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Ecology and regeneration of forest communities on the alluvial fan ...

Ecology and regeneration of forest communities on the alluvial fan ...

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-Study area-<br />

Alluvial <strong>fan</strong>s are typical l<str<strong>on</strong>g>and</str<strong>on</strong>g>forms <str<strong>on</strong>g>of</str<strong>on</strong>g> regi<strong>on</strong>s with a c<strong>on</strong>siderably high amount <str<strong>on</strong>g>of</str<strong>on</strong>g><br />

mechanical wea<strong>the</strong>ring. They are composed <str<strong>on</strong>g>of</str<strong>on</strong>g> fluvial sediments build up by means <str<strong>on</strong>g>of</str<strong>on</strong>g><br />

river sedimentati<strong>on</strong> processes (Fig. 2.3). They preferentially appear in semiarid areas, at<br />

<strong>the</strong> foot slopes <str<strong>on</strong>g>of</str<strong>on</strong>g> high mountain ranges <str<strong>on</strong>g>and</str<strong>on</strong>g> also in periglacial regi<strong>on</strong>s. Not <strong>the</strong> whole<br />

<strong>fan</strong> surface is active at a given time. Eventually, accumulati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> sediments downstream<br />

makes it easier for a new flood to flow over ano<strong>the</strong>r part <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> <strong>fan</strong>. This switch from<br />

<strong>on</strong>e part to ano<strong>the</strong>r is called avulsi<strong>on</strong>. The typical c<strong>on</strong>e shape <str<strong>on</strong>g>of</str<strong>on</strong>g> most <strong>alluvial</strong> <strong>fan</strong>s<br />

results from regular avulsi<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> river. Due to decreasing erosi<strong>on</strong> <str<strong>on</strong>g>and</str<strong>on</strong>g> transportati<strong>on</strong><br />

rates <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> rivers towards <strong>the</strong>ir distal margins a characteristic series <str<strong>on</strong>g>of</str<strong>on</strong>g> sediments is<br />

given. The coarsest material is dropped at <strong>the</strong> top <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> <strong>fan</strong>, s<str<strong>on</strong>g>and</str<strong>on</strong>g> <str<strong>on</strong>g>and</str<strong>on</strong>g> gravel in <strong>the</strong> mid<strong>fan</strong>,<br />

<str<strong>on</strong>g>and</str<strong>on</strong>g> fine material at <strong>the</strong> lower reaches (Ahnert 1996).<br />

Fig. 2.3 Outline <str<strong>on</strong>g>of</str<strong>on</strong>g> an <strong>alluvial</strong> <strong>fan</strong> (Strahler 1975)<br />

2.3 Climate<br />

The warm temperate climate <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> Alasan-Awtoran depressi<strong>on</strong> with sufficient rainfall<br />

during <strong>the</strong> whole vegetati<strong>on</strong> period provides excellent c<strong>on</strong>diti<strong>on</strong>s for <str<strong>on</strong>g>forest</str<strong>on</strong>g> growth. The<br />

Greater Caucasus mountain ranges protect it from cold wea<strong>the</strong>r <str<strong>on</strong>g>and</str<strong>on</strong>g> str<strong>on</strong>g winds.<br />

Durati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> vegetati<strong>on</strong> period varies between eight <str<strong>on</strong>g>and</str<strong>on</strong>g> ten m<strong>on</strong>ths. Spring, summer<br />

<str<strong>on</strong>g>and</str<strong>on</strong>g> fall receive each about <strong>on</strong>e third <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> annual rainfall. Mean temperature in January<br />

is 0°C, <strong>the</strong> mean temperatures in July range from 22,5°C to 25°C. The end <str<strong>on</strong>g>of</str<strong>on</strong>g> summer<br />

-<str<strong>on</strong>g>Ecology</str<strong>on</strong>g> <str<strong>on</strong>g>and</str<strong>on</strong>g> <str<strong>on</strong>g>regenerati<strong>on</strong></str<strong>on</strong>g> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>forest</str<strong>on</strong>g> <str<strong>on</strong>g>communities</str<strong>on</strong>g> <strong>on</strong> <strong>the</strong> <strong>alluvial</strong> <strong>fan</strong> near Qakh (Northwestern Azerbaijan)-<br />

5

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