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Post-Grenvillian cooling of Marble Domain rocks through 500 °C nearly 200 m.y. after cooling of the Quartzite Domain suggests a protracted middle crustal residence of the Marble domain under thermally elevated conditions, implying that portions of the orogenic lid remained warm (above 500 °C) during the Grenville orogeny.
The formation of silver sulfide can occur at both room temperature [15] and elevated conditions.
Although the correlations between porosity and strength for several engineering materials have been intensively investigated, its pertinence to the Class G oilwell cement under elevated conditions still needs to be carefully examined.
Further, given that NMR relaxation is readily extended to measurements at elevated conditions of temperature and pressure, these results suggest that the technique might be considered a useful addition to the toolkit of techniques employed to characterise adsorption in porous media used for applications in catalysis and separations processes.
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A yellow alert would reflect an "elevated condition" and "significant risk" of a terrorist strike.
However, its pertinence to the Class G oilwell cement under an elevated condition still needs to be examined.
These phenomena were already apparent under elevated CO2 conditions (5%, high CO2, HC), and were enhanced under the low-CO2-availability conditions of ambient air (∼0.035%, low CO2, LC) [14], [15].
For example, a complementary acclimatization of photosynthesis in water stressed rice growth under elevated CO2 conditions has been reported, despite an increased rate of net leaf photosynthesis under these same conditions ([Imai and Murata 1978]; [Makino et al., 1997]).
Previous studies have reported that net photosynthesis almost always increases for plants under elevated CO2 conditions, but the extent and duration of this enhancement varies with plant species and interacting environmental conditions.
This extreme situation typically occurs with maritime aerosols under elevated humidity conditions.
In contrast TOC from root exudates decreased significantly with elevated CO2 conditions.
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