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Carbonate acidizing origins

Soil reaction (pH) The relationship between the environment and development of acid or alkaline conditions in soil has been discussed with respect to formation of soils from the parent rock materials. Soil acidity comes in part by the formation of carbonic acid from carbon dioxide of biological origin and water. Other acidic development may come from acid residues of weathering, shifts in mineral types, loss of alkaline or basic earth elements by leaching, formation of organic or inorganic acids by microbial activity, plant root secretions, and man-made pollution of the soil, especially by industrial wastes. [Pg.383]

Economizers are not usually designed to generate steam, and any deposits found in them therefore are not likely to be a result of carbonic acid corrosion or contamination from steam. Rather, the transport and buildup of corrosion debris within an economizer tends to originate from corrosion processes occurring either in the economizer itself or in some upstream part of the pre-boiler system. Economizer deposits typically develop in the presence of oxygen and possess a high iron content. [Pg.153]

The difference in solubility between carbonates and hydrogen carbonates is responsible for the behavior of hard water, which is water that contains dissolved calcium and magnesium salts. Hard water originates as rainwater which dissolves carbon dioxide from the air and forms a very dilute solution of carbonic acid. [Pg.446]

A chemical reaction in which the products react to re-form the original reactants is called a reversible reaction. For example, club soda is a mixture of carbon dioxide gas and water. The water and carbon dioxide react forming carbonic acid (H2C03). Carbonic acid decomposes to again form water and carbon dioxide. A state of equilibrium is reached in which the amounts of carbonic acid, water, and carbon dioxide remain constant. The overall reaction can be written as follows. [Pg.141]

Compounds containing a carbon atom united with four different atoms or groups are called asymmetric compounds and this carbon atom is called an asymmetric carbon atom. Originally the presence of an asymmetric carbon atom was regarded to impart optical activity. But later compounds were discovered which showed optical activity but were devoid of asymmetric carbon atoms, e.g., methyl cyclo-hexylidence acetic acid. [Pg.123]

The chemical diversity of carboxylic acid esters (R-CO-O-R ) originates in both moieties, i.e., the acyl group (R-CO-) and the alkoxy or aryloxy group (-OR7). Thus, the acyl group can be made up of aliphatic or aromatic carboxylic acids, carbamic acids, or carbonic acids, and the -OR7 moiety may be derived from an alcohol, an enol, or a phenol. When a thiol is involved, a thioester R-CO-S-R7 is formed. The model substrates to be discussed in Sect. 7.3 will, thus, be classified according to the chemical nature of the -OR7 (or -SR7) moiety, i.e., the alcohol, phenol, or thiol that is the first product to be released during the hydrolase-catalyzed reaction (see Chapt. 3). Diesters represent substrates of special interest and will be presented separately. [Pg.383]

Sadly, Priestley missed the significance of his discovery. From knowledge of Priestley s findings, Antoin-Laurent Lavoisier realised the theoretical importance of them the gas that he had found that reacted with carbon in food to form a weak acid (carbonic acid) was Priestley s gas. He called the new air oxygen , from the Greek words oxys (sour, acidic) and genous (origin, descent). [Pg.195]

From the reaction of D-ribose-J-14C with secondary amine salts in aqueous acid, Peer and van den Ouweland215 isolated 4-hydroxy-5-methyl-3(2H)-furanone (120) (11.4%), and found it to be labeled entirely at the methyl carbon atom. Thus, in the presence of amines, the formation of 120 must proceed through the 1-deoxydiulose by the mechanism described in Section II (see p. 168). In contrast, the reaction of D-ribose-J-14C 5-phosphate218 gave 120 having no radioactivity in the methyl carbon atom, from which it was concluded that the methyl carbon atom originates from C-5 of the D-ribose. The... [Pg.217]


See other pages where Carbonate acidizing origins is mentioned: [Pg.174]    [Pg.174]    [Pg.174]    [Pg.174]    [Pg.172]    [Pg.269]    [Pg.354]    [Pg.16]    [Pg.376]    [Pg.174]    [Pg.25]    [Pg.20]    [Pg.82]    [Pg.313]    [Pg.69]    [Pg.86]    [Pg.102]    [Pg.115]    [Pg.359]    [Pg.17]    [Pg.43]    [Pg.157]    [Pg.166]    [Pg.167]    [Pg.333]    [Pg.342]    [Pg.491]    [Pg.598]    [Pg.599]    [Pg.638]    [Pg.681]    [Pg.685]    [Pg.729]    [Pg.1017]    [Pg.1018]    [Pg.1087]    [Pg.1093]    [Pg.1095]    [Pg.1098]    [Pg.1114]    [Pg.523]    [Pg.112]    [Pg.141]    [Pg.36]   
See also in sourсe #XX -- [ Pg.7 ]

See also in sourсe #XX -- [ Pg.7 ]




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