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Cátedra:
HIDROLOGÍA
P á g i n a 1 | 10
Trabajo Práctico No
: 2
Tema: Abstracciones, Infiltración y Exceso de Precipitación
Fecha de presentación: 02/10/2020
Presentación en término: SI NO
Integrantes:
1. GOMEZ BALMACEDA, Francisco R
Cátedra:
HIDROLOGÍA
P á g i n a 2 | 10
Ejercicio 1:
Determinar el HEP (hietograma de exceso de precipitación) del evento registrado que se
adjunta, a partir del método planteado por Horton. Como dato, se presenta la planilla
resultante del ensayo de infiltración realizado en la misma zona.
Primeramente, se obtuvo la tasa de infiltración Ft, y Ln(Ft-Fc) que el mismo obtuvo del
despeje de la ecuación de Horton
Cátedra:
HIDROLOGÍA
P á g i n a 3 | 10
Luego con los valores de Ln(Ft-Fc) y Tiempo Acumulado se confecciono una gráfica,
que nos da una tendencia a la ecuación de una recta (y=mx+a), en donde m=-k y
a=𝑙𝑙𝑙𝑙 (𝑓𝑓0−𝑓𝑓𝑓𝑓)
0
2
4
6
8
10
12
14
16
0,00 0,50 1,00 1,50 2,00 2,50 3,00 3,50 4,00
Infiltracion
[mm/hs]
Tiempo [Hs]
Variacion de la tasa de Infiltracion
y = -2,0543x + 2,7379
R² = 0,9571
-5
-4
-3
-2
-1
0
1
2
3
4
0,00 0,50 1,00 1,50 2,00 2,50 3,00 3,50 4,00
ln
(ft
-
fc)
Tiempo [Hs]
Ln vs Tiempo
Cátedra:
HIDROLOGÍA
P á g i n a 4 | 10
Luego se construyó el grafico de Variación de la tasa de infiltración para la ecuación de
Horton
-2,00
-
2,00
4,00
6,00
8,00
10,00
12,00
14,00
16,00
0 0,5 1 1,5 2 2,5 3 3,5 4 4,5 5
Infiltracion
[mm/hs]
Tiempo [Hs]
Variacion de la Tasa de infiltracion
Datos
experimentales
Curva deHorton
Cátedra:
HIDROLOGÍA
P á g i n a 5 | 10
Finalmente se obtuvo el Hietograma de Exceso de precipitaciones con la ecuación de Horton
1,80
9,00
11,59
13,14
11,34
7,41
3,44
-
2,00
4,00
6,00
8,00
10,00
12,00
14,00
05:00 05:30 06:00 06:30 07:00 07:30 08:00
P[mm]
Tiempo[mm]
Hietograma de Exceso de precipitaciones
Cátedra:
HIDROLOGÍA
P á g i n a 6 | 10
Ejercicio 2:
2- Determinar la Lamina Neta y el HEP para el evento registrado en la cuenca del TP1 y TP2,
sabiendo que:
a- El uso del suelo de la misma esta compuesta por 70 % de flora autóctona, 20 % de plantaciones,
5 % de zonas industriales y 5 % de zona urbanizada (viviendas residenciales).
b- El uso del suelo de la cuenca esta compuesto por un 70 % de zona urbanas (viviendas
residenciales), 20 % zona industriales y 10 % de plantaciones.
Aplicar el método planteado por el Servicio de Conservación de Suelos (S.C.S.). Considere Suelo
"Tipo C" y antecedentes de tormentas, en los 5 días previos, mayores a 53 mm.
Primeramente, se observó que la condición de suelo es tipo III, como la tabla 5.2.2 del libro Ven
te Chow es para condición de suelo es tipo II, se extrajeron los Valores de CN(II) para el uso de
suelo solicitado, con esto se hizo el promedio ponderado y final mente mediante la formula que
relaciona CN(II) se obtuvo CN(III).
Como se muestra en la tabla también se obtuvieron los valores de Retención Potencial Máxima y
Abstracción Inicial.
Cátedra:
HIDROLOGÍA
P á g i n a 7 | 10
Finalmente, con los valores obtenidos se confecciono el Hietograma De Excesos De
Precipitaciones
6
8
13
15
12
10
7
5
3
-
0,97
5,73
10,84
14,94
19,07
20,91
23,41 23,55
0
5
10
15
20
25
11:00 12:00 13:00 14:00 15:00 16:00 17:00 18:00 19:00
P[mm]
Tiempo [hs]
HEP caso A
Hietograma Observado
Hietograma de P Exc
Cátedra:
HIDROLOGÍA
P á g i n a 8 | 10
Se realizo el mismo Procedimiento para el caso B.
Cátedra:
HIDROLOGÍA
P á g i n a 9 | 10
Finalmente, el grafico de Hietograma De Excesos De Precipitaciones para el caso b
6
8
13
15
12
10
7
5
3
-
1,87
6,49
12,17
15,90
20,50
21,92
24,88 24,58
0
5
10
15
20
25
30
11:00 12:00 13:00 14:00 15:00 16:00 17:00 18:00 19:00
P[mm]
Tiempo[Hs]
HEP Caso B
Hietograma Observado
Hietograma De P Exc
Cátedra:
HIDROLOGÍA
P á g i n a 10 | 10
Ejercicio 3:
Determinar el hietograma de exceso de precipitación HEP a partir de la lámina neta del Ejercicio1,
asumiendo que la tasa de abstracciones es constante (Método del Índice φ)
Se consideraron los datos del ejercicio 1 y se calcularon los valores necesarios para realizar el
Hietograma de Exceso de Precipitación.
-
2,00
4,00
6,00
8,00
10,00
12,00
14,00
16,00
05:00 05:30 06:00 06:30 07:00 07:30 08:00
P[mm]
Tiempo[Hs]
Hietograma de Exceso de P.
Hietograma de Exceso de P.
7,10 9,10 11,10 12,10 10,10 6,10
2,10
6,10
2,10
1,90

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  • 1. Cátedra: HIDROLOGÍA P á g i n a 1 | 10 Trabajo Práctico No : 2 Tema: Abstracciones, Infiltración y Exceso de Precipitación Fecha de presentación: 02/10/2020 Presentación en término: SI NO Integrantes: 1. GOMEZ BALMACEDA, Francisco R
  • 2. Cátedra: HIDROLOGÍA P á g i n a 2 | 10 Ejercicio 1: Determinar el HEP (hietograma de exceso de precipitación) del evento registrado que se adjunta, a partir del método planteado por Horton. Como dato, se presenta la planilla resultante del ensayo de infiltración realizado en la misma zona. Primeramente, se obtuvo la tasa de infiltración Ft, y Ln(Ft-Fc) que el mismo obtuvo del despeje de la ecuación de Horton
  • 3. Cátedra: HIDROLOGÍA P á g i n a 3 | 10 Luego con los valores de Ln(Ft-Fc) y Tiempo Acumulado se confecciono una gráfica, que nos da una tendencia a la ecuación de una recta (y=mx+a), en donde m=-k y a=𝑙𝑙𝑙𝑙 (𝑓𝑓0−𝑓𝑓𝑓𝑓) 0 2 4 6 8 10 12 14 16 0,00 0,50 1,00 1,50 2,00 2,50 3,00 3,50 4,00 Infiltracion [mm/hs] Tiempo [Hs] Variacion de la tasa de Infiltracion y = -2,0543x + 2,7379 R² = 0,9571 -5 -4 -3 -2 -1 0 1 2 3 4 0,00 0,50 1,00 1,50 2,00 2,50 3,00 3,50 4,00 ln (ft - fc) Tiempo [Hs] Ln vs Tiempo
  • 4. Cátedra: HIDROLOGÍA P á g i n a 4 | 10 Luego se construyó el grafico de Variación de la tasa de infiltración para la ecuación de Horton -2,00 - 2,00 4,00 6,00 8,00 10,00 12,00 14,00 16,00 0 0,5 1 1,5 2 2,5 3 3,5 4 4,5 5 Infiltracion [mm/hs] Tiempo [Hs] Variacion de la Tasa de infiltracion Datos experimentales Curva deHorton
  • 5. Cátedra: HIDROLOGÍA P á g i n a 5 | 10 Finalmente se obtuvo el Hietograma de Exceso de precipitaciones con la ecuación de Horton 1,80 9,00 11,59 13,14 11,34 7,41 3,44 - 2,00 4,00 6,00 8,00 10,00 12,00 14,00 05:00 05:30 06:00 06:30 07:00 07:30 08:00 P[mm] Tiempo[mm] Hietograma de Exceso de precipitaciones
  • 6. Cátedra: HIDROLOGÍA P á g i n a 6 | 10 Ejercicio 2: 2- Determinar la Lamina Neta y el HEP para el evento registrado en la cuenca del TP1 y TP2, sabiendo que: a- El uso del suelo de la misma esta compuesta por 70 % de flora autóctona, 20 % de plantaciones, 5 % de zonas industriales y 5 % de zona urbanizada (viviendas residenciales). b- El uso del suelo de la cuenca esta compuesto por un 70 % de zona urbanas (viviendas residenciales), 20 % zona industriales y 10 % de plantaciones. Aplicar el método planteado por el Servicio de Conservación de Suelos (S.C.S.). Considere Suelo "Tipo C" y antecedentes de tormentas, en los 5 días previos, mayores a 53 mm. Primeramente, se observó que la condición de suelo es tipo III, como la tabla 5.2.2 del libro Ven te Chow es para condición de suelo es tipo II, se extrajeron los Valores de CN(II) para el uso de suelo solicitado, con esto se hizo el promedio ponderado y final mente mediante la formula que relaciona CN(II) se obtuvo CN(III). Como se muestra en la tabla también se obtuvieron los valores de Retención Potencial Máxima y Abstracción Inicial.
  • 7. Cátedra: HIDROLOGÍA P á g i n a 7 | 10 Finalmente, con los valores obtenidos se confecciono el Hietograma De Excesos De Precipitaciones 6 8 13 15 12 10 7 5 3 - 0,97 5,73 10,84 14,94 19,07 20,91 23,41 23,55 0 5 10 15 20 25 11:00 12:00 13:00 14:00 15:00 16:00 17:00 18:00 19:00 P[mm] Tiempo [hs] HEP caso A Hietograma Observado Hietograma de P Exc
  • 8. Cátedra: HIDROLOGÍA P á g i n a 8 | 10 Se realizo el mismo Procedimiento para el caso B.
  • 9. Cátedra: HIDROLOGÍA P á g i n a 9 | 10 Finalmente, el grafico de Hietograma De Excesos De Precipitaciones para el caso b 6 8 13 15 12 10 7 5 3 - 1,87 6,49 12,17 15,90 20,50 21,92 24,88 24,58 0 5 10 15 20 25 30 11:00 12:00 13:00 14:00 15:00 16:00 17:00 18:00 19:00 P[mm] Tiempo[Hs] HEP Caso B Hietograma Observado Hietograma De P Exc
  • 10. Cátedra: HIDROLOGÍA P á g i n a 10 | 10 Ejercicio 3: Determinar el hietograma de exceso de precipitación HEP a partir de la lámina neta del Ejercicio1, asumiendo que la tasa de abstracciones es constante (Método del Índice φ) Se consideraron los datos del ejercicio 1 y se calcularon los valores necesarios para realizar el Hietograma de Exceso de Precipitación. - 2,00 4,00 6,00 8,00 10,00 12,00 14,00 16,00 05:00 05:30 06:00 06:30 07:00 07:30 08:00 P[mm] Tiempo[Hs] Hietograma de Exceso de P. Hietograma de Exceso de P. 7,10 9,10 11,10 12,10 10,10 6,10 2,10 6,10 2,10 1,90