At intermediate compositions and T < 873 K, a BCC alloy (B2) phase occurs, which has superior separation characteristics to those of the FCC phases that form at high Cu and high Pd compositions.
The preference of rosmarinic acid in intermediate compositions and in methanol-rich or ethanol-rich mixtures could be explained in terms of the higher acidic behavior of rosmarinic acid molecules interacting with the hydrogen acceptor groups in methanol or ethanol.
Specific ultraviolet absorbance measured at 254 nm (SUVA254) performed better as a discrimination index than did two previously recommended absorbance ratios, both in terms of making better predictions of intermediate compositions and in exhibiting a more linear correlation with PAHA mass ratio.
The number of 'free' Li+ ions away from the particle surface is largest for the intermediate composition x=35 and at 290 K (∼23% of the total number of lithium ions in the system); smaller for x=50 (∼11% at both temperatures), and even smaller at x=20 (∼5% at 290 K and ∼9% at 330 K).
The protamine-like type encompasses a highly structurally heterogeneous group of proteins with intermediate composition between protamines and histones (lysine- and arginine-rich) which are evolutionarily related to histone H1 [ 13, 17].
All the indices revealed a significant reduction of the bacterial richness and diversity in the root samples (TukeyHSD, p < 0.05; Figure S1), while the rhizosphere microbiota displayed an intermediate composition between soil and root samples.
The Bradys geologic framework is characterized by a highly faulted Oligocene to Quaternary ~1500-m-thick ~1500-m-thick ~1500-m-thickterfingering and distratigraphicafic to intermediate composectionlava flofs, ash flow tuffs, and varinterfingeringry units including siltstone, diandmite, andiscontinuousFaulds et al. 2012).
For example, continental crust has been approximated as "granodiorite", "dacite", or other intermediate composition igneous/volcanic rocks (e.g., Taylor and McLennan 1985), and therefore distinguishing eroded continental crust from wind-blown dacitic ash is challenging.
The end materials ZrMn2, ZrNi2 and the intermediate composition ZrMn1.5Ni0.5 liberate hydrogen only marginally with very poor desorption kinetics.
