ESCUELA PROFESIONAL DE INGENIERIA CIVIL
HIDROLOGIA GENERAL “TRABAJO ENCARGADO”
INSTITUCIONES ENCARGADOS DEL ESTUDIO DEL AGUA
PRESENTADO POR:
CUSI TARAPA, Renzo
VENTURA CONTRERAS, William Iban
CHINO PEÑA, Carlos
ALIAGA QUISPE, Smath Pool
VILCA HUAQUISTO, Brigido
DOCENTE: ING. BORIS J. CHIQUE CALDERÓN
FECHA: 17 DE OCTUBRE DEL 2017
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1.
INTRODUCCIÓN .............................................. ..................................................................... .............................................. ................................. .......... 4
2. INSTITUTOS DEDICADOS AL ESTUDIO Y PROTECCIÓN DEL AGUA Error! Bookmark not defined. 2.1.
Autoridad Nacional Del Agua (Ana) ................. Error! Bookmark not defined.
2.2. Servicio nacional de meteorología e hidrología (SENAMHI) Error! defined.
Bookmark
not
2.3. El Instituto de Investigaciones de la Amazonía Peruana (IIAP) Error! Bookmark not defined.
2.4. El Instituto Nacional de Investigación en Glaciares y Ecosistemas de Montaña ( INAIGEM) ............................................... ..................................................................... ......................Error! Error! Bookmark not defined. 2.5.
Proyecto Especial Binacional Lago Titicaca (PELT) Error! Bookmark not defined.
2.6. El Organismo de Evaluación y Fiscalización Ambiental (OEFA) Error! Bookmark not defined.
3.
2.7.
Ministerio de transportes transportes y Comunicaciones (Perú)Error! (Perú) Error! Bookmark not defined.
2.8.
Ministerio del Ambiente (Perú) ......................... ......................... Error! Bookmark not defined.
CONCLUSIONES .............................................. .................................................... ...... Error! Bookmark not defined.
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DEDICATORIA: Queremos dedicar este trabajo A Dios que nos ha dado la vida y fortaleza para terminar este trabajo, A nuestros Padres por estar ahí cuando cuando más los necesitamos; necesitamos; en especial a nuestras madres por su ayuda y constante cooperación en los momentos más difíciles.
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1. INTRODUCCIÓN La cuenca es el área de la superficie terrestre drenada por sistema fluvial, sus límites están formados por la divisoria de las aguas que separan de las zonas adyacentes adyacentes pertenecientes a otras cuencas fluviales. El tamaño y la forma de una cuenca viene determinar generalmente por las condiciones geológicas del territorio y el rió que drenan drenan este territorio, el presente trabajo tiene como como objetivo principal poder determinar los Parámetros Geomorfológicos de la cuenca Río Ayaviri, ubicada en el Distrito de Ayaviri y en la Provincia de Melgar. Para ello nosotros contamos con el plano de la cuenca, para lo cual aplicaremos la metodología respectiva. La realización de este trabajo es de mucha importancia ya que para la determinación de los parámetros geomorfológicos de una cuenca se deben de realizar una serie de estudios hidrológicos, es decir para determinar la posibilidad hídrica de una cuenca, cuenca, también se mencionan mencionan conceptos conceptos preliminares del curso para lograr el entendimiento entendimiento del trabajo tales como el desarrollo del ciclo del agua en la naturaleza que es muy importante en este trabajo. La caída de las lluvias, la variación de los niveles de los ríos, y el almacenamiento de agua en depósitos superficiales o subterráneos son temas en cuyo estudio se ha venido profundizando a lo largo de los años, conformando una rama de la física físi ca que se conoce como Hidrología. Lo cual nos servirá de mucho, para realizar estudios y proyectos, pro yectos, en este caso el estudio hidrológico, implica un estudio exhaustivo del aporte hídrico de la cuenca de estudio, para poder determinar los parámetros hidrológicos hidrológicos que sirva para el el diseño de obras hidráulicas hidráulicas proyectadas proyectadas para el sistema sistema de evacuación evacuación y drenaje de las aguas pluviales de la migro cuenca rio Ayaviri. 2. . OBJETIVOS
Determinar los Parámetros Geomorfológicos de la Cuenca Río Ayaviri. A yaviri. Determinación de precipitación media Delimitacion de Cuenca
3. MATERIALES Y EQUIPOS EQUIPOS Los materiales y equipos utilizados para el presente trabajo es la siguiente: Puntos tratados en civil 3D y carta nacional
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4. UBICACIÓN Y LIMITES LIMITES 4.1. UBICACIÓN GEOGRÁFICA Geográficamente Geográficamente la cuenca de Ayaviri A yaviri se encuentra en coordenadas UTM (WGS84): Coordenadas
14°52′55″S 70°35′24″O Coordenadas: 14°52′55″S 70°35′24″O (mapa)
Capital Entidad • País • Región • Provincia Alcalde
Ayaviri Distrito Perú Puno Melgar Víctor Jesús Huallpa Quispe (2015-2018)
Superficie • Total 1013,14 km² 1013,14 km² Altitud • Media 3907 m 3907 m s. n. m. Población (2007) • Total 22 667 hab. • Densidad 22 4 hab/km²
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4.3. UBICACIÓN POLITICA La cuenca del río Ayaviri, A yaviri, políticamente se encuentra ubicada en:
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4.4. LIMITES
Por el norte, con los distritos de Nuñoa Por el sur, con los distritos de Vila Vila Por el este, con los distritos de Tirapata y Pucara Por el Oeste, con el distrito de Umachiri
4.5. CLIMA Siendo una provincia andina por excelencia, su clima es el característico de la sierra, esto es totalmente variado: gélido y casi inhabitado en las cordilleras con las de 4,000 m. s. n. m., frío desde los 3,000 m. s. n. m., donde ya se levantan poblaciones. Los vientos dominantes son los alisios, los locales son ocasionales y fuertes, las lluvias son torrenciales, acompañados acompañados casi siempre de granizos y descargas eléctricas. Las nevadas son frecuentes en el invierno, sólo que se distinguen dos estaciones perfectamente demarcadas: demarcadas: una lluviosa y templada desde octubre hasta marzo y una seca e invernal de abril a setiembre caracterizado por su sol radiante, durante las principales horas del día y por heladas penetrante durante la noche. (PORTAL MUNICIPAL) MUNICIPAL)
5. MARCO TEORICO 5.1. CUENCA HIDROGRÁFICA Se llama cuenca hidrográfica al área territorial de drenaje natural donde todas las aguas pluviales confluyen hacia un colector común de descarga. Los límites de una cuenca está determinados por la línea de “divortiun aquarium” o divis oria de aguas. Debemos hacer hincapié que no siempre los límites geográficos suelen suelen coincidir con los los límites del acuífero, pudiendo pudiendo existir transferencias transferencias de masas líquidas entre una cuenca y otra. La línea de divortiun aquarium se inicia y termina en la cota de captación del proyecto.
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La metodología seguida para la determinación de las características físicas de una cuenca y para alcanzar los objetivos trazados se describe a continuación. Una cuenca hidrográfica es una área de terreno que desagua en un quebrada, río, lago, pantano, bahía o en un acuífero subterráneo. En un valle, toda el agua proveniente de lluvias y riego, que corre por la superficie del suelo (lo ( lo que se denomina agua de escurrimiento) desemboca en desagües pluviales, quebradas y ríos que fluyen directamente al mar, lago, etc. Usted vive en una cuenca hidrográfica que desemboca en una quebrada local, y toda el agua de escurrimiento proveniente de su hogar, jardín y vecindario vecindario desemboca a dicho quebrada o río.
5.2. CARACTERÍSTICAS DE UNA CUENCA HIDROGRÁFICA SON:
La curva cota superficie: esta característica da una indicación del potencial hidroeléctrico de la cuenca. El coeficiente de forma: da indicaciones preliminares de la onda de avenida que es capaz de generar. El coeficiente de ramificación: también da indicaciones preliminares respecto al tipo de onda de avenida.
5.3. TÉRMINOS IMPORTANTES A DISTINGUIR EN UN RÍO SON: a) Cauce. Cauce o Lecho de los ríos y arroyos. Conducto descubierto descubi erto o acequia por donde corren
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5.4. PARTES DE UNA CUENCA HIDROGRÁFICA 5.4.1. 5.4.1. Cuenca alta.-
Es la parte de la cuenca hidrográfica en la cual predomina el fenómeno de la socavación. Es decir que hay aportación de material terreo hacia h acia las partes bajas de la cuenca, visiblemente se ven trazas de erosión 5.4.2. 5.4.2. Cuenca media.-
Es la parte de la cuenca hidrográfica en la cual mediamente hay un equilibrio entre el material sólido que llega traído por la corriente y el material que baja. 5.4.3. 5.4.3. Cuenca baja.-
Es la parte de la cuenca sale. Visiblemente no hay erosión. 5.5. TIPOS DE CUENCAS
Exorreicas: avenan Exorreicas: avenan sus aguas al mar o al océano. Un ejemplo es la cuenca del Plata, en Sudamérica. Endorreicas: desembocan Endorreicas: desembocan en lagos o lagunas, siempre dentro del continente. filtr an en el terreno. Los arroyos, aguadas y cañadones Arreicas: Arreicas : las aguas se evaporan o se filtran de la meseta central patagónica pertenecen a este tipo, ya que no desaguan en ningún río u otro cuerpo hidrográfico de importancia.
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5.7. PARÁMETROS GEOMORFOLÓGICOS GEOMORFOLÓGICOS Las características de la cuenca pueden ser explicadas a partir de ciertos parámetros o constantes que se obtienen del procesamiento hgmhgde la información cartográfica y conocimiento de la topografía de la zona de estudio.
5.8. IMPORTANCIA DE LA CUENCA La selección selección de las cuencas que serán incluidas en los planes los planes de manejo, depende de la importancia de cada una, de su estado de deterioro y del nivel de información básica información básica que se posea
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Implementación, prueba y aplicación de un programa computarizado que permita evaluar la prioridad de cada cuenca, según la metodología usada y la ponderación estimada de las variables consideradas y ordenadas jerárquicamente según los resultados obtenidos. 1.1. PARÁMETROS GEOMORFOLÓGICOS Las características de la cuenca cuenca pueden ser explicadas a partir de ciertos parámetros o constantes constantes que se obtienen del del procesamiento de la información cartográfica y conocimiento conocimiento de la topografía de la zona de estudio. La cuenca como unidad dinámica natural es un sistema hidrológico en el que se reflejan acciones recíprocas entre parámetros y variables. Las variables pueden clasificarse en variables o acciones externas, conocidas como entradas y salidas al sistemaza, tales como: precipitación, escorrentía directa, evaporación, infiltración, transpiración y variables de estado, tales tal es como: contenido de humedad del suelo, salinidad, cobertura vegetal, entre otros. Los parámetros en cambio permanecen constantes en el tiempo y permite explicar las características fisiomorfométricas de la cuenca. 1.2. IMPORTANCIA DE LA CUENCA La selección de las cuencas que serán incluidas en los l os planes de manejo, depende de la importancia de cada una, una, de su estado de deterioro y del nivel de información básica básica que se posea sobre sobre ella, por lo que se requiere efectuar un proceso de jerarquización de las cuencas cuencas hidrográficas que se ejecutará a través del Inventario Nacional de Cuencas Hidrográficas y
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2. RESULTADOS 2.1. ÁREA DE LA CUENCA (A) Es la superficie de la cuenca comprendida dentro de la curva cerrada de divortiun aquarium. La magnitud del área se obtiene mediante el planimetrazo de la proyección del área de la cuenca sobre un plano horizontal. Dependiendo Dependiendo de la ubicación de la cuenca, cuenca, su tamaño influye en mayor o menor grado en el aporte de escorrentía, tanto directa como de flujo de base o flujo sostenido. Su importancia radica en las siguientes razones: a) Para una misma región hidrológica o regiones similares, se puede decir que a mayor área mayor caudal o viceversa. b) Bajo las mismas condiciones hidrológicas, hidrológicas, cuencas con áreas mayores producen hidrógrafas con variaciones en el tiempo más suaves y más llanas. Sin embargo, en cuencas grandes, se pueden dar hidrógrafas hidrógrafas picudas cuando cuando la precipitación fue intensa y en las cercanías, cercanías, aguas arriba, de la estación de aforo. En este caso, el área de la cuenca Ayaviri. Es la siguiente: A = 413 846.1539 m2 Para la determinación del cálculo de área haremos uso del método de la balanza analítica para el cual se se hizo uso de la balanza analítica, analítica, el mismo que tiene el siguiente
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b) Dibujar con la misma escala, una figura f igura geométrica conocida (cuadrado, rectángulo, etc) cuya área que se puede calcular geométricamente, es AF.
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Para el desarrollo El peso Wc de la cuenca y Wf peso de la figura. Aplicar la regla de tres:
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2.2. PERÍMETRO DE LA CUENCA (P) Se refiere al borde de la forma de la cuenca proyectada en un plano horizontal. La mayoría de las cuencas tienen forma irregular, por lo tanto el perímetro se obtiene después de delimitar la cuenca. Es la medida medida del contorno de de la cuenca cuenca y sirve de apoyo apoyo para el cálculo de de otros parámetros. parámetros. Una Una cuenca tiene un área y un perímetro perfectamente definido, pero dos cuencas de igual área pueden tener perímetros diferentes , consecuentemente consecuentemente comportamientos diferentes , en ellas el concepto de tiempo de concentración puede variar: el tiempo de concentración concentración es el tiempo que tarda a la sección de agua considera, una gota de agua que iniciase su recorrido en el punto más lejano de una cuenca. Es una cuenca rectangular o alargada, las distancias a recorrer son mucho mayores, se puede ver que la relación area-perimetro tiene una influencia en las características hidrográficas de la cuenca. Para poder encontrar la longitud de la cuenca se tiene los siguientes pasos: CALCULO DEL PERIMETRO DE UNA CUENCA
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En este caso, el Perímetro de la cuenca Ayaviri. Es la siguiente: P = 352.2445 km
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permanentes, intermitentes y efímeros, entre el área de la cuenca (A):
Dd
LT A
Donde: LT = longitud total de ríos de la cuenca (km)
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2.7.
RELIEVE DE LA CUENCA.
Son muy importantes ya que el relieve de una cuenca puede tener mas influencia sobre la respuesta hidrológica que la forma misma de la cuenca. Los parámetros relativos al relieve son: Índice de pendiente de la cuenca (Ip). Para el cálculo del índice de pendiente, previam ente se requiere definir el término de: Rectángulo equivalente: Este representa las fórmulas geométricas de la cuenca y sirve para determinar la distribución de las alturas y sus áreas correspondientes donde el lado mayor es “L” y lado menor es “I” están
relacionadas con el perímetro (P) y el área (A) de la cuenca.
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4100 - 4200
43846,15385
4200 - 4300
49230,76923
4300 - 4400
38461,53846
4400 - 4500
29230,76923
4500 - 4600
20769,23077
4600 - 4700
10000
4700 - B
2307,692308
TOTAL
413846,1538
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4700 4600 4500 4400 4300 4200
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UNIVERSIDAD NACIONAL DEL ALTIPLANO E scuela scuela Pr ofesi fesi onal nal de de I ngenier ngenier í a C i vil