화학공학소재연구정보센터
Journal of Polymer Science Part B: Polymer Physics, Vol.32, No.15, 2445-2459, 1994
Thermophysical Properties of Azomethine Ether Main-Chain Liquid-Crystalline Polymers at Pressures to 200-MPa
This article reports on an experimental investigation of the equation of state and the transition behavior of main-chain thermotropic liquid crystalline polymers over a wide temperature range, and at pressures to 200 MPa. The materials studied were a series of azomethine ether polymers. A varying number n (= 4, 7, 8, 9, 10 and 11) of methylene spacer units in the backbone provided systematic variation of the structure. Experimental techniques used included high-pressure dilatometry (PVT measurements) to 200 MPa, high-pressure differential thermal analysis, also to 200 MPa, and conventional (atmospheric-pressure) differential scanning calorimetry (DSC). The equation of state of the materials can be well represented by the Tait equation in distinct regions, separated by a glass transition, T-g(P), a first-order transition to a nematic state, T-k-n(P), and a first-order transition to an isotropic melt state T,(P). The atmospheric pressure values of T-k-n and T,decreased with increasing number of spacer units and showed a clear odd-even effect. T, and T-k-n both increased with pressure. The pressure dependence of T, could not be observed due to the onset of degradation in the same temperature region. On isobaric cooling at 3 degrees C/min, the crystallization from the nematic state occurred a few tens of degrees below T-k-n This supercooling was independent of pressure for some materials, while for others it increased with increasing pressure. The values of the enthalpy and entropy associated with the first-order transition into the nematic state were lower than those of typical isotropic polymers at their melting transitions. The transition enthalpy did not have any systematic variation with increasing number of spacer units. Values of the transition enthalpy calculated from the Clapeyron equation did not always agree with the values measured by DSC. This may be due to the two-phase nature of the low-temperature state. At the transition to the isotropic state, the transition enthalpy at P = 0 decreased with n and showed an odd-even effect.