Presentation is loading. Please wait.

Presentation is loading. Please wait.

THE HYDROLOGIC CYCLE. The Hydrologic Cycle The Hydrologic Cycle - Fresh Water Storage Reservoir % of Total Fresh Water Glaciers (Frozen)76% Groundwater22%

Similar presentations


Presentation on theme: "THE HYDROLOGIC CYCLE. The Hydrologic Cycle The Hydrologic Cycle - Fresh Water Storage Reservoir % of Total Fresh Water Glaciers (Frozen)76% Groundwater22%"— Presentation transcript:

1 THE HYDROLOGIC CYCLE

2 The Hydrologic Cycle

3 The Hydrologic Cycle - Fresh Water Storage Reservoir % of Total Fresh Water Glaciers (Frozen)76% Groundwater22% Rivers & Lakes < 2% Although it only makes up < 2% of total fresh water on earth, surface water is the most utilized and perhaps precious natural resource!

4 The Hydrologic Cycle How Does Water Move Within The Cycle?

5 The Hydrologic Cycle 1) RIVER SYSTEMS A)Important source of fresh water. B)Most important agent of erosion. C)Most abundant continental landform. D)Essential to agriculture & industry

6 Three Main Parts To A River System Collection system; Transportation system; Dispersing system

7 DIFFERENCES IN RIVER SUB-SYSTEM CHARACTERISTICS

8 The Collection System – A Drainage Basin

9

10 Types of Drainage Basins – Controlled by Geology

11 The Dynamics of Stream Flow 1)Velocity 2)Discharge 3)Channel Parameters 1)Roughness 2)Dimensions 4)Sediment Load 5)Gradient and Base Level The Transportation System

12 1) VELOCITY – Straight Channel

13 1) VELOCITY – Curving Channel

14 High V: Erosion LowV: Deposition 2) GRADIENT

15 MEASURING DISCHARGE (Q): Q m 3 /sec = V (AVG. ) X Width meters X Depth meters

16 4) SEDIMENT LOAD AND TRANSPORTATION

17 TRANSPORTING SEDIMENT

18 Ideal Stream Profile Increasing discharge, velocity & sediment load Decreasing gradient, turbulence & competence Base level – level of deepest possible erosion.

19 Dynamic Equilibrium – “You can never change just one thing about a stream.” The sensitive, ever-evolving balance between erosion and deposition. Graded Stream: erosion = deposition. If deposition > erosion, stream builds up its bed, thus increasing gradient and average velocity to restore balance. If erosion > deposition, stream erodes bed, decreasing gradient and velocity.

20 Departures from Equilibrium Waterfalls – signs of a shifting balance: increased discharge or gradient

21 Dam That Stream! A System Out of Balance Dam Effects  Upstream deposition  Discharge of clear, turbulent water & potential erosion.  Elimination of floods (reduced competence);  Choke off down- stream sediment flow.  Disturbed ecosystems

22 Meandering Streams

23 Floodplains have a purpose!


Download ppt "THE HYDROLOGIC CYCLE. The Hydrologic Cycle The Hydrologic Cycle - Fresh Water Storage Reservoir % of Total Fresh Water Glaciers (Frozen)76% Groundwater22%"

Similar presentations


Ads by Google