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Increasing values of m gives minima at correspondingly larger angles.
Melting enthalpies showed similar minima at ca. 35 wt-% PA-6,T.
The results show that with a power law hardening relationship, martensite produces two unique minima (at n=0 and 0.1).
Generally, this algorithm finds many local minima at the beginning and gradually converges to a global minimum.
The sampling depth includes two pore water chlorinity minima at ~120 and ~136 m CSF (Expedition 316 Scientists 2009).
When T = TM, f (T,φ) has two minima at φ = 0 (solid) and φ = 1 (liquid).
Furthermore, the diurnal variation shows two minima at 0900 LT and 1900 LT, during the post-sunrise and sunset hours.
The contribution of leaf litter peaked while that of deeper soils decreased to minima at peak flows.
The α-helical content of cytochrome c is transformed into β-sheet structure (single minima at 218 nm) in the presence of ≥ 0.5 mM of sarkosyl.
Specifically, both precipitation and winter temperature reconstructions show changes in interglacial maxima and glacial minima at around 3 2.8 Ma, 2 Ma, 1.3 1.4 Ma and 0.5 Ma.
The experimental results show that the pressure drop for two-phase flow in rectangular microchannels experiences minima at an aspect ratio of about 1.6.
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