首页> 外文期刊>Journal of Agricultural and Food Chemistry >Mechanisms of Water Interaction with Pore Systems of Hydrochar and Pyrochar from Poplar Forestry Waste
【24h】

Mechanisms of Water Interaction with Pore Systems of Hydrochar and Pyrochar from Poplar Forestry Waste

机译:杨树林业废弃物中水与焦炭和毛孔孔隙系统水相互作用的机理

获取原文
获取原文并翻译 | 示例
       

摘要

The aim of this study was to understand the water—surface interactions of two chars obtained by gasification (pyrochar) and hydrothermal carbonization (hydrochar) of a poplar biomass. The two samples revealed different chemical compositions as evidenced by solid state ~(13)C NMR spectroscopy. In fact, hydrochar resulted in a lignin-like material still containing oxygenated functionalities. Pyrochar was a polyaromatic system in which no heteronuclei were detected. After saturation with water, hydrochar and pyrochar were analyzed by fast field cycling (FFC) NMR relaxometry. Results showed that water movement in hydrochar was mainly confined in very small pores. Conversely, water movement in pyrochar led to the conclusion that a larger number of transitional and very large pores were present. These results were confirmed by porosity evaluation derived from gas adsorption. Variable-temperature FFC NMR experiments confirmed a slow-motion regime due to a preferential diffusion of water on the solid surface. Conversely, the higher number of large pores in pyrochar allowed slow movement only up to 50 °C. As the temperature was raised to 80 °C, water interactions with the pore surface became weaker, thereby allowing a three-dimensional water exchange with the bulk liquid. This paper has shown that pore size distribution was more important than chemical composition in affecting water movement in two chemically different charred systems.
机译:这项研究的目的是了解通过杨木生物质的气化(焦炭)和水热碳化(水炭)获得的两种炭在水-表面的相互作用。固态〜(13)C NMR光谱证明这两个样品显示出不同的化学组成。实际上,水焦炭导致木质素样材料仍然含有氧化功能。焦炭是一种多芳族体系,其中未检测到杂核。用水饱和后,通过快速场循环(FFC)NMR弛豫法分析水碳和焦碳。结果表明,水在炭中的运动主要局限在很小的孔中。相反,焦炭中的水运动得出结论,存在大量的过渡孔和非常大的孔。这些结果通过源自气体吸附的孔隙率评估得到证实。可变温度FFC NMR实验证实,由于水在固体表面上的优先扩散,因此存在慢速运动。相反,焦炭中较大的大孔数量仅允许缓慢移动直至最高50°C。当温度升至80°C时,与孔隙表面的水相互作用变弱,从而允许与本体液体进行三维水交换。本文表明,在两个化学不同的烧焦系统中,孔径分布比化学成分对影响水的流动更为重要。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号