.709]    [Pg.196]    [Pg.42]    [Pg.248]    [Pg.111]    [Pg.75]    [Pg.313]    [Pg.129]    [Pg.204]    [Pg.78]    [Pg.187]    [Pg.318]    [Pg.709]    [Pg.196]    [Pg.42]    [Pg.80]    [Pg.81]    [Pg.418]    [Pg.45]    [Pg.137]    [Pg.331]    [Pg.356]    [Pg.314]    [Pg.199]    [Pg.206]    [Pg.57]    [Pg.169]    [Pg.97]    [Pg.548]    [Pg.378]    [Pg.115]    [Pg.116]    [Pg.461]    [Pg.125]    [Pg.127]    [Pg.229]    [Pg.433]    [Pg.203]    [Pg.40]    [Pg.217]    [Pg.268]   
See also in sourсe #XX -- [ Pg.11 , Pg.21 , Pg.23 , Pg.25 , Pg.47 ]




SEARCH



Formation in the Environment

Formation mechanisms natural environments

Formation solvent-free environments

Soils - a unique environment for iron oxide formation in terrestrial ecosystems

Solar system formation environment

© 2024 chempedia.info