scholarly journals Deposition of ultrananocrystalline diamond at low temperature using CO, CH4 mixed carbon source

2021 ◽  
pp. 100237
Author(s):  
Yi Zeng ◽  
Yukihiro Sakamoto
Author(s):  
Ping Guo ◽  
Weiwei Xu ◽  
Shi Tang ◽  
Binxia Cao ◽  
Danna Wei ◽  
...  

One cold-adapted strain, named Planococcus sp. XW-1, was isolated from the Yellow Sea. The strain can produce biosurfactant with petroleum as sole source of carbon at low temperature (4 °C). The biosurfactant was identified as glycolipid-type biosurfactant species by thin-layer chromatography (TLC) and Fourier transform infrared spectroscopy (FTIR). It reduced the surface tension of water to 26.8 mN/m with a critical micelle concentration measurement of 60 mg/L. The produced biosurfactant possesses high surface activity at wide ranges of temperature (−18–105 °C), pH values (2–12), and salt concentrations (1–18%). The biosurfactant exhibited higher surface activity and higher growth rate of cells with hexadecane and diesel as carbon source. The strain Planococcus sp. XW-1 was also effective in degrading crude oil, after 21 days of growth at 4 °C in medium with 1% crude oil and 1% (v/v) bacteria broth, 54% of crude oil was degraded. The results suggest that Planococcus sp. XW-1 is a promising candidate for use in the bioremediation of petroleum-contaminated seawater in the Yellow Sea during winter. This study reported for the first time that Planococcus isolated from the Yellow Sea can produce biosurfactant using petroleum as the sole carbon source at low temperature (4 °C), showing its ecological role in the remediation of marine petroleum pollution.


2013 ◽  
Vol 37 (3) ◽  
pp. 575-584 ◽  
Author(s):  
Jiushun Zhou ◽  
Menghao Cai ◽  
Tao Jiang ◽  
Weiqiang Zhou ◽  
Wei Shen ◽  
...  

2006 ◽  
Vol 70 (4) ◽  
pp. 397-404 ◽  
Author(s):  
J. González del Tánago ◽  
A. La Iglesia ◽  
A. Delgado

AbstractKamphaugite-(Y) occurs as white to cream-coloured spherical to semi-spherical aggregates of radial crystals in the La Cabrera granitic pluton (Spanish Central System). It mainly occurs on the free surfaces of alkali feldspar, quartz, calcite, kainosite-(Y) and laumontite, and inside miarolitic cavities. La Cabrera kamphaugite-(Y) has an average composition of Ca0.94Y0.89REE0.21(CO3)2 [F0.05(OH)0.95]·1.19H2O. Negative δ13CV-PDB values (–14 to –15‰) indicate a meteoric carbon source. Textural relations between kamphaugite-(Y) and coexisting minerals, its relatively high δ18OV-SMOW values (+25 to +26‰), and the occurrence of laumontite inclusions in kamphaugite-(Y), point to a genesis at < 50°C during very low-temperature post-magmatic hydrothermal activity.


2014 ◽  
Vol 104 (22) ◽  
pp. 229901
Author(s):  
Lin Li ◽  
Jing Zhao ◽  
Zhaosheng Hu ◽  
Baogang Quan ◽  
Junjie Li ◽  
...  

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