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Introducción al Cálculo de Caudales Ecológicos - Endesa..

Introducción al Cálculo de Caudales Ecológicos - Endesa..

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Low risk<br />

and high<br />

baseflow<br />

Low risk<br />

and low<br />

baseflow<br />

Risk of <strong>de</strong>leterious effect<br />

Mo<strong>de</strong>rate<br />

risk and<br />

high baseflow<br />

Mo<strong>de</strong>rate<br />

risk and<br />

low baseflow<br />

High risk<br />

and high<br />

baseflow<br />

Tabla B8<br />

Relación entre el grado <strong>de</strong> <strong>al</strong>teración hidrológica y el tot<strong>al</strong> <strong>de</strong> extracción expresado como % <strong>de</strong>l caud<strong>al</strong> medio anu<strong>al</strong> para varias clasificaciones<br />

<strong>de</strong> riesgo, basada en el tamaño <strong>de</strong>l cauce y la composición <strong>de</strong> especies.<br />

Fuente: Draft gui<strong>de</strong>lines for the selection of methods to <strong>de</strong>termine ecologic<strong>al</strong> flows and water levels.<br />

Tabla B9<br />

Métodos empleados para <strong>de</strong>terminar requerimientos <strong>de</strong> caud<strong>al</strong> ecológico según grados <strong>de</strong> <strong>al</strong>teración hidrológica y significancia para<br />

cursos <strong>de</strong> agua.<br />

Fuente: Draft gui<strong>de</strong>lines for the selection of methods to <strong>de</strong>termine ecologic<strong>al</strong> flows and water levels.<br />

High risk<br />

and low<br />

baseflow<br />

Degree of<br />

hydrologic<strong>al</strong><br />

<strong>al</strong>teration<br />

20% High<br />

Degree of<br />

hydrologic<strong>al</strong><br />

<strong>al</strong>teration<br />

Low Historic<strong>al</strong> flow method<br />

Expert panel<br />

Medium Historic<strong>al</strong> flow method<br />

Expert panel Gener<strong>al</strong>ised<br />

habitat mo<strong>de</strong>ls<br />

High Gener<strong>al</strong>ised habitat mo<strong>de</strong>ls<br />

1D Hydraulic habitat mo<strong>de</strong>l<br />

Connectivity/fish passage<br />

Periphyton biomass mo<strong>de</strong>l<br />

Nombre <strong>de</strong>l<br />

Proyecto<br />

Fuente: Jamett 2005.<br />

INTRODUCCIÓN AL CÁLCULO DE CAUDALES ECOLÓGICOS / Un análisis <strong>de</strong> las ten<strong>de</strong>ncias actu<strong>al</strong>es<br />

Significance of instream v<strong>al</strong>ues<br />

Low Medium High<br />

Región<br />

<strong>de</strong> Chile<br />

Año <strong>de</strong><br />

ingreso<br />

<strong>al</strong> SEIA<br />

Historic<strong>al</strong> flow method Expert<br />

panel<br />

Gener<strong>al</strong>ised habitat mo<strong>de</strong>ls<br />

1D hydraulic habitat mo<strong>de</strong>l<br />

Connectivity/fish passage<br />

Entrainment mo<strong>de</strong>l 1D Hydraulic<br />

habitat mo<strong>de</strong>l 2D Hydraulic<br />

habitat mo<strong>de</strong>l Bank stability<br />

Dissolved oxygen mo<strong>de</strong>l<br />

Temperature mo<strong>de</strong>ls Suspen<strong>de</strong>d<br />

sediment Fish bioenergetics<br />

mo<strong>de</strong>l Inundation mo<strong>de</strong>lling<br />

Groundwater mo<strong>de</strong>l Seston<br />

flux Connectivity/fish passage<br />

Periphyton biomass mo<strong>de</strong>l<br />

Gener<strong>al</strong>ised habitat mo<strong>de</strong>ls<br />

1D hydraulic habitat mo<strong>de</strong>l<br />

Connectivity/fish passage Flow<br />

duration an<strong>al</strong>ysis<br />

1D hydraulic habitat mo<strong>de</strong>l 2D<br />

hydraulic habitat mo<strong>de</strong>l Dissolved<br />

oxygen mo<strong>de</strong>l Temperature<br />

mo<strong>de</strong>ls Suspen<strong>de</strong>d sediment Fish<br />

bioenergetics mo<strong>de</strong>l Groundwater<br />

mo<strong>de</strong>l Seston flux Connectivity/fish<br />

passage Flow variability an<strong>al</strong>ysis<br />

Entrainment mo<strong>de</strong>l 1D Hydraulic<br />

habitat mo<strong>de</strong>l 2D Hydraulic habitat<br />

mo<strong>de</strong>l Bank stability Dissolved<br />

oxygen mo<strong>de</strong>l Temperature<br />

mo<strong>de</strong>ls Suspen<strong>de</strong>d sediment Fish<br />

bioenergetics mo<strong>de</strong>l Inundation<br />

mo<strong>de</strong>lling Groundwater mo<strong>de</strong>l<br />

Seston flux Connectivity/fish<br />

passage Periphyton biomass mo<strong>de</strong>l<br />

Flow variabiity an<strong>al</strong>ysis<br />

Tipo <strong>de</strong> método Forma <strong>de</strong> <strong>de</strong>terminación <strong>de</strong> un caud<strong>al</strong><br />

ecológico (Q e<br />

Emb<strong>al</strong>se Illapel IV 1999 Hidrológico simple Qe = X (Q * 0,7)<br />

mensu<strong>al</strong><br />

Emb<strong>al</strong>se Corr<strong>al</strong>es IV 1998 Hidrológico simple Qe = 0.2 * Q mensu<strong>al</strong> míni modiariomensu<strong>al</strong><br />

Convento Viejo<br />

Etapa II<br />

VI 2004<br />

Hidrológico simple<br />

(Tennat)<br />

Qe = CAM10%<br />

Proyecto<br />

Hidroeléctrico La<br />

VI 2004 Hidrológico simple<br />

Qe = 10%CAM corregido por<br />

estacion<strong>al</strong><br />

resultados aplicando Ley francesa y Norma<br />

Higuera<br />

suiza<br />

Centr<strong>al</strong> Hidroeléctrica<br />

Quilleco<br />

VIII 1998 Simulación <strong>de</strong> hábitat Qe según método IFIM<br />

Centr<strong>al</strong> Hidroeléctrica<br />

Lago Atravesado<br />

Tabla B10<br />

XI 1998 Hidrológico simple<br />

Qe según análisis estadísticos simples sobre<br />

caud<strong>al</strong>es observados <strong>de</strong> 1979 a 1997<br />

Métodos utilizados para <strong>de</strong>terminar un caud<strong>al</strong> ecológico por proyectos ingresados <strong>al</strong> SEIA hasta el año 2004.<br />

49

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