Impermeable Sentence Examples

impermeable
  • Thus in the western mountain districts of Great Britain, largely composed of nearly impermeable rocks more Lion.

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  • It is now a requirement to use virtually impermeable Film in methyl bromide treatments.

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  • The surface of the earth is rarely impermeable, and the structure of the rocks largely determines the direction of flow of so much of the rainfall as sinks into the ground and is not evaporated.

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  • The finished surface is totally impermeable, resistant to frost and repeated freeze-thaw cycles.

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  • Yet another option is winding the insert into a diaper itself, and then placing a rubber or other impermeable cover over the cloth diaper.

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  • The boiler suits normally worn by University tradesmen may not be suitable and they should be encouraged to wear impermeable disposable coveralls.

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  • Ideal for domestic garages, the finished floor is glossy, seamless, and completely impermeable.

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  • The seed coat hardens and becomes impermeable as the seeds ripen.

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  • He points out that many people can avoid illness simply by ensuring that the basement of dwellings is made impermeable to such gases.

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  • This large evaporation, which constitutes the so-called transpiration of plants, takes place not into the external air but into this same intercellular space system, being possible only through the delicate cell-walls upon which it abuts, as the external coating, whether bark, cork or cuticle, is impermeable by watery vapour.

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  • Air, whether cold or hot, cannot flow through vapor barriers because they are impermeable.

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  • If you don't have a waterproof underlayment, like sheet vinyl, you may want to consider adding an impermeable membrane or sealer.

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  • If you select a moisture wicking Capri for this purpose, then sweat is less likely to get trapped between impermeable outerwear and your skin.

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  • The amount of watery vapour in the air passing through a stoma has no effect upon it, as the surfaces of the guard cells abutting on the air chamber are strongly cuticularized, and therefore impermeable.

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  • The base of a puddle trench is often found to have been placed upon rock, perfectly sound in itself, but having joints which are not impermeable.

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  • These PET carboys are food grade and gas impermeable, and they weigh about 10lbs less than a glass carboy and can not shatter.

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  • Whilst flows in neighboring impermeable catchments responded rapidly to the lack of rainfall, and were notable depressed by month end.

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  • The positions of springs are determined by permeable depressions in the surface of the ground below the general level of saturation, and frequently also by the holding up of that level locally by comparatively impermeable strata, sometimes combined with a fault or a synclinal fold of the strata, forming the more permeable portion into an underground basin or channel lying within comparatively impermeable boundaries.

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  • Even the beds of sluggish rivers flowing over porous strata generally become so impermeable that excavations made in their neighbourhood, though freely collecting the subsoil water, receive no FIG.

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  • In mountain valleys, rock or shale, commonly the most impermeable materials met with in such positions, are sometimes not reached till considerable depths are attained.

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  • Wherever the base of a puddle wall cannot be worked into a continuous bed of clay or shale, or tied into a groove cut in sound rock free from water-hearing fissures, the safest course is to base it on an artificial material at once impermeable and incapable of erosion, interposed between the rock and the puddled clay.

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  • This gray and relatively impermeable Chalk was the main tunneling horizon for the Channel Tunnel.

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  • The finished surface is almost impermeable, resistant to frost and repeated freeze-thaw cycles.

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  • It is more likely that dolomitisation fronts formed on the sides of the fault-controlled pathway, with the unaltered marbles remaining essentially impermeable.

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  • These fissures take the place of the streams in an impermeable area, and those beneath the valleys must obviously be called upon to discharge more water from the surface, and thus be brought in contact with more carbonic acid, than similar fissures elsewhere.

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  • Hence the best position for a well in the Chalk is generally that over which, if the strata were impermeable, the largest quantity of surface water would flow.

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  • The Lower Chalk formation is for the most part impermeable, though it contains many ruptures and dislocations or smashes, in the interstices of which large bodies of water, received from the Upper and Middle Chalk, may be naturally stored, or which may merely form passages for water derived from the Upper Chalk.

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  • Dams Any well-made earthen embankment of moderate height, and of such thickness and uniformity of construction as to ensure freedom from excessive percolation at any point, will in the course of time become almost impermeable to surface water standing against it; and when permeable rocks are covered with many feet of soil, the leakage through such soil from standing water newly placed above it generally diminishes rapidly, and in process of time often ceases entirely.

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  • Of these methods one of the chief is the plan of tubbing, or lining the excavation with an impermeable casing of wood or iron, generally the latter, built up in segments forming rings, which are piled upon each other throughout the whole depth of the water-bearing strata.

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  • The first filter which was more or less completely impermeable to bacteria was the Pasteur-Chamberland, which was devised in Pasteur's laboratory, and is made of dense biscuit porcelain.

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  • It is impermeable to water, and is therefore used in northern countries for roofing, for domestic utensils, for boxes and jars to contain both solid and liquid substances, and for a kind of bark shoes, of which it is estimated 25 millions of pairs are annually worn by the Russian peasantry.

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  • But these protective layers are in the main impermeable by gases and by either liquid or vapour, and prevent the access of either to the protoplasts which need them.

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  • Pfeffer, made known the phenomena of the osmotic pressure which is set up by the passage of solvent through a membrane impermeable to the dissolved substance or solute.

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  • The soil of yards and the floors and walls of houses rapidly become contaminated, and the ideal condition would be to have an impermeable flooring covering the whole area, and supplied with suitable layers of sand, sawdust, peat-moss or other absorbent substances which can be changed at frequent intervals.

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  • The clays of the Rolling Downs formation overlie a series of sands and drifts, saturated with water under high pressure, which discharges at the surface as a flowing well, when a borehole pierces the impermeable cover.

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  • We have hitherto dealt only with the collection and storage of that portion of the rainfall which flows over the surface of nearly impermeable areas.

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  • Among the sedimentary rocks we have, for example, in the clay slates of the Silurian formations, rocks no less cracked and fissured than others, but generally quite impermeable by reason of the joints being packed with the very fine clay resulting from the rubbing of slate upon slate in the earth movements to which the cracks are due.

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  • Thus natural or artificial surfaces which are completely permeable to rainfall may become almost impermeable when protected by surface water from drought and frost, and from earth-worms, vegetation and artificial disturbance.

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  • If the membrane is of some impermeable substance, like gold leaf, the hyphae cannot dissolve its way through, but the tip finds the most minute pore and traverses the barrier by means of it, as it does a stoma on a leaf, We may hence conclude that a parasitic hyphae pierces some plants or their stomata and refuses to enter others, because in the former case there are chemotropically attractive substances present which are absent from the latter, or are there replaced by repellent poisonous or protective substances such as enzymes or antitoxins.

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  • The most trying time-distribution of which the author has had experience in the United Kingdom, or which he has been able to discover from a comparison of rainfalls upon nearly impermeable areas exceeding woo acres, is graphically represented by the thick irregular line in the left-hand half of fig.

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  • If any rock be taken (even a piece of pure quartz) and crushed to a very fine powder, it will show some of the peculiarities of clays; for example, it will be plastic, retentive of moisture, impermeable to water, and will shrink to some extent if the moist mass be kneaded, and then allowed to dry.

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