We analyse cross-wind-integrated statistics of the concentration field of a
conserved scalar for point and line sources in grid turbulence. In particu
lar, using wind-tunnel measurements we calculate the cross-wind integrated
probability density function (pdf) for the scalar concentration. We then us
e that quantity in the exact evolution equation for the pdf to calculate th
e cross-wind integrated mean of the rate of dissipation of scalar variance,
conditional on the scalar concentration. Much of the variation of these st
atistics with distance downstream is accounted for by scaling with concentr
ation, length and time scales based on the development of the mean plume. T
his scaling thus suggests some simple practical parameterisations of these
statistics in terms of mean-field quantities. One of the motivations for th
is work is to find a simple parameterisation for the scalar dissipation tha
t can be used for modelling chemical reactions in plumes.
We also consider the cross-wind integral of the first few moments of the co
ncentration field and show that the integration greatly simplifies the budg
ets for these moments. Thus the first moment is just the downstream flux of
the scalar, which is constant. The second moment budget provides a check o
n the mean dissipation estimated directly from the pdf evolution equation.