Formation mechanisms natural environments

FORMATION MECHANISMS OF HUMIC SUBSTANCES IN THE ENVIRONMENT 2.6.4. Natural Soils... 

During the weathering process, elements can disperse from source mineralisation by a variety of chemical processes. For reasons discussed below, electrochemical processes are increasingly thought to be the primary transport mechanism in environments of thick, young, exotic (i.e., transported) overburden. They are also likely to operate in other environments but their dominance as a transport mechanism is less certain. This chapter presents the principles behind electrochemical masj transport and discusses the role of natural geoelectrochemical processes in the formation of selective leach and conventional geochemical soil anomalies. 

During the course of biomethylation the methyl group is most likely transferred as a bridging intermediate rather than a free entity. Such an intermediate is assumed to form during an associative mechanism [4]. The methyl group may be electrophilic (cationic), radical or nucleophilic (anionic), depending on the specific donor moiety. A broad variety of methyl transfer reactions are therefore possible. Besides the two biological donors, methylcobalamin (see below) and S-adenosyl-methonine (1) nonenzymatic transmethylation is also possible in the natural environment, probably also very important for the formation and decomposition of metal methyl compounds [3b],... 

While inheritance dominates in the sedimentary environment at generally ambient conditions characterized by slow reaction rates, layer transformation requires a considerable input of activation energy, and thus is found preferentially in the diagenetic and hydrothermal realms, where higher temperatures prevail. In between these two environments, the weathering environment exists in which all three mechanisms discussed above can be operational. Hence, when these three mechanisms occur in three different geologic environments, it leads to nine pos-sibiUties of clay mineral formation in nature, attesting to the exceptional variability and complexity of day mineral chemistries. 

The investigation of naturally weathered micas indicates that the principal mechanisms observed in the laboratory also affect vermiculitization in soils. However, Nourish [1972] suggested that, due to the lower chemical potential of interlayer potassium exchange and to the corresponding less intensive physical strain, the formation of regularly interstratified phases may be favored in the natural environment. 

Acids and bases are found throughout nature. In fact, acids and bases are used as a defense mechanism by insects and can produce beautiful limestone cave formations. If not monitored carefully, however, acids and bases in the environment can cause a lot of harm. 

Fuerstenau (1980) found that sulphide minerals are naturally floatable in the absence of oxygen. Yoon (1981) ever attributed the natural floatability of some sulphide minerals to their very low solubility. Finkelstein et al. (1975) considered that the natural floatability of sulphide minerals are due to the formation of elemental sulphur and related to the thickness of formation of elemental sulphur at the surface. Some authors reported that the hydrophobic entity in collectorless flotation of sulphide minerals were the metal-deficient poly sulphide (Buckley et al., 1985). No matter whichever mechanism, investigators increasingly concluded that most sulphide minerals are not naturally floatable and floated only under some suitable redox environment. Some authors considered that the natural floatability of sulphide minerals was restricted to some special sulphide minerals such as molybdenite, stibnite, orpiment etc. owing to the effects of crystal structure and the collectorless floatability of most sulphide minerals could be classified into self-induced and sulphur-induced floatability (Trahar, 1984 Heyes and Trahar, 1984 Hayes et al., 1987 Wang et al., 1991b, c Hu et al, 2000). 

Supplementary studies of the mechanism were conducted. The dependence of the reaction rate on the nature of environment at the cationic carbon has shown that the concurrent formation of the protic acid proceeds, if the substituents can undergo the isomerization (Scheme 61), and thus the carbenium catalysis is utterly negligible. It was shown that the reaction was still catalyzed, even when a base was added in order to rule out a TfOH catalyzed reaction. Obviously, the protonated base was then a catalyst. 

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