By Aleksey N. Kosarev, Andrey G. Kostianoy (auth.), Andrey G. Kostianoy, Aleksey N. Kosarev (eds.)
With extraordinary imaginative and prescient, Prof. Otto Hutzinger initiated The instruction manual of Envir- psychological Chemistry in 1980 and have become the founding Editor-in-Chief. at the moment, environmental chemistry was once an rising ?eld, aiming at an entire description of the Earth’s surroundings, encompassing the actual, chemical, organic, and geological modifications of chemicals taking place on an area in addition to a world scale. Environmental chemistry was once meant to supply an account of the impression of man’s actions at the typical setting through describing saw alterations. whereas a large amount of wisdom has been accrued over the past 3 many years, as re?ected within the greater than 70 volumes of The guide of Environmental Chemistry, there are nonetheless many scienti?c and coverage demanding situations forward end result of the complexity and interdisciplinary nature of the ?eld. The sequence will for that reason proceed to supply compilations of present wisdom. Contri- tions are written through best specialists with functional event of their ?elds. The instruction manual of Environmental Chemistry grows with the raises in our scienti?c figuring out, and gives a worthwhile resource not just for scientists but additionally for environmental managers and decision-makers. this present day, the sequence covers a vast variety of environmental subject matters from a chemical viewpoint, together with methodol- ical advances in environmental analytical chemistry.
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Extra resources for The Aral Sea Environment
Example text
2 Historical Evolution of the Aral Sea . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 Prehistory of the Aral Sea Basin . . . . . . . . . . . . . . . . . . . . . . . . . . . 2 History of the Aral Sea . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3 Geological Setting . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .
A chain of small islands borders it on the west; structurally it corresponds to a large tectonic uplift trending from south to north (Arkhangelsky’s swell). The maximum depths are confined to a deep trough in the west, close to the Ustyurt scarp. As for the bottom relief formation, deposition distinctly prevailed over erosion. Various constructional landforms occur all over the sea bottom, while abrasion landforms are mostly found along steeper western and northern coasts of the Aral. Another distinctive feature of the sea floor morphology is that relict subaerial landforms are usually well preserved and only slightly modified by marine processes [20].
References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . G. P. N. V. G. N. N. G. Kostianoy 1 Introduction The Aral Sea being a land-locked water basin having no connection with the World Ocean is, in fact, a lake. However, it can also be referred to as a sea if we take into account its size and oceanographic conditions. Not long ago (up to the 1960s) this was a unique natural feature: blue water in the midst of yellow desert sands.