abstract:Mill Inlet () is an ice-filled inlet which recedes in a northwesterly direction and is some wide at its entrance between Cape Robinson and Monnier Point, along the east coast of Graham Land, Antarctica. It was charted by the Falkland Islands Dependencies Survey in 1947 and named for Hugh Robert Mill.
The paper presents the internal structures and performance featuresof thefluidized bed opposed jetmill based onthe jet nozzlesstructure, impellertypes, feedinginletandbottomstructure.