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Peru evaluationhydropowerpotential finalupdate
1. Peru - Evaluation of Hydropower Potential
Eduardo Zolezzi David Menéndez Arán
WB Consultant Halcrow
Washington DC, March 14, 2011
World Bank – Energy Week 2011
Sustainable Energy: Low Carbon, Access and Governance
2. Peru – The Long Path to Hydropower Development
1973: the “First” Evaluation of
Hydropower Potential (German
Technical Assistance)
2008, 2009: ESMAP Studies
Hydropower Development
Framework and Barriers
2011: New Evaluation of
Hydropower Potential (Peru
RE Project – WB Financing)
3. Peru – Evaluation of Hydropower Potential
Contents
Context (Motivation)
Basic Data and Processing
Hydrological Modeling and Processing
Hydropower Potential
Best 100 Potential Small, Mid-Sized Hydro Plants
Products: Hydropower Atlas, Web HidroGIS
12. Precipitation Data
Basic Data: 457 original, plus 155
additional, recordings from
SENAMHI stations; TRMM
(NASA) data; and FAO Cleanwat
2.0 (2006).
Results: 472 consolidated/
processed recordings.
13. Temperature Data
Basic Data: 264 original, plus 70
additional, recordings from
SENAMHI stations; FAO Cleanwat
2.0 (2006); GHCN data (NOOA);
and RETScreen weather data.
Results: 265 consolidated/
processed recordings.
14. Stream Flow Data
Basic Data: 144 original, plus 58
additional, recordings from
SENAMHI stations; 279 original
recordings from ANA Peru and 30
recordings from ANA Brazil; and
14 recordings from INRENA Peru.
Results: 187 consolidated/
processed stream flow recordings
of more than 5 years duration, in
the period 1970-2010.
15. SENAMHI Basic Data Availability
Ene-70
Ene-72
Ene-74
Ene-76
Ene-78
Ene-80
Ene-82
Ene-84
Ene-86
Ene-88
Ene-90
Ene-92
Ene-94
Ene-96
Ene-98
Ene-00
Ene-02
Ene-04
Ene-06
Ene-08
Disponibilidad
de datos
Región 6
Precipitación, Caudal
y Temperatura
Precipitación
Caudal
Temperatura
Water Flow
Temperature
Precipitation
Region 6
19. Peru – Evaluation of Hydropower Potential
Hydrological Modeling and Processing
20. Processing of Hydrology & Weather Data
20
10
0
Jan-10Jan-00Jan-90Jan-80Jan-70 Jan-10Jan-00Jan-90Jan-80Jan-70
20
10
0
Jan-10Jan-00Jan-90Jan-80Jan-70
20
10
0
Jan-10Jan-00Jan-90Jan-80Jan-70
PA MPA BLA NC A
Temperatura(°C)
C A RUMA S C A NDA RA V E C A BA NA C O NDE
C A MA NA EL FRA YLE PA UZA SA N C A MILO
PA MPA GA LERA S PUQ UIO BUENA V ISTA HUA RO C HIRI
Temperatura
200
150
100
50
0
Jan-06Jan-94Jan-82Jan-70
400
300
200
100
0
300
200
100
0
Jan-06Jan-94Jan-82Jan-70
300
200
100
0
200
150
100
50
0
Jan-06Jan-94Jan-82Jan-70
300
200
100
0
Curahuasi
Preicipitación(mm)
Chilcayoc Pisac
Acomayo Urubamba Granja Kcayra
Precipitación Enero
EDA
Time series analysis
Double mass analysis,
Regional accumulations
Analysis of seasonal and
inter-annual variations
Analysis of atypical values
Correlations analysis
Continuity analysis
Statistics (X, S, CV, CS)
21. Processing of Hydrological Data
Región 2: Caudal Medio Mensual
0
5
10
15
20
25
Sep Oct Nov Dic Ene Feb Mar Abr May Jun Jul Ago
Mes
Caudal(m3/s)
0,0
50,0
100,0
150,0
200,0
250,0
Caudal(m3/s)
Dique Los Espanoles
MARIA PEREZ (ANA2)
Salamanca
Aguada Blanca (ANA)
El Frayle (ANA)
Sumbay
Tingo Grande
Huatiapa
Negropampa (D)
PALLCA-HUARURO
(ANA2)
Puente Carretera Camana
Puente Colgante-Sibayo
Charcani
Region 2: Average Monthly Water Flow
Región 2: Curvas de permanencia
0,0
0,5
1,0
1,5
2,0
2,5
3,0
3,5
4,0
0% 20% 40% 60% 80% 100%
% de tiempo superado
Q%/Qa
Chucarapi
Huatiapa
MARIA PEREZ
Negropampa
PALLCA-HUARURO
Puente Carretera Camana
Puente Colgante-Sibayo
Salamanca
Aguada Blanca
Charcani
Sumbay
Tingo Grande
Promedio Region 2
Altura : 20-4500 msnm
Área: 60-17000 km
2
Region 2: Water Flow Duration Curves
Hydrological Regions
22. Hydrological (& Related) Processed Data
Average Annual Precipitation Specific Flow
Annual Evapo-Transpiration
23. Regression Formulae for Regional Hydrology
Qmedio = Average Water Flow
Area = Watershed Area
Pm = Average precipitation
Dd = Drainage surface density
S1085 = Slope index
With Most Significant Coefficients
25. Qi
Qi+1
Hi
zi
TRAMO i
zi+1
i
i+1
Li (1)
Qi, Zi , Ai
Qi+1, Zi+1, Ai+1Nodo creado
automáticamente
Nodo Intermedio
Li (2)
Li (2.1)
Li (2.2)
Determination of Hydropower Potential (Theoretical)
If L < 5 km, then Li=L
If L > 5 km, then Li=L/2
i: Upstream node
i+1: Downstream node
Ai [km2
]: Drain area at node i
Zi [m]: Elevation of upstream node
Li: Length of river reach at node i
( )2/)( 1 iiiiiiTOTAL HQQHQgPPHT ⋅−+⋅⋅== +∑∑
Qi [m3
/s]: Water flow at node i
Qi+1 [m3
/s]: Water flow at node i+1
Hi [m]: Difference of elevation [Zi – Zi+1]
between nodes i and i+1
28. Determination of Hydropower Potential (Technical)
g: Gravity constant
η: Efficiency
Hi [m]: Difference of elevation [Zi – Zi+1]
between nodes i and i+1
Qi [m3
/s]: Water flow at node i
Penstock
Power House
Intake
Restitution
TecP g Hi Qiη= ⋅ ⋅ ⋅
Electromechanical Costs (Ce): f(PTec) [Water Power – 2009]
Penstock Costs (Cp): f(Qturb, Hi, LPenstock) [RETScreen – 2006]
Civil Works Costs (Cc): f (Qturb, PTec, Hi) [RETScreen – 2006]
29. Cost – Benefit Index (ICB)
TAC
ICB
E
=
3
10TA TecC C FRC P COM= ⋅ + ⋅ ⋅
24 365TecE P Fu= ⋅ ⋅ ⋅
E: Annual average generated energy
PTec: Technical hydropower potential
Fu: Utilization factor
24 x 365: Number of hours in a year
CTA: Annuity of total investment
C: Total investment amount
PTec: Technical hydropower potential
COM: O & M costs
FRC: Capital recuperation factor
i: interest rate
n: useful life
0.3716
40,7COM P−
= ⋅
( )
( )
1
1 1
n
n
i i
FRC
i
⋅ +
=
+ −
35. Peru – Evaluation of Hydropower Potential
Best 100 Potential Small, Mid-Sized Hydro Plants
(1 < P < 100 MW)
36. Multi-Criteria for Merit Order
Multi-Criteria Matrix
Economic [ ]
Environmental [ ]
Other Criteria [ ]
Cost/Benefit Index (ICB) [wec1]
Net Present Value [wec2]
Internal Rate of Return [wec3]
Length of affected river reach [wen1]
Number of downstream tributaries [wen2]
Length of access roads [wen3]
Basic data availability [wo1]
Distance to existing electricity network [wo2]
Development of areas of interest [wo3]
ecP
enP
oP
Weight of Indexes in
First Scheme
= 0.8
wec1 = 1.0
= 0.2
wen1 = 0.6
wen2 = 0.4
ecP
enP Weight of Indexes in
Second Scheme
= 0.6 wen1 = 0.2
wec2 = 0.5 wen2 = 0.2
wec3 = 0.5 wen3 = 0.1
( + ) = 0.4
wo1 = 0.3 wo2 = 0.2
ecP
enP oP