4.7 Article

Delving into the heterocoagulation between coal and quartz at different shear rates by the focused beam reflectance measurement (FBRM) and particle vision and measurement (PVM) techniques

Journal

FUEL
Volume 286, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.fuel.2020.119445

Keywords

Mineral; Heterocoagulation; Shear rate; Slime coating

Funding

  1. Natural Science Foundation of Jiangsu Province [BK20180657]
  2. Priority Academic Program Development of Jiangsu Higher Education Institutions

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This study quantitatively investigated the heterocoagulation in a binary mineral mixture of coal and quartz using experimental systems based on in-situ FBRM and PVM. Results showed that heterocoagulation degree was influenced by shear rates and agitation time.
In the present work, two experimental systems based on in-situ focused beam reflectance measurement (FBRM) and particle vision and measurement (PVM) were developed to quantitatively investigate the heterocoagulation that occurs in a binary mineral mixture consisting of coal and quartz at different shear rates. The former was used to determine the heterocoagulation degree between quartz and coal particles, while the latter was employed to obtain visual information of coagulation behavior of quartz particles on a coal flat surface. The results of the FBRM system obtained at suspension pH varying from 3 to 9 showed that the heterocoagulation degree between quartz and coal particles increased over time. These results also showed that the heterocoagulation degree gradually decreased as the shear rate increased from 30 s(-1) to 68 s(-1) regardless of pH change. The results of the PVM system showed that the effect of agitation time on heterocoagulation between quartz particles and a coal flat surface was similar to that obtained between quartz and coal particles. However, the heterocoagulation between quartz particles and a coal surface was less severe than that between quartz and coal particles and was more sensitive to the change of shear rate.

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