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CE 3354 Engineering Hydrology Lecture 2: Surface and Groundwater Hydrologic Systems.

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Presentation on theme: "CE 3354 Engineering Hydrology Lecture 2: Surface and Groundwater Hydrologic Systems."— Presentation transcript:

1 CE 3354 Engineering Hydrology Lecture 2: Surface and Groundwater Hydrologic Systems

2 Outline Fundamental Definitions Water Budget Surface Water Systems Groundwater Systems

3 What is Hydrology? Study of the occurrence, circulation, storage, and distribution of surface and groundwater on the Earth. Engineering hydrology is the quantification of amounts of water at various locations (spatially) as a function of time (temporally) for surface water applications.

4 What is a Watershed? Topographic area from which water collects and discharges as surface streamflow through or past one point of interest (outlet, mouth, pour point, or engineering site). The area on the surface of the Earth that drains to a specific location In groundwater a similar concept is called a groundwater basin – only the boundaries can move depending on relative rates of recharge and discharge

5 Hydrologic Systems A hydrologic system is simply a collection of connected components that form the hydrologic cycle These components can be grouped into subsystems, treated separately, and the results combined according to interactions between the subsystems (CMM pg 5)

6 Hydrologic Cycle

7 Surface Water Component

8 Groundwater Component

9 As a System Diagram

10 Another View of Hydrologic Cycle

11 Water Budget The water budget, or hydrologic balance is simply the expression of the conservation of mass in hydrologic terms for a hydrologic system. Generally it is expressed as a rate (or volume) balance. The hydrologic equation is the fundamental tool in hydrology to describe amounts of water in storage in different compartments at different scales. The equation expressed in “words” is Rate of inflow - Rate of outflow = Rate of change of storage + Rate of internal mass generation.

12 Water Budget Compare to Equation 2.2.4 in CMM; Except for notation, and absence of internal generation they equations are identical.

13 Surface Water Systems

14 Surface Water Budget From the surface water system diagram, an appropriate budget would be Inflows: Rainfall; Surface water from outside boundary, recharge from Groundwater. Outflows: Evapotranspiration; Surface water leaving boundary; Infiltration to groundwater. Storage: Water levels in lakes, rivers, ponds within the boundary; water stored on leaves and other surfaces.

15 Ground Water Systems

16 Ground Water Budget From the surface water system diagram, an appropriate budget would be Inflows: Groundwater flow from outside boundary; Recharge from surface system (via infiltration) Outflows: Groundwater flow out of the boundary; Discharge (pumping; springs) to surface system Storage: Water levels in aquifers within the boundary

17 The Combined System

18 Conceptual Model of Water Budget Infiltration (mm)

19 Water Budget Example

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22 Aquifers An aquifer is a geologic formation that stores and transmits water Storage is in the interstitial (pore) space between the solid particles that comprise the formation Transmission is in the interconnected pore space

23 Porosity and Water Content

24 Types of Porous Structure

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26 Moisture Zones

27 Aquifer Types

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30 Summary Definitions Surface water system introduction Subsurface water system introduction Concept of a water balance Porous media and aquifers

31 Next Time Hydrologic Data Watershed Delineation


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