A Comparison of a Quick Evaporative Technique for Determining Diffusivity with the One-step Outflow Method: Comparison of Water Retention Characteristics of Soil C Horizons Developed in Three Glacial Lobes; C Horizons of Wisconsin Soils ; A Review of Woodfordian and Subsequent Glacial Geology in Parts of Eastern Wisconsin |
Contents
Laboratory setup for the quick evaporative | 7 |
Moisture distribution data for sample | 11 |
Curves of diffusivity as a function of gravi | 14 |
26 other sections not shown
Common terms and phrases
acid Aeric Alfic analysis Aquic areas Argiudoll association bars basis bedrock bulk density calc calcareous characteristic clay CONCLUSION conductivity cores curves deposits depth determined developed differences diffusivity distribution et al evaporation evaporative method field Figure function Geological and Natural glacial Glossoboralf gravel gravimetric Green Bay Haplorthod heat Histosol Hole horizon hydraulic influence Lake Lake Michigan Langlade limit lines loamy Lobe map unit meter of silty method Michigan miles moisture content moraines Nashville Natural History Survey Ochraqualf Onaway orders outflow parent material maps percentages Pleistocene plot potential presented Proc produced properties quick evaporative represented respectively Rocks roughly sample sand sandy loam saturated showed silt silty cover similar Soil Sci Soil Science Spodosols surface Table taken Tension texture till Typic Haplaquoll Typic Hapludalf Univ values variability vertical water content weathering Wisconsin