Environmental Engineering Reference
In-Depth Information
Lake
Reservoir
Especially abundant in glaciated areas; orogenic
areas are characterized by deep, ancient lakes;
riverine and coastal plains are characterized by
shallow lakes and lagoons
Located worldwide in most landscapes, including
tropical forests, tundra and arid plains; often
abundant in areas with a scarcity of natural lakes
Generally circular water basin
Elongated and dendritic water basin
Drainage: Surface area ratio usually <10:1
Drainage: Surface area ratio usually >10:1
Stable shoreline (except for shallow, lakes in
semiarid zones)
Shoreline can change because of ability
to artificially regulate water level
Water level fluctuation generally small
(except for shallow lakes in semiarid zones)
Water level fluctuation can be great
Long water flushing time in deeper lakes
Water flushing time often short for their depth
Rate of sediment deposition in water basin is
usually slow under natural conditions
Rate of sediment deposition often rapid
Variable nutrient loading
Usually large nutrient loading their depth
Slow ecosystem succession
Ecosystem succession often rapid
Stable flora and fauna (often includes endemic
species under undisturbed conditions)
Variable flora and fauna
Water outlet is at surface
Water outlet is variable, but often at some depth
in water column
Water inflow typically from multiple,
small tributaries
Water inflow typically from one or more large
rivers
FIGURE 9.14 General characteristics of lakes and reservoirs. (Modiied from Loucks and van Beek, Water
Resources Systems Planning and Management, Appendix A: Natural system processes and interactions,
United Nations Educational, Scientiic and Cultural Organization, Delft, 2005. With permission.)
28,383
30,000
25,000
20,000
13,528
15,000
12,507
7,967
10,000
7,132
5,095
3,400
5,000
2,210
1,963
847
418
426
258
0
FIGURE 9.15 Project purposes of dams in the U.S. Army Corps of Engineers National Inventory of Dams
2009 database (the y -axis is the number of dams in the database).
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