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Throughout deglaciation, deposition within the lake was characterized by abrupt changes in grain size and in the architecture of individual sediment bodies, reflecting changing delivery paths and sediment supply, and by dynamic margin oscillations typical of water-terminating glaciers.
Changes in grain boundary composition were examined for 304 stainless steel.
The hardness variation correlates with changes in grain size and film morphology.
The elevated [CO2] induced changes in grain mineral concentration have been well studied, and lowered nutritional value of wheat by raising atmospheric [CO2] is significant1,18,19,20.
The changes in grain size and organic matter content of the top layer were also highest in these fields.
Relatively drastic changes in grain size at the internal coating interfaces did not exhibit sharp changes in microhardness.
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The changes in texture, grain size, and crystallinity were more obvious in the specimens with a thickness less than 214 nm.
To avoid changes in grains and grain barriers (GBs) from wafer to wafer, samples were selected from consecutive mc-Si wafers sharpened successively in the same ingot.
Note that the abrupt change in grain size between the fine-grained and coarse-grained parts.
Here, there was no significant change in grain size or crystallographic texture due to nanoparticle addition.
No change in grain structure near substrate surface was examined for deposition temperatures up to 135 °C.
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