用250 MHz核磁共振弛豫仪和扩散仪研究水化玉米茎秆和大麻茎秆的长期水分迁移

IF 2.624
Matthew C. Young , Sarah L. Codd , Joseph D. Seymour
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引用次数: 0

摘要

植物纤维是目前生物复合材料的研究热点,已知植物纤维的亲水性,如玉米茎秆和大麻茎秆,需要进一步了解水对纤维结构的影响。利用核磁共振(NMR) T2弛豫仪和扩散仪将水化过程中这些纤维中的水分分布与纤维纤维素介质进行比较。从3-237 h每6 h测量一次,或直到平衡。核磁共振T2测量了两种水化水的结合层、中间结合层和大孔隙水的数量。核磁共振扩散测量法测量了每种物质中可移动水种群的扩散系数D。得到扩散系数D作为分子迁移时间的函数Δ来检测受限扩散。D(Δ)的行为表明,在高度饱和的大麻中,孔间连通性增加,而在饱和的髓中,孔肿胀。D(Δ)值适合于表面体积比S/V,以确定平均孔隙半径r作为水化的函数。将S/V值与T2分布配对,以提供水化过程中有效的平均横向磁表面弛豫率ρ´2,然后将其用于将T2分布重新缩放为孔径分布。1μm孔隙中存在束缚水,1 ~ 30μm孔隙中存在半束缚水,30 ~ 300μm孔隙中存在大孔隙水,与文献一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Long-term water migration in hydrated corn stalk pith and hemp stalk by 250 MHz NMR relaxometry and diffusometry

Long-term water migration in hydrated corn stalk pith and hemp stalk by 250 MHz NMR relaxometry and diffusometry
Plant fibers are of current interest in biocomposites and known hydrophilicity of plant fibers, e.g. corn stalk pith and hemp stalk, require enhanced understanding of water impacts on fiber structure. Water distribution during hydration in these fibers is compared to fibrous cellulose media using nuclear magnetic resonance (NMR) T2 relaxometry and diffusometry. Measurements were made every 6 h from 3237 h, or until equilibrium. NMR T2 measured bound, intermediate bound and macropore water populations at two water mass hydrations. NMR diffusometry measured diffusion coefficients D of mobile water populations in each material. The diffusion coefficient D was acquired as a function of molecular migration time Δ to detect restricted diffusion. D(Δ) behavior indicated increased interpore connectivity in highly saturated hemp, versus swollen pores saturated pith. D(Δ) values were fit for surface to volume ratio S/V to determine average pore radius r as a function of hydration. S/V values were paired to T2 distributions to provide an effective average transverse magnetic surface relaxivity ρ̄2 throughout hydration, which is then used to rescale T2 distributions as pore size distributions. Bound water was found in pores <1μm, semi-bound water in pores from 130μm and macropore water in pores from 30300μm, in agreement with prior literature.
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CiteScore
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