EHG311

 

 

                 EHG 311 COURSE IN DETAILED

 

 

COURSE NAME : Applied Hydrology

 COURSE NUMBER : 311

 

PART II

COURSE SYLLABUS

Hydrologic Cycle,  basic equations, Precipitation, average and surface runoff, hydrographic analysis and components, Floods prediction. (Field trip one day in Jeddah district).

Instructor Information

  ¨ Name of the instructor: Dr. Masoud  Eid  Masoud  Al-ahmadi

                                             · Assistance Professor  

     · Faculty of Earth Sciences

                                             · Hydrogeology Department

 

   ¨ Office location:   Faculty of Earth Sciences/ Building No. 55/ First Floor/ Office No. 213

    ¨ Office hours:      :  11.00 - 1:30 Sat-Tues., 10:00- 1:30 Wed

   ¨ E-mail                 : m_al_ahmadi@ yahoo.com

    ¨Tel. Office          : 6952689

    ¨ Fax                      : 6952095

Course Information

 

    · Course name and number:  Applied Hydrology ( EHG 311 )  (Credit Units: 3)

    · Course meeting times: Building 27,  Room 210/ Time  10-10:50  Sat – Mon 

                                         Lab. Hours: 1:00 – 3:00 Sat. (Hydrology Laboratory), Building 55/Room 142

   ·Course website address http//www.edu.sa/malahmadi

   · Course prerequisites and requirements: Math 101, EMR 102

   ·Description of the course (what, why, philosophy, teaching methodology)

       It is a Surface Water Hydrology Analysis of the basic principles of surface hydrology. The precipitation, evapotranspiration, infiltration, and run off components of the hydrologic cycle are discussed in detail. Topics include water balance, precipitation analysis, unit hydrograph theory and Flood prediction.

 

Course Objectives

    • Students will obtain an understanding of hydrologic processes, particularly the

processes of precipitation, evaporation, infiltration, and surface water.

    • Students will learn about methods of hydrologic analysis, including unit hydrograph,

flow routing, statistical methods and frequency analysis in hydrology.

    • Students will learn about methods of hydrologic design, including the development of

design storms and design flows.

    • Students can estimate the time of concentration of a watershed, based on

information about surface type and travel length, slope, and rainfall intensity.

        • Students can estimate peak discharges and develop unit hydrographs and design

hydrographs for small-scale watersheds.

    • Students have a basic understanding of hydrologic and hydraulic methods of flow

routing.

    • Students can apply current software to the hydrologic design of small-scale rural or

urban watersheds.

Prerequisites by Topics:

    • Calculus

    • Statistics

    • Fluid Mechanics

    • Open channel Flow

..

  Computer Usage: Students have the option to complete homework using compute        applications such as spreadsheets and word processors

 

  Approach: The homework and tests are designed to train the students to think about a variety of hydrology-related problems, show the interconnection between the various components of the hydrologic cycle.,  . In the context of this design process, students develop skills that constitute design components:

                    analysis and synthesis skills, creative and original thinking,

                    problem-solving when the problem itself and problem constraints

                    are not clearly defined.

Outline :

Week #

Date

Topic

What is Due?

1

Sept.10

Introduction

 

Copy lecture desk  

Sep.12

Hydrologic  Cycle

¨Definition

¨Hydrologic  Cycle components

 

2

Sept.17

Rainfall

 

 

 

Sept.19

Methods  of average Rainfall

 Arithmetic Average Method 

Thiessen Polygon Method    

 Isohyetal Method

 

Homework assignment #1

3

Sept.24

Evaporation   &  Evapotranspiration

Meteorological factors

 

 Sept.26

Measurements of Evaporation & Evapotranspiration

Direct Measurement in the field

 

4

Oct.1

Calculation of Evaporation &   Evapotranspiration

 

 Homework assignment #  2

 

Oct.3

Runoff

 

5

Oct.8

 

Infiltration

 Porosity

 Hydraulic conductivity

 Moisture/water content

 

 

Oct.10

F-Index

Horton's Model

Infiltrometer

measurements of actual infiltration.

 

 

6

Oct.15

 

Water Budget Equation

 

Homework assignment #3

 

Oct.17

First    Exam

 

7

Oct.22

 

 

Channel  flow  Measurements

Introduction

Definition 

 

 

 

Oct.24

Water Stage  Gages

 

 

8

Nov. 12

Water Stage  Gages ( Continue )

 

Nov. 14

Discharge

Measurements of Discharge

Homework assignment #4

 

9

Nov. 19

 

Chemical Gagging

Other Methods of Measuring Discharge

 

 

 

 

Nov. 21

Stage discharge ( Rating ) Curve 

 

10

Nov.26

 

SlopeStageDischarge  Curve

 

 

Nov.28

 

Extension of Rating Curve

 

 

11

 Dec.3

 

Hydrograph

Introduction

Definition

Hydrograph components

Type of Hydrograph

  

 

Dec.5

 

Hydrograph  Separation

Methods of Separations

 

 

12

 Dec.10

 

Unit Hydrograph

 

 Dec.12

 

Estimating Unit Hydrograph from  Hydrograph

 

13

 Dec.17

 

Estimating Unit Hydrograph for different Precipitations

 

 Dec.19

 

Synthetic Unit Hydrograph

 

14

 Dec.24

 Flood  Routing

 

Dec.26

Second     Exam

 

 

15

Dec.31

Revision

 

 

Jan.2

 

Revision

 

 

 

 

Final Exam

 

 

 

 

 

 

 

  

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

References:

 ¨ Chow, V. T, D. R. Maidment, and L. W. Mays.  1988.  Applied Hydrology.   McGraw-Hill, Inc.

 ¨Viessman, Jr. W., Lewis, G. R., and Knapp, J. W., 1989.  Introduction to hydrology.  Harper & ow publishers. 3th   Ed. New York, 780 p.

 ¨Subramanya, K., 1988. Engineering hydrology. Tata McGraw Hill Publishing Company Limited. 2th  Ed. New Delhi,  316 p.

 ¨Schwartz, F. W., and Z hang, H., 2003. Fundamental of Groundwater. John Wily &Sons, Inc.

 ¨McCuen, R.H., 1998. Hydrologic Design and Analysis; Prentice Hall, New  Jersey, 814 pages.

 ¨Search in Internet subject related to course topics (http://www Hydrologic Parameters, Surfaces Runoff, Unit Hydrographs etc…)

 ¨http://www2010.atmos.uiuc.edu/(Gh)/guides/mtr/hyd/smry.rxm1

 

Grading Policy

 Your grade depends on in-class participation and performance on your quizzes, exams, and assignments.

 Quizzes: Bi-weekly quizzes will be brief (about 5 mins.) and are intended to help prepare you for the exams.

 Exams: Exams will be a combination of multiple choice and short-answer questions, and will also have components similar to the work you do on the problem sets. Make-up exams can be arranged if extraordinary circumstances prevent you from taking the exam at the scheduled time. Be sure to arrange for a make-up as soon as extenuating circumstances arise.

 

 Assessment of final course grade will be based on:

Quizzes                   10%

Homework              20%

Exam 1                    15%

Exam 2                    15%

Final  Exam             40% 

  TOTAL                     100%
 

 

Hydrogeology Links

Organizations/Links Pages

    USGS Water Page

    National Ground Water Association

    Geological Society of America

    Hydrology Web Homepage

    U.S . Environmental Protection Agency (EPA) Homepage

    NYSDEC Division of Water

 

REVIEW OF BASIC MATHEMATICS

 The following short review of basic mathematics may be useful to you in solving the problems.

 

    LOGARITHMS

     The logarithm of a number is the exponent of that power to which a base number must be raised to yield the value of the number. There are two bases. Common logarithms use the base 10 and are designated by log. Natural logarithms use the base 2.718… and are designated by ln. The number 2.718… is also designated by the letter e.

  The log of 25.7 is 1.409933 and may be found by entering the number 25.7 on your calculator and then pressing the “log" key. This means that if you take the number 10 and raise it to the 1.409933 power, you will get 25.7. You can do this on your calculator by entering 10, pressing the “yx" key, entering 1.409933 and then pressing the “=” key. This process is known as finding the antilog or inverse log of a number. Thus, if 1.409933 is the log of 25.7, then 25.7 is the inverse log of 1.409933.

 The ln of 25.7 is 3.246491 and may be found by entering the number 25.7 on your calculator and then pressing the "ln x" [or “ln"] key. This means that if you start with e and raise it to the 3.24691 power, you will get 25.7. If you have an “ex" key on your calculator, you can enter 3.246491 and the press the “ex" key to yield 25.7. If you don't have an “ex" key, you can still perform the operation. Since we are finding the inverse ln, enter 3.246491 and press the “INV" key followed by the “ln" [or "ln x"] key.

  

Logarithms have the following relationships:

                 log ab = log a + log b

                 log a/b = log a -log b

                 log an = n log a

 Both the natural and common logarithm of 1.0000 is 0. The logarithm of any number greater than 1.0000 is positive. The logarithm of any number less than 1.0000 is negative.

             The log of 10 is 1, the log of 100 is 2, the log of 1000 is 3, etc.

 

 

    EQUATIONS FOR AREA

                Area of a circle with radius r

     A =  pr2           (pi = 3.1416)

              Area of a triangle with a base b and altitude h    

    A = 1/2 bh

Area of a rectangle with sides a and b

    A = ab

             Area of a parallelogram with sides a and b and an included angle z

    A = ab sin z.

             Area of a trapezoid whose parallel sides are a and b and with an altitude h

    A = 1/2(a + b)h.

 

    EQUATIONS FOR CIRCUMFERENCE

             Circumference of a circle with a diameter  d

        C = p d.

 

Circumference of a triangle of sides  a, b and  c

        C = a + b + c.

 

Circumference of a rectangle with sides a  and  b

                    C  = 2 a +  2b.

 

    EQUATIONS FOR VOLUME

             Volume of a regular prism

    V = area of base x altitude.

             Volume of a pyramid

    V= 1/3 area of base x altitude.

             Volume of a cylinder with radius r and height h

    V = p r2 h

Volume of a cone with radius r and height h

    V = 1/3 p r2 h

 

    EQUATION OF A STRAIGHT LINE IN RECTILINEAR 

    COORDINATES

                             y  =   m x + b

        where :

        m     is the slope of the line 

        b     is the intercept of the y axis.

 

    TRIGONOMETRIC FUNCTIONS OF A RIGHT TRIANGLE

             Sine A = sin A = a/h

            Cosine A = cos A = b/h

            Tangent A = tan A = a/b

            Cotangent A = cot A = b/a

            Secant A = sec A = h/b

            Cosecant A = csc A = h/a

 

    DIFFERENTIALS

             d ax = a dx

             d (u + v) = du + dv

             d uv = udv + vdu

             d (u/v) = (vdu – udv)/v2

             d xn = n xn-l dx

    d xy = yxy-1 dx + xy ln x dy

             d ex = ex dx

             d eax = a eaxdx

             d ax = ax ln a dx

             d ln x = x -1 dx

             d log x = x -1 log e dx

 

 


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10/29/2010 8:54:49 AM