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aquifer –
geological formation of permeable rock, gravel, or sand containing or
conducting groundwater |
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barrens –
also known as shrubland, are derived by drought-induced landscape-level
fires in woodlands or savannas. |
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benthic organisms –
organisms living on or in the benthon (bottom) of a lake |
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best management practices (BMP) –
a measure used to control the
adverse stormwater-related effects of development. BMPs include structural
devices (e.g., swales, infiltration basins, and detention basins) designed
to remove pollutants, reduce runoff rates and volumes, and protect aquatic
habitat. BMPs also include non-structural urban site design measures such
as minimizing impervious surfaces, utilizing native landscaping, and
establishing buffers along streams, lakes, and wetlands. Finally, BMPs
include institutional measures such as public education efforts to stop
dumping of household chemicals into storm drains. |
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biotechnology –
the use of living organisms or other biological systems in
the manufacture of drugs or other products or for environmental management. |
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bog
– glacial
relict wetlands restricted to hydrologically isolated kettles. |
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buffer –
strip of land along a stream, lake, or wetland planted with native
vegetation. The width of the buffer is measured from the ordinary high water
mark of the perennial or intermittent stream, lake or pond, or the edge of a
wetland. Development within buffers is typically limited to improvements
such as piers or docks necessary to allow access to the water. |
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calcareous
– groundwater where tufa (recrystallized calcium and magnesium carbonate
deposits) forms. |
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channel –
any river, stream, creek, brook, branch, natural or artificial depression,
ponded area, flowage, slough, ditch, conduit, culvert, gully, ravine, wash,
or natural or manmade drainage way, which has a definite bed and bank or
shoreline, in or into which surface or groundwater flows, either perennially
or intermittently. |
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detention basin –
a facility designed to temporarily store runoff either on,
below, or above the ground surface, accompanied by controlled release of the
stored water. |
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erosion –
the general process whereby earth is removed by flowing water, wave action,
or wind. |
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fen
– created
and maintained by the continuous flow of mineralized groundwater
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filter –
layer of fabric, sand, gravel, or graded rock placed between bank revetment
and soil for the following purposes: 1) to prevent the soil from moving
through the revetment by piping, extrusion, or erosion; 2) to prevent the
revetment from sinking into the soil; and 3) to permit natural seepage from
the streambank, thus preventing the buildup of excessive hydrostatic
pressure. |
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floodplain –
a relatively level, continuous area adjacent to a lake or
stream channel which is submerged during times of flood; and natural
depressions including wetlands which are periodically inundated by
stormwater. |
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floodway –
the channel and that portion of the floodplain adjacent to a stream or
watercourse which is needed to convey the anticipated existing 100-year
frequency flood discharge with no more than a 0.1 flood increase in stage
due to any loss of flood conveyance or storage and no more than a ten
percent increase in velocities. In some cases, the floodway may include that
portion of the floodplain containing 90% of the floodplain storage volume.
Floodways can be calculated based on either existing or future land use
runoff condition. |
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graminoid –
containing a formation of Sphagnum peat |
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greenway –
scenic trail or route set aside for recreational activities |
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heronry –
place where a colony of herons breeds |
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hydric –
pertaining to, or adapted to a wet or moist environment |
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hydrologic budget –
the components of
atmospheric water which include precipitation, evaporation, surface runoff,
subsurface runoff, and groundwater recharge. |
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impervious surfaces –
manmade or natural
materials through which water, air or roots cannot penetrate and which
prevents the movement of surface water down to the water table. |
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littoral zone –
the region of freshwater lake beds from the sublittoral zone
up to and including damp areas on shore. |
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mainstem –
the principal course of a river |
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marsh –
hydrologically cyclical wetlands dominated by emergent reed, graminoids,
cyperoids, and aquatic plants. Basin marshes occur in glacial
kettles, potholes and swales, most often found in community complexes with
savannas or prairies. Streamside marshes are restricted to the
floodplains of creeks and rivers. |
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meanders –
a meander in a river consists of two consecutive loops, one flowing
clockwise and the other counter-clockwise. |
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multi-use trail –
trails that allow more than one type of recreational use,
i.e. hiking, biking, cross-county skiing |
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native vegetation –
plants that are inherent and original to an area |
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nonpoint source pollution –
pollution which has no single
discharge point or origin. Pollutants are usually comprised of sediment,
organic compounds, toxic metals and various pathogens. Sources of nonpoint
source pollution typically include urban and agricultural runoff and
effluent from septic systems and landfills. |
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pervious surfaces –
areas that can be penetrated by moisture |
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panne –
unique interdunal wetlands on calcareous moist sands of the lake plain
within one mile of Lake Michigan. |
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point source pollution –
pollution which is discharged from a single point or
structure. Most often, a point source is a pipe delivering effluent from a
wastewater treatment facility or industrial facility. |
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prairie –
area dominated by grasses on mineral soil. Trees may be present, but less
than 10% of the area has a tree canopy. Four natural communities:
fine-textured-soil prairie, sand prairie, gravel prairie, dolomite prairie. |
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riparian zone –
bank area of a river or other body of water |
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riverine –
situated or dwelling beside a river |
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runoff –
water which moves through the landscape, either as surface or subsurface
flow, which originates from atmospheric precipitation, initially in the form
of rain or snow. Runoff is that portion of the hydrologic budget which
produces surface water in streams, lakes, and wetlands. |
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savanna –
wooded community with graminoid groundcover. Two natural communities:
fine-textured-soil savanna and sand savanna. |
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sedge – any
rushlike or grasslike plant of the genus Carex, growing in wet places. |
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sedge meadow –
sedge dominated grasslands with wet prairie grass
co-dominants on organic or sand substrates. |
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seep – a
small spring, pool, or the like, where liquid from the ground has oozed to
the surface. |
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sinuosity –
a curve, bend or turn. |
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wetland –
area with saturated or flooded soils fro all or most of the year. This
condition excludes or greatly reduces oxygen availability to plant roots and
soil dwelling animals and decomposers. This oxygen deficiency is the most
important factor determining the function and composition of wetlands.
Important factors differentiating the six wetland natural communities
recognized are fire frequency, water source, water chemistry, and
topographic location. Wetland types: marsh, bog, fen, sedge meadow, panne,
and seep & spring.
Glossary
in printable pdf file
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