CIV 3102 Module 06: Discharge Measurements and Storage Reservoir Management

0.0(0)
Studied by 0 people
call kaiCall Kai
learnLearn
examPractice Test
spaced repetitionSpaced Repetition
heart puzzleMatch
flashcardsFlashcards
GameKnowt Play
Card Sorting

1/24

flashcard set

Earn XP

Description and Tags

Practice flashcards for CIV 3102 Module 06 covering runoff estimation, streamflow measurement techniques, and the management and hydrology of storage reservoirs.

Last updated 7:06 PM on 6/19/26
Name
Mastery
Learn
Test
Matching
Spaced
Call with Kai

No analytics yet

Send a link to your students to track their progress

25 Terms

1
New cards

Surface Runoff

The water that flows over the ground surface, consisting of overland flow and interflow, occurring when the rain falls with an intensity (II) greater than the rate of infiltration (ff).

2
New cards

Hortonian Overland Flow

Occurs when the rainfall intensity exceeds the infiltration capacity of the soil.

3
New cards

Rational Method

A method used to estimate runoff rate given by the equation Q=C×I×A360Q = \frac{C \times I \times A}{360} where QQ is the runoff rate (m3/sm^3/s), CC is the dimensionless runoff coefficient, II is the rainfall intensity (mm/hrmm/hr), and AA is the total area (haha).

4
New cards

Time of Concentration (TcT_c)

The time taken by a drop of water to flow from the furthest or most hydraulically distant part of the catchment to the outlet or pour point.

5
New cards

Kirpich Methods

Equations used to estimate the time of concentration for either overland flow in small watersheds or channel flow within the watershed, based on the longest distance of flow (LL) and slope (SS).

6
New cards

Cook's Method

A runoff estimation technique that sums numbers assigned to three factors—vegetation cover, soil type and drainage, and land slope—to calculate a catchment characteristic (CCCC).

7
New cards

Curve Number (CN) Method

A relationship developed by the Soil Conservation Service (SCSSCS) that estimates direct runoff from storm rainfall based on soil hydrologic group and land use/cover.

8
New cards

Initial Abstraction (IaI_a)

The amount of water including surface storage, interception, and infiltration that occurs prior to runoff, estimated as Ia=0.2×SI_a = 0.2 \times S in the Curve Number method.

9
New cards

Unit Hydrograph

A hydrograph with a runoff depth of 1 cm1\text{ cm} or 1 mm1\text{ mm} resulting from a rainstorm of a specified duration and areal pattern.

10
New cards

Hydrometry

The science of water measurement, including the measurement of river stage and discharge.

11
New cards

Stage

The water level of rivers, lakes, and reservoirs measured using instruments like staff gauges, float-operated gauges, or depth sensors.

12
New cards

Price Current Meter

A device consisting of six cone-shaped cups mounted on a vertical axis that rotate in flowing water to measure local water velocity.

13
New cards

Mean-section Method

A discharge computation method where discharge is calculated as Q=vi1+vi2×di1+di2×(bibi1)Q = \frac{v_{i-1} + v_i}{2} \times \frac{d_{i-1} + d_i}{2} \times (b_i - b_{i-1}).

14
New cards

Mid-section Method

A discharge computation method where discharge is calculated as Q=vi×di×bi+1bi12Q = v_i \times d_i \times \frac{b_{i+1} - b_{i-1}}{2}.

15
New cards

Rating Curve

A graph establishing the relationship between the height of water in the river (stage) and several spot discharge measurements.

16
New cards

Dilution Gauging

A tracer method for discharge measurement based on the two-component mixing equation: Q=q(C1C2)C2C0Q = \frac{q(C_1 - C_2)}{C_2 - C_0}, where C1C_1 is the tracer concentration and C0C_0 is the background concentration.

17
New cards

Manning Equation

A formula used in the slope-area method to estimate river velocity (VV) as a function of the hydraulic radius (RR), downstream slope (SS), and Manning's roughness coefficient (nn).

18
New cards

Dead Storage

The volume of water stored below the outlet level of a reservoir that cannot be released by gravity, used for sediment accumulation and ecological stability.

19
New cards

Live (Active) Storage

The usable volume of water stored between the Full Reservoir Level (FRLFRL) and the Minimum Drawdown Level (MDDLMDDL).

20
New cards

Safe Yield

The maximum dependable withdrawal that can be reliably provided from a reservoir during critical dry periods.

21
New cards

Mass Curve Method

A procedure used to estimate reservoir capacity by plotting cumulative inflow against time and determining the maximum vertical deficit below a demand line.

22
New cards

Rule Curve

A management tool that guides storage targets and release decisions, defining upper limits for maximum storage and lower limits for minimum desirable storage.

23
New cards

Flood Attenuation

The process by which a reservoir stores part of an incoming flood to reduce the peak discharge and downstream flooding.

24
New cards

Eutrophication

A water quality problem in reservoirs characterized by excess nutrients causing algal blooms, foul smell, and fish deaths.

25
New cards

Piezometer

An instrument used for monitoring reservoir safety by measuring water pressure or seepage within the dam structure.