M odu le 3 – ( L8 - L1 1 ) : I n t e gr a t e d W a t e r sh e d M a n a ge m e n t I n t r odu ct ion t o I n t e gr a t e d Appr oa ch , I n t e gr a t e d W a t e r Re sou r ce s M a n a ge m e n t , Con j u n ct ive Use of W a t e r Re sou r ce s, Ra in w a t e r
H a r ve st in g; Roof Ca t ch m e n t Syst e m .
9
Con j u n ct ive Use of W a t e r
R
1 1
1
9
L9
Groundwat er, Surface wat er, Conj unct ive
Groundwat er, Surface wat er, Conj unct ive
use, necessit y, advant ages, lim it at ions,
use, necessit y, advant ages, lim it at ions,
h
h
i
Keywords:
Keywords:
surface w at er, Groundw at er, Conj unct ive surface w at er, Groundw at er, Conj unct ive use, st reamuse, st ream ––aquifer int eract ionsaquifer int eract ions use, st ream
Photo A K Singh 2002
Wat er Managem ent problem ?
Photo, A.K. Singh, 2002
Gr ow in g
Popu la t ion Econ om yGr ow in g Am ou n t of Con st a n t
W a t e r in Th e
I ncreasing Dem and for Wat er
Cycle
Dem and for Wat er
I n cr e a sin g com pe t it ion for Sca r ce W a t e r
Unequal Dist ribut ion in Tim e & Space
N e e d For Alloca t ion a n d Con flict
3 3
Re solu t ion
Su r fa ce w a t e r Or Gr ou n dw a t e r ?
Su r fa ce w a t e r Or Gr ou n dw a t e r ?
I ssu e s: I ssu e s:
– Precipit at ion & peak runoff of t he rivers – only few m ont hs of t he year - sm allest wat er dem and.
– Wat er developm ent problem - t ransferring w at er from high – Wat er developm ent problem - t ransferring w at er from high
supply season t o t he high dem and season.
– Solut ion t o t he problem - surface wat er st orage ( reservoirs) or groundwat er st orage ( aquifer recharge & use) .
g g ( q g )
– Surface reservoirs have m any drawbacks, especially:
– e va por a t ion: wat er losses – m ore t han 20 % of average annual runoff; More losses wit h a larger open wat er area.
– se dim e n t a t ion: soil erosion result s in silt at ion in t he surface reservoirs and reduct ion of t he st orage capacit y.
Su r fa ce w a t e r Or Gr ou n dw a t e r ?
Su r fa ce w a t e r Or Gr ou n dw a t e r ?
( Ref.) Keller A.,Sakt hivadivel, R., Seckler David. Wat er Scarcit y and t he Role of St orage in
5 5
Developm ent . I nt ernat ional Wat er Managem ent I nst it ut e, Research Report 39.
St r e a m – Aqu ife r I n t e r a ct ion s
Till lat e 1950’s Surface and Ground wat er dealt and Ground wat er dealt separat ely
I nt eract ion bet ween surface & groundwat er surface & groundwat er Hydraulic connect ion
bet ween aquifer
C
C
onj unct ive Use of Surface & Groundw at er
onj unct ive Use of Surface & Groundw at er
Conj unct ive use - com bined use of surface wat er
resources & groundwat er, in a unified way, t o opt im ize
& i i i d ff t f i
resource use & m inim ize adverse effect s of using a single source.
Conj unct ive usej - act ively m anaging aquifer syst em s y g g q y as an underground reservoir. During wet years, when m ore surface wat er is available, surface wat er is
st ored underground by recharging t he aquifers wit h st ored underground by recharging t he aquifers wit h surplus surface wat er. During dry years, t he st ored wat er is available in t he aquifer syst em t o supplem ent
l d h d f l
or replace dim inished surface wat er supplies.
Judicious use of surface & ground wat er is conj unct ive
use
7 7
use.
Conj unct ive Use
Surface wat er Operat ion of a GW basin
Why?
What?
Art ificially recharge t he
basin during years of
– decline in GW t able during years of below average precipit at ion, w hen SW supplies are below norm al
N e ce ssit y of Con j u n ct ive Use
Groundw at er and surface w at er are closely linked
Groundw at er m aint ains t he base flow of rivers, and w at er in
rivers can infilt rat e int o t he ground. g
Abst ract ion of surface wat er and groundw at er cannot be
planned in isolat ion — one will affect t he ot her. eg. abst ract ion of groundw at er can reduce base flow abst ract ion of groundw at er can reduce base flow cont ribut ion t o rivers by low ering w at er t able.
I f carefully planned, how ever, t he conj unct ive use of rivers
and groundw at er can even out t he seasonal variat ions in and groundw at er can even out t he seasonal variat ions in river flow . I n t he sum m er w hen t he river flow is low , w at er
Con j u n ct ive Use - Adva n t a ge s
Exploit s st orage capacit y of an aquifer & ease of t ransport of wat er by a river/ channel.
Aquifer is used t o st ore surface wat er when t here is an excess of it & it would ot herwise be wast ed, say in
w int er.
River is used t o t ransport wat er from t he aquifer t o where it is needed when river discharge is t oo low on it s own as oft en happens in sum m er
it s own, as oft en happens in sum m er
Conj unct ive use can reduce abst ract ion from rivers when discharge is low by using groundwat er inst ead. Problem s of wat er logging/ groundwat er over use
reduced
Con j u n ct ive Use - Lim it a t ion s
I ncreased energy consum pt ion for pum ping from wells and for coping wit h reduct ion in pum p efficiency, due and for coping wit h reduct ion in pum p efficiency, due t o large fluct uat ions of wat er levels.
Appropriat e m anagem ent plans t o be developed.
f d h
Const ruct ion of appropriat e groundwat er recharge st ruct ures
Adm inist rat ive difficult ies in defining accept able and Adm inist rat ive difficult ies in defining accept able and equit able groundwat er rat es, when surface wat er is available.
People apat hy people part icipat ion essent ial People apat hy – people part icipat ion essent ial
1 1 1 1
Con j u n ct ive Use - Ch a lle n ge s
I solat ed use of surface wat er ignoring opt im al groundwat er use in irrigat ion com m and - result ed int o various environm ent al problem s.
St orage of excess surface wat er underground in an aquifer - a t ype
f j t i ll d d if h k t h
of conj unct ive use called m anaged aquifer recharge - m akes t he m ost of excess wat er by direct ing it int o t he ground where it can be st ored for fut ure use.
Managed aquifer recharge is not a sim ple process & it is difficult t o Managed aquifer recharge is not a sim ple process, & it is difficult t o
do on a useful scale; it cannot absorb large volum es of flood wat er in a short t im e.
I t involves t ransferring w at er from surface t o underground, - by g g , y
dispersing it over t he surface t o increase infilt rat ion, or t hrough aquifer inj ect ion wells.
Surface dispersal involves divert ing wat er int o an unlined canal or
h ll l i bl di k h h
shallow lagoon in perm eable sedim ent s or rock so t hat t he wat er can percolat e downwards int o t he aquifer.
I t works best in areas wit h highly perm eable soils and unconfined
C
C
onj unct ive Managem ent
onj unct ive Managem ent
Conj unct ive m anagem ent - coordinat ed use of
available surface wat er & groundwat er supplies t o m eet wat er dem ands & increase wat er supply supply is plent iful & saving groundwat er for t he
periods when surface wat er supplies are short . Developm ent of conj unct ive m anagem ent plan
-includes considerat ion of surface wat er & groundwat er hydrology, wat er dem and groundwat er hydrology, wat er dem and
Conj unct ive Managem ent - Obj ect ives
Evaluat ion of wat er resources - quant ificat ion of surface & ground wat er in space & t im e - t o det erm ine wat er balance.
I dent ificat ion of crit ical areas of wat er logging & soil salinit y.
Mat ching dem ands of various sect ors wit h available wat er resources & evolve st rat egy t o m eet dem and of t he fut ure.
Mat hem at ical m odeling - t o sim ulat e hydro geological sit uat ion,
generat ion of various scenarios opt im um developm ent plans generat ion of various scenarios, opt im um developm ent plans.
To evolve plan for cont rolling problem of rising wat er levels by
adopt ing t echnique of conj unct ive use and drainage.
To prepare sect or/ block wise plans for developm ent of ground
To prepare sect or/ block wise plans for developm ent of ground wat er resource in conj unct ion wit h surface wat er based on m at hem at ical m odel result s.
To t est sust ainabilit y of present irrigat ion pat t ern w.r.t . Conj unct ive o t est sust a ab t y o p ese t gat o pat t e t Co j u ct e
use & suggest im provem ent for fut ure. ·
To evaluat e t he econom ic aspect of groundwat er developm ent plan
Conj unct ive use
Conj unct ive use -- Schem es
Schem es
A if h b i h / i j t i ll d
Aquifer recharge - basin recharge / inj ect ion w ells- used
w hen no suit able land for a recharge basin, or w it h confined aquifers.
Aquifer st orage and recovery schem es - use t he sam e
borehole t o inj ect and recover w at er -w at er banking.
St orm runoff - can be used for m anaged aquifer recharge I n som e areas - use sew age effluent for m anaged aquifer
recharge
Anot her t ype of conj unct ive use is t he use of groundw at er t o Anot her t ype of conj unct ive use is t he use of groundw at er t o
increase t he flow of a river, called river augm ent at ion.
Advant age - river can be used t o convey groundw at er t o it s dest inat ion.
Effect is sim ilar t o river regulat ion, except wat er is st ored
underground inst ead of in surface reservoirs.
1 5 1 5
Art ificial Recharge Techniques
Art ificial Recharge Techniques
D ir e ct su r fa ce t e ch n iqu e sq
Flooding
Basins or percolat ion t anks
Com bin a t ion su r fa ce –
Basin or percolat ion t anks wit h pit shaft or I nj ect ion wells or recharge wells
Recharge pit s and shaft s
D g ell echa ge
Conj unct ive Use & I rrigat ion Developm ent
Use of groundw at er helps cope w it h peak dem ands for
irrigat ion & hence reduce size of canals and consequent ly const ruct ion cost s.
Supplem ent al supplies from groundw at er ensure proper
irrigat ion scheduling, even if rainfall fails or is delayed
Groundw at er w it hdraw als low er t he w at er t able t hus Groundw at er w it hdraw als low er t he w at er t able t hus
reducing t he risk of wat er- logging, soil salinizat ion and consequent w ast age of w at er for leaching t he soils;
Surface & subsurface out flows are m inim ized, causing Surface & subsurface out flows are m inim ized, causing
reduct ion in peak runoff;
When conj unct ive use is int egrat ed w it h art ificial recharge,
need for lining canals reduced- seepage feeds groundw at er need for lining canals reduced seepage feeds groundw at er
Conj unct ive use allow s ut ilizat ion of saline or brackish
ground – or surface – w at er resources, - by m ixing wit h freshwat er or by using alt ernat e resources for irrigat ion
1 7 1 7
freshw at er, or by using alt ernat e resources for irrigat ion.
Conj unct ive Use Planning
• Develop Local Part nership • Basin Assessm ent
• Dat a Collect ion • Modeling Analysis
Alt t i E l t i
• Alt ernat ives Evaluat ion • Pilot Proj ect
• Feasibilit y St udyFeasibilit y St udy
• I m plem ent at ion and Monit oring.
Ground Wat er Hydraulic Managem ent Models ( Managem ent
Conj unct ive Wat er Use - Mechanism
Use of m at hem at ical m odels for conj unct ive use – sim ulat ion opt im izat ion m odels – Opt im um use sim ulat ion opt im izat ion m odels Opt im um use
Tackle problem of rise in wat er level – w at er logging – drainage
kl l bl
Tackle salinit y problem s
Reschedule operat ion of canals
Manage crop wat er requirem ent s – proposed surface & Manage crop wat er requirem ent s proposed surface &
ground wat er use pat t ern in t im e & space. Dem and & supply m anagem ent
Developm ent of suit able surface st orage schem es
Developm ent of suit able groundwat er recharge schem es
1 9 1 9
Conj unct ive Use – Concerns & Solut ions
program s and est ablishm ent of regulat ory agencies
g
flow regulat ions
Com pelling groundwat er
Form ulat e t he overall goal of t he perm it t ing syst em s
Conj unct ive Managem ent - Modeling
Surface wat er sim ulat ion – Hydrologic m odeling -Sim ulat ion of int errelat ionships am ong hydrologic processes – dist ribut ed m odel in space & t im e – eg. MI KE- SHE
Groundwat er sim ulat ion – groundwat er flow st ream - Groundwat er sim ulat ion groundwat er flow , st ream
aquifer int eract ions– dist ribut ed m odel in space & t im e – eg. MODFLOW
O t i i t i d l O t i l f & d t
Opt im izat ion m odel – Opt im al surface & groundw at er allocat ion – Sim ulat ion opt im izat ion m odels – eg. : Linear program m ing; Dynam ic program m ing,
evolut ionary AI t echniques such as GA, PSO et c. I nt egrat ed m odeling approach
2 1 2 1
Conj unct ive Wat er Use Proj ect s in I ndia
Proj ect s ( Ref: ht t p: / / cgw b.gov.in/ groundw at er/ conj unct ive_use.ht m)
I ndira Gandhi nahar paryoj na, st age - I , Raj ast hanp y j g j
Sarda sahayak irrigat ion proj ect , U.P.
Tungabhadra canal com m and area, Andhra Pradesh & Karnat aka
Ghat aprabha canal com m and area, Karnat akap ,
Hirakud canal com m and area, Orissa
Mahi- kadana canal com m and area, Guj arat
Nagarj una sagar proj ect , Andhra PradeshNagarj una sagar proj ect , Andhra Pradesh
I ndira gandhi nahar pariyoj na st age - I I , Raj ast han
Kosi canal com m and area, Bihar
Gandak canal com m and, Bihar
Gandak canal com m and, Bihar
Sriram sagar canal com m and area, Andhra Pradesh
West ern yam una canal com m and area, Haryana
Case St udy: Conj unct ive Use
Hirakud Canal Com m and Area, Orissa,
I ndia, covering an area of about 2540 km2 Tot al lengt h of canal net o k 3500 km
Tot al lengt h of canal net w ork - 3500 km Average slopes : 1- 6%
Surface drainage – Mahanadi
Mean annual rainfall 1245 m m - 90% June
– Oct ober
Dept h t o w at er level
0 8 9 b l ( )
– 0.8 - 9.7m bgl ( pre- m onsoon) – 0.3- 4.03 m bgl ( post - m onsoon) – 0 t o 2 m bgl ( m onsoon)
Re f: Ra u l S. K., Pa n da S. N ., H olla e n de r H ., Billib M ., Su st a in a bilit y of r ice
-dom in a t e d cr oppin g syst e m in t h e H ir a k ud ca n a l com m a n d, Or issa , I n dia , I r r ig. & D r a in 5 7 : 9 3 – 1 0 4 ( 2 0 0 8 ) W ile y I n t e r scie n ce
2 3 2 3
Prof. T I Eldho, Department of Civil Engineering, IIT Bombay
Case St udy: Conj unct ive Use ..
Ava ila bilit y & D e m a n d Of W a t e r Ut ilizable ground w at er resources
– 508.04 MCM ( Kharif) ; 764.44 MCM ( Rabi)
Availabilit y of surface wat er
– 1360.8 MCM ( Kharif) ; 1494.8 MCM ( Rabi)
Annual w at er dem and ( 2025)
– 49.89 MCM ( Dom est ic) ; 261 MCM ( I ndust rial)
Pr oble m s in t h e st u dy a r e a : Wat er logging ( 1994)
– 1494 sq.km ( Post - Monsoon) ; 174 sq.km ( Pre- Monsoon)
Causes
– Topographic set up; unlined canalsp g p p – over irrigat ion
Case St udy: Conj unct ive Use ..
Con j u n ct ive u se pla n .
Various possible conj unct ive use st rat egies have been t est ed
it h t h d t i l t i d l w it h t he ground w at er sim ulat ion m odel
Dem and for irrigat ion ( Kharif &Rabi) can be m et from
– surface w at er ( 90% ) ; ground w at er ( 10% )
Surface wat er irrigat ion cheaper m axim um use of available
Surface wat er irrigat ion - cheaper - m axim um use of available
surface w at er in conj unct ion w it h groundw at er t o get m axim um ret urn
Developm ent of groundw at er p g
– 17,526 dug w ells
Wat er logging reduces w it h increase in use of groundw at er
Addit ional invest m ent of Rs.953.99 m illion t he B.C rat io w orked out t o 1.66.
2 5 2 5
Case St udy: Conj unct ive Use ..
Le sson s le a r n t :
During m onsoon, m aj orit y of t he com m and rem ains
w at erlogged & it is required t hat groundw at er w it hdraw al gg q g during non- m onsoon period be increased so t hat
groundwat er reservoir will have sufficient capacit y t o accom m odat e m onsoon recharge.
During non- m onsoon period, t here is no danger of w at er
logging but st ill t here is a lot of scope for groundwat er developm ent .p
I ncreasing st orage t hrough a com binat ion of groundw at er &
large & sm all surface w at er facilit ies
Judicious allocat ion of wat er Judicious allocat ion of wat er
Vigilant m onit oring t o avoid over irrigat ion Creat ing public aw areness
f bl
Re fe r e n ce s
Re fe r e n ce s
De Wrachien D. , Fassò C. ( 2002) , Conj unct ive use of surface and groundwat er : overview and perspect ive. I rrigat ion and Drainage ( 2002) , 51 ( 1) , pp. 1- 15.
FAO ( 1995) L d d t i t t i d i b i t
FAO ( 1995) Land and w at er int egrat ion and river basin m anagem ent ,
FAO Land and Wat er Bullet in, 1995
Kakum anu Krishna Reddy, Bauer Siegfried. ( 2008) Conj unct ive use of
wat er: valuing of groundwat er under irrigat ion t anks in sem iarid region wat er: valuing of groundwat er under irrigat ion t anks in sem iarid region of I ndia. I nt . J. Wat er, Vol. 4, Nos. 1/ 2, 2008, pp.87- 104
Medina M. A.( 2000) “ Science View I m port ance of Groundw at er and
Surface- Subsurface I nt eract ions” First GEF Biennial I nt ernat ional Wat ers Conference ( Oct ober 14 – 18, 2000) , Budapest , Hungary
Raul S. K., Panda S. N., Hollaender H., Billib M., Sust ainabilit y of rice-dom inat ed cropping syst em in t he Hirakud canal com m and, Orissa, I di i i A d d i 57 93 104 ( 2008) bli h d li 8 j
I ndia, irrig. And drain. 57: 93–104 ( 2008) published online 8 j anuary 2008 in Wiley I nt erscience.
CGWB, ht t p: / / cgwb.gov.in/ groundwat er/ conj unct ive_use.ht m ( Last
accessed on 08- 03- 2010)
2 7 2 7
accessed on 08- 03- 2010)
Tu t or ia ls - Qu e st ion !.?.
I llu st r a t e t h e Con j u n ct ive Use of Su r fa ce
& Gr ou n dw a t e r w it h a ca se st u dy.
For ca se st u die s Re f: ( Ref:
ht t p: / / cgwb.gov.in/ groundwat er/ conj unct ive_use.ht m)
I dent ify t he problem s of using surface wat er/ I dent ify t he problem s of using surface wat er/
I dent ify t he problem s of using surface wat er/ I dent ify t he problem s of using surface wat er/ groundwat er alone.
groundwat er alone.
St udy t he dem and for t he areaSt udy t he dem and for t he area
I llust rat e how conj unct ive use can be used t o solve I llust rat e how conj unct ive use can be used t o solve t he problem s.
t he problem s.
Discuss t he lesson learnt .Discuss t he lesson learnt .Discuss t he lesson learnt .Discuss t he lesson learnt .
Se lf Eva lu a t ion - Qu e st ion s!.
Q
Discuss t he issues relat ed t o overuse
of surface wat er & groundwat er
of surface wat er & groundwat er.
What is t he necessit y of conj unct ive
use?
use?.
Discuss advant ages & lim it at ions of
conj unct ive wat er use
conj unct ive wat er use.
I llust rat e groundwat er recharge
t echniques wit hin t he perspect ive of
t echniques wit hin t he perspect ive of
Conj unct ive wat er m anagem ent .
P f T I Eldh D t t f Ci il E i i IIT B b
2 9 2 9
Assign m e n t - Qu e st ion s?.
g
Q
Discuss st ream – aquifer int eract ions and
im port ance in conj unct ive use
im port ance in conj unct ive use.
Describe conj unct ive m anagem ent of surface
w at er & groundw at er w it h various
w at er & groundw at er w it h various
challenges.
Discuss conj unct ive use plan and
Discuss conj unct ive use plan and
m echanism s.
How t o develop conj unct ive m anagem ent
p
j
g
Un solve d Pr oble m !.
Un solve d Pr oble m !.
For your Wat ershed area, prepare a m ast er
For your Wat ershed area, prepare a m ast er
plan for conj unct ive use of surface &
plan for conj unct ive use of surface &
d
t
Check t he applicabilit y of m odeling t ools.
Check t he applicabilit y of m odeling t ools.
–
– Carry out det ailed st udyCarry out det ailed st udy –
– Consider int egrat ed approach for surface & ground Consider int egrat ed approach for surface & ground Consider int egrat ed approach for surface & ground Consider int egrat ed approach for surface & ground w at er
w at er –
– Consider opt ions for groundwat er rechargeConsider opt ions for groundwat er recharge
3 1 3 1
Dr. T. I. Eldho Dr. T. I. Eldho
Professor, Professor,
Department of Civil Engineering, Department of Civil Engineering, pp gg gg
Indian Institute of Technology Bombay, Indian Institute of Technology Bombay, Mumbai, India, 400 076.
Mumbai, India, 400 076.
Email:
Email: [email protected]@iitb.ac.in
Email:
Email: [email protected]@iitb.ac.in
Phone: (022)
