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The basal distance of montmorillonite (d 001) evolved from 14.21 to 14.98 Å.
As a result of the clay saturation by Na+, the basal distance (d001) of montmorillonite decreased from 15.7 to 13.2 Å (Fig. 1).
Table 2 shows the BET surface area (m2/g), the total pore volume (cm3/g) and the average pore diameter (nm) and the basal distance (d001) of the clay, clay-CPC adsorbent and clay-HDTMA.
At low Ca/Si ratio (< 0.9), the basal distance is close to 13.5 Å.
The basal distance (coalescence) between the two main Pacific lineages, from simple UPGMA averaging, was 1.54% in cyt-b (GTR+I+Γ), i.e. 33% of the interspecies distance.
Note that when C-S-H of the Ca/Si ratio = 1.19 is heated at 473 K for 3 h, the basal distance further reduces to 9.6 Å (Cong & Kirkpatrick, 1995 ▶).
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On heating from ambient temperature to 200 °C, the removal of interlayer water reduced the basal distances to 9.6 Å.
UPGMA basal distances with corresponding TMRCA ages (Time to Most Recent Common Ancestor), based on the operational u=0.75 My-1 lineage-1 site-1 rate.
The 14, 11 and 9 Å distances for tobermorite are schematized in Fig. 4 ▶; because these three basal distances are also observed in C-S-H, the assumption of structural similarity between C-S-H and tobermorite is reinforced.
The ∼ 11 and 14 Å basal distances are also observed in natural tobermorite (Bonaccorsi et al., 2005 ▶; Merlino et al., 2001 ▶), and a ∼ 11 Å variant has also been observed to collapse to 9.6 Å upon heating at 498 K for 3 h (Merlino et al., 1999 ▶).
Flagellum length, inter-basal body distance and basal body positioning relative to the posterior end were measured in bi-flagellated cells with the anti-PFR2 monoclonal antibody L8C4 [22] allowing direct monitoring of PFR2 presence.
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