Human Impacts and Management of Wetlands

 

The concept of wetland management has evolved from the destruction of wetlands as the primary management tool to the preservation and restoration of wetlands as it is practiced now.

 

Early history of wetland management

 

Wetland drainage has been the primary management technique applied to wetlands in North American since colonial times.  The common wisdom, supported by the professions of engineering, public health, and agriculture, has said that wetlands have more value when they are drained.

 

Wetland alteration

 

One model of wetland alteration (Fig.17-1) assumes three main factors influencing wetland ecosystems:  water level, nutrient status, and natural disturbances.

 

Modification of any of these directly can lead to a modification of the other two indirectly.

 

 

Most common wetland conversions:

 

A. Draining, dredging, filling

 

The most common reason for wetland loss is conversion to agriculture.  This happened early in the U.S. breadbasket (Illinois, Iowa, Minnesota).

 

Most rapid recent conversion has been the elimination of the bottomland forest along the Mississippi River floodplain.  It has been leveed for flood protection and converted to row crops. Soybean crops that could be planted late (June or July), and miss the annual floods, were a boon to this effort.

 

On the coasts, conversion to urban and industrial development has caused the greatest wetland conversion.

 

B. Hydrologic modifications

 

1.  Flood control

 

Canals have generally been constructed to convey water out of wetlands quickly, rather than as the natural sheet flow.  Levees have been constructed to keep flood waters confined to river channels rather than distribute themselves across wetlands as they do in a natural system.

 

2.  Navigation and transportation

 

Navigation canals are larger and deeper than drainage canals.  They have been constructed primarily to carry long-range barge traffic

 

3.  Industrial activity

 

Many canals are dredged to provide access to sites for oil or gas wells, refinery sub-units, to lay pipelines directly into without backfilling, or for other kinds of development.

 

C. Highway construction

 

Highway construction causes an alteration in the hydrology, elimination of sediment nourishment, direct loss of habitat for the right-of-way, loss of habitat in adjacent areas that are dredged to provide fill.

 

The least intrusive highway is one on pilings, because it will cause minimal disruption of water flow, which carries with it nutrients, fresh or salty water, sediment, detrital export, etc.  Highways on pilings are very expensive.

 

D. Peat mining

 

Northern countries have most of the world’s peat (half is in Russia, a quarter in Canada).  Most European peat is used for fuel for electric power.  In North America peat is used in horticulture and agriculture.

 

E. Mineral and water extraction

 

Phosphate mining in central Florida.  Surface mining of coal in Appalachia. Water withdrawal around Houston has resulted in as much as 18 feet of subsidence along Galveston Bay.  Karst cave-ins.

 

F. Water pollution

 

Agricultural eutrophication can lead to simplification of natural systems and spread of invasive, weedy species.  Ag runoff into Kesterson NWR in San Joaquin Valley led to concentration of selenium that killed or deformed wildlife.

 

Wetland management by objective

 

A set of common goals for wetland management might include:

 

          1.  Maintain water quality

          2.  Reduce erosion

          3.  Protect from floods

          4.  Process airborne pollutants

5.  Provide a buffer between wetlands and adjacent urban or industrial uses.

6.  Maintain a diverse community of wetland plants and a diverse gene pool.

          7.  Provide aesthetic and psychological support.

          8.  Produce wildlife.

          9.  Control insect populations.

          10.  Provide habitats for fish and other organisms

          11.  Produce food, fiber and fodder.

          12.  Expedite scientific enquiry.

 

Wildlife enhancement

 

Best management practices enhance the natural processes of the wetland involved.  This would involve maintaining natural hydrology, native vegetation, local and migratory wildlife habitats.

 

          Marsh management

 

          Water level manipulation is a very common management technique in flat landscapes where there is much water.  It is described extensively in the literature for the north-central U.S. and south-central Canada (prairie potholes), and for coastal Louisiana.  It is essentially forbidden by governmental policy in Puget Sound.

 

          Managing the (animal) managers

 

          Some animals are drawn to marsh environments and have an impact.  Included are beaver, muskrat, nutria and geese.  They have all had a long-term relationship with wetland ecosystems, and the systems may have evolved under the pressures of their impacts.  If constraints on their number are totally gone now, then some population control may be necessary.

 

 

Agriculture and aquaculture

 

Agriculture that actually works with the natural cycles of coastal or inland wetlands has been practiced for millennia.  Examples are double cropping of rice fields for rice, then crawfish or finfish.  In Europe, saltmarsh hay has been considered an important resource (Spartina patens).

 

Current practice is to dredge natural systems and create an industrial environment for the production of shrimp or other marketable seafood.

 

Water quality enhancement

 

Natural wetlands may be managed for water quality improvement.  See lecture on the last class day for elaboration of this process.

 

Flood control and groundwater recharge

 

Wetlands may, in different ways and with different efficiencies, impound water and recharge aquifers or abate flood damage.

 

Managing wetlands in changing climate

 

Coastal wetlands

 

With predicted sea level rise of 0.5 to 2 m per century for the next century, many coastal wetlands will be lost.  Accretion rates are high, however, in many coastal wetlands (they must have sediment inputs or will disappear), so the question is whether the normal accretion rates will be adequate.  For some systems they will, for others they will not.

 

Inland wetlands

 

Melting of northern permafrost tundras will probably have the greatest effects.  Decreases in precipitation and increased aridity will cause many depressional wetlands to either no longer be wet, or to become intermittent wetlands.