TY - JOUR
T1 - Large electric fields due to industrial chimney stack plumes
AU - Jones, C. D.
AU - Jennings, S. G.
PY - 1977
Y1 - 1977
N2 - Large values of electric field due to a charged plume from an industrial chimney stack have been observed. Downwind and crosswind profiles of the electric field were measured using 4 field mills. Average values of between 5 and 6 kV m-1 over 10 minute periods were measured at distances within 200 m of the stack. Electric field values as large as 3.5 kV m-1 were present at a distance of 3 km from the stack. It was found that the electric field did not return to its normal fair-weather value until the downwind distance from the stack had exceeded 9 km. The decrease in the average value of the electric field, Ep, under the plume gave good agreement with an equation derived from line charge theory, modified by an empirical decay factor exp(-R/D) Ep = -λexp(- R D)/2πε{lunate}0h.[1+ R √h2+R2] where λ is the charge per unit length, h the plume height, R the distance of the position P downwind, and D the distance at which λ is reduced by 1 e. The experimental results yielded a value for D of about 1.5 km. Point discharge currents as large as 3 μA were measured at a distance of 700 m from the stack. Measurements at heights ranging from 9.25 m to 3.25 m agreed with the theoretical relation i = k(E-E0) where E is the measured value of electric field at a distance 10 m upwind from the discharge point, E0 the critical value of electric field above which point discharge will occur and k is a constant. Values of E0 of about 2kV m-1 were found for the two highest points. The results suggest that electric field measurements may be a valuable supplement to concentration data in atmospheric diffusion experiments using charged plumes.
AB - Large values of electric field due to a charged plume from an industrial chimney stack have been observed. Downwind and crosswind profiles of the electric field were measured using 4 field mills. Average values of between 5 and 6 kV m-1 over 10 minute periods were measured at distances within 200 m of the stack. Electric field values as large as 3.5 kV m-1 were present at a distance of 3 km from the stack. It was found that the electric field did not return to its normal fair-weather value until the downwind distance from the stack had exceeded 9 km. The decrease in the average value of the electric field, Ep, under the plume gave good agreement with an equation derived from line charge theory, modified by an empirical decay factor exp(-R/D) Ep = -λexp(- R D)/2πε{lunate}0h.[1+ R √h2+R2] where λ is the charge per unit length, h the plume height, R the distance of the position P downwind, and D the distance at which λ is reduced by 1 e. The experimental results yielded a value for D of about 1.5 km. Point discharge currents as large as 3 μA were measured at a distance of 700 m from the stack. Measurements at heights ranging from 9.25 m to 3.25 m agreed with the theoretical relation i = k(E-E0) where E is the measured value of electric field at a distance 10 m upwind from the discharge point, E0 the critical value of electric field above which point discharge will occur and k is a constant. Values of E0 of about 2kV m-1 were found for the two highest points. The results suggest that electric field measurements may be a valuable supplement to concentration data in atmospheric diffusion experiments using charged plumes.
UR - http://www.scopus.com/inward/record.url?scp=0017706854&partnerID=8YFLogxK
U2 - 10.1016/0004-6981(77)90096-8
DO - 10.1016/0004-6981(77)90096-8
M3 - Article
AN - SCOPUS:0017706854
SN - 0004-6981
VL - 11
SP - 1197
EP - 1207
JO - Atmospheric Environment (1967)
JF - Atmospheric Environment (1967)
IS - 12
ER -