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4.
b`xR f~wgiƒc we‡klb- 1964
mv‡j ÷ªjvi b`xR f~wgiƒc†K mvavibZ wbgœwjwLZ wZb fv‡e we‡klb K‡ib - 1| b`xAeevwnKvi mij ˆiwLK cÖK…wZ, 2| b`xAeevwnKvi AvqZwbK cÖK…wZ I 3| b`xgvjv AeevwnKv Ges b`x LvZ RvwjKv eÜziZv| 1| b`xAeevwnKvi mij ˆiwLK cÖK…wZt A) U‡cvjwR‡Kj `„wó‡KvY-- b`x ch©vq µg (Order) wØfvRb AbycvZ(bifurcation ratio) Av) R¨vwgwZ¨K `„wó‡KvY b`xi ˆ`N©¨ (Stream Length) b`xi Mo ˆ`N©¨( Average Stream Length) b`xi ‰`N¨©AbycvZ(Stream -Length Ratio) AeevwnKvi AwfKl© †K›`ª †_‡K `yiZ¡ (The Distance to the centre of Gravity of the Drainage Basin) `xN©¨Zg AeevwnKvi e¨v‡mi ˆ`N©¨ b`xi ˆ`N©¨ I DcZ¨Kv ˆ`‡N©¨iAbycvZ
5.
b`x AeevwnKvi AvqZwbK
we‡klb (Areal aspects of the Basin) K) b`x AeevwnKvi AvqZb (Area of the Basin) L) AeevwnKvi b`x NbZ¡ (Drainage Density of the Basin) M) AeevwnKv I AvqZ‡bi cvi¯úvwiK cv_©K¨ (Basin –Area Ratio) N) AeevwnKvi AvK…wZ (Shape of the Basin) b`x gvjv AeevwnKv Ges b`x LvZ RvwjKv eÜziZv(Relief aspects of the Basin) K) b`x Lv‡Zi Xvj L)AeevwnKvi Xvj M) AeevwnKv eÜziZv N) b`x ˆ`N©¨I Xv‡ji m¤úK©
6.
7.
K) b`x ch©vqµg
(Order) mvs¸ b ` x e v›` i e vb c Ö_ g c h ©vq 2 q c h ©vq 3 q c h ©vq 4 _ ©c h ©vq nU©‡bi b`x ch©vq µg
8.
mvs¸ b `
x e v›` i e vb c Ö_ g c h ©vq 2 q c h ©vq 3 q c h ©vq 4 _ ©c h ©vq StrahlerGi b`x ch©vq µg
9.
mvs¸ b `
x e v›` i e vb 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 12 2 2 2 2 2 2 2 5 14 18 28 19 5 9 ‡kª‡fi b`x ch©vq µg
10.
wØfvRbAbycvZ (bifurcation ratio) Rb= Nu Nu+1GLv‡b, Rb=
wØ-fvRb AbycvZ, Nu= †Kvb ch©v‡qi b`x Lv‡Zi †gvU msL¨v, Nu+1= cieZx© ch©v‡qi b`x Lv‡Zi †gvU msL¨v| (k-u) Nu= Rb †Kvbch©v‡qi b`x Lv‡Zi †gvU msL¨v(Nu) wbY©‡qi Rb¨ wb‡gœv³ myÎ e¨envi K‡ib - GLv‡b, k= AeevwnKvi D”PZg ch©vq msL¨ u = b`x avcevch©vq
11.
K L ZvwRbWscvnvo b`xiˆ`N© DcZvKvˆ`N© b`xi eµZv= b`xi ˆ`N©¨ DcZ¨Kvi
ˆ`N©¨
12.
g‡nkLvjx†P‡bj C ` Mv I b ` x A e e v wn K
v C` MvI b ` x K · e v R v i ‡R j v K · e vR vi Dc ‡R j v
13.
L)AeevwnKvi b`x NbZ¡
(Drainage Density of the Basin)t †Kvb GjvKvi b`x ¸‡jvi †gvU ˆ`N©¨‡K H GjvKvi AvqZb Øviv fvM Ki‡j AeevwnKvib`x NbZ¡ cvIqv hvq| GLv‡b, D =AeevwnKvib`x NbZ¡, ∑Lk=†Kvb GjvKvi b`x ¸‡jvi †gvU ˆ`N©¨, Ak =AeevwnKviAvqZb| Dc‡ii wPÎ I mviYx †_‡K K·evRvi ‡Rjvi 35 wKwg ˆ`N©¨wewkóC`MvI b`x AeevwnKviAvqZb 142 eM© wKwg I b`x ¸‡jvi †gvU ˆ`N©¨ 516.2 wKwg| myZivs C`MvI AeevwnKvib`x NbZ¡ 3.6 wKwg/ eM© wKwg| Ak Lk D
14.
g‡nkLvjx†P‡bj C ` Mv I b ` x A e e v wn K
v C` MvI b ` x K · e v R v i ‡R j v K · e vR vi Dc ‡R j v 198wg 28wKwg b`xLv‡Zi Xvj t b`xiDrmn‡Z †gvnbv ch©š— D”PZvI Abyf~wgK`~i‡Z¡iAbycvZ‡Kb`x Lv‡Zi Xvj ejv nq| b`xLv‡Zi Xvj †K wgUvi/wK‡jvwgUv‡i cÖKvkKiv nq| f~`„‡k¨Xvj D‡jL †hvM¨ f~wgKv cvjb K‡i _v‡K| Xvj wb®‹vkbaiY wba©vibK‡i Ges f~-c„‡ôi cwieZ©b NUvq| Xvj AeevwnKvi Dw™¢`,cÖvYx,emwZ , †mP,cwienb, AbycÖ‡ek,cvwb aviY, cvwb cÖevn BZ¨vw` wbqš¿Y K‡i _v‡K| wewfbœ ch©v‡q b`xiXvj mgvb _v‡K bv| mvavibZt 1g ch©v‡q b`xiXvj †ekx _v‡K Ges b`xi ch©vq I Xvj wecixZ fv‡e m¤úK©hy³| wP‡Î C`MvI AeevwnKvi b`xLv‡Zi Mo Xvj 5.65wg/wKwg| Xvj (S) = H = †gvnbv n‡Z Drmch©š— D”PZv(198wg) L = b`xLv‡Zi Abyf~wgK`~iZ¡(38wKwg)| C`MvI b`xAeevwnKv,K·evRvi L H
15.
K¨vwj‡dvwbq©v wek¦we`¨vj‡qi f~‡Mv‡ji
mn‡hvMx Aa¨vcK Leal A. K. Mertes b`xLvZ m¤ú‡K© e‡jb- “River, any body of fresh water flowing from an upland source to a large lake or to the sea, fed by such sources as springs and tributary streams. The main parts of a river include a channel, in which the water flows, and a floodplain—a flat region of a valley on either side of the channel”. - Microsoft ® Encarta ® 2008. ÷ªjvi(1964) Gi g‡Z b`xLvZ nj cÖevwnZ cvwbi kw³i d‡j MwVZ GKwU mi“ ev PIov, Mfxi ev AMfxi, †mvRv ev evuKv, Lvov mylg Xvj wewkó GB c_ hvi ga¨w`‡q axi ev cÖej †e‡M KL‡bv mweivg ev KL‡bv Aweivg fv‡e cvwb cÖevwnZ nq| Bnv KL‡bv Ggb mi“ nq †h GK jv‡dB cvi nIqv hvq Avevi K‡qK gvBj ch©š— cÖk¯’ n‡q _v‡K|
16.
the River Severn
17.
18.
Meanders on the
Severn (middle course)
19.
20.
21.
22.
23.
mvaviY fv‡e b`xi
†h ¯’vbw`‡qcvwb cÖevwnZnq Zv‡K b`x LvZ e‡j| AvK…wZ I ˆewk‡ó¨iDci wfwË K‡i b`x LvZ †K K‡qK fv‡efvM Kiv hvq| George Harry Dury Introduction to Fluvial Processes cy¯—‡K G‡K AvU †kªbx‡ZfvM K‡i‡Qb| †hgb- mwc©j (Meandering) webywb (Braided) mij (Straight) Straight- simulating Deltaic- distributary Anabranching Reticulate Irregular.
24.
Channel Length (ft.) SINUOSITY
= ------------------------------ Valley Length (ft.)
25.
mwc©j b`xLvZ (Meandering
channel) t b`x Lv‡Z Pjvi c‡_ †h mvgÄm¨ c~Y© eµZvi m„wó K‡i Zv‡K mwc©j b`xLvZ (Meandering channel) e‡j| Dbwesk kZvãxi ga¨fvM †_‡K mwc©j b`xLvZ(Meandering) Gi msL¨vZvwË¡K w`K wb‡q cÖPzi M‡elYv n‡q‡Q| 1954 mv‡j cvwbweÁvbx iv‡gj b`xi mvgÄm¨ c~Y© eµZvi †¶‡Î Meander kãwU cÖ_g e¨enviK‡ib
26.
27.
28.
29.
30.
31.
32.
A Braided channel is
one that have development into sevsral channels which successively meet and redivided. - Leopold Wolman & Miller.
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