Английский Язык - Турецкий язык
Определение silting в Английский Язык Турецкий язык словарь
- siltasyon
- siltlenme
- silt
- toz
- silt
- (Mukavele) mil, balçık, suyun getirip biriktirdiği kum veya çamur
- silt
- (Madencilik) kum tabakası
- silt
- suyun getirip biriktirdiği kum veya çamur
- silt
- (Madencilik) çakıl tabakası
- silt
- ince kum
- silt
- alüvyon
Büyük nehir, alüvyonla kararmıştı.
-The great river was dark with silt.
- silt
- balçık
- silt
- mil
- silt
- {i} çökelme sonucu oluşan çamur ve kum tabakası
- silt
- {f} up kum ve çamurla doldurmak/dolmak
- silt
- lığ
- silt
- (isim) alüvyon
- silt
- silt tıkan/tıka
- silt
- dane boyu (çapı) 0.0004-0.0063 mm olan kayaç kırıntıları
- silt
- up ile böyle kum ve çamurla doldurmak veya dolmak
- silt
- silt
Связанные Термины
Турецкий язык - Турецкий язык
Определение silting в Турецкий язык Турецкий язык словарь
- silt
- inorganik karakterli çökelti
Связанные Термины
Английский Язык - Английский Язык
Определение silting в Английский Язык Английский Язык словарь
- The process whereby waterways become choked by mud and soil that has washed off the land through erosion
- The deposition of silt from a body of standing water; choking, filling, or covering by stream-deposited silt that occurs in a place of retarded flow or behind a dam or reservoir The term often includes particles from clay to sand-size
- A failure generally associated with a valve which movements are restricted due to small particles that have wedged in between critical clearances (e g , the spool and bore )
- silt
- Material with similar physical characteristics, whatever its origins or transport
- silt
- To clog or fill with silt
- silt
- To become clogged with silt
- silt
- Sedimentary materials composed of fine mineral particles with diameters ranging from 0 0002 to 0 05 mm
- silt
- soil type composed of extremely fine sediment particles
- silt
- {f} fill or obstruct with silt; become filled with or obstructed by silt
- silt
- Sedimentary particles smaller than sand particles, but larger than clay particles
- silt
- A rock fragment or mineral particle with a diameter of 1/16 mm to 1/256 mm, smaller than a very fine sand grain and larger than coarse clay
- silt
- Soil particles having diameters between 0 004 and 0 062 mm (millimeters) Sometimes they may be too small to be trapped by the circulation system In those cases, a clarifier or an alum product may be needed
- silt
- mud or clay or small rocks deposited by a river or lake
- silt
- 1 Particles between 0 05 and 0 002 mm diameter, or a soil textural class 2 Mineral particles that range in diameter from 0 02 to 0 002 mm in the International System, or 0 05 to 0 002 mm in the USDA system
- silt
- Fine particles of sand or rock that can be picked up by the air or water and deposited as sediment
- silt
- Fine particles of soil suspended or deposited in water and streams, usually from upstream erosion
- silt
- -Fine soil particles in the size range 0 02 - 0 002 mm
- silt
- – Soil inorganic particles in the 0 002-0 02 mm size range, smaller than sand but larger than clay Silt, which washes off the land into a body of water, can settle out of the water and smother benthic organisms such as oysters
- silt
- As a soil separate, individual mineral particles that range in diameter from the upper limit of clay (0 002 millimeter) to the lower limit of very fine sand (0 05 millimeter) As a soil textural class, soil that is 80 percent or more silt and less than 12 percent clay
- silt
- A sedimentary material composed of fine mineral particles intermediate in size between sand and clay
- silt
- {i} fine particles of sand and other earthy matter which are carried and deposited by water
- silt
- Soil particles with diameter between 0 053 and 0 002 mm
- silt
- become chocked with silt; "The river silted up"
- silt
- Mud or fine earth deposited from running or standing water
- silt
- As a soil separate, individual mineral particles that range in diameter from the upper limit of clay (0 002 millimeter) to the lower limit of very fine sand (0 05 millimeter) As a soil textural class, soil that is 80 percent or more silt and less than 12 percent clay
- silt
- Silt falls between sand and clay on a scale of particle size at about 002 to 05 mm across Silt is fragments of minerals and rock and is thus an inorganic component of soil
- silt
- Contaminant particles 5 µm and less in size
- silt
- Silt is fine sand, soil, or mud which is carried along by a river. The lake was almost solid with silt and vegetation. sand, mud, soil etc that is carried in water and then settles at a bend in a river, an entrance to a port etc (Probably from a language). silt up if something silts up or is silted up, it becomes filled with silt. Sediment particles
- silt
- A soil separate consisting of particles between 0 063 and 0 002mm in equivalent diameter (UK classification)
- silt
- Sedimentary materials composed of fine or intermediate-sized mineral particles
- silt
- Mineral soil particles 002 to 05 mm in size
- silt
- Sediment particles with a grain size between 0 004 mm and 0 062 mm, i e coarser than clay particles but finer than sand
- silt
- Mineral particle with a size between 0 004 and 0 06 millimeters in diameter Also see clay and sand
- silt
- To flow through crevices; to percolate
- silt
- fine particles of soil that can be picked up by air or water and deposited as sediment
- silt
- To choke, fill, or obstruct with silt or mud
- silt
- Fragments of rock or organic matter sediment most of the individual particles of which are between 1/16 and 1/256 millimeters (0 05 and 0 002 millimeters) in diameter A soil texture type consisting of 80 percent or more of silt particles and less than 12 percent clay particles
- silt
- 00016-0.0024 in. (0.004-0.06 mm) in diameter, regardless of mineral type. Silt is easily transported by moving currents but settles in still water. An unconsolidated aggregate of silt particles is also called silt, whereas a consolidated aggregate is called siltstone. Silt deposits formed by wind are known as loess. Sediments are seldom composed entirely of silt but rather are a mixture of clay, silt, and sand. Clay-rich silt, upon consolidation, frequently develops parting along bedding surfaces and is then called shale. If parting does not develop, the massive rock is called mudstone
- silt
- fine rock particles, 0 004-0 08 mm (0 00015-0 003 inches) in diameter