Changes in oxygen uptake kinetics after exercise caused by differences in loading pattern and exercise intensity by Yuri Ichikawa, Tomoko Maeda, Tetsuya Takahashi, Kohei Ashikaga, Shiori Tanaka, Yuki Sumi, Haruki Itoh

“…In all RTs, subjects began exercise by warming up (20 W). In CT, T1/2 was significantly lengthened as exercise intensity increased (CT‐low: 34.0 ± 3.9 s, CT‐moderate: 39.5 ± 3.5 s, CT‐high:44.6 ± 4.2 s; P < 0.01, ANOVA), whereas no significant change was observed in RT, which began with the same work rate (RT‐low: 46.0 ± 5.7 s, RT‐moderate: 45.7 ± 4.8 s, RT‐high: 44.6 ± 3.5 s, RT‐max: 44.8 ± 3.2 s; P = 0.868, ANOVA). …”
Get full text

Solid and Gaseous Methane in IRAS 23385+6053 as Seen with Open JWST Data by Ruslan Nakibov, Varvara Karteyeva, Igor Petrashkevich, Maksim Ozhiganov, Mikhail Medvedev, Anton Vasyunin

“…We were able to describe the wide feature of solid methane with the following laboratory spectra: CH _4 : CO _2 = 1 : 5 (at $27.{4}_{-10.8}^{+6.0}$ K) and CH _4 : H _2 O = 1 : 10 (at $8.{4}_{-1.7}^{+16.4}$ K) deposited at 6.7 K and warmed up at a rate of 0.5 K per minute. The derived column densities are ${N}_{{\,\rm{CH}\,}_{4}}$ (CO _2 ) = $2.9{7}_{-0.57}^{+0.37}\times 1{0}^{17}$ cm ^−2 and ${N}_{{\,\rm{CH}\,}_{4}}$ (H _2 O) = $1.0{2}_{-0.27}^{+0.46}\times 1{0}^{17}$ cm ^−2 . …”
Get full text