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Transport water

Water transport is associated with various physiological processes in whole living organisms and single cells. [Pg.39]

When cells are exposed to hyper- or hypo-osmotic solutions, they immediately lose or gain water, respectively. Even in an isotonic medium a continuous exchange of water occurs between living cells and their surroundings. Most cells are so small and their membrane so leaky that the exchange of water molecules measured with isotopic water reaches equilibrium in a few milliseconds. [Pg.39]

The degree of water permeability differs considerably between tissues and cell types. Mammalian red blood cells and renal proximal tubules are extremely permeable to water molecules. Transmembrane water movements are involved in diverse physiological secretion processes. [Pg.39]

How water passes through cells has begun to come clear only in the last live years. Water permeates living membranes through both the lipid bilayer and specific water transport proteins. In both cases water flow is passive and directed by osmosis. Water transport in living cells is therefore under the control of ATP and ion pumps. [Pg.39]

The most general water transport mechanism is diffusion through lipid bilayers, with a permeability coefficient of 2-5 x 10 4 cm/sec. The diffusion through lipid bilayers depends on lipid structure and the presence of sterol (Subczyhski et al., 1994). It is suggested that the lateral diffusion of the lipid molecules and the water diffusion through the membrane is a single process (Haines, 1994). [Pg.39]

According to analysis by differential scanning calorimeter (DSC), water molecules in the membranes can be classified into three types, non-freezing, freezing bound and free water.40 Also, the weight ratios of freezable water and [Pg.109]

Transmembrane movement of water in the absence of or against a limited osmotic gradient may theoretically occur by a number of mechanisms, since classical osmosis cannot be involved. Active transport of water has not been observed in vertebrates (Pappius, 1964). During pinocytosis (see above) a small quantity of the aqueous medium surrounding the membrane may be engulfed in the pinocytotic vesicle. The subsequent secretion of the water from the vesicle results in a net movement of the fluid from one side of the membrane to the other. [Pg.418]

and Christensen, H. N., 1962, Transfer of amino acids across the intestine A new model amino acid, /. Biol. Chem. 237 113. [Pg.419]

Albers, R. W., 1976, The (sodium plus potassium)-transport ATPase, in The Enzymes of Biological Membranes, Vol. 3, Membrane Transport (A. Martonosi, ed.), pp. 283-301, Plenum Press, New York. [Pg.419]

and Crumpton, M. J., 1970, Preparation and characterization of the plasma membrane of pig lymphocytes, Biochem. J. 120 133. [Pg.419]

Altman, P. L., and Katz, D. D., eds., 1976, Changes in cell surface membranes associated with malignant transformation, in Cell Biology, pp. 134-138, Federation of American Societies for Experimental Biology, Bethesda, Md. [Pg.419]


Marrink, S.-J., Berendsen, H.J.C. Simulation of water transport through a lipid membrane. J. Phys. Chem. 98 (1994) 4155-4168. [Pg.35]

The pressure difference between the high and low pressure sides of the membrane is denoted as AP the osmotic pressure difference across the membrane is defined as Att the net driving force for water transport across the membrane is AP — (tAtt, where O is the Staverman reflection coefficient and a = 1 means 100% solute rejection. The standardized terminology recommended for use to describe pressure-driven membrane processes, including that for reverse osmosis, has been reviewed (24). [Pg.146]

Solution—Diffusion Model. In the solution—diffusion model, it is assumed that (/) the RO membrane has a homogeneous, nonporous surface layer (2) both the solute and solvent dissolve in this layer and then each diffuses across it (J) solute and solvent diffusion is uncoupled and each is the result of the particular material s chemical potential gradient across the membrane and (4) the gradients are the result of concentration and pressure differences across the membrane (26,30). The driving force for water transport is primarily a result of the net transmembrane pressure difference and can be represented by equation 5 ... [Pg.147]

United States Code Annotated, West Publishing Co., St. Paul, Minn. A compilation of U.S. laws of a general and permanent nature consisting of 50 Tides. Although many provisions of various Tides affect transportation. Tides 49 (Transportation) and 46 (Shipping) are of particular iaterest. Among other important statutes iacluded ia Tide 49 are the ICC Termination Act of 1995 ( 10101 et seql), the Department of Transportation Act ( 101 et seql), and the Hazardous Materials Transportation Act ( 5101 et seq.). Tide 46 collects various statutes pertaining primarily to water transportation. [Pg.264]

Water Transport. Two methods of measuring water-vapor transmission rates (WVTR) ate commonly used. The newer method uses a Permatran-W (Modem Controls, Inc.). In this method a film sample is clamped over a saturated salt solution, which generates the desired humidity. Dry air sweeps past the other side of the film and past an infrared detector, which measures the water concentration in the gas. For a caUbrated flow rate of air, the rate of water addition can be calculated from the observed concentration in the sweep gas. From the steady-state rate, the WVTR can be calculated. In principle, the diffusion coefficient could be deterrnined by the method outlined in the previous section. However, only the steady-state region of the response is serviceable. Many different salt solutions can be used to make measurements at selected humidity differences however, in practice,... [Pg.500]

Commercially available membranes are usually reinforced with woven, synthetic fabrics to improve the mechanical properties. Several hundred thousand square meters of IX membranes are now produced aimuaHy, and the mechanical and electrochemical properties are varied by the manufacturers to suit the proposed appHcations. The electrochemical properties of most importance for ED are (/) the electrical resistance per unit area of membrane (2) the ion transport number, related to current efficiency (2) the electrical water transport, related to process efficiency and (4) the back-diffusion, also related to process efficiency. [Pg.172]

Pipe Lines For quantities of fluid which an economic investigation indicates are sufficiently large and continuous to justify the investment, pipe lines are one of the lowest-cost means of transportation. They have been built up to 1.22 m (48 in) or more in diameter and about 3200 km (2000 mi) in length for oil, gas, and other products. Water is usually not transported more than 160 to 320 km (100 to 200 miles), but the conduits may be much greater than 1.22 m (48 in) in diameter. Open canals are also used for water transportation. [Pg.1020]

Salt flux across a membrane is due to effects coupled to water transport, usually negligible, and diffusion across the membrane. Eq. (22-60) describes the basic diffusion equation for solute passage. It is independent of pressure, so as AP — AH 0, rejection 0. This important factor is due to the kinetic nature of the separation. Salt passage through the membrane is concentration dependent. Water passage is dependent on P — H. Therefore, when the membrane is operating near the osmotic pressure of the feed, the salt passage is not diluted by much permeate water. [Pg.2035]

Water Transport Barges, scows, and special boats have been used in the past to transport sohd wastes to processing locations and to seaside and ocean disposal sites, but ocean disposal is no longer practiced by the United States. Although some self-propelled vessels (such as U.S. Navy garbage scows and other special boats) have been used, most common practice is to use vessels towed by tugs or other special boats. [Pg.2241]

Department of Transportation - has sponsored work on air, ground, rail, and water transportation, using PSA methods. [Pg.17]

Daviskas, E., Gonda, I., and Anderson, S. D. (1990). Mathematical modeling of heat and water transport in human respiratory tract. /. Appl. Physiol. 69, 362-372. [Pg.229]

Scherer, P. W., and Hanna, L. M. (1985). Heat and water transport in the human respiratory tract. In Mathematical Modeling m Medicine and Biology (A. Shitzer and R. C. Eberh.trt, Eds. , pp. 287-306. Plenum Press, New York. [Pg.231]

The Department of Transportation is responsible for setting safety standards for rail, highway, air and water transportation and providing law enforcement and traffic management for airspace and waterways. Also regulates manufacturers of containers and transporters of hazardous materials. [Pg.287]

Less-than-carload-lol rates are very higli. Therefore, the distance that the material must be shipped should be kept to a minimum. Each of the four major transportation methods in use today (railroad freight, trucking, water transport, and air travel) has its benefits and drawbacks. [Pg.166]

A cargo barge travels up the Rhine. Though weather conditions can affect timeliness, the economies of scale usually make water transport cheaper than rail. (Corbis Corporation)... [Pg.263]

Prior to 1900, water transport of oil was carried out in makeshift vessels, such as barges and converted freighters and ore-carrying ships. These were often contracted out (in contrast to pipelines that more often were owned by the producers). There was an increase in water transport of oil during the first two decades of the centui y. [Pg.949]

With the Norman conquest of England, industry moves from the abbeys and country estates to the towns because of energy— water mills and water transportation. [Pg.1247]

Aquaporins (AQP) are a family of integral membrane proteins expressed in all organisms and play a fundamental role in the regulation of water transport into and out of cells. [Pg.213]

Steam quality relates to the amount of entrained water transported into dry steam on a weight/weight basis. Because the water may contain TDS, steam quality is generally very closely allied with steam purity. [Pg.276]

Introducing the values into the equation, using a minimum Kd-value of >300, gives a retention factor of >750. If this value is combined with a representative water transport time from repository to recipient (>1000 years for a distance >100 m), the transport equation indicates that it will take the plutonium >750,000 years to reach the recipient which is the water man may use. This estimate is supported by findings at the ancient natural reactor site at Oklo in Gabon (67). [Pg.291]

The rate of water transport through polyaniline has been measured by mass spectrometry.198 Consistent with the gravimetric results cited above, the permeability of the oxidized state was found to be much higher than that of the reduced state. [Pg.582]

Zauker, F. and Broecker, W. S. (1992). Influence of interocean fresh water transports on ocean thermohaline circulation. /. Geophys. Res. 97, 2765-2773. [Pg.278]

Boyer, J.S. (1985). Water transport. Annual Review of Plant Physiology, 36, 473-516. [Pg.90]


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Air-Water Transport Processes

Airway Heat and Water Vapor Transport

Analysis of water transport through MPL

Aquatic water transportable degradation product

Atmosphere water transport

Atmospheric water transport, effects

Colloidal and Sediment Transport into Surface Water

Contaminant-transport models ground water

Coupled proton and water transport

Drinking water transport

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Fish transport water

Fluid meters water transport

Ionomer water transport

Lipids water transport, cellular

Liquid water transport

Membrane transport water channels

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Meridional Transport of Water The ITCZ

Migration water transport

Nafion water transport

Oxide-water interface transport

Pesticides ground water transport

Physical Transport in Surface Waters

Plant water vapor transport measure

Plant water vapor transportation, valve

Proton Transport Near the Polymer-Water Interface

Proton Transport in Water and Aqueous Networks

Proton exchange membrane water transport

Proton transport in bulk water

Proton transport in water

Soil water transport

Soil water transport diffusion

Soil water transport hydrodynamic dispersion

Soil water transport mass flow

Stopper water vapor transport

Storage, Transport and Preservation of Pore Water

Taking and transporting water samples for microbiological investigations

The transport of substances by water

Transmembrane transport water

Transport Mechanisms of Protons and Water

Transport behavior water

Transport in Water

Transport into surface waters

Transport of Adsorbable Constituents in Ground Water and Soil Systems

Transport of Protons and Water

Transportation waste water

Water Layer Rate-Limiting Transport (Lipophilic Molecules)

Water Transport Equation

Water Transport Rate Equation

Water Transport Under Osmotic Pressure Mismatch

Water Transport in Electrodialysis

Water Transport in Electrolyte Membranes

Water Transport in MEAs

Water Transport in the Unsaturated Zone

Water Transportable Degradation Products

Water Vapor Transport Properties

Water Vapor Transport during Drying

Water and Solute Transport Processes

Water contaminant transport

Water driven injector transport

Water membrane transport

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Water transport across membranes

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Water transport in gas diffusion layers

Water transport in membranes

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