Estuary (tidal): Difference between revisions
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|Description=The estuary of a river is the transitional zone between the freshwater river environment and the sea. They are very dynamic places as they have both marine influences, such as tides, waves, and saline water; and riverine influences, such as flows of fresh water and sediment. The inflow of both seawater and freshwater provide high levels of nutrients in both the water column and sediment, making estuaries | |Description=The estuary of a river is the transitional zone between the freshwater river environment and the sea. They are very dynamic places as they have both marine influences, such as tides, waves, and saline water; and riverine influences, such as flows of fresh water and sediment. The inflow of both seawater and freshwater provide high levels of nutrients in both the water column and sediment, making estuaries very productive natural habitats. They are very important feeding and nursery areas for fish, birds and many specially adapted plants and invertebrates make estuaries their home. [http://en.wikipedia.org/wiki/Estuary Estuary] | ||
The uppermost limit is most easily defined as mean high water spring. The bottom of the estuary can be defined as headland to headland. You can also use salinity and all coastal water in the UK are euhaline, i.e. > 30 ppt. | The uppermost limit is most easily defined as mean high water spring. The bottom of the estuary can be defined as headland to headland. You can also use salinity and all coastal water in the UK are euhaline, i.e. > 30 ppt. | ||
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1) At a physical barrier (e.g. a weir) | 1) At a physical barrier (e.g. a weir) | ||
2) If there is no physical barrier then the chloride content should not exceed 200 mg/l at high water of mean spring tides and during low freshwater flow. | 2) If there is no physical barrier then the chloride content should not exceed 200 mg/l at high water of mean spring tides and during low freshwater flow. | ||
3) If there is no physical barrier and no appropriate data for (2) then we use the mean high-water mark as given in Ordnance Survey 10K maps. | 3) If there is no physical barrier and no appropriate data for (2) then we use the mean high-water mark as given in Ordnance Survey 10K maps. | ||
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Latest revision as of 17:20, 22 August 2012
The estuary of a river is the transitional zone between the freshwater river environment and the sea. They are very dynamic places as they have both marine influences, such as tides, waves, and saline water; and riverine influences, such as flows of fresh water and sediment. The inflow of both seawater and freshwater provide high levels of nutrients in both the water column and sediment, making estuaries very productive natural habitats. They are very important feeding and nursery areas for fish, birds and many specially adapted plants and invertebrates make estuaries their home. Estuary
The uppermost limit is most easily defined as mean high water spring. The bottom of the estuary can be defined as headland to headland. You can also use salinity and all coastal water in the UK are euhaline, i.e. > 30 ppt.
In England and Wales for the Water Framework Directive the freshwater limits of transitional water bodies were determined in this manner: 1) At a physical barrier (e.g. a weir) 2) If there is no physical barrier then the chloride content should not exceed 200 mg/l at high water of mean spring tides and during low freshwater flow. 3) If there is no physical barrier and no appropriate data for (2) then we use the mean high-water mark as given in Ordnance Survey 10K maps.
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