Browsing by Subject "Soil compaction"

Now showing 1 - 4 of 4
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    Effects of Soil Compaction and Organic Matter Removal on Ground-flora Diversity in the Great Lakes Forests
    (University of Minnesota Duluth, 1996) Host, George E
    Soil is one of the key factors regulating the productivity and diversity of forest ecosystems. Soil organic matter resulting from the decomposition of leaf litter provides an important reservoir of nutrients for future forest growth. The structure of soils, in conjunction with soil texture, determines the ability of a soil to retain moisture. Forest harvest operations, through the use of heavy equipment and slash management practices, have the potential to damage soil structure and remove organic matter from the forest floor. We lack a clear understanding, however, of which soil types are most susceptible, and what degree of impact soils can sustain before the potential productivity and diversity are reduced. To address this issue, a nationwide Long-Tenn Soil Productivity (LTSP) study was initiated to assess the effects of logging operations on the structure and organic matter content of forest soils (Powers et al. 1990). In the Lake States, study plots were installed on the Chippewa, Ottawa, and Huron National Forests. These plots represent the range of soil textures which occur across the Lake States: silt loams, clays, and sands, respectively. Using an experimental approach, different levels of soil compaction and organic matter removal were applied to harvested aspen stands across this soil gradient. Aspen reproduction, forest biomass, and the diversity of the ground-flora layers are being monitored on an annual or biennial basis to assess their response to these treatments. The results of this experiment will allow us to predict the degree of protection required to sustain productivity and floristic diversity in aspen stands across a range of common Lake State soil types. The Lake States LTSP study has included an analysis of floristic diversity to the suite of measurements made on the study plots. Biodiversity and forest management has become a critical issue in the Lake States Forests. In Minnesota's Generic Environmental Impact Statement, diversity was one of the key focal issues. Ground-flora has received wide use in ecological indicators and in ecological land classification systems across the Great Lakes (Spies and Barnes 1986, Host and Pregitzer 1991, Coffmann et al. 1983, Shadis et al. 1995). A primary objective of this study was assess the response of the ground-flora community to the soil compaction and organic matter removal treatments within the LTSP study. This response can be assessed not only on a year-by-year basis, but also in describing the rate and trajectory of recovery toward the compositional state of the uncut forest.
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    Performance-Based Measurement of Optimum Moisture for Soil Compaction
    (Minnesota Department of Transportation, 2013-11) Hansen, Bradley J.; Nieber, John L.
    Part of the challenge achieving maximum field density in subgrade materials is transferring the optimal compaction and moisture content data from laboratory testing to the field. This research investigated the proficiency of four different instruments at accurately predicting moisture contents of three subgrade soils (loam, silt, silty/clay) commonly used in Minnesota roadway construction projects. The four instruments were; DOT600 (moisture content), WP4C dewpoint potentiometer (matric suction), the Button Heat Pulse Sensor (BHPS) (temperature rise vs. moisture content), and an exudation pressure test device. The DOT600 showed a strong correlation between the output period (measured in micro-seconds) and volumetric water content. The WP4C did not accurately measure matric suction for any of the loam, silt or silt/clay soils at suctions below 250 kPa. Published data shows that the matric suction of soils compacted at optimum moisture content is usually in the range of 200 – 300 kPa. The BHPS showed a strong correlation between measured temperature rise and water content but in its current configuration is not rigorous enough to withstand field conditions. The exudation pressure device was applied to soils compacted in a AASHTO T99 mold at various moisture contents. Water was exuded from the packed samples at pressures between 100 and 500 psi corresponding to AASHTO-T99 moisture contents of 10 to 25 %. Accurate moisture content readings from any of these instruments may not be as important as a more precise and simple calibration between the measurement units of the instrument and the optimum moisture content determined from the AASHTO T99 test.
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    Soil Compaction in Upper Midwestern Crop Production
    (2024-09-12) Bolwerk, Gabrielle; DeJong-Hughes, Jodi; Daigh, Aaron
    This fact sheet explains the causes, effects, diagnosis, and management of soil compaction in upper Midwestern cropping systems.
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    Tillage and wheel traffic affect soil compaction
    (University of Minnesota, Agricultural Extension Service, 1979) Nelson, W.W.; Bauder, J.W.; Blake, G.R.; University of Minnesota, Agricultural Extension Service; Voorhees, W.B.