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bdkbZ 10 % le&mRikn oØ
mRiknu dk Lrj ftruk vfèkd gksxk] le&mRikn oØ mruh gh ewy fcanq ls nwj gksxhA IQ , IQ , vkSj IQ uksV
1 2 3
oozasQ mRiknu osQ fofHkUu Lrjksa dks O;Dr dj jgh gSaA ,d le&mRikn oØ tks nwljh oØ ls nkb± vksj gS og
mRiknu osQ vfèkd Lrj dks O;Dr dj jgh gSA vr% IQ oØ IQ oØ ls vkSj IQ oØ] IQ oØ dh rqyuk
2 1 3 2
esa mRiknu osQ m¡Qps Lrj dks izdV dj jgh gSaA le&mRikn oØ ftruh m¡Qph gksaxh] mruk gh os m¡Qps mRiknu
osQ Lrj dks O;Dr djsaxhA ijarq izR;sd le&mRikn oØ ifjorZu'khy lkèku dh fofHkUu ek=kkvksa dks O;Dr
djrh gSA
10-6 le&mRikn oØksa dh fo'ks"krk,¡
(Characteristics or Properties of Isoquant Curves)
le&mRikn oØksa dh fo'ks"krk,¡ rVLFkrk oØksa ls feyrh tqyrh gSaA ;s fo'ks"krk,¡ fuEufyf[kr gSaμ
1- le&mRikn oØksa dh <yku mQij ls uhps dh vksj gksrk gS (Isoquant Curves Slope
Downwards)μ,d le&mRikn oØ] tSlk fd fp=k 10-3 ls izdV gksrk gS] ck,a ls nk,a uhps dh
vksj fxjrh gqbZ gksrh gSA vU; 'kCnksa esa bldk <yku ½.kkRed gksrk gSA bldk dkj.k ;g gS fd ,d
lkèku nwljs dk izfrLFkkiu (Substitute) gksrk gSA fdlh oLrq osQ mRiknu dh ,d fuf'pr ek=kk
izkIr djus osQ fy, ;fn ge ,d lkèku dk vfèkd mi;ksx djsaxs rks nwljs lkèku dk de iz;ksx fd;k
tk,xkA ;fn nksuksa lkèkuksa dk ,d lkFk vfèkd ;k de iz;ksx fd;k tk,xk rks oqQy mRiknu leku ugha
jgsxk] og Øe'k% vfèkd ;k de gks tk,xkA rkfydk 1 ls Kkr gksrk gS fd 100 ?kfM+;ksa osQ oqQy
mRiknu osQ fy, ;fn vfèkd iw¡th vFkkZr~ 90 bdkb;ksa dk iz;ksx fd;k tkrk gS rc bldk la;ksx Je
dh de bdkb;ksa vFkkZr~ 10 bdkb;ksa osQ lkFk fd;k tk,xkA blh izdkj ;fn 100 ?kfM+;ksa dk leku
mRiknu izkIr djus osQ fy, ;fn de iw¡th vFkkZr~ 30 bdkb;ksa dk iz;ksx fd;k tkrk gS rks bldk la;ksx
Je dh vfèkd bdkb;ksa vFkkZr~ 40 bdkb;ksa osQ lkFk fd;k tk,xkA ,d le&mRikn oØ osQ uhps dh
vksj <yku dk dkj.k lkèkuksa dh izfrLFkkiUurk gSA mRiknu osQ lkèku ,d&nwljs osQ izfrLFkkiu gS
blfy, leku ek=kk dk mRiknu djus osQ fy, ;fn ,d lkèku dh de bdkb;ksa dk iz;ksx fd;k tkrk
gS rks nwljs lkèku dh vfèkd bdkb;ksa dk iz;ksx fd;k tk,xkA blh dkj.k ls le&mRikn oØ dk <yku
mQij ls uhps dh vksj gksrk gSA
fp=k 10-3
Y
IQ
1
Iso-quant Curve
Slopes Downward
Capital
100
O
X
Labour
2- le&mRikn oØ ewy fcanq dh vksj mUurksnj gksrh gS (Isoquant Curves are Convex to the
Origin)μ le&mRikn oØ vius ewy fcanq O dh vksj lnk mUurksnj gksrh gS tSlk fd fp=k 10-4
ls izdV gks jgk gSA bldk vfHkizk; gS fd lkèku iw.kZ LFkkukiUu (Perfect Substitutes) ugha gSA
bldk dkj.k ;g gS fd lkèkuksa dh rduhdh izfrLFkkiu dh lhekar nj ?kVrh gqbZ gksrh gSA rkfydk 1
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