Rotational Equilibrium and Dynamics Rotational Inertia and Angular Momentum.
Study on performance of dry season rotational irrigation for Mae Lao irrigation project, Thailand
description
Transcript of Study on performance of dry season rotational irrigation for Mae Lao irrigation project, Thailand
Study on performance of dry season Study on performance of dry season rotational irrigation for Mae Lao irrigation rotational irrigation for Mae Lao irrigation
project, Thailandproject, Thailand
Naritaka KUBO: Univ. of Tokyo, JapanNaritaka KUBO: Univ. of Tokyo, JapanTakuya TAKEUCHI: Tokyo Univ. of Agri. & Tec., JapanTakuya TAKEUCHI: Tokyo Univ. of Agri. & Tec., JapanUnggoon WONGTRAGOON: Rajamangala Uni. of Tec., Unggoon WONGTRAGOON: Rajamangala Uni. of Tec., ThailandThailandHajime TANJI: NIRE, NARO, Tsukuba, JapanHajime TANJI: NIRE, NARO, Tsukuba, Japan
Back GroundBack GroundIn south east Asian countriesIn south east Asian countries……
Irrigation projects were developed primarily Irrigation projects were developed primarily for supplemental supply during rainy seasonfor supplemental supply during rainy season
Constructing new reservoirs makes Constructing new reservoirs makes irrigation possible during dry seasonirrigation possible during dry season
Restricted irrigation areas Restricted irrigation areas because of scare waterbecause of scare water
Necessity of effective water Necessity of effective water useuse
Water supply is not Water supply is not enoughenough
Mae Lao Project site
Mae Lao Mae Lao irrigation irrigation schemescheme
Tributary of the Tributary of the Kok River Kok River belonging to belonging to Mekong River Mekong River basinbasin
Chiang Rai in Chiang Rai in North ThailandNorth Thailand
Irrigation Area : Irrigation Area : 23680 ha23680 ha
Branch 34,848 ha
Branch 25,264 ha
Branch 17,968 ha
Branch 45,600 ha
Mae Lao river
Left Main Canal
Right Main Canal
Mae Lao weir
Mae Suai Dam
Laterals
Streams 0 5 10 km
Mae Lao project siteMae Lao project site
18,080 ha
Right Main Canal Right Main Canal (( RMCRMC ))
- RMC length - RMC length :: about about 5050 km km
- Secondary canals - Secondary canals : : 2323
- Max Q- Max Q : : about about 2727 mm33/s/s
Mae Suai Dam
Mae Lao Weir
Water deficit in dry seasonWater deficit in dry season
InterviewsInterviews
Branch 1Branch 1 ・ ・ Water deficit occurs partiallyWater deficit occurs partially Branch 2Branch 2 ・ ・ Irrigation area is expanded beyond Irrigation area is expanded beyond
allotted area allotted area
・ ・ Water deficit occurs in downstream areasWater deficit occurs in downstream areas Branch 3Branch 3 ・ ・ Water deficit is seriousWater deficit is serious
・ ・ No water comes to downstream areasNo water comes to downstream areas
Summary of Summary of interviewsinterviews
Mae Suai Dam can Mae Suai Dam can store 73,000,000 store 73,000,000 mm33
Functional Functional problemsproblems
Managerial Managerial problemsproblems
Illegal activitiesIllegal activities Problem Problem
identificationidentification
Low distribution Low distribution efficiencyefficiency
Unequal water Unequal water distributiondistribution
ObjectivesObjectives
Quantitative analysis of effects of facilitiesQuantitative analysis of effects of facilities and and water management on water distribution water management on water distribution performanceperformance
1. Planning phase1. Planning phase Continuous irrigation by non-uniform flow Continuous irrigation by non-uniform flow
modelmodel Effects by physical causes of facilities & Effects by physical causes of facilities &
structuresstructures
2. Execution phase2. Execution phase Rotational irrigation simulated by UIWDC Rotational irrigation simulated by UIWDC
modelmodel Effects by managerial & institutional causesEffects by managerial & institutional causes
MethodologyMethodology
Water consumption in Water consumption in paddy fieldpaddy field
⇒⇒ Paddy Tank modelPaddy Tank model
Numerical simulation by Numerical simulation by UIWDC modelUIWDC model(( Unggoon Unggoon et alet al., 2010., 2010 ))
(( UUnsteady nsteady IIrrigation rrigation WWater ater DDistribution and istribution and CConsumptiononsumption ))
Water movement in Water movement in canalcanal
⇒⇒ 1-D unsteady flow 1-D unsteady flow modelmodel
qx
Q
t
A
quSSgAx
hgA
A
Q
xt
Q
f0
2
Saint-Venant Saint-Venant EquationsEquations
AA :: Area, Area, QQ :: Flow, Flow, qq :: side flow, side flow, hh ::depth, depth, gg :: gravitational acceleration, gravitational acceleration, SS
00 :: bed slope, bed slope, SSff :: friction slope, friction slope, uu ::mean velocitymean velocity
inundated
Plow layer
Ground Water
Modeling of irrigation Modeling of irrigation systemsystem
Branch 1
Branch 2
5L~12L
Branch 3
13L~22L
HW
1L
2L
3L
4L
Paddy field
CK
Check structure
PFPF
PF
PF
PF
PF PF
PF PF
PF PF
PF PF
PF
PF
Dir
ect
w
ith
dra
wal
Dir
ect
w
ith
dra
wal
Dir
ect
w
ith
dra
wal
Dir
ect
w
ith
dra
wal
CK
CK
CK
Modeling of FTOs and water Modeling of FTOs and water distributiondistribution
HW
J
1R-1L
E
J CK E
CK
CK
SI
SW
CK
J
E
FT
O 2R
FT
O 3R
FT
O 4R
FT
O 5R
FT
O 8R
FT
O 10R
FT
O 11R
FT
O 13R
FT
O 14R
FT
O 9
L
FT
O 1
2L
FT
O 6R
FT
O 7
L
CK1L-RMC
J FT
O 1R
FT
O 2
L
FT
O 3R
FT
O 4
L
FT
O5R
FT
O 6R
FT
O 7
L
FT
O 8
L
1R-2L
E
J
FT
O 9R
FT
O 1
0L
FT
O 1
1L
2L-RMC
SW
J
SW
FT
O 2R
FT
O 1
L
FT
O 3R
FT
O 4
L
FT
O5R
FT
O 7R
FT
O 6
L
FT
O 8
L
FT
O 9R
FT
O 1
0L
FT
O 11R
FT
O 12R
FT
O 1
3L
FT
O 1
4L
FT
O 15R
FT
O 16R
FT
O 17R
3L-RMCCK
FT
O 1
L
FT
O 1R
FT
O 2
L
FT
O 2R
FT
O 3
L
FT
O 3R
RMC
FT
O 4
L
FT
O 4R
CK CK CK
E
E
SI
FT
O 5R
FT
O 5
L
1R-4L
E
JCK CK
E
J FT
O 6R
2R-4L
E
J JSI
FT
O 7R
FT
O 6
L
FT
O 7
L
FT
O 8
L
JFT
O 8R
J
FT
O 9R
FT
O 10R
FT
O 11R
FT
O 9
L
FT
O 12R
CK
FT
O 1
0L
FT
O 13R
CK
FT
O 1
1L
FT
O 1
2L
FT
O 14R
CK
FT
O 1
3L
FT
O 15R
CK
E : Ended Point
J : Joint
CK : Check Gate
SW : Spill Way
SI : Siphon
HW : Head Work
4L-RMCE
1L-4
L
3R-4L
E
4R-4L
E
2L-4
L
E
CK
SI
J
Q2
Q1
Q3
Q4
Q5
Q7
Q6
Q8
Q9
Q10
Q11
Q12
Q13
Q14
Q15
Q16
Q17
3L-RMCCK E
Reach
Reach
Reach
: Computational mesh point
CK
SI
J
Q17
CK E
Reach
Reach
Reach
: Computational mesh point
ΔX
q
(a)
(b)
3L-RMC
Intake flow rate Intake flow rate (IFR)(IFR)
Assumptions for CalculationAssumptions for Calculation
Equal water distribution within a branchEqual water distribution within a branch Daily water consumption in paddy field:14.7 Daily water consumption in paddy field:14.7
mm/daymm/day Each branch is calculated independently Each branch is calculated independently Total paddy field area in Branch i : Total paddy field area in Branch i : Ai
Scheduled area to be irrigated in Branch i : Scheduled area to be irrigated in Branch i : Asi
1. Based on water requirement Q1. Based on water requirement Qss
2. Base on non-uniform flow 2. Base on non-uniform flow calculation Qcalculation Qee (( considering physical considering physical propertiesproperties ))
Exact water volume to irrigate area of Exact water volume to irrigate area of AAsisi
⇒ ⇒ Scheduled QScheduled Qsisi for Branch i for Branch i Based on water requirementBased on water requirement
= = Paddy water consumption ×APaddy water consumption ×Asisi
+ Seepage loss+ Seepage loss
1. Calculation of scheduled IFR Q1. Calculation of scheduled IFR Qss
Canal seepage losses are Canal seepage losses are calculated assuming Full calculated assuming Full
Supply LevelSupply LevelPF
PF PF
PFto be
irrigated
not to beirrigated
Calculated by numerical simulation for Calculated by numerical simulation for non-uniform flow non-uniform flow
IFR at equilibriumIFR at equilibrium
( ( useless spillageuseless spillage == deficitdeficit ) )
Spillage
deficit
⇒⇒Equilibrium QEquilibrium Qeiei for Branch ifor Branch i
Canal seepage loss Canal seepage loss considering Non-uniform considering Non-uniform
Flow LevelFlow Level
Paddy field
canal
Inlet of FTO
2. Calculation of equilibrium IFR 2. Calculation of equilibrium IFR QQee
Result (1)Result (1) Scheduled area vs. Scheduled area vs. IFR Q IFR Q
No differences No differences at no seepage at no seepage losseslosses
→ → caused by caused by seepage lossesseepage losses
Lower water Lower water level than that of level than that of FSLFSL
Longer distance Longer distance causes more causes more losseslosses
Scheduled Qsi & Equilibrium Scheduled Qsi & Equilibrium QeiQei
Maximum Flow Maximum Flow Rate 27 mRate 27 m33/sec/sec
Scheduled area ratio (Asi/Ai)
Inta
ke F
low
Rate
(m
3/s
)
Result (2)Result (2) Scheduled area vs. Scheduled area vs. WSRWSR
Larger canal sectionLarger canal section Lower water levelLower water level Higher threshold of Higher threshold of
FTOFTO
WSR = [WSR = [Actually distributed waterActually distributed water]/[]/[Volume to be Volume to be
distributeddistributed]] (Water supply ratio)(Water supply ratio)
More difficult More difficult withdrawalwithdrawal
Lower WSRLower WSR
More upstream
WS
R
Branch 1 Branch 2 Branch 3
Scheduled area ratio (SAR Asi/Ai)
Rotational irrigationRotational irrigation ( ( execution execution phasephase ))
5 days
5 days
5 days
Intake Flow Rate Q : 10 Intake Flow Rate Q : 10 mm33/s/s
Field water supply : 3 Field water supply : 3 times of daily water times of daily water requirementrequirement
Observance of rotationObservance of rotation : :
Upstream branches do not Upstream branches do not withdraw water during off-turn withdraw water during off-turn
Strict application ruleStrict application rule::
Water withdrawal stops when Water withdrawal stops when ponded water exceeds 100 ponded water exceeds 100 mm depth, and irrigation re-mm depth, and irrigation re-starts at 80 starts at 80 % % of soil of soil moisturemoisture
Water management Water management conditionsconditions
Observance of rotationObservance of rotation Strict application ruleStrict application rule
Planning water managementPlanning water management (( Type OType O ))
Possible water managementsPossible water managements Type AType A : :
Direct FTOs use Direct FTOs use riparian rightriparian right and application rule is strict and application rule is strict Type BType B : :
All FTOs observe All FTOs observe rotationrotation and application rule is and application rule is not strictnot strict Type ABType AB : :
Direct FTOs use Direct FTOs use riparian rightriparian right and application rule is and application rule is not not strictstrict
Result (3)Result (3) WSRWSR corresponding to water management corresponding to water management typestypes
1. Low WSR for Branch 1 along RMC1. Low WSR for Branch 1 along RMC
2. High WSR for Branch 2 along RMC at 2. High WSR for Branch 2 along RMC at AB type AB type managementmanagement
3. Low WSR for Branch 3 along lateral 3. Low WSR for Branch 3 along lateral canal at canal at AB type AB type managementmanagement
Along RMCAlong RMC
WS
R
Branch 1 Branch 2 Branch 3
WS
R
Branch 1 Branch 2 Branch 3
Along lateral Along lateral canalcanal
Result (4)Result (4) Direct FTO Direct FTO WSRWSR along RMCalong RMC based on type O based on type O
Larger cross sectionLarger cross section
High inlet of FTOHigh inlet of FTOLower water levelLower water level
Difficult withdrawalDifficult withdrawal
0
0. 2
0. 4
0. 6
0. 8
1
給水
率
Branch 2
Branch 3
Branch 1
Upstream
Downstream
WS
R
OO
Checks, Laterals and Spill ways along Checks, Laterals and Spill ways along
RMCRMC
Sure water withdrawal
Excessive withdrawal
at off-rotation
Result (5)Result (5) Direct FTO Direct FTO WSRWSR in Branches 2 and 3, in Branches 2 and 3, along along RMCRMC based on types of O and AB based on types of O and AB
OO
ABAB
WS
R
Branch 2
Branch 3
WS
R
Branch 2
Branch 3
Excessive withdrawal
at midstream
Water deficit at
downstream
Result (6)Result (6) FTO FTO WSRWSR at lateralsat laterals in Branch 3 in Branch 3 based on types of O and AB based on types of O and AB
OO
ABAB
13L 14L 15L 17L 17La 18L 19L 20L 21L 22L
WS
R
14L 15L 17L 17La 18L 19L 20L 21L 22L13L
WS
R
ConclusionConclusion
Influence by structuresInfluence by structures Water withdrawal is restricted when water level is Water withdrawal is restricted when water level is
low.low. Influence by strictness of water managementInfluence by strictness of water management One of two observances of rules improves One of two observances of rules improves
waterwater distribution performance considerably distribution performance considerably Other wiseOther wise Excessive withdrawal at middle branchExcessive withdrawal at middle branch Serious water deficit at downstream branchSerious water deficit at downstream branch
Water distribution performance is Water distribution performance is influenced by structures and strictness of influenced by structures and strictness of water managementwater management