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the coking properties of coal at elevated pressures. - Argonne ...

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BED AGGLOMERATES FORMED BY ATMOSPHERIC FLUIDIZED<br />

BED COMBUSTION OF A NORTH DAKOTA LIGNITE<br />

Steven A. Benson, Frank R. Karner, and Gerald M. Goblirsch<br />

Grand Forks Energy Technology Center<br />

U.S. Department <strong>of</strong> Energy<br />

Grand Forks, North Dakota 58202<br />

David W. Brekke<br />

Department <strong>of</strong> Geology<br />

University <strong>of</strong> North Dakota<br />

Grand Forks, North Dakota 58202<br />

INTRODUCTION<br />

The goal <strong>of</strong> <strong>at</strong>mospheric fluidized bed combustion (AFBC) research <strong>at</strong> <strong>the</strong><br />

Grand Forks Energy Technology Center is to provide a d<strong>at</strong>a base for design, opera-<br />

tion, process control, and emission control requirements for low-rank <strong>coal</strong>s. The<br />

applic<strong>at</strong>ion <strong>of</strong> <strong>the</strong> AFBC process has <strong>the</strong> potential to solve some <strong>of</strong> <strong>the</strong> problems<br />

associ<strong>at</strong>ed with conventional combustion. These problems are .ash fouling on he<strong>at</strong><br />

exchange surfaces, <strong>the</strong> expense and reliability <strong>of</strong> SO2 control devices such as<br />

scrubbers, and <strong>the</strong> system sensitivity to fuel variables (moisture, Na20 concentra-<br />

tion, etc.).<br />

These problems can be reduced by <strong>the</strong> AFBC process for low-rank <strong>coal</strong>s be-<br />

cause <strong>the</strong> alkaline characteristics <strong>of</strong> <strong>the</strong> ash or sorbent added directly to <strong>the</strong> com-<br />

bustion zone provides <strong>the</strong> sulfur retention, which would elimin<strong>at</strong>e or reduce <strong>the</strong><br />

need for post combustion SO2 controls. The temper<strong>at</strong>ures in <strong>the</strong> combustion zone<br />

are <strong>at</strong> <strong>the</strong> right levels to provide maximum reaction <strong>of</strong> SO2 and alkali to form solid<br />

alkali sulf<strong>at</strong>e waste. One problem which <strong>the</strong> fluidized bed combustion <strong>of</strong> low-rank<br />

<strong>coal</strong>s seems to exhibit is a tendency toward <strong>the</strong> form<strong>at</strong>ion <strong>of</strong> agglomer<strong>at</strong>es <strong>of</strong> <strong>the</strong><br />

m<strong>at</strong>erial which are used to make up <strong>the</strong> bed. Agglomer<strong>at</strong>es in this case are defined<br />

as a cluster <strong>of</strong> individual bed m<strong>at</strong>erial particles held toge<strong>the</strong>r by a substance not<br />

yet well understood, and manifest in many differing forms. The understanding <strong>of</strong><br />

<strong>the</strong> mechanism <strong>of</strong> form<strong>at</strong>ion <strong>of</strong> <strong>the</strong>se agglomer<strong>at</strong>es is vital to <strong>the</strong>ir control, and <strong>the</strong>re-<br />

fore <strong>the</strong> full utiliz<strong>at</strong>ion <strong>of</strong> low-rank <strong>coal</strong> in AFBC.<br />

Once formed <strong>the</strong>se agglomer<strong>at</strong>es will tend to decrease he<strong>at</strong> transfer, and fluidi-<br />

z<strong>at</strong>ion quality resulting in poor combustion efficiency and loss <strong>of</strong> control <strong>of</strong> bed oper-<br />

<strong>at</strong>ional parameters (i.e., excess air, temper<strong>at</strong>ure, etc.). In severe cases <strong>the</strong> forma-<br />

tion <strong>of</strong> agglomer<strong>at</strong>es can lead to a forced prem<strong>at</strong>ure shutdown <strong>of</strong> <strong>the</strong> system.<br />

While <strong>the</strong> addition <strong>of</strong> limestone, or calcium bearing m<strong>at</strong>erials into <strong>the</strong> fluid bed,<br />

or <strong>the</strong> forming <strong>of</strong> <strong>the</strong> bed itself by limestone particles has shown a tendency to in-<br />

hibit <strong>the</strong> form<strong>at</strong>ion <strong>of</strong> agglomer<strong>at</strong>es, agglomer<strong>at</strong>es <strong>of</strong> a severe n<strong>at</strong>ure have been ob-<br />

served in a bed <strong>of</strong> limestone alone, or limestone and sand particle mixtures while<br />

burning a high sodium <strong>coal</strong> for an extended period <strong>of</strong> time.<br />

In general with a high sodium <strong>coal</strong> <strong>the</strong> agglomer<strong>at</strong>ion <strong>of</strong> limestone bed m<strong>at</strong>erial<br />

is dependent only on <strong>the</strong> length <strong>of</strong> run time, if <strong>the</strong> run is long enough agglomera-<br />

tion in a limestone bed will occur, and can be as devast<strong>at</strong>ing as those which occur<br />

with a silica bed.<br />

174

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