Ecology and regeneration of forest communities on the alluvial fan ...
Ecology and regeneration of forest communities on the alluvial fan ...
Ecology and regeneration of forest communities on the alluvial fan ...
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-Discussi<strong>on</strong>-<br />
5 Discussi<strong>on</strong><br />
5.1 Vegetati<strong>on</strong> z<strong>on</strong>ati<strong>on</strong> <str<strong>on</strong>g>and</str<strong>on</strong>g> site c<strong>on</strong>diti<strong>on</strong>s<br />
The observed <strong>alluvial</strong> <strong>fan</strong> is a ra<strong>the</strong>r diverse structured l<str<strong>on</strong>g>and</str<strong>on</strong>g>form generated by erosi<strong>on</strong><br />
<str<strong>on</strong>g>and</str<strong>on</strong>g> depositi<strong>on</strong> due to recurring inundati<strong>on</strong>. The map <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> vegetati<strong>on</strong> <str<strong>on</strong>g>communities</str<strong>on</strong>g><br />
(Fig. 5.1) shows a characteristic pattern <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> apparently following an<br />
altitudinal gradient.<br />
5 0 0 m<br />
Q<br />
a k h<br />
1<br />
b<br />
2<br />
a<br />
4 0 0 m<br />
3<br />
3 0 0 m<br />
N<br />
4 k m<br />
2 0 0 m<br />
r i v e r b e d<br />
Q u e r c u s i b e r i c a - C a r p i n u s o r i e n t a l i s<br />
Q u e r c u s r o b u r - C a r p i n u s b e t u l u s<br />
F r a x i n u s e x c e l s i o r - P t e r o c a r y a p t e r o c a r p a<br />
S w i d a s a n g u i n e a - P o p u l u s a l b a<br />
E q u i s e t u m t e l m a t e i a - A l n u s b a r b a t a<br />
O p l i s m e n u s u n d u l a t i f o l i u s - A c e r v e l u t i n u m<br />
r o a d<br />
S c l e r o p o a r i g i d a - P o p u l u s n i g r a<br />
r a i l r o a d<br />
P u n i c a g r a n a t a - P a l i u r u s s p i n a - c h r i s t i c r o s s - s e c t i o n<br />
v e r y l a r g e P o p u l u s a l b a<br />
c o n c r e t e e m b a n k m e n t<br />
a g r i c u l t u r e , p a s t u r e o r s m a l l f o r e s t p a t c h e s<br />
s e t t l e m e n t<br />
Fig. 5.1 Rough map <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> <strong>alluvial</strong> <strong>fan</strong> <str<strong>on</strong>g>and</str<strong>on</strong>g> <strong>the</strong> distributi<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> <str<strong>on</strong>g>forest</str<strong>on</strong>g> <str<strong>on</strong>g>communities</str<strong>on</strong>g> based <strong>on</strong> a satellite<br />
image (Google Earth 2008) Mixed st<str<strong>on</strong>g>and</str<strong>on</strong>g>s are depicted striped. The two <strong>fan</strong> cross secti<strong>on</strong>s are indicated by<br />
bold dashed lines ( ) with a = upper <strong>fan</strong>, b =lower <strong>fan</strong>. The three riverbed cross secti<strong>on</strong>s are indicated<br />
with 1 = upper <strong>fan</strong>, 2 = mid-<strong>fan</strong>, 3 =lower <strong>fan</strong>.<br />
This gradient was c<strong>on</strong>sidered highly significant within both c<strong>on</strong>ducted DCA analyses.<br />
Fur<strong>the</strong>r significant gradients revealed by both DCA were soil moisture <str<strong>on</strong>g>and</str<strong>on</strong>g> substrate<br />
compositi<strong>on</strong>. The correlati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> higher located sites to high fracti<strong>on</strong>s <str<strong>on</strong>g>of</str<strong>on</strong>g> coarse material<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 />
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