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Solutions The Atmosphere

Just as water bodies such as rivers, lakes, and the ocean can be considered enormous aqueous solutions, the atmosphere is a gigantic gaseous solution. The atmosphere is composed primarily of nitrogen, 78%, and oxygen, 21%. The third most abundant gas in the atmosphere is argon, which makes up about 0.9%. The remaining 0.1% consists of... [Pg.278]

As rain, water brings into solution the atmospheric gases of oxygen, nitrogen and carbon dioxide. As it percolates through the soil, it dissolves and picks up many minerals harmful to boiler operation. Surface waters frequently contain organic matter that must be removed before the water is satisfactory for use in a boiler. [Pg.1739]

Gaseous solutions the atmosphere, anesthetic gas mixtures, helium and air in a balloon... [Pg.361]

When volumes of 0 2-2 ml. of solutions are to be analysed using a mercury pool reference electrode, the semimicro-vessel depicted in Fig. 20b can be used. The wide arm of the vessel serves to keep the level of mercury constant in the narrower part, where the solution to be analysed is placed. This vessel is equipped with a side arm for deaeration of the solution. The atmospheric oxygen is removed from the solution to be electrolysed by bubbling an inert gas (nitrogen, hydrogen or carbon dioxide) through the solution. The outlet of the gas is in the upper right section of the vessel and is usually connected to a water seal. [Pg.35]

S3. A small sample of pure air is a homogeneous mixture and is therefore a solution. The atmosphere, even if it were pure air, is a very tall sample that becomes less dense at higher elevations. The atmosphere is therefore not homogeneous, and consequently it is not a solution. 154. The density of a solution must be known in order to convert concentrations based on mass only (percentage, molality) to those based in volume (molarity, normality). [Pg.733]

Rainwater brings into solution the atmospheric gases of oxygen, nitrogen and carbon dioxide. As it passes through the solids, it picks up minerals. [Pg.587]

Solution The fraction of liquid vaporized on release is calculated from a heat balance. The sensible heat above saturated conditions at atmospheric pressure provides the heat of vaporization. The sensible heat of the superheat is given by... [Pg.269]

Atmospheric corrosion results from a metal s ambient-temperature reaction, with the earth s atmosphere as the corrosive environment. Atmospheric corrosion is electrochemical in nature, but differs from corrosion in aqueous solutions in that the electrochemical reactions occur under very thin layers of electrolyte on the metal surface. This influences the amount of oxygen present on the metal surface, since diffusion of oxygen from the atmosphere/electrolyte solution interface to the solution/metal interface is rapid. Atmospheric corrosion rates of metals are strongly influenced by moisture, temperature and presence of contaminants (e.g., NaCl, SO2,. ..). Hence, significantly different resistances to atmospheric corrosion are observed depending on the geographical location, whether mral, urban or marine. [Pg.2731]

Silver has little tendency to formally lose more than one electron its chemistry is therefore almost entirely restricted to the + 1 oxidation state. Silver itself is resistant to chemical attack, though aqueous cyanide ion slowly attacks it, as does sulphur or a sulphide (to give black Ag S). hence the tarnishing of silver by the atmosphere or other sulphur-containing materials. It dissolves in concentrated nitric acid to give a solution of silver(I) nitrate. AgNOj. [Pg.427]

The boiling point increases regularly. The boiling point - composition diagram for such a system is shown in Fig. 1, 4, 2 (the complementary vapour pressure - composition diagram is depicted in Fig. I, 4, 3 for purposes of comparison only). Let us consider the behaviour of such a liquid pair upon distillation. If a solution of composition is heated, the vapour pressure will rise until at the point ij it is equal to the pressure of the atmosphere, and boiling commences at temperature The com-... [Pg.8]

Deliquescence and efflorescence. A substance is said to deliquesce (Latin to become liquid) when it forms a solution or liquid phase upon standing in the air. The essential condition is that the vapour pressure of the saturated solution of the highest hydrate at the ordinary temperature should be less than the partial pressure of the aqueous vapour in the atmosphere. Water will be absorbed by the substance, which gradually liquefies to a saturated solution water vapour will continue to be absorbed by the latter until an unsaturated solution, having the same vapour pressure as the partial pressure of water vapour in the air, is formed. In order that the vapour pressure of the saturated solution may be sufficiently low, the substance must be extremely soluble in water, and it is only such substances (e.g., calcium chloride, zinc chloride and potassium hydroxide) that deliquesce. [Pg.43]

Hydrochloric acid should not be used for acidifying the alkaline solution since the yellow colour, due to the ferric chloride formed, causes the Prussian blue to appear greenish. For the same reason, ferric chloride should not be added—as is frequently recommended a sufficient concentration of ferric ions is produced by atmospheric oxidation of the hot alkaline solution. The addition of a little dfiute potassium fluoride solution may be advantageous in assisting the formation of Prussian blue in a readily filterable form. [Pg.1039]

Solid NaOH is always contaminated with carbonate due to its contact with the atmosphere and cannot be used to prepare carbonate-free solutions of NaOH. Solutions of carbonate-free NaOH can be prepared from 50% w/v NaOH since Na2C03 is very insoluble in concentrated NaOH. When CO2 is absorbed, Na2C03... [Pg.299]

One standard method for determining the dissolved O2 content of natural waters and wastewaters is the Winkler method. A sample of water is collected in a fashion that prevents its exposure to the atmosphere (which might change the level of dissolved O2). The sample is then treated with a solution of MnS04, and then with a solution of NaOH and KI. Under these alkaline conditions Mn + is oxidized to Mn02 by the dissolved oxygen. [Pg.345]

One of the first successful techniques for selectively removing solvent from a solution without losing the dissolved solute was to add the solution dropwise to a moving continuous belt. The drops of solution on the belt were heated sufficiently to evaporate the solvent, and the residual solute on the belt was carried into a normal El (electron ionization) or Cl (chemical ionization) ion source, where it was heated more strongly so that it in turn volatilized and could be ionized. However, the moving-belt system had some mechanical problems and could be temperamental. The more recent, less-mechanical inlets such as electrospray have displaced it. The electrospray inlet should be compared with the atmospheric-pressure chemical ionization (APCI) inlet, which is described in Chapter 9. [Pg.55]

The LC/TOF instmment was designed specifically for use with the effluent flowing from LC columns, but it can be used also with static solutions. The initial problem with either of these inlets revolves around how to remove the solvent without affecting the substrate (solute) dissolved in it. Without this step, upon ionization, the large excess of ionized solvent molecules would make it difficult if not impossible to observe ions due only to the substrate. Combined inlet/ionization systems are ideal for this purpose. For example, dynamic fast-atom bombardment (FAB), plas-maspray, thermospray, atmospheric-pressure chemical ionization (APCI), and electrospray (ES)... [Pg.163]

When gases that are somewhat soluble in a Hquid concentrate are used, both concentrate and dissolved gas are expeUed. The dissolved gas then tends to escape into the atmosphere, dispersing the Hquid into fine particles. The pressure within the container decreases as the product is dispersed because the volume occupied by the gas increases. Some of the gas then comes out of solution, partially restoring the original pressure. This type of soluble compressed gas system has been used for whipped creams and toppings and is ideal for use with antistick cooking oil sprays. It is also used for household and cosmetic products either where hydrocarbon propeUants cannot be used or where hydrocarbons are undesirable. [Pg.348]

In some cases, particularly with iaactive metals, electrolytic cells are the primary method of manufacture of the fluoroborate solution. The manufacture of Sn, Pb, Cu, and Ni fluoroborates by electrolytic dissolution (87,88) is patented. A typical cell for continous production consists of a polyethylene-lined tank with tin anodes at the bottom and a mercury pool (ia a porous basket) cathode near the top (88). Pluoroboric acid is added to the cell and electrolysis is begun. As tin fluoroborate is generated, differences ia specific gravity cause the product to layer at the bottom of the cell. When the desired concentration is reached ia this layer, the heavy solution is drawn from the bottom and fresh HBP is added to the top of the cell continuously. The direct reaction of tin with HBP is slow but can be accelerated by passiag air or oxygen through the solution (89). The stannic fluoroborate is reduced by reaction with mossy tin under an iaert atmosphere. In earlier procedures, HBP reacted with hydrated stannous oxide. [Pg.168]


See other pages where Solutions The Atmosphere is mentioned: [Pg.156]    [Pg.113]    [Pg.238]    [Pg.156]    [Pg.113]    [Pg.238]    [Pg.115]    [Pg.172]    [Pg.302]    [Pg.584]    [Pg.2731]    [Pg.238]    [Pg.149]    [Pg.315]    [Pg.485]    [Pg.9]    [Pg.43]    [Pg.71]    [Pg.150]    [Pg.518]    [Pg.879]    [Pg.77]    [Pg.131]    [Pg.97]    [Pg.300]    [Pg.403]    [Pg.304]    [Pg.244]    [Pg.114]    [Pg.213]    [Pg.216]    [Pg.269]    [Pg.10]    [Pg.47]   


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Evaporation of a Solute to the Atmosphere

Primary Reactions of the Calcite-Carbonate-Equilibrium with Atmospheric Contact in Infinitely Diluted Solutions

Solution of the Atmospheric Diffusion Equation for an Instantaneous Source

Solutions of the Steady-State Atmospheric Diffusion Equation

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