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The temperature dependence of the relative resistivity of isotropic high-density graphite, extruded graphite and graphite sheets showed an initial decrease to a minimum at around 600 °C followed by a linear increase up to 3000 °C.
In both shoot and young panicle ROC curves, FPR seemed to have a minimum at around 0.1.
After passing through its minimum at around 1000 °C, resistance of graphite materials for most experimental conditions increases monotonically with increasing temperature up to 3000 °C.
For 3.5 ≤ ΦB ≤ 1.5, EINOx decreases further with decreasing ΦB to a minimum at around ΦB = 1.5, followed by a sharp increase as ΦB approaches unity.
Neither Weber number nor surface tension was suitable for correlating bubble sizes since σ decreased steadily from pure water to IPA whilst bubble size passed through a minimum at around 5% IPA.
The Ec was found to show the minimum at around m = 4 6 and increased gradually with an increment of m and approached the crystallite modulus of polyethylene, 235 GPa (X-ray value) ∼ 316 GPa (calculate) at an infinite m value.
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The porosity-aspect ratio curve has minima at around 0.5 for oblate spheroids and 1.5 for prolate spheroids, but the cusp at 1.0 varies from convex to concave when particle size reduces as a result of the increasing role of the cohesive forces between particles.
The BII form became the lowest energy minimum for the orphan Gua7 base position with two low energy paths connecting it to the location of the original BI form and to another minimum at ε around 270° and ζ around 270°.
It is maximum at intermediate periods (0.1 0.4 s, up to 45%) and minimum at long periods (around 10%).
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 CD spectrum of Rad51 with negative double minima at around 210 and 222 nm is characteristic of an alpha-helical protein.
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