Main Article Content
Abstract
Permeability is the process and capacity of soil that allows for the vertical movement of water according to the properties of the soil profile, which may face impermeable bedrocks. This indicates that water remains in the soil for some time, where it is used by animals and plants. The velocity of water movement through soil is calculated in inches per hour. To calculate permeability accurately, measurements from the surface to the bedrock are taken. When the soil becomes saturated, it forms a shiny crust on the surface. Permeability is related to soil particle size, but in general, permeability in soil occurs very slowly. Additionally, when the soil surface has a higher angle and precipitation intensity is lower, a smaller amount of water infiltrates the soil. For agriculture and cultivation, high permeability allows a greater amount of water to be stored in the soil. High permeability can also help recover groundwater. However, poor management and high permeability may wash away essential elements and components important for microorganisms in the soil. Plant cover can be beneficial for soil management and percolation.
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References
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- Netherlands. 2015.
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- Contents
- ارزیابی ظرفیت نفوذپذیری آب در خاکهای قلعه زمان خان، شهرکابل 1
References
Baytas, A. F. and Akbal, S. Determination of soil parameter by gamma – ray
transmission. Radiation measurements, Colorado, university. 2002. 35, 17- 21.
Beschta, R., Jackson, W. L. The intrusion of fine sediments into a stable gravel bed.
Journal of the Fisheries Research Board of Canada. 2015. 36, 204 -210.
Becker’s, F., Haun, S., et al. Experimental investigation of Reservoir sediments. E3S
Web Conf. 2018. 40-30.
Blois, G., Sambrook Smith, G. H., et al. Quantifying the dynamics of flow within a
Permeable Bed using time resolved endoscopic particle imaging velocimetry
(EPIV).Experiments in Fluids. 2012. 53, p. 51-76.
Dudill, A., et al. Infiltration of fine sediment into a coarse Mobil bed, a Phenomenological Study. Earth Surface processes and Landform. 2017. 42, 1171 - 1185.
Einstein, H. A. Deposition of suspended particle in gravel bed. Journal of Hydraulic
Engineering. 1968. 94, 1197-1205
Frostick, L. E. Lukas, M., Reid, I. The infiltration of Fine matrices into course grained
alluvialSediments and its implications for stratigraphical integration. Journal of the
Geological Society (London). 2007. 141, 955 - 965.
Gayraud, S. and phillipe, M. Influence of bed sediment features on the interstitial
Habitat Available for Macroinvertebrates in 15 French Streams. International Review
of Hydrobiology. 2003. 88, 77-93.
Gibson, S., et al. Vertical gradational variability of fines deposited in a gravel
Framework, Sedimentology. 2009. 56, 661- 676.
Herrero, A., Berni, C., Cemenen, B. Laboratory Analysis on silt infiltration into
Gravel Bed. In: E- Proceedings of the 36th IAHR World Congress, The Hague,
Netherlands. 2015.
Mayar, M.A., Wieprecht, S., Noak. Preliminary experiments to use gamma ray
attenuation for Undisturbed measurements of fine sediment infiltration mass. Proceedings of the 12th international Symposium on Ecohydraulics, Tokyo, Japan. 2018.
Noack, M., Ortlepp, J., and Wieprecht, S. An approach to simulate interstitial Habitat Conditions during the incubation phase of Gravel Spawning Fish. River research
and Application. 2017. 33, 192- 201.
Nourollah, S. Laboratory Investigation of sediment infiltration masses in
Rhombohedral packing Arrangement of spheres. Master Thesis, institute for
modeling Hydraulic and Environmental Systems, University of Stuttgart. 2019.
Taniwal, M. Zarif. General Geography of Afghanistan, Kabul University, Kabul,
Afghanistan. 2010, p 87.
Contents
ارزیابی ظرفیت نفوذپذیری آب در خاکهای قلعه زمان خان، شهرکابل 1