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(5.5)
(5.5) Hydraulics and Hydrology (Breadth)
| Question | Answer |
|---|---|
| Prismatic Channel | A channel in which the cross-sectional shape, size, and bottom slope are constant. |
| Steady Flow | Flow rate is constant with respect to time |
| Unsteady Flow | Occurs when discharge varies with time |
| Uniform Flow | Change in flow depth with respect to channel length is zero |
| Nonuniform Flow | Varied flow, occurs when flow depth changes along the length of the channel |
| Rapidly Varied Flow (RVF) | Short or abrupt transitions in depth |
| Gradually Varied Flow (GVF) | The change in flow depth happens over a long distance |
| Continuity | The flow rate at any two locations along a channel must be equal if flow is not added or removed. |
| Critical Depth | Normal flow depth in the channel at critical flow |
| Froude Number | Dimensionless number that is used to determine flow patterns |
| Manning's Equation | Used for solving steady and uniform flow problems |
| Chezy Formula | The first known uniform flow formula used to solve for mean flow velocity |
| Stormwater Inlets | Are entryways into storm-sewer systems for runoff collected in channels or concentrating at low points on a site. |
| Grate | An opening directly in the path of channel flow covered by a metal grate |
| Curb-Opening | A vertical opening in the curb covered by a top slab |
| Combination | Both a curb-opening and a grate placed in a side-by-side configuration |
| Slotted | A pipe cut along the longitudinal axis with perpendicular bars |
| Culverts | Are enclosed channels that run underneath embankments that allow water to pass from one side to the other. |
| Tailwater (TW) | The depth of water above the outlet invert (at the downstream end of the culvert) |
| Headwater (HW) | Max. depth of water at the culvert entrance |
| Inlet Control - Flow Capacity | Controlled by headwater depth, cross sectional area, and the type of inlet edge |
| Culvert Barrel | Always partially flow |
| Inlet Control - Flow | Passes through critical depth at the inlet and remains supercritical through the culvert |
| Hydrologic Cycle | Continuous process of evaporation, transport from the earth's surface to the atmosphere and return to the land and oceans. |
| Precipitation | Any type of water that forms in the earth's atmosphere and then drops onto the surface of the earth. |
| Rainfall (or storm) Hyetograph | A plot of rainfall depth or intensity versus time. |
| Rainfall Mass Curve | A cumulative rainfall hyetograph |
| Nonrecording Gauges | Provide only a measure of the cumulative amount at the end of a time period |
| Recording Gauges | Automatically records the amount of rainfall reaching the surface as a function of time throughout the duration of a storm. |
| Mean Areal Precipitation (MAP) | An equivalent uniform depth of rainfall over a given area, such as a watershed or a political subdivision |
| Theissen Polygon Method | A common method used to determine average precipitation over an area when there is more than one measurement |
| Isohyetal Method | The most accurate and the most time consuming of the three methods for computing mean areal precipitation. |
| Isohyet | A line on a map that connects points of equal rainfall for a given duration or a specific storm event. |
| Frequency | Used to describe the probability of a given precipitation or peak streamflow event occurring. |
| Recurrence Interval (F) | The average number of years between rainfall or streamflow events of a defined magnitude. |
| Stormwater (or direct) Runoff | Portion of precipitation that reaches the ground and flows over surfaces until it reaches its destination |
| Rational Method | Most widely accepted methodology in the US for calculating peak flow rates for stormwater conveyances. |
| NRCS Curve Number (CN) | Most commonly used method for converting rainfall quantities to runoff quantities |
| Hydrograph | A continuous plot of discharge versus time |
| Hydrograph-Discharge | Volume of water flowing past a location per unit time |
| Natural Hydrograph | Obtained directly from flow records of a gauged stream |
| Unit Hydrograph | Direct runoff hydrograph from a gauged watershed representing one unit (in or cm) of excess precipitation distributed uniformly over the watershed |
| Synthetic Hydrograph | Watershed parameters and storm characteristics used to simulate a natural hydrograph on an ungauged stream |
| Basin Lag Time | The time between the centroid of precipitation and the centroid of direct runoff. |
| Time of Concentration | The time from the end of direct runoff to the inflection point of the falling limb of the direct runoff hydrograph. |
| Sheet Flow | Shallow, slow moving flow over a parking lot |
| Channel Flow | Flow conveyed through a storm sewer |
| Shallow Concentrated Flow | Surface flow that does not resemble sheet flow or channel flow |
| Runoff Coefficient | Dimensionless ratio intended to indicate the amount of rainfall converted to runoff by a drainage area |
| Storm Intensity (I) | A function of geographic location, design frequency (or return period), and storm duration. |
| Intensity-Duration-Frequency (IDF) Curves | The relation among storm duration, storm intensity, and storm return period is represented by a family of curves |
| Drainage Area (A) | The rational equation is simply the total area that contributes surface runoff to the point of interest |
| Detention Pond | To temporally store and gradually release stormwater runoff using some type of flow control structure. |
| Retention Pond | Provide temporary non-discharge storage of stormwater runoff, meaning that the stored water can only be reduced by evaporation and infiltration |
| Stage-Storage Curve | Indicates the volume of storage available at incremental elevations within the basin |
| Absolute Viscosity | A measure of internal resistance |
| Kinematic Viscosity | A ratio of absolute viscosity to density |
| Hydrostatic Pressure | Pressure exerted by a fluid due to the force of gravity |
| Absolute Pressure | The total pressure of an object in a body of water or a container when the container is open to the atmosphere. |
| Total Stagnation Pressure | Sum of the static and dynamic pressures in a piping system |
| Static Pressure | Measured with gauges attached to the side of a pipe or tank wall |
| Dynamic Pressure | Represents the kinetic energy of water in motion and is a function of flow velocity and density |
| Constant Flow | The product of the area and velocity will be the same for any two cross sections within that channel. |
| Bernoulli Equation | Says that in a frictionless environment, energy is conserved |
| Velocity Head | A moving mass of water possesses more energy that a stationary one - the difference is kinetic energy |
| Pressure Head | A mass of water at a high pressure possesses more energy than one at a lower pressure - the difference is pressure energy |
| Elevation Head | Water at a high elevation possesses more energy than water at a lower elevation - the difference is potential energy |
| Friction Loss | The loss of pressure that occurs in a pipe because of the fluid's viscosity and the movement of molecules against the interior wall of the pipe. |
| Relative Roughness | Is the ratio of roughness height to the inside pipe diameter. |
| Darcy-Weisbach Equation | Used to calculate friction head for laminar and turbulent flow. |
| Hazen-Williams Equation | An empirical formula based on laboratory and field observations |
| System Curve | Developed by engineers to indicate the energy head needed to overcome static and friction energy losses in the hydraulic at different flow rates. |
| Pump Performance Curve | Indicates the TDH provided by the pump at different flow rates |
| Operating Point | Intersection of a pump curve and a system curve |
| Siphons | A liquid reservoir with an inverted U-shaped tube |