agrosoil.blogspot.com
AGRO SOIL: August 2008
http://agrosoil.blogspot.com/2008_08_01_archive.html
Agronomy, Soil, and Environment. In this recent time, we face the truth about land resources decrease, that's means we should race to increase the agriculture products in order to offering feeds and seeds for helping human being. We invited you to joint with us in share and discuss about many problems and solutions about how to increased the agriculture product, so welcome in domain about "we feed the world". Subscribe to: Posts (Atom). Powered by TagBoard Message Board.
agrosoil.blogspot.com
AGRO SOIL: September 2008
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Agronomy, Soil, and Environment. Mollisols from Greenwood County, Kansas. Pittstown series: New Emgland soil profiles. Pittstown soils are in a catena with well drained Newport soils, poorly drained Stissting soils and very poorly drained Mansfield soils. These soils are mapped primarily in the Narragansett Basin. And in the Boston Basin in southern New England (taken from. Http:/ nesoil.com/images/pittstown.htm, page maintained by Jim Turenne). Subscribe to: Posts (Atom).
agrosoil.blogspot.com
AGRO SOIL: Mollisols from Greenwood County, Kansas
http://agrosoil.blogspot.com/2008/09/mollisols-from-greenwood-county-kansas.html
Agronomy, Soil, and Environment. Mollisols from Greenwood County, Kansas. Im writing a book on the Great Plains. Id like to use this photo in it. Owner of photo, please contact me. 2 April 2011 at 11:39. Subscribe to: Post Comments (Atom). Powered by TagBoard Message Board. Mollisols from Greenwood County, Kansas. Pittstown series: New Emgland soil profiles.
agrosoil.blogspot.com
AGRO SOIL: Pittstown series: New Emgland soil profiles
http://agrosoil.blogspot.com/2008/09/pittstown-series-new-emgland-soil.html
Agronomy, Soil, and Environment. Pittstown series: New Emgland soil profiles. Soils are moderately well drained soils formed in loamy dense till derived primarily from carboniferous rocks and minerals dominated by sandstone, slate, schist, phyllite, and shale. The dark colored till is due to the high carbon contained in minerals within the parent rocks. The dark colors of the soil causes some difficulty to determine the depth to estimated average seasonal high water table.