Configuration of Isoprene Structure in Butyl Rubber by Time-Averaging High Resolution Nuclear Magnetic Resonance

1969 ◽  
Vol 42 (2) ◽  
pp. 392-393 ◽  
Author(s):  
Hung Yu Chen ◽  
J. E. Field

Abstract In making butyl rubber, a small amount of isoprene is usually copolymerized with the isobutylene to facilitate vulcanization. The isoprene component thus incorporated in the butyl rubber can be present in three possible configurations, i.e., 1,4-, 1,2-, and 3,4-. The question concerning which of these configurations was the prevalent one in butyl rubber was investigated by Rehner in 1944. His chemical method was based on the fact that only butyl rubber with isoprene units in 1,2- or/and 3,4-configurations would yield formaldehyde and formic acid on ozonization. Since these compounds were not detected in this reaction product, he concluded, indirectly, that the isoprene segment in the butyl rubber was essentially in the 1,4-configuration. In this communication, we would like to report that, by means of a time-averaging high resolution nuclear magnetic resonance method, we are able to observe the absorption peak due to the 1,4-isoprene unit in a typical commercial grade butyl rubber. Since the IR has failed to detect such low concentrations of isoprene in the butyl rubber, the present NMR result seems to be the only direct observation of this structural component. We would also like to point out that such measurements may be useful in determining quantitatively the isoprene unit in butyl rubber as well as other polymers with minor constituents such as the third monomer unit in ethylene propylene terpolymer.

Energies ◽  
2020 ◽  
Vol 13 (2) ◽  
pp. 445 ◽  
Author(s):  
Liu Yang ◽  
Chuanqing Zhang ◽  
Jianchao Cai ◽  
Hongfeng Lu

Field observations show that less than one percent of dissociation water can be produced during gas hydrate production, resulting from spontaneous water imbibition into matrix pores. What’s more, the hydrate sediments are easily dispersed in water, and it is difficult to carry out spontaneous imbibition experiments. At present, there is little research work on the imbibition capacity of hydrate sediments. In this paper, a new method of water imbibition is proposed for hydrate sediments, and nuclear magnetic resonance (NMR) technique is used to monitor water migration. The results show that as the imbibition time increases, the water is gradually imbibed into matrix pores. Water imbibition can cause dramatic changes in pore structure, such as microfracture initiation, fracture network generation and skeleton dispersion. When the imbibition time exceeds a critical value, many secondary pores (new large pores and micro-fractures) start to appear. When imbibition time exceeds the dispersion time, fracture networks are generated, eventually leading to dispersion of the sediment skeleton. The imbibition curves of hydrate sediments can be divided into two linear stages, which corresponds, respectively, to water imbibition of primary pores and secondary pores. The imbibition rate of secondary pores is significantly larger than that of primary pores, indicating that the generation of new fractures can greatly accelerate the imbibition rate. Research on the characteristics of water imbibition in hydrate sediments is important for optimizing hydrate production regime and increasing natural gas production.


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