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Soil particle size, soil carbon, respiration, microbial biomass and extractable nitrogen were also determined.
Element size, soil stiffness, damping, boundary conditions and finite element method (FEM) software have been varied.
The effects of particle size, soil development/alteration and diagenesis processes on the source discrimination were investigated.
10 g air-dried and sieved (0.45 μm, pore size) soil samples were extracted in triplicate with DCM for 10 hr in a soxhlet extractor.
We found P. calleryana survival and establishment to be a function of seedling size, soil humic matter content, and sowing treatment.
Rill erodibility could be satisfactorily estimated by the median soil grain size, soil cohesion, water stable aggregate and root mass density.
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Nonetheless, modeling applications for water resources management require knowledge of plot-scale (1 5 m grid-size) soil moisture by using measurements through spatially-distributed sensor network systems.
The fine particle-size fraction contained a high amount of alkyl-C and high humification, which implied that the undecomposed recalcitrant substances tended to accumulate in fine particle-size soil fractions.
Loess soils are aeolian deposits of primarily silt sized soil particles, which are often lightly cemented.
This paper firstly introduced the design of an innovative guided electromagnetic wave sensor called Time Domain Reflectometry (TDR) tube that can non-destructively monitor the freeze/thaw process in standard sized soil specimens.
Here, we present the first results using 5 mm sized soil aggregate samples with contrasting C-contents in which we obtained maps of organic matter distributions in relation to the pore networks at the aggregate scale.
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