Skip to content

Commit 397d75b

Browse files
authored
Merge pull request #15725 from rmcdermo/master
FDS Validation Guide: correct section labels for Plume Height and Eva…
2 parents ee77a7b + 92c7a92 commit 397d75b

File tree

2 files changed

+2
-1
lines changed

2 files changed

+2
-1
lines changed

Manuals/FDS_Validation_Guide/Species_Chapter.tex

Lines changed: 1 addition & 0 deletions
Original file line numberDiff line numberDiff line change
@@ -958,6 +958,7 @@ \subsection{NIST Soot Deposition Gauge Experiments}
958958
\clearpage
959959

960960
\section{Droplet Evaporation}
961+
\label{Evaporation Rate}
961962

962963
This section presents the results of simulations of liquid droplet evaporation experiments. The titles of the sections below are named for the experimentalists.
963964

Manuals/FDS_Validation_Guide/Wind_Chapter.tex

Lines changed: 1 addition & 1 deletion
Original file line numberDiff line numberDiff line change
@@ -256,7 +256,7 @@ \section{LNG Dispersion Experiments}
256256
\clearpage
257257

258258
\section{Stack Emission Plume Rise}
259-
\label{Plume_Height_Discussion}
259+
\label{Plume Height}
260260

261261
A common exercise in atmospheric dispersion modeling is predicting the plume rise height of stack emissions. In an example given by Stull~\cite{Stull:2000}, a $z_{\rm s}=75$~m stack emits SO$_2$ at a rate of 250~g/s with an exit velocity of $W_0=20$~m/s and temperature of $\Delta T=180$~K above ambient ($T_0=293$~K) through an orifice with radius $R_0=2$~m. The wind speed is $U=5$~m/s. Three cases are considered where the atmosphere is stably stratified with temperature gradients, $\d T/\d z$, of -4.8, -8.8 and 5.2~K/km. The expected equilibrium height is given by the empirical expression:
262262
\be

0 commit comments

Comments
 (0)