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2. Olentangy River Wetland Research Park - Wikipedia

   en.wikipedia.org/wiki/Olentangy_River_Wetland...

   The Wilma H. Schiermeier Olentangy River Wetland Research Park is an experimental wetland complex located adjacent to the campus of Ohio State University in Columbus, Ohio, United States and is part of the School of Environment and Natural Resources at the university.

3. Silt fence - Wikipedia

   en.wikipedia.org/wiki/Silt_fence

   Silt fence installed up-slope of a vegetated stream buffer. A silt fence, sometimes (misleadingly) called a filter fence, [1] is a temporary sediment control device used on construction sites to protect water quality in nearby streams, rivers, lakes and seas from sediment (loose soil) in stormwater runoff.

4. Columbus and Franklin County Metro Parks - Wikipedia

   en.wikipedia.org/wiki/Columbus_and_Franklin...

   The Columbus and Franklin County Metro Parks system was created in 1945 after a study was commissioned by the Columbus and Franklin County planning commissioners.

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   Get breaking Finance news and the latest business articles from AOL. From stock market news to jobs and real estate, it can all be found here.

6. AOL Mail

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   Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!

7. Soil nailing - Wikipedia

   en.wikipedia.org/wiki/Soil_nailing

   The most favorable conditions for soil nailing are as follows: The soil should be able to stand unsupported one to two meters high for a minimum of two days when cut vertical or nearly vertical. Also, all soil nails within a cross section should be located above the groundwater table. If the soil nails are not located above the groundwater ...

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   SYSTEM REQUIREMENTS. Mobile and desktop browsers: Works best with the latest version of Chrome, Edge, FireFox and Safari. Windows: Windows 7 and newer Mac: MacOS X and newer Note: Ad-Free AOL Mail ...

9. Frost line - Wikipedia

   en.wikipedia.org/wiki/Frost_line

   The frost line—also known as frost depth or freezing depth—is most commonly the depth to which the groundwater in soil is expected to freeze. The frost depth depends on the climatic conditions of an area, the heat transfer properties of the soil and adjacent materials, and on nearby heat sources.