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Transport in Water

In aqueous systems, the inorganic and organic compounds of lead have unique chemistries and transport mechanisms. Normally, naturally occuring lead in ore deposits do not move appreciably in the environment. [Pg.14]

In lotic (running water) conditions, lead may be carried in an undissolved state. This undissolved inorganic lead may consist of suspended colloidal particles and larger undissolved particles of lead carbonate, oxide, and hydroxide. The undissolved lead may also be transported by sorption on mineral particles or carried as part of the suspended living or nonliving organic matter [44]. [Pg.14]


Transport in water is an important mechanism for transfer of biogeochemical elements between the atmosphere, land, and oceans. In particular, rain is the primary means of removal from the atmosphere for many substances, and rivers (and to some extent groundwater) convey weathering products and runoff from the land surface to the oceans. [Pg.127]

This review mostly summarizes the scientific information available in developed countries, where the prevalence of diseases associated with water use is kept under very acceptable levels. However, there are reasons to think that the situation might worsen as a consequence of the effects of the climatic change, the increase of population in certain areas and the deterioration of sanitation infrastructures. It may be necessary to take new measures to maintain the present situation. Better knowledge of the water-borne pathogens, where they originate, how they persist or replicate in the environment, how they survive water treatments, and how they are transported in water and soil, will allow us to take the necessary measures to prevent the effects of water scarcity as well as the effects of extreme climatic events foreseen for the future by the experts in climatic change [13]. [Pg.149]

As discussed elsewhere in this volume, another field where the use of U-series disequilibria has proven to be very useful is the study of chemical transport in waters, either marine (see Cochran and Masque 2003 Henderson and Anderson 2003), estuarine (Swarzenski et al. 2003) or continental waters. In the continental domain, in addition to characterization of transfer processes related to groundwater flows (Porcelli and Swarzenski 2003), radioactive disequilibria have also helped in constraining chemical exchanges between particulate, dissolved and colloidal loads of waters, as well as the origin of chemical fluxes carried by waters. [Pg.553]

The jet plane has made it easy to travel to and from previously inaccessible parts of the world, for business or vacation. Infectious diseases or agents that transmit these diseases can, therefore, be rapidly transferred to countries in which the population has never encountered the diseases, so that the infection rapidly spreads throughout the population. Such transport of pathogens is reminiscent of the transmission of diseases that were previously unknown in North America but were transported from Africa in the slave ships. For example, the mosquito Aedes aegypti, which transmits the virus that causes yellow fever, was probably transported in water barrels on these ships. [Pg.411]

Burrill, K.A. "Corrosion Product Transport in Water Cooled Nuclear Reactors - Part 1, Pressurized Water Operation"... [Pg.334]

Tin in water may partition to soils and sediments. Cations such as Sn and Sn will generally be adsorbed by soils to some extent, which reduces their mobility. Tin is generally regarded as being relatively immobile in the environment (WHO 1980). However, tin may be transported in water if it partitions to suspended sediments (Cooney 1988), but the significance of this mechanism has not been studied in detail. [Pg.137]

The cost of transporting wood chips by truck and by pipeline as a water slurry was determined. In a practical application of field delivery by truck of biomass to a pipeline inlet, the pipeline will only be economical at large capacity (>0.5 million dry t/yr for a one-way pipeline, and >1.25 million dry t/yr for a two-way pipeline that returns the carrier fluid to the pipeline inlet), and at medium to long distances (>75 km [one-way] and >470 km [two-way] at a capacity of 2 million dry t/yr). Mixed hardwood and softwood chips in western Canada rise in moisture level from about 50% to 67% when transported in water the loss in lower heating value (LHV) would preclude the use of water slurry pipelines for direct combustion applications. The same chips, when transported in a heavy gas oil, take up as much as 50% oil by weight and result in a fuel that is >30% oil on mass basis and is about two-thirds oil on a thermal basis. Uptake of water by straw during slurry transport is so extreme that it has effectively no LHV. Pipeline-delivered biomass could be used in processes that do not produce contained water as a vapor, such as supercritical water gasification. [Pg.27]

The effect of solvents on PT is complicated by the fact that usually the solvents which exhibit a strong activity are both proton donor and proton acceptor, like water, and thus can participate in the reactions. A model of proton transport in water which uses the EVB model has been recently published by Schmidt and Voth [28]. [Pg.433]

R. L. Kay, Ionic Transport in Water arid Mixed Aqueous Solvents, in Water, edited by F. Franks, Vol. 3, Chap. 4 (Plenum, New York, 1973). [Pg.360]

Cossa D., Sanjuan J., and Noel J. (1994) Mercury transport in waters of the Strait of Dover. Mar. Pollut. Bull. 28(6), 385-388. [Pg.4682]

Mok YS, Lee SC, and Lee WK. Water transport in water-in-oil-in-water liquid emulsion membrane system for the separation of lactic acid. Sep Sci Techrwl 1994 29 743-764. [Pg.740]

Chemical transport in the atmosphere has many parallels with transport in water both advection and Fickian processes are important. However, the velocities and the Fickian transport coefficients tend to be larger in the atmosphere, and the distances over which pollutant sources have influence... [Pg.397]

Schmitt, U.W. and Voth, G.A. (1998). Multistate empirical valence bond model for proton transport in water. J. Phys. Chem. B 102, 5547-5551... [Pg.301]

The first section (i.e., 1 in Table 2) serves as an introduction and defines the scope of the subject. As implied in the title, it is one of chemodynamics or the movement of chemicals. Chemical transport is the primary focus of the material. Critics have noted that production and degradation rates of chemical reactions are all but absent in the course syllabus. Environmental reaction is a very important but is also a very broad subject and its inclusion at even a basic technical level into EC would detract from the transport message. Two basic subjects are necessary for understanding transport. These are chemical equilibrium at interfaces and the fundamentals of transport phenomena. Highly condensed material on these two key subjects are presented in chapters 2 and 3. The last chapter, number 7, is on the fate and transport in water, air, and soil. These are the traditional subjects of environmental modeling which treat each of the three media separately and as isolated units from a multimedia perspective. Nevertheless, this approach is very appropriate for numerous EC applications. The section stresses the commonalities of fate and transport in the three media however, the brief coverage offered on each belies the importance of these respective intraphase transport topics. [Pg.894]

A problem present in the refinery is that, due to its fast transport in water and low biodegradabUity, MTBE addition to gasoline pool has been banned in some countries (from 2003 in Cahfomia). MTBE is formed by add-catalyzed reaction of isobutene with methanol. Other alcohols could be used to form different oxygenated additives, as discussed below, but the alternative is to use isobutene for conversion into another high octane number component such as isooctane, which could substitute in part the need of the alkylation process and related environmental/safety problems. [Pg.142]

Bhagat, S. K., Gloyna, E. F., Radioactivity Transport in Water—Trans-... [Pg.200]

Schmitt, U. W., Voth, G. A., Multistate Empirical Valence Bond Model for Proton Transport in Water, f Phys. Chem. B 1998, 102, 5547-5551. [Pg.1202]


See other pages where Transport in Water is mentioned: [Pg.488]    [Pg.141]    [Pg.416]    [Pg.315]    [Pg.92]    [Pg.62]    [Pg.257]    [Pg.395]    [Pg.62]    [Pg.257]    [Pg.98]    [Pg.259]    [Pg.225]    [Pg.31]    [Pg.83]    [Pg.2097]    [Pg.205]    [Pg.223]    [Pg.452]    [Pg.897]    [Pg.74]    [Pg.48]    [Pg.200]    [Pg.201]    [Pg.201]    [Pg.1177]    [Pg.395]    [Pg.5]   


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Water transport

Water transportation

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