С Википедије, слободне енциклопедије
Шљунак. Највеће зрно на слици је величине око 4 cm.

Шљунак је седиментна стена која се састоји од невезаних зрна одређене величине. У геологији, шљунак је било која растресита стена са заобљеним зрнима која су већа од 2 и мања од 75 милиметара.

Gravel is classified by particle size range and includes size classes from granule- to boulder-sized fragments. In the Udden-Wentworth scale gravel is categorized into granular gravel (2—4 mm or 0,079—0,157 in) and pebble gravel (4—64 mm or 0,2—2,5 in). ISO 14688 grades gravels as fine, medium, and coarse, with ranges 2–6.3 mm to 20–63 mm. One cubic metre of gravel typically weighs about 1,800 kg (or a cubic yard weighs about 3,000 lb).

Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as aggregate for concrete. Much of the rest is used for road construction, either in the road base or as the road surface (with or without asphalt or other binders.) Naturally occurring porous gravel deposits have a high hydraulic conductivity, making them important aquifers.

Дефиниција и својства[уреди | уреди извор]

Sand and gravel separator in a gravel pit in Germany

Colloquially, the term gravel is often used to describe a mixture of different size pieces of stone mixed with sand and possibly some clay.[1] The American construction industry distinguishes between gravel (a natural material) and crushed stone (produced artificially by mechanical crushing of rock.)[2][3][4]

The technical definition of gravel varies by region and by area of application. Many geologists define gravel simply as loose rounded rock particles over 2 mm (0,079 in) in diameter, without specifying an upper size limit.[5][6][7][8] Gravel is sometimes distinguished from rubble, which is loose rock particles in the same size range but angular in shape.[9] The Udden-Wentworth scale, widely used by geologists in the US, defines granular gravel as particles with a size from 2 to 4 mm (0,079 to 0,157 in) and pebble gravel as particles with a size from 4 to 64 mm (0,16 to 2,52 in). This corresponds to all particles with sizes between coarse sand and cobbles.[10]

The U.S. Department of Agriculture and the Soil Science Society of America define gravel as particles from 2 to 80 mm (0,079 to 3,150 in) in size, while the German scale (Atterburg) defines gravel as particles from 2 to 200 mm (0,079 to 7,874 in) in size.[11] The U.S. Army Corps of Engineers defines gravel as particles under 3 in (76 mm) in size that are retained by a number 4 mesh, which has a mesh spacing of 476 mm (18,7 in).[12][5] ISO 14688 for soil engineering grades gravels as fine, medium, and coarse with ranges 2 mm to 6.3 mm to 20 mm to 63 mm.[13]

The bulk density of gravel varies from 1.460 to 1.920 kg/m3 (2.460 to 3.240 lb/cu yd).[14] Natural gravel has a high hydraulic conductivity, sometimes reaching above 1 cm/s.[15]

Порекло[уреди | уреди извор]

Most gravel is derived from disintegration of bedrock as it weathers. Quartz is the most common mineral found in gravel, as it is hard, chemically inert, and lacks cleavage planes along which the rock easily splits. Most gravel particles consist of multiple mineral grains, since few rocks have mineral grains coarser than about 8 mm (0,31 in) in size. Exceptions include quartz veins, pegmatites, deep intrusions, and high-grade metamorphic rock. The rock fragments are rapidly rounded as they are transported by rivers, often within a few tens of kilometers of their source outcrops.[16]

Gravel is deposited as gravel blankets or bars in stream channels;[17] in alluvial fans;[18] in near-shore marine settings, where the gravel is supplied by streams or erosion along the coast;[19][20][17] and in the deltas of swift-flowing streams.[21] The upper Mississippi embayment contains extensive chert gravels thought to have their origin less than 100 mi (160 km) from the periphery of the embayment.[22]

It has been suggested that wind-formed (aeolian) gravel "megaripples" in Argentina have counterparts on the planet Mars.[23]

Производња и употреба[уреди | уреди извор]

A gravel road in Finland

Gravel is a major basic raw material in construction.[24] Sand is not usually distinguished from gravel in official statistics, but crushed stone is treated as a separate category. In 2020, sand and gravel together made up 23% of all industrial mineral production in the U.S., with a total value of about $12.6 billion. Some 960 million tons of construction sand and gravel were produced. This greatly exceeds production of industrial sand and gravel (68 million tons), which is mostly sand rather than gravel.[25]

It is estimated that almost half of construction sand and gravel is used as aggregate for concrete. Other important uses include in road construction, as road base or in blacktop; as construction fill; and in myriad minor uses.[24]

Gravel is widely and plentifully distributed, mostly as river deposits, river flood plains, and glacial deposits, so that environmental considerations and quality dictate whether alternatives, such as crushed stone, are more economical. Crushed stone is already displacing natural gravel in the eastern United States, and recycled gravel is also becoming increasingly important.[25]

Етимологија[уреди | уреди извор]

The word gravel comes from the Old French gravele[26] or gravelle.[27]

Типови[уреди | уреди извор]

Naturally occurring sedimentary gravel bed
Graded mechanically crushed stone, with particle sizes roughly between 5 and 15 mm

Types of gravel include:

  • Bank gravel: naturally deposited gravel intermixed with sand or clay found in and next to rivers and streams. Also known as "bank run" or "river run".[28]
  • Bench gravel: a bed of gravel located on the side of a valley above the present stream bottom, indicating the former location of the stream bed when it was at a higher level. The term is most commonly used in Alaska and the Yukon Territory.[29]
  • Crushed stone: rock crushed and graded by screens and then mixed to a blend of stones and fines. It is widely used as a surfacing for roads and driveways, sometimes with tar applied over it. Crushed stone may be made from granite, limestone, dolomite, and other rocks. Also known as "crusher run", DGA (dense grade aggregate) QP (quarry process), and shoulder stone.[30] Crushed stone is distinguished from gravel by the U.S. Geological Survey.[25]
  • Fine gravel: gravel consisting of particles with a diameter of 2 to 63 mm (0,079 to 2,480 in)[13]
  • Stone dust: fine, crushed, gravel from the final stage of screen separation, such that the gravel is not separated out from fine dust particles. As with other forms of crushed stone, this is distinguished from gravel by the U.S. Geological Survey.[25]
  • Lag gravel: a surface accumulation of coarse gravel produced by the removal of finer particles.
  • Pay gravel: also known as "pay dirt"; a nickname for gravel with a high concentration of gold and other precious metals. The metals are recovered through gold panning.
  • Pea gravel: also known as "pea shingle" is clean gravel similar in size to garden peas.[31] Used for concrete surfaces, walkways, driveways and as a substrate in home aquariums.
  • Piedmont gravel: a coarse gravel carried down from high places by mountain streams and deposited on relatively flat ground, where the water runs more slowly.[32]
  • Plateau gravel: a layer of gravel on a plateau or other region above the height at which stream-terrace gravel is usually found.[33]

Однос према биљном животу[уреди | уреди извор]

In locales where gravelly soil is predominant, plant life is generally more sparse.[34] This is due to the inferior ability of gravels to retain moisture, as well as the corresponding paucity of mineral nutrients, since finer soils that contain such minerals are present in smaller amounts.

У геолошком запису[уреди | уреди извор]

Sediments containing over 30% gravel that become lithified into solid rock are termed conglomerate.[6] Conglomerates are widely distributed in sedimentary rock of all ages, but usually as a minor component, making up less than 1% of all sedimentary rock.[7] Alluvial fans likely contain the largest accumulations of gravel in the geologic record.[18] These include conglomerates of the Triassic basins of eastern North America and the New Red Sandstone of south Devon.[35]

Сепарација[уреди | уреди извор]

Шљунак је најкоришћенији материјал у грађевинарству. У зависности од примене јављају се потребе за употребом шљунка чија зрна припадају одређеном опсегу величина. Такав шљунак се добија просејавањем, односно сепарацијом.

На тај начин шљунак се процесом сепарирања разврстава у групе које се називају сепарације.

У Србији се шљунак, најчешће, добија ископом материјала из речног корита. Након прања такав шљунак се неформално назива „природни шљунак“, чијом сепарацијом добијамо следеће групе:

  • Сепарација 1: (песак) 0 до 4 mm
  • Сепарација 2: 4 до 8 mm
  • Сепарација 3: 8 до 16 mm
  • Сепарација 4: 16 до 32 mm и
  • Сепарација 5 (иберлауф): дијаметра преко 32 mm.

Сепарацијом 1 m³ природног шљунка добија се запремина производа која је већа од 1 m³. Просечна специфична маса природног шљунка је ρ = 1800 kg/m³, док су специфичне масе сепарација следеће:

  • Сепарација 1: 1450 kg/m³
  • Сепарација 2: 1520 kg/m³
  • Сепарација 3: 1550 kg/m³
  • Сепарација 4: 1550 kg/m³
  • Сепарација 5: 1500 kg/m³.

Види још[уреди | уреди извор]

Референце[уреди | уреди извор]

  1. ^ „gravel”. Oxford English Dictionary (3rd изд.). Oxford University Press. септембар 2005.  (Потребна је претплата или чланска картица јавне библиотеке УК.)
  2. ^ Dolley, Thomas P. (2021). „Sand and gravel (construction)”. U.S. Geological Survey Mineral Commodies Summary: 141. doi:10.3133/mcs2021. 
  3. ^ „The complete guide to crushed stone and gravel”. Gra-Rock. 16. 6. 2020. Приступљено 24. 11. 2021. 
  4. ^ „Crushed stone vs. gravel”. A.L.Blair Construction Ltd. 24. 10. 2017. Приступљено 24. 11. 2021. 
  5. ^ а б Jackson, Julia A., ур. (1997). „gravel”. Glossary of geology. (Fourth изд.). Alexandria, Viriginia: American Geological Institute. ISBN 0922152349. 
  6. ^ а б Blatt, Harvey; Tracy, Robert J. (1996). Petrology : igneous, sedimentary, and metamorphic. (2nd изд.). New York: W.H. Freeman. стр. 523. ISBN 0716724383. 
  7. ^ а б Boggs, Sam (2006). Principles of sedimentology and stratigraphy (4th изд.). Upper Saddle River, N.J.: Pearson Prentice Hall. стр. 135. ISBN 0131547283. 
  8. ^ Allaby, Michael (2013). „gravel”. A dictionary of geology and earth sciences (Fourth изд.). Oxford: Oxford University Press. ISBN 9780199653065. 
  9. ^ Prothero, Donald R.; Schwab, Fred (2004). Sedimentary geology : an introduction to sedimentary rocks and stratigraphy (2nd изд.). New York: W.H. Freeman. стр. 67. ISBN 0-7167-3905-4. 
  10. ^ Krumbein, W. C. (1934). „Size frequency distributions of sediments”. Journal of Sedimentary Petrology. 2 (4). doi:10.1306/D4268EB9-2B26-11D7-8648000102C1865D. 
  11. ^ Blatt, Harvey; Middletone, Gerard; Murray, Raymond (1980). Origin of sedimentary rocks (2d изд.). Englewood Cliffs, N.J.: Prentice-Hall. стр. 57. ISBN 0136427103. 
  12. ^ Blatt, Harvey; Middletone, Gerard; Murray, Raymond (1980). Origin of sedimentary rocks (2d изд.). Englewood Cliffs, N.J.: Prentice-Hall. стр. 631. ISBN 0136427103. 
  13. ^ а б „ISO 14688-1:2002 – Geotechnical investigation and testing – Identification and classification of soil – Part 1: Identification and description”. ISO. 
  14. ^ Hartman, H L., ур. (1992). Society for mining, metallurgy and exploration (SME) Mining Engineering Handbook. 2 (2nd изд.). Littleton, Colorado, USA: Society for mining, metallurgy and exploration (SME). ISBN 978-0873351003. 
  15. ^ Freeze, R. Allan (1979). Groundwater. Cherry, John A. Englewood Cliffs, N.J.: Prentice-Hall. ISBN 0-13-365312-9. OCLC 4493153. 
  16. ^ Prothero & Schwab 2004, стр. 68-70.
  17. ^ а б Prothero & Schwab 2004, стр. 74.
  18. ^ а б Leeder, Mike (2011). Sedimentology and sedimentary basins : from turbulence to tectonics (2nd изд.). Chichester, West Sussex, UK: Wiley-Blackwell. стр. 290. ISBN 9781405177832. 
  19. ^ Jennings, S.; Smyth, C. (јануар 1990). „Holocene evolution of the gravel coastline of East Sussex”. Proceedings of the Geologists' Association. 101 (3): 213—224. doi:10.1016/S0016-7878(08)80006-5. 
  20. ^ Bridgland, D. R.; Saville, A.; Sinclair, J. M. (јун 1997). „New evidence for the origin of the Buchan Ridge Gravel, Aberdeenshire”. Scottish Journal of Geology. 33 (1): 43—50. S2CID 129225730. doi:10.1144/sjg33010043. 
  21. ^ Cary, Allen S. (јануар 1951). „Origin and Significance of Openwork Gravel”. Transactions of the American Society of Civil Engineers. 116 (1): 1296—1308. doi:10.1061/TACEAT.0006486. 
  22. ^ Potter, Paul Edwin (јануар 1955). „The Petrology and Origin of the Lafayette Gravel: Part 1. Mineralogy and Petrology”. The Journal of Geology. 63 (1): 1—38. Bibcode:1955JG.....63....1P. S2CID 128550835. doi:10.1086/626223. 
  23. ^ de Silva, S. L.; Spagnuolo, M. G.; Bridges, N. T.; Zimbelman, J. R. (1. 11. 2013). „Gravel-mantled megaripples of the Argentinean Puna: A model for their origin and growth with implications for Mars”. Geological Society of America Bulletin. 125 (11–12): 1912—1929. Bibcode:2013GSAB..125.1912D. doi:10.1130/B30916.1. 
  24. ^ а б Bolen, W.P. (2000). „Sand and gravel construction” (PDF). US Geological Survey Minerals Yearbook. Приступљено 26. 7. 2021. 
  25. ^ а б в г U.S. Geological Survey (2021). „Mineral Commodity Summaries”: 141—143. doi:10.3133/mcs2021Слободан приступ. 
  26. ^ Collins English Dictionary – Complete & Unabridged 11th Edition. Retrieved 30 August 2012 from CollinsDictionary.com website:http://www.collinsdictionary.com/dictionary/english/gravel
  27. ^ Gravel, n., Oxford English Dictionary Second Edition on CD-ROM (v. 4.0) © Oxford University Press 2009
  28. ^ Jackson 1997, "bank gravel".
  29. ^ Jackson 1997, "bench gravel".
  30. ^ „Quarry Process – QP, DGA – NJ, NY, NYC, PA”. braenstone.com. 
  31. ^ Jackson 1997, "pea gravel".
  32. ^ Jackson 1997, "piedmont gravel".
  33. ^ Jackson 1997, "plateau gravel".
  34. ^ C.Michael Hogan. 2010. Abiotic factor. Encyclopedia of Earth. eds Emily Monosson and C. Cleveland. National Council for Science and the Environment Архивирано 8 јун 2013 на сајту Wayback Machine. Washington DC
  35. ^ Blatt, Middleton & Murray 1980, стр. 631.

Литература[уреди | уреди извор]

  • Ђорђевић В., Ђорђевић П., Миловановић Д. 1991. Основи петрологије. Београд: Наука

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