Upgrading Biocrude of Grindelia Squarrosa to Jet Fuel Precursors by Aqueous Phase Hydrodeoxygenation

2018 ◽  
Vol 6 (9) ◽  
pp. 1832-1843 ◽  
Author(s):  
Xiaokun Yang ◽  
Marcus V. Pereira ◽  
Bishnu Neupane ◽  
Glenn C. Miller ◽  
Simon R. Poulson ◽  
...  
Keyword(s):  
2021 ◽  
Author(s):  
Lulin Wang ◽  
Guangyi Li ◽  
Cong Yu ◽  
Ai-Qin Wang ◽  
Xiaodong Wang ◽  
...  

For the first time, propane-2,2-diyldicyclohexane, a jet fuel range C15 dicycloalkane was directly produced by the aqueous-phase hydrodeoxygenation (APHDO) of polycarbonate (PC). Among the investigated catalyst systems, a mixture of...


2015 ◽  
Vol 17 (12) ◽  
pp. 5131-5135 ◽  
Author(s):  
Hongliang Wang ◽  
Hao Ruan ◽  
Haisheng Pei ◽  
Huamin Wang ◽  
Xiaowen Chen ◽  
...  

A New Lignin BioJet: Jet fuel-range hydrocarbons (C7–C18) can be produced directly from biomass-derived lignin by selective C–O–C bond cleavage and simultaneous hydrodeoxygenation using combinations of noble metal catalysts (Ru/Al2O3) and acidic zeolites (H+-Y) in the aqueous phase.


Water ◽  
2020 ◽  
Vol 12 (2) ◽  
pp. 334
Author(s):  
Elias Hideo Teramoto ◽  
Hung Kiang Chang

Accidental leakage of hydrocarbons is a common subsurface contamination scenario. Once released, the hydrocarbons migrate until they reach the vicinity of the uppermost portion of the saturated zone, where it accumulates. Whenever the amplitude of the water table fluctuation is high, the light non-aqueous phase liquid (LNAPL) may be completely entrapped in the saturated zone. The entrapped LNAPL, comprised of multicomponent products (e.g., gasoline, jet fuel, diesel), is responsible for the release of benzene, toluene, ethylbenzene, and xylenes (BTEX) into the water, thus generating the dissolved phase plumes of these compounds. In order to estimate the time required for source-zone depletion, we developed an algorithm that calculates the mass loss of BTEX compounds in LNAPL over time. The simulations performed with our algorithm provided results akin to those observed in the field and demonstrated that the depletion rate will be more pronounced in regions with high LNAPL saturation. Further, the LNAPL depletion rate is mostly controlled by flow rate and is less sensible to the biodegradation rate in the aqueous phase.


1981 ◽  
Vol 11 ◽  
Author(s):  
M.H. Bradbury ◽  
D. Lever ◽  
D. Kinsey

One of the options being considered for the disposal of radioactive waste is deep burial in crystalline rocks such as granite. It is generally recognised that in such rocks groundwater flows mainly through the fracture networks so that these will be the “highways” for the return of radionuclides to the biosphere. The main factors retarding the radionuclide transport have been considered to be the slow water movement in the fissures over the long distances involved together with sorption both in man-made barriers surrounding the waste, and onto rock surfaces and degradation products in the fissures.


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