capillary rise वाक्य
उदाहरण वाक्य
मोबाइल
- Salt crusts form from the repeated capillary rise of salty groundwater, followed by evaporation.
- The capillary rise of water in a small-diameter tube involves the same physical process.
- The height of capillary rise is inversely proportional to the diameter of void space in contact with water.
- Simpler models, like SaltMod, based on monthly or seasonal water and soil balances and an empirical capillary rise function, are also available.
- In the unirrigated ( sacrificial ) strips the soil is dry and the groundwater comes up by capillary rise and evaporates leaving the salts behind, so that here the soil salinizes.
- The normal capillary rise in a clayey soil is less than 1.80 m ( six feet ) but can range between 0.3 and 10 m ( one and 30 ft ).
- For example, a rise of the water table towards the soil surface may lead to an increase of capillary rise, actual evaporation, and subsurface drainage, or a decrease of percolation losses.
- To obtain accuracy in the computations of the ground water flow ( sect . 2.8 ), the actual evaporation and the capillary rise, the computer calculations are done on a daily basis.
- Freeze-thaw cycles and capillary rise affect the architectural support of the mural and lead to salt efflorescence, cracking, and lifting of the paint layers if incompatible paints or coatings are used and the mural extends to ground level.
- Capillary effects in soil are more complex than in free water due to the randomly connected void space and particle interference through which to flow; regardless, the height of this zone of capillary rise, where negative pore water pressure is generally peaks, can be closely approximated by a simple equation.
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