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This potential "mass wasting" and decomposition of the mineral layer (between 10 and 30 cm depth) soil carbon in severely burned areas of the Alaska interior could have occurred at any time between the end of the 2015 fires and the sampling period for this study of July 2017.
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They are the interface between earth mineral layer and the biosphere.
A soil column consists of one organic ([O layer] 0 – 1 cm) and 4 mineral soil layers (A1: 1 – 5 cm, A2: 5 – 10 cm, A3: 10 – 15 cm, A4: 15 cm down to the weathered mineral layer [C layer] at 16 to 30 cm depending on region).
Additionally mineral layer soil C in soils similar to that of Hop Creek area that are mineral-stabilized only accounts for a small fraction of the soil C [ 21].
Piñon and juniper encroachment influenced the spatial distribution of the duff/litter but not the distribution of mineral layer SOC.
We also estimated aboveground (sagebrush, grass, and tree) and soil (organic and mineral layer) C stocks within each plot.
Mineral layer SOC was randomly distributed in all plots (Table 5) regardless of aboveground vegetation cover or condition.
In simulated body fluid (SBF), a biomimetic mineral layer is formed on the material resembling the function of BAGs [ 9].
These were similar to the mineral layers comprising fully mineralized Alvinella spp. tubes (see later).
The shear forces in the melt-preparation of polymer layered mineral nanocomposites facilitate the break-up of large-sized agglomerates, whereas the extent of further exfoliation of the mineral layers is determined by the compatibility between the polymer matrix and the mineral layers rather than by shear forces.
We show how the crack paths can be drastically altered by varying the elastic modulus mismatch between the organic and mineral layers, and by changing the thickness of the organic layer.
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