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Volcanic rocks in western China are dominated by meso-basic rocks, such as the Permian Formation in the Tarim Basin, Carboniferous Batamayineishan Formation in the Junggar Basin and Permian Jiamuhe Formation in the Tuha Basin and the Carboniferous-Permian system in the Santanghu Basin (Fig. 1) (Zhou et al. 2010; Zhang et al. 2013a, b).
Q 1 is calculated according to Eq. (1) (Zhou and Lin 1999): Q_{1} = 2uppi{it d}alpha_{1} lambda_{1} frac{{p_{text{m}}^{2} - p_{1}^{2} }}{{1440ln left( {R_{1} /R} right)}} (1 where R 1 is the radius of the gas extraction area of the overlying coal seam, m, and α 1 is the flow correction coefficient for gas extraction from the overlying coal seam.
The differences between the two studies were as follows: (1) Zhou used fMRI, but we used PET; and (2) Zhou studied humans, but we studied rats.
Quantitative polymerase chain reaction (qPCR) primers were either designed using Eurofins online primer design software (www.eurofinsdna.com) or were identified from previous publications (Supplementary Table 1) (Zhou et al., 2003).
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The current results provide a direct experimental evidence that distributed reactions can be a common combustion mode along with the results (Ref. [1], Zhou et al., 2015) recently reported in the highly turbulent premixed jet flames.
"Wow, this is a 2.5!" Zhou exclaimed.
"It does not matter whether we will end up at stage 3," Zhou wrote to me in an e-mail.
8. Zhou 1, a wool-and-silk needlepoint design from Tai Ping's Fret Collection, is made to order; $81 a square foot from Tai Ping, 860 Broadway (17th Street), (212) 979-2123.
Halophilic strain Thalassospira sp. SL5-1 (Zhou et al. 2016) has been identified to degrade pyrene through both gentisic acid and o-phthalic acid.
This metabolite was identified as TMS-derivatized o-phthalic acid and was also detected in the phenanthrene-degrading process by Thalassospira sp. TSL5-1 (Zhou et al. 2016).
Greater Cr concentrations in pre- (mean 1.58 mg L−1) and post-monsoon (1.08 mg L−1) were recorded to those from Hong Kong (0.001 0.059 mg g−1) (Zhou et al. 2007).
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