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Siltation

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440:. When sediments are placed on or near beaches in order to replenish an eroding beach, any fines in the material will continue to be washed out for as long as the sand is being reworked. Since all replenished beaches are eroding or they would not need replenishment, they will contribute to nearshore siltation almost for as long as it takes to erode away what was added, albeit with somewhat decreasing intensity over time. Since the leakage is detrimental to coral reefs, the practice leads to a direct conflict between the public interest of saving beaches, and preserving any nearshore coral reefs. To minimize the conflict, beach replenishment should not be done with sand containing any silt or clay fractions. In practice the sand is often taken from offshore areas, and since the proportion of fines in sediments typically increases in the offshore direction, the deposited sand will inevitably contain a significant percentage of siltation-contributing fines. 837: 117: 1533: 279:, correlating turbidity to sediment concentration (using a regression developed from water samples that are filtered, dried, and weighed), multiplying the concentration with the discharge as above, and integrating over the entire plume. To distinguish the spill contribution, the background turbidity is subtracted from the spill plume turbidity. Since the spill plume in open water varies in space and time, an integration over the entire plume is required, and repeated many times to get acceptably low uncertainty in the results. The measurements are made close to the source, in the order of a few hundred meters. 69: 89: 417: 1559: 1547: 20: 312: 1165: 200: 147:. The result will be an increased amount of silt and clay in the water bodies that drain the area. In urban areas, the erosion source is typically construction activities, which involve clearing the original land-covering vegetation and temporarily creating something akin to an urban desert from which fines are easily washed out during rainstorms. 443:
It is desirable to minimize the siltation of irrigation channels by hydrologic design, the objective being not to create zones with falling sediment transport capacity, as that is conducive to sedimentation. Once sedimentation has occurred, in irrigation or navigation channels, dredging is often the
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While the effect of the siltation on the biota (once the harm is already done) can be studied by repeated inspection of selected test plots, the magnitude of the siltation process in the impact area may be measured directly by monitoring in real time. Parameters to measure are sediment accumulation,
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bottom communities since empirical data show that fish effectively avoid the impacted area. The siltation affects the bottom community in two main ways. The suspended sediment may interfere with the food gathering of filtering organisms, and the sediment accumulation on the bottom may bury organisms
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polyps. Generally speaking, hard bottom communities and mussel banks (including oysters) are more sensitive to siltation than sand and mud bottoms. Unlike in the sea, in a stream, the plume will cover the entire channel, except possibly for backwaters, and so fish will also be directly affected in
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During dredging, the spill can be minimized but not eliminated completely by the way the dredger is designed and operated. If the material is deposited on land, efficient sedimentation basins can be constructed. If it is dumped into relatively deep water, there will be a significant spill during
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One may distinguish between measurements at the source, during transport, and within the affected area. Source measurements of erosion may be very difficult since the lost material may be a fraction of a millimeter per year. Therefore, the approach taken is typically to measure the sediment in
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to the point that they starve or even die. It is only if the concentration is extreme that it decreases the light level sufficiently for impacting primary productivity. An accumulation of as little as 1 mm (0.039 in) may kill coral polyps.
49:. It refers both to the increased concentration of suspended sediments and to the increased accumulation (temporary or permanent) of fine sediments on bottoms where they are undesirable. Siltation is most often caused by 424:
In rural areas, the first line of defense is to maintain land cover and prevent soil erosion in the first place. The second line of defense is to trap the material before it reaches the stream network (known as
429:). In urban areas, the defenses are to keep land uncovered for as short a time as possible during construction and to use silt screens to prevent the sediment from getting released in water bodies. 219:, it acts as a pollutant for those who require clean water, such as for cooling or in industrial processes, and it includes aquatic life that are sensitive to suspended material in the water. While 463:"The International Journal of Climate Change: Impacts and Responses » Rate of Siltation in Wular Lake, (Jammu and Kashmir, India) with Special Emphasis on its Climate & Tectonics" 243:
Siltation can also affect navigation channels or irrigation channels. It refers to the undesired accumulation of sediments in channels intended for vessels or for distributing water.
154:, the transportation of dredged material on barges, and the deposition of dredged material in or near water. Such deposition may be made to get rid of unwanted material, such as the 996: 1488: 252: 282:
Anything beyond a work area buffer zone for sediment spill is considered the potential impact area. In the open sea, the impact of concern is almost exclusively with the
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Also, sediment spill is better measured in transport than at the source. The sediment transport in open water is estimated by measuring the
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dumping but not thereafter, and the spill that arises has minimal impact if there are only fine-sediment bottoms nearby.
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of material dredged from harbours and navigation channels. The deposition may also be to build up the coastline, for
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The origin of the increased sediment transport into an area may be erosion on land or activities in the water.
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10 lb/cu in) times 30 m/s (1,100 cu ft/s) gives 1.5 kg/s (200 lb/min).
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One of the most difficult conflicts of interest to resolve, as regards siltation mitigation, is perhaps
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transport in the stream, by measuring the sediment concentration and multiplying that with the
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Siltation of the magnitude that it affects shipping can also be monitored by repeated
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turbidity at the level of the filtering biota, and optionally incident light.
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collected from pit latrines and dumped into a river at the Korogocho slum in
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Resuspension of fines from a replenished beach causing siltation offshore
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organisms have no way of escape. Among the most sensitive organisms are
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that are discharged from households or business establishments with no
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Water pollution caused by particulate terrestrial clastic material
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by intensive or inadequate agricultural practices, leading to
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have been found to avoid spill plumes in the water (e.g. the
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In water, the main pollution source is sediment spill from
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Siltation Monitoring Plan excerpt, retrieved 2010-07-11,
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It is sometimes referred to by the ambiguous term "
1575: 135:In rural areas, the erosion source is typically 797:Stable isotope analysis in aquatic ecosystems 507: 246: 175:Another important cause of siltation is the 41:material, with a particle size dominated by 862:Freshwater environmental quality parameters 340:. Unsourced material may be challenged and 143:, especially in fine-grained soils such as 514: 500: 460: 404:Learn how and when to remove this message 415: 250: 198: 115: 87: 67: 18: 120:Siltation caused by sewage sludge from 1576: 521: 484:http://lindorm.com/beaches/sedmon2.php 1050: 1049: 533: 495: 338:adding citations to reliable sources 305: 1125:Oceanic physical-biological process 987:List of freshwater ecoregions (WWF) 227:project during the building of the 13: 203:Silted river polluted by sediment. 194: 14: 1605: 255:A sensor for measuring siltation 1558: 1557: 1545: 1531: 1163: 835: 652:Colored dissolved organic matter 310: 268:; for example, 50 mg/L (1.8 997:Latin America and the Caribbean 191:facilities to bodies of water. 1479:Ecological values of mangroves 1022:North Pacific Subtropical Gyre 476: 454: 172:also affects siltation rates. 1: 447: 301: 1499:Marine conservation activism 1484:Fisheries and climate change 7: 1494:Human impact on marine life 1371:Davidson Seamount § Ecology 607:Aquatic population dynamics 461:U.D. Kulkarni; et al. 10: 1610: 247:Measurement and monitoring 1525: 1464: 1336: 1272: 1234: 1181: 1172: 1161: 1110:Marine primary production 1062: 1058: 1045: 1004:List of marine ecoregions 979: 844: 833: 547: 543: 529: 63: 1356:Coastal biogeomorphology 1351:Marine coastal ecosystem 225:environmental monitoring 1264:Paradox of the plankton 1075:Diel vertical migration 969:Freshwater swamp forest 687:GIS and aquatic science 535:General components and 23:Siltation of a waterway 1090:Large marine ecosystem 782:Shoaling and schooling 421: 260: 204: 129: 113: 85: 34:caused by particulate 24: 1509:Marine protected area 1436:Salt pannes and pools 1211:Marine larval ecology 1186:Census of Marine Life 1070:Deep scattering layer 1027:San Francisco Estuary 992:Africa and Madagascar 817:Underwater camouflage 597:Aquatic biomonitoring 537:freshwater ecosystems 419: 254: 202: 119: 91: 71: 22: 1244:Marine bacteriophage 1206:Marine invertebrates 334:improve this section 189:wastewater treatment 110:Calexico, California 92:Siltation caused by 72:Siltation caused by 1120:Ocean fertilization 929:Trophic state index 887:Lake stratification 617:Aquatic respiration 164:beach replenishment 53:or sediment spill. 1386:Intertidal wetland 1381:Intertidal ecology 1249:Marine prokaryotes 1191:Deep-sea community 1085:Iron fertilization 1008:Specific examples 934:Upland and lowland 852:Freshwater biology 717:Microbial food web 627:Aquatic toxicology 570:Aquatic adaptation 523:Aquatic ecosystems 422: 261: 205: 160:artificial islands 130: 114: 104:as it passes from 86: 58:sediment pollution 25: 1571: 1570: 1552:Oceans portal 1521: 1520: 1517: 1516: 1396:Hydrothermal vent 1332: 1331: 1221:Seashore wildlife 1052:Marine ecosystems 1041: 1040: 1037: 1036: 807:Thermal pollution 772:Ramsar Convention 712:Microbial ecology 672:Fisheries science 612:Aquatic predation 438:beach nourishment 414: 413: 406: 388: 94:raw sewage sludge 1601: 1561: 1560: 1554: 1550: 1549: 1540: 1538:Lakes portal 1536: 1535: 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605: 603: 602:Aquatic plant 600: 598: 595: 591: 588: 586: 583: 581: 578: 577: 576: 573: 571: 568: 566: 565:Anoxic waters 563: 561: 558: 556: 553: 552: 550: 546: 542: 538: 532: 528: 524: 517: 512: 510: 505: 503: 498: 497: 494: 485: 479: 464: 457: 453: 445: 444:only remedy. 441: 439: 434: 430: 428: 418: 408: 405: 397: 394:February 2019 386: 383: 379: 376: 372: 369: 365: 362: 358: 355: –  354: 350: 349:Find sources: 343: 339: 335: 329: 328: 324: 319:This section 317: 313: 308: 307: 299: 297: 292: 288: 285: 280: 278: 273: 267: 258: 253: 244: 241: 238: 234: 231:), filtering 230: 226: 222: 218: 214: 210: 201: 192: 190: 186: 182: 178: 173: 171: 167: 165: 161: 157: 153: 148: 146: 142: 138: 133: 127: 123: 118: 111: 107: 103: 99: 95: 90: 83: 79: 75: 70: 61: 59: 54: 52: 48: 44: 40: 37: 33: 29: 21: 1466:Conservation 1317:Pelagic fish 1297:Coastal fish 1201:Marine fungi 939:Water garden 822:Water column 786: 767:Productivity 742:Pelagic zone 702:Macrobenthos 692:Hydrobiology 662:Ecohydrology 478: 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Index


water pollution
terrestrial
clastic
silt
clay
soil erosion

fecal sludge
Nairobi
Kenya

raw sewage sludge
industrial waste
New River
Mexicali
Calexico, California

shipyard
Rio de Janeiro
soil degradation
soil erosion
loess
dredging
offshore dumping
artificial islands
beach replenishment
Climate change
septage
sewage sludges

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