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WATER BALANCE WATER BALANCE NEXT GENERATION NEXT GENERATION A TOOL FOR THE WATER RESOURCES MANAGEMENT PRESENTED BY: ANA DEISY LOPEZ – EL SALVADOR NINTH WATER INFORMATION SUMMIT – (WIS-9) WEST PALM BEACH, FLORIDA, JUNE 5 – 7 , 2007

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  • WATER BALANCEWATER BALANCENEXT GENERATION NEXT GENERATION

    A TOOL FOR THE WATER RESOURCES MANAGEMENT

    PRESENTED BY: ANA DEISY LOPEZ – EL SALVADOR

    NINTH WATER INFORMATION SUMMIT –(WIS-9)

    WEST PALM BEACH, FLORIDA, JUNE 5 – 7 , 2007

  • Traditionally in our countries the Hydrologist have been Traditionally in our countries the Hydrologist have been working in Water Balances that consider just the working in Water Balances that consider just the elements of the surface water supply elements of the surface water supply ––How much is the How much is the precipitation, how much is lose by the precipitation, how much is lose by the evapotranspiration, how much is the quantity of the evapotranspiration, how much is the quantity of the water that became surface runoff and how much of the water that became surface runoff and how much of the quantity of water goes to the ground.quantity of water goes to the ground.But in order to be useful to the water planning and But in order to be useful to the water planning and water management, is necessary to have more water management, is necessary to have more information: What is the real availability of the water due information: What is the real availability of the water due its quality? What can be the changes on the water its quality? What can be the changes on the water availability if the use of the land changes or if there are availability if the use of the land changes or if there are changes on the precipitation or temperature? Where can changes on the precipitation or temperature? Where can be planned water related projects? be planned water related projects?

    JUSTIFICATION

  • To answer those questions is necessary to go further To answer those questions is necessary to go further with the analysis and investigationwith the analysis and investigation

    The objective is to determine the actual status and its The objective is to determine the actual status and its future projections of the water resources in quantity and future projections of the water resources in quantity and quality, determining the pressure over the water quality, determining the pressure over the water considering its spatial and temporal distribution, the considering its spatial and temporal distribution, the availability and the demand, to be a tool that allows to availability and the demand, to be a tool that allows to the planning people and the decision makers the the planning people and the decision makers the guidelines to the use and protection of the resources and guidelines to the use and protection of the resources and improve the life quality of the population, and finally, improve the life quality of the population, and finally, ensure the investments of the water related projects.ensure the investments of the water related projects.

    OBJECTIVE

  • “The water balance is the fundamental tool that allow us to know the real availability of the water in quantity and in quality to achieve and adequated management and ensure the availability of the water for the future

    generations”

    Water Monitoring and Research

    Protection AreasVulnerabilityScarcity IndexesPressure Indexes

    DINAMIC AND INTEGRATED WATER BALANCE

    Meteorology

    Precipitation

    Evapotranspiraton

    Hidrology

    Evaluation of the surface andGroundwater

    SUPPLY

    Quality Restrictions

    ÷ =Real Availability Demand

  • SURFACE RUNNOFF

    STORAGE CHANGES

    EVAPOTRANSPIRATIONPRECIPITATION

    WATER SUPPLY: QUANTITY AND SPATIAL AND TEMPORAL ANALYSIS

  • INTEGRATION OF THE QUANTITY WITH THE QUALITY

    The water in the basin is not always available, due that is important to know its quality and with this quality, which can be its potential use – or to know the actual limitations of the quality of the water to be used for the desired and planned use

    The inner circle correspond to the Water Quality Index considering the Environmental Quality of the water that can be (depending of the value of the Index): Worst, Bad, Regular, Good and Excellent

    This will indicate the capability of the water to accept aquatic life

    The external band correspond to the use aptitude, and can be divided in three sections (The color means its aptitude to this use)

    Green: Irrigation

    Turquoise: Raw Water to covert on drinkable with conventional methods

    Light Blue: human contact – tourism

    WATER NATIONAL DIAGNOSIS AND USES PROPOSAL

  • http://www.kulmbach.net/~MGF-Gymnasium/bilderdaten/latinoam-elsalvador/Bilder/Lago de Coatepeque_jpg.jpg

  • WATER THAT CAN BE USE FOR IRRIGATION PURPOSES

    http://www.kulmbach.net/~MGF-Gymnasium/bilderdaten/latinoam-elsalvador/Bilder/Lago de Coatepeque_jpg.jpg

  • SERVICIO HIDROLOGICO SERVICIO HIDROLOGICO NACIONALNACIONAL

    EVALUATION CARACTERIZATION CARACTERIZATIONOF THE AQUIFER OF THE RESERVOIR OF THE WATER

    Medición de niveles piezometricos

    PrecipitacionesEvapotranspiraciónCaudales

    HIDROLOGIA

    Mapas geol. y topo.Columnas litológicasCarac. de los terrenos

    Pruebas de bombeoCálculos hidráulicos

    HIDRAULICA

    ProspeccioneselectromagnéticasProspeccioneseléctricasRegistros eléctricos

    GEOFISICA

    Param. de campoAnálisis químicos

    AREA DE ESTUDIO

    MONITOREOGEOLOGIA

    (actualmente niveles freáticos)

    INTEGRATION OF THE SURFACE AND GROUNDWATER

  • INTEGRATION OF THE AVAILABILITY AND THE INTEGRATION OF THE AVAILABILITY AND THE DEMANDS DEMANDS –– SCARCITY INDEXESSCARCITY INDEXES

    INTERNAL DEMANDS EXTERNAL DEMANDS FUTURE NEEDS

    • Sectors demands: irrigation, water supply, hydroelectricity, tourism, ecological needs

    •Quantification of the returns to the system

    INDICE DE INDICE DE ESCASEZ %ESCASEZ %

    CATEGORIACATEGORIA

    < 1< 1 NO SIGNIFICATIVONO SIGNIFICATIVO

    1 1 -- 1010 MINIMOMINIMO

    11 11 -- 2020 MEDIOMEDIO

    21 21 -- 5050 MEDIO ALTOMEDIO ALTO

    > 50> 50 ALTOALTO

    http://images.google.com.sv/imgres?imgurl=http://quantum.ucting.udg.mx/admin010/img/agua.jpg&imgrefurl=http://quantum.ucting.udg.mx/noticias/&h=183&w=273&sz=7&tbnid=I1uQMJfQA20J:&tbnh=72&tbnw=107&start=23&prev=/images%3Fq%3Dllave%2Bde%2Bagua%26start%3D20%26hl%3Des%26lr%3D%26sa%3DN

  • DINAMIC ANALYSISDINAMIC ANALYSISAnnual Water Balance

    • Impacts on the availability of water on Niño or Niña years

    • Impacts due extreme events (droughts, hurricanes)

    Future Scenarios

    • Land Use changes

    • Water demand changes

    • Climate variability and climate changes

    SISTEMATIZATION

    http://www.lademajagua.co.cu/IMAGES/reforestacion.jpg

  • WATER BALANCE IN ACTUAL CONDITIONS

    pp RET. EV CUERPO DE AGUA EVT REAL EV URB.Q

    REGISTRADO

    DEM. INT DEM. EXT.CAMBIO DE

    ALMAC.

    ANUAL (Mm3) 334.26 7.91 130.51 122.65 3.84 44.11 15.82 5.59 19.65IE = 33.58 %

    BALANCE HIDRICO CUENCA LAGO DE ILOPANGO

    ESTACION DESAGUE

    -150.00

    -50.00

    50.00

    150.00

    250.00

    350.00

    ENER

    O

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    D (m

    m)

    PRECIPITACION

    IM PORTACIONES

    RETORNO DE DEM ANDA INTERNA

    EVAPORACION DE CUERPOS DE AGUA +EVAPOTRANSPIRACION REAL + EVAPORACIONAREAS URBANASCAUDAL REGISTRADO EN ESTACION DESAGUE

    DEM ANDA INTERNA

    DEM ANDA EXTERNA

    CAM BIO DE ALM ACENAM IENTO

  • BALANCE HIDRICO CUENCA LAGO DE ILOPANGO

    ESTACION DESAGUEESCENARIO 1

    -150.00

    -50.00

    50.00

    150.00

    250.00

    350.00

    ENER

    O

    FEB

    RER

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    D (m

    m)

    PRECIPITACION

    IM PORTACIONES

    RETORNO DE DEM ANDA INTERNA

    EVAPORACION DE CUERPOS DE AGUA +EVAPOTRANSPIRACION REAL +EVAPORACION AREAS URBANASCAUDAL REGISTRADO EN ESTACION DESAGUE

    DEM ANDA INTERNA

    DEM ANDA EXTERNA

    CAM BIO DE ALM ACENAM IENTO

    PP RET. EV CUERPO DE AGUA EVT REAL EV URB.Q

    REGISTRADO

    DEM. INT. DEM. EXT.CAMBIO DE

    ALMAC.

    ANUAL (Mm3) 334.26 7.91 130.51 112.50 3.84 44.11 15.82 5.59 29.80

    RESULTS: INCREASE ON THE STORAGE VOLUME IN 10.15 Mm3

    IE = 28.97 %

    BENEFIT:

    Water for 160.000 additional persons = 32.000 families

    SCENARIO 1: INCREASE OF 50% OF FOREST AREA

  • PP RET. EV CUERPO DE AGUA EVT REAL EV URB.Q

    REGISTRADO

    DEM. INT. DEM. EXT.CAMBIO DE

    ALMAC.

    ANUAL (Mm3) 334.26 7.91 130.51 122.65 3.84 44.11 15.82 5.59 19.65IE = 33.58 %

    BALANCE HIDRICO CUENCA LAGO DE ILOPANGO

    ESTACION DESAGUE

    -150.00

    -50.00

    50.00

    150.00

    250.00

    350.00

    ENER

    O

    FEB

    RER

    O

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    RZO

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    m)

    PRECIPITACION

    IM PORTACIONES

    RETORNO DE DEM ANDA INTERNA

    EVAPORACION DE CUERPOS DE AGUA +EVAPOTRANSPIRACION REAL + EVAPORACIONAREAS URBANASCAUDAL REGISTRADO EN ESTACION DESAGUE

    DEM ANDA INTERNA

    DEM ANDA EXTERNA

    CAM BIO DE ALM ACENAM IENTO

    WATER BALANCE IN ACTUAL CONDITIONS

  • BALANCE HIDRICO CUENCA LAGO DE ILOPANGO

    ESTACION DESAGUEESCENARIO 2

    -150.00

    -50.00

    50.00

    150.00

    250.00

    350.00

    ENER

    O

    FEB

    RER

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    PRECIPITACION

    IM PORTACIONES

    RETORNO DE DEM ANDA INTERNA

    EVAPORACION DE CUERPOS DE AGUA +EVAPOTRANSPIRACION REAL + EVAPORACIONAREAS URBANASPOSIBLE CAUDAL REGISTRADO

    DEM ANDA INTERNA

    DEM ANDA EXTERNA

    CAM BIO DE ALM ACENAM IENTO

    PP RET. EV CUERPO DE AGUA EVT REALEV

    URBANAS

    Q REGISTRA

    DODEM. INT. DEM. EXT.

    CAMBIO DE ALMAC.

    ANUAL (Mm3) 334.26 7.91 130.51 119.38 5.78 51.29 15.82 5.59 13.80

    RESULTS : DECREASE OF STORAGE VOLUME 5.85 Mm3

    IE = 36.97 %

    CONSEQUENCE

    91.600 persons = 18.400 families affected

    SCENARIO 2: INCREASE OF URBAN AREA

  • PP RET. EV CUERPO DE AGUA EVT REAL EV URB.Q

    REGISTRADO

    DEM. INT. DEM. EXT.CAMBIO DE

    ALMAC.

    ANUAL (Mm3) 334.26 7.91 130.51 122.65 3.84 44.11 15.82 5.59 19.65IE = 33.58 %

    BALANCE HIDRICO CUENCA LAGO DE ILOPANGO

    ESTACION DESAGUE

    -150.00

    -50.00

    50.00

    150.00

    250.00

    350.00

    ENER

    O

    FEB

    RER

    O

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    PRECIPITACION

    IM PORTACIONES

    RETORNO DE DEM ANDA INTERNA

    EVAPORACION DE CUERPOS DE AGUA +EVAPOTRANSPIRACION REAL + EVAPORACIONAREAS URBANASCAUDAL REGISTRADO EN ESTACION DESAGUE

    DEM ANDA INTERNA

    DEM ANDA EXTERNA

    CAM BIO DE ALM ACENAM IENTO

    WATER BALANCE IN ACTUAL CONDITIONS

  • BALANCE HIDRICO CUENCA LAGO DE ILOPANGO

    ESTACION DESAGUE

    -150.00

    -50.00

    50.00

    150.00

    250.00

    350.00

    ENER

    O

    FEB

    RER

    O

    MA

    RZO

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    PRECIPITACION

    IM PORTACIONES

    RETORNO DE DEM ANDA INTERNA

    EVAPORACION DE CUERPOS DE AGUA +EVAPOTRANSPIRACION REAL + EVAPORACIONAREAS URBANASCAUDAL REGISTRADO EN ESTACION DESAGUE

    DEM ANDA INTERNA

    DEM ANDA EXTERNA

    CAM BIO DE ALM ACENAM IENTO

    RESULTS : OVER EXPLOTATION OF THE AQUIFER

    PP RET.EV.

    CUERPO DE AGUA

    EVT REALEV

    AREAS URBANAS

    Q ESTIMADO DEM. INT.

    DEM. EXT.

    CAMBIO DE ALMAC.

    ANUAL (Mm3) 209.31 7.91 130.51 104.27 3.09 25.42 15.82 5.59 -67.48

    SCENARIO 3: REDUCTION OF 35% ANNUAL PRECIPITATIONSTRONG NIÑO YEAR

  • WATER SUPPLY MODULE

    CALCULATION PERIODGEOGRAPHICAL LOCATION

    CALCULATION UNITS

  • RESULTADOS DE OFERTA HIDRICA POR CUENCA

  • POSSIBILITIES TO CHANGE THE LAND USES TO SEE THE IMPACT ON THE WATER OFERT RESULTS

  • WATER DEMAND MODULE

  • The irrigation demand is calculated in another module that is integrated after to the system

  • DEMANDA HUMANA

    UBICACIÓN GEOGRAFICA PERIODO DE CALCULO

    RESULTADOS

  • DEMANDA INDUSTRIAL

  • IRRIGATION DEMAND

    OPTION OF THE CALCULATION METHODOLOGY

  • RESULTS OF THE WATER OFERT MODULE

    DEMANDS AND RETURNS

    WATER BALANCE AND SCARCITY INDEX OF THE BASIN

    WATER BALANCE�NEXT GENERATION OBJECTIVEINTEGRATION OF THE AVAILABILITY AND THE DEMANDS – SCARCITY INDEXESDINAMIC ANALYSIS