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In the uplands, soils are primarily moderately well drained brown calcareous silty clay loam till. In the lowlands, soils are primarily very poorly drained non-acid mucks or silty and clayey lacustrine types.
The Michigan series consists of very deep well drained soils that formed in alluvium. The Michigan soils are on alluvial flats. Slopes range from 0 to 3 percent. Mean annual air temperature is about 65 degrees F.
The pH range for most Michigan soils is 4 (acid) to 9 (alkaline), with 7 being neutral.
Kalkaska sand is the official soil of the U.S. state of Michigan. Kalkaska sand was identified in 1927 and named after Kalkaska County located in the northern Lower Peninsula of Michigan. This soil is a multi-layer soil composed of humus, light sand, dark sand, and yellowish sand.
Environmental samples were analyzed for the presence of VOCs, PAHs, Michigan 10 metals (arsenic, barium, cadmium, chromium, copper, lead, mercury, selenium, silver, and zinc), ammonia, cyanide, and nitrates-nitrites combined.
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Most soils are sandy loam and silty clay loams of moderate fertility. Fifteen soil series representing four soil orders (Alfisols, Entisols, Histosols, and Mollisols) have been mapped and characterized within the boundaries of KBS.
Part 201 of the Natural Resources and Environmental Protection Act (NREPA) is Michigans primary environmental cleanup program, and provides the regulatory framework for the majority of contaminated sites in Michigan (for information on the cleanup of leaking underground storage tank or LUST sites click here).
The soils of Michigan vary greatly. Sandy soils are dominant in the western and northern portions of the Lower Peninsula; clays and loams, in the southern Lower Peninsula. The size of particles, or texture, varies in different kinds of soil.

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