MbrlCatalogueTitleDetail

Do you wish to reserve the book?
Raman spectroscopic characterization of cracking and hydrolysis of n-pentane and n-octadecane at 300–375°C with geological implications
Raman spectroscopic characterization of cracking and hydrolysis of n-pentane and n-octadecane at 300–375°C with geological implications
Hey, we have placed the reservation for you!
Hey, we have placed the reservation for you!
By the way, why not check out events that you can attend while you pick your title.
You are currently in the queue to collect this book. You will be notified once it is your turn to collect the book.
Oops! Something went wrong.
Oops! Something went wrong.
Looks like we were not able to place the reservation. Kindly try again later.
Are you sure you want to remove the book from the shelf?
Raman spectroscopic characterization of cracking and hydrolysis of n-pentane and n-octadecane at 300–375°C with geological implications
Oops! Something went wrong.
Oops! Something went wrong.
While trying to remove the title from your shelf something went wrong :( Kindly try again later!
Title added to your shelf!
Title added to your shelf!
View what I already have on My Shelf.
Oops! Something went wrong.
Oops! Something went wrong.
While trying to add the title to your shelf something went wrong :( Kindly try again later!
Do you wish to request the book?
Raman spectroscopic characterization of cracking and hydrolysis of n-pentane and n-octadecane at 300–375°C with geological implications
Raman spectroscopic characterization of cracking and hydrolysis of n-pentane and n-octadecane at 300–375°C with geological implications

Please be aware that the book you have requested cannot be checked out. If you would like to checkout this book, you can reserve another copy
How would you like to get it?
We have requested the book for you! Sorry the robot delivery is not available at the moment
We have requested the book for you!
We have requested the book for you!
Your request is successful and it will be processed during the Library working hours. Please check the status of your request in My Requests.
Oops! Something went wrong.
Oops! Something went wrong.
Looks like we were not able to place your request. Kindly try again later.
Raman spectroscopic characterization of cracking and hydrolysis of n-pentane and n-octadecane at 300–375°C with geological implications
Raman spectroscopic characterization of cracking and hydrolysis of n-pentane and n-octadecane at 300–375°C with geological implications
Journal Article

Raman spectroscopic characterization of cracking and hydrolysis of n-pentane and n-octadecane at 300–375°C with geological implications

2018
Request Book From Autostore and Choose the Collection Method
Overview
Hydrous and anhydrous isothermal experiments on n-pentane and n-octadecane were conducted at 300–375°C for durations up to 1094 h to evaluate the cracking and hydrolysis of hydrocarbons, using fused silica capillary capsules as micro-reactors. The chemical compositions of the gaseous products during cracking of n-octadecane at 350 and 375°C weremethane, ethane, propane, and n-butane. The aqueous product in the hydrolysis of n-pentane and n-octadecane at 300–375°C was alcohol. Alkenes and hydrogen were not detected throughout all the isothermal experiments. Results showed that the gaseous yields were characterized by higher contents of wet gas than those in natural gas accumulations. Mechanisms regulating the enrichment of methane in reservoirs should be further studied. The hydrolysis and oxidation of hydrocarbon were relatively limited in the absence of iron-bearing mineral buffers, suggesting that hydrocarbons might be more stable in iron-poor reservoirs (e.g. carbonate and quartz arenite) than in iron-bearing-mineral-rich ones (e.g. mudstone and arkose) under deep burial conditions. The absence of hydrogen was ascribed to its high diffusion rate in fused silica than in gold tube; any hydrogen produced in the reaction tends to diffuse out of the fused silica capsule with no or limited hydrogen accumulation, similar to those in geological environment. The diffusion of hydrogen should be considered during calculating the volume and pressure changes in the thermal cracking of oil to gas in reservoirs, because the loss of hydrogen would result in a decrease in the conversion rate of oil to gas.