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Titlebook: Estuaries; Peter J. Wangersky Book 2006 Springer-Verlag Berlin Heidelberg 2006 biogeochemistry.chemistry.environment.environmental protect

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Book 2006of these rivers have been altered by dams or diversions; the results of these changes on the nature of the estuary are also discussed, where such data is available. In the case of the Tasmanian rivers, the estuary of the Huon, a largely untouched river, is contrasted with that of the Derwent, a rive
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,The São Francisco Estuary, Brazil,uth Atlantic. The estuary (Lat.10°36′S Long. 36° 23′W) is fed by the humid to semiarid SF river basin (AB = 634 × 10. km.,L = 2700 km), the second largest of Brazil‘s territory. Since the 1950s, SF hasevolved into a unique system almost solely impacted by a cascade of dams, which now control98% of t
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The Mackenzie Estuary of the Arctic Ocean,trongly modulated seasonal cycle. Ice cover plays a crucial role in the physical setting by limiting air--sea interaction (energy and gas exchange), reducing mixing, and withdrawing freshwater from the estuary while leaving behind the bulk of the dissolved components. Few studies have been conducted
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Biogeochemistry and Chemical Contamination in the St. Lawrence Estuary,ndward part of the estuary is relatively shallow with a partially mixed poorly productive water column and high turbidity. The seaward portion of the estuary is deep with a permanently stratified water column. It is substantially more productive and the turbidity is low. In recent years, research on
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The Nile Estuary,At the point of discharge of the Nile into the Mediterranean, the great Nile delta has formed and furnishes the most fertile area for cultivation in the Egyptian territory. The delta is embraced by two large branches of the Nile (the Rosetta and Damietta branches and their promontories), as the nort
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